天山哈密榆树沟流域夏季洪水期河水水化学特征及其成因

doi:10.7522/j.issn.1000-0240.2016.0162

冰川冻土 ›› 2016, Vol. 38 ›› Issue (5): 1385-1393.doi: 10.7522/j.issn.1000-0240.2016.0162

天山哈密榆树沟流域夏季洪水期河水水化学特征及其成因

王晓艳¹, 李忠勤², 蒋缠文¹, 周平², 若孜罕·塔依尔³

1. 渭南师范学院化学与环境学院/陕西省河流湿地生态环境重点实验室, 陕西渭南 714000;
2. 中国科学院寒区旱区环境与工程研究所冰冻圈科学国家重点实验室/天山冰川站, 甘肃兰州 730000;
3. 哈密水文水资源勘测局, 新疆哈密 839000

收稿日期:2016-03-24 修回日期:2016-07-31 出版日期:2016-10-25 发布日期:2017-01-22
作者简介:王晓艳(1984-),女,山东临沂人,讲师,2015年在中国科学院寒区旱区环境与工程研究所获博士学位,从事同位素水化学研究.E-mail:wangxiaoyan_84@163.com.
基金资助:
国家重大科学研究计划项目（2013CBA01801）；陕西省军民融合基金项目（16JMR13）；渭南师范学院人才基金项目（16ZRRC02；16ZRRC03）；渭南师范学院特色学科项目（14TSXK05）；国家自然科学基金项目（41171061）资助

Hydrochemical characteristics and causes of the summer river water in Yushugou basin, Eastern Tianshan Mountains

WANG Xiaoyan¹, LI Zhongqin², JIANG Chanwen¹, ZHOU Ping², Ruozihan Tayier³

1. College of Chemistry and Environment Sciences, Weinan Normal University/Key Laboratory for Ecology and Environment of River Wetlands in Shaanxi Province, Weinan 714000, Shaanxi, China;
2. State Key Laboratory of Cryospheric Sciences/Tianshan Glaciological Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China;
3. Hami Hydrology and Water Resources Survey Bureau, Hami 839000, China

Received:2016-03-24 Revised:2016-07-31 Online:2016-10-25 Published:2017-01-22

摘要/Abstract

摘要：

利用2013年7-8月在哈密榆树沟水文站采集的河水样品，对主要的化学离子、pH值、电导率EC、总可溶性固体TDS进行了系统的分析，阐明了研究区离子的来源及成因.分析结果表明：榆树沟流域夏洪期径流水体呈弱碱性；HCO₃^-、Ca²⁺分别为最主要的阴、阳离子，Ca²⁺质量浓度占阳离子总数的69.45%，HCO₃^-质量浓度占阴离子总数的84.18%；水化学类型为HCO₃^--Ca²⁺；径流中所含的水化学物质一定程度上受水量的稀释作用控制；通过Gibbs图、阴阳离子三角图示法以及主要离子比值法的综合分析得出，水化学离子主要来源于H₂CO₃风化碳酸盐岩，同时还伴有少量的H₂SO₄风化碳酸盐岩，岩石风化主要以方解石矿物的溶解作用为主.

关键词: 离子含量, 水化学类型, 离子比值, 榆树沟流域

Abstract:

Using the water samples collected in Yushugou River basin during July-August, 2013, the main chemical ions, pH value, electrical conductivity and total dissolved solid were analyzed systematically, and the sources and causes of the ions were discussed. The analysis results show that the river water was weak alkaline. The main anion and cation were HCO₃^- and Ca²⁺. The concentration of Ca²⁺ accounted for 69.45% in cations, and that of HCO₃^- accounted for 84.18% in anions. Thus, hydrochemical type of the river water was H₂CO₃-Ca²⁺. During the flood period, water chemicals contained in river water were partly effected by water dilution. Based on the comprehensive analysis by Gibbs Figure, triangular diagrams of anions and cations and main ion ratio method, it was revealed that the main source of major ion in water was rock weathering. Carbonate rock weathering was mainly controlled by weathering H₂CO₃ rock accompanied by a small amount of H₂SO₄at the same time. Rock weathering were mainly composed of calcite mineral dissolution.

Key words: ion content, hydrochemical type, ionic ratio, Yushugou River basin

中图分类号:

P332.7

王晓艳, 李忠勤, 蒋缠文, 周平, 若孜罕·塔依尔. 天山哈密榆树沟流域夏季洪水期河水水化学特征及其成因[J]. 冰川冻土, 2016, 38(5): 1385-1393.

WANG Xiaoyan, LI Zhongqin, JIANG Chanwen, ZHOU Ping, Ruozihan Tayier. Hydrochemical characteristics and causes of the summer river water in Yushugou basin, Eastern Tianshan Mountains[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2016, 38(5): 1385-1393.

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天山哈密榆树沟流域夏季洪水期河水水化学特征及其成因

Hydrochemical characteristics and causes of the summer river water in Yushugou basin, Eastern Tianshan Mountains

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