Department of Civil Engineering, Hindusthan College of Engineering and Technology (Autonomous), Coimbatore, 641032, India.
Department of Geology, University of Peradeniya, Peradeniya, 20400, Sri Lanka.
Environ Geochem Health. 2024 Jul 16;46(9):326. doi: 10.1007/s10653-024-02111-2.
This research examines whether the groundwater in the Sivakasi Region of South India is suitable for consumption, and assesses the possible health hazards for various age demographics including infants, children, teenagers, and adults. A total of 77 groundwater samples were gathered, covering a total area of 580 km and analyzed for major and minor ions. The hydrogen ion concentration (pH) of the samples indicates neutral to marginally alkaline. The total dissolved solids (TDS) fluctuate from 255 to 2701 mg/l and electrical conductivity varies from 364 to 3540 µS/cm. A wide range of fluoride concentration was detected (0.1 to 3.2 mg/l) with nearly 38% groundwater samples surpassing the proposed limit (1.5 mg/l) suggested by the World Health Organization in 2017. Gibbs plot analysis suggested that most of the samples were influenced by geogenic factors, primarily rock weathering in this region. Correlation analysis showed that most of the samples were impacted by both natural and human sources. The pollution index of groundwater (PIG) fluctuated from 0.67 to 2.60 with approximately 30% and 53% of samples falling into insignificant and low pollution categories, respectively. Furthermore, 10% and 5% of total samples were characterized as moderate and high pollution levels, and 2% as very high pollution category. Spatial analysis using GIS revealed that 440.63 km were within safe fluoride levels according to the WHO standards, while 139.32 km were identified as risk zone. The principal component analysis (PCA1) showed strong positive loadings on EC (0.994), TDS (0.905), Mg (0.910), Cl (0.903) and HCO (0.923) indicating rock water interaction. PCA2 accounts the high positive factor loading on HCO (0.864) indicating ion exchange and mineral leaching. The PCA1 and PCA2 indicated that variables such as mineral leaching and rock water interaction are the major mechanisms contributing to the chemical signatures in groundwater, which may support for the elevated fluoride levels in certain areas. Risk assessments, including Hazard Quotient results showed that 71%, 61% 38%, and 34% of groundwater samples exceeded the permissible THI limit (THI > 1) for infants, children, teenagers, and adults, respectively. The study recommends implementing measures such as denitrification, defluorination, rainwater harvesting, and improved sanitation infrastructure to enhance the health conditions in the study region. Additionally, it suggests introducing educational programs in rural areas to create awareness about the health dangers due to consumption of water with high fluoride levels.
本研究旨在探讨印度南部锡瓦克西地区的地下水是否适合饮用,并评估不同年龄段(包括婴儿、儿童、青少年和成年人)可能面临的健康危害。共采集了 77 个地下水样本,覆盖了 580 平方公里的总面积,并对主要和次要离子进行了分析。样本的氢离子浓度(pH)呈中性至弱碱性。总溶解固体(TDS)波动范围为 255 至 2701mg/L,电导率变化范围为 364 至 3540µS/cm。检测到的氟化物浓度范围很广(0.1 至 3.2mg/L),近 38%的地下水样本超过了世界卫生组织(WHO)在 2017 年提出的建议限值(1.5mg/L)。Gibbs 图分析表明,大多数样本受地质因素影响,主要是该地区的岩石风化。相关分析表明,大多数样本受到自然和人为因素的共同影响。地下水污染指数(PIG)波动范围为 0.67 至 2.60,约 30%和 53%的样本分别属于无显著污染和低污染类别。此外,10%和 5%的总样本属于中等和高污染水平,2%属于极高污染水平。利用 GIS 进行空间分析显示,根据世卫组织标准,有 440.63 公里的区域处于安全氟化物水平,而有 139.32 公里的区域被确定为风险区域。主成分分析(PCA1)显示,EC(0.994)、TDS(0.905)、Mg(0.910)、Cl(0.903)和 HCO(0.923)的电导率呈强正负荷,表明存在岩石水相互作用。PCA2 显示 HCO(0.864)的高正因子负荷,表明存在离子交换和矿物浸出。PCA1 和 PCA2 表明,矿物浸出和岩石水相互作用等变量是导致地下水化学特征的主要机制,这可能是某些地区氟化物水平升高的原因。风险评估包括危害商数(HQ)结果表明,有 71%、61%、38%和 34%的地下水样本超过了婴儿、儿童、青少年和成年人可允许的 THI 限值(THI>1)。研究建议采取一些措施,如脱氮、脱氟、雨水收集和改善卫生基础设施,以改善研究区域的健康状况。此外,还建议在农村地区开展教育计划,提高人们对高氟水平饮用水健康危害的认识。