Page
    1
    STATE OF ILLINOIS
    )
    RECEIVED
    CLERKS
    OFFICE
    COUNTY
    OF C 0 0 K
    )
    FEB
    27
    2009
    STATE
    OF
    IWNOIS
    ILLINOIS POLLUTION
    CONTROL BO”
    ControIBoar
    February 17, 2009
    IN
    THE
    MATTER OF:
    WATER QUALITY STANDARDS AND
    )
    R08-9
    EFFLUENT LIMITATIONS
    FOR THE
    CHICAGO AREA WATERWAY SYSTEM
    AND
    )
    (Rulemaking -
    LOWER DES PLAINS RIVER PROPOSED
    )
    Water)
    AMENDMENTS TO
    35
    ILL. ADM.
    CODE
    301, 302, 303, and 304
    TRANSCRIPT
    OF PROCEEDINGS held in the
    above-entitled
    cause
    before Hearing
    Officer
    Marie
    Tipsord, called by the Illinois Pollution
    Control
    Board, pursuant
    to
    notice,
    taken before Rebecca
    Graziano, CSR, within and for the
    County of Cook
    and
    State of Illinois, at the Thompson Center, 100
    West
    Randolph, Room 2-025,
    Chicago,. Illinois, on the
    17th
    Day of February, A.D., 2009,
    commencing
    at
    10:00
    a.m.
    .

    Page 2
    1
    APPEARANCES
    2
    ILLINOIS POLLUTION CONTROL BOARD:
    3
    Ms. Marie Tipsord, Hearing
    Officer
    4
    Ms. Alisa Liu, P.E., Environmental
    Scientist
    Dr.
    Tanner Girard, Acting Chairman
    5
    Mr. Anand Rao
    Mr. Thomas Johnson
    6
    Dr. Shundar
    Lin
    Ms. Andrea Moore
    7
    8
    ILLINOIS ENVIRONMENTAL
    PROTECTION AGENCY:
    9
    Ms. Stefanie Diers
    Ms. Deborah Williams
    10
    Mr. Robert Sulski
    Mr.
    Scott
    Twait
    11
    Mr. Roy Smogor
    12
    ENVIRONMENTAL LAW AND POLICY CENTER:
    13
    Ms. Jessica Dexter
    14
    METROPOLITAN
    WATER RECLAMATION DISTRICT OF
    15
    GREATER CHICAGO:
    Mr. Fredric Andes
    16
    Mr. Marcelo Garcia
    17
    18
    19
    20
    21
    22
    23
    24

    Page 3
    1
    MS.
    TIPSORD:
    Good morning.
    My name
    2
    is
    Marie Tipsord, and
    I’ve been appointed
    by
    the
    3
    Board to
    serve
    as
    hearing officer in this procedure
    4
    entitled
    Water Quality Standards and
    Effluent
    5
    limitations
    for the Chicago
    Area Waterway System and
    6
    Lower Des Plaines
    River Proposed Amendments
    to
    35
    7
    Ill. Adm. Code
    301, 302, 303, and 304. The
    docket
    8
    number
    is R08-9.
    9
    With me today to
    my left is acting
    10
    chairman,
    G. Tanner
    Girard, the presiding Board
    11
    Member. To his
    immediate left is Board Member
    12
    Andrea
    Johnson -- Andrea
    Moore, and
    to
    her left is
    13
    Board Member Dr.
    Shundar Lin. To my far right is
    14
    Board Member
    Thomas Johnson.
    To my
    immediate right
    15
    is
    Anand Rao, and to
    his right, Alisa Liu from our
    16
    technical staff.
    In addition,
    today
    we have
    Brian
    17
    Lambel,
    who is our etern this semester
    from Kent.
    18
    This
    is the ninth
    set
    of hearings
    19
    to be
    held in
    this proceeding, and I
    believe we’re
    20
    on days
    24 and 25. The purpose of today’s
    hearing
    21
    is to
    continue hearing
    testimony from the
    22
    participants,
    other than the proponent, the Illinois
    23
    Environmental
    Protection Agency. At
    the close of
    24
    hearing
    on December 3rd,
    2009, we had finished with

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    Page
    5
    1
    preconceived notion or bias. We will
    go
    until
    2
    around 5:00 p.m.
    today
    with
    a
    lunch break, and then
    3
    we’ll start again tomorrow morning
    at
    9:00 a.m.
    4
    Also, I have heard from some of
    5
    you about
    future
    dates, and at this time, I plan
    to
    6
    continue
    this hearing on the record.
    The
    plan
    was
    7
    to go
    for March 3rd and 4th. I have rooms in the
    8
    building across the street and here, and
    lTd
    like
    to
    9
    finish the witnesses from the District
    at that time.
    10
    Mr.
    Andes,
    you
    indicated before we went
    on
    the
    11
    record that those
    days
    might not work for the
    12
    District?
    13
    MR. ANDES: I believe that’s right,
    14
    but
    I will
    get
    back
    to
    you later today
    to
    nail that
    15
    down.
    16
    MS. TIPSORD: All right.
    Because my
    17
    intent,
    fraiikly,
    at
    this point is if the District is
    18
    not
    available, then I would
    be
    inclined
    to, since we
    19
    have rooms for those
    days,
    move ahead and come back
    20
    to
    the District when they
    are
    available. Because of
    21
    the
    difficulty
    of
    the scheduling that I’ve already
    22
    seen from the IEPA and others, that would, sort of
    23
    -- I would, kind of, like to try
    to do
    that. So if
    24
    you
    could
    get back to
    me later in the
    day,
    that

    Page 6
    1
    would
    be
    very helpful.
    2
    MR. ANDES:
    I will.
    3
    MS. TIPSORD:
    So I can give notice
    to
    4
    whoever else can
    be available on those
    days.
    Thank
    5
    you.
    6
    I also received
    a motion from Corn
    7
    Products seeking
    to
    withdraw their testimony of
    both
    8
    James Huff and Alan
    Gerick (phonetic). I think
    9
    they’re going
    to
    withdraw and
    then re-file. I
    10
    didn’t, frankly, read the motion.
    I just saw it and
    11
    I spoke briefly with Katherine Huff. Citgo also,
    in
    12
    conversations with Jeff Ford,
    would also like
    to,
    13
    perhaps, amend their testimony with some
    additional
    14
    information.
    15
    Given this
    -- these, sort
    of,
    16
    developments, and given that it has been awhile
    17
    since
    we’ve
    talked about the schedule,
    as
    far
    as who
    18
    would
    be
    testifying next and where
    we’re going, I
    19
    would like
    to
    schedule
    a
    pre-hearing conference for
    20
    -- I picked
    February
    27th, which is
    a
    week from
    21
    Friday. If people can’t
    be available that day, we
    22
    can
    do
    it the afternoon of the 26th. But check
    your
    23
    calendars and
    get
    back with me, and I will
    put a
    24
    hearing
    officer
    order out on Thursday reflecting the

    Page 7
    1
    additional hearings and the pre-hearing conference,
    2
    which would talk
    about
    where we’re going, who we’re
    3
    proceeding with, and
    based
    on an email I
    got
    from
    4
    Ms. Dexter,
    too,
    I also understand that the
    5
    environmental groups might want
    to
    decide what order
    6
    their witnesses are
    presented as
    well.
    7
    So that will
    be
    what we’ll talk
    8
    about.
    We’ll talk
    about
    who’s going next, where
    9
    we’re
    going, after we’re
    finished with the District.
    10
    MS.
    DEXTER:
    Did
    you
    say,
    Marie, that
    11
    those would
    be
    in the afternoon on either of those
    12
    dates,
    or at any time?
    13
    MS. TIPSORD:
    It could
    be at
    any
    time
    14
    during the
    day
    on the 27th and the afternoon of the
    15
    26th. It
    would have
    to be
    the afternoon of the
    26th
    16
    because
    we have
    a
    closed session in the morning.
    17
    MS. DEXTER:
    All right.
    Thanks.
    18
    MS. TIPSORD:
    So I
    won
    Tt
    be available
    19
    until afternoon until the 26th. And with that, Dr.
    20
    Girard.
    21
    DR. GIRARD:
    Thank
    you.
    Good
    morning.
    22
    On
    behalf of the Board, I welcome everyone
    to
    23
    another
    set
    of hearings in this rulemaking. The
    24
    Board is very grateful
    for
    the amount of
    time
    and

    Page 8
    1
    effort that everyone is putting into both preparing
    2
    testimony and also preparing questions and
    3
    continuing the questions in
    the
    cross
    examination
    of
    4
    the
    hearings. It helps
    us
    immensely in putting
    5
    together a
    record, especially in these
    days
    of,
    you
    6
    know, lean governmental
    budgets
    and lean staffing.
    7
    We really do need the help, so we appreciate
    8
    everything
    you’re doing. We realize this is
    a
    very
    9
    extensive
    rulemaking,
    but
    this,
    you
    know, is
    a
    very
    .10
    complicated
    topic.
    So
    we look forward
    to
    the
    11
    testimony and questions today.
    Thank
    you.
    12
    MS. TIPSORD:
    And with that, Mr.
    13
    Andes, I think we’re ready to
    swear in
    your witness.
    14
    (Witness sworn.)
    15
    MR. ANDES:
    This is a
    copy
    of
    16
    Dr. Garcia’s
    testimony.
    17.
    MS. TIPSORD: And it is Dr. Garcia?
    18
    DR. GARCIA:
    Yes.
    19
    MS.
    TIPSORD:
    Just
    wanted
    to
    check.
    20
    DR. GARCIA:
    Yes,
    yes.
    21
    MS. TIPSORD: And you’re going to have
    22
    to
    speak
    up.
    I can tell already.
    They’re not
    going
    23
    to be
    able
    to
    hear
    you
    in the back of the room.
    24
    DR. GARCIA: Don’t worry about that.

    Page
    9
    1
    MS. TIPSORD: If there’s no objection,
    2
    we will mark the pre-filed testimony of Dr. Garcia
    3
    as
    Exhibit 139. Seeing none, the testimony and
    4
    attachments are
    marked
    as Exhibit 193.
    Thank
    you.
    5
    And I believe the Agency had pre-filed some
    6
    questions.
    7
    MS. DIERS:
    Yes.
    Good morning, Dr.
    8
    Garcia.
    My name is Stephanie Diers,
    and
    ITil
    be
    9
    asking questions on behalf of Illinois EPA, and I’ll
    10
    begin with our pre-filed question one. How might
    11
    density occurrence affect water quality and
    12
    transport little oxygen, sediment laden water,
    and
    13
    contaminants for long distance? And I think this
    14
    refers
    to
    on Page
    3
    of your pre-filed testimony.
    15
    DR. GARCIA:
    Right.
    Okay.
    Let me
    16
    first explain
    what
    is a density current. A density
    17
    flow is
    a
    name given
    to a
    flow that happens when
    you
    18
    have differences in density between two fluids.
    So
    19
    the best and
    simplest way
    to
    imagine this,
    imagine
    a
    20
    lake, and imagine that
    you go
    through the winter,
    21
    and all of
    a
    sudden spring comes along, and there’s
    22
    no
    -- and
    all
    the
    water
    -- all the runoff finds
    its
    23
    way into the river, and eventually the water in the
    24
    river flows into the lake.

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    Page
    13
    1
    current once it reaches the basin in the south
    2
    branch.
    3
    We have modeled that. We have
    a
    4
    paper that is going
    to be
    presented
    at a
    conference
    5
    in May
    in Kansas
    City. We will
    be
    happy
    to
    share
    6
    copies with
    you
    with my students,
    and
    what we
    see is
    7
    that, indeed --
    8
    MR. ANDES: Actually, should we
    -- do
    9
    you
    want
    to use
    the chart?
    10
    DR. GARCIA:
    Yeah,
    sure.
    11
    MR. ANDES:
    Okay.
    Well, I think
    you
    12
    have
    one here.
    I
    can pass them
    out.
    13
    DR. GARCIA:
    Yeah.
    We -- I had made
    a
    14
    poster,
    which
    was -- the idea was
    to be
    able
    to
    show
    15
    it
    to you, but
    last night I was trying
    to
    catch
    a
    16
    train and the poster --
    17
    MR.
    ANDES:
    Well, let me take those.
    18
    DR. GARCIA:
    Sure.
    19
    MR. ANDES:
    We have two reports and
    a
    20
    chart
    that we can introduce
    that are relevant to
    21
    this issue.
    22
    DR. GARCIA:
    This is the one
    you --
    23
    MR. ANDES:
    That’s the one
    you
    want
    to
    24
    use
    right now?

