The resuspension rate of sediments in 32°N section on the East China sea

Sun Zhi-tao; Zhan Bin-qiu

doi:10.1007/BF02849658

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The resuspension rate of sediments in 32°N section on the East China sea

OriginalPaper | Updated：2023-05-16

- The resuspension rate of sediments in 32°N section on the East China sea
- The resuspension rate of sediments in 32°N section on the East China sea
- 海洋湖沼学报（英文） 2002年20卷第2期页码：191-196
- Affiliations：
  
  Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
  
  Contribution No. 4017 from the Institute of Oceanology, Chinese Academy of Sciences.;Project 49636210 supported by NSFC.
- DOI：10.1007/BF02849658
  中图分类号：
- 纸质出版：2002
- Accepted：
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The resuspension rate of sediments in 32°N section on the East China sea[J]. 海洋湖沼学报（英文）, 2002,20(2):191-196.

Zhi-tao, S., Bin-qiu, Z. The resuspension rate of sediments in 32°N section on the East China sea., Chin. J. Ocean. Limnol. 20, 191–196 (2002). https://doi.org/10.1007/BF02849658
The resuspension rate of sediments in 32°N section on the East China sea[J]. 海洋湖沼学报（英文）, 2002,20(2):191-196. DOI： 10.1007/BF02849658.

Zhi-tao, S., Bin-qiu, Z. The resuspension rate of sediments in 32°N section on the East China sea., Chin. J. Ocean. Limnol. 20, 191–196 (2002). https://doi.org/10.1007/BF02849658 DOI：

摘要

Abstract

This research on the influence of sediment resuspension on the flux of materials in the margin of the East China Sea showed that the sediment resuspension rates

was 47.40%–79.18% in the surface layers

and 72.75%–96.96% in the bottom layers. The research confirmed that the Changjiang River runoff and the eddy area upwelling flow near 125°E were two important factors affecting the sediment resuspension in summer; the transformation of DOC to POC through the flocculation in the transitional region (123°–124°E) was also confirmed by comparison of the resuspension rate. The sediment resuspension was shown to be influenced by the seasonal factor

especially in the surface layer.

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references

Bloesch, J., 1982. Inshore-offshore sedimentation differences resulting from resuspension in the Eastern Basin of Lake Erie.Can. J. Fish. Aquat. Sci. 39: 748–759.

Bloesch, J., 1994. A review of methods used to measure sediment resuspension.Hydrobiologia 284: 13–18.

Cacchione, D. A., Southard, J. B., 1974. Incipient sediment movement by shoaling internal gravity waves.Journal of Geophysical Research 79: 2237–2242.

Charlton, M. N., 1975. Sedimentation: Measurements in experimental enclosures.Verh. Int. Ver. Limnol. 19: 67–272.

Davis, A. B., 1968. Pollen grains in lake sediments: redeposition caused by seasonal water circulation.Science 162: 796–799.

Deter, B. G., 1978. Carbon dioxide and climate.Oceanus 21(4): 13–17.

Gabrielson, J. O., Lukatelich, R. J., 1985. Wind-related resuspension of sediments in the Peel-Harvey estuarine system.Estuarine, Coastal and Shelf Science 20: 135–145.

Gardner, W. D., 1980a. Sediment trap dynamics and calibration: A laboratory evaluation.Journal of Marine Research 38: 17–39.

Gardner, W. D., 1980b. Field assessment of sediment traps.Journal of Marine Research 38: 41–52.

Gasith, A., 1975. Tripton sedimentation in eutrophic lakes-simple correction for the resuspended matter.Verh. Int. Ver. Limnol. 19: 116–122.

Hu, D. X., Ding, Z. X., Xiong, Q. C., 1984. A preliminary investigation of cyclonic eddy in Northern East China Sea in summer.Studia Marina Sinica 21: 87–99. (in Chinese with English abstract)

Kenney, B. C., 1985. Sediment resuspension and currents in Lake Manitoba.Journal of Great Lakes Research 11: 85–96.

Lesht, B. M., Clarke, T. L., Freeland, G. L., et al., 1980. An empirical relationship between the concentration of resuspended sediment and near-bottom wave-orbital velocity.Geophys. Res. Lett. 2: 1049–1052.

Lund-Hansen, L. C., Petersson, M., Nurjaya, W., 1999. Vertical sediment fluxes and wave-induced sediment resuspension in a shallow-water coastal lagoon.Estuaries 22(1): 39–46.

Sanford, L. P., 1994. Wave-forced resuspension of upper Chesapeake Bay muds.Estuaries 18: 148–165.

Sanford, L. P., Panageotow, W., Halka, J. P., 1991. Tidal resuspension of the sediments in northern Chesapeake Bay.Marine Geology 97: 87–103.

Zhan, B. Q., Song J. M., 1997. Study on resuspension rate of the East China Sea suspended matter.Studia Marina Sinica 37: 99–102. (in Chinese with English abstract)

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