Effects of soil conservation practices on soil losses from slope farmland in northeastern China using runoff plot data

被引:31
|
作者
Xin, Yan [1 ]
Liu, Gang [1 ]
Xie, Yun [1 ]
Gao, Yan [2 ]
Liu, Baoyuan [1 ]
Shen, Bo [2 ]
机构
[1] Beijing Normal Univ, Fac Geog Sci, State Key Lab Earth Surface Proc & Resource Ecol, 19 Xinjiekouwai St, Beijing 100875, Peoples R China
[2] Minist Water Resources, Songliao Water Resources Commiss, Changchun 130021, Jilin, Peoples R China
基金
中国博士后科学基金;
关键词
Conservation assessment; Slope model; Conservation practice; Slope farmland; Runoff plot-year; P factor; WEST USAMBARA HIGHLANDS; LOSS EQUATION; NO-TILL; EROSION; AGRICULTURE; SYSTEM;
D O I
10.1016/j.catena.2018.11.029
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Various conservation practices have been used to control soil erosion in cropland which makes assessing the effects of soil conservation more important. Northeastern China is an important crop-producing regions, with severe soil erosion. In the study, 110 runoff plot-year observations from seven experimental stations distributed over the region were used to assess the effects of local conservation practices on soil erosion, using a simplified USLE. Under the assumption that there were no significant differences in rainfall erosivity and soil erodibility in the study area under the "no practice scenario", we described a simplified linear model based slope steepness and soil loss rate. The Jixing watershed was selected as a case study to test the model. The results indicate that the derived model can be used in the NE region of China for conservation assessment. The P factor values, related to main soil conservation practices, were derived from the observed plot-year data. The average values of P factor were around 0.01 to 0.35, which were low enough to justify their conservation effects of implementation through the assessment Comparing to the conventional slope ridging tillage, the conservation rates of terraces, strip ridging, orchards and agro-forestry in the Jixing Watershed were 0.57, 0.6, 1.07, and 0.62 mm/ha, respectively, obtained by the assessment method in the study case. The paper neglected the seasonal variation which should be grouped to the C factor for the annual data and discussed the limitations of the assessment model for application.
引用
收藏
页码:417 / 424
页数:8
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