Assessment and Characterization of Groundwater Quality of Malabar Coast in Kerala, India
P. S. Sheeja, D. K. Singh, A. Sarangi, Vinay Sehgal, M. A. Iquebal
International Journal of Environment and Climate Change · pp. 1399–1413 · Published 18 Jul 2023
10.9734/ijecc/2023/v13i92370Abstract
A study was conducted to assess and characterize the groundwater quality of coastal aquifer of the Vatakara-Koyilandy stretch in the Kozhikode district of Kerala. Mann-Kendall Test was used for analysing the trend in groundwater levels. The Piper diagram was applied to determine the chemical facies of the groundwater and identify the evolution of hydrochemical parameters of groundwater sources. The source of the dissolved ions in the groundwater was described by the Gibbs diagram. The suitability of groundwater for irrigation was determined using the United States Salinity Laboratory diagram. Geostatistical tools were used to describe the spatial variability of groundwater levels and salinity and the ordinary kriging method was used to plot the spatial variability maps. It was found that Na+ was the predominant cation with maximum concentration varying from 455.6 mg/l to 1844 mg/l during pre-monsoon and post-monsoon; respectively. Concentration of Cl- in pre-monsoon and post-monsoon varied from 184 mg/l to 2417 mg/l and 99 mg/l to 714 mg/l; respectively. Other anions in the groundwater were SO42- and HCO3- with an average concentration of 239.79 mg/l and 129.59 mg/l in pre-monsoon and 110.73 mg/l and 75 mg/l in post-monsoon; respectively. The trend in groundwater in confined and semi-confined aquifers showed negative trends whereas eight wells resulted in a significantly negative trend. However, a significant decreasing trend was observed in wells near the coasts. The most dominant cations were (Na+, and K+) and the dominant anions were SO42- and Cl-. The dominant cations and anions were from the mixing of seawater with the groundwater. The Na+ ions were also found to be from the same source. In most of the area, the groundwater was highly to very high highly saline with medium sodium and not suitable for irrigation. In the unconfined aquifer, 25.2% and, in the semi-confined aquifer 24.0% area was found to be unfit for irrigation.
Cited by 2
Abu Reza Md Towfiqul Islam, Md. Abdullah-Al Mamun, Mehedi Hasan · Journal of Contaminant Hydrology · 2025
Asit Kumar Dandapat, Prafulla Kumar Panda, Sovan Sankalp · Discover Sustainability · 2024
Related research
- Aerobic Biodegradation of Petroleum Hydrocarbons in Laboratory Contaminated Groundwater — shares topic coverage
- Impact of Extreme Floods on Groundwater Quality (in Pakistan) — shares topic coverage
- Simulating the Impact of Drought on California’s Central Valley Hydrology, Groundwater and Cropping — shares topic coverage
- Watershed Modeling of Surface Water-Groundwater Interaction under Projected Climate Change and Water Management in the Haihe River Basin, China — shares topic coverage
- Efficacy of Fuzzy c-Means Cluster Analysis of Naturally Occurring Radioisotope Datasets for Improved Groundwater Resource Management under the Continued Risk of Climate Change — shares topic coverage
Article metrics
Real usage data collected on this platform.
1
Page views
0
PDF downloads
0
Outbound clicks
2
Citations
Views over time
Views by country
Approximate, from request IP at view time — not citizenship or institution. Countries with fewer than 5 views are grouped as "Other".
Traffic sources
Referring site, by host.
Views and downloads exclude known bots/crawlers. Citations combines this platform's own DOI-resolved index with each external source's own reported total — see Cited by above for individually listed citing works. Last refreshed 0 seconds ago.