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^(210)Pb,^(228)Th及一些有关同位素在浅海沉积柱样中之分布特征初探 被引量:1

A PRELIMINARY EXPLORATION ON DISTRIBUTIONAL CHARACTERISTICS OF ^(210)pb, ^(228)Th AND SOME RELATED ISOTOPES IN SEDIMENT CORES COLLECTED FROM SHALLOW SEA
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摘要 本文分析了三个岩芯和一个剖面。结果表明,^(210)Pb比度与有机质含量及粉砂粘土含量呈很好的正相关关系;^(228)Th未过剩;Th放射性强度及^(228)Th/^(232)Th比值皆向深处增大。 Three cores and one shoal section collected from Shapa Port,Yangxi County arc analysed in this paper. The radioactive intensity and ratio of (210)Pb, (228)Ra,(228)Th,(230)Th,(232)Th and the content of organic matter, silty clay, and some minerals in common use from each layer sample have been calculated.The intensity of (210)Pb was clear positive interrelated with the content rf organic matter and silty clay. But it was also clear that it was not interrelated with some minerals which arc in common use.The ratio of (228)Th/(232)Th was less than one. There was no excess of (228)Th. The intensity of Th increased with depth,particularly the intensity of (228)Th and ratio of (228)Th/(232)Th.But the intensity of (228)Ra was negatively interrelated with depth. It is impossible to measure the deposit rate of sediments by (228)Th/(232)Th ratio method in this area.
作者 温孝胜
出处 《热带海洋》 CSCD 1989年第4期52-60,共9页
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参考文献4

  • 1吴良基,热带海洋,1987年,6卷,3期,1页
  • 2苏贤泽,台湾海峡,1984年,3卷,1期,50页
  • 3邹汉阳,台湾海峡,1982年,1卷,2期,30页
  • 4李志远,海洋放射性调查方法,1981年

同被引文献12

  • 1温孝胜,南海海洋科学集刊,1992年,10期,63页
  • 2温孝胜,南沙群岛及其邻近海区海洋环境研究论文集.1,1991年
  • 3赵焕庭,珠江河口演变,1990年
  • 4刘韶,热带海洋,1988年,7卷,1期,57页
  • 5孙恢礼,热带海洋,1987年,6卷,4期,55页
  • 6吴良基,热带海洋,1987年,6卷,3期,1页
  • 7徐明广,海洋地质与第四纪地质,1986年,6卷,3期,93页
  • 8龙云作,海洋地质与第四纪地质,1985年,5卷,4期,49页
  • 9夏明,中国科学.B,1983年,9期,843页
  • 10赵焕庭,海洋学报,1982年,4卷,5期,596页

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