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半干旱区农牧交错带风水交互侵蚀特点研究——以内蒙古四子王旗南部为例
引用本文:常月明,王军花,赵爱荣,沙俊英.半干旱区农牧交错带风水交互侵蚀特点研究——以内蒙古四子王旗南部为例[J].内蒙古师范大学学报(自然科学版),2006,35(4):485-489.
作者姓名:常月明  王军花  赵爱荣  沙俊英
作者单位:[1]内蒙古师范大学地理科学学院,内蒙古呼和浩特010022 [2]呼和浩特市第34中学,内蒙古呼和浩特010051 [3]呼和浩特市第35中学,内蒙古呼和浩特010010 [4]内蒙古四子王旗实验中学,内蒙古四子王旗011800
基金项目:内蒙古师范大学校科研和教改项目
摘    要:以内蒙古四于王旗南部为例,研究了半干旱区农牧交错带风水交互侵蚀的特点.结果表明,该地区低山丘陵与宽谷相间分布,坡地上有大量疏松的沉积物;夏季降水以暴雨为主,春秋季多大风,形成风水复合侵蚀发育.每年夏秋季节的水蚀为风蚀提供了大量的沙物质,第2年春季的大风将沙物质进一步吹扬扩散,为水蚀的搬运提供了物质基础,如此反复.使水系的上游形成沟谷,中下游沙化迅速.

关 键 词:风水交互侵蚀  荒漠化  发育
文章编号:1001-8735(2006)04-0485-05
收稿时间:2006-04-21
修稿时间:2006年4月21日

The Characters of the Wind-Water Alternate Happening Erosion in the Farming-pasture Interlaced Belt of Semi-arid Area——Taking the South in Siziwangqi of Inner Mongolia as An Example
CHANG Yue-ming,WANG Jun-hua,ZHAO Ai-rong,SHA Jun-ying.The Characters of the Wind-Water Alternate Happening Erosion in the Farming-pasture Interlaced Belt of Semi-arid Area——Taking the South in Siziwangqi of Inner Mongolia as An Example[J].Journal of Inner Mongolia Normal University(Natural Science Edition),2006,35(4):485-489.
Authors:CHANG Yue-ming  WANG Jun-hua  ZHAO Ai-rong  SHA Jun-ying
Institution:1. College of Geographical Science, Inner Normal University ,Huhhot 010022,China; 2. The 34th Middle school of Huhhot, Huhhot 010051 ,China;3, The 35th Middle schoole of Huhhot ,Huhhot 010010, China ; 4. The Experiment Middle School of Siziwangqi in Inner Mongolia, Siziwangqi 011800, China
Abstract:Taking the south of Siziwang county as example, the characters of wind-water erosion of agro pasture zigzag zone in semi-arid region were studied. The results indicate that alternate there are ; In lternate erosions develops very much. in every summer and autumn,the water erosion provides much sand for the wind erosion. In the next spring, the strong wind blows and diffuses the sand everywhere, which provides with material elements for the water to carry. Repeating so and on,the gouge develops quickly in the upriver and sand spreads fast in the middle-downriver.
Keywords:alternate action of wind erosion and water erosion  desertification  development
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