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Transports of Organic Carbon and Nutrients in the Kaoping River-Sea System
J.-J. Hung, H.-M. Yang, E.-T. Yeh, Y.-C. Yeh, C.-M. Ho and I..-J. Lai
Institute of Marine Geology and Chemistry, National Sun Yat-
Sen UniversityKaohsiung, Taiwan E-mail: [email protected]
Outlines
Riverine fluxes of suspended sediment, and dissolved and particulate carbon, nitrogen and phosphorus Meterological conditions vs. riverine fluxes Transformation of riverine CNP in the Kaoping Estuary (net fluxes) Coastal CNP budgets (on-going studies)
Dadson et al., 2003
Kaoping River
1999 2000
里嶺大橋
Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec0
200
400
600
800
1000(C) 歷年平均
2002年
Dis
char
ge
(c.m
.s.)
Time(month)
Sampling period:
Aug/1999-July/2000 (1998-2000 La Nina event)
2002 (2002-04 El Nino event)
Historical
Sampling locations in the Kaoping River
Sampling locations and their elevations and discharge contributions
Sediment Yield(Kaoping watershed)
1999/2000: 3.6*103 g/m2/yr 2002: 0.656*103 g/m2/yr World’s rivers (mean): 150 g/m2/yr Island’s rivers (mean): 3*103 g/m2/yr
# derived from suspended load only
Particle size vs. river discharge (water elevation)
0
20
40
60
80
100
Sampling Date (2007-2008)
>150 µm 63-150 µm 10-63 µm 3-10 µm 0.4-3 µm
Wate
r ele
vati
on
(m
)
Ind
ivid
ual S
ize f
racti
on
(%
)
3
4
5
6
7
8 Water elevation
Pabuk
Typhoon
Wutip
TyphoonSepat
Typhoon
Krosa Typhoon
Dry season
Wet season
0
20
40
60
80
100
Sampling Date (2007-2008)
Fra
cti
on
( %
)
>150 µm 63-150 µm 10-63 µm 3-10 µm
Particulate organic carbon (POC)
Particulate inorganic nitrogen (PON)
0
20
40
60
80
100
Sampling Date (2007-2008)
Fra
cti
on
( %
)
>150 µm 63-150 µm 10-63 µm 3-10 µm
0
20
40
60
80
100
Sampling Date (2007-2008)
Fra
cti
on
(%
)
>150 µm 63-150 µm 10-63 µm 3-10 µm
Particulate organic phosphorus (POP)
0
20
40
60
80
100
Sampling Date (2007-2008)
Fra
cti
on
(%
)
>150 µm 63-150 µm 10-63 µm 3-10 µm
Particulate inorganic phosphorus (PIP)
Chemical Yield(Ca, Mg, K, Na, Cl, SO4, HCO3, Si)
1999/2000: 1.14*103 g/m2/yr
2002: 0.416*103 g/m2/yr
World’s rivers (ave): 33~40 g/m2/yr
63%
1.3%10%
25%
POC PIC DOC DIC
36%33%
31%
DIN DON PON
Transport of C and N in the Kaoping River
Data source: EPA, Taiwan
°ª«Ì·Ë
¨ä¥L
¤u·~¼o¤ô
59%¯bªª¼o¤ô
®a®x¼o¤ô
1%
28%
59%12%
Kaoping River
Industrial
wastewater
Others
DomesticAnimal
wasterwater
1979 1981 1983 1985 1987 1989 1991 1993 1995 1997 1999 2001