    Page 14
    1
    DR. GARCIA: The density current one.
    2
    MR. ANDES:
    Okay.
    Just
    a
    moment.
    3
    DR. GARCIA: Essentially,
    what we have
    4
    done with the model,
    to
    answer
    your question, is
    to
    5
    try to
    explore different
    scenarios
    that have the
    6
    potential to
    generate density current in the south
    7
    branch of the Chicago River.
    8
    MR.
    ANDES:
    Let
    me
    stop you
    there.
    9
    We’ll
    introduce the reports, and then we can
    go
    on.
    10
    We
    have
    a
    report entitled Upstream Intrusion Effect
    11
    of CSO Events in Bubbly Creek,
    Illinois.
    12
    MS. TIPSORD: If there’s no objection,
    13
    we’ll mark this report, Upstream Intrusion Effect of
    14
    CSO Events
    in Bubbly Creek, Illinois,
    as
    15
    Exhibit 194. Seeing none, it’s Exhibit 194.
    16
    MS.
    DIERS:
    Can I ask just a
    quick
    17
    clarifying
    question on this? IS this the paper
    that
    18
    you’re
    referring
    to
    that you’ll present in Kansas
    19
    City?
    20
    DR. GARCIA:
    Yes.
    21
    MS. DIERS:
    Okay.
    Thank you.
    22
    MR. ANDES:
    And then we have
    a chart
    23
    with
    the title Upstream Intrusion Induced
    by
    CSO
    24
    Events.

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    Page 18
    1
    one
    step
    further -- and
    this
    is
    getting
    to
    the
    2
    question,
    which is that -- one of the questions --
    3
    depending
    on how much water is coming down the south
    4
    branch
    -- and there is
    a
    table here. If
    you
    go
    to
    5
    table
    two, okay, which is
    about
    the fourth page in
    6
    the
    paper, these are the
    cases
    that
    we have
    tested.
    7
    So
    we say
    the flow
    coming
    down the main channel of
    8
    the
    south branch, it can range, let’s
    say,
    anywhere
    9
    from not moving
    at
    all,
    but
    let’s just put a
    low
    10
    flow,
    a
    kilometer per second -- that’s about
    11
    1,000 liters.
    That’s
    about
    250 gallons per
    12
    second
    -- all the way
    to
    30 kilometers per second,
    13
    and we
    see
    the amount
    of water, with sediments,
    14
    coming out
    of Bubbly Creek.
    15
    And then what
    we
    see
    is that
    when
    16
    the water
    gets
    to
    the junction, it actually takes
    17
    off as a
    density current, and it tries
    to
    actually
    18
    go
    upstream into the south branch. So it’s almost
    19
    like the
    river has lost its memory. You know, it
    20
    remembers
    that 100 years
    ago
    it
    used to
    flow that
    21
    way, and the water of the river is
    still
    sloped in
    22
    that
    way.
    The water
    surface may slow the other way
    23
    depending on what we
    do to
    the river.
    24
    So what it does is it tries to
    go

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    Page
    20
    1
    you
    the idea of how far this phenomenon can go.
    2
    So if
    you
    have
    a
    water
    intake
    3
    there,
    it’s not very
    good
    for New
    Orleans
    because
    4
    you’re going
    to
    be pumping in salty
    water. In our
    5
    case,
    we
    want
    to
    understand what is the role played
    6
    in this
    phenomenon. Because wherever it
    goes,
    it’s
    7
    going
    to
    deposit materials there, and
    it’s also
    8
    going
    to
    bring in the
    BOD
    that was
    in there, in the
    9
    CSO, not just
    the sediments.
    10
    So
    anybody who -- or anything that
    11
    is
    transported in low oxygen water is
    going
    to
    come
    12
    with it as part
    of the flow itself. So it’s going
    13
    to
    take it
    to
    different places. As you go to the
    14
    other side -- and
    I know this is long.
    15
    MS. DIERS:
    That’s fine.
    16
    DR.
    GARCIA:
    But upstream
    is trying
    to
    17
    intrude, but it’s
    facing
    the
    flow coming down the
    18
    south
    branch,
    but
    then it’s also going
    to
    try to
    go
    19
    with the flow,
    and what
    we find out
    is that it mixes
    20
    up
    more
    with the flow that is going down the south
    21
    branch.
    22
    So what we have
    been trying
    to do
    23
    is model
    -- in particular we have concentrated
    a
    lot
    24
    on
    Bubbly Creek
    because
    early on,
    as
    part of
    a
    phase

    Page
    21
    1
    one study,
    between Grand
    Avenue,
    Lake Michigan
    and
    2
    Cicero
    Avenue, we
    said,
    “Okay.
    Let’s
    do a
    3—D model
    3
    of
    all these,”
    and then
    it became quite
    apparent
    4
    that the
    role played
    by
    Bubbly
    Creek was not
    only
    5
    unique,
    but it has
    a
    large impact
    on the
    system
    6
    depending
    on
    flow
    conditions.
    7
    So
    that’s what
    steps
    have
    been
    8
    taken
    as to try
    to
    model this type
    of
    phenomenon.
    9
    And
    I
    have
    to
    say
    that -- I’m
    not sure
    if we
    have it
    10
    in the testimony,
    but also
    the city,
    the
    water
    11
    department
    for the
    city, they’re
    known as two
    12
    outlookers,
    which
    are sensors
    that basically
    send
    13
    acoustic
    waves
    and they
    measure how
    much water is
    14
    moving
    on the south
    branch.
    So
    we can
    put one
    in
    15
    correlation
    with
    a
    geological
    survey.
    There is
    one
    16
    upstream
    of the junction
    between Bubbly
    Creek
    and
    17
    the south
    branch and
    there is
    one downstream.
    18
    And
    what
    we’re trying
    to
    see
    if
    we
    19
    can catch
    these events
    in the acts,
    basically,
    not
    20
    just
    model
    them.
    You
    know,
    modeling is
    just
    a tool.
    21
    But
    to see actually,
    you
    know, when they
    happen,
    how
    22
    often they
    happen,
    you
    know, what
    is the
    frequently,
    23
    you
    know, how
    much
    water
    you’re
    actually
    getting
    24
    into it.

    Page
    22
    1
    MS. DIERS:
    When
    did you
    start
    doing
    2
    that?
    3
    DR.
    GARCIA:
    This
    we
    started
    about
    a
    4
    year
    and
    a
    half ago,
    yes.
    5
    MS. DIERS:
    And
    is it currently
    6
    ongoing?
    7
    DR.
    GARCIA:
    We are
    going
    full
    force,
    8
    yes.
    9
    MS.
    DIERS:
    And
    I think
    you
    said
    that
    10
    you have
    three
    scenarios
    that
    you
    looked
    at.
    How
    11
    did you
    decide
    the
    scenarios?
    12
    DR.
    GARCIA:
    Basically
    we decided
    it
    13
    was based
    on what
    the
    range
    of
    flows
    is
    from
    the
    14
    Racine
    Avenue
    pumping
    station,
    and also
    the
    range
    of
    15
    flows
    that
    we know
    can come
    down
    the
    south
    branch.
    16
    MS. DIERS:
    And
    on
    Exhibit
    194,
    17
    Figure
    5,
    you
    have
    CSO particle
    concentration
    equals
    18
    1,000
    milligrams
    per
    liter.
    Is that
    measured
    or
    19
    assumed?
    20
    DR. GARCIA:
    That’s
    --
    it’s
    an assumed
    21
    value,
    but
    based
    on
    records
    taken by
    the
    history.
    22
    You’re
    talking
    --
    can you
    clarify
    which
    one
    is
    the
    23
    one
    you’re
    looking
    at?
    24
    MS.
    DIERS:
    I
    have a
    report.
    It’s

    Page
    23
    1
    Exhibit 194.
    2
    DR. GARCIA:
    Yes.
    3
    MS. DIERS:
    And I’m looking
    at
    4
    Figure 5. I’m not
    sure what
    page.
    5
    DR. GARCIA:
    Yes.
    This is --
    6
    MS. DIERS:
    I thinks it’s the sixth
    7
    page.
    8
    DR.
    GARCIA:
    This is an assumed
    value
    9
    for the purpose of the
    modeling exercise. It
    10
    doesn’t mean -- therefore,
    it doesn’t mean that all
    11
    the CSO5
    that
    come
    out
    of
    a
    scene are going
    to come
    12
    out
    are going
    to
    have
    35 millimeters per second
    and
    13
    are
    going
    to
    have
    a
    concentration of
    1,000. But
    14
    that’s
    a
    value that we
    estimated
    to be a reasonable
    15
    value for the purpose of modeling.
    16
    MS.
    DIERS:
    And I know
    you mentioned
    17
    the Mississippi River.
    So have
    you
    measured
    density
    18
    current in other places?
    Outside of the Chicago
    19
    River area, have
    you measured in the Mississippi
    20
    River?
    21
    DR. GARCIA:
    No.
    22
    MS. DIERS:
    Have
    you
    measured
    anywhere
    23
    else?
    24
    DR. GARCIA:
    I, myself, cannot

    Page 24
    1
    measure,
    but
    I did my PSE on density currents a long
    2
    time
    ago
    at the University of Minnesota. And the
    3
    motivation
    for
    that was actually a
    problem in Lake
    4
    Superior,
    and it had
    to do
    with mining and disposal
    5
    of
    mine tailings. And that’s according
    to
    this
    6
    topic, because
    the tailings were going into Lake
    7
    Superior. This was near Duluth, and
    people
    thought,
    8
    “Well,
    we’ll dump it into the lake, and this
    goes
    9
    and
    takes the tailings all the way
    to
    the
    deep
    end
    10
    of
    Lake Superior.”
    11
    And
    at
    the
    time, I calculated
    that
    12
    they
    could travel for
    80
    kilometers, these flows.
    13
    But
    there was -- there was an issue, and
    the
    issue
    14
    was
    that depending on the time of the year, Lake
    15
    Superior would stratify, and that would mean that
    16
    the density of the water column,
    particularly in
    the
    17
    summer, it
    wouldn’t
    be
    the same.
    So
    what these
    18
    flows were doing, they were coming down, and when
    19
    they found
    a
    layerof water that
    had the same
    20
    density,
    they made an intrusion there.
    21
    But,
    see,
    the lake was
    22
    circulating. It was taking the water all
    the way
    to
    23
    the
    water intake
    of
    Superior, Wisconsin, and the
    24
    People in superior, Wisconsin, they didn’t like

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    Page 26
    1
    another professor, Jack Lucat
    (phonetic), who is
    a
    2
    geotechnical engineer,
    to
    try
    to figure out
    a
    way
    to
    3
    move the pipes that
    put
    the tailings into the
    lake
    4
    so
    that, first of all, the particles circulate,
    they
    5
    are
    not on
    the surface,
    because
    it’s
    a
    lake
    used for
    6
    recreational purposes, and
    then the particles don’t
    7
    go
    sideways.
    8
    MS. DIERS:
    And
    do you
    know what the
    9
    impact of the density
    currents are on aquatic life?
    10
    DR. GARCIA:
    The impact -- we don’t
    11
    know much
    about
    what the impact is,
    but
    I can
    12
    imagine
    a
    situation
    in which
    you
    could have these
    13
    density flows reaching
    out to
    places
    on a hot summer
    14
    day
    where fish
    might seek refuge,
    you
    know, what
    15
    people call thermal refuge,
    you know. You go there
    16
    because
    it’s cold, the water is colder than the
    17
    surface of anywhere else. nd since these flows
    are
    18
    always trying
    to
    reach
    a
    point
    of lowest elevation,
    19
    they might reach that, and that might not
    be good
    20
    for the fish.
    21
    MS. DIERS:
    But
    you don’t know for
    22
    sure, correct?
    23
    DR.
    GARCIA:
    I don’t know for sure,
    24
    but
    I have seen this
    happen
    when
    somebody makes
    a

