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丹江流域山区地表水-地下水水化学特征及其影响因素
摘要点击 791  全文点击 127  投稿时间:2023-04-06  修订日期:2023-06-28
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中文关键词  丹江流域  水化学特征  同位素  岩石风化  离子交换
英文关键词  Danjiang River Basin  hydrochemical characteristics  isotope  rock weathering  ion exchange
作者单位E-mail
张子燕 中国地质调查局武汉地质调查中心(中南地质科技创新中心), 武汉 430205
中国地质大学地质调查研究院, 武汉 430074 
2416517557@qq.com 
伏永朋 中国地质调查局武汉地质调查中心(中南地质科技创新中心), 武汉 430205  
王宁涛 中国地质调查局武汉地质调查中心(中南地质科技创新中心), 武汉 430205
中国地质大学地质调查研究院, 武汉 430074 
 
谭建民 中国地质调查局武汉地质调查中心(中南地质科技创新中心), 武汉 430205
中国地质大学地质调查研究院, 武汉 430074 
281490085@qq.com 
刘亚磊 中国地质调查局武汉地质调查中心(中南地质科技创新中心), 武汉 430205  
中文摘要
      丹江流域是南水北调中线工程重要水源涵养区,深入研究丹江流域水化学特征及其影响因素,对区域水资源保护及合理利用具有重要意义.通过对丹江流域水样采集与分析,综合运用描述性统计、Piper三线图、Gibbs图、离子比例系数法及氢氧同位素的方法,分析丹江流域水化学特征及其影响因素.结果表明,丹江流域水体整体呈弱碱性,主要水化学类型为HCO3-Ca型,中游离子质量浓度及水化学类型变化频繁.流域水体均受大气降水补给,地表水受蒸发作用影响明显,水化学组分受岩石风化溶解、离子交换和人类活动共同影响.Ca2+和Mg2+源于方解石、白云石及石膏等碳酸盐和硫酸盐矿物溶解,农业活动是水中硝酸盐的主要来源.地表水与地下水频繁转化和支流汇入影响是丹江干流空间分布特征差异化的主要原因.
英文摘要
      The Danjiang River Basin is an important water conservation area in the middle route of the South-to-North Water Transfer Project. Studying the hydrochemical characteristics and influencing factors of the Danjiang River Basin is of great significance for the protection and rational utilization of regional water resources. In this study, water samples in the Danjiang River Basin were collected and analyzed. Descriptive statistics, Piper trilinear diagram, Gibbs diagram, ion ratio coefficient, and hydrogen and oxygen isotopes were utilized to analyze the hydrochemical characteristics and influencing factors of the Danjiang River Basin. The results showed that the water body in the study area was weakly alkaline, and the main hydrochemical type was HCO3-Ca. The ion mass concentration and hydrochemical types changed frequently in the middle reaches. The water bodies in the basin were all recharged by atmospheric precipitation, and surface water was obviously affected by evaporation. The hydrochemical compositions were influenced by rock weathering and dissolution, ion exchange, and human activities. Ca2+ and Mg2+ originated from the dissolution of carbonate and sulfate minerals such as calcite, dolomite, and gypsum. Agricultural activities were the main source of nitrate in the water. The frequent exchange of surface water and groundwater and the influence of tributary inflow were the main reasons for the spatial distribution differentiation of the Danjiang main stream.

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