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中国沙漠 ›› 2003, Vol. 23 ›› Issue (4): 391-397.

• 研究论文 • 上一篇    下一篇

青海共和盆地土壤风蚀的137Cs法研究(Ⅱ)——137Cs背景值与风蚀速率测定

严平1, 董光荣2, 张信宝3, 邹学勇1   

  1. 1. 北京师范大学 中国沙漠研究中心, 环境演变与自然灾害教育部重点实验室, 北京 100875;
    2. 中国科学院 寒区旱区环境与工程研究所, 甘肃 兰州 730000;
    3. 中国科学院、水利部 成都山地灾害与环境研究所, 四川 成都 610041
  • 收稿日期:2001-12-31 修回日期:2002-03-11 出版日期:2003-08-20 发布日期:2003-08-20
  • 作者简介:严平(1966-),男(汉族),安徽宁国人,理学博士,副教授,主要从事土壤风蚀与干旱区环境研究。E-mail:yping@bnu.edu.cn
  • 基金资助:
    国家自然科学基金(40001001);国家重大基础研究规划项目(G2000048702);"十五"国家科技攻关项目"沙区农田、草地土壤风蚀防治技术研究"课题(2002BA517A10)资助

Application of Caesium-137 Technique on Wind Erosion in Gonghe Basin,Qinghai Province(Ⅱ)-137Cs Reference Inventory and 137Cs Model for Wind Erosion Estimation

YAN Ping1, DONG Guang-rong2, ZHANG Xin-bao3, ZOU Xue-yong1   

  1. 1. China Center of Desert Research at Beijing Normal University, Key Laboratory of Environmental Change and Natural Disaster, the Ministry of Education of China, Beijing Normal University, Beijing 100875, China;
    2. Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
    3. Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, China
  • Received:2001-12-31 Revised:2002-03-11 Online:2003-08-20 Published:2003-08-20

摘要: 通过对高寒草原背景值样点(RS7)的分析,将共和盆地的137Cs背景值含量确定为(2691.78±196.08) Bq·m-2,基本接近北半球137Cs背景值的平均水平,其137Cs剖面满足尖峰分布函数,与公认的理论分布(即负指数分布)相比,呈现出峰值下移和曲线趋平的现象,可能与近几十年来137Cs的稳定下渗有关。应用137Cs背景值剖面分布函数,建立了风蚀速率的137Cs估算模型,估算出四个样方的土壤风蚀速率,并由此转化为区域风蚀速率,计算出共和盆地区域土壤风蚀速率为12.556 t·hm-2·a-1,通过蚀积平衡检验,其误差水平小于10%。并分析了风蚀物的输出途径及其所占比例。

关键词: 土壤风蚀, 137Cs背景值, 137Cs风蚀模型, 蚀积平衡, 共和盆地

Abstract: Analyzing results of the 137Cs distribution along soil profile suggest that the cold grassland that maintained the relatively perfect profile of original 137Cs fallout can be regarded as ideal sampling site of 137Cs reference.Therefore the value of 137Cs reference inventory of the Gonghe Basin is calculated to be(2 691.78±196 08) Bq·m-2 at the site of RS7,which is close to the globe average of the Northern Hemisphere.The depth distribution of 137Cs activity fits the peak type remarkably,and comparing with the exponential type regarded as classical and theoretical one,it exhibites the descent of peak layer and smoothing of the 137Cs curve,which is possibly related to stable infiltration of 137Cs in recent decades.Therefore by means of the 137Cs model derived from the 137Cs reference distribution,the rate of wind erosion on the four sampling plots was estimated,and then transforming the point erosion estimates to the area,the rate of wind erosion in the Gonghe Basin averaged 12 556 t·hm-2·a-1,which is in according with the erosion deposition equilibrium with a relatively small error less than 10%.

Key words: wind erosion, 137Cs reference inventory, 137Cs model, erosion-deposition equilibrium, Gonghe Basin

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