Jodhani Keval H, Gupta Nitesh, Dadia Sanidhya, Patel Harsh, Patel Dhruvesh, Jamjareegulgarn Punyawi, Singh Sudhir Kumar, Rathnayake Upaka
Department of Civil Engineering, Institute of Technology, Nirma University, Ahmedabad, 382481, Gujarat, India.
Department of Mechanical Engineering, Institute of Technology, Nirma University, Ahmedabad, 382481, Gujarat, India.
Sci Rep. 2025 Mar 13;15(1):8769. doi: 10.1038/s41598-025-92053-1.
Groundwater quality assessment is crucial for sustainable water resource management and public health protection. This study evaluated the Water Quality Index (WQI) of groundwater in the southern part of Gujarat focusing on the Valsad District. Groundwater in this region occurs in porous, unconsolidated formations and fracture formations, both under groundwater table conditions and confined aquifers. Various parameters including Nitrate (NO¯), pH, Calcium (Ca), Electrical Conductivity (EC), Total Hardness (TH), Magnesium (Mg), Total Dissolved Solids (TDS), Potassium (K), Sodium (Na), Sulphate (SO), Chloride (Cl¯), Bicarbonate (HCO¯), Silicate (SiO), and Fluoride (F¯) were analyzed to assess groundwater quality. Results indicate that most of the parameters fell within acceptable permissible limits for drinking water, except for Muli and Nanaponda villages with the parameters Cl¯, EC, and TDS exceeding the permissible limit. The WQI analysis revealed that 31.25% of water samples from different villages were found in the excellent category (WQI < 25). About 68.75% of samples from 16 villages were classified as good quality category (WQI ∼ 25-50). Overall, the WQI ranged from 14.20 to 41.98, suggesting that groundwater in the Valsad district is suitable for drinking. The Piper diagram analysis of water samples collected from the field indicated unique geochemical compositions and good water. The diagram revealed that the Ca was the predominant cation, followed by K, Na, and Mg. Among the anions, the HCO showed the highest concentrations, followed by SO, NO, and Cl. This dominance pattern demonstrated that the weathering of minerals significantly influenced the groundwater. This study recommends remediation for areas with reduced water quality to address geogenic and anthropogenic contamination.
地下水质量评估对于可持续水资源管理和公共卫生保护至关重要。本研究评估了古吉拉特邦南部瓦尔萨德区地下水的水质指数(WQI)。该地区的地下水存在于多孔、未固结地层以及裂隙地层中,包括潜水位条件下的和承压含水层中的。分析了包括硝酸盐(NO¯)、pH值、钙(Ca)、电导率(EC)、总硬度(TH)、镁(Mg)、总溶解固体(TDS)、钾(K)、钠(Na)、硫酸盐(SO)、氯化物(Cl¯)、碳酸氢盐(HCO¯)、硅酸盐(SiO)和氟化物(F¯)等各种参数,以评估地下水质量。结果表明,除了穆利村和纳纳蓬达村的氯化物(Cl¯)、电导率(EC)和总溶解固体(TDS)参数超过允许限值外,大多数参数都在饮用水可接受的允许限值范围内。WQI分析显示,来自不同村庄的31.25%的水样属于优良类别(WQI < 25)。来自16个村庄的约68.75%的样本被归类为良好质量类别(WQI ∼ 25 - 50)。总体而言,WQI范围为14.20至41.98,表明瓦尔萨德区的地下水适合饮用。对实地采集的水样进行的派珀图分析表明,其具有独特的地球化学组成且水质良好。该图显示,Ca是主要阳离子,其次是K、Na和Mg。在阴离子中,HCO浓度最高,其次是SO、NO和Cl。这种优势模式表明,矿物的风化对地下水有显著影响。本研究建议对水质下降的地区进行修复,以应对地质成因和人为污染。