Eid Mohamed Hamdy, Saeed Omar, Szűcs Péter, Ruman Marek, Dąbrowska Dominika, Nourani Vahid
Faculty of Earth Science, Institute of Environmental Management, University of Miskolc, Miskolc-Egyetemváros, 3515, Hungary.
Geology Department, Faculty of Science, Beni-Suef University, Beni-Suef, 65211, Egypt.
Sci Rep. 2025 Jul 15;15(1):25459. doi: 10.1038/s41598-025-10322-5.
This study investigates seasonal hydrochemical characteristics of spring water at six sites in southern Poland (Leśniów, Zygmunt, Halszka, Dobro Woda, Święto Woda, and Zimny Sztok) using integrated geochemical modeling, health risk assessment, and water quality indexing. Seasonal sampling revealed distinct temporal patterns in major ion concentrations. Calcium and magnesium concentrations were significantly higher during winter (Ca: 90-96 mg/L; Mg: 5.1-7.2 mg/L) compared to summer (Ca: 19-45 mg/L; Mg: 3-5 mg/L), attributed to reduced biological uptake and enhanced carbonate dissolution at lower temperatures. Conversely, sodium (2.5-11 mg/L) and chloride (13-28 mg/L) concentrations peaked during summer due to evaporative concentration and anthropogenic influences. Heavy metals (Fe, Mn, Hg) showed maximum concentrations in summer. Hydrogeochemical analysis identified two water types: Ca-Mg-HCO and Ca-Mg-Cl/SO. PHREEQC modeling revealed undersaturation in calcite (-4.27 to 0.1), dolomite (-9.08 to -1.25), and gypsum (-2.6 to -1.78). Canadian Water Quality Index (CWQI) values (84.57-96.52) classified all samples as "Good," while Heavy Metal Pollution Index (HPI) values (20.27-120.10) and Metal Index (MI) values (0.58-2.35) indicated highest contamination at Zimny Sztok and Leśniów. Ecological Risk Index (ERI) values (0.18-4.17) suggested low ecological risk. Health risk assessment demonstrated children face 1.5-2× higher non-carcinogenic risks than adults, with maximum hazard index (HI) of 3.37 at Leśniów, primarily from mercury exposure with hazard quotient (HQ) = 3.01. Corrosion indices indicated predominantly corrosive conditions with minimal scaling potential.
本研究采用综合地球化学建模、健康风险评估和水质指数法,对波兰南部六个地点(莱斯诺夫、齐格蒙特、哈尔什卡、多布罗沃达、圣沃达和齐姆尼什托克)的泉水季节性水化学特征进行了调查。季节性采样揭示了主要离子浓度明显的时间变化模式。与夏季(钙:19 - 45毫克/升;镁:3 - 5毫克/升)相比,冬季钙和镁的浓度显著更高(钙:90 - 96毫克/升;镁:5.1 - 7.2毫克/升),这归因于较低温度下生物吸收减少和碳酸盐溶解增强。相反,由于蒸发浓缩和人为影响,钠(2.5 - 11毫克/升)和氯(13 - 28毫克/升)的浓度在夏季达到峰值。重金属(铁、锰、汞)在夏季浓度最高。水文地球化学分析确定了两种水型:钙 - 镁 - 重碳酸盐型和钙 - 镁 - 氯化物/硫酸盐型。PHREEQC建模显示方解石(-4.27至0.1)、白云石(-9.08至-1.25)和石膏(-2.6至-1.78)处于不饱和状态。加拿大水质指数(CWQI)值(84.57 - 96.52)将所有样本归类为“良好”,而重金属污染指数(HPI)值(20.27 - 120.10)和金属指数(MI)值(0.58 - 2.35)表明齐姆尼什托克和莱斯诺夫的污染程度最高。生态风险指数(ERI)值(0.18 - 4.17)表明生态风险较低。健康风险评估表明,儿童面临的非致癌风险比成年人高1.5 - 2倍,莱斯诺夫的最大危害指数(HI)为3.37,主要来自汞暴露,危害商(HQ) = 3.01。腐蚀指数表明主要为腐蚀性条件,结垢潜力最小。