巴丹吉林沙漠湖泊对浅层沙含水量的影响
Interdune lakes affects the water content of shallow sand layer： a situ observation from the Badain Jaran Sand Sea， China
巴丹吉林沙漠湖泊对浅层沙含水量的影响 |
| 牛震敏, 王乃昂, 温鹏辉, 苏贤保, 于昕冉, 张文佳 |
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Interdune lakes affects the water content of shallow sand layer： a situ observation from the Badain Jaran Sand Sea， China |
| Zhenmin Niu, Naiang Wang, Penghui Wen, Xianbao Su, Xinran Yu, Wenjia Zhang |
| 图5 沙层含水量随时间和深度的变化。A、B、C分别为苏木巴润吉林、巴嘎吉林和乌兰敖格钦30 cm内各层次的含水量，其中，“-2.5”代表0—5 cm深度，“-7.5”代表5—10 cm深度，以此类推；D为苏木巴润吉林、巴嘎吉林和乌兰敖格钦30 cm内平均含水量随时间的变化；E为苏木巴润吉林、巴嘎吉林和乌兰敖格钦30 cm内各层次的平均含水量随深度的变化；在D和E中，a为苏木巴润吉林，b为巴嘎吉林，c为乌兰敖格钦；F高大沙山背风坡0—4 m深度内6个剖面含水量随深度的变化及其均值（据文献［ |
| Fig.5 Variation of soil water content over time and depth. A， B and C are the soil water content at different depths within 30 cm in Sumubarunjilin， Bagajilin and Wulanaogeqin， respectively， where "-2.5" represents 0-5 cm depths， "-7.5" represents 5-10 cm depths， and so on； D is variation of the average soil water content within 30 cm over time in Sumubarunjilin， Bagajilin and Wulanaogeqin； E is variation of the average soil water content with depth of each layer within 30 cm in Sumubarunjilin， Bagajilin and Wulanaogeqin； in D and E， “a” represents Sumubarunjilin， “b” represents Bagajilin and “c” represents Wulanaogeqin； F is the variation of soil water content with depth and the average value of 6 profiles within the leeward slope of mega-dunes from 0 to 4 m （revised from literature ［35］） |
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