pearl culture waste, nutrient load from land or loss of ... · from land cod in sediment cod in...
TRANSCRIPT
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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?
-
N
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
N
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)
-
N
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)