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EMECS 9 2011 Aug 28 Satoshi Chiba Faculty of Environmental and Information Sciences, Yokkaichi University, Mie, Japan Yasuhiro Shimizu , Hideki Kokubu, Hiroshi Tachi Mie Prefecture Fisheries Research Institute, Mie, Japan Pearl Culture Waste, Nutrient Load from Land or Loss of Tidal Flat, What is the Cause of the Deterioration and what should be controlled for the Restoration of Ago Bay Environment?

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  • EMECS 9 2011 Aug 28

    Satoshi Chiba

    Faculty of Environmental and Information Sciences,

    Yokkaichi University, Mie, Japan

    Yasuhiro Shimizu , Hideki Kokubu, Hiroshi Tachi

    Mie Prefecture Fisheries Research Institute, Mie, Japan

    Pearl Culture Waste, Nutrient Load from Land

    or Loss of Tidal Flat, What is the Cause of the

    Deterioration and what should be controlled

    for the Restoration of Ago Bay Environment?

  • 0 1 2 3 4km

    Ugata

    Inlet

    Shinmei

    Inlet

    Tategami

    Inlet

    Funakoshi

    Inlet

    Hamajima

    Inlet

    Location, Landscape and Bathymetry of Ago Bay

    Owase

    Kumano

    Ago Bay

    Tsu

    Ise Bay

    Yokkaichi

    Pacific Ocean

    N

    Nagoya

    Islands of Japan

    Ago Bay

    Pacific

    Ocean

    Ise

    Bay

  • Environmental Problems of Ago Bay

    1. Organic Pollution in Sediment

    2. Hypoxia in Water Column

    3. Reduction of Benthos Diversity and Density

    4. Break Out of Toxic Plankton and Infectious

    Disease for Pearl Oyster

  • History of Environmental

    Matters

    1900 1920 1940 1960 1980 2000 2020

    Nutrient Load

    From LandCOD

    in Sediment

    COD in

    Water Colum

    Pearl

    Production

    DO in Water

    near Seafloor

    Reclamation

    Red Tide

    Hypoxia in water column

    Toxic Dinoflagellate,

    Infectious Disease of

    Pearl Oyster

    YEAR

    Mass Mortality of Pearl Oyster

    Birth of Pearl

    Culture

    WW2

    70mg/g-dw

    30mg/g-dw

    50ton/y

    100tonN/y

    200tonN/y

    5ton/y

    Nutrient Load

    From Outer Sea

  • Previous Research for Environment of Ago bay

    Research for the organic pollution by the pearl culture

    Research for the material budget around Ago bay

    • Y.Sawada and M.Taniguchi (1968)

    • H.Uemoto (1981)

    • S.Ueno, et.al. (2000)

    • others

    • Ago Bay Project (2003-2007)

  • Objectives of This Study

    1. To quantify the effect of several environmental

    factors on organic pollution of sediment and

    hypoxia in seawater of Ago bay, with the aid of

    numerical models.

    2. To provide helpful data for policy making and

    restoration activity in the future.

  • Hydrodynamic Model

    Physiology Model

    Of Pearl Oyster(3-Generation Model)

    Pelagic Ecosystem

    Model

    Early Diagenesis Model

    of Sediment

    Numerical Models of Ago Bay

    Not Coupled.

    Coupled

    Coupled

  • Mean Distance Between Rafts : 38m

    Raft Width : 6m (typical)

    Me

    an

    Wa

    ter

    De

    pth

    = 1

    0m

    Enhanced

    Sedimentation

    Water Surface

    Sediment

    Waste

    Deposition

    Localization of POC Sedimentation of

    Suspended Pearl Culture

    Trapping of

    PlanktonPearl Oysters

    DispersionReduced

    Sedimentation

    Anoxia

  • Block Division of Sediment Model

    All the waste from the pearl

    culture is assumed to settle

    on the culture area.

