艾比湖区域地表水水化学特征干湿季变化及其控制因素

doi:10.7522/j.issn.1000-0240.2016.0163

冰川冻土 ›› 2016, Vol. 38 ›› Issue (5): 1394-1403.doi: 10.7522/j.issn.1000-0240.2016.0163

艾比湖区域地表水水化学特征干湿季变化及其控制因素

李瑞^1,2,3, 张飞^1,2,3, 高宇潇^1,2, 周梅^1,2,3, 王东芳^1,2,3, 李晓航^1,2,3

1. 新疆大学资源与环境科学学院, 新疆乌鲁木齐 830046;
2. 新疆大学绿洲生态教育部重点实验室, 新疆乌鲁木齐 830046;
3. 新疆大学智慧城市与环境建模普通高校重点实验室, 新疆乌鲁木齐 830046

收稿日期:2016-04-09 修回日期:2016-08-19 出版日期:2016-10-25 发布日期:2017-01-22
通讯作者: 张飞,E-mail:zhangfei3s@163.com. E-mail:zhangfei3s@163.com
作者简介:李瑞(1989-),女,陕西咸阳人,2016年在新疆大学获硕士学位,主要从事干旱区资源与环境遥感应用研究.E-mail:lirui001yaya@126.com
基金资助:
国家自然科学基金项目（41361045；41130531）；自治区青年科技创新人才培养工程项目（青年博士科技人才培养项目）（2013731002）资助

Surface hydrochemistry characteristics and controlling factors in the Ebinur Lake region during dry and wet seasons

LI Rui^1，2，3, ZHANG Fei^1，2，3, GAO Yuxiao^1，2, ZHOU Mei^1，2，3, WANG Dongfang^1，2，3, LI Xiaohang^1，2，3

1. College of Resources and Environment Science, Xinjiang University, Ürümqi 830046, China;
2. Key Laboratory of Oasis Ecology under Ministry of Education, Xinjiang University, Ürümqi 830046, China;
3. Key Laboratory of Xinjiang Wisdom City and Environment Modeling, Xinjiang University, Vrümqi 830046, China

Received:2016-04-09 Revised:2016-08-19 Online:2016-10-25 Published:2017-01-22

摘要/Abstract

摘要：

对2014年艾比湖区域的地表水进行观测和取样，综合运用多元统计、Piper阴阳离子三角图、Gibbs图等方法，对艾比湖区域干湿季地表水化学特征及控制因素进行了分析.结果表明：在湿季5月，Na⁺和Cl^-是占绝对优势的离子，分别占阳离子和阴离子总量的70.34%和52.97%，其次是Mg²⁺和SO₄^2-；在干季10月，Na⁺和Cl^-是占绝对优势的离子，分别占阳离子和阴离子总量的70.57%和66.48%，其次是Mg²⁺和SO₄^2-.进而判断出在湿季，艾比湖区域地表水水化学类型为以碳酸盐岩石和蒸发岩来源为主的HCO₃^--Ca²⁺-Na⁺型；而在干季，艾比湖区域地表水水化学类型为以碳酸盐岩石和蒸发岩来源为主的HCO₃^--Ca²⁺型.此外，探讨了离子控制的因素.就自然因素而言，在干湿季，艾比湖区域地表水化学离子组成受岩石风化作用和蒸发结晶作用的共同影响，大气降水的输入作用十分微弱.就人为因素而言，根据相关研究，干湿季人为活动中的主要因素是人口和地区生产总值，说明该区域受到人为活动的影响.本研究为我国干旱地区对于河水水化学变化、水质特征、水质保护都具有重要的意义.

关键词: 艾比湖区域, 地表水, 水化学特征, 干湿季, 控制因素

Abstract:

In 2014, the surface water in Ebinur Lake region was sampled and its chemical characteristics and controlling factors in dry and wet seasons were determined with multivariate statistics and piper plot of anions and cations, as well as Gibbs graphs. The results indicate that both in May (wet season) or in October (dry season), Na⁺ and Cl^- are the dominant ions, respectively, followed by Mg²⁺ and SO₄^2-. In May, Na⁺ and Cl^- account for 70.34% and 52.97% of the total cations and anions and in October, Na⁺ and Cl^- account for 70.57% and 66.48% of the total cations and anions. The hydrochemical type of the surface water in Ebinur Lake region is dominated by weathering reaction and evaporative crystallization, thus as a result, in wet season it is HCO₃^--Ca²⁺-Na⁺ type and in dry season it is HCO₃^--Ca²⁺ type. In addition, the controlling factors for the ion components in the surface water were investigated. It is found that the weathering reaction and evaporative crystallization are the major natural factors that impact the hydrochemical composition of the surface water in Ebinur Lake region during both dry and wet seasons. The influence of atmospheric precipitation input is weak. According to the relative research, the population and regional gross domestic product (GDP) are the major human activity factors that affect the hydrochemical composition of the surface water. This investigation is useful for the study of river water chemistry and water quality and for the water protection in arid regions of China.

Key words: Ebinur Lake region, surface water, hydrochemical characteristics, dry and wet seasons, controlling factors

中图分类号:

P342

李瑞, 张飞, 高宇潇, 周梅, 王东芳, 李晓航. 艾比湖区域地表水水化学特征干湿季变化及其控制因素[J]. 冰川冻土, 2016, 38(5): 1394-1403.

LI Rui, ZHANG Fei, GAO Yuxiao, ZHOU Mei, WANG Dongfang, LI Xiaohang. Surface hydrochemistry characteristics and controlling factors in the Ebinur Lake region during dry and wet seasons[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2016, 38(5): 1394-1403.

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艾比湖区域地表水水化学特征干湿季变化及其控制因素

Surface hydrochemistry characteristics and controlling factors in the Ebinur Lake region during dry and wet seasons

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