Study of Plot Soil Erosion Characteristic Under Different Underlying Horizon
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Study of Plot Soil Erosion Characteristic Under Different Underlying Horizon
Bulletin of Soiland Water ConservationVol. 25, Issue 3, Pages: 6-9(2006)
作者机构:
1. 西北农林科技大学资源环境学院, 陕西杨凌,712100
2. 中国科学院水利部水土保持研究所 土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌,712100
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Published:2006
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SHEN Zhenzhou, LIU Puling, XIE Yongsheng, et al. Study of Plot Soil Erosion Characteristic Under Different Underlying Horizon[J]. Bulletin of Soiland Water Conservation, 2006, 25(3): 6-9.
DOI:
SHEN Zhenzhou, LIU Puling, XIE Yongsheng, et al. Study of Plot Soil Erosion Characteristic Under Different Underlying Horizon[J]. Bulletin of Soiland Water Conservation, 2006, 25(3): 6-9.DOI:
Study of Plot Soil Erosion Characteristic Under Different Underlying Horizon
Three original physiognomy plots (besides bare slope
grass slope and shrubby slope) were const ructed in the Yaner watershed. The amounts of the runoff
erosion and seeping rate in different sections in two years were analyzed. The data were found to vary with different rainfall events. Under the same condition
the amount of runoff on bare slope was 6 times greater than that on grass slope
and 2. 4 times greater than shrubby slope
which indicated that bare slope produced more runoff than other two. The amount of erosion on bare slope was 82 times greater than that on shrubby slope
and 150 times greater than that on shrubby slope. This suggest s that grass and shrubby can greatly reduce soil erosion in the Loess Plateau. Seeping rate varies with all the rainfall event s. Gener2 ally speaking
seeping rate on shrubby slope is 90%
grass slope
85%
and bare slope
60%.It is a comparative advantage in melioration of the Loess Plateau to grow grass or shrub.