Research on Soil Moisture in the Typical Shrub-grass Zone in Karst Regions
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Research on Soil Moisture in the Typical Shrub-grass Zone in Karst Regions
Bulletin of Soiland Water ConservationVol. 26, Issue 4, Pages: 100-106(2007)
作者机构:
1. 北京师范大学地理学与遥感科学学院国家遥感科学重点实验室,北京,100875
2. 北京师范大学环境学院国家水环境模拟重点实验室,北京,100875
3. 贵州省水利厅,贵州,贵阳,550002
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Published:2007
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YANG Sheng-tian, WANG Yu-juan, WEN Zhi-qun, et al. Research on Soil Moisture in the Typical Shrub-grass Zone in Karst Regions[J]. Bulletin of Soiland Water Conservation, 2007, 26(4): 100-106.
DOI:
YANG Sheng-tian, WANG Yu-juan, WEN Zhi-qun, et al. Research on Soil Moisture in the Typical Shrub-grass Zone in Karst Regions[J]. Bulletin of Soiland Water Conservation, 2007, 26(4): 100-106.DOI:
Research on Soil Moisture in the Typical Shrub-grass Zone in Karst Regions
Guizhou Province. Based on long-term data and hydrological methods
soil moisture capacity is studied in views of its temporal and spatial patterns and dynamic characteristics. Different types of vegetation cover have different forms of soil moisture movement. Shrub land
grass land and corn field are selected for comparison. Land types rank in the descendant order of corn field
grass land and shrub land in terms of the initial content
whereas they rank in the descendant order of corn field
shrub land and grass land in terms of the descending rate. The analyses of soil moisture indicate the descending rate of the soil moisture on grass land is slower than that on shrub land
and their water retention property is stronger. Vegetation on grass land is different from other regions