Zhang Xiaochen, Zhang Yongcheng, Gui Yingjia, Sun Ruiyan, Li Jun, Wu Qi, Ding Yongkang, Chen Kang
Hebei Province Collaborative Innovation Center for Sustainable Utilization of Water Resources and Optimization of Industrial Structure, Hebei GEO University, Shijiazhuang, 050031, China.
Hebei Province Key Laboratory of Sustained Utilization and Development of Water Resources, Hebei GEO University, Shijiazhuang, 050031, China.
Sci Rep. 2025 Mar 18;15(1):9294. doi: 10.1038/s41598-025-93318-5.
Water resources, as critical ecological and environmental assets, are essential to the social and economic development of countries and regions worldwide. The Jinzi River valley functions as a discharge area for industrial and domestic sewage from mining operations and residential communities along both banks. However, due to human activities, both groundwater and surface water in the region have been contaminated to varying extents. Multiple gold mines are located in the research area. Due to years of unregulated mining, this has had a serious impact on the local ecological environment and water quality. However, research on groundwater and surface water in this region, which are crucial components of the ecological environment, remains limited. This study integrates local socio-economic and hydrogeological conditions, employing methods such as multivariate statistical analysis, the Piper trilinear diagram, the Gibbs model, and ionic ratio relationships to analyze the characteristics and origins of major ions in the region. (1) The primary hydrochemical type of surface water was HCO-Ca·Na, while groundwater was predominantly of the HCO-Ca·Mg type. This hydrochemical pattern was consistent across the region, with ion concentrations significantly higher in areas dominated by carbonate rock compared to those with silicate rock. (2) Using principal component analysis, water-rock interaction modeling, and ion source analysis, it was determined that groundwater chemistry was primarily influenced by the weathering of diorite and carbonate rock, along with inputs from domestic and agricultural wastewater. In contrast, surface water chemistry was largely controlled by the weathering of carbonate rocks and the discharge of industrial wastewater. (3) Components such as SO, NO, Cl, and total dissolved solids in surface water exhibited a pronounced sensitivity to human activities, with their concentrations significantly exceeding those in groundwater. This indicates that surface water is more heavily impacted by human activities, particularly from industrial, agricultural, and domestic wastewater sources.
水资源作为重要的生态和环境资产,对全球各国和地区的社会经济发展至关重要。金子河流域是两岸采矿作业和居民区工业及生活污水的排放区。然而,由于人类活动,该地区的地下水和地表水均受到不同程度的污染。研究区域内有多个金矿。由于多年的无序开采,这对当地生态环境和水质造成了严重影响。然而,作为生态环境关键组成部分的该地区地下水和地表水的研究仍然有限。本研究结合当地社会经济和水文地质条件,采用多元统计分析、派珀三线图、吉布斯模型和离子比率关系等方法,分析该地区主要离子的特征和来源。(1)地表水的主要水化学类型为HCO-Ca·Na型,而地下水主要为HCO-Ca·Mg型。这种水化学模式在整个区域是一致的,碳酸盐岩为主的地区离子浓度明显高于硅酸盐岩地区。(2)通过主成分分析、水岩相互作用建模和离子源分析,确定地下水化学主要受闪长岩和碳酸盐岩风化以及生活和农业废水输入的影响。相比之下,地表水化学主要受碳酸盐岩风化和工业废水排放的控制。(3)地表水中的SO、NO、Cl和总溶解固体等成分对人类活动表现出明显的敏感性,其浓度明显超过地下水。这表明地表水受人类活动影响更大,特别是来自工业、农业和生活废水源的影响。