Soil Anti-scourability under Different Land Uses in Dry-Warm Valleys of the Jinshajiang River Basin
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Soil Anti-scourability under Different Land Uses in Dry-Warm Valleys of the Jinshajiang River Basin
Bulletin of Soiland Water ConservationVol. 25, Issue 5, Pages: 26-30(2006)
作者机构:
1. 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
2. 中国农业科学院 农业环境与可持续发展研究所,北京,100039
3. 中国科学院,研究生院,北京,100039
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Published:2006
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ZHOU Wei, ZHANG Jian-hui, LI Yong, et al. Soil Anti-scourability under Different Land Uses in Dry-Warm Valleys of the Jinshajiang River Basin[J]. Bulletin of Soiland Water Conservation, 2006, 25(5): 26-30.
DOI:
ZHOU Wei, ZHANG Jian-hui, LI Yong, et al. Soil Anti-scourability under Different Land Uses in Dry-Warm Valleys of the Jinshajiang River Basin[J]. Bulletin of Soiland Water Conservation, 2006, 25(5): 26-30.DOI:
Soil Anti-scourability under Different Land Uses in Dry-Warm Valleys of the Jinshajiang River Basin
Soil anti-scourability for four different land uses in the Dry-Warm Valleys of the Jinsha River Basin was studied by the flume experiment.The anti-scourability of surface soil increased with time
and the relationships for the land uses can be fitted by power function.The anti-scourability followed the order of stable gully>active gully>cultivated land>bare land.The ratio of the mean values of soil anti-scourability was 1.0:1.4:3.0:21.5 for stable gully
active gully
cultivated land and bare land
respectively.The same relationships held for subsurface soil in the period of the first 5 minute infiltration.Grass roots play an effective role in increasing soil anti-scourability. Soil anti-scouring ability is closely related to soil organic matter
and the content of>0.25 mm water-stable aggregate size fractions (especially of 3~5 mm
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Related Institution
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