Hydrogeochemical processes, and health risk assessment of groundwater, in Santa Maria del rio aquifer: A case study of San Luis Potosi valley, Mexico

被引:0
|
作者
Fuentes-Rivas, Rosa Maria [1 ,3 ]
Santacruz-De Leon, German [2 ]
Ramos-Leal, Jose Alfredo [1 ]
Alvarez-Bastida, Carolina [3 ]
Moran-Ramirez, Janete [4 ]
机构
[1] Potosin Inst Sci & Technol Res CA IPICYT, Appl Geosci Div, Camino Presa San Jose 2055,Lomas 4a, San Luis Potosi 78216, San Luis Potosi, Mexico
[2] Coll San Luis CA COLSAN, Water & Soc Program, Parque Macul 155, San Luis Potosi 78294, San Luis Potosi, Mexico
[3] Autonomous Univ State Mexico, Fac Engn, Cerro Coatepec S-N,Ciudad Univ, Toluca De Lerdo 50110, Mexico
[4] Potosin Inst Sci & Technol Res CA IPICYT, IPICYT, Catedras CONACYT, Appl Geosci Div, San Luis Potosi, Mexico
关键词
Health risk; Hydrogeochemical processes; Groundwater quality; Mexico; San Luis Potosi; WATER-QUALITY INDEX; HYDROCHEMICAL CHARACTERISTICS; HEAVY-METALS; RIVER-BASIN; TAMIL-NADU; DRINKING; CITY; SALINITY; DISTRICT; REGION;
D O I
10.1016/j.gsd.2024.101268
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The main objectives of this research were to the hydrogeochemical processes that control the groundwater chemistry, groundwater quality, and assessment of health risks of water. The drinking water that supplies the community of Santa Mar & iacute;a del Rio, S.L.P., comes from groundwater, in some municipality localities, groundwater Fluorine and arsenic are reported. Twenty-one representative groundwater samples were taken. Physicochemical parameters in situ: pH, OD, ORP, Alkalinity, STD, EC, Salinity, Total Coliforms, and E-coli, were analyzed, and in the laboratory, the heavy metals, metalloids and major constituents, cations: calcium, sodium, magnesium, and potassium, were determined by the ICP, and anions: chlorides, and sulfates, by colorimetry techniques. The results of the analyses were compared with the Mexican and EPA drinking water standards to verify their suitability and ensure that they do not exceed the permitted limit values. The results of the chemistry of the principal groundwater ions in the study area suggest that the main hydrogeochemical process that controls the variation of groundwater quality is the rock-water interaction. Groundwater has been classified into two hydrochemical facies, CaMgHCO3 and NaHCO3, consistent with the type of rock. The samples with the CaMg-HCO3 facie are associated with less evolved waters located in areas with local recharge. The dominant reactions in the aquifer are calcite, dolomite, and gypsum solutions. The presence of the N-NO3- ion is associated with agricultural and urban zone influence, which indicates that this activity has impacted the water quality. The risk index (HI) results show that values > 0.1 < 1 of HI, for Pb present low chronic risks for adults and children. In contrast, HI values > 4 for both population groups represent high chronic risk. Excessive use of fertilizers should be controlled in the study area to prevent groundwater contamination by heavy metals and metalloids and be measured regularly to check drinking water quality.
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页数:16
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