Exposure of Fluoride in Coal Basin

International Journal of Clean Coal and Energy, 2016, 5, 1-12 Published Online February 2016 in SciRes. http://www.scirp.org/journal/ijcce http://dx.doi.org/10.4236/ijcce.2016.51001 Exposure of Fluoride in Coal Basin Khageshwar Singh Patel1*, Ankit Yadav1, Keshaw Prakash Rajhans1, Shobhana Ramteke1, Reetu Sharma1, Irena Wysocka2, Irena Jaron2 1 2 School of Studies in Chemistry/Environmental Science, Pt. Ravishankar Shukla University, Raipur, India Polish Geological Institute, Rakowiecka, Warsaw, Poland Received 12 November 2015; accepted 16 February 2016; published 19 February 2016 Copyright © 2016 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract Coal is a dirty fuel contaminated with F− and other elements. Several million tons of coal are burnt in Korba basin, central India to generate electricity with pouring fluorine and other elements into the environment. The water is contaminated with F− and other chemicals beyond the permissible limits. The contaminated water is consumed by the human and animals by excreting the balanced toxicants through the stool and urine. Several folds higher concentration of F− in urine (44 mg/L) and stool (266 mg/kg) samples of the cattle are observed. The prevalence of fluorosis diseases in cattle of the Korba basin is reported. Keywords Coal, Fluoride, Contamination, Toxicity 1. Introduction Coal is a dirty fuel contaminated with toxic elements at the traces [1] [2]. The fluoride content in the coals is ranged from 20 - 500 mg/kg [3]. The environments in coal burning areas were severely contaminated with F− and other toxicants [4]-[9]. The human and other animals living in the coal burning areas were affected by chronic endemic fluorosis diseases due to the excessive intake of F− from air, water and food [10]-[12]. Several states of the country are suffered with fluorosis diseases due to intake of contaminated groundwater [13]-[20]. In the present work, the contamination of ground and surface water of the largest coal basin of India with F− and other elements is described. The exposure assessment of the F− toxicity in the domestic animals is described. * Corresponding author. How to cite this paper: Patel, K.S., Yadav, A., Rajhans, K.P., Ramteke, S., Sharma, R., Wysocka, I. and Jaron, I. (2016) Exposure of Fluoride in Coal Basin. International Journal of Clean Coal and Energy, 5, 1-12. http://dx.doi.org/10.4236/ijcce.2016.51001 K. S. Patel et al. 2. Materials and Methods 2.1. Study Area Korba basin, CG, India (22˚21'0"N and 82˚40'48"E) has rich deposit of coal over ≈ 1.0 × 104 km2 area. It is a power capital of Chhattisgarh state, India. The basin is composed of four blocks: Kartala, Katghora, Korba and Pali with population of ≈ 1 million distributed over 710 cities, towns and villages. A huge amount of coal > 10000 MT/Yr has been consumed by various units of thermal power plants for generation of ≈ 40000 KW electricity. At least 12 open and underground coal mines are in operation with annual production of ≈3 BT coal by discharging > 100 BT/Yr liquid effluents in the environment. In addition, the Asia biggest Aluminum Plant (BALCO) is running in the Korba basin. 