Characterization, variations, fluxes, and sources of contaminants in coal mine water of Korba basin, Chhattisgarh, India

Author:

Patel Khageshwar Singh1ORCID,Pandey Piyush Kant1,Agarwal Chandresh2,Sahu Bharat Lal3,Sharma Sanjay Kumar4,Wysocka Irena5,Yurdakul Sema6,Varol Simge7,Martín‐Ramos Pablo8ORCID

Affiliation:

1. Department of Applied Sciences Amity University Raipur Chhattisgarh India

2. Cerafrik Dubai UAE

3. Department of Chemistry Guru Ghasidas University Koni, Bilaspur Chhattisgarh India

4. Department of Mechanical Engineering Amity University Raipur Chhattisgarh India

5. Polish Geological Institute Warsaw Poland

6. Environmental Engineering Department Suleyman Demirel University Isparta Turkey

7. Department of Geology Faculty of Engineering Suleyman Demirel University Çünür Isparta Turkey

8. Instituto de Investigación en Ciencias Ambientales de Aragón (IUCA) Universidad de Zaragoza, Escuela Politécnica Superior Huesca Spain

Abstract

AbstractSeveral million tons of coal are extracted which discharge the contaminated mineral water into the environment in the coal mines located in the Korba basin (Chhattisgarh, India) chosen as the study area. The aim of this work is to describe: (i) the physico‐chemical characteristics (pH, EC, TDS, DO, RP, CC (carbonate carbon), OC (organic carbon) F, Cl, NO3, SO42−, SiO44−, PO43−, Na+, K+, Mg2+, Ca2+, Al, As, Sb, Fe, Mn, Zn, Cd, Pb, and Hg) of the coal mine water samples, (ii) spatial, seasonal (i.e. PrM (pre‐monsoon), M (monsoon) and PtM (post monsoon) and temporal (over the period of 2012–2017) variations, (iii) sources of contaminants from fourteen coal mines, (iv) suitability of the water for drinking and other uses, and (v) health impact of the mine water in view of developing remedial approaches.The mine water is neutral in nature with high TDS (total dissolved solid) values ranging from 620 to 13711 mg L−1 due to mainly high carbon content. The concertation of all species lies between 519–11432 mg L−1 with maximum value of OC. The most dominating species were OC, CC, Cl, NO3, SO42−, Na, and Ca. Species, that is, F, OC, Al, Fe, As, Sb, Cd, Pb, and Hg occurred beyond their limits. Their higher concentration in the PtM is observed. Water quality index (WQI) values ranged from 17.52 to 95.68 in the PtM period. 42.85%, 21.42%, and 7.14% of water samples represent “excellent water”, “good water” and “poor water” respectively in the PtM period. In addition, the fertilizer and trace element concentrations in the water samples were compared with the limit values determined for usability as drinking water. Accordingly, it was concluded that it is not suitable for use as drinking water in terms of TDS, F, and NO3 concentrations. In addition, AsT (total arsenic), F and NO3 pollutants were detected in the water samples, and it was observed that F and NO3 ions did not have a carcinogenic effect. A health risk assessment of As has been made, and it is found that adults and children have a low risk of developing cancer from the exposure. However, arsenic has high non‐carcinogenic and potentially harmful effects.

Publisher

Wiley

Subject

Management, Monitoring, Policy and Law,Public Health, Environmental and Occupational Health,Pollution,Waste Management and Disposal

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