Chin J Plant Ecol ›› 2005, Vol. 29 ›› Issue (6): 910-917.DOI: 10.17521/cjpe.2005.0122
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JIA Hai-Kun, LIU Ying-Hui*(), XU Xia, WANG Kun, GAO Qiong
Received:
2004-11-01
Accepted:
2005-04-07
Online:
2005-11-01
Published:
2005-09-30
Contact:
LIU Ying-Hui
JIA Hai-Kun, LIU Ying-Hui, XU Xia, WANG Kun, GAO Qiong. SIMULATION OF SOIL WATER DYNAMICS IN A CARAGANA INTERMEDIA WOODLAND IN HUANGFUCHUAN WATERSHED: RELATIONSHIPS AMONG SLOPE, ASPECT, PLANT DENSITY AND SOIL WATER CONTENT[J]. Chin J Plant Ecol, 2005, 29(6): 910-917.
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URL: https://www.plant-ecology.com/EN/10.17521/cjpe.2005.0122
特征指标 Character indexes | 数值 Value | |||||
---|---|---|---|---|---|---|
砂粒含量 Sand-grain fraction | 82.16% | |||||
粉粒含量 Silt fraction | 6.78% | |||||
黏粒含量 Clay fraction | 11.06% | |||||
田间持水量 Field moisture capacity | 0.19 m3·m-3 | |||||
剩余含水量 Residual moisture content | 0.025 m3·m-3 | |||||
饱和含水量 Saturation moisture content | 0.37 m3·m-3 | |||||
萎蔫含水量 Wilting point moisture | 0.027 m3·m-3 | |||||
饱和导水率 Saturated hydraulic conductivity | 10 cm·h-1 | |||||
容重 Bulk density | 1.44 g3·cm-3 |
Table 1 Soil character indexes
特征指标 Character indexes | 数值 Value | |||||
---|---|---|---|---|---|---|
砂粒含量 Sand-grain fraction | 82.16% | |||||
粉粒含量 Silt fraction | 6.78% | |||||
黏粒含量 Clay fraction | 11.06% | |||||
田间持水量 Field moisture capacity | 0.19 m3·m-3 | |||||
剩余含水量 Residual moisture content | 0.025 m3·m-3 | |||||
饱和含水量 Saturation moisture content | 0.37 m3·m-3 | |||||
萎蔫含水量 Wilting point moisture | 0.027 m3·m-3 | |||||
饱和导水率 Saturated hydraulic conductivity | 10 cm·h-1 | |||||
容重 Bulk density | 1.44 g3·cm-3 |
坡度 Slope | 0° | 45° | 90° | 135° | 180° |
---|---|---|---|---|---|
土壤水分与坡度的关系 Soil water content versus slope | ↗ | ↗ | ∩ | ∪ | ↘ |
Table 2 Types of function between soil water content and slope of different aspect
坡度 Slope | 0° | 45° | 90° | 135° | 180° |
---|---|---|---|---|---|
土壤水分与坡度的关系 Soil water content versus slope | ↗ | ↗ | ∩ | ∪ | ↘ |
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