2.2. Sample Collection The main river flowing through Korba basin is the Hasdeo River. The Bango dam has been constructed across this river through which water flows into canals. Several pit lakes are found to exist in the Korba basin due to mining out of the coal. The ground and surface water samples were collected from 30 and 6 locations of the basin in month of January, 2013 [21] (Figure 1). A 1-L cleaned narrow mouth polyethylene bottle was used for the collection. The container was rinsed three times with the sample water and filled with the water up to the mouth. The physical parameters i.e. temperature (T), pH, dissolved oxygen (DO), reduction potential (RP) and electrical conductivity (EC) of the water were measured at the spot by using HANNA sensors. The first morning stool (1 kg) of the domestic animals (n = 20) was collected manually. The stool sample was stored in the polyethylene bottle and dried in oven at 60˚C till the dryness. They were crushed and sieved out the particles of mesh sizes ≤0.1 mm. A 5.0 g stool sample was extracted out with 25 mL hot deionized water (50˚C) for 6 hr to measure the F− and pH values. The first morning urine sample (100 mL) was collected in a plastic bottle containing 0.2 g EDTA. Total 20 (4 × 5) urine samples of domestic animals (i.e. cattle, buffalo, sheep and goat) were collected in January, 2013. The samples was shipped to the laboratory in insulated container at about 4˚C and stored at −20˚C until use. 2.3. Analysis The Metrohm ion meter-781 was used for the measurement of F− by using TISAB-III buffer in 1:1 ratio. The Figure 1. Representation of sampling locations in Korba basin. 2 K. S. Patel et al. buffer was prepared by dissolving 300 g sodium citrate, 22 g 1,2-cyclohexanediamine-N,N,N,N-tetraaceticacid and 60 g NaCl in a volume of 1-L with the de-ionized water with subsequent adjustment of pH value to 5.0 5.5). The Dionex ion chromatography-1100 was used for monitoring of ions i.e. Cl−, NO3− , SO 24 − , Na+, K+, Mg2+ and Ca2+. The Thermos ICP-OES and ICP-MS (Polish Geological Institute, NRI, Central Chemical Laboratory, Warsaw) were employed for analysis of the elements. 3. Results and Discussion 3.1. Geology and Hydrology The rock of the studied area was formed in the Archaean to Cenozoic ages. They consist of granite gneiss and granitoids covering with medium to coarse grained arkosic sandstone, a few pebble beds, conglomerate and shale of coal. The ground water occurs under phreatic, semi-confined and con-fined conditions control of the inter granular pore spaces in the shallow weathered zones and joints, fractures and caverns in deeper horizons. The water level depth is varied from 3.4 - 11.6 mbgl (meter below ground level) during the post-monsoon period in the aquifers. 3.2. Physico-Chemical Characteristics of Groundwater The physico-chemical parameters of the groundwater are presented in Tables 1-3. The age and depth of 30 tube wells was ranged from 4.0 - 130 Yr and 4 - 18 m with mean value of 7 ± 1 Yr and 11 ± 1 m, respectively. A slight variation in temperature of the groundwater was recorded, ranging from 29.5 - 31.2˚C with mean value of 30.6 ± 0.1˚C. The pH value of the water was varied from 5.9 - 8.2 with mean value of 7.1 ± 0.2. The groundwater was found to be acidic in few locations (i.e. Surabahar, Sutara, Turali, Lalmatiya, Jenara, Dhelawdih, Banki Mongara, Dipka, Kusmunda, Bhilai, Hardibazar and Rumgara) due to the existence of higher content of the acids. The EC,TDS, DO and RP value of the groundwater was varied from 296 - 964 μS/cm, 414 - 990 mg/L, 5.6 6.7 mg/L and 199 - 241 mV with mean value of 497 ± 56 μS/cm, 628 ± 61 mg/L, 