    Hamajim

    a

    Ugata

    Shinmei

    Tategami

    GozaFunakoshi

    Fukaya

    Wagu

    12

    3

    4

    5

    6

    789

    10

    Non-Culture

    Area

    Culture

    Areaone-tenth of N-C Area

    Sediment

    Model

    Pelagic

    Ecosystem

    Model

    One Block

    Vertical section (image)

  • Ugata

    WD=12.8m

    Tategami

    WD=9.0m

    Takonobori

    WD=26.7m

    0m

    20m

    40m

    Water Depth

    Location of Observation Sites

  • J A S O N D J F M A M J J A S O N D

    J A S O N D J F M A M J J A S O N D

    Comparison of Dissolved Oxygen in Water Column

    Observed Data at Takonobori Unit(mgO2/liter)2003 July 1 to 2004 Dec.31

    Computational Result for Takonobori

    Observed Data at Tategami

    Computational Result for Tategami

  • 0

    5

    10

    15

    20

    25

    30

    0 10 20 30 40 50

    Dep

    th(cm)

    POC(mgC/g-dw)

    Tategami

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 10 20 30 40 50

    Dep

    th(cm)

    POC(mgC/g-dw)

    Takonobori

    Non-Culture Zone

    Culture Zone

    Observation

    Comparison of POC in Sediment

  • 0

    5

    10

    15

    20

    25

    30

    0 1 2 3

    Dep

    th(cm)

    FeS(mgS/g-dw)

    Tategami

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 1 2 3

    Dep

    th(cm)

    FeS(mgS/g-dw)

    Takonobori

    Non-Culture Zone

    Culture Zone

    Observation

    Comparison of FeS in Sediment

  • Calculation Cases

    Case Name

    Heterocapsa

    Circulari

    Squama

    Nutirent

    Load

    from

    Land

    Nutrient

    Load

    from

    Outer

    Sea

    Factor for

    Number of

    Cultured

    Pearl

    Oysters

    Tidal

    Flat

    Returning

    Factor of

    Nutrient

    from TF

    nonhetero None 100% 100% 1.0 None

    land50%

    (nh)None 50% 100% 1.0 None

    ocean50%

    (nh)None 100% 50% 1.0 None

    akoya5(nh) None 100% 100% 5.0 None

    tflat0(nh) None 100% 100% 1.0 Included 0.0

    tflat1(nh) None 100% 100% 1.0 Included 1.0

    hetero Included 100% 100% 1.0 None

    tflat0(h) Included 100% 100% 1.0 Included 0.0

    Note : (h) and (nh) indicate condition with and without Heterocapsa Circularisquama.

    Tidal flat area : 266 hectare

  • 1.18

    1.02

    1.10

    1.10

    1.14

    1.23

    0.8 1.0 1.2 1.4

    nonhetero

    land50%(nh)

    ocean50%(nh)

    akoya5(nh)

    tflat0(nh)

    tflat1(nh)

    GPP(gC/m2/day)

    Gross Primary Production and POC Loading on Sea FloorAverage of Bay Head Area in Warm Months (May to October)

    2.126

    1.653

    1.882

    1.446

    1.938

    2.062

    0.116

    0.067

    0.105

    0.231

    0.100

    0.122

    0.0 1.0 2.0 3.0

    POC Loading (tonC/day)

    POC Loading without Culture Waste

    POC Loading due to Culture Waste

    decrease!!

  • Nitrogen Budget in Ago Bay

    360

    350

    194

    274 13 160

    127

    Unit:ton-

    N/year

    Case : Nonhetero

    Elution

    Culture

    WastePON

    Sea Floor

    Permanent

    Sedimentation

    Land

    (without toxic plankton)

    287=

    353

    357

    194

    217 31 135

    113

    Case : Akoya5

    Elution

    Culture

    WastePON

    Sea Floor

    Permanent

    Sedimentation

    Land

    (Increased oyster density)

    Outer

    Sea

    Outer

    Sea

    248=

  • 0.21

    0.16

    0.18

    0.14

    0.19

    0.20

    0.32

    0.23

    0.29

    0.37

    0.29

    0.32

    0.0 0.1 0.2 0.3 0.4 0.5

    nonhetero

    land50%(nh)

    ocean50%(nh)

    akoya5(nh)

    tflat0(nh)

    tflat1(nh)

    POC Flux (gC/m2/day)

    POC Flux of Non-Culture Area

    POC Flux of Culture Area

    POC Flux to Sea Floor around Bay Head Area

    Culture Area Non-Culture Area

    POC FluxPOC Flux

    Increase,

    but slightly!

