Soil Erosion and Its Spatial Differentiation of a Small Watershed in Water Source Areas of Beijing City and Tianjin City
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Soil Erosion and Its Spatial Differentiation of a Small Watershed in Water Source Areas of Beijing City and Tianjin City
Bulletin of Soiland Water ConservationVol. 30, Issue 1, Pages: 249-255(2011)
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, 陕西 杨凌,712100
作者简介:
基金信息:
DOI:
CLC:P901F293.2
Published:2011
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JIANG Qing-long, XIE Yong-sheng, ZHANG Ying-long, et al. Soil Erosion and Its Spatial Differentiation of a Small Watershed in Water Source Areas of Beijing City and Tianjin City[J]. Bulletin of Soiland Water Conservation, 2011, 30(1): 249-255.
DOI:
JIANG Qing-long, XIE Yong-sheng, ZHANG Ying-long, et al. Soil Erosion and Its Spatial Differentiation of a Small Watershed in Water Source Areas of Beijing City and Tianjin City[J]. Bulletin of Soiland Water Conservation, 2011, 30(1): 249-255.DOI:
Soil Erosion and Its Spatial Differentiation of a Small Watershed in Water Source Areas of Beijing City and Tianjin City
In the water source areas of Beijing City and Tianjin City
ecological environment is highly fragile
and soil and water loss often exhibits strong spatial variability and occurs unpredictably.Along with data of climate
soil
terrain
land use and vegetation coverage
soil erosion and its spatial differentiation were studied based on the revised universal soil loss equation (RUSLE)model and geographic information system (GIS)
in Xibeigou watershed of Luanping County
Hebei Province.The results show that the annual average rate of soil erosion was3816.835t/(km 2·a)
classified as middle-grade erosion.Annual average of potential soil erosion was 31583.15t/(km2·a)
about 8.28 times of the former.Meanwhile
soil loss was obviously spatially differentiated.Among different land uses
sporadically distributed farmlands with steep slopes had the strongest soil erosion intensity
and next to it was highly weathered and degraded grassland's
which accounts for 59.38% of the total area of the watershed and 88.48% of the total sediment as the main source of the soil loss.With the increasing slope
the soil erosion intensity increased markedly.Approximately one third of the total area of this region has a slope degree higher than 25°
while this proportion contributed two third of soil loss.Soil losses also differed among lands of various aspects
as in order of sunny slope>half-sunny slope>half-shady slope>shady slope>flatland.