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西南地区典型岩溶盆地夏季水文系统水-岩反应及离子特征分析

朱国锋 张真一 何元庆 蒲焘

水土保持通报2011,Vol.31Issue(6):21-25,5.
水土保持通报2011,Vol.31Issue(6):21-25,5.

西南地区典型岩溶盆地夏季水文系统水-岩反应及离子特征分析

Water-Rock Interaction and Ion Characteristics of Summer Hydrologic Systems in Typical Karst Basins

朱国锋 1张真一 2何元庆 1蒲焘3

作者信息

  • 1. 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/玉龙雪山冰川与环境观测研究站,甘肃兰州730000
  • 2. 兰州商学院图书馆,甘肃兰州730000
  • 3. 兰州大学资源环境学院,甘肃兰州730000
  • 折叠

摘要

Abstract

Different typical water samples were collected from July 22 to July 28 in 2005 in Lijiang Basin of the Hengduan Mountainous Region for chemical characteristics study.Principal component analysis(PCA) and correlation analysis were used for data analysis,the results showed that the dominant cations were Ca2+ and Mg2+,whereas SO-24 were major anions.The analytical results suggested that the orders of water concentration,from high to low,were the glacial lake water,melt water runoff,lake water,surface runoff and groundwater.PCA results showed the lithological characters definitively influenced the ion content of water in the Lijiang basin,which also were effected by human activities.Correlation analysis showed that the concentration of Na+,K+,Mg2+,Ca2+ highly correlated with the lithology,whereas Cl-,and NO-3 concentration had a positive correlation with human activities.High correlation between Ca2+ and Mg2+ suggested their strong common source.Further analysis shows that H2SO4 participating in and accelerating the carbonate and sulfate mineral dissolution related to the above.Cl-and NO-3 with strong correlation were closely related to human activities indicating Cl-and NO-3 have similar sources of which most come from human activities.

关键词

丽江盆地/可溶性离子/主成分分析法/相关分析法/物质迁移

Key words

Lijiang Basin/soluble ions/principal component analysis/correlation analysis/mass transfer

分类

天文与地球科学

引用本文复制引用

朱国锋,张真一,何元庆,蒲焘..西南地区典型岩溶盆地夏季水文系统水-岩反应及离子特征分析[J].水土保持通报,2011,31(6):21-25,5.

基金项目

国家自然科学基金项目“典型温冰川流域水文径流变化对区域水资源的影响”(40971019) 国家自然科学基金项目 ()

中国科学院“西部之光”人才培养计划 ()

国家重点基础研究发展(973)计划 ()

水土保持通报

OA北大核心CSCDCSTPCD

1000-288X

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