地下水
氟化物
钾
碳酸氢盐
干旱
优势(遗传学)
氯化物
总溶解固体
环境科学
环境化学
水文学(农业)
环境工程
化学
地质学
无机化学
古生物学
岩土工程
生物化学
有机化学
基因
作者
Narsimha Adimalla,Ravi Manne,Yunhui Zhang,Panpan Xu,Hui Qian
标识
DOI:10.1080/10106049.2022.2040603
摘要
In the present study, the quality of groundwater for drinking purposes was evaluated. The following parameters were analyzed using American Public Health Association standard method: pH, total hardness (TH), total dissolved solids (TDS), electrical conductivity (EC), bicarbonate (HCO3−), chloride (Cl−), sulphate (SO42−), fluoride (F−), calcium (Ca2+), magnesium (Mg2+), sodium (Na+) and potassium (K+). These values were compared with limits recommended by the World Health Organization (WHO) and the Bureau of Indian Standards (BIS) for drinking purposes. The cation and anion dominance of the study region groundwater samples were Na+ > Ca2+ > Mg2+ > K+ and HCO3− > Cl− > SO42− > F−, respectively. Bicarbonate was the dominant anion and Na+ was identified as the dominant cation in the groundwater of the study region. The Na+ and Cl− concentration of 43% and 37% of groundwater samples were found to be more than the acceptable limit of WHO in the study region. Most of the groundwater samples in the study region were categorized as a very hard category. The groundwater was highly affected by the fluoride and about 60% of groundwater samples were unfit for drinking purposes in the study region.
科研通智能强力驱动
Strongly Powered by AbleSci AI