    Page
    27
    1
    mistake at a nuclear power plant, and all of
    a
    2
    sudden
    they release
    very cold water into
    a
    lake
    that
    3
    is using for cooling
    purposes,
    you get a
    density
    4
    flow, and it
    goes
    all the way under
    the water and
    5
    you get
    fish kill.
    So
    the answer is I
    don’t know
    6
    for sure, but
    you
    are going
    to get
    water of poor
    7
    quality
    to a
    place
    where it might affect it.
    8
    MR. ANDES:
    If I can
    follow
    up
    on that
    9
    for a
    moment,
    I think it might help
    to
    -- this
    is
    10
    Exhibit 1 to
    Dr.
    Garcia’s testimony. I
    just thought
    11
    this map might
    be
    helpful
    for people
    to
    visualize in
    12
    addition
    to
    the color maps,
    just to
    make sure
    people
    13
    have that.
    14
    So Doctor, I
    see
    -- is
    your point,
    15
    looking
    at
    the map
    of Bubbly Creek, that the
    density
    16
    current leads
    to
    potential impacts
    during wet
    17
    weather events
    up
    in the south fork?
    18
    DR.
    GARCIA:
    No -- yeah.
    Part of my
    19
    conclusion is that, that
    you
    have the
    potential
    to
    20
    have density flows and that they are going
    to
    21
    impact --
    22
    MR. ANDES:
    Beyond
    Bubbly Creek?
    23
    DR. GARCIA:
    They are going
    to impact
    24
    Bubbly Creek,
    and they could impact beyond Bubbly

    Page 28
    1
    Creek, too,
    depending on the impact in the
    south
    2
    branch.
    3
    So, for
    instance, if
    you
    have no
    4
    flow down the south
    branch -- let’s assume that we
    5
    call that
    the freshwater flow, which comes
    down
    the
    6
    south
    branch -- the chances of having an
    intrusion
    7
    going upstream are going to be
    larger, of course,
    8
    and the extension of it
    is going
    to be
    larger. But
    9
    also, you
    could have
    a
    flow going downstream
    on the
    10
    south
    branch.
    11
    Now, one
    thing I want
    to
    clarify
    12
    is that it
    doesn’t mean that all the flows
    emanating
    13
    from the scene are going to
    lead -- all the CSOs are
    14
    going to
    lead
    to
    density currents, okay? But the
    15
    potential is there, and that’s why
    we are doing the
    16
    modeling, that’s
    why we are studying, and that’s why
    17
    we’re
    trying
    to
    measure
    this.
    18
    MS. DIERS: Do you
    know if it’ll
    19
    •affect any other segments
    besides tte south branch?
    20
    DR. GARCIA:
    Well, nobody’s
    coming
    out
    21
    of here. I think what is coming out
    of here has the
    22
    potential to affect
    the south branch itself.
    Now,
    23
    one
    question that someone may ask is whether
    -- how
    24
    far down the south branch is
    this going
    to go,
    and I

    Page 29
    1
    imagine that it could
    go
    pretty far.
    2
    However, having said that, when
    3
    these
    flows happen,
    at the interface, what we call
    4
    the ambient water and the water that makes
    it flow,
    5
    this is constantly mixing
    too. So
    the flow keeps
    6
    diluting as it travels. So the further away
    you go
    7
    from the source of
    the flow or where the flow plans
    8
    and it went underneath, the turning basin
    -- after
    9
    the turning basin, the impact is going
    to
    diminish
    10
    with distance.
    11
    One thing I want
    to clarify is
    12
    that -- which I mentioned before, is that if
    you
    13
    look at
    this exhibit, this
    figure,
    you see
    all these
    14
    leaps across. So what that means is if
    you
    have
    a
    15
    flow going up
    the
    south branch, okay, the minute it
    16
    finds an open door there on this
    leap, it’s going
    to
    17
    try
    to go
    in there, and it’s probably going
    to
    it
    18
    there, and it’s going
    to
    deposit whatever the hazard
    19
    is. Then the river has no other mechanism
    to
    20
    actually
    get
    this
    out
    of there, whatever it is that
    21
    the density
    flow
    put on the bottom of those leaps,
    22
    and that obviously brings other questions probably
    23
    into your mind
    too.
    24
    MS. DIERS:
    I’m going to
    go
    back
    to

    Page 30
    1
    our pre-f lied question three.
    2
    DR. GARCIA:
    Yes.
    3
    MS. DIERS:
    And on Page
    3
    of your
    4
    pre-filed testimony,
    you’re talking
    about -- you say
    5
    your recommendations
    have been implemented. Are
    you
    6
    referring
    to
    MWRDGC
    accepting those recommendations?
    7
    DR. GARCIA:
    You mean accepting,
    8
    right?
    9
    MS. DIERS:
    Mm-hmm.
    10
    DR.
    GARCIA:
    Because the question
    says
    11
    accepting. But which one is
    at
    -- I need some
    12
    clarification on
    that.
    13
    MS. DIERS:
    I’m sorry.
    On Page
    3 of
    14
    your pre-filed testimony,
    “Our recommendations have
    15
    been implemented.” And question -- the
    pre-filed
    16
    question three is asking who -- what
    recommendations
    17
    are you
    referring
    to, and who did
    you
    make them
    to?
    18
    MR. ANDES:
    So
    you’re referring --
    19
    DR. GARCIA:
    Oh, yeah.
    20
    MR.
    ANDES:
    So you’re referring to
    21
    recommendations
    about
    the SEPA stations.
    22
    DR. GARCIA:
    Yes.
    23
    MS.
    DIERS:
    I think -- yeah.
    I think
    24
    that’s what it’s trying
    to ask.

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    Page
    35
    1
    specifically with
    respect
    to
    number six, when
    did
    2
    your research begin with
    the density currents you
    3
    were looking
    at
    in the system?
    4
    DR. GARCIA:
    In the system? A long
    5
    time ago. You mean the Chicago River System?
    6
    MS. DIERS:
    Mm-hmm.
    7
    DR. GARCIA:
    Almost ten years
    ago,
    8
    nine years ago.
    9
    MS.
    DIERS:
    Okay.
    And then with
    10
    respect to
    Bubbly
    Creek?
    11
    DR. GARCIA:
    Bubbly Creek
    a
    year and
    a
    12
    half ago, as
    I
    stated before.
    13
    MS. DIERS: And when will your
    study
    14
    be
    completed?
    15
    DR. GARCIA:
    I think in
    about a year.
    16
    MS. TIPSORD: For clarification, the
    17
    study
    on
    Bubbly
    Creek.
    18
    DR. GARCIA:
    On Bubbly Creek,
    yes.
    19
    This I have
    to
    -- I think it’s in the testimony.
    20
    MR. ANDES:
    This is the
    study to
    21
    develop the 3-D model. Am I correct?
    22
    DR. GARCIA:
    Yes.
    We -- this -- what
    23
    we’re doing now is part of
    a
    larger project with
    the
    24
    idea of being able
    to
    model the Chicago waterways

    Page
    36
    1
    and develop a 3-D model of the waterways, and
    what
    2
    we’re
    doing
    right now is what we call phase one,
    and
    3
    it entails the
    Chicago River from Grand Avenue in
    4
    the north branch
    all the way
    to
    the dock
    by
    the lake
    5
    in the main stem, and then
    all the way down the
    6
    south branch
    to
    Cicero Avenue
    just upstream of
    7
    Stickney.
    8
    And the
    reason why we broke this
    9
    down in phases is
    because
    originally,
    I wanted
    to do
    10
    the whole 80 miles in one shot, and something
    called
    11
    me
    to
    my senses, and
    I said, “Well, isn’t that
    a
    12
    little bit
    too
    much?” And
    as it turns out, yes. If
    13
    you
    try
    to do everything
    at
    once, it’s
    a
    lot.
    14
    So what we
    are doing now -- this
    15
    is phase one, like I explained -- and inside
    phase
    16
    one is Bubbly Creek.
    This project, phase one, is
    a
    17
    36-month project, and I think
    that we started
    to
    18
    work on it somewhere in June of 2007. We finally
    19
    got
    everything going in 2007.
    20
    MS. DIERS:
    Okay.
    And phase
    one is
    21
    not completed?
    22
    DR. GARCIA:
    Phase one is the one
    that
    23
    we are working on, and
    you
    can
    say
    we
    are halfway --
    24
    a
    little
    bit more than halfway.

    Page 37
    1
    MS. DIERS:
    Okay.
    And what would
    2
    phase
    two
    be?
    3
    DR. GARCIA:
    Phase
    two is
    going to
    4
    build the north branch. It’s going
    to
    include --
    5
    excuse me
    a
    second,
    because
    I don’t want
    to --
    6
    MR. ANDES:
    I believe we’re referring
    7
    to a
    progress report
    that was attached
    to
    the
    8
    testimony. That would
    be
    attachment three
    to
    the
    9
    testimony.
    10
    DR. GARCIA: No. Actually, this is --
    11
    MR. ANDES:
    That’s
    a
    progress
    report
    12
    on phase one.
    13
    DR. GARCIA:
    Just a second.
    14
    MR. ANDES:
    Let me clarify.
    The
    15
    document
    that Dr. Garcia
    is referring to is not
    16
    attachment three. The progress report is
    a separate
    17
    document, which is the research proposal, and we
    can
    18
    provide
    copies.
    So this would be a new exhibit.
    19
    It’s
    titled Research Proposal, the Chicago
    Waterway
    20
    System, Environmental Modeling, Phase One, Chicago
    21
    River Main Stem, South Branch,
    South
    Fork
    (Bubbly
    22
    Creek) and Sanitary and Ship Canal.
    23
    MS. TIPSORD: If there’s no objection,
    24
    we
    will mark this research
    proposal as Exhibit

    Page
    38
    1
    No. 196. Seeing none, it’s
    Exhibit 196.
    2
    DR. GARCIA: So
    this -- this proposal,
    3
    just
    for clarification,
    because
    I think it’s
    a
    lot
    4
    easier to
    read the document, this was the original
    5
    proposal we prepared for the District
    to
    develop
    6
    this 3-D
    model
    of the waterways,
    okay? The proposal
    7
    was
    written in mid-2006,
    but because
    of different
    8
    circumstances,
    things didn’t start until mid-2007.
    9
    If you
    go to
    -- this
    explains
    what
    10
    we are doing and what we
    were doing. It talks
    about
    11
    density
    currents, what we knew
    about
    density
    12
    currents
    at
    the time, which was the main stem
    of
    the
    13
    Chicago
    River, the motivation for doing the 3-D
    14
    modeling. And then if you
    go
    to Page 12 of the
    15
    proposal,
    it tells
    you
    what are the different phases
    16
    of
    this project.
    So you
    have the phase one, which
    17
    is the one that we are on right now, and it says
    18
    this
    proposal is one I was trying
    to
    explain, that
    19
    goes
    from the main stem of the Chicago
    River,
    and
    20
    then the
    north
    branch;
    and then the south branch of
    21
    the
    Chicago River, the Sanitary and Ship Canal, and
    22
    the
    south fork of the south branch of the Chicago
    23
    River -- that
    would
    be
    Bubbly Creek -- and if
    you
    24
    can see
    there in parenthesis, we said Bubbly Creek

    Page 39
    1
    will be initially
    modeled with -- it’s
    a
    model
    2
    that -- a
    2-D model.
    3
    We decided that there
    was no point
    4
    in
    trying
    to
    throw the kitchen sink
    initially
    at --
    5
    in terms of modeling Bubbly
    Creek,
    because
    we knew
    6
    very little about
    it.
    So
    we said why don’t we --
    7
    you
    know, people
    got
    one model of it,
    that was
    a
    8
    Marquette University model
    of it. We said, “Why
    9
    don’t
    we
    go 2-D
    and try
    to see
    what happens on
    a
    10
    plane
    before we try
    to see
    what happens on the
    11
    column,” which we have already
    done,
    but
    we started
    12
    with a 2-D
    model. That’s another paper that will
    be
    13
    presenting in Kansas that we can
    also enter.
    14
    But let’s continue with this right
    15
    now. So you
    can
    see
    here, the
    proposal called for
    16
    that 36-month study, and
    that’s what we have done,
    a
    17
    little bit
    more than halfway into it, and then we
    18
    have a
    phase two, which is 24 months,
    and then we
    19
    have a phase
    three.
    20
    One thing that is
    important
    to
    21
    mention is that together,
    with this proposal, they
    22
    use a
    logical
    survey, and also submitted
    a
    proposal
    23
    to
    do
    synoptic measurements, that is
    measurements
    of
    24
    flow and water quality at
    different locations,

    Page 40
    1
    including the symmetry of the water elevation in the
    2
    river
    so
    that we can
    put
    that into the mathematical
    3
    model
    to
    run it, basically,
    to do
    the model
    4
    predictions. And those are still ongoing, and
    5
    they’re going to -- they’re going to
    continue.
    6
    So
    that, in
    a
    way -- if we
    go back
    7
    to
    your question, when did the research begin, it
    8
    began mid-2007. Who is involved in this
    research?
    9
    Well,
    the University of Illinois, our group, and
    10
    also
    the geological survey is involved with
    a
    few
    11
    measurements, along with the District
    as
    well.
    12
    They’re monitoring
    at
    the research branch. They
    are
    13
    also working with
    us
    on the mission. We need
    to
    run
    14
    them
    all.
    15
    MS. DIERS:
    After the 3-D model
    16
    results become available,
    how
    will these results
    be
    17
    used to
    determine the aquatic life potential for
    the
    18
    south fork, south branch of the Chicago River?
    19
    DR. GARCIA: What is
    that question?
    20
    MS. DIERS:
    It’s
    a
    followup
    based on
    21
    what we’ve been talking about.
    22
    DR. GARCIA:
    Oh, okay.
    23
    MR. ANDES:
    Can
    you
    repeat the
    24
    question?