6.0 ± 0.1 mg/L and 218 ± 5 mV, respectively. The value of DO, EC and TDS was found moderately higher to the recommended value of 4.0 mg/L, 300 μS/cm and 500 mg/L, respectively [22] [23]. However, the RP value was observed to be at least 3-times less than the recommended value of 600 mV. The concentration of F −, Cl−, NO3− , SO 24 − , Na+, K+, Mg2+, Ca2+, Al, SiO2, Fe, Mn and Zn was ranged from 2.1 - 12, 11 - 92, 10 - 90, 10 - 72, 10 - 70, 0.6 - 8.7, 3.0 - 44, 8.0 - 78, 7.2 - 45, 9.0 - 70, 0.4 - 8.2, 0.2 - 1.5 and 1.0 - 2.4 mg/L with mean value of 5.5 ± 0.9, 34 ± 7, 28 ± 7, 21 ± 5, 24 ± 6, 3.7 ± 0.8, 11 ± 3, 31 ± 6, 16 ± 3, 31 ± 6, 2.2 ± 0.6, 0.5 ± 0.1 and 1.5 ± 0.1 mg/L, respectively. Similarly, concentration of other metals: Li, Be, Rb, Co, Ni, Cu, Sn, Sb, Mo, Cd, La, Ce, Pb and U was observed in microgram levels, ranging from 4.7 - 36, 1.1 - 6.7, 1.4 - 38, 1.1 - 7.7, 2.4 - 27, 2.3 - 22, 1.2 - 11, 0.9 - 9.8, 0.1 - 5.0, 0.11 - 0.33, 0.1 - 2.1, 0.1 - 0.8, 1.1 - 29 and 1.0 -12 µg/L with mean value of 16 ± 3, 2.1 ± 0.5, 16 ± 5, 3.3 ± 0.8, 9.2 ± 2.4, 8.0 ± 2.1, 3.0 ± 1.0, 3.2 ± 0.8, 1.0 ± 0.4, 0.19 ± 0.02, 0.4 ± 0.2, 0.4 ± 0.1, 7.0 ± 2.4 and 2.5 ± 1.0 µg/L, respectively. Among them, the highest content of Cl− was observed, may be due to leaching from the coal. The occurrence trend of 27 elements in the water was found in following decreasing order: Cl− > Ca ≈ SiO2 < NO3− < Na+ > SO 24 − > Al > Mg > K+ > F− > Fe > Zn > Mn >> Li ≈ Rb > Ni > Cu > Pb > Sb ≈ Co > Sn > U > Be < Mo > La ≈ Ce > Cd. The concentration of F− in the groundwater of the studied area was found to be comparable to F− contents reported in the water of other locations of the country [5]-[18]. Factor analysis was used for 17 variables of the water. Four factors were extracted which explain 83.27% of the total variance. A 58.49% of the total variance was explained by Factor-1, showing strong positive loadings on EC, TDS, F−, Cl−, SO 24 − , Na+, Mg2+, Fe, Mn, Zn, Be, Rb, Co, Ni, Cu, Cd, Pb, La, Ce and Ca2+. They were related to the mineralization of the groundwater which involved also weathering of gypsum and fluoride bearing minerals such as CaF2. They were correlated well in the water as shown in Table 4, Table 5. A 10.93% of the total variance was accounted by factor-2, pyrite with strong positive loadings on NO3− and K+, related to coal burning and mining activities. A 7.78% of the total variance was explained by factor-3, describing a strong loading on SiO2. A 6.06% of total variance was explained by factor-4 related to the age factor of tube wells. 3.3. Physico-Chemical Characteristics of Surface Water The physico-chemical characteristic of the surface water is shown in Tables 6-8. The value of T, pH, DO, RP, 3 K. S. Patel et al. Table 1. Physical characteristics of groundwater in Korba basin, January 2013. S. No. Location pH EC, µS/cm TDS, mg/L DO, mg/L RP, mV 1 Pauli 7.4 296 745 5.9 199 2 Surabahar 6.6 527 627 5.8 228 3 Sutara 5.9 398 563 5.8 241 4 Katghora 7.8 388 509 5.9 202 5 Konkona 7.3 514 589 5.7 221 6 Turali 6.6 964 813 6.2 230 7 Lalmatiya 6.4 312 588 6.1 237 8 Jenara 6.8 464 574 5.6 199 9 Lakhanpur 7.1 633 611 5.8 215 10 Dhelawdih 6.7 515 628 6.1 212 11 Churri 7.2 629 738 6.7 201 12 Gopalpur 7.7 519 922 5.9 241 13 Darri 7.2 523 650 5.8 202 14 Banki Mongara 6.8 634 722 5.8 221 15 Dipka 6.9 511 441 5.9 230 16 Ghordeva 7.2 534 487 5.7 199 17 Balgi 7.0 713 933 6.2 228 18 Kuchana 7.3 391 633 6.1 