干旱区生态环境知识资源中心(Arid): 敦煌月牙泉域沉积环境及泉湖水化学成因分析

Arid

	敦煌月牙泉域沉积环境及泉湖水化学成因分析
其他题名	Strata sedimentary environment and hydrochemistry cause of Lake Grescent Moon Spring in Dunhuang
	黎涛 1; 杨俊仓 2; 苏春丽 1; 马腾 1
来源期刊	干旱区地理
ISSN	1000-6060
出版年	2013
卷号	36 期号:5 页码:812-817
中文摘要	在系统分析月牙泉水文地质条件的基础上,通过野外示踪实验和地下水调查采样,结合地下水同位素研究和第四纪沉积学特征分析的方式,对区域地下水运移规律和泉域地下水径流特征进行了研究,对月牙泉地下水水化学特征及其成因进行了深入分析,对党河地表水人工回灌入渗后形成的新的地下水流与南部地下水双重补给月牙泉进行了进一步论证,并提出了该区域第四纪浅层含水层风力沉积、河流沉积成因和地下水流速之间的关系:风积砂含水层为月牙泉域地下水快速径流提供了良好的径流条件,使泉湖水与周边地下水快速循环,月牙泉周边地下水水-盐循环均衡,是月牙泉淡水湖形成的重要因素之一。
英文摘要	The Dunhuang Grescent Moon Spring is surrounded by three sides of desert, and freshwater spring lake was formed owning to groundwater overflow. The Grescent Moon Spring is renowned in the wide world as the desert and the spring coexistence. In recent decades, because of the influence of the nature factor and the artificial factor, water level of the Grescent Moon Spring continues to decline and water environment is getting worsening. At present, the main research objects on the Grescent Moon Spring are the variation of water leverl and water quantity of spring region groundwater and regional groundwater. Therefore, based on the analysis of its hydrogeologic conditions, the sedimentary environments and hydrochemistry characteristic were investigated and deeply analyzed. First, it has been verified by the field tracer test, which chose ammonium molybdate as the indicator. The test shows that the shallow groundwater flowrate is much greater than the velocity of percolation of complete aquifer. It can be concluded that this high flowrate causes the rapid water alterations of the Grescent Moon Spring and groundwater to reach the water-salt balance by the determination of twelve samples’ isotopes and sedimentary characteristics in the Quaternary period in this region, and it is also the most essential factor for the emergence of the Grescent Moon Spring in the desert region. On that basis, the research on regional groundwater migration regularity and characteristics of groundwater runoff of spring region were carried out, demonstrating that hydrochemical indexes of the spring are controlled by both groundwater formed from the filtered water after artificial recharge and groundwater from the south area. In this paper, the relation of the causes of wind deposition in the Quaternary shallow aquifer, fluvial deposition and groundwater flow velocity was demonstrated for the first time. In the spring region, depositional environment of the Quaternary loose stratum is multi-phase deposition, and vertical distribution of groundwater aquifers is obvious. Aeolian sands aquifer provides the good condition for the high flow velocity of groundwater and the rapid alternation of the water in the spring. On the other hand, knowledge is gained from studying hydrochemistry characteristics of the spring and its surrounding area, and gives some informative and powerful evidence on the causes resulting in the great differences between lake water and its surounding groundwater in hydrochemistry index. On the impact of paleogeography and sedimentary environment, the water channel swung and shrank, making the sediments contain tiny grain of material in certain areas. Relatively poor ground water runoff condition and strong evaporation lead to high-sodium in aquifer and poor water quality in the peripheral areas of Grescent Moon Spring Lake. To sum up, detailed sedimentary environment of spring area can provide strong support for the further study of groundwater flowing and hydrochemistry characteristics in this region; the research of the cause of hydrochemical index reveals the hydrodynamic relationship between spring region groundwater and regional groundwater. This paper also further demonstrates the spring formation mechanism and provides scientific foundation for emergency controlling measures.
中文关键词	月牙泉 ; 地下水 ; 水化学 ; 水盐平衡
英文关键词	the Grescent Moon Spring groundwater hydrochemistry water-salt balance
语种	中文
国家	中国
收录类别	CSCD
WOS类目	GEOLOGY ; CHEMISTRY MULTIDISCIPLINARY
WOS研究方向	Geology ; Chemistry
CSCD记录号	CSCD:4960924
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/229547
作者单位	1.(武汉)中国地质大学, 生物地质与环境地质教育部重点实验室, 武汉, 湖北 430074, 中国; 2.甘肃省地质环境监测院, 兰州, 甘肃 730050, 中国
推荐引用方式 GB/T 7714	黎涛,杨俊仓,苏春丽,等. 敦煌月牙泉域沉积环境及泉湖水化学成因分析[J],2013,36(5):812-817.
APA	黎涛,杨俊仓,苏春丽,&马腾.(2013).敦煌月牙泉域沉积环境及泉湖水化学成因分析.干旱区地理,36(5),812-817.
MLA	黎涛,et al."敦煌月牙泉域沉积环境及泉湖水化学成因分析".干旱区地理 36.5(2013):812-817.