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中国沙漠 ›› 2004, Vol. 24 ›› Issue (3): 365-370.

• 研究简报 • 上一篇    下一篇

沙柳沙障的防风固沙效益研究

高永1,2, 邱国玉3, 丁国栋4, 清水英幸2, 虞毅2, 胡春元1, 刘艳萍5, 户部和夫2, 王义6, 汪季1   

  1. 内蒙古农业大学| 北京师范大学| 北京林业大学| 日本国立环境研究所| 水利部牧区水利科学研究所| 神府东胜煤田环保处| 内蒙古农业大学 内蒙古呼和浩特 0 1 0 0 1 9日本国立环境研究所| 日本茨城 3 0 5850 6| 北京1 0 0 875| 北京 1 0 0 0 83| 内蒙古呼和浩特 0 1 0 0 1 9| 内蒙古呼和浩特 0 1 0 0 1 0| 内蒙古伊金霍洛旗 0 1 72 0 0| 内蒙古呼和浩特 0 1 0 0 1 9|
  • 收稿日期:2003-02-21 修回日期:2003-05-25 出版日期:2004-06-20 发布日期:2004-06-20
  • 作者简介:高永(1962-),男(汉族),内蒙古包头市人,博士,教授,博士生导师,主要从事荒漠化防治方面的研究与教学工作。E-mail:gaoyong315@yahoo.com.cn
  • 基金资助:
    国家自然科学基金项目(30360088)资助

Effect of Salix psammophila Checkerboard on Reducing Wind and Stabilizing Sand

GAO Yong1,2, DING Guo-dong3, SHIMIZU Hideyuki4, YU Yi2, HU Chun-yuan2, LIU Yan-ping1, TOBE Kazuo5, WANG Yi2, WANG Ji6   

  1. 1. Inner Mongolia Agricultural University, Hohhot 010019, China;
    2. National Institute for Environmental Studies, Tsukuba, Ibaraki 3058506, Japan;
    3. Beijing Normal University, Beijing 100875, China;
    4. Beijing Forestry University, Beijing 100083, China;
    5. Grassland Hydraulic Research Institute of the Ministry of Water Resources, Hohhot 010010, China;
    6. Environment Protection Department of Shen-fu Dongsheng Coalfield, Yijinhuoluo 017200, Inner Mongolia, China
  • Received:2003-02-21 Revised:2003-05-25 Online:2004-06-20 Published:2004-06-20
  • Contact: 汪季

摘要: 研究测定了1m×1m, 1m×2m, 2m×2m, 2m×3m, 2m×4m, 2m×5m, 3m×3m, 3m×4m, 4m×4m, 4m×5m, 3m×6m等11种规格沙柳沙障内的风沙活动过程和分布规律。结果说明, 不同规格沙障内输沙率随着风速的变化其变化趋势不同, 小规格沙障内输沙率与风速呈对数曲线关系, 大规格沙障内输沙率与风速之间呈指数曲线关系。沙柳沙障中近地表0~4cm范围内, 风沙流中的相对含沙量沙丘下部明显大于沙丘中部和上部, 说明沙障导致了近地表风沙流结构发生变化。面积等于或小于1m2的沙障可以完全控制地表风蚀, 当沙障面积增加到一定程度后, 风蚀深度增加很快。不同规格沙障的防护效益, 在大风条件下, 小规格沙障的成本效益高于大规格的沙障; 在小风情况下, 大规格沙障的成本效益大于小规格沙障。

关键词: 沙柳, 沙障, 防风固沙, 荒漠化

Abstract: In this study, the material used to build straw checkerboard is branch of \%Salix psammophila,\% one native shrub in desert area. The sizes of checkerboard are 1 m×1 m,1 m×2 m, 2 m×2 m,2 m×3 m,2 m×4 m, 2 m×5 m,3 m×3 m, 3 m×4 m, 4 m×4 m, 4 m×5 m, 3 m×6 m. Results show that different sized checkerboards have different effects to reduce the sand flux intensity. Sand flux intensity varies logarithmically with wind velocity in the small sized checkerboard. Meanwhile, sand flux intensity varies exponentially with wind velocity in the large sized checkerboard. At the foot of dune with checkerboard on it, the sand flux intensity in 0~4 cm surface layer is significantly larger than that at the slope and the top of dune. The checkerboards with a size area equal to or less than 1 m2 can completely control wind erosion. If the size of checkerboard increases to over certain area, wind erosion will increase fast considerably. When considered both the effect of checkerboard on wind erosion control and its cost, small sized checkerboard has good effect under strong wind condition; the larger sized checkerboard is better under relatively weak condition.

Key words: Salix psammophila, checkerboard, reducing wind and stabilizing sand, desertification

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