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.
Yao Dongmei
,
Feng Jinchao
,
Feng Wei
,
Liang Hairong
,
Yang Wenbin
,
Dang Hongzhong
,
Wu Lili
. Water Seepage and Its Dynamic Characteristics in Deep Layer of Typical Mobile Dune in Mu Us Sandland[J]. Journal of Desert Research, 2017
, 37(2)
: 222
-227
.
DOI: 10.7522/j.issn.1000-694X.2017.00011
[1] 雷雅凯,郭伟,张军红,等.毛乌素沙地气候与植被变迁[J].西北林学院学报,2012(6):242-247.
[2] 包岩峰,丁国栋,吴斌,等.毛乌素沙地风沙流结构的研究[J].干旱区资源与环境,2013(2):118-123.
[2] 冯起,程国栋.我国沙地水分分布状况及意义[J].土壤学报,1999,36(2):225-236.
[3] 刘新平,张铜会,赵哈林,等.流动沙丘降雨入渗和再分配过程[J].水利学报,2006,37(2):166-171.
[4] 刘元波,高前兆.沙地水分动力学研究新视角[J].中国沙漠,1997,17(1):95-98.
[5] 黄利江,于卫平,张广才,等.盐池沙地水分与植被恢复关系的研究[J].林业科学研究,2004,17(B12):148-151.
[6] 何志斌,赵文智.半干旱区流动沙地土壤湿度变异及其对降水的依赖[J].中国沙漠,2002,22(4):359-362.
[7] 陈有君,刘钟龄.内蒙古浑善达克沙地土壤水分状况的分析[J].干旱区资源与环境,2000,l4(1):80-85.
[8] 蒙宽宏.土壤水分入渗测定方法及影响因素[D].哈尔滨:东北林业大学.2006.
[9] 张志才.降雨入渗补给地下水研究[D].南京:河海大学.2006,1-78.
[10] 周春华.大埋深条件下降雨入渗补给过程分析[D].西安:长安大学,2007:3-11.
[11] 王建新,王恩志,王思敬.降雨自由入渗阶段试验研究及其过程的水势描述[J].清华大学学报:自然科学版,2010,50:1920-1924.
[12] Finch J W.Estimating direct groundwater recharge using a simple water balance model-sensitivity to land surface parameters[J].Journal of Hydrology,1998,211:112-125.
[13] 刘廷玺,朝伦巴根,马龙,等.规定时段降雨入渗补给系数的确定[J].内蒙古农业大学学报,2002,23:44-48.
[14] 冯伟,杨文斌,党宏忠等.毛乌素沙地流动沙丘土壤水分对降雨的响应[J].中国沙漠,2015,35(2):400-406.
[15] Gogolev,Mikhail I. Assessing groundwater recharge with two unsaturated zone modeling technologies[J].Environmental Geology,2002,42:248 258.
[16] Yang W B,Tang J N,Liang H R,et al.Deep soil water infiltration and its dynamic variation in the shifting sandy land of typical deserts in China[J].Science China:Earth Sciences,2014,57(8):1816-1824.
[17] 冯伟,杨文斌,唐进年,等.中国沙漠(地)深层渗漏量及动态特征[J].中国沙漠,2015,35(5):1362-1370.