In the study region of Peddapanjani revenue area, twenty-five groundwater samples have been gathered in dissimilar panchayats to inspect the groundwater quality for suitability of irrigation and drinking. It was evaluated by pH, EC, TDS, hardness, and alkalinity other than considerable cations (Na⁺, K⁺ Ca²⁺Mg²⁺) and anions (HCO₃⁻, Cl⁻, SO₄²⁻, F⁻). Based on the results obtained, sodium absorption ratio (SAR), sodium percent (Na%), permeability index (PI), residual sodium carbonate (RSC), Kelley’s ratio (KR), magnesium ratio (MR), and non-carbonate hardness (NCH) were calculated. The chemical elements generated rock-water interaction, i.e., indicate Gibbs plot diagram. The sulfate concentration was observed high due to extensive usage of fertilizers and pesticide in agriculture cultivation. Sixty percent of area is magnesium elevated due to the presence of ferro magnesium minerals (silicate group of minerals, olivine, amphiboles, and pyroxenes). The USSL diagram indicates no alkalinity hazard in focused region, and Wilcox suggests that groundwater of that particular province is good to permissible category. Factor analysis and cluster analysis were performed of water chemistry.

在 Peddapanjani 收入区的研究区域，在不同的 panchayats 收集了 25 个地下水样本，以检查地下水质量是否适合灌溉和饮用。除了相当多的阳离子（Na ⁺、K ⁺ Ca ²⁺ Mg ²⁺）和阴离子（HCO ₃ ^-、Cl ^-、SO ₄ ^2-、F ^-）。根据所得结果，钠吸收率 (SAR)、钠百分比 (Na%)、渗透指数 (PI)、残留碳酸钠 (RSC)、凯利比 (KR)、镁比 (MR) 和非碳酸盐硬度(NCH) 进行计算。化学元素产生岩水相互作用，即表示吉布斯图。由于在农业种植中大量使用化肥和杀虫剂，观察到硫酸盐浓度很高。由于铁镁矿物（硅酸盐矿物、橄榄石、角闪石和辉石）的存在，60% 的区域镁含量升高。USSL 图表表明重点区域没有碱度危害，Wilcox 表明该特定省份的地下水符合允许类别。对水化学进行因子分析和聚类分析。