土壤侵蚀的中子活化示踪法研究

Study on the Neutron Activate Analysis Method for Soil Erosion

  • 摘要: 利用中子活化示踪法研究坡面土壤的侵蚀过程,发现坡面的相对侵蚀量从坡脚到坡顶随坡长的变化符合Weibull分布,其形状参数主要受降雨量、降雨历时和径流深度的影响,尺度参数主要与平均雨强、I30相关.坡面在侵蚀的同时也发生沉积,一般来说短历时高强度的降雨沉积量较小,而长历时低强度的降雨沉积量较大,某一部位侵蚀产沙的沉积量与其距离之间有y=axb的关系.坡面径流直接影响着坡面的输移比,当径流深和径流系数较高时,输移比接近于1,否则输移比降低.

     

    Abstract: A new method called Neutron Activate Analysis Tracer Method(NAATM)for studying soil erosion was formed through combination tracer method with neutron activate analysis technique,and the method was used to study the erosion process on slope.The research results showed that the changes of relative erosion amount with the distance from slope bottom to top accord with the Weibull distribution.The shape parameters of the Weibull distribution are mainly affected by precipitation,duration of rainfall and depth of runoff,and the scale parameters are related with aver age rainfall intensity and I30.Soil erosion and deposition happened at the same time on slope.Generally,deposition is less under the short duration rainfall with high rainfall intensity than that of long duration rainfall with low intensity.The relationship between deposition amount at acertain slope position and its distance was derived.The runoff directly affects delivery ratio(DR).When the depth and coefficient of runoff is large,the DR approaches 1,otherwise the DR will decreases.

     

/

返回文章
返回