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黄土区坡耕地侵蚀输移特征

Characteristics of Erosion and Moving of Sloping Field in Loess Area

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【作者】 赵晓光李光录刘秉正吴发启

【Author】 Zhao Xiaoguang;Li Guanglu;Liu Bingzheng;Wu Faqi (Dept. of Soil and Water Conservation, NWFC, Yangling Shaanxi 712100)

【机构】 西北林学院水土保持系

【摘要】 文章推荐了确定侵蚀、输移量的方法,指出坡耕地侵蚀过程中的"填洼"作用是引起输移比变化的原因,并分析了其变化规律。通过不同坡长的输移变化试验,发现单宽最小径流率qmin和最大含沙量ρmax可判别其侵蚀输移变化,并划分出"侵蚀─输移区"、"侵蚀─堆积─输移区"和"侵蚀─输移挠动区"。对小集水区回归出输移比与坡长、面积的幂函数关系式。

【Abstract】 A method for determining the quantity of erosion and moving was discussed in the paper. Duriny erosion the main cause of the variation of moving ratio was the "filling of low-lying lands" in the sloping fields. Contral experiments were conducted on moving of different lengths of slope. It was found that the maximum of runoff ratio Per unit width and the maximum of sand carrying Per unit width sand could be used to discriminate the variation of erosion and moving.Areas of "erosion-moving" erosion-heaping - moving" and " erosion - moving interference"were divided. An exponent function equation for small water sheds was regressed according to the data of moving ratio, length of slope and size of slope.

【关键词】 黄土区坡耕地侵蚀输移输移比
【Key words】 loess areasloping fielderosionmovingmoving ratio.
  • 【文献出处】 西北林学院学报 ,JOURNAL OF NORTHWEST FORESTRY COLLEGE , 编辑部邮箱 ,1995年S1期
  • 【分类号】S157.1
  • 【被引频次】9
  • 【下载频次】88
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