中文关键词水化学氢氧稳定同位素黄河流域黄土高原地下水汾河 英文关键词hydrochemistrystable isotopesYellow RiverChinese Loess PlateaugroundwaterFenhe River

作者	单位	E-mail
刘鑫	西北农林科技大学旱区农业水土工程教育部重点实验室, 杨凌 712100	Liuxin213@nwafu.edu.cn
向伟	西北农林科技大学旱区农业水土工程教育部重点实验室, 杨凌 712100
司炳成	西北农林科技大学旱区农业水土工程教育部重点实验室, 杨凌 712100 萨斯喀彻温大学土壤学系, 加拿大萨斯卡通市 S7N5A8	bing.si@usask.ca

中文摘要 汾河流域是黄河的第二大支流，本文利用Piper三线图、Gibbs模型、主成分分析法、相关矩阵和正向演替模型等方法，分析了汾河流域浅层地下水的水化学和氢氧稳定同位素分布特征及其控制因素，揭示了流域水循环及水质演化过程.结果表明，汾河流域地下水属弱碱性和微硬水；优势阴阳离子分别为HCO₃^-和Ca²⁺；地下水水化学类型以Mg-Ca-HCO₃和Mg-Ca-Cl-SO₄为主，水质整体较好，Ⅰ~Ⅲ类水占比超94%.地下水δD和δ¹⁸O平均值分别为-70.2‰和-9.6‰，与7~9月降水同位素值相似，指示地下水可能主要来源于该时期的降水，并发现地下水补给方式（优势流和活塞流）存在一定的空间变化.岩石风化是地下水溶质的主要来源（87%），而大气输入和人类活动相对较小，分别占8%和5%.在岩石风化中，硅酸盐岩、蒸发盐岩和碳酸盐岩对地下水溶质的贡献相当，分别占32%、28%和26%.本研究结果可为促进可持续开发利用汾河流域地下水资源提供依据. 英文摘要 The Fenhe River basin is the second largest tributary of the Yellow River. Piper diagrams, Gibbs, PCA, correlation analysis and forward derivation modeling were used to analyze the distribution characteristics and the controlling factors of the groundwater chemistry and stable isotopes in the Fenhe River basin, which revealed the water cycle and water quality evolution process. The results indicated that the groundwater is a weakly alkaline, micro-hard water, the dominant anions and cations are HCO₃^- and Ca²⁺, the major groundwater types are Mg-Ca-HCO₃ and Mg-Ca-Cl-SO₄, the groundwater quality is good, and more than 94% of the samples belong to classes Ⅰ-Ⅲ. The average values of δD and δ¹⁸O of the Fenhe River groundwater are -70.2‰ and -9.6‰, which are similar to the isotope values of the precipitation from July to September, indicating that the groundwater may have originated from this period and that the groundwater recharge mode (dominant flow and piston flow) has a spatial variation. Rock weathering is the dominant source of ions in the groundwater, with an average contribution of 87%, while the contributions of atmospheric input and human activity are 8% and 5%, respectively. For rock weathering, silicate, evaporate, and carbonate rock contribute equally to the groundwater solutes, accounting for 32%, 28%, and 26%, respectively. The results of this study provide the basis for promoting the sustainable development and utilization of groundwater resources in the Fenhe River basin.

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