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    Page 42
    1
    happens when
    you don’t -- just normal operations of
    2
    the
    river, what
    goes on in the river, that’s what
    3
    makes Bubbly Creek kind
    of unique,
    because
    it’s in
    4
    two completely different
    stages. You
    know, one
    were
    5
    there’s practically no flow, and one were there’s
    6
    flow.
    7
    So the
    answer
    to -- your question
    8
    is how are we going
    to use a
    model. I think the
    9
    model
    is
    going
    to
    help people that want
    to
    figure
    10
    out
    or want
    to assess water quality in the Chicago
    11
    waterways determine -- how
    do you say -- if not with
    12
    more precision, in
    a
    more
    educated
    fashion, I would
    13
    say,
    what are the true
    conditions in the river.
    14
    MS. DIERS: I’ll
    go to
    pre-filed
    15
    question eight. What
    other options were there
    16
    besides the environmental fluid
    dynamics code? I
    17
    guess
    I should also ask first what is
    the
    18
    environmental fluid
    dynamics code?
    19
    DR. GARCIA:
    Yeah.
    The environmental
    20
    dynamics code -- yeah. We have
    a
    -- if
    you
    want,
    we
    21
    can give
    you
    the --
    22
    MR. ANDES:
    We have
    an exhibit, which
    23
    is
    titled
    Environmental Fluid Dynamics
    Code,
    EFDC.
    24
    MS. TIPSORD:
    If there’s no objection,

    Page
    43
    1
    we
    will mark
    Environmental Fluid Dynamics
    Code,
    2
    EFDC, as
    Exhibit 197.
    Seeing none, it’s
    3
    Exhibit 197.
    4
    DR.
    GARCIA: The environmental fluid
    5
    dynamics
    code, as
    the name indicates,
    is
    a
    6
    three-dimensional
    code
    that can
    be used to model
    7
    dynamic sediment
    transport, and it also has
    8
    nitrification components,
    for example, and it was
    9
    available
    by
    Dr. Joe Hambrick (phonetic)
    when he was
    10
    a
    professor at the Virginia Institute of Marine
    11
    Science in the early
    ‘90s, and it was there
    12
    originally for rivers going into
    estuaries. But
    13
    it’s a
    model that
    has received wide application --
    14
    MR. ANDES:
    If
    I can
    stop you
    there,
    15
    Marcelo,
    we have
    another exhibit, which is
    a list of
    16
    known EFDC
    applications as of January 2004.
    17
    MS. TIPSORD:
    If there’s no objection,
    18
    we
    will mark
    the list of known EFDC
    applications
    as
    19
    Exhibit 198. Seeing
    none, it’s Exhibit 198:
    20
    MR. SUISKI:
    Two from
    200.
    21
    DR.
    GARCIA:
    So what
    you
    can
    see from
    22
    this second -- if we were
    in class I would
    say a
    23
    handout -- exhibit, is
    because
    it’s
    been widely
    used
    24
    in places like
    the Everglades, and it’s
    a code that

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    Page 45
    1
    I
    also had the opportunity
    to
    have
    2
    been
    exposed
    to
    this
    code as part of a five-year
    3
    review panel, and this was
    a case
    between General
    4
    Electric and U.S. EPA, and I was part of the review
    5
    planning
    of
    the modeling, and one of the models that
    6
    they use
    is
    a
    river model,
    and
    a
    fish dynamics
    7
    model, and
    a
    risk of human exposure
    to
    model, and
    8
    the model that they had
    used at
    the time was the
    9
    EFDC.
    And in that
    particular
    case,
    the model
    10
    struggled a
    little
    bit, because it was a natural
    11
    river, very different from what they have in this
    12
    particular case.
    13
    But that’s how
    you
    begin
    to
    14
    intimate
    with
    the EFDC. And
    so
    when the time came
    15
    to
    choose
    a
    tool, I thought the learning
    curve, if
    16
    we
    go
    with this model, is going
    to be a
    lot shorter
    17
    than
    if we try
    to start
    to
    work with another model,
    18
    commercial or public, or if we try
    to develop it on
    19
    our
    own.
    -
    20
    MS. DIERS: Okay.
    Pre-filed question
    21
    number nine, which I think we might have talked
    22
    about, but
    Ill
    go
    ahead and ask it, what conditions
    23
    might
    cause
    the south branch
    of the Chicago River
    to
    24
    act as a barrier
    to
    the flow coming
    out
    of
    the south

    Page
    46
    1
    fork
    of the
    south branch
    of
    the
    Chicago River?
    2
    DR.
    GARCIA:
    Right.
    Yes.
    What
    I --
    3
    what
    I tried
    to
    -- when I
    referred to
    that
    on the
    4
    testimony,
    the way
    to
    visualize
    this is that
    5
    depending
    on
    what the
    water
    levels
    are in
    the south
    6
    branch
    of
    the Chicago
    River,
    you
    know that
    the
    7
    models of
    the waterways
    is that when
    there
    is
    a
    8
    storm on
    the
    way,
    at
    Rockport
    they open
    up the
    9
    gates,
    and
    they
    say,
    “Okay.
    We need
    to
    lower the
    10
    water
    surface elevation
    in the waterways
    in
    11
    anticipation
    of the rain
    that we
    are going
    to
    get.”
    12
    So
    the
    idea
    is that
    you
    remain
    some storage
    capacity
    13
    by
    doing that.
    14
    Now,
    there
    are other instances
    in
    15
    which
    you do that,
    but
    still
    it starts to
    rain,
    the
    16
    water level
    in the river
    starts to go
    up. So
    17
    depending
    on
    what the
    water elevation
    is
    compared to
    18
    the water
    coming out
    of Bubbly
    Creek, you
    are going
    19
    to
    have
    what
    we call
    a
    backwater
    effect.
    20
    Essentially,
    the
    south branch
    is going
    to
    back
    up
    21
    the water coming
    out
    of Bubbly
    Creek.
    22
    Now, that
    is
    going
    to depend on
    23
    how
    much Racine
    Avenue is pumping,
    and
    how
    much is
    24
    coming out of
    the storm outfalls,
    the ones
    that
    you

    Page
    47
    1
    can
    see
    in Exhibit 1 right here.
    So
    all
    of those
    2
    are going to contribute water, particularly during
    a
    3
    storm
    event, and
    depending on what the south branch
    4
    is
    doing in terms
    of water surface elevation, this
    5
    is
    going
    to
    backup, more
    or less, water into Bubbly
    6
    Creek, and that’s what I meant
    by
    that.
    7
    It’s
    a
    dynamic situation, and
    the
    8
    way this works
    -- because Bubbly Creek has an
    9
    inoperative flow -- all it
    does
    is
    get all the
    10
    kinetic energy, or the water coming
    out
    of
    the
    11
    pumps, transforms
    that kinetic energy
    to
    potential
    12
    energy, essentially, and raises the
    water level,
    13
    into
    then Racine,
    you
    know, the pumping station,
    14
    until the water starts
    to
    flow
    towards the south
    15
    branch. Now, if the water in the south branch
    is
    16
    too
    high, well, it’s
    going to flow less.
    17
    And the effect
    of that, if I could
    18
    elaborate more, is that
    at
    times, you’re going
    to
    19
    have Bubbly Creek moving with
    a certain regime of
    20
    flow velocity. The flow discharge is going
    to
    be
    21
    the same,
    but depending on what the south branch
    is
    22
    doing, the water is
    going to move faster, more
    23
    slowly, in Bubbly Creek, and it could work.
    24
    Depending on the
    effects, sometimes it could work
    as

    Page 48
    1
    a
    settling tank, and
    sometimes it could actually
    2
    transport
    -- you
    could
    be swift enough
    to
    resuspend,
    3
    and move whatever came in,
    plus
    whatever
    it can pick
    4
    up
    from the bottom of the creek.
    5
    So what the south branch
    does,
    6
    it’s
    important
    to the dynamics of the CSOs in Bubbly
    7
    Creek. And therefore, that’s
    the
    need
    to have a 3-D
    8
    model, because the only thing
    you
    can
    do
    is
    -- I can
    9
    come
    here and
    try to explain this,
    but
    the only way
    10
    you
    can
    do
    this
    is through direct observation, doing
    11
    as
    many measurements
    as you
    can.
    12
    MR. ANDES:
    If I can follow
    up
    on
    13
    that.
    So
    if
    you
    have these wet
    weather events where
    14
    the flow may
    be
    coming
    out
    of Bubbly Creek and
    going
    15
    into the south branch, if
    one, then, were
    to add
    16
    flow augmentation, supplemental aeration
    to address
    17
    issues, what effect could that have, in. terms
    of
    18
    changing the phenomenon?
    What impacts would that
    19
    have outside of Bubbly Creek?
    20
    DR. GARCIA:
    You’re asking me now?
    21
    MR. ANDES:
    Yes,
    yes.
    22
    DR. GARCIA:
    Well,
    you know, there is
    23
    consideration
    of,
    as
    Fred is saying, increasing
    the
    24
    amount of flow,
    particularly in dry weather

    Page
    49
    1
    conditions, so that the water moves, injecting
    air
    2
    and
    so
    forth. We
    have more than that
    as
    well with
    3
    our 2-D model, and what
    we have found is we need
    to
    4
    know more about the
    sediments along the bottom of
    5
    Bubbly Creek.
    6
    And the reason why we need
    to know
    7
    more is
    because, as you know, there is
    a
    legacy
    8
    there of material that was
    -- that found its way
    9
    into Bubbly Creek for many, many years from
    the
    10
    stockyards and the packing -- the meatpacking
    11
    houses, and there is
    always buildup, and then on
    top
    12
    of that buildup there is
    a contemporary -- and I
    13
    call it contemporary
    for lack of.a better word --
    14
    the contemporary sediments
    have found their way
    15
    there
    from the
    outfalls and the water coming
    out of
    16
    the pumping station.
    17
    MR. ANDES:
    Should we use your report
    18
    on
    that issue?
    19
    DR. GARCIA:
    Yes.
    Yeah, we can
    use
    20
    that.
    21
    MR.
    ANDES:
    We have an exhibit on
    this
    22
    issue. It’s titled Two
    Dimensional BOD and D.O.
    23
    Water Quality Model for Engineering
    Applications,
    24
    the
    Case
    of Bubbly
    Creek in Chicago, Illinois.