  • 0.08

    0.03

    0.02

    0.02

    0.06

    0.09

    0.26

    0.18

    0.0 0.1 0.2 0.3 0.4

    nonhetero

    land50%(nh)

    ocean50%(nh)

    akoya5(nh)

    tflat0(nh)

    tflat1(nh)

    hetero

    tflat0(h)

    Hypoxic Area (km2)

    Average Hypoxic Area of

    Seafloor during May to October

    0.0

    1.0

    2.0

    3.0

    4.0

    J F M A M J J A S O N D

    Hypoxic

    Are

    a

    (Km

    2)

    hetero

    0.0

    1.0

    2.0

    3.0

    4.0

    J F M A M J J A S O N D

    Hyp

    oxic

    Are

    a

    (Km

    2)

    nonhetero

    Hypoxic Area of Seafloor

    Effective

    for hypoxia

    reduction

  • 0.91

    0.60

    0.75

    0.26

    0.78

    0.99

    1.31

    1.13

    1.25

    1.25

    1.25

    1.21

    0.0 0.5 1.0 1.5 2.0

    nonhetero

    land50%(nh)

    ocean50%(nh)

    akoya5(nh)

    tflat0(nh)

    tflat1(nh)

    FeS(mgS/g-dw)

    Non-Culture Area Culture Area

    18.8

    15.5

    16.6

    12.4

    17.3

    18.8

    26.3

    20.9

    23.2

    26.6

    23.9

    26.5

    10 15 20 25 30 35

    nonhetero

    land50%(nh)

    ocean50%(nh)

    akoya5(nh)

    tflat0(nh)

    tflat1(nh)

    POC (mgC/g-dw)

    Non-Culture Area Culture Area

    Average POC in Upper 3cm of

    Surface Sediment at Tategami

    Average FeS in Upper 3cm of

    Surface Sediment at Tategami

  • Evaluation of Environmental Factors

    Environmental

    Factor

    Hypoxia in

    Water Column

    OM Accumulation

    in Sediment of

    Non-Culture Area

    OM Accumulation

    in Sediment of

    Culture Area

    Nutrient Loading

    from LandE E E

    Nutrient Loading

    from Outer SeaE E E

    Pearl Culture R R E

    Tidal Flat R R R

    Heterocapsa

    CircularisquamaE U U

    E : Enhance, R : Reduce, U : Unknown

  • • This study with new computer models quantified

    the effect of several environmental factors and

    brought some new insights for the environmental

    deterioration of Ago bay.

    Summary

  • • The nutrient loading from the drainage area and

    the outer sea are found to be the most probable

    cause for the environmental change for recent

    years, and it corresponds to the actual change of

    nutrient loading.

    Summary (continued)

  • • Although the pearl culture enhances the organic

    pollution in the sediment near the raft, it also

    reduces the organic pollution in the non-culture

    area and the hypoxia in the water column.

    Summary (Continued)

  • • The effect of tidal flat for environmental change

    was not significant. It is clear that the present

    model neglects the biological aspect for the tidal

    flat such as the role of the nursing for marine

    creatures. This suggests the need for the

    simulation with the higher trophic model.

    Summary (Continued)

  • END

    Thank you for your cooperation.

  • Information of Ago BayGovernmental

    body

    Shima City

    Drainage Area abt.70km2

    Water Basin

    Area

    abt.25km2

    Population in

    Drainage Basin

    abt.36,000

    Number of

    tourists

    abt.10million/y

  • Pearl Oysters in culture net

    Maintenance Work (Shell Cleaning)

    Harvest of Pearls

    Pearl Oyster(pinctada fucata

    martensii)

    All photos were taken

    by T.Atsumi.

    Culture Raft

    Number of groups

    farming pearl culture

    abt.500

    Number of pearl oysters abt.100 mill.

    Population density of p.o. abt.4 /m2

    Information of Pearl Culture

  • Hypoxic Water Distribution

    2003 Sep.11

    2003 Aug.21 2003 Aug.26

    3 mgO2/L

    2 mgO2/L

    Dissolved Oxygen data were

    measured at 26 sites in the bay

    from observation vessel and

    processed as 3-D contour map.

