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陕南低山丘陵区水土流失规律及与森林的关系

SOIL EROSION DYNAMICS IN THE LOWER MOUNTAIN AND HILLS REGION OF SOUTHERN SHAANXI AND ITS RELATION TO THE FOREST

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【作者】 唐德瑞李根前何景峰王迪海

【Author】 Tang Derui ; Li Genqian ;He Jingfeng(Shaanxi Forestry Institute of Sciences)

【机构】 陕西省林业科学研究所

【摘要】 对陕南低山丘陵区水土流失状况的调查和径流观测表明,低山丘陵区是陕西省长江流域水上流失最为严重的地带,坡耕地又是水土流失的主要来源,25°以上的坡耕地年土壤侵蚀量可达3万吨/km2以上,土壤侵蚀的绝对临界坡度为5.557°,许可临界坡度为18°,速增点为22°,速增区间为19°~24.75°;森林植被的覆盖是防止水土流失的根本措施。

【Abstract】 The investigation of soil and water erosion on the lower mountain and hills region and the experiment result from the runoff plots show that the lower mountain and hills region is the most serious zone with siol and water losses, the farm land on the steep slope is a major source for soil and water loosing ,the soil erosion modulus on steeping farm land with 25° reaches 30000t/km2. Year ; the absolute critical slope for soil erosion is 5. 557°,allowancing critical slope is 18°, accelerating point is at 22°, the acceleraing period are from 19°to 24. 75°,the forest covering is a fundamental measure to control the soil and water erosion.

  • 【文献出处】 陕西林业科技 ,SHANXI FOREST SCIENCE AND TECHNOLOGY , 编辑部邮箱 ,1994年03期
  • 【分类号】S714.7
  • 【被引频次】16
  • 【下载频次】132
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