祁连山黑河源区八一冰川-黄藏寺段河水水文地球化学特征

doi:10.7522/j.issn.1000-0240.2017.0077

冰川冻土 ›› 2017, Vol. 39 ›› Issue (3): 680-687.doi: 10.7522/j.issn.1000-0240.2017.0077

祁连山黑河源区八一冰川-黄藏寺段河水水文地球化学特征

冯亚伟¹, 孙自永², 补建伟², 蔡鹤生²

1. 山东省鲁南地质工程勘察院, 山东兖州 272100;
2. 中国地质大学, 湖北武汉 430074

收稿日期:2017-01-09 修回日期:2017-03-16 出版日期:2017-06-25 发布日期:2017-09-09
通讯作者: 孙自永,E-mail:ziyong.sun@gmail.com E-mail:ziyong.sun@gmail.com
作者简介:冯亚伟(1990-),男,山东济宁人,助理工程师,2014年毕业于中国地质大学(武汉),从事盆地岩溶水方面研究.E-mail:1102844258@qq.com
基金资助:
地质矿产调查评价国家专项“青藏高原矿产资源开发地质环境承载力评价”（12120113038400）资助

The hydrogeochemical characteristics of the river water in the section from Bayi Glacier to Huargzangsi of the Heihe River, Qilian Mountains

FENG Yawei¹, SUN Ziyong², BU Jianwei², CAI Hesheng²

1. Shandong Lunan Geological Engineering Investigation Institute, Yanzhou 272100, Shandong, China;
2. China University of Geosciences, Wuhan 430074, China

Received:2017-01-09 Revised:2017-03-16 Online:2017-06-25 Published:2017-09-09

摘要/Abstract

摘要： 黑河源区河水水文地球化学特征的研究有助于了解黑河源区河水沿流域水质变化概况，对黑河源区生态环境的保护具有积极意义。以黑河源区干流为研究对象，对河水进行取样检测，结果显示：河水化学组成以K⁺、Na⁺、Ca²⁺、Mg²⁺和Cl^-、NO₃^-、HCO₃^-、SO₄^2-为主。通过聚类分析、舒卡列夫分类和Piper三线图分析发现主要离子中，阳离子主要来源于石灰岩风化产物，SO₄^2-主要来源于蒸发岩矿物风化产物和人类活动，HCO₃^-主要来源于纯碳酸盐风化产物。通过对重金属污染调查发现，V、Co、Cu、Pb、Cr、Mn和Zn含量较高，矿山开采是重金属污染的主要来源。

关键词: 黑河源区, 地表水, 水文地球化学, 水质分析, 聚类分析

Abstract: Research of the hydrogeochemistry in the source regions of the Heihe River is useful to search the basic changes in water quality along the river, and has positive significance for protecting the eco-environment in the regions. Through the previous researches, the lack of relevant background information about water quality in the source regions has improved. In this study, the source regions of the Heihe River are taken as the research object to understand the water quality of the river basin, through sampling and tasting the river water. The results show that the major chemical composition of the river water are K⁺, Na⁺, Ca²⁺, Mg²⁺ and Cl^-, NO₃^-, HCO₃^-, SO₄^2-. According to cluster analysis, Schukalev classification and trilinear diagram analysis, it was found that among the major ions, cations mainly comes from limestone weathering products, SO₄^2- mainly comes from evaporating of mineral weathering products and human activities, and HCO₃^- mainly comes from pure carbonate weathering substances. Through heavy metal pollution surveying, it was found that the content of V, Co, Cu, Pb, Cr, Mn and Zn are much higher, and mine exploration is the main cause of heavy metal pollution.

Key words: Heihe River riparian areas, surface water, hydrogeochemistry, water quality analysis, cluster analysis

中图分类号:

P342

冯亚伟, 孙自永, 补建伟, 蔡鹤生. 祁连山黑河源区八一冰川-黄藏寺段河水水文地球化学特征[J]. 冰川冻土, 2017, 39(3): 680-687.

FENG Yawei, SUN Ziyong, BU Jianwei, CAI Hesheng. The hydrogeochemical characteristics of the river water in the section from Bayi Glacier to Huargzangsi of the Heihe River, Qilian Mountains[J]. JOURNAL OF GLACIOLOGY AND GEOCRYOLOGY, 2017, 39(3): 680-687.