    Page
    50
    1
    MS. TIPSORD: If there’s no objection,
    2
    I
    will mark the report
    as
    described
    as
    Exhibit 199.
    3
    Seeing none, it’s Exhibit 199. There are extra
    4
    copies of these last four exhibits,
    too,
    that are
    5
    still up
    here on
    the front table if somebody needs
    6
    one.
    7
    DR. GARCIA: So if
    you
    -- this is also
    8
    another word
    with
    my graduate students -- here what
    9
    we tried to do
    was model
    the
    water quality in
    Bubbly
    10
    Creek,
    and
    to
    try
    to
    understand what was going on.
    11
    And
    the main -- the main thing coming
    out
    of it, if
    12
    you
    look at
    figure
    -- don’t look at the equations,
    13
    because
    you’re not going
    to
    like the equations. But
    14
    if
    you
    look at Figure 4, there we
    have
    the symmetry
    15
    of
    Bubbly Creek, and then we look
    at
    the flow
    16
    velocity field in different colors.
    17
    So what we
    were
    trying
    to do here
    18
    is figure out
    how fast
    does
    the water move in Bubbly
    19
    Creek when the Racine Avenue pumping station is
    20
    discharging
    water
    at a certain
    rate.
    So
    if
    you look
    21
    at
    this figure, it corresponds
    to a
    rate of
    about
    22
    69
    cubic meters per second. And then what we try
    to
    23
    do
    is, besides
    modeling
    the
    flow velocity,
    you can
    24
    see
    that near the pumping station the flow moves

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    Page 54
    1
    But also, if
    you’re trying to
    do
    2
    any type
    of
    -- or you’re considering any
    type of
    3
    remediation
    alternative
    to
    try
    to
    keep dissolved
    4
    oxygen levels
    at the certain value, then
    you
    have
    to
    5
    take that into account,
    the possibility that, “Okay.
    6
    We could recirculate the water, which
    is one of the
    7
    things
    that we
    can look
    at.
    Besides pumping
    water
    8
    from the south branch,
    besides adding oxygen
    to
    that
    9
    water, we also have
    to
    look
    at
    what
    if we
    just
    10
    recirculate and we increase, we pump
    in air.” Well,
    11
    this seems to
    work
    on the surface,
    but
    we still
    have
    12
    this question of all the
    solids, the sediments in
    13
    the water. So there’s that.
    14
    MR. ANDES:
    So to follow
    up, does
    that
    15
    mean that if
    you
    apply these methods, the
    aeration,
    16
    recirculation, but
    you
    don’t
    do
    it correctly,
    you
    17
    could
    actually
    worsen
    the problem?
    18
    DR. GARCIA:
    That would
    be
    correct,
    19
    yes.
    20
    MR. ANDES:
    And you
    would
    need to
    do
    21
    these additional 3-D modeling and further
    studies in
    22
    order to determine what
    to do
    and what levels
    you
    23
    could
    get to.
    Am I
    correct?
    24
    DR. GARCIA:
    Yes.
    Besides the 3-D

    Page 55
    1
    modeling, what we are in the process of doing now is
    2
    basically turning Bubbly Creek into
    a
    lab, an
    3
    experimental lab, in the sense that we are trying
    to
    4
    add
    more
    sensors to the ones that the District
    5
    already
    has, the water quality sensors that we have.
    6
    We are going
    to
    have flow sensors
    as
    well,
    but
    also
    7
    we just build
    a
    gizmo, which is
    just
    half a pipe --
    8
    and
    I saw it yesterday. It’s not done
    yet, but
    we
    9
    follow the experience of the Illinois
    state
    water
    10
    survey with Tom Butts. He did
    a
    lot of measurements
    11
    of sediment oxygen in demand on the waterways of
    12
    Illinois. This is
    a
    report that people can download
    13
    from the web.
    14
    But basically, they
    use
    what is
    15
    called
    a
    ventichamber that
    you
    lower it, you put it
    16
    on the bottom of a
    stream
    or lake,
    and then
    you run
    17
    water
    through
    it, and
    you do a test,
    and
    you
    can
    18
    figure
    out
    how the sediment oxygen demand changes.
    19
    We can modify that, and
    now we
    are
    building -- in
    20
    our shop, in the department, we are building
    a
    new
    21
    flow with the idea that was
    used
    before of
    this
    22
    ventichamber, but it’s a little
    bit optimized from
    a
    23
    highly dynamic point of view.
    24
    So we are going
    to
    lower
    it in
    the

    Page
    56
    1
    water of Bubbly Creek in different locations,
    2
    because
    there is
    a
    lot of spacial variability on the
    3
    quality of the sediments, we think, and then we are
    4
    going to do a test where we are going
    to
    run with
    a
    5
    pump from
    a pontoon.
    We
    are going to
    recirculate --
    6
    and this is in collaboration with
    a
    geological
    7
    survey with the District -- we are going
    to
    8
    recirculate the water, and
    we are going to get water
    9
    that is in sediment oxygen demand
    at
    different
    10
    locations in Bubbly Creek for different flow
    11
    conditions.
    12
    So
    you
    may
    say,
    “Well, that’s
    13
    fine. What is going to come
    out
    of it?” Well, what
    14
    is going
    to
    come
    out
    of it is going
    to
    allow
    us
    to
    15
    obtain, experimentally, laws that is basically in
    16
    equation,
    that then we
    are going to be able to
    put
    17
    irto our l-D model, like the Marquette Model, or
    18
    you’re going
    to
    be able
    to put
    this in
    a
    3-D model
    19
    that gives
    you
    all the -- what
    could be
    potentially
    20
    the resuspension
    at
    different locations, and what is
    21
    going to
    be
    the sediment oxygen demand as
    a
    function
    22
    of flow velocity
    at
    different locations in Bubbly
    23
    Creek.
    24
    MS. TIPSORD: Dr.
    Garcia,
    you referred

    Page 57
    1
    to a
    report
    that could
    be
    download from the
    web.
    2
    Could you
    please tell
    us
    the website where
    that’s
    3
    available?
    4
    DR. GARCIA:
    Yes.
    I can give you
    a
    5
    copy
    of the report, but
    I only have one
    copy.
    6
    MS. TIPSORD:
    If it’s --
    7
    DR. GARCIA:
    If you do -- yes.
    8
    MS.
    TIPSORD: If it’s available on the
    9
    web, I
    think if
    you
    could
    just
    give us a
    citation of
    10
    what --
    11
    DR. GARCIA:
    It’s the Illinois State
    12
    Water Survey.
    13
    MR. ANDES:
    We can
    provide
    a
    link
    14
    later.
    15
    MS. TIPSORD:
    Okay.
    That would be
    16
    great.
    17
    DR. GARCIA: I can’t tell you
    what it
    18
    is
    now,
    because
    all the surveys
    have
    just
    been
    19
    transferred to
    the University.
    20
    MS. TIPSORD: Yes.
    That’s all right.
    21
    If
    we can
    get
    it later that’s
    fine.
    22
    DR. GARCIA: But if you do
    Illinois
    23
    State
    Water Survey and
    you
    type
    Butts, B-u-t-t-s,
    24
    Thomas Butts
    was
    the
    author of the report.

    Page
    58
    1
    MS.
    TIPSORD:
    Thank
    you.
    2
    DR.
    GARCIA:
    And
    this
    is
    ISWS,
    3
    Illinois
    State
    Water Survey
    dash
    74-R --
    like
    in
    4
    Robert
    -- I
    -- like
    in Irwin
    --
    no pun
    intended
    --
    5
    dash 76.
    So
    ISWS-74-R176.
    And
    there
    are
    other
    6
    reports
    of
    interest
    by
    this
    same person,
    7
    coworkers
    --
    8
    MS.
    TIPSORD:
    Thank
    you.
    9
    DR.
    GARCIA:
    --
    on
    the
    subject.
    10
    MS. flIERS:
    With
    respect
    to
    11
    Exhibit
    199
    -- and
    I’m
    going
    to
    ask
    a question
    about
    12
    Figure
    4 in
    your
    report.
    13
    DR. GARCIA:
    199
    is -- did
    --
    14
    MS.
    TIPSORD:
    The
    two
    dimensional
    BOD.
    15
    MS.
    DIERS:
    The
    two
    dimensional
    BOD.
    16
    DR.
    GARCIA:
    Yes.
    17
    MS.
    flIERS:
    The
    numbers
    that
    you
    have
    18
    in
    your
    Figure
    4,
    are
    they
    measured
    or
    modeled?
    19
    DR.
    GARCIA:
    Figure
    4,
    these
    are
    20
    modeled.
    But
    we
    have
    to
    put
    it under
    the
    condition
    21
    at the
    Racine
    Avenue
    pumping
    station.
    22
    MS.
    flIERS:
    So based
    on
    this
    modeling,
    23
    is
    it -- are
    you
    assuming
    fl.O.
    won’t
    go
    below
    8.1?
    24
    DR.
    GARCIA:
    Well,
    what
    this
    shows is

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    Page 60
    1
    in
    this
    case.
    2
    While if
    you go to
    the other
    3
    monitoring station, the
    one on 36th Street, which
    is
    4
    a
    lower
    set
    of curves than
    the red one, then
    you see
    5
    that the oxygen
    goes
    down,
    and it has a hard time
    6
    coming back and making it
    up
    above two milligrams
    7
    per liter, even after
    72 hours. So after --
    8
    72 hours after this
    CSO
    event
    happened, according
    to
    9
    our model and according
    to
    the measurements
    taken
    by
    10
    the District,
    you
    can
    see
    that it takes awhile
    to go
    11
    back.
    12
    So what this is telling
    us is that
    13
    even though Bubbly
    Creek is relatively short
    14
    compared
    to
    the rest of the waterways,
    it doesn’t
    15
    behave the same. You know, in its first half,
    if
    16
    you
    want
    to
    call it, in
    the first portion that it
    17
    does -- as you get
    closer
    to
    the south
    branch.
    18
    Therefore,
    we go back
    to
    what we said before,
    the
    19
    dynamics of what happens
    both aerodynamically and
    20
    intensive water quality in the creek is
    influenced
    21
    by
    what the south
    branch is doing.
    22
    MS. DIERS: I have nothing
    further.
    23
    Thank you.
    24
    MS.
    TIPSORD:
    Miss Dexter?

    Page 61
    1
    MS. DEXTER: Jessica Dexter with the
    2
    Environmental Law and Policy Center.
    3
    MR. JOHNSON:
    Before
    you get
    started,
    4
    Jessica, just
    a
    quick question.
    5
    Dr. Garcia, our
    environmental
    6
    engineering
    students
    at U
    of I are lucky,
    because
    7
    clearly
    you enjoy
    teaching and have done
    a
    great
    job
    8
    today.
    9
    DR. GARCIA:
    Thank
    you.
    10
    MS. TIPSORD:
    You
    say
    in your
    11
    conclusions here that
    you
    think additional study is
    12
    essential
    prior
    to us
    setting water quality
    13
    standards.
    Do
    you
    think the District and the Agency
    14
    and
    us,
    ultimately,
    will have enough information
    to
    15
    do
    that
    by
    the end of phase one, or
    do you
    think
    16
    each of the proposed additional phase two
    and
    phase
    17
    three would be --
    18
    DR. GARCIA: Well, with regards
    to
    19
    Bubbly Creek, I would hope that yes,
    we are going
    to
    20
    have
    enough --
    21
    MR. JOHNSON:
    Okay.
    22
    DR. GARCIA:
    -- at the
    end of phase
    23
    one.
    24
    MR. JOHNSON: Which is a little
    over
    a

    Page 62
    1
    year down the line?
    2
    DR. GARCIA:
    About,
    yes.
    3
    MR. JOHNSON:
    Thank you.
    4
    MS. DEXTER:
    One second. All right.
    5
    Most
    of my
    pre-filed questions
    have been answered
    6
    during IEPA’s questions,
    but
    I
    do
    have
    a
    few
    7
    followups
    about
    the density currents. The density
    8
    currents
    that
    your
    model
    is
    predicting,
    just so it’s
    9
    clear to
    me, are those
    due to
    increased sediment
    10
    density, or is there
    a
    temperature density factor
    11
    also?
    12
    DR. GARCIA:
    It could
    be a
    combination
    13
    of all of them.
    14
    MS. DEXTER:
    Okay.
    15
    DR. GARCIA: And we have found, after
    16
    awhile, when
    we look
    at
    the density currents
    that we
    17
    started
    in the -- around 2000, we found
    out
    that
    the
    18
    north branch at times, particularly in the winter,
    19
    it could be
    denser in the main stem, and this had
    to
    20
    do
    with the diversion from Lake Michigan. We
    21
    submitted that, you
    know,
    this would be the
    wind
    22
    blowing, but
    it could also
    be a
    stratified flow.
    At
    23
    the beginning, we thought the temperature was the
    24
    main cause
    of this,
    because it
    was in winter
    so we

