干旱区生态环境知识资源中心(Arid): Magnetic resonance sounding evidence shows that shallow groundwater discharge maintains the lake landscape in the Hunshandake Sandy Land, North China

Arid

DOI	10.1007/s12665-020-09076-2
	Magnetic resonance sounding evidence shows that shallow groundwater discharge maintains the lake landscape in the Hunshandake Sandy Land, North China
	Yu, Xiangqian 1,2; Wu, Yongsheng 2; Jiang, Chuandong 3; Zhang, Zhifu 2; Du, Xiaofeng 2; Liu, Tiejun 2
通讯作者	Yu, Xiangqian ; Wu, Yongsheng
来源期刊	ENVIRONMENTAL EARTH SCIENCES
ISSN	1866-6280
EISSN	1866-6299
出版年	2020
卷号	79 期号:13
英文摘要	The Hunshandake Sandy Land (HSL) is a well-known water-rich sandy region in China that is home to many lakes. Most of these lakes are sustained by groundwater inflow. However, due to the limited hydrogeological survey data, the mechanism by which the lakes interact with groundwater is not well understood. Magnetic resonance sounding (MRS) is a geophysical method that has emerged in recent years that can directly detect the distribution of groundwater and determine the lithology of the aquifer medium. Compared with drilling, this method is convenient, rapid, and inexpensive. In this study, to determine how the lakes are recharged by groundwater, a field experiment using MRS was conducted on Haoletuyin Lake, which is located in the central HSL. The results showed that compared with borehole data, the MRS-derived aquifer depth has an uncertainty of 6.88%. Additionally, the lithology of the media derived from the MRS is consistent with that derived from the borehole data. This finding suggests that the MRS-derived results are highly accurate. Based on the MRS-derived results, two hydrogeological profiles were plotted, and they show that the lake in the experimental area is recharged primarily by shallow groundwater and not by deep groundwater. This study is significant because it not only reveals the mechanism by which Haoletuyin Lake is maintained, but also proves that MRS is an excellent tool for studying lake-groundwater relations in desert (sandy land) regions with limited hydrogeological survey data.
英文关键词	Lake-groundwater relation Magnetic resonance sounding Hunshandake sandy land China
类型	Article
语种	英语
国家	Peoples R China
收录类别	SCI-E
WOS记录号	WOS:000545998000002
WOS关键词	BADAIN JARAN DESERT ; HYDRAULIC TRANSMISSIVITY ; SOUTHERN PART ; WATER-BALANCE ; HARD ROCKS ; MRS ; AQUIFER ; RECHARGE ; INVERSION ; DESERTIFICATION
WOS类目	Environmental Sciences ; Geosciences, Multidisciplinary ; Water Resources
WOS研究方向	Environmental Sciences & Ecology ; Geology ; Water Resources
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/319502
作者单位	1.China Inst Water Resources & Hydropower Res, State Key Lab Simulat & Regulat Water Cycle River, Beijing 100038, Peoples R China; 2.China Inst Water Resources & Hydropower Res, Inst Water Resources Pastoral Area, Hohhot 010020, Peoples R China; 3.Jilin Univ, Coll Instrumentat & Elect Engn, Changchun 130061, Peoples R China
推荐引用方式 GB/T 7714	Yu, Xiangqian,Wu, Yongsheng,Jiang, Chuandong,et al. Magnetic resonance sounding evidence shows that shallow groundwater discharge maintains the lake landscape in the Hunshandake Sandy Land, North China[J],2020,79(13).
APA	Yu, Xiangqian,Wu, Yongsheng,Jiang, Chuandong,Zhang, Zhifu,Du, Xiaofeng,&Liu, Tiejun.(2020).Magnetic resonance sounding evidence shows that shallow groundwater discharge maintains the lake landscape in the Hunshandake Sandy Land, North China.ENVIRONMENTAL EARTH SCIENCES,79(13).
MLA	Yu, Xiangqian,et al."Magnetic resonance sounding evidence shows that shallow groundwater discharge maintains the lake landscape in the Hunshandake Sandy Land, North China".ENVIRONMENTAL EARTH SCIENCES 79.13(2020).