0.0
0.5
1.0
1.5
2.0
2.5
3.0
20031977
Kaoping River
NH
4 -
N (
mg
/l)
Time
Foot and Mouth Disease
Nitrogen Fluxes(Anthropogenic contributions)
• Estimated from wastewater discharge: 5.6*104 kg/day
• Estimated from difference between baseline and in-situ measurements: 6.5*104 kg/day (Particulate nitrogen: 4.8 *103 kg/day)
• EPA(ROC) report: 5.7 *104 kg/day
• Anthropogenic contributions to total fluxes: 89% (64715/72977=89%)
Phosphorus Fluxes(Anthropogenic contributions)
• Estimated from wastewater discharge: 4.7 *103 kg/day
• Estimated from the difference between baseline and in-situ measurements: 7.4 *103 kg/day(Particulate P: 4.4 *103 kg/day)
• EPA(ROC) report: 1.3 *104 kg/day
• Anthropogenic contributions to total fluxes: 61% (7399/12124=61%)
Carbon and nutrient yields from the Kaoping Watershed
08/1999-07/2000 (a)2002
(b)a/b
Discharge (cms) 270 102 2.6
POC (g/m2/yr) 44.9 2.92 15.4
PIC (g/m2/yr) 18.4 1.27 14.5
DOC (g/m2/yr) 2.27 1.8 1.3
DIC (g/m2/yr) 111 47.7 2.3
PN (g/m2/yr) 0.70 0.47 1.5
DIN (mol/m2/yr) 0.59 0.13 4.5
DIP (mmol/m2/yr) 6.29 5.43 1.2
DSi (mol/m2/yr) 0.41 0.31 1.3
Meterological conditions primarily determine the material fluxes and proportions of natural and ant
hropogenic contributions
119°E 122°E
26° N
Taiwan Strait
24° N
22° N
Kaoping River
121°E
0 5 10 15 20 25 30 35
0
2
4
6
8
10
12
14
16
18
SR
P (µ
M)
Salinity
Surface Bottom
0
50
100
150
200
250
300
350
DO
(µM)
0 5 10 15 20 25 30 35
0
10
20
30
40
50
60
70
Nitr
ate+
Nitr
ite (
µM)
Salinity
Surface Bottom
0
50
100
150
200
250
300
350
DO
DO
(µM)
0 5 10 15 20 25 30 35
0
50
100
150
200
250
300
350
Sili
cate
(µM
)
Salinity
Surface Bottom
0
50
100
150
200
250
300
350
DO
DO
(µM)
0 5 10 15 20 25 30 35
0
50
100
150
200
250
300
350
DO
(µM
)
Salinity
DO
6.8
7.0
7.2
7.4
7.6
7.8
8.0
8.2
pH-DO (r=0.8119, p<0.0001)
pH
Dec./20030 5 10 15 20 25 30 35
0
10
20
30
40
50
60
Dec/2003
Chl-a (µg
l-1)
Salinity
Surface Bottom
DO
0 10 20 30 40
0
10
20
30
40
50
60
70
SR
P (
µM)
July,1999
NH4
NO2
NO3
DIN
Nitr
ogen
Con
cent
ratio
n (
µM)
0 10 20 30 40
0.0
0.4
0.8
1.2
1.60 10 20 30 40
0
5
10
15
20
25
Si (
µM)
0 10 20 30 40
0
2
4
6
Chl
a (µ
g l-1
)
July, 2003
Salinity Salinity
-12 -8 -4 0 4 8 12 16 20 24 28 320
50
100
150
200
250
300
350
40011/22/1989
River st.
C
DO
C (
µ M
)
Salinity
1. Dissolved inorganic nutrients (except for DIP-addition in high S range) and DOC were transported conservatively through the estuary during the wet season.