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    Page
    64
    1
    contribute.
    2
    But for clarification,
    for
    Bubbly
    3
    Creek, from what
    we know
    so
    far,
    now
    we are
    going to
    4
    do
    more measurements,
    and
    this
    creek
    is going
    to
    5
    measure
    exactly -- you’re
    going
    to
    see what’s
    coming
    6
    out
    of the pumps.
    7
    MS. DEXTER:
    Okay.
    Does the
    8
    temperature
    of the flow
    coming
    out
    of Bubbly
    Creek
    9
    tend
    to be
    warmer
    or
    cooler
    than that in
    the south
    10
    branch?
    11
    DR. GARCIA:
    That’s
    a good question.
    12
    If
    I had
    to guess,
    I
    think
    it’s going
    to
    be cooler
    13
    than what
    is
    there on
    a
    hot
    summer
    day.
    You
    know,
    14
    things
    are sizzling
    pretty
    good.
    That’s
    why
    it’s
    15
    called
    Bubbly
    Creek in the
    summer.
    So
    I
    come and
    16
    look at
    it
    -- we have
    bodies of
    temperature,
    and now
    17
    we’re
    going
    to
    measure
    more,
    but
    I think
    if
    we look,
    18
    we’re probably
    going
    to
    find
    out
    that
    it’s
    going
    to
    19
    be
    cooler.
    20
    Now, having
    said
    that,
    if
    you
    look
    21
    at
    a
    diagram
    -- and
    if
    I could
    just
    take
    a moment
    22
    here
    -- if
    you
    plot
    temperature
    versus density,
    it
    23
    looks
    like
    -- something
    like
    that.
    24
    MS. TIPSORD:
    I’m sorry.
    Dr. Garcia,

    Page 65
    1
    you’re going
    to
    have
    to
    explain that for the
    record.
    2
    DR. GARCIA:
    Oh, okay.
    3
    MS. TIPSORD:
    Remember, people will
    be
    4
    reading
    the transcript and they won’t know what --
    S
    DR. GARCIA: Well, let me
    just say,
    6
    then, in simple words: To create
    -- to
    create the
    7
    density current, just based
    on temperature
    8
    differences, you
    need
    to
    have very large temperature
    9
    differences.
    10
    MS. DEXTER:
    Okay.
    And you don’t
    11
    think
    that those temperature differences
    12
    currently --
    13
    DR. GARCIA:
    I don’t.
    14
    MS. DEXTER:
    There’s not
    a
    great
    15
    difference that you
    know of?
    16
    DR. GARCIA:
    Not in the summer.
    17
    MS. DEXTER:
    Okay.
    18
    DR. GARCIA:
    But if
    you
    probably
    have
    19
    a CSO today,
    it would probably float in Bubbly
    20
    Creek.
    21
    MS. DEXTER:
    All right.
    22
    DR. GARCIA:
    It will
    be
    lighter. So
    23
    you
    will
    have,
    like,
    an
    overflow
    instead of an
    24
    underf low.

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    Page 67
    1
    undeveloped. If
    you don’t have enough density
    2
    difference,
    just
    the
    motion or the water itself will
    3
    disrupt the formation of
    the density current, and
    4
    you’ll just have
    a
    regular river flow,
    or what we
    5
    call
    an open
    channel flow or
    a
    free surface flow.
    I
    6
    don’t
    know if this
    clarifies it.
    7
    MR. GIRARD:
    Yes,
    it did.
    Thank
    you.
    8
    DR. GARCIA:
    The
    difference would have
    9
    to be
    large.
    10
    MS.
    DEXTER:
    Okay. And if that
    -- if
    11
    there was such
    a
    large difference
    and there -- let’s
    12
    see.
    Let
    me
    back
    up
    one
    step.
    13
    How often
    throughout the year
    14
    would you expect a density current
    to
    occur?
    Do
    you
    15
    know that from your model?
    16
    DR. GARCIA:
    You mean
    in Bubbly Creek?
    17
    MS.
    DEXTER:
    Yes.
    In Bubbly Creek,
    18
    how -- is this
    a
    constant
    problem?
    19
    DR. GARCIA:
    We haven’t
    done a long
    20
    term analysis of it
    because we’re still working
    on
    21
    the model,
    but
    depending on
    the conditions of the
    22
    CSO, there’s a sediment. You’re going
    to
    have --
    23
    you
    could have
    a density current when -- amidst
    24
    Bubbly Creek,
    but you
    could
    also have
    -- you
    know,

    Page 68
    1
    Bubbly
    Creek is going
    to
    mix
    up
    pretty
    good, too,
    2
    but
    it’s small compared
    to
    the amount of water that
    3
    comes
    in.
    4
    But
    at
    the junction
    with the south
    5
    branch,
    depending what
    is
    below the sediment, the
    6
    flow
    might
    get
    there and
    just say,
    “I’m going
    to
    7
    continue
    as a
    regular flow,”
    but
    the conditions
    8
    could
    be
    such -- that’s why
    we’re showing one of the
    9
    exhibits
    -- that it made plans and may become
    a
    10
    density
    flow.
    11
    So the answer to your question is
    12
    I don’t
    know,
    because
    it’s going
    to
    depend on the
    13
    frequency of CSO events and the characteristics of
    14
    CSO events,
    and that’s why now we’re going back with
    15
    the
    District, and we are going
    to
    measure exactly --
    16
    not
    just
    the
    flow, how
    much
    is coming
    out, but
    what
    17
    are
    the characteristics of what is coming
    out
    of
    18
    there in terms of suspended solids, BOD, D.O., and
    19
    so
    forth, and other parameters.
    MS. DEXTER:
    Okay.
    21
    DR. GARCIA:
    So the answer is going
    to
    22
    vary.
    It’s going
    to depend
    on -- and the whole
    23
    purpose is,
    you
    know, things are optimized, and TARP
    24
    gets
    bigger. The frequency
    of this flow is going to

    Page 69
    1
    go
    down, and the characteristics
    of the flows are
    2
    going
    to be
    bigger. But as
    long
    as you
    pump, the
    3
    possibility
    of having the phenomenon are going to be
    4
    there.
    5
    MS. DEXTER: Would you
    characterize it
    6
    as
    being
    a
    rare occurrence
    or
    a
    common occurrence
    7
    that
    -- from -- can
    you
    tell right now if this
    is
    8
    something
    that
    you
    think happens quite
    frequently,
    9
    or
    is this something that happens
    more or less --
    10
    DR. GARCIA:
    I
    don’t know how
    11
    frequently
    it happens,
    but
    I think thepotential is
    12
    there
    for this to happen each
    time
    you
    have
    a
    CSO
    13
    event.
    14
    MS. DEXTER:
    Okay.
    15
    DR. GARCIA: The potential is there.
    16
    It
    doesn’t mean that it’s going
    to
    happen
    each time,
    17
    but
    it’s there.
    18
    MS. DEXTER:
    Okay.
    I think that
    19
    covers
    my followup questions, and
    now I’ll
    just
    ask
    20
    my pre-filed
    questions four and five. Do
    you
    know
    21
    if
    the District or the University of
    Illinois,
    22
    Urbana-Champaign, or anyone else to
    your knowledge
    23
    has studied
    fish
    passage
    through the CAWS?
    24
    DR. GARCIA:
    Fish passage?

    Page 70
    1
    MS. DEXTER:
    Fish
    passage.
    You
    2
    mentioned something
    about
    fish
    passage
    standards in
    3
    your testimony.
    4
    DR. GARCIA: Right.
    I
    can tell
    you
    5
    what U
    of I is doing right now. We haven’t studied
    6
    fish
    passage
    in Bubbly Creek, okay? That’s number
    7
    one. What we are doing right now is
    we are
    looking
    8
    at
    a
    small dam located in the northbranch of the
    9
    Chicago River
    just
    before the junction with the
    10
    north shore channel, and the Friends of the Chicago
    11
    River
    wanted
    to
    look
    at the
    possibility
    of
    modifying
    12
    the
    dam and
    put
    in
    a
    fish way there, something they
    13
    call
    a
    fish
    way,
    a fish passage.
    14
    At that time, we were contacted
    by
    15
    the District. U of I was contacted
    by
    the District
    16
    to
    see, you
    know, if we had any experience with
    17
    these, and we had done work in the mid-90s. We
    did
    18
    a
    substantial
    amount
    of work for the state,
    19
    actually. First from IDOT, and then when
    the
    20
    division of water resources went from IDOT
    to
    the
    21
    Illinois Department
    of National Resources
    -- I
    think
    22
    that was with Governor Jim Edgar.
    23
    We were asked
    to
    look
    at a
    way
    to
    24
    prevent drowning accidents
    at
    low hit
    dams,
    and
    the

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    1
    DR. GARCIA:
    So what we did then --
    2
    this
    is how we
    get
    into the fish passage analysis.
    3
    So
    now what we are trying to do in the lab,
    we build
    4
    a
    model.
    We
    have to
    remove the model that we have
    5
    of the
    Chicago River. We have
    a
    model there, and if
    6
    you
    go to
    Wilkie and
    you say
    density currents
    in
    the
    7
    Chicago River, you’re going
    to
    find it, because
    it’s
    8
    going
    to
    take
    you there to a
    picture of the model.
    9
    We had to
    take it
    out because
    we have no more room,
    10
    and
    now we built
    a
    model of
    a
    little bit of
    the
    11
    north shore branch, the
    north shore channel, and
    12
    whatever space
    we have for the north branch.
    13
    And that -- we
    have this very old
    14
    structure,
    and
    as you
    know in September there was
    a
    15
    lot
    of flooding there,
    so
    all of a sudden
    the model
    16
    became very important,
    and what we are trying
    to do
    17
    is
    see
    if
    we can modify
    -- you
    can’t remove it,
    18
    because
    it’s
    a
    great control structure,
    meaning that
    19
    it controls the
    grading of the bottom of the river.
    20
    So
    if
    you
    take that
    out,
    the river is going to
    try
    21
    to
    level itself again,
    and
    all these
    buildings that
    22
    you
    have encroaching
    on the river, they’re -- you’re
    23
    going
    to
    have structural problems.
    24
    But what we’re trying to do
    is

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    Page
    76
    1
    STATE OF ILLINOIS
    SS
    2
    COUNTY
    OF
    COOK
    3
    4
    5
    REBECCA
    A.
    GRAZIANO, being first
    6
    duly
    sworn on oath
    says
    that she is
    a
    court reporter
    7
    doing
    business in the City of Chicago; that she
    8
    reported in shorthand the proceedings
    given
    at
    the
    9
    taking of
    said hearing and that the foregoing is
    a
    10
    true
    and correct transcript of her shorthand notes
    11
    so
    taken
    as
    aforesaid and contains all
    the
    12
    proceedings
    given
    at
    said hearing.
    13
    14
    15
    REBECCA
    A.
    RAZIANO, CSR
    16
    29 South LaSalle Street, Suite 850
    Chicago, Illinois 60603
    17
    License
    No. :
    084-004659
    18
    19
    SUBSCRIBED
    AND SWORN
    TO
    before
    me this 17th
    day
    20
    of February, A.D., 2009.
    21
    Notary Public
    22
    23
    1
    Not&yPubIIe-
    stteof
    HIhb
    24
    MyComEXPlrè5A7.
    2009

    Page 77
    A
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    Page 78
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    63:10
    causing 63:14
    CAWS 69:23
    celebrating
    72:23
    cell
    71:14
    center 1:16 2:12
    4:11
    11:861:2
    centigrade
    63 :21,22 66:9
    66:9,13,22
    Centigrades
    66:17
    certain 34:5
    47:19
    50:20
    52:1,2
    54:4
    chairman 2:4
    3:10
    challenge 72:17
    73:18
    chances 28:6
    53:20
    changes
    55:18
    changing
    15:20
    16:2
    48:18
    channel 18:7
    67:5 70:10
    74:11
    characteristics
    44:7
    68:13,17
    69:1
    characterize
    17:18 69:5
    chart
    13:9,20
    14:22
    15:2,6
    check 6:22 8:19
    Chicago 1:8,17
    2:15 3:5 4:2
    10:11 12:11
    14:7 19:23
    23:18 32:7
    35:5,24 36:3
    37:19,20 38:13
    38:19,21,22
    40:18 41:6
    42:10 44:14
    45:23 46:1,6
    49:24
    51:5
    63:5
    66:15
    70:9,10
    72:24
    74:5,7
    76:7,16
    choose 45:15
    chute
    72:1,4,14
    72:16 75:1,6
    Cicero 21:2 36:6
    circulate 26:4
    circulating
    24:22
    circumstances
    38:8
    citation 57:9

