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~(95)Zr在土壤中的淋溶和迁移分布
引用本文:邵敏,赵希岳,蔡志强,李定龙,冯俊生,王寿祥.~(95)Zr在土壤中的淋溶和迁移分布[J].农业环境保护,2010(5):895-898.
作者姓名:邵敏  赵希岳  蔡志强  李定龙  冯俊生  王寿祥
作者单位:[1]江苏工业学院环境与安全工程学院,江苏常州213164 [2]江苏工业学院化学化工学院,江苏常州213164 [3]浙江大学原子核农业科学研究所,杭州310029
基金项目:国家自然科学基金项目(39970147); 江苏省环境保护厅项目(2003076)
摘    要:采用模拟土柱法研究了95Zr在2种淹水土壤(小粉土、红黄壤)中的淋溶和垂直迁移。结果表明:(1)淋溶后收集到的全部淋溶液中95Zr的含量较少,小粉土淋溶液中95Zr为总活度的3.05%,黄红壤淋溶液中95Zr为总活度的3.00%;(2)滞留于土壤中的95Zr绝大部分分布在土壤表层0~1.0cm范围内,小粉土中有67.80%~80.18%的95Zr滞留于0~1.0cm土层范围内,黄红壤中有74.05%~86.95%的95Zr滞留于0~1.0cm土层范围内;(3)土壤中95Zr比活度与距土壤表层深度分布呈单项指数规律。

关 键 词:95Zr  淋溶  迁移与分布  放射生态学

Leaching and Vertical Transference of Zirconium-95 in Soils
SHAO Min,ZHAO Xi-yue,CAI Zhi-qiang,LI Ding-long,FENG Jun-sheng,WANG Shou-xiang.Leaching and Vertical Transference of Zirconium-95 in Soils[J].Agro-Environmental Protection,2010(5):895-898.
Authors:SHAO Min  ZHAO Xi-yue  CAI Zhi-qiang  LI Ding-long  FENG Jun-sheng  WANG Shou-xiang
Institution:1.School of Environmental and Safety Engineering,Jiangsu Polytechnic University,Changzhou 213164,China;2.School of Chemical Engineering,Jiangsu Polytechnic University,Changzhou 213164,China;3.Institute of Nuclear Agricultural Sciences,Zhejiang University,Hangzhou 310029,China)
Abstract:The leaching characteristics and vertical transference of radioactive nuclide zirconium-95 in two representational soils(paddy soil,yellow-red earth)were studied with soil-pole simulation installation.The results showed that:(1)The specific activity of zirconium-95 in collected leachate was low after passing through soil column.The amount of zirconium-95 in leachate of paddy soil was 3.05%,and yellowred earth was 3.00%.(2)In paddy soil and yellow-red earth,67.80%~80.18% and 74.05%~86.95% radioactivity of zirconium-95 was concentrated in the 0~1.0 cm upper layer soils respectively,which illustrated that most of zirconium-95 remained in the surface soils.(3)The specific activity of zirconium-95 in soil present was an individual exponential declining with depth of soil.
Keywords:95Zr  leaching  transference and distribution  radioecology
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