

FOLLOWUS
MEES Institute of Oceanology the Chinese Academy of Sciences
Online First:31 January 2013,
Published:2003
Scan QR Code
Jinming, S., Yanxin, L., Xiaoxia, L. et al. Forms of phosphorus and silicon in the natural grain size surface sediments of the southern Bohai Sea., Chin. J. Ocean. Limnol. 21, 286–292 (2003). https://doi.org/10.1007/BF02842845
The forms of phosphorus and silicon in the natural grain sizes surface sediments of the southern Bohai Sea were studied. In sediments
the organic matter bound form of phosphorus was the main form of transferable phosphorus and ranged from 0.37 μmol/g to 1.57 μmol/g
accounting for 10.7% of the total phosphorus
others were the carbonate bound form
iron-manganese oxide bound form and ion-exchange able form; the transferable form of phosphorus accounted for 19.2% of the total phosphorus. Silicon’s carbonate bound form was predominant over others among its transferable forms
and content ranged from 1.55 μmol/g to 8.94 μmol/g
accounting for 0.05% of the total silicon; the total amount of transferable silicon forms accounted for only 0.12% of the total silicon. Therefore
19.2% of the total phosphorus and 0.12% of the total silicon contained in the surface sediments of the southern Bohai Sea could participate in the biogeochemical cycling.
Aller, R. C., Yingst, Y., 1985. Effect of the marine deposit-feeders Heteromastus Filiformis (Polychaeta), Macroma Baltica (Bivalvia) and Tellina Texana (Bivalvia) on averaged sedimentary solute transport, reaction rates and microbial distributions.J. Mar. Res. 43: 615–645.
Conley, D. J., Johnstone, R. W., 1995. Biogeochemistry of N, P, and Si in Baltic Sea sediments: Response to a simulated deposition of a spring diatom bloom.Mar. Ecol. Prog. Ser. 122(1–3): 266–276.
Conter, J. B., Waizel, R. G., 1992, Uptake of dissolved inorganic and organic phosphorus compounds by phytoplankton and bacterioplankton.Limnol. Oceanol. 37(2): 232–243.
Gehlen, M., Malschaert, H., van Raaphorst, W. R., 1995. Spatial and temporal variability of benthic silica fluxes in the southeastern North Sea.Continental Shelf Res. 15(13): 1675–1696.
Mortlock, A. R., Froelich, P. N., 1989. A simple method for the rapid determination of biogenic opal in pelagic marine sediments.Deep-Sea Res. 36(9): 1415–1426.
Overnell, J., 1995. Sediment water column coupling and the fate of the spring phytoplankton bloom in Loch Linnhe a Scottish fjordic sea-loch, Sediment process and sediment-water fluxes.Estuar. Coast. Shelf 41(1): 1–10.
Ruttenberg, K. C., 1992. Development of a sequential extraction method for different forms of phosphorus in marine sediments.Limnol. Oceanogr. 37: 1460–1482.
Song, J. M., 1997. Chemistry of sediment-seawater interface of the China Seas. China Ocean Press, Beijing, 222p.
Song, J. M., 2001. Transferable phosphorus on sediments of the Huanghe River estuary’s adjacent waters,Chin. J. Oceanol. Limnol. 19(1): 81–86.
Song, J. M., Luo, Y. X., Li, P. C. et al., 2000. Phosphorus and silicon in sediments near sediment-seawater interface of the southern Bohai Sea.The Yellow Sea 6: 59–72.
Tarpchak, S., Moll, R. A., 1990. Phosphorus sources for phytoplankton and bacteria in Lake Michigan,J. Plankton Res. 12: 743–758.
Tessler, A., 1979. Sequential Extraction Procedure for the Speciation of Particulate Trace Metals.Anal. Chem. 51 (7): 844–850.
Vaithiyanathan, P., Jha, P. K., Subramanian, V., 1993. Phosphorus distribution in the sediments of the Hooghly (Ganges) Estuary, India.Estuar. Coast. and Shelf Sci. 37: 603–614.
van Duyl, F. C., van Raaphorst, W., Kop, A. J., 1993. Benthic bacterial production and nutrient sediment-water exchange in sandy North Sea sediments.Mar. Ecol. Prog. Ser. 100(1–2): 85–95.
0
Views
3
Downloads
6
CSCD
Publicity Resources
Related Articles
Related Author
Related Institution
京公网安备11010802024621