    Page 79
    Citgo 6:11
    city 13:5
    14:19
    21:10,11 76:7
    clarification
    30:12 31:4
    35:16 38:3
    64:2
    clarifies 67:6
    clarify
    22:22
    28:11 29:11
    37:14
    clarifying 14:17
    class 43:22
    clean 33:21
    cleaning 34:20
    Cleanup 33:2 1
    clear 62:9
    clearly 61:7
    close3:23 11:6
    71:2,17
    closed 7:16
    closer 51:4
    60:17
    code
    1:9
    3:7
    15:10 42:16,18
    42:20,23 43:1
    43:5,6,24 44:4
    44:12,13,19,20
    44:22 45:2
    codes
    44:5
    coefficient 53:14
    cold 10:6
    26:16
    27:2 63:1
    colder 26:16
    66:20
    collaboration
    56:6
    colleagues 25:24
    color 15:20 16:2
    16:12 27:12
    colors 50:16
    column 24:16
    39:11 52:22
    53:22
    columns 33:8,12
    33:15
    34:3
    combination
    62:12
    come 5:19 20:11
    22:15 23:11,11
    25:13 48:9
    56:13,14
    64:15
    comes
    9:21
    11:15 12:21
    28:5 51:9 68:3
    coming 10:5
    11:11
    18:3,7
    18:14 20:17
    24:18 28:20,21
    45:24 46:18,21
    46:24 47:10
    48:14 49:15
    50:11 59:23
    60:6 64:5,8
    68:16,17 72:23
    commencing
    1:18
    commercial
    45:18
    commission
    32:12
    common 69:6
    company 32:2 1
    compared 46:17
    60:14 68:2
    comparing 59:4
    59:4
    complete 4:23
    completed 35:14
    36:21
    completely 42:4
    complexity
    16:19
    complicated
    8:10
    17:13
    31:24
    66:15
    components
    43:8
    concentrated
    20:23 32:3
    concentration
    16:10,13,14
    22:17 23:13
    concentrations
    16:17
    conclusion
    27:19 63:4
    conclusions
    61:11
    condition
    5 8:20
    conditions
    11:14
    12:9 19:19
    21:6 41:13
    42:13 45:22
    49:1 52:8
    56:11
    67:21
    68:7
    conference 6:19
    7:1 13:4
    consider 66:10
    consideration
    48:23
    considerations
    44:23
    considered
    53:5
    considering 54:2
    constant 15:15
    67:18
    constantly 29:5
    consultant 32:2 1
    consultants
    44:22
    contacted 70:14
    70:15
    contain 25:11
    contains 76:11
    contaminants
    9:13 10:24
    25:12
    contemporary
    49:12,13,14
    continue 3:21
    4:2
    5:6 39:14
    40:5 68:7
    continuing 8:3
    contribute 47:2
    64:1
    control 1:4,13
    2:2 44:10
    74:18
    controls 74:19
    conversations
    6:12
    Cook
    1:15
    76:2
    cooler 64:9,12
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    cooling 27:3
    copies 13:6
    37:18 50:4
    73:22
    copy 8:15
    57:5,5
    Corn
    6:6
    correct
    26:22
    35:21 51:23
    54:18,23 76:10
    correctly 54:16
    correlation
    21:15
    corresponds
    50:21
    County 1:3,15
    76:2
    course 19:18,22
    28:7 53:23
    courses 44:20
    court 4:20
    76:6
    covers 69:19
    coworkers
    58:7
    create
    65:6,6
    creekll:7,12
    12:11,22 14:11
    14:14
    15:13,19
    16:4 18:14
    20:24 21:4,16
    27:15,22,24
    28:1 35:10,11
    35:17,18 36:16
    37:22 3
    8:23,24
    39:5
    42:3
    46:18,21
    47:6
    47:8,19,23
    48:4,7,14,19
    49:5,9,24
    50:10,15,19
    51:18 55:2
    56:1,10,23
    60:13,20 61:19
    63:12 64:3,4,8
    64:15 65:20
    67:16,17,24
    68:1 70:6
    cross 8:3
    25:21
    CSO 14:11,14
    14:23 15:3,14
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    20:9
    22:17 41:24
    51:19 59:17,21
    60:8 65:19
    67:22 68:13,14
    69:12
    CSOs
    23:11
    28:13
    48:6
    CSR 1:15 76:15
    cubic 15:16
    50:22
    current 9:16
    10:10,12
    13:1
    14:1,6
    16:3
    17:22
    18:17
    19:12
    23:18
    25:17
    27:16
    33:16 65:7
    67:3,14,23
    currently 22:5
    65:12
    currents
    24:1
    26:9 28:14
    35:2
    38:11,12
    62:7,8,16
    63:10,15 74:6
    curve 45:15
    curves
    59:7 60:4
    D
    D 17:14
    daily 44:2
    dam 70:8,12
    71:17
    73:11,13
    73:16
    damage
    73:12
    dams
    70:24
    dash
    58:3,5
    data 17:19
    dates 5:5 7:12
    daughter 71:15
    71:16
    day 1:18 5:24
    6:21 7:14
    26:14 64:13
    76:19
    days 3:20
    5:11
    5:19
    6:4 8:5
    44:1
    Deborah 2:9
    December
    3:24
    decide
    7:5 22:11

    Page 80
    72:5
    75:2
    decided
    22:12
    39:3
    decision
    4:24
    decisions
    33:7
    deep
    24:9
    33:22
    degree
    44:9
    degrees
    63:2 1
    63:21 66:8,9
    66:13,16,22
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    51:3,13
    52:3,4,10,19
    53:18,22 55:11
    55:18
    56:9,21
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    4:5
    dense
    12:23,24
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    19:11
    62:19
    density
    9:11,16
    9:16,18
    10:4,5
    10:10,12 11:10
    12:24
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    17:21
    18:17
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    23:17
    24:1,16
    24:20
    26:9,13
    27:3,15,20
    28:14
    29:21
    35:2
    38:11,11
    62:7,7,10,10
    62:16
    63:9,10
    63:15
    64:22
    65:7
    66:12,24
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    68:10
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    21:11
    55:20
    70:21
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    46:22
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    11:14 12:8
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    67:21
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    72:18
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    72:13
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    71:21 72:1
    detail
    17:4
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    40:17
    41:5 42:11
    54:22
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    developments
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    Dexter
    2:13 7:4
    7:10,17
    60:24
    61:1,1 62:4,14
    64:7 65:10,14
    65:17,21 66:1
    66:4 67:10,17
    68:20
    69:5,14
    69:18 70:1
    75:14
    diagram 64:2 1
    66:12
    Diers
    2:9
    9:7,8
    11:24 12:4,6
    12:10,15 14:16
    14:21 20:15
    22:1,5,9,16,24
    23:3,6,16,22
    26:8,21
    28:18
    29:24
    30:3,9
    30:13,23
    31:2
    32:17
    34:23
    35:6,9,13
    36:20 37:1
    40:15,20
    41:3
    42:14
    45:20
    58:10,15,17,22
    60:22
    difference 10:18
    65:15 66:8,23
    66:23 67:2,8
    67:11 75:7
    differences
    9:18
    63:9
    65:8,9,11
    75:11
    different 10:4
    14:5 15:11
    20:13 38:7,15
    39:24
    42:4
    45:11
    50:16
    53:4,11
    56:1,9
    56:10,20,22
    difficult 51:23
    difficulty 5:21
    diffusion 5 9:23
    59:24
    diluting
    29:6
    dimension 15:8
    dimensional
    49:22 58:14,15
    diminish
    29:9
    direct48:10
    discharge 47:20
    discharging
    15:13 50:20
    disposal
    24:4
    disrupt
    67:3
    dissipate 71:12
    dissolved 10:23
    31:8
    51:6
    54:3
    59:17
    distance
    9:13
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    10:20
    12:1
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    11:1
    District
    2:14 4:2
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    55:4
    56:7 59:5
    59:15 60:10
    61:13 68:15
    69:21 70:15,15
    diversion
    62:20
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    70:20
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    3:7
    Doctor 27:14
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    37:17 38:4
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    8:8 10:22
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    35:23
    36:2,14
    38:10,10,13
    46:13 47:4,22
    48:10 51:16
    53:23 55:1
    60:21
    63:2
    70:5,7 75:12
    76:7
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    12:10,16
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    53:12
    55:8
    61:7
    67:19
    70:17
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    5:15
    10:5
    16:7 18:3,7
    20:17,20 22:15
    24:18
    28:4,5
    28:24 3 1:17
    32:14 36:5,9
    51:1
    59:10
    60:5 62:1
    63:5
    63:7 69:1 71:6
    72:16
    download
    55:12
    57:1
    downstream
    11:13 21:17
    28:9
    Dr2:4,6
    3:13
    7:19,21 8:16
    8:17,18,20,24
    9:2,7,15
    12:3,5
    12:7,14,17
    1 .1 0 1 ‘ 10
    13.IU,I3,1O,
    14:1,3,20
    15:5
    20:16 22:3,7
    22:12,20
    23:2
    23:5,8,21,24
    26:10,23
    27:10
    27:18,23
    28:20
    30:2,7,10,19
    30:22
    31:1,5
    32:19
    35:4,7
    35:11,15,18,22
    36:22
    37:3,10
    37:13,15
    38:2
    40:19,22
    41:1
    41:7
    42:19
    43:4,9,21 46:2
    48:20,22 49:19
    50:7
    54:18,24
    56:24
    57:4,7
    57:11,17,22
    58:2,9,13,16
    58:19,24
    61:5
    61:9,18,22
    62:2,12,15
    64:11,24
    65:2
    65:5,13,16,18
    65:22
    66:2,5,7
    66:11 67:8,16
    67:19 68:21
    69:10,15,24
    70:4
    73:23
    74:1
    75:16
    draw 66:12
    drops5l:11
    59:20
    drowned
    71:19
    drowning
    33:10
    70:24
    71:1,8
    71:13 72:20
    dry
    41:24 48:24
    due 12:20
    51:18
    62:9
    Duluth 24:7
    duly
    76:6
    dump
    24:8
    25:5
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    7:14
    19:18
    27:16
    41:24
    47:2

