[1]KUANG Gao-ming,ZHU Qing-ke,LIU Zhong-qi,et al.Effect of Microrelief on the Soil Water and Vegetation Arrangement in Loess Hilly and Gully Region[J].Research of Soil and Water Conservation,2012,19(03):74-77.
Copy
Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume:
19
Number of periods:
2012 03
Page number:
74-77
Column:
Public date:
2012-06-20
- Title:
-
Effect of Microrelief on the Soil Water and Vegetation Arrangement in Loess Hilly and Gully Region
- Author(s):
-
KUANG Gao-ming1, ZHU Qing-ke1, LIU Zhong-qi1,2, ZHAO Hui1,3, WANG Jing1
-
1. Key Laboratory of Soil and Water Conservation and Desertification Combating of Ministry of Education, Beijing Forestry University, Beijing 100083, China;
2. Inner Mongolia University for the Nationalities, Tongliao, Inner Mongolia 028000, China;
3. China Forest Exploration&Design Institute on Kunming, Kunming 650216, China
-
- Keywords:
-
loess hilly and gully region; microrelief; soil water; vegetation arrangement
- CLC:
-
S152.7
- DOI:
-
-
- Abstract:
-
In loess hilly and gully region, fluctuating land surface forms microrelief. Microrelief-based vegetation arrangement has become an important method in ecological restoration and construction. By using sampling surveys and random sampling, the biomass and the soil water content were surveyed by TDR on microrelief and the corresponding original slope in Hejia valley, Wuqi County, Shaanxi Province. Results showed that the coefficient of variation of microrelief soil water decreased with the increase of soil depth. The variation coefficient of soil water (0-60 cm soil) at scarp was the biggest (0.259) while at shallow gully was the smallest (0.226). In terms of soil water on sunny slope and soil water, landform units might be ranked in the descendant order of collapse, gully>platform>collapse>shallow gully>original slope>scarp, in addition, the sequence of vegetation arrangement was collapse>gully>shallow gully>original slope>platform>scarp, and the vegetation arrangement of microrelief was correlated negatively the variation coefficient of soil water (0-60 cm depth of soil).