稀土元素示踪法在坡面土壤侵蚀垂直分布研究中的应用


Autoria(s): 刘普灵; 武春龙; 琚彤军; 杨明义
Data(s)

2001

Resumo

通过野外全坡长侵蚀小区试验,证明了稀土元素示踪法在土壤侵蚀垂直分布研究中的可应用性。结果表明该径流小区产沙强度坡长存在三种变化模式:增长型,增长 递减型和波动型,其形成机理可能与径流过程有关。利用稀土元素在坡面的再分析,初步建立了估算坡面沟蚀率的关系式。

The vertical variability is one of basic components of soil erosion on loess slope. The experiments on a erosion plot have firstly revealed that the vertical distribution pattern of sediment yield have three types: the continued-increasing type, the increase-decreasing type and the wave type. We have primarily developed a method estimating ration of rill erosion according to redistribution of the rare earth element on loess slope.

Identificador

http://ir.iswc.ac.cn/handle/361005/1233

http://www.irgrid.ac.cn/handle/1471x/141750

Idioma(s)

中文

Fonte

刘普灵, 武春龙, 琚彤军, 杨明义.稀土元素示踪法在坡面土壤侵蚀垂直分布研究中的应用.水科学进展,2001,3:331-335

Tipo

期刊论文