地理科学 ›› 2008, Vol. 28 ›› Issue (6): 782-787.doi: 10.13249/j.cnki.sgs.2008.06.782

• 论文 • 上一篇    下一篇

苏打盐渍土土壤水分动态及其与浅层地下水的交换关系

刘强1, 何岩2, 章光新3   

  1. 1. 北京师范大学环境学院水环境模拟国家重点实验室, 北京 100875;
    2. 中国科学院, 北京 100864;
    3. 中国科学院东北地理与农业生态研究所, 吉林 长春 130012
  • 收稿日期:2008-02-08 修回日期:2008-06-15 出版日期:2008-11-20 发布日期:2008-11-20
  • 作者简介:刘强(1978- ),男,山东省青岛人,博士后,研究方向为水资源与水环境。E-mail:liuqiangbnu@163.com
  • 基金资助:
    国家自然科学基金(40701189)、中国博士后科学基金项目(20060400405)资助。

Soil Water Dynamics and Its Exchange with Shallow Groundwater in Sodic Soil Region

LIU Qiang1, HE Yan2, ZHANG Guang-xin3   

  1. 1. State Key Laboratory of Water Environment Simulation, School of Environment, Beijing Normal University, Beijing 100875;
    2. Chinese Academy of Sciences, Beijing 100864;
    3. Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Changchun, Jilin 130012
  • Received:2008-02-08 Revised:2008-06-15 Online:2008-11-20 Published:2008-11-20

摘要: 以松嫩平原西部典型苏打盐渍土区为研究对象,以野外定位试验和室内模拟分析相结合,借助于分层土壤水分平衡模型,探讨苏打盐渍土壤水分运移的基本特征和规律,并分析其与浅层地下水之间的交换关系。研究结果表明,研究区内蒸降比较大,一般达到2:1以上,剖面土壤水分随蒸发、入渗过程呈现相应的转化;强烈地表蒸发作用下,地下水对上层土壤水分具有明显调控作用,土壤水分在50cm以下相对稳定,50cm以上受地表过程的影响变化较为显著。

Abstract: The soil water dynamics is the precondition to explore the formation and evolution of the sodic soil. Especially, in the shallow groundwater, the exchange of the soil water and groundwater has become one of the main factors to drive surficial eco-environment change. In order to get the dynamics of the soil water in the sodic soil region, the field experiment was conducted in Da’an Sodic Land Experimental Station of China in 2004. The results presented that the ratio of the evaporation to precipitation reached to 2:1 and soil water content changed with evaporation and infiltration processes. As regulated by the shallow groundwater, the soil water was less changeable in the soil layer below 50 cm than in the upper soil layer. Furthermore, influenced by the strong evaporative demand, the exchange between groundwater and soil water reached 11.7:1 and the groundwater has become one of the main water sources to influence the soil water dynamics.

中图分类号: 

  • S156.4+1