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珠江三角洲土壤镉高含量区的化学形态特征
引用本文:赖启宏,余海平,李国平,夏斌.珠江三角洲土壤镉高含量区的化学形态特征[J].物探与化探,2005,29(4):334-335,341.
作者姓名:赖启宏  余海平  李国平  夏斌
作者单位:1. 中国科学院,广州地球化学研究所,广东,广州,510640;广东省地质调查院,广东,广州,510080
2. 广东省地质调查院,广东,广州,510080
3. 江苏省地质矿产局,第四地质大队,江苏,苏州,215000
4. 中国科学院,广州地球化学研究所,广东,广州,510640
基金项目:中国地质调查局(200214200022)
摘    要:珠江三角洲冲积平原区存在镉的高含量区, 其主要分布于第四纪海陆和陆海交互相。第四纪不同沉积相镉的全量和不稳定相态的含量特征也存在显著的差异, 海陆交互相、陆海交互相、陆相的全量和不稳定相态的含量呈逐渐降低的趋势。从地表至深部, 在地下水位附近不稳定相态的含量比例相对较大。

关 键 词:土壤中镉  海陆交互相  陆海交互相  陆相  不稳定相态  含量比例
文章编号:1000-8918(2005)04-0334-02
收稿时间:2004-10-10
修稿时间:2004-10-10

CHEMICAL CHARACTERISTICS OF SOIL Cd-HIGH AREAS IN ZHUJIANG DELTA
LAI Qi-hong,YU Hai-ping,LI Guo-ping,XIA Bin.CHEMICAL CHARACTERISTICS OF SOIL Cd-HIGH AREAS IN ZHUJIANG DELTA[J].Geophysical and Geochemical Exploration,2005,29(4):334-335,341.
Authors:LAI Qi-hong  YU Hai-ping  LI Guo-ping  XIA Bin
Institution:1. Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China;
2. Geological Survey of Guangdong Province, Guangzhou 510080, China;
3. No.4 Geological Party, Jiangsu Bureau of Geology and Mineral Resources, Suzhou 215000, China
Abstract:There exist Cd-high areas in alluvial plain of Zhujiang delta, which are distributed in Quaternary marine - continental and continental-marine alternating facies sediments. The characteristics of total Cd content and unstable Cd phase content are obviously different in different sedimentary facies. The total Cd content and unstable Cd phase content tend to decrease gradually from marine-continental alternating facies through continental-marine alternating facies to continental facies. From the surface to the depth, the content ratio of unstable Cd phase is relatively high near the underground water level.
Keywords:Cd in soil  marine-continental alternating facies  continental-mating facies  continental facies  unstable phase  content ratio  Zhujiang delta
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