参考文献

[1] Ma Shenglin. The ecological changes of Tibetan Plateau[M]. Beijing:Social Sciences Academic Press, 2011.[马生林. 青藏高原生态变迁[M]. 北京:社会科学文献出版社, 2011.]
[2] Qin Jiahai, Zhang Yong, Zhao Yunchen, et al. Soil physicochemical properties and variations of nutrients and enzyme activity in the degrading grasslands in the upper reaches of the Heihe River, Qilian Mountains[J]. Journal of Glaciology and Geocryology, 2014, 36(2):335-346.[秦嘉海, 张勇, 赵芸晨, 等. 祁连山黑河上游不同退化草地土壤理化性质及养分和酶活性的变化规律[J]. 冰川冻土, 2014, 36(2):335-346.]
[3] Lu Zhixiang, Zou Songbing, Xiao Honglang, et al. How to determine drainage area threshold in alpine regions of upper reaches of Heihe River[J]. Journal of Glaciology and Geocryology, 2015, 37(2):493-499.[陈志翔, 邹松兵, 肖洪浪, 等. 黑河上游高寒山区集水面积阈值确定方法探讨[J]. 冰川冻土, 2015, 37(2):493-499.]
[4] Ruan Yunfeng, Zhao Liangju, Xiao Honglang, et al. The groundwater in the Heihe River basin:isotope age and renewability[J]. Journal of Glaciology and Geocryology, 2015, 37(3):767-782.[阮云峰, 赵良菊, 肖洪浪, 等. 黑河流域地下水同位素年龄及可更新能力研究[J]. 冰川冻土, 2015, 37(3):767-782.]
[5] Zhang Jishi, Kang Ersi, Lan Yongchao, et al. Studies of the transformation between surface water and groundwater and the utilization ratio of water resources in Hexi region[J]. Journal of Glaciology and Geocryology, 2001, 23(4):375-382.[张济世, 康尔泗, 蓝永超, 等. 河西内陆河地表水与地下水转化及水资源利用率研究[J]. 冰川冻土, 2001, 23(4):375-382.]
[6] Feng Ling, Su Junxi, Shen Beiping. Characteristics and composition analysis of water and sediment in the upper reaches of Heihe River[C]//Proceedings of the Fourth Symposium on Hy-drology and Sediment Professional Committee of China Hydropower Engineering Society. Beijing:China Water Power Press, 2003:202-204.[冯玲, 苏军希, 沈北平. 黑河上游水沙特征及组成分析[C]//中国水力发电工程学会水文泥沙专业委员会第四界学术讨论会论文集. 北京:中国水利水电出版社, 2003:202-204].
[7] Wang Chenghai, Jin Shuanglong, Shi Hongxia. Area change of the frozen ground in China in the next 50 year[J]. Journal of Glaciology and Geocryology, 2014, 36(1):1-8.[王澄海, 靳双龙, 施红霞. 未来50 a中国地区冻土面积分布变化[J]. 冰川冻土, 2014, 36(1):1-8.]
[8] Wu Xiaobo, Li Quanlian, He Jianqiao, et al. Hydrochemical characteristics and inner-year process of upper Heihe River in summer half year[J]. Journal of Desert Research, 2008, 28(6):1190-1196.[武小波, 李全莲, 贺建桥, 等. 黑河上游夏半年河水化学组成及年内过程[J]. 中国沙漠, 2008, 28(6):1190-1196.]
[9] Zhang Renquan, Liang Xing, Jin Menggui, et al. Fundamentals of hydrogeology[M]. Beijing:Geological Publishing House, 2011.[张人权, 梁杏, 靳孟贵, 等. 水文地质学基础[M]. 北京:地质出版社, 2011.]
[10] Fetter C W. Applied hydrogeology[M]. 4th ed. Sun Jinyu. trans. Beijing:Higer Education Press, 2011.[Fetter C W. 应用水文地质学[M]. 4版. 孙晋玉, 译. 北京:高等教育出版社, 2011.]
[11] 沈照理, 朱宛华, 钟佐燊. 水文地球化学基础[M]. 北京:地质出版社, 1993.[Shen Zhaoli, Zhu Wanhua, Zhong Zuoshen. Fundamentals of hydrogeochemistry[M]. Beijing:Geological Press, 1993.]
[12] Xiang Dongjin, Li Hongwei, Liu Xiaoya, et al. Applied multivariate statistical analysis[M]. Wuhan:China University of Geosciences Press, 2011.[向东进, 李宏伟, 刘小雅, 等. 实用多元统计分析[M]. 北京:中国地质大学出版社, 2005.]
[13] Bu Jianwei, Zhou Aiguo, Zhou Jianwei, et al. Application of different hierarchical clustering methods to hydrochemical classification[J]. Geotechnical Investigation & Surveying, 2013, 41(10):42-48.[补建伟, 周爱国, 周建伟, 等. 不同系统聚类法在水化学分类中的应用[J]. 工程勘查, 2013, 41(10):42-48.]

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祁连山黑河源区八一冰川-黄藏寺段河水水文地球化学特征

The hydrogeochemical characteristics of the river water in the section from Bayi Glacier to Huargzangsi of the Heihe River, Qilian Mountains

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