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- みりあ かつもと
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1 1km 15m 75km 12km 8km 85% COD 29ton 28ton 23ton COD ton 5% 75% COD mg/l 1
2 15km 2 2km
3 km
4 1989 km 15km m km km
5 ,2 4.8cm/s 1.5km 9 5km km km 1.5km
6 Y(cm/s)=1.94*X(cm/s) Y(cm/s)=.889*X(cm/s) RADAR, Y RADAR, Y R cm/s R cm/s ADP(+19m), X ADP(+19m), X cm/s2cm/s 6cm/s4cm/s 7cm/s 15cm/s
7
8 COD
9 Box,1999 o
10 o o e e o o e e o o e o
11 Large Eddy Simulation(LES) 21 Tokyo l 6 Chiba Chlorophyll-a Kawasaki Yokohama Yokosuka Box 3 Box 2 Box 1 Box 4 Kisaradu l 4 Futtsu l 3 l 1 Box 5 Ichihara l 5 l 2 1 Km Chlorophyll-a 1
12 LES Phytoplankton Potential Growth Rate at, 1:.852(day-1) Temperature Coefficient,1: Half saturation for PO4-PKNut:.69(-1).2(mgC/m3) Optimum light intensity for photosynthesisiopt:2(ly/day) Mortality at 2:.3(day-1) Temperature Coefficient 2:.693(-1) Sinking RatewPhy: at mdepth4m:.5(m/day) at Depth4m :.2(m/day) [Chl-a:CPhy] Ratio of Phytoplankton:.26 Nutrient [P:CPhy] Ratio of Phytoplankton.786E-3 Release rate PO4-P from Bottom 4[DO] Detritus Sinking RatewDet: at mdepth4m: 1.(m/day) at Depth4m :.1(m/day) DO Reaeration Coefficientka:.15(day-1) [TOD:CPhy] Ratio of Phytoplankton 3.47E-3 Sediment Oxygen Demand at 2 SOD2 3 Correction Coefficient of Temperature at 2 (T-2) 1.5 Box α Box SOD β
13 () () () () () Box5 Box4 Box3 Box2 Box1 (day) ( ) (u g/l) Salinity (psu) ( ) Temperature () Depth (m) 1 15 Depth (m) Chlorophyll.a (ug/l) ( ) DO (mg/l) ( ) Depth (m) Depth (m) Stn.No Stn.1 Stn.2 Stn.3 Stn.4 Stn.5 Stn.6 Stn.7 Stn.8 Stn.9 Cal.-Jul. Cal.-Aug.
14 ,1991
15 ,1997 2m
16 1mm 2a2b 2
17 COD 1.5mg/l 2 Horie,1991 (,1998)
18 (1993) (1997) (1999) (1999) (2)
19 p. (1997) 36(1)3-35 (2a) (2b) (1999) 11 p.674 (2) (21) MEL1D-MB (1997) 82(8) (2) (1987) 26(4) (1998) 36(1) (1997) DIPDIN 35(1)93-97 (1989) 154p. Horie.T. (1991): Numerical modeling for the prediction of sedimentary improvement by sand capping over a contaminated seabed, Journal Hydraulic Research, 29(6)
20
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