Soil Anti-erodibility Under Different Landuse Types in Dabie Mountainous Area of Western Anhui Province——A Case Study in Yuexi County of Anhui Province
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Soil Anti-erodibility Under Different Landuse Types in Dabie Mountainous Area of Western Anhui Province——A Case Study in Yuexi County of Anhui Province
Bulletin of Soiland Water ConservationVol. 36, Issue 2, Pages: 38-41(2016)
ZHANG Wei. Soil Anti-erodibility Under Different Landuse Types in Dabie Mountainous Area of Western Anhui Province——A Case Study in Yuexi County of Anhui Province[J]. Bulletin of Soiland Water Conservation, 2016, 36(2): 38-41.
DOI:
ZHANG Wei. Soil Anti-erodibility Under Different Landuse Types in Dabie Mountainous Area of Western Anhui Province——A Case Study in Yuexi County of Anhui Province[J]. Bulletin of Soiland Water Conservation, 2016, 36(2): 38-41. DOI: 10.13961/j.cnki.stbctb.2016.02.008.
Soil Anti-erodibility Under Different Landuse Types in Dabie Mountainous Area of Western Anhui Province——A Case Study in Yuexi County of Anhui Province
[Objective] Soil anti-erodibility under different landuse types in the Dabie mountainous area of Western Anhui Province was researched to provide basis for soil erosion control. [Methods] Soil anti-sourability and disintegration rate under different landuse types were tested and analyzed. [Results] Soil anti-sourability and disintegration rate increased with the drop of slope position
indicating a decrease in soil anti-erodibility. Landuse types
in terms of soil anti-sourability and disintegration rate
ranked in a descendant order as Pinus massonian woodland
tea plantation
and wasteland. The values of soil disintegration rate of different landuses were listed as follows: Pinus massonian woodland
-0.16
-0.11 and 0.03 g/min; tea plantation
0.20
0.24 and 0.52 g/min; wasteland
0.12
0.60 and 0.82 g/min. [Conclusion] For all the three landuse types
the relation between the anti-sourability and the disintegration rate presented obvious positive linearity. Soil disintergration rate for wasteland varied fast as soil anti-sourability changed and slope gradient of the linear equation was 0.246. There does not exist obvious difference between the linear equation slope gradient of tea plantation and that of Pinus massonian woodland.
Elison W D. Soil erosion studies[J]. Agricultural Engineering, 1947,28(4):15-146.
Wischmeier W H, Smith D. D. Predieting Rainfall Erosion Losses:A Guide to Conservation Planning[M]. Washington D C:USDA Agriculture Handbook, 1978.
Gussak V B. Advice for the rapid detennination of erodibility of soils and some results of its applieation[J]. Abstract in Soils and Fertilizers, 1946,10:41.
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Related Author
ZENG Guang
Yang Qinke
YAO Zhihong
XU Xiao-hong
SUI Yuan-yuan
ZHANG Yu
WANG Yong-feng
LIU Ming-yi
Related Institution
Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resources, Yangling
Graduate University of the Chinese Academy of Sciences
Water and Soil Conservation Research Institute of Jilin Province
Shenyang Agricultural University
Liaoning Provincial Environmental Monitoring Station of Agriculture