    Page
    81
    62:6
    Dutch 75:8
    dynamic 15:8
    43:7 47:7
    55:23
    dynamics 15:10
    42:16,18,20,23
    43:1,5 45:6
    48:6 60:19
    D.049:22 58:23
    68:18
    E
    E2:1,1
    each 4:20 61:16
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    early 20:24 33:2
    41:12 43:11
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    72:17 73:4
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    educated 42:12
    EFDC 42:23
    43:2,16,18
    44:6,11 45:9
    45:14
    effect 14:10,13
    46:19 47:17
    48:17
    effects 47:24
    efficient 73:18
    Effluent 1:7 3:4
    effort 8:1
    eight 42:15
    either 7:11
    elaborate 47:18
    Electric 45:4
    elevation 26:18
    40:1
    46:10,17
    47:4
    email 7:3
    emanating
    28:12
    encroaching
    74:22
    end 24:9 52:21
    61:15,22
    energy 47:10,11
    47:12 71:12
    engineer 26:2
    engineering
    49:23 61:6
    enjoy 61:7
    enjoyed 75:17
    enough 12:23,24
    17:1 48:2
    61:14,20
    67:1
    entails
    36:3
    enter 39:13
    entering 10:7
    33:10
    entitled 3:4
    14:10
    entrances 11:8
    environmental
    2:4,8,12 3:23
    4:10
    7:5 37:20
    42:16,18,19,23
    43:1,4 61:2,5
    EPA 9:9 44:19
    44:20 45:4
    equals 22:17
    equation 56:16
    63:17
    equations 50:12
    50:13
    especially 8:5
    essential6l:12
    essentially 14:3
    46:20 47:12
    establish 44:1
    estimated 23:14
    estuaries 43:12
    estuary 44:8
    even 52:19
    60:7
    60:13
    event
    12:21
    15:14 17:21
    41:24 47:3
    51:19 59:17,21
    60:8 69:13
    events 14:11,14
    14:24 15:3
    21:19 27:17
    41:24 48:13
    68:13,14
    eventually 9:23
    Everglades
    43:24
    every 33:20
    everyone 7:22
    8:1
    everything
    8:8
    36:13,19
    exactly
    64:5
    68:15
    exaggerate 66:2
    examination 8:3
    example 11:4
    43:8 44:2 52:6
    53:14
    excuse 37:5
    exercise 23:9
    31:24 59:1,13
    exercises
    51:8
    51:17
    exhibit 4:7,8 9:3
    9:4 14:15,15
    15:3,4 22:16
    23:1 27:10
    29:13 37:18,24
    38:1 42:22
    43:2,3,15,19
    43:19,23 47:1
    49:21 50:2,3
    58:11
    exhibits 50:4
    68:9
    exit 72:2473:2
    expect 67:14
    experience
    55:9
    70:16
    72:20
    experiencing
    31:9
    experimental
    55:3
    experimentally
    56:15
    explain 9:16
    12:15 15:5
    38:18 48:9
    65:1
    explained 36:15
    explaining
    15:10
    explains 17:2
    38:9
    explore 14:5
    15:11
    exposed 45:2
    exposure 45:7
    express 4:24
    extension 28:8
    extensive 8:9
    extent 59:23
    extern 3:17
    extra 50:3
    F
    facell:8
    facing 20:17
    fact73:18
    factor 62:10
    failure 33:5
    fair 51:11
    fairly 51:12
    familiar 34:15
    41:1
    far3:13 6:17
    20:1
    25:18
    28:24
    29:1
    64:3
    fashion 42:12
    fast
    50:18 51:1
    52:17
    53:19
    72:11,12
    73:3
    faster
    47:22
    53:15
    February 1:5,18
    6:20 76:20
    federal 44:2 1
    few 25:4 40:10
    62:6 72:21
    field 25:8 50:16
    63:2
    figure 17:2,3
    22:17 23:4
    26:2 29:13
    42:9 50:12,14
    50:18,21 53:13
    55:18
    58:12,18
    58:19
    59:3,4,6
    59:6
    72:14
    fill 33:16
    finally
    36:18
    71:22
    find 10:17 15:22
    20:19
    25:22
    33:14 41:18
    64:18 74:7
    finding 19:5
    finds 9:22 29:16
    fine20:15 25:13
    31:12 33:11,14
    33:14
    56:13
    57:21
    finish 5:9
    finished 3:24 7:9
    first 9:16 15:24
    16:9 26:4 34:2
    34:4,12 42:17
    59:20 60:15,16
    70:19
    76:5
    fish 26:14,20
    27:5
    45:6
    52:8
    52:23 69:23,24
    70:1,2,6,12,13
    70:13 72:5,13
    72:16 73:15,19
    73:20 74:2
    75:2,8,12
    fishes 72:10
    five 34:24
    66:8
    69:20
    five-year 45:2
    flat 34:4
    flip 73:7
    float 65:19
    flooding 74:15
    flow 9:17,17
    10:7
    11:10
    12:9 15:15
    16:9,18,19,22
    17:13 18:7,10
    18:20
    20:12,17
    20:19,20
    21:6
    27:4
    28:4,5,9
    29:4,5,7,7,15
    29:21
    31:21
    39:24 42:5,6
    45:24 47:9,14
    47:16,20,20
    48:14,16,24
    50:15,23,24
    51:14,15 52:11

    Page 82
    52:16 53:7,18
    55:6,21 56:10
    56:22 62:22
    64:8
    66:24
    67:4,5,5
    68:6,7
    68:10,16,24
    72:15
    flowing 11:3
    flows 9:24
    10:14
    11:2,9,19
    22:13,15 24:12
    24:18 26:13,17
    27:20
    28:12
    29:3
    34:11
    69:1
    fluctuating
    59:10
    fluid42:16,18
    42:23 43:1,4
    fluids
    9:18
    flush 34:6
    folks 73:11 75:6
    follow 27:8
    48:12 54:14
    55:9
    following 75:23
    followup
    4:13
    40:20 69:19
    followups
    62:7
    force 22:7
    Ford 6:12
    foregoing 76:9
    fork 27:17
    37:21
    38:22 40:18
    41:6 46:1
    form 19:11
    25:17
    formation 67:3
    forms 52:23
    forth 11:9 44:15
    44:17 49:2
    68:19
    fortunately
    25:11
    forward 8:10
    found 17:16,22
    24:19 25:1
    49:3,8,14
    62:15,17 72:11
    four 4:12 32:17
    50:4 66:13
    69:20 72:21
    fourth 18:5
    Fox 71:5
    frankly 5:17
    6:10
    Fred48:23
    53:8
    Fredric 2:15
    free67:5
    Freidman 4:4
    frequency 68:13
    68:24
    frequently 21:22
    69:8,11
    freshwater 28:5
    Friday 6:21
    Friends 70:10
    73:16
    from 3:15,17,21
    4:1 5:4,9,22
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    41:11 43:20,21
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    V
    49:9,15 51:9
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    70:19,20 72:6
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    G3:10
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    8:17,18,20,24
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    40:19,22 41:1
    41:7 42:19
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    48:20,22 49:19
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    54:18,24
    56:24
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    64:11,24
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    65:22 66:2,5,7
    66:11 67:8,16
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    69:10,15,24
    70:4 73:23
    74:1 75:16
    Garcia’s 8:16
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    V
    General 45:3
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    12:24 14:6
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    26:2
    Gerick 6:8
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    66:7
    67:7
    Girl 71:15
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    19:24 42:21
    57:4,9 66:18
    71:20 73:19
    given
    6:15,16
    9:17
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    56:19
    gizmo 55:7
    glasses 15:22
    go 5:1,7 9:20
    10:9 11:12,14
    11:20 14:9
    15:7,23 16:1
    16:24 17:2,3,7
    17:24 18:4,18
    18:24 19:4,10
    19:20,21 20:1
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    26:15 28:24
    29:1,6,17,24
    33:20,22
    38:9
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    39:9
    40:6
    42:14
    45:16,22 46:16
    58:23 59:2,3
    60:2,10,18
    66:17 69:1
    71:3,16 72:3
    72:22 73:6,7,8
    73:9 74:6
    75:18
    goes 12:20 16:2
    19:20 20:6
    24:8 27:4
    34:16 38:19
    42:2 51:14
    60:5
    63:7
    going 6:9,18 7:2
    7:8,9
    8:21,22
    10:8,9,9
    11:22
    13:4
    15:18
    17:7,7,8,9,15
    19:5 20:4,7,8
    20:11,12,18,20
    22:723:11,12
    23:13 24:6
    27:6,20,23
    28:7,7,8,9,13
    28:14,24 29:9
    29:15,16,17,18
    29:24 3 1:16
    33:13 36:19
    37:3,4 40:5,5
    41:18 42:8,9
    43:12 45:16
    46:11,18,20,22
    47:2,5,16,18
    47:20,22
    48:14
    50:10,13 51:7
    51:10 53:7
    55:6,24 56:4,4
    56:5,7,8,13,14
    56:14,16,18,21
    58:11 59:1,10
    61:19 63:12,14
    63:23,24 64:3
    64:4,5,12,17
    64:18,18
    65:1
    67:22
    68:1,6
    68:12,14,15,21
    68:22,24
    69:2
    69:3,16
    71:16
    72:3,15,16,17
    73:20
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    75:2
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    64:11,14 68:1
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    74:19
    graduate
    50:8
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    36:3
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    51:2
    grateful 7:24
    68:24

    Page
    83
    Graziano 1:15
    76:5,15
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    61:7
    65:14 74:18
    Greater 2:15
    4:2
    greatest 3 2:23
    ground 25:6
    33:18
    group 40:9
    groups 7:5
    guess
    42:17
    64:12
    H
    half 12:18 22:4
    35:12
    55:7
    60:15
    halfway 3 6:23
    36:24 39:17
    Hambrick 43:9
    hand 4:15
    handout 43:23
    happen
    11:19
    16:17
    17:23
    19:18
    21:21,22
    26:24 29:3
    69:12,16
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    60:8
    happening 19:3
    19:16
    happens 9:17
    17:4 39:9,10
    42:1 51:17
    59:16 60:19
    69:8,9,11
    happy 13:5
    hard 60:5
    having 11:21
    28:6 29:2
    33:10 34:7
    41:21 64:20
    69:3
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    hear 8:23
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    3:3,20,21,24
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    76:12
    hearings 3:18
    7:1,23 8:4
    heavier 63:19,20
    63:23,24
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    53:9
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    helps 8:4
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    highly 55:23
    Highstef 52:6
    him 71:19
    history 22:2 1
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    homogeneous
    41:13
    hope 61:19
    hot 26:13 64:13
    hours
    5
    9:22
    60:7,8
    House 71:6
    houses 49:11
    Huff
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    human 45:7
    hurt
    33:10
    I
    ice 52:9 63:5,6
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    15:7
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    35:24 46:12
    53:15 55:21
    66:18
    71:20
    IDOT 70:19,20
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    4:10
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    1111:9 3:7
    Illinois 1:2,4,13
    1:16,17 2:2,8
    3:22 9:9 14:11
    14:14 32:24
    40:9 49:24
    55:9,12 57:11
    57:22 58:3
    69:21 70:21
    72:7,11 73:9
    76:1,16
    image
    15:24
    16:6 17:14
    images
    15:21
    imaginary 25:2 1
    imagine9:19,19
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    29:1
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    3:11
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    impact 12:13
    21:5 26:9,10
    26:11 27:21,23
    27:24 28:1
    29:9
    impacts
    27:16
    48:18
    implemented
    30:5,15 31:3
    implies 16:2
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    39:20 48:6
    51:22 74:16
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    53:20 54:10
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    indeed 13:7
    17:23
    indicated
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    indication
    53:1
    Induced 14:23
    15:3
    influenced
    59:22
    60:20
    information
    6:14 61:14
    initially 39:1,4
    injecting 49:1
    52:20
    innovations
    32:23
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    instance
    11:5
    28:3
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    Institute 43:10
    intake 20:2
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    31:21
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    58:4
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    intent 5:17
    17:17
    interest 34:1
    58:6
    interface 29:3
    52:11
    intimate 45:14
    introduce 13:20
    14:9
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    intrude 20:17
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    14:13,23 15:3
    19:2,2,22
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    involved 33:1
    40:8,10
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    1
    24:13,13 49:18
    49:22
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    ISWS 58:2
    ISWS-74-R176
    58:5
    Italian 53:2
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    1-55 59:15
    J
    Jack26:1
    James 6:8
    January43:16
    Jeff 6:12
    Jessica 2:13
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    Jim 70:22
    job6l:7
    Joe43:9
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    61:3
    61:21,24
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    11:6
    16:19 18:16
    21:16 68:4
    70:9
    June
    36:18
    just6:10
    8:19
    10:7
    11:13
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    19:24
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    21:20,20 27:10
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    42:1 44:9
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    55:7,7 57:9,18
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    64:21
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    66:18 67:2,4
    68:6,16 69:19
    70:9 73:2
    K
    K1:3
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    29:5
    Kent 3:17
    Kickapoo 72:2
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    kilometers
    10:21 18:12
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    kitchen
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    knew
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    know
    8:6,9
    10:20
    15:16

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    18:19
    19:23
    20:14
    21:20,21
    21:22,23 22:15
    23:16 25:6,22
    26:8,11,14,15
    26:21,23 27:5
    28:18 3
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    32:24 34:15
    39:742:4
    44:21 46:6
    47:13 48:22
    49:4,6,7 51:10
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    59:20
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    63:7
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    68:23 69:10,20
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    69:22
    known 21:11
    43:16,18
    L
    lab 55:2,3 74:3
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    laden 9:12 10:13
    lake 9:20,24
    10:2,7,7
    21:1
    24:3,6,8,10,14
    24:21
    25:5,15
    26:3,5
    27:2
    32:10
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    51:12,13 65:8
    66:8,10 67:9
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    76:16
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    71:12
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    57:14,21
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    61:2
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    3
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    M
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    60:6
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    March 5:7
    Marie 1:12 2:3
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    Marjorie
    72:6
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    Marquette 39:8
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    means 29:14
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    64:5,17
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    measured 22:18

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    23:17,19,22
    58:18
    measurements
    3 1:19
    39:23,23
    40:11
    48:11
    55:10 59:5,15
    60:9 63:2 64:4
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    49:10
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    33:23
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    member3:11,11
    3:13,14 4:22
    memory 18:19
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    mentioned
    23:16 29:12
    70:2
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    Metropolitan
    2:14 4:1
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    Michigan 21:1
    62:20
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    miles 10:21 12:2
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    19:21 36:10
    milligrams
    16:11 22:18
    60:6
    millimeters
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    mind 29:23
    mine 24:5 25:10
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    Miss 60:24
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    mission 40:13
    Mississippi 19:9
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    models
    45:5
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    ninth 3:18
    nitrification
    43:8
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    Notary
    76:2 1
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    Page

    Page
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    table 18:4,5
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    Page
    90
    76:11
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    Page
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