[1]JIANG Fang-shi,HUANG Yan-he,LIN Jin-shi,et al.Effects of Different Rainfall Intensities and Slope Gradients on Rill Erosion of Coluvial Deposits in Granite Benggang[J].Research of Soil and Water Conservation,2014,21(01):1-5.
Copy

Effects of Different Rainfall Intensities and Slope Gradients on Rill Erosion of Coluvial Deposits in Granite Benggang

References:
[1] 唐克丽.中国水土保持[M].北京:科学出版社,2004:80-82.
[2] 丘世钧.红土坡地崩岗侵蚀过程与机理[J].水土保持通报,1994,14(6):31-40.
[3] 蒋芳市,黄炎和,林金石,等.崩岗崩积体土壤渗透特性分析[J].水土保持学报,2013,27(3):49-54.
[4] 蒋芳市,黄炎和,林金石,等.坡面水流分离崩岗崩积体土壤的动力学特征[J].水土保持学报,2013,27(1):86-89,229.
[5] 林敬兰,黄炎和.崩岗侵蚀的成因机理研究与问题[J].水土保持研究,2010,17(2):41-44.
[6] 李君兰,蔡强国,孙莉英,等.细沟侵蚀影响因素和临界条件研究进展[J].地理科学进展,2010,19(11):1319-1325.
[7] 张科利.黄土坡面侵蚀产沙分配及其与降雨特征关系的研究[J].泥沙研究,1991(4):39-45.
[8] Dunkerley D. Rain event properties in nature and in rainfall simulation experiments:a comparative review with recommendations for increasingly systematic study and reporting[J]. Hydrological Processes,2008,22(22):4415-4435.
[9] Auerswald K, Fiener P, Dikau R. Rates of sheet and rill erosion in Germany:a meta-analysis[J]. Geomorphology,2009,111(3):182-193.
[10] 王治国,魏忠义,段喜明,等.黄土残塬区人工降雨条件下坡耕地水蚀的研究:Ⅰ.影响细沟侵蚀因素的综合分析[J].水土保持学报,1995,9(2):51-57.
[11] 杨具瑞,史正涛,曹叔尤,等.细沟侵蚀临界坡度研究[J].干旱区资源与环境,2008,22(5):64-67.
[12] 周佩华,窦保璋,孙清芳.降雨能量的试验研究初报[J].水土保持通报,1981,1(1):51-61.
[13] 李君兰,蔡强国,孙莉英,等.坡面水流速度与坡面含砂量的关系[J].农业工程学报,2011,27(3):73-78.
[14] 林敬兰,黄炎和,蒋芳市,等.崩岗土体的渗透性能机理研究[J].水土保持学报,2013,27(2):53-56,144.
[15] 陈俊杰.不同土壤坡面细沟侵蚀影响试验研究[D].武汉:华中农业大学,2012.
[16] 耿晓东.主要水蚀区坡面土壤侵蚀过程与机理对比研究[D].北京:中国科学院研究生院,2010.
Similar References:

Memo

-

Last Update: 1900-01-01

Online:8298       Total Traffic Statistics:27439309

Website Copyright: Research of Soil and Water Conservation Shaanxi ICP No.11014090-10
Tel: 029-87012705 Address: Editorial Department of Research of Soil and Water Conservation, No. 26, Xinong Road, Yangling, Shaanxi Postcode: 712100