4.7 Article

Assessment of groundwater geochemistry for drinking and irrigation suitability in Jaunpur district of Uttar Pradesh using GIS-based statistical inference

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ENVIRONMENTAL SCIENCE AND POLLUTION RESEARCH
卷 30, 期 11, 页码 29407-29431

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SPRINGER HEIDELBERG
DOI: 10.1007/s11356-022-23959-w

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Groundwater; Irrigation; PCA; GIS; Kriging interpolation; Heavy metals

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The quality of groundwater in the Jaunpur district of Uttar Pradesh, which is the only source of water for drinking and irrigation, has been poorly studied. This study evaluated the groundwater's suitability for drinking and irrigation using various chemical parameters. The findings revealed that most of the groundwater samples had high levels of EC, TDS, and TH, indicating unsuitability for drinking and irrigation. The study suggests that the groundwater in the area should be treated before drinking. However, it is suitable for irrigation.
The quality of groundwater in the Jaunpur district of Uttar Pradesh is poorly studied despite the fact that it is the only supply of water for both drinking and irrigation and people use it without any pre-treatment. The evaluation of groundwater quality and suitability for drinking and irrigation is presented in this study. Groundwater samples were collected and analysed by standard neutralisation and atomic emission spectrophotometry for major anions (HCO3-, SO42-, Cl-, F-, NO3-), cations (Ca2+, Mg2+, Na+, K+), and heavy metals (Cd, Mn, Zn, Cu, and Pb). The geographic information system (GIS) and statistical inferences were utilised for the spatial mapping of the groundwater's parameters. The potential water abstraction (i.e. taking water from sources such as rivers, streams, canals, and underground) for irrigation was assessed using the sodium absorption ratio (SAR), permeability index (PI), residual sodium carbonate (RSC), and Na percentage. According to the findings, the majority of the samples had higher EC, TDS, and TH levels, indicating that they should be avoided for drinking and irrigation. The positive correlation coefficient between chemical variability shows that the water chemistry of the studied region is influenced by geochemical and biological causes. According to the USSL (United States Salinity Laboratory) diagram, most of the samples fall under the C2-S1 and C3-S1 moderate to high salt categories. Some groundwater samples were classified as C4-S3 class which is unfit for irrigation and drinking. This study suggests that the groundwater in the study area is unfit for drinking without treatment. However, the majority of the samples were suitable for irrigation.

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