Zhao Chun-Hong, Shen Hao-Yong, Wang Zhi-Heng, Liang Yong-Ping, Zhao Yi, Xie Hao, Tang Chun-Lei
Key Laboratory of Karst Dynamics, Ministry of Natural Resources/Guangxi, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, China.
School of Environment and Spatial Informatics, China University of Mining and Technology, Xuzhou 221116, China.
Huan Jing Ke Xue. 2022 Oct 8;43(10):4440-4448. doi: 10.13227/j.hjkx.202201103.
The Fenhe River Basin is the mother river of Shanxi Province. Due to the over-exploitation of water resources and the impact of social and economic development, the ecological environment has deteriorated. After a series of treatment and protection measures, the water quality has since been improved. Mathematical statistics, Piper diagrams, Gibbs model, hydrogen and oxygen isotopes, and other methods were used to analyze the characteristics and sources of hydrochemistry in the surface water of the Fenhe River basin, which revealed the evolution process of surface water quality of the Fenhe River basin. The results showed that the content of the main hydrochemical components in the main stream surface water of Fenhe River basin increased gradually along the runoff path. The hydrochemical types of surface water of Fenhe River basin were mainly HCO·SO·Cl-Ca·Na·Mg and SO·HCO·Cl-Ca·Na·Mg. There were great differences in hydrochemical components of tributaries and karst water in the basin. There were also great differences in hydrochemical components of tributaries in the basin. The hydrochemical types of surface water of karst water were mainly SO·HCO-Ca·Mg. The hydrochemical composition of surface water in Fenhe River basin was mainly affected by rock weathering and evaporation crystallization, whereas rainfall had little effect. Na and K mainly came from the dissolution of evaporated salt rocks with Na in the surrounding loess. Ca, Mg, and HCO mainly came from the dissolution of carbonate rocks. SO may have also come from the dissolution of sulfide minerals in the loess layer around Fenhe River in addition to the dissolution of gypsum. The values of D and O of Fenhe River surface water were gradually enriched from upstream to downstream. The characteristics of hydrogen and oxygen isotopes further showed that the surface water was mainly affected by evaporation. The results of this study can provide evidence for ecological restoration and protection and ecological civilization construction in the Fenhe River basin.
汾河流域是山西省的母亲河。由于水资源过度开发以及社会经济发展的影响,生态环境已恶化。经过一系列治理与保护措施后,水质自此得到改善。运用数理统计、Piper图、吉布斯模型、氢氧同位素等方法,对汾河流域地表水水化学特征及来源进行分析,揭示了汾河流域地表水水质演变过程。结果表明,汾河流域干流地表水主要水化学组分含量沿径流路径逐渐增加。汾河流域地表水水化学类型主要为HCO·SO·Cl-Ca·Na·Mg和SO·HCO·Cl-Ca·Na·Mg。流域内支流与岩溶水的水化学组分存在较大差异,流域内各支流的水化学组分也存在较大差异。岩溶水地表水水化学类型主要为SO·HCO-Ca·Mg。汾河流域地表水水化学组成主要受岩石风化和蒸发结晶影响,而降雨影响较小。Na和K主要来源于周边黄土中含Na蒸发盐岩的溶解。Ca、Mg和HCO主要来源于碳酸盐岩的溶解。SO除来源于石膏溶解外,可能还来源于汾河周边黄土层中硫化物矿物的溶解。汾河地表水D和O值自上游至下游逐渐富集。氢氧同位素特征进一步表明地表水主要受蒸发影响。本研究结果可为汾河流域生态修复与保护及生态文明建设提供依据。