Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary

Lin Ronggen; Wu Jingyang

doi:10.1007/BF02843821

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Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary

OriginalPaper | Updated：2023-05-16

- Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary
- Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary
- 海洋湖沼学报（英文） 1992年10卷第3期页码：204-214
- Affiliations：
  
  Institute of Oceanology
- Author bio：
- Funds：
  
  This project was supported by the National Science Foundation of China.;Contribution No. 2028 from the Institute of Oceanology, Academia Sinica.
- DOI：10.1007/BF02843821
  中图分类号：
- 纸质出版：1992
- Accepted：
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Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary[J]. 海洋湖沼学报（英文）, 1992,10(3):204-214.

Ronggen, L., Jingyang, W. Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary., Chin. J. Ocean. Limnol. 10, 204–214 (1992). https://doi.org/10.1007/BF02843821
Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary[J]. 海洋湖沼学报（英文）, 1992,10(3):204-214. DOI： 10.1007/BF02843821.

Ronggen, L., Jingyang, W. Distributions of total, inorganic and organic phosphorus in the sediments near the Huanghe River Estuary., Chin. J. Ocean. Limnol. 10, 204–214 (1992). https://doi.org/10.1007/BF02843821 DOI：

摘要

Abstract

For some hundred surface sediment samples from five cores taken in two cruises near the Huanghe River Estuary

total phosphorus (TP)

inorganic phosphorus (IP) and organic phosphorus (OP) were determined. On the average

527×10−6

455×10−6 and 72×10−6

were found for TP

IP and OP for the surface sediments taken in the two cruises. The distribution of OP and IP was controlled by the sample particle size: OP content increased with the decreasing of the sample particle size

while the maximal value of IP was found in the silt fraction due to the existence of apatite in our samples. Vertical distributions reflected well the channel change of the Huanghe River. Results from the multiple regressions between the three forms of phosphorus and the percentages of different particle size agreed well with the analytical data.

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references

Andersen, J. M., 1976. An ignition method for determination of total phosphorus in the lake sediments.Wat. Res. 10(4): 329–331.

Baturin, C.N., 1981. Phosphorities in the Sea Floor—Origin, Composition and Distribution. Developments in Sedimentology 33. Elsevier Scientific Publishing Company, pp. 343.

Callender, E. and D.E. Hammond, 1982. Nutrient exchange across the sediment-water interface in the Potomac River Estuary.Est. Coast. Shelf Sci. 15: 395–413.

Dai Minying, Zhou Chennian, Gu Tangxiu et al. 1988 The characteristics of distribution of phosphorus in the Haihe River Estuary of the Bohai Bay.Studia Marina Sinica 29: 57–64 (in Chinese with English abstract).

Qin Yunshan and Li Fan, 1986. Study of the influence of sediment loads discharged from Huanghe River on sedimentation in Bohai and Yellow Seas.Studia Marina Sinica 27: 125–135. (in Chinese with English abstract)

Qin Yunshan, Zhao Yiyang, Chen Lirong et al., 1989. Geology of the Huanghai Sea. Ocean Press, Beijing, 289 pp. (in Chinese).

Yamada, H. and M. Kayama, 1987. Distribution and dissolution of several forms of phosphorus in coastal marine sediments.Oceanol. Acta 10(3): 311–321.

Zhao Yiyang, Che Chenghui, Yang Huilan, et al., 1981. Geochemistry of Fe, Mn, Ti and P in the seabed sediments of the Taiwan Bank, China.Acta Geologia Sinica 2: 118–181 (in Chinese with English abstract).

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