2. Nitrate reduction/denitrification occurred in the low S range during the dry season
3. Non-conservative transports - for particulate phases of carbon and nutrients
4. Using Biogeochemical (box) model to derive net fluxes
0
1
2
3
4
5
6
POC
( m
g L
-1 )
KPR941018
0 5 10 15 20 25 30 35
SurfaceMiddleBottom
Salinity10 9 8 7
Station
圖 2 -1、 高 屏 海 域 採 樣 站 位 圖
Lat
itud
e (N
)
L o n g itu d e (E )
A 1
A 2
A 3
A 4
B 1B 2
B 3
B 4
B 5C 1
C 2
C 3
C 4
D 1
D 2
D 3E 1
E 2
E 3
1 2 0 .31 2 0 .1 1 2 0 .5
2 2 .5
2 2 .7
2 2 .3
2 2 .1
K a o p in g R iv er
T u n gk a n g R iver
T ap on g B ay
L iu ch iu Islan d
Dissolved
CNP
Budgets
Particulate CNP
Budgets
Kaoping Watershed
Kaoping Estuary● Addition● Removal
River
Dissolved Particulater matter
Netfluxes Coastal Zone
● Primary production● Recycling
Sediments ● Recycled ● Preserved
SettlingDissolvedRelease Denitrification
Carbon, Nitrogen and Phosphorus Budgets
On-going studies
圖4-1、研究期間於高屏海域各測站之溫鹽圖
0
4
8
12
16
20
24
28
3231.532.032.533.033.534.034.535.0
CR724 ( 2001/08 ) KW SCS A1 A4 B1 B3 B5 C1 C4
SCS
KW
Temperature ( °C )
Salinity
0
4
8
12
16
20
24
28
3231.532.032.533.033.534.034.535.0
CR738 ( 2001/11 ) KW SCS A1 A4 B1 B3 B5 C1 C4
SCS
KW
Temperature ( °C )
Salinity
0
4
8
12
16
20
24
28
3231.532.032.533.033.534.034.535.0
CR762 ( 2002/03 ) KW SCS A1 A4 B1 B3 B5 C1 C4
SCS
KW
Temperature ( °C )
Salinity
0 4000 8000 12000 16000 200000.00.10.20.30.40.5
DIP
( µ
M )
Discharge ( m3 month-1 )
0 4000 8000 12000 16000 200000.51.01.52.02.53.0
DIN
( µ
M )
0 4000 8000 12000 16000 2000002468
101214
DS
i ( µ
M )
0 4000 8000 12000 16000 200000.00.30.60.91.21.5
Ch
l. a
( µ
g L
-1 )
0 4000 8000 12000 16000 200002.02.53.03.54.04.55.0
TS
M (
mg
L-1 )
圖 4-42、高屏溪輸出流量對高屏海域各化學參數( D O C、D O N、D O P、
PO C、 PN、 T SM、 C hl. a、 D Si、 D IN 及 D IP)平均濃度分佈之影響
0 4000 8000 12000 16000 200000.00.30.60.91.2
PN
( µ
M )
D ischarge ( m 3 m on th -1 )
0 4000 8000 12000 16000 200002468
1012
PO
C (
µM
)
0 4000 8000 12000 16000 200000.20.30.40.50.60.7
DO
P (
µM
)
0 4000 8000 12000 16000 200006
8
10
12
DO
N (
µM
)
0 4000 8000 12000 16000 20000
708090
100110120
DO
C (
µM
)
表 4-3、研究期間於高屏海域 DIP<0.2μM、DIN<1μM、P及 N limitation zone之百分比
P limitation zone (%) N limitation zone (%) Cruise
DIP<0.2μM (%) DIP<0.2μM N/P>30
DIN<1μM (%) DIN<1μM N/P<10
724 ( 2001/08 ) 56 - 42 42 738 ( 2001/11 ) 86 - 21 4 762 ( 2002/03 ) 75 - 46 7 797 ( 2002/07 ) 65 4 35 13 837 ( 2002/12 ) 96 - 72 38 853 ( 2003/03 ) 86 3 31 11
0.0 0.2 0.4 0.6 0.8
0
40
80
120
160
Chl. a ( µg L-1 )
P=0.0822R=0.4212
Chl. a ( µg L-1 )
DCR ( mg C m
-3 d
-1 )
0.0 0.2 0.4 0.6 0.8
0
50
100
150
200
250R=0.2680P=0.0076
GP ( mg C m
-3 d
-1 )
0 2 4 6 8 10 12
0
40
80
120
160
DIN ( µM )
P=0.0694R=0.4972
DIN ( µM )
DCR ( mg C m
-3 d
-1 )
0 2 4 6 8 10 12
0
50
100
150
200
250 R=0.4154P<0.0001
GP ( mg C m
-3 d
-1 )
0.0 0.4 0.8 1.2 1.6 2.0
0
40
80
120
160
DIP ( µM )
P=0.0860R=0.3999
DIP ( µM )
DCR ( mg C m
-3 d
-1 )
0.0 0.4 0.8 1.2 1.6 2.0
0
50
100
150
200
250 R=0.4791P<0.0001
GP ( mg C m
-3 d
-1 )
圖 4-50、研究期間高屏海域GP/DCR Ratio於各站位之分佈圖
0
2
4
6
Ratio = 1
Mar-02 Jul-02 Dec-02 Mar-03
A1 B1 B3 B5 C1
GP
/ D
CR
( R
atio
)
Time ( month )