    Bay Mouth Bay Mouth

    Bay Center

    Bay Head

    Bay Mouth

    Contour Level

  • Seasonal Change of Benthos Population

    Benthos Data (2002)

    Unpublished data for the benthos population by Naoa Hata of

    Mie Prefecture Fisheries Research Institute, 2002.

    0

    1000

    2000

    3000

    4000

    5000

    1 2 8 9 10 11 12 13 14 15 16 19 20 21 22 23 24 25 26 27 28 29 30 31 32

    Nu

    m.o

    fIn

    div

    idu

    als

    (1/m

    2)

    Site No.

    2002 April

    0

    1000

    2000

    3000

    4000

    5000

    1 2 8 9 10 11 12 13 14 15 16 19 20 21 22 23 24 25 26 27 28 29 30 31 32

    Num

    .of In

    div

    idu

    als

    (1

    /m2

    )

    Site No.

    2002 September

    Protochordate

    Echinodermata

    Pogonophora

    Arthropoda

    Mollusca

    Tentaculata

    Annelida

    Sipuncula

    Nemertea

    Platyhelminthes

    Coelenterata

    April September

    Wet

    Weight17.1 g/m2 10.7 g/m2

    Number of

    Individuals 3098 /m2 764 /m2

  • Feature of Numerical Models

    1. Three-dimensional, Time Dependent, Hydro-Static Model

    2. Sea Surface Conformed Grid System

    3. Quickest Scheme for Advection

    4. Time Splitting Integration for External and Internal Modes

    5. One Equation Turbulent Model (M & Y Level 2.0 Modification)

    1. (ERSEM Like) Low Trophic Model

    2. Coupled with Pearl Oyster Model

    3. Coupled with Sedimentary Model

    1. One-dimensional Early Diagenesis Model

    2. Ideas of H.Fossing (2004) and P.Berg (2003) are largely

    borrowed for set-up.

    Pelagic Ecosystem Model (original)

    Sedimentary Model (original)

    Hydrodynamic Model (original)

  • X

    ZY

    20

    0m

    Region I (Offshore Region,

    X axis : Eastward, Y axis : Northward)

    Region II (Core of

    Ago Bay Region)Region II

    Grid System of Numerical Models

    Lo

    we

    r P

    art

    (F

    ixe

    d)

    Up

    pe

    r P

    art

    (Mo

    va

    ble

    ) High Water

    Low Waterabt.2m

    7grids

    28m

    18grids

    abt.3m

    Vertical Arrangement of Grids

  • Model of Pelagic Ecosystem

    Diatom

    Dinoflagellates

    Zooplankton

    DIP

    DIN POP

    PON

    Dissolved

    OxygenPhotosynthesis

    respiration

    Settling

    Effluent

    Consumption by sediment

    Predation

    Uptake

    ReleaseDeath

    Atmospheric

    OxygenSea Surface

    Sediment

    Sun Ray

    Exchange with

    Outer Sea

    POC

    DOP

    DON

    DOC

    Consumption by OM dissolution

    Dissolution

    Dissolved

    Organic Matter

    Particulare

    Organic Matter

    Inorganic

    Nutrient

    Resuspension

    Pearl Oyster

    Egestion

    Inflow from

    Drainage Basin

    Waste of

    Shell Cleaning

    DIP

    DINCell

    Quota

    DIN, DIP

    respiration

    respiration

    Effluent

    Settling

    Predation

    Egestion

    Mortality

    Dis-

    solution

    Dis-

    solution

    Release

    Egestion

  • Model Geometry (1-D)

    Sediment ModelSea Bed

    Computational Cell

    z

    DBL

    Bottom Boundary

    Upper Boundary

    Early Diagenesis Model

    30 c

    m in

    dep

    th, 60 G

    rid

    Po

    ints

    Bio-GeoChemical

    Reactions

  • J A S O N D J F M A M J J A S O N D

    J A S O N D J F M A M J J A S O N D

    Computational Result for Tategami

    Comparison of Salinity in Water Column

    Observed Data at Tategami

    Observed Data at Takonobori Unit(PSU)2003 July 1 to 2004 Dec.31

    Computational Result for Takonobori

  • 2003 July 1 to 2004 Dec.31

    Computational Result for St.B

    Comparison of Sea Water Temperature

    Observed Data at St.B

    Computational Result for St.A

    Observed Data at St.A Unit(Celsius)

  • Note: Heterocapsa Circulary Squama

    included in the computation.

