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中国沙漠 ›› 2017, Vol. 37 ›› Issue (2): 222-227.DOI: 10.7522/j.issn.1000-694X.2017.00011

• 沙漠与沙漠化 • 上一篇    下一篇

毛乌素沙地典型流动沙丘水分深层渗漏量及动态特征

姚冬梅1, 冯金超2, 冯伟3, 梁海荣4, 杨文斌2, 党宏忠2, 吴丽丽2   

  1. 1. 通辽市森林公园管理处, 内蒙古 通辽 028000;
    2. 中国林业科学研究院荒漠化研究所, 北京 100091;
    3. 锡林郭勒职业学院, 内蒙古 锡林浩特 026010;
    4. 内蒙古自治区林业科学研究院, 内蒙古 呼和浩特市 010010
  • 收稿日期:2016-11-17 修回日期:2017-03-07 出版日期:2017-03-20 发布日期:2017-03-20
  • 通讯作者: 杨文斌(E-mail:nmlkyywb@163.com)
  • 作者简介:姚冬梅(1964-),女,内蒙古通辽人,林业高级工程师,主要从事林业建设等方面工作。E-mail:sbj006688@163.com
  • 基金资助:
    国家自然科学基金项目(41661006)

Water Seepage and Its Dynamic Characteristics in Deep Layer of Typical Mobile Dune in Mu Us Sandland

Yao Dongmei1, Feng Jinchao2, Feng Wei3, Liang Hairong4, Yang Wenbin2, Dang Hongzhong2, Wu Lili2   

  1. 1. Tongliao Forest Park Management Office, Tongliao 028000, Inner Mongolia, China;
    2. Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100091, China;
    3. Xilingol Vocational College, Xilinhot 026010, Inner Mongalia, China;
    4. Inner Mongolia Academy of Forestry, Hohhot 010010, China
  • Received:2016-11-17 Revised:2017-03-07 Online:2017-03-20 Published:2017-03-20

摘要: 水分是干旱、半干旱区生态系统中最重要的限制因子,一直以来都是研究的热点问题。然而由于测定方法的缺失,流动沙丘深层水分渗漏量的动态变化特征缺少令人信服的直接证据。采用YWB-01型水分深层渗漏记录仪,研究了毛乌素沙地流动沙丘降雨入渗过程及150 cm深度处的深层渗漏特征。结果表明:2011年5月14日到2014年7月14日,深层渗漏量≤1 mm的天数为793天,占总观测到渗漏时长的81.5%,深层渗漏量占总渗漏量的21.3%;深层渗漏量≥10 mm的天数为18天,占总观测到渗漏时长的1.85%,深层渗漏量占总渗漏量的33.3%。集中补给期主要在6-9月,渗漏量分别占各年总渗漏量的70%以上。深层渗漏量和降雨量之间均呈显著正相关关系。

关键词: 降雨, 渗漏, 水分动态, 流动沙丘

Abstract: Water is the most important limiting factor in arid and semi-arid ecosystems, and has always been a research hotspot. However, due to the lack of measurement methods, the scientific explanation of the dynamic variation characteristics of water seepage in deep layer of mobile dunes still lacks convincing direct evidence. In this paper, the YWB-01 water seepage recorder was used to study the process of rainfall infiltration and the characteristics of deep seepage at the depth of 150 cm in mobile sand dune in Mu Us sandy land. The results showed that, from May 14, 2010 to July 14,2014, the number of days with ≤1 mm deep seepage was 793, and was 81.5% of the total observed seepage time, the deep seepage accounted for 21.3% of the total seepage volume. The number of days with ≥10 mm deep seepage was 18 days, and was 1.85% of the total observed seepage time, the deep seepage accounting for 33.3% of the total seepage volume. Concentrated supply period was mainly in June to September, the seepage accounted for more than 70% of the total annual seepage volume. There was a significant positive correlation between seepage and rainfall.

Key words: rainfall, seepage, moisture dynamic, mobile sand dune

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