叶普曲高寒岩溶流域水化学特征及水质评价OA
Hydrochemical characteristics and water quality assessment of Yepuqu alpine karst basin
高寒岩溶水作为亚洲水塔的重要组成部分,其水质是青藏高原可持续发展最重要的环境问题之一.文章选取拉萨河流域北侧叶普曲岩溶流域为研究对象,开展流域地表水、地下水水化学特征及水质评价研究,运用水化学分析、主成分分析、单因子评价和综合污染指数评价进行研究,结果表明叶普曲岩溶流域水体中Ca2+、HCO3-的毫克当量百分数均大于对应阴阳离子的50%,岩溶地下水和地表水水化学类型为HCO3-Ca和HCO3·SO4-Ca型;离子平衡图分析表明地表水以方解石溶解、方解石与白云石共同溶解作用的占比为83%、17%;地下水以方解石溶解、方解石和白云石共同溶解的占比为67%、33%.岩石风化溶解作用是控制是水化学组成的主要机制,此外还伴有阳离子交换作用.叶普曲岩溶流域水质分析表明单因子评价分析的21组水样中Ⅲ类水占86%,Ⅳ和Ⅴ类水占14%,综合污染指数评价结果表明研究区为优质水.TN是单因子评价中的关键指标参数,水体中超标指标参数氮主要来自化肥输入.主成分分析表明研究区水质主要受3个主因子控制:人类活动、天然地层背景值以及二者的复合影响.
As a vital component of the"Asian Water Tower",the water quality of alpine karst water is one of the most critical environmental challenges for sustainable development on the Qinghai-Xizang Plateau.The Lhasa river basin,a core water source area in Xizang,plays a pivotal role in both the health of local residents and the ecological security of Asia's water systems.However,current research on karst water predominantly focuses on low-altitude regions,leaving significant gaps in understanding high-altitude karst systems.This study focuses on the Yepuqu karst basin,a tributary of the Lhasa river in northern Xizang,to investigate the hydrochemical characteristics and water quality of both surface water and groundwater.The research aims to reveal the hydrochemical composition and water quality features of a typical alpine karst basin,as well as the key controlling factors influencing the water quality.The systematic collection of surface water and groundwater in the Yepuqu karst basin was analyzed using methods such as hydrochemical analysis,principal component analysis,single-factor index,and comprehensive pollution index.The results indicated that the milliequivalent percentages of Ca2+and HCO3-in the water bodies both exceeded 50%of their corresponding cations and anions,with the hydrochemical types of karst groundwater and surface water classified as HCO3-Ca and HCO3·SO4-Ca types,respectively.Ion balance diagram analysis showed that surface water was dominated by 83%calcite dissolution and 17%a combination of calcite and dolomite dissolution,while groundwater exhibited 67%calcite dissolution and 33%combined calcite-dolomite dissolution.The weathering and dissolution of rocks were the primary mechanisms controlling water mineralization,with both surface water and groundwater dominated by calcite dissolution,followed by combined dissolution of calcite and dolomite.Additionally,cation exchange reactions were also involved.The water quality analysis of the Yepuqu karst basin indicated that 86%of the 21 water samples evaluated by single-factor assessment belong to Class Ⅲ,while 14%were Class Ⅳ and Ⅴ.The comprehensive pollution index assessment further showed that the study area was of high-quality water.The results of two assessments showed certain discrepancies,primarily due to their differing assessment principles.Decision-makers can adopt a dual-track evaluation system combining"single-factor qualitative assessment+comprehensive pollution index quantitative assessment"to define different water quality conditions,thereby implementing more effective water resource management measures.This approach holds significant practical value for the comprehensive governance of water resources.Among them,Total Nitrogen(TN)was a key parameter in single-factor assessment,and the excessive nitrogen in water bodies primarily originates from fertilizer inputs.To address the issue of excessive TN levels in agricultural areas,an integrated prevention and control strategy of"source reduction,process interception,and smart monitoring"is recommended.This includes implementing crop rotation to reduce nitrogen fertilizer demand,applying soil testing-based formula fertilization with furrow-covering techniques to enhance nitrogen utilization efficiency,replacing chemical fertilizers with organic alternatives,and transforming drainage ditches into ecological filter beds to intercept nitrogen in runoff.Additionally,deploying soil moisture sensors for variable-rate fertilization can improve nitrogen agronomic efficiency.These measures collectively contribute to effective nitrogen management and water quality protection.The principal component analysis revealed that the primary factors influencing groundwater quality in the study area,ranked in order of significance,were anthropogenic activities,natural geological background values,and the composite effects of natural geological background and anthropogenic activities.For surface water quality,the key influencing factors followed the order of natural formation background values,anthropogenic activities,and the composite effects of natural geological background and anthropogenic activities.The results indicated that water quality in the study area was primarily influenced by three key factors:anthropogenic activities,natural formation background values,and the composite effects of natural geological background and anthropogenic activities.This study investigated the hydrochemical characteristics and water quality assessment of the Yepuqu alpine karst basin,which held significant theoretical and practical value for establishing a plateau water source protection system and safeguarding the ecological security of the"Asian Water Tower".
廖红为;任坤;马俊飞;吴华英;贺丽;王雨;王艳;刘海永;潘晓东;黄奇波;李腾芳;邹昌霈
中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406西藏自治区地质调查院,西藏拉萨 850000西藏自治区地质调查院,西藏拉萨 850000西藏自治区地质调查院,西藏拉萨 850000西藏自治区地质调查院,西藏拉萨 850000中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室/联合国教科文组织国际岩溶研究中心/岩溶动力系统与全球变化国际联合研究中心,广西桂林 541004||广西平果喀斯特生态系统国家野外科学观测研究站,广西平果 531406
天文与地球科学
叶普曲高寒岩溶流域岩溶水水化学特征水质评价
Yepuqualpine karst basinkarst waterhydrochemical characteristicswater quality assessment
《中国岩溶》 2026 (1)
112-127,16
中央引导地方项目(XZ202301YD0005C)广西基金项目(2025GXNSFAA069189)国家基金项目(42372294,42572328)省部合作项目(2024ZRBSHZ091)中国地质调查局项目(DD20250501408)广西科技计划项目(桂科AB25069138)广西科技计划项目(桂科AB24010016)中国地质科学院岩溶地质研究所基本业务费项目(2023007)
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