    Unit(μg/liter)

    2003 July 1 to 2004 Dec.31

    Computational Result for St.B

    Comparison of Chlorophyll

    Observed Data at St.B

    Computational Result for St.A

    Observed Data at St.A

    Note: Heterocapsa Circulary Squama

    included in the computation.

  • 0

    5

    10

    15

    20

    25

    30

    0 1 2 3

    De

    pth

    (cm

    )

    FeS(mgS/g-dw)

    Tategami

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 1 2 3 D

    ep

    th(c

    m)

    FeS(mgS/g-dw)

    Ugata

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 1 2 3

    De

    pth

    (cm

    )

    FeS(mgS/g-dw)

    Takonobori

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 10 20 30 40 50

    De

    pth

    (cm

    )

    POC(mgC/g-dw)

    Tategami

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 10 20 30 40 50

    De

    pth

    (cm

    )

    POC(mgC/g-dw)

    Ugata

    Non-Culture Zone

    Culture Zone

    Observation

    0

    5

    10

    15

    20

    25

    30

    0 10 20 30 40 50

    De

    pth

    (cm

    )

    POC(mgC/g-dw)

    Takonobori

    Non-Culture Zone

    Culture Zone

    Observation

    Comparison of POC and FeS in Sediment

  • Gross Primary Production- Comparison with Observation Data -

    Solid Line : Computational Results for 2004

    Solid Circle : Observation data in 2009

    Calculation Case : nonhetero

    0.0

    1.0

    2.0

    3.0

    4.0

    5.0

    GP

    P (

    gC/m

    2/d

    ay)

    J F M A M J J A S O N D

    0.0

    1.0

    2.0

    3.0

    4.0

    5.0

    GP

    P (

    gC/m

    2/d

    ay)

    Takonobori (Bay Center) Tategami (Bay Head)

    J F M A M J J A S O N D

  • 0

    2

    4

    6

    8

    10

    12

    J F M A M J J A S O N D

    Dis

    so

    lve

    d O

    xyg

    en

    (m

    gO

    2/L

    )

    nonheteroland50%ocean50%akoya5tflat0observation data

    0

    2

    4

    6

    8

    10

    12

    J F M A M J J A S O N D

    Dis

    so

    lve

    d O

    xyg

    en

    (m

    gO

    2/L

    )heterononheteroobservation data

    3mgO2/L

    Dissolved Oxygen in Water Column near Sea Floor at Tategami

    Data of 2004

  • 11.4

    8.4

    10.9

    4.4

    15.8

    27.3

    19.0

    25.2

    13.3

    40.3

    0 10 20 30 40 50

    1

    2

    3

    4

    5

    Blo

    ck N

    o.

    Eflux of H2S (mgS/m2/day)

    Non-Culture Area Culture Area

    Ugata

    0

    2

    4

    6

    8

    10

    0 100 200 300 400

    De

    pth

    (cm

    )

    H2S(μM)

    Culture Area

    1112131415

    0

    2

    4

    6

    8

    10

    0 100 200 300 400

    De

    pth

    (cm

    )

    H2S(μM)

    Non-Culture Area

    1 2 3

    4 5

    Average H2S Eflux

    During Warm MonthsVertical Distribution of H2S

    on September at Tategami

    Tategami

    All data : Nonhetero Condition

  • Increase of Nutrient Load from

    Drainage Area & Outer Sea

    Excess Deposition of Organic

    Waste from Pearl Culture

    Hypoxia in

    Water Column

    Decrease of Decomposition

    rate of OM and Vertical-Mixing

    Capability of sediment

    Enrichment of

    Sediment

    Attenuation of Benthos

    Increase of Toxic

    Dinofllagelate

    Increase of Anoxic

    Decomposition

    The Sequence of Environmental Deterioration

    in Ago Bay (Estimation)