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荒漠绿洲边缘不同粒径砂砾凝结水量

方静;丁永建   

  1. 中国科学院寒区旱区环境与工程研究所黑河生态水文与流域科学实验室, 中国生态系统研究网络临泽内陆河流域研究站, 兰州 730000
  • 收稿日期:2008-09-25 修回日期:1900-01-01 出版日期:2009-06-10 发布日期:2009-06-10

Condensation water on different size sand gravels at fringe of desert oasis.

FANG Jing;DING Yong-jian   

  1. Linze Inland River Basin Comprehensive Research Station, Chinese Ecosystem Research Network, Heihe Laboratory of Ecohydrology and Integrated River Basin Science, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2008-09-25 Revised:1900-01-01 Online:2009-06-10 Published:2009-06-10

摘要: 根据临泽荒漠绿洲边缘的凝结水观测数据,分析了砂砾粒径与凝结水形成量的关系。结果表明:粒径<0.02 mm的粉砂凝结量最大,7—10月日平均凝结量为(0.097±0.032) mm,其次是砂壤土,日平均凝结量(0.072±0.026) mm;而粒径为5.0~2.0 mm、2.0~0.2 mm和0.2~0.02 mm的砂砾凝结量较小,日平均凝结量分别为(0.052±0.021) mm、(0.057±0.018) mm和(0.059±0.016) mm。总之,凝结量随砂砾粒径的减小而增大,同时本文还分析了旱季农田砂土覆盖对土壤水分蒸发的抑制作用。

关键词: 氮沉降增加, 南亚热带, 森林, 土壤动物

Abstract: Based on the measurement of condensation water on different size sand gravels at the fringe of desert oasis in Linze County from July to October 2006, the relationships between the grain size of sand gravels and the amount of cond ensation water were analyzed. During the period of July-October, the sand grave ls with grain size <002 mm had the highest average amount of condensation wate r (0097±0032 mm·d-1), followed by those of <2 mm (0072±0026 mm· d-1), 02〖KG-*2〗-〖KG-*7〗002 mm (0059±0016 mm·d-1), 2〖K G-*2〗-〖KG-*7〗02 mm (0057±0018 mm·d-1), and 5〖KG-*2〗-〖KG-*7〗 2 mm (0052±0021 mm·d-1). In a word, the amount of condensation w ater on the sand gravels decreased with their increasing grain size. The effect of sand-mulching in decreasing farmland soil evaporation in dry season was discussed.

Key words: N deposition addition, South subtropics, Forests, Soil fauna