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[1]LI Shaohua,YIN Shule,WANG Xuequan,et al.Survey on Hydrology and Water Quality in the Gobi Desert Region of Northwestern China[J].Research of Soil and Water Conservation,2016,23(02):148-151,156.

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Survey on Hydrology and Water Quality in the Gobi Desert Region of Northwestern China

Research of Soil and Water Conservation[ISSN 1005-3409/CN 61-1272/P] Volume: 23 Number of periods: 2016 02 Page number: 148-151,156 Column: Public date: 2016-04-28

Title:: Survey on Hydrology and Water Quality in the Gobi Desert Region of Northwestern China

Author(s):: LI Shaohua¹, YIN Shule¹, WANG Xuequan¹, CUI Xianghui¹, GAO Qi²; 1. Institute of Desertification Studies, Chinese Academy of Forestry, Beijing 100093, China;
2. College of Ecology and Environmental Science, Inner Mongolia Agriculture University, Hohhot 010019, China

Keywords:: gobi; hydro-graphic survey; impermeable channel; water chemistry

CLC:: X824

DOI:: -

Abstract:: In order to find out the current situation of hydrology and water chemistry of rivers in Gobi region, we went to the Tarim Basin and the south of the Qaidam Basin in September 2014 and surveyed 12 typical rivers. We reached our goals through collecting water samples, measuring the flow rate in the field, acquiring data analyzing samples in laboratory. The results showed that: (1) the impermeable channel and reservoir built in Gobi region had the adverse influence on normal development of rivers; (2) the contents of F^- were more than 1 mg/L, so it couldn’t meet the drinking standard, however, F^- and Ca²⁺ showed negative correlation; (3) cation intensity of water decrease in the order: Ca²⁺ > Na⁺ > Mg²⁺ > K⁺, the mainly chemical type of river water were Cl^-·SO₄^2-·HCO₃^-/Na⁺·Ca²⁺; (4) the total dissolved solid (TDS) in river water was general high, and ranged between 718.3 mg/L and 8 254.1 mg/L; pH varied between 7.44 and 8.07, and presented the alkalinity.

References:: [1] 冯益明,吴波,周娜,等.基于遥感影像识别的戈壁分类体系研究[J].中国沙漠,2013,33(3):635-641.
[2] 王涛,陈广庭.西部地标:中国的沙漠、戈壁[M].上海:上海科学技术文献出版社,2008:216-224.
[3] 李静,孙虎,邢东兴,等.西北干旱与半干旱区湿地特征与保护[J].中国沙漠,2003,23(6):670-674.
[4] 毛德华,夏军,黄友波.西北地区水资源与生态环境问题及其形成机制分析[J].自然灾害学报,2004,13(4):55-61.
[5] 刘蔚,王涛,高晓清,等.黑河流域水体化学特征及其演变规律[J].中国沙漠,2004,24(6):755-762.
[6] 陈亚宁,杨青,罗毅,等.西北干旱区水资源问题研究思考[J].干旱区地理,2012,35(1):1-9.
[7] 迪丽努尔·阿吉,艾克巴尔.新疆主要河流径流量变化的时空特征研究[J].干旱区资源与环境,2009,23(11):100-104.
[8] 谭毅.柴达木盆地水系、地表水资源及其特点[J].水利科技与经济,2014,20(4):51-54.
[9] 中国地质调查局.柴达木盆地地下水资源及其环境问题调查评价[M].北京:地质出版社,2008:25-28.
[10] 郭慕萍,王志伟,秦爱民.54a来中国西北地区降水量的变化[J].干旱区研究,2009,26(1):120-125.
[11] 卢爱刚,熊友才.全球气候变化背景下近五十年中国湿度区域变化趋势[J].水土保持研究,2013,20(1):141-143.
[12] 王建,韩海东,赵求东,等.塔里木河流域水化学组成分布特征[J].干旱区研究,2013,30(1):10-15.
[13] 郝永娟,吐尔逊·哈斯木,杨家军,等.塔里木河径流量变化对下游沙漠化的影响研究[J].水土保持研究,2013,20(6):145-150.
[14] 冉景江,陈敏,陈永柏.三峡工程影响下游水生态环境的径流调节作用分析[J].水生态学杂志,2011,32(1):1-6.
[15] 刘蔚,王涛,高晓清,等.黑河流域水体化学特征及其演变规律[J].中国沙漠,2004,24(6):755-761.
[16] 严平,李文赞,王学全,等.库姆塔格沙漠水文调查初步结果[J].中国沙漠,2011,31(1):242-246.
[17] 周长进,董锁成.柴达木盆地主要河流的水质研究及水环境保护[J].资源科学,2002,24(2):37-41.
[18] Meybeck M. Global chemical weathering of surficial rocks estimated from river dissolved loads[J]. American Journal of Science, 1987,287(5):401-428.
[19] 王根绪,程国栋.西北干旱区水中氟的分布规律及环境特征[J].地理科学,2000,20(2):153-159.
[20] 张芳,段汉明,张婷.北疆城镇区域社会经济与绿洲生态系统协调发展评价[J].干旱区资源与环境,2014,28(5):7-12.

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