毛乌素沙地典型流动沙丘水分深层渗漏量及动态特征
发布时间：2018-07-16 21:23
【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150cm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≤1mm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≥10mm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。
[Abstract]:Water is the most important limiting factor in arid and semiarid ecosystem. However, due to the lack of measurement methods, there is no convincing direct evidence for the dynamic characteristics of water leakage in the deep layer of flowing sand dunes. The process of rainfall infiltration in flowing sand dunes in Maowusu sandy land and the characteristics of deep seepage at the depth of 150cm were studied by using YWB-01 deep water leakage recorder. The results show that from May 14, 2011 to July 14, 2014, the number of days of deep leakage 鈮，
本文编号：2127715
[Abstract]:Water is the most important limiting factor in arid and semiarid ecosystem. However, due to the lack of measurement methods, there is no convincing direct evidence for the dynamic characteristics of water leakage in the deep layer of flowing sand dunes. The process of rainfall infiltration in flowing sand dunes in Maowusu sandy land and the characteristics of deep seepage at the depth of 150cm were studied by using YWB-01 deep water leakage recorder. The results show that from May 14, 2011 to July 14, 2014, the number of days of deep leakage 鈮，
本文编号：2127715
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