Assessing the Groundwater Quality and Hydrogeochemical Characteristics of Karst Aquifers in Kinta Valley, Perak

Abstract

The rich karstic limestone aquifer in Kinta Valley, Perak is a potential resource of clean water in the future when the surface water resources will deplete and insufficient to support the growing population. A proper preliminary evaluation of groundwater hydrogeochemistry is essential for knowing the proper application and maintaining the available groundwater as a sustainable resource. Four production wells in Kinta Valley are sampled and analyzed for physicochemical parameters from 2018 to 2020. In this study, major chemical compounds, pH, total hardness (TH), and total dissolved solids (TDS) are interpreted to construct Piper’s trilinear diagram and Gibbs plot which describe the hydrochemistry of the samples. Drinking Water Quality Standard from the Ministry of Health Malaysia (MOH) and the United States Environmental Protection Agency (US EPA) National Primary Drinking Water Regulation is used as guideline standards for water quality evaluation. Based on the results from this study, the quality of groundwater in Kinta Valley is healthy and has the potential to be used as drinking water besides using as irrigation water. The predominant hydrochemical reaction of the groundwater is found to be a bicarbonate-calcium-magnesium reaction, which shows the aquifers are in contact with the subsurface karst system as the main ions originated from the dissolution of carbonate bedrocks.