Abstract

Impacts of geogenic and anthropogenic sources change seriously quality of groundwater. Inferior groundwater quality directly affects the human health, agricultural output and industrial sector. The aim of the present study is to evaluate the groundwater quality for drinking purpose and also to identify the pollutants responsible for variation of chemical quality of groundwater, using pollution index of groundwater (PIG). Groundwater samples collected from a rural part of Telangana State, India, were analyzed for pH, total dissolved solids (TDS), calcium (Ca2+), magnesium (Mg2+), sodium (Na+), potassium (K+), bicarbonate ( {text{HCO}}_{3}^{ - } ), chloride ( {text{Cl}}^{ - } ), sulfate ( {text{SO}}_{4}^{2 - } ), nitrate ( {text{NO}}_{3}^{ - } ) and fluoride ( {text{F}}^{ - } ). The groundwater is characterized by Na+ and {text{HCO}}_{3}^{ - } ions. The values of TDS, Mg2+, Na+, K+, {text{HCO}}_{3}^{ - } , {text{Cl}}^{ - } , {text{SO}}_{4}^{2 - } , {text{NO}}_{3}^{ - } and {text{F}}^{ - } are more than their threshold limits prescribed for drinking purpose in a few groundwater samples. The computed values of PIG varied from 0.69 to 1.37, which classify the 80% of the present study area into the insignificant pollution zone (PIG: < 1.0) caused by geogenic origin associated with rock-weathering, mineral dissolution, ion exchange and evaporation processes, and the rest (20%) into the low pollution zone (PIG: 1.0 to 1.5) due to influence of anthropogenic source (waste waters and agricultural activities) on the groundwater system, which are proved by ANOVA test. The diagrams (Ca2+ + Mg2+) versus ( {text{HCO}}_{3}^{ - } + {text{SO}}_{4}^{2 - } ), Na+ versus (Ca2+ + Mg2+), Na+ versus {text{Cl}}^{ - } , Ca2+ versus {text{SO}}_{4}^{2 - } and Ca2+ versus Mg2+ support the geogenic origin, whereas the diagram TDS with ( {text{NO}}_{3}^{ - } + {text{Cl}}^{ - } )/ {text{HCO}}_{3}^{ - } confirms the impact of anthropogenic activities on the aquifer chemistry, which substantially proved the explanation of PIG. The characterization of geochemical evolution of groundwater, using trilinear diagram, also further supports the assessment of PIG in the variation of groundwater quality. From this study, the TDS, Mg2+, Na+, {text{Cl}}^{ - } , {text{SO}}_{4}^{2 - } and {text{NO}}_{3}^{ - } are considered as indicators in assessing the groundwater pollution sources.

Highlights

  • Groundwater is a natural replenishable and most precious resource

  • Subba Rao (2018) studied the groundwater quality from a part of Prakasam district, Andhra Pradesh, India, and the results showed that the groundwater chemistry is regulated by rock-weathering, ion exchange and evaporation processes and interference of human activities such as drainage wastes and agricultural chemicals

  • The lower total dissolved solids (TDS) may be a result of natural origin, while the higher TDS specifies the influence of anthropogenic source on aquifer system (Subba Rao 2017a)

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Summary

Introduction

Groundwater is a natural replenishable and most precious resource. In arid and semiarid countries like India, especially in rural regions, most population depends on the1 3 Vol.:(0123456789) 227 Page 2 of 13Applied Water Science (2018) 8:227Geochemical processes, occurring within the aquifer system and their chemical reactions, control the changes in groundwater chemistry, and the study of chemical variations in groundwater can be useful for identifying the hydrogeochemical factors that control the sources of ions in groundwater, which needs water treatment before application (Subba Rao et al 2012; Nagaraju et al 2018; Sun and Gui 2015; Selvam et al 2018).In recent time, the impacts of geogenic and anthropogenic activities on the aquifer system have been studied and assessed the groundwater quality and pollution for its sustainable development and protection: Kumar et al (2006) evaluated the hydrogeochemical processes like dissolution, mixing, weathering of carbonate minerals ­(CaCO3 concretions), ion exchange and surface water interaction that control the groundwater quality in Delhi, India. Barzegar et al (2016a, b, 2017a, b) assessed the hydrogeological, hydrogeochemical and water quality properties from different parts of Iran, and the results of Piper diagram and bivariate diagrams showed the hydrochemical processes such as weathering and dissolution of rocks, evaporation and ion exchange as the primary factors, while the anthropogenic activities as secondary factors that are responsible for variation of groundwater quality. Subba Rao (2018) studied the groundwater quality from a part of Prakasam district, Andhra Pradesh, India, and the results showed that the groundwater chemistry is regulated by rock-weathering, ion exchange and evaporation processes and interference of human activities such as drainage wastes and agricultural chemicals

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