2010
DOI: 10.1007/s10230-010-0108-2
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Quality Assessment of Mine Water in the Raniganj Coalfield Area, India

Abstract: In a qualitative assessment of mine water from the Raniganj coalfield, 77 mine water samples were analyzed to assess water quality and suitability for domestic, industrial, and irrigation uses. The pH of the mine water ranged from 6.5 to 8.8. Total dissolved solids (TDS) ranged from 171 to 1,626 mg L -1 ; spatial differences between the TDS values reflect variations in lithology, activities, and prevailing hydrological regime. The anion chemistry was dominated by HCO 3 -and SO 4 2-. On average, Cl -contributes… Show more

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Cited by 112 publications
(52 citation statements)
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“…The RCF also contains large reserves of iron ore occurring chiefly as nodules along with good quality fire clay in the Barakar stage of RCF (Sikdari et al 2004). The high demand for coal from this area has ensued in intensive mining activities and expansion of the lease hold areas, along with the piling up of vast areas of overburden material and tailings, thus resulted in significant long-term environment hazards in the form of acid mine drainage and contamination of local water resources with toxic trace metals (Singh and Singh 2010;Banerjee 2011;Singh et al 2012). …”
Section: Methodsmentioning
confidence: 99%
“…The RCF also contains large reserves of iron ore occurring chiefly as nodules along with good quality fire clay in the Barakar stage of RCF (Sikdari et al 2004). The high demand for coal from this area has ensued in intensive mining activities and expansion of the lease hold areas, along with the piling up of vast areas of overburden material and tailings, thus resulted in significant long-term environment hazards in the form of acid mine drainage and contamination of local water resources with toxic trace metals (Singh and Singh 2010;Banerjee 2011;Singh et al 2012). …”
Section: Methodsmentioning
confidence: 99%
“…On the basis of this limit, all water samples under investigation area were not problematic for , respectively with the mean value of 9.03 mg L -1 (Table 3) and it contributed 3% to the total anionic mass balance (Figure 2a). On a global basis, one third of the SO 4 in aquatic systems derived from rock weathering (include two major forms of sulphur sedimentary rocks, pyrite and gypsum), about 60% from fossil fuel combustion and minor amounts from volcanism (5%) and cycling salts (2%) (Berner and Berner, 1987;Singh et al, 2010). According to Ayers and Westcot (1985), the acceptable limit of SO 4 in irrigation water is less than 20 mg L -1…”
Section: Quality On the Basis Of Anionic Constituentsmentioning
confidence: 99%
“…As per this limit, all samples were not troublesome for irrigating soils and crops grown in the investigated area. On a global basis, one third of the SO 4 in aquatic systems derived from rock weathering (include two major forms of sulphur sedimentary rocks, pyrite and gypsum), about 60% from fossil fuel combustion and minor amounts from volcanism (5%) and cycling salts (2%) [28][29] . On the other hand, trace amount of phosphate was detected in most of the groundwater samples ( (Table 3).…”
Section: Groundwater Quality On the Basis Of Physicochemical Propertiesmentioning
confidence: 99%
“…While high salinity (high EC) in water leads to formation of saline soil, a high sodium concentration changes soil properties and reduce soil permeability, which leads to development of an alkaline soil 29 . The computed sodium adsorption ratio of groundwater samples was within the limit of 0.99 to 6.93 with a mean value of 1.86 (Table 4).…”
Section: Sodium Adsorption Ratio (Sar)mentioning
confidence: 99%