利用137Cs估算土壤侵蚀速率的定量模型 |
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作者姓名: | YANG Hao DU Ming-Yuan CHANG Qing K. MINAMI T. HATTA |
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作者单位: | [1]InstituteofSoilScience,theChineseAcademyofSciences,P.O.Box821,Nanjing210008(China) [2]JapanInternational,theChineseAcademyofSciences,P.O.Box821,Nanjing210008(China) |
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基金项目: | *1Project supported by the Ministry of Agriculture, Forestry and Fisheries of Japan. |
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摘 要: | A quantitative model was developed to relate the amount of ^137Cs loss from the soil profile to the rate of soil erosion,According th mass balance model,the depth distribution pattern of ^137Cs in the soil profile ,the radioactive decay of ^137Cs,sampling year and the difference of ^137Cs fallout amount among years were taken into consideration.By introducing typical depth distribution functions of ^137Cs into the model ,detailed equations for the model were got for different soil,The model shows that the rate of soil erosion is mainly controlled by the depth distrbution pattern of ^137Cs ,the year of sampling,and the percentage reduction in total ^137Cs,The relationship between the rate of soil loss and ^137Cs depletion i neither linear nor logarithmic,The depth distribution pattern of ^137Cs is a major factor for estimating the rate of soil loss,Soil erosion rate is directly related with the fraction of ^137Cs content near the soil surface. The influences of the radioactive decay of ^137Cs,sampling year and ^137Cs input fraction are not large compared with others.
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关 键 词: | 土壤侵蚀 铯 模型 流失 放射性 |
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