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Pan Shaoming, Zhu Dakui, Li Yan, Xu Qigao. Cs-137 Profile in Sediments in Estuaries and Its Application in Sedimentology[J]. Acta Sedimentologica Sinica, 1997, 15(4): 67-71,66.
Citation: Pan Shaoming, Zhu Dakui, Li Yan, Xu Qigao. Cs-137 Profile in Sediments in Estuaries and Its Application in Sedimentology[J]. Acta Sedimentologica Sinica, 1997, 15(4): 67-71,66.

Cs-137 Profile in Sediments in Estuaries and Its Application in Sedimentology

  • Received Date: 1996-06-12
  • Publish Date: 1997-12-10
  • Six sediment cores, collected in Yangpu Harbour on Hainan Island, Out of Xiamen Harbour in Fu-jian Province and Xiangshan Harbour in Zhejiang Province, were analyzed for Cs- 137 activity, both theposition of the peak (corresponding to the period of maximum deposition) and the position of the horizon(corresponding to the first appearance of Cs- 137 in the environment)were been used to determine sedi-mentation rates.The results showed that it is possiable to use the Cs- 137 profile to determine sedimen-tation rate in estuaries, Rates for these cores based on the position of peak of Cs- 137 profile were 1.14cm /a, 1.56cm /a, 0.82cm /a, 0.75cm /a, 1.26cm /a, respectively.1.66cm /a, which are in good agreementwith that based on Pb- 210 dating and rates based on the occurrence of the horizon were larger than thatbased on Pb- 210 dating, Nhieh this indicates physical mixing or reworking of seidments in estuaryies.
  • [1] (1) 李树庆.中国近海放射性水平.海洋出版社, 1987, 163~169.

    (2) 陈绍勇,李文权,施文远等.湄州湾沉积物的混合速率和沉积速率的研究.海洋学报, 19886, 10: 567~574.

    (3) 项亮,王苏民.137 Cs 和 240 Am 在滇池、剑湖沉积孔柱中的蓄积及时标意义,湖泊科学, 1996, 8: 27~34.

    (4) 潘少明,王雪瑜, John N.Smith等.海南岛洋浦港现代沉积速率.沉积学报, 1994, 12: 86~93.

    (5) He Q.and Walling, D.E.Interpreting particle size effects inthe adsorption of137 Cs and unsrpported 210 Pb by mineral soil-sand sediments, J.Environ.Radioactivity, 1996, 30: 117~137.

    (6) Mccall, P.L., et al.137 Cs and 210Pb transpo rt and geochronolo-gies in urbanized reserv oir with rapidly increasing sedimenta-tion rates.Chemical Geology, 1984, 44: 151~185.

    (7)Milan, C.S.et al.Assessment of the137 Cs method for estimat-ing sediment accumlation rates: Louisiana salt marshes, J.ofCoastal Research, 1995, 11: 296~307.

    (8) Oldfield F., et al.241 Am and 137 Cs activity in fine g rained Salt-marsh sediments from parts of the N.E.Irish Sea Shoreline, J.Environ.Radioactivity, 1993, 19: 1~24.

    (9)Robbins, J.A.and Edgington, D.N.Determination of recentsedimentation ev eents in Lake Mechigan using,sup>210 Pb and 137 Cs,Geochim.Cosmochim Acta, 1975, 39: 285~ 304.

    (10) Schaffner, L.C.et al.Faunal characteristics and sediment ac-cumulation processes in the James Riv er estuary, Virginia, Es-tuarine, Coastal and Shelf Science, 1987, 25: 211~226.

    (11) Simpson, et al.Man- made radionuclides and sedimentationin the Hudson Riv er estuaty, Science, 1976, 194: 176~183.

    (12) Smith J.n.and Ellis, K.M., 1982 Transport mechanism fo r210Pb、 137 Cs and Pu fllout radionuclides through fluvial- ma-rine systems, Geochim.Cosmochim.Acta, 46, 941- 954.

    (13) Walling, D.E.et al.Use of137 Cs measurements to inv estigatesoil erosion on arable fields in the UK: potential applicationsand lmitations.J.Soil Sci.1991, 42: 147~165.

    (14) Whicker J.J.137Cs in sediments of Utah Lakes and Reser-voirs: Effects of elevation, sedimentation rate and fallout histo-ry, J.Environ.Radioactivity.1994, 23: 73~81.

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  • Received:  1996-06-12
  • Published:  1997-12-10

Cs-137 Profile in Sediments in Estuaries and Its Application in Sedimentology

Abstract: Six sediment cores, collected in Yangpu Harbour on Hainan Island, Out of Xiamen Harbour in Fu-jian Province and Xiangshan Harbour in Zhejiang Province, were analyzed for Cs- 137 activity, both theposition of the peak (corresponding to the period of maximum deposition) and the position of the horizon(corresponding to the first appearance of Cs- 137 in the environment)were been used to determine sedi-mentation rates.The results showed that it is possiable to use the Cs- 137 profile to determine sedimen-tation rate in estuaries, Rates for these cores based on the position of peak of Cs- 137 profile were 1.14cm /a, 1.56cm /a, 0.82cm /a, 0.75cm /a, 1.26cm /a, respectively.1.66cm /a, which are in good agreementwith that based on Pb- 210 dating and rates based on the occurrence of the horizon were larger than thatbased on Pb- 210 dating, Nhieh this indicates physical mixing or reworking of seidments in estuaryies.

Pan Shaoming, Zhu Dakui, Li Yan, Xu Qigao. Cs-137 Profile in Sediments in Estuaries and Its Application in Sedimentology[J]. Acta Sedimentologica Sinica, 1997, 15(4): 67-71,66.
Citation: Pan Shaoming, Zhu Dakui, Li Yan, Xu Qigao. Cs-137 Profile in Sediments in Estuaries and Its Application in Sedimentology[J]. Acta Sedimentologica Sinica, 1997, 15(4): 67-71,66.
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