CHEMICAL CHARACTERISTICS OF SOIL Cd-HIGH AREAS IN ZHUJIANG DELTA
LAI Qi-hing1,2, YU Hai-ping2, LI Guo-ping3, XIA Bin1
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
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.
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.
LAI Qi-hing, YU Hai-ping, LI Guo-ping, XIA Bin. CHEMICAL CHARACTERISTICS OF SOIL Cd-HIGH AREAS IN ZHUJIANG DELTA. Geophysical and Geochemical Exploration, 2005, 29(4): 334-335,341.