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Analysis of Sediment Source of Watershed in Western Shanxi of the Loess Plateau

Analysis of Sediment Source of Watershed in Western Shanxi of the Loess Plateau
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摘要 The paper analyzes the sediment source of watershed by means of studying watershed in westernShanxi of the Losses Plateau. On the basis of watersheds classification, 7 typical watersheds were chosen andobserved for 11 years. The result shows that the sediment at the small watershed mainly comes from gullies,which is 60% of the total sediment. Erosion modulus of valley (including gully head, gully bed, valley side)is 1.28~2.48 times as that of the area between channels(including hill slope and mound of the Loess Plateau).The main sediment source of slope erosion is cultivated land on slope without water and soil conservationmeasures. The paper analyzes the sediment source of watershed by means of studying watershed in westem Shanxi of the Losses Plateau. On the basis of watersheds classification, 7 typical watersheds were chosen and observed for 11 years. The result shows that the sediment at the small watershed mainly comes from gullies, which is 60% of the total sediment. Erosion modulus of valley (including gully head, gully bed, valley side) is 1.28-2.48 times as that of the area between channels(including hill slope and mound of the Loess Plateau). The main sediment source of slope erosion is cultivated land on slope without water and soil conservation measures.
出处 《Chinese Forestry Science and Technology》 2004年第2期71-76,共6页 中国林业科技(英文版)
关键词 Loess Plateau small watershed EROSION sediment source 黄土高原 陕西西部地区 小流域 沉积物资源 土壤侵蚀
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