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Data on appraisal of groundwater quality in north-eastern Haryana

This dataset paper aimed to analyse the quality of groundwater of Yamunanagar and Ambala districts in North-Eastern Haryana, India rooted on the various analytical elements and hydro-chemical parameters. Also, Piper and Gibbs diagram were applied to observe hydro-chemical characteristics and control...

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Detalles Bibliográficos
Autores principales: Ravish, Sandeep, Setia, Baldev, Deswal, Surinder
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6700504/
https://www.ncbi.nlm.nih.gov/pubmed/31453276
http://dx.doi.org/10.1016/j.dib.2019.104164
Descripción
Sumario:This dataset paper aimed to analyse the quality of groundwater of Yamunanagar and Ambala districts in North-Eastern Haryana, India rooted on the various analytical elements and hydro-chemical parameters. Also, Piper and Gibbs diagram were applied to observe hydro-chemical characteristics and controlling constituents of the underground aqua region. The impendence of anions was noted to be tolerable in 93.33% of the spots while 86.67% groundwater samples were observed to be in the desirable limit for cations. The analytical constituents of TH, TA, TDS, and pH were reported to be tolerable in 76.66%, 80%, 60%, and 100% of the water-samples, respectively. Eight water-sampling spots manifested unacceptable ranges of one or more of the physico-chemical constituents. Seven spots were observed to be suffering from one constituent and therefore were classified to be falling in the ‘Grey-Zone’. One location (i.e. 23) has been found to be severely influenced by excess of TH, TA, TDS, SO(4)(2−), and Ca(2+) and is reported to be falling in the ‘Red-Zone’. The classification of groundwater based on Piper diagram depicted that pre-dominant type of sub-surface water hydro-chemical facies of area was ‘Ca– Mg– HCO(3)–Cl(’). Gibb's figure revealed that underground water pre-eminence distribution is probably resulted by water-rock dominance in sub-surface water.