241 19 Kusmunda 6.7 704 926 5.6 202 20 Bhilai 6.8 362 455 5.8 221 21 Dadar 7.0 322 464 6.1 230 22 Hardibazar 6.9 367 434 6.7 237 23 NTPC 7.4 380 471 5.7 199 24 Barpali 7.6 342 414 6.1 215 25 Manikpur 7.2 650 821 6.2 212 26 Korba 7.3 756 990 6.1 201 27 Balco 7.1 410 497 5.6 221 28 Rumgara 6.9 390 449 5.8 230 29 Urga 8.2 418 680 6.1 237 30 Bilaikhund 7.8 347 462 6.3 199 4 K. S. Patel et al. Table 2. Concentration of major elements in groundwater during January 2013, mg/L. S. No. F− Cl− NO3− SO 24− Na+ K+ Mg2+ Ca2+ Al SiO2 Fe Mn Zn 1 2.8 32 28 14 11 6 16 52 17 64 3.7 0.51 1.4 2 4.5 18 11 12 17 2 12 36 15 11 1.2 0.31 2.4 3 3.7 39 17 12 12 5 6 18 14 23 2.0 0.55 2.2 4 5.8 53 14 15 14 2 7 22 15 19 1.1 0.33 1.3 5 10 39 35 14 22 2 9 30 9.1 23 1.0 0.17 2.0 6 4.6 92 23 72 17 5 6 17 10 18 4.1 0.69 1.6 7 3.5 32 21 24 23 6 16 51 7.2 9 1.1 0.38 1.7 8 3.8 39 21 44 17 2 8 22 18 12 2.8 0.68 1.2 9 3.8 39 30 22 28 2 9 24 16 26 1.1 0.93 2.0 10 4.5 50 31 10 16 3 11 36 11 35 0.4 0.22 1.3 11 6.0 67 31 26 18 3 11 36 11 35 0.4 0.22 1.3 12 4.8 39 25 30 24 1.6 22 66 19 70 4.2 0.48 1.2 13 3.6 11 10 13 18 1.3 5 22 17 12 1.4 0.29 2.0 14 8.4 39 15 16 60 2.7 18 36 16 25 2.3 0.52 1.8 15 11 18 13 10 16 1.5 5 32 17 21 1.2 0.31 1.1 16 4.6 28 31 15 10 5.9 8 22 10 25 1.1 0.16 1.7 17 5.8 67 90 40 38 3.3 14 48 45 20 4.7 0.65 1.3 18 3.7 11 19 13 15 4.8 6 18 7.5 10 1.2 0.36 1.4 19 7.9 43 19 20 53 1.3 26 78 21 68 3.2 0.64 1.0 20 6.2 14 27 14 18 8.5 3 10 18 29 1.3 0.88 1.7 21 2.9 14 28 14 17 3.9 4 18 12 39 0.5 0.21 1.1 22 2.9 14 28 14 17 3.9 4 8 12 39 0.5 0.21 1.1 23 2.1 21 13 16 10 1.7 8 10 30 42 1.4 0.35 1.3 24 3.5 14 15 12 14 3.3 4 14 26 29 1.7 0.35 1.1 25 12 38 83 50 65 3.9 44 60 18 55 8.2 1.53 1.8 26 7.3 70 78 40 58 3.9 16 50 11 58 5.9 0.86 1.2 27 7.7 28 31 15 10 5.9 8 22 10 25 1.3 0.16 1.7 28 3.5 14 18 16 11 6.7 6 24 7.6 40 1.7 0.27 1.0 29 9.2 18 17 10 70 0.6 12 36 27 23 1.8 0.32 1.8 30 3.9 18 19 15 10 8.7 5 16 24 31 2.1 0.35 1.0 5 K. S. Patel et al. Table 3. Concentration of trace elements in groundwater during January 2013, µg/mL. S. No. Li Be Rb Co Ni Cu Sn Sb Mo Cd La Ce Pb U 1 18 2.4 3.8 1.9 7.4 6.5 1.6 2.3 0.66 0.25 0.24 0.51 4.7 2.8 2 20 2.4 37 2.9 13.3 4.8 3.4 4.7 1.76 0.13 0.22 0.23 2.7 1.6 3 18 2.5 3.2 2.2 10.6 3.0 2.7 3.4 2.08 0.22 0.15 0.20 1.2 1.4 4 17 1.5 4.9 1.7 5.1 8.6 1.7 2.8 2.05 0.14 0.52 0.71 5.6 1.4 5 12 1.5 25.5 5.0 3.9 8.8 2.0 6.0 0.28 0.17 0.27 0.08 9.0 1.3 6 11 1.5 8.3 4.2 10.0 4.1 2.6 4.6 2.10 0.13 0.24 0.31 1.9 1.6 7 9 1.5 21.1 3.0 9.8 4.7 2.2 3.3 1.11 0.20 0.56 0.67 7.3 1.6 8 19 1.8 2.2 1.4 2.9 2.9 1.5 1.0 0.65 0.19 0.20 0.13 4.3 3.8 9 36 2.2 33 7.6 11.4 6.0 2.9 9.8 1.20 0.20 0.41 0.70 3.6 1.4 10 11 5.2 38 7.7 26.6 18 11 1.7 0.06 0.33 2.11 0.80 9.6 1.6 11 11 5.2 28 7.7 23.8 18 10 1.9 0.08 0.33 1.11 0.60 9.1 1.6 12 16 1.7 3.4 1.6 6.1 5.1 1.3 2.1 0.56 0.21 0.19 0.44 4.3 2.1 13 18 1.7 34 2.4 11 3.8 2.8 4.2 1.49 0.11 0.17 0.2 2.5 1.2 14 16 1.8 2.9 1.8 8.8 2.4 2.2 3.1 1.76 0.19 0.12 0.17 1.1 1.1 15 15 1.1 4.4 1.4 4.2 6.8 1.4 2.5 1.74 0.12 0.41 0.61 5.1 1.1 16 11 1.1 23 4.2 3.2 6.9 1.6 5.4 0.24 0.14 0.21 0.07 8.3 1.0 17 10 1.1 7.5 3.5 8.3 3.2 2.1 4.1 1.78 0.11 0.19 0.27 1.7 1.2 18 8.6 1.1 19 2.5 8.1 3.7 1.8 3.0 0.94 0.17 0.44 0.58 6.7 1.2 19 17 1.3 2 1.2 2.4 2.3 1.2 0.9 0.55 0.16 0.16 0.11 3.9 2.9 20 33 1.6 30 6.3 9.4 4.7 2.4 8.8 1.02 0.17 0.32 0.61 3.3 1.1 21 10 3.7 35 6.4 22 14 9.1 1.5 0.05 0.28 1.66 0.69 27 1.2 22 10 3.7 35 6.4 23 14 9.1 1.5 0.05 0.28 1.66 0.69 29 1.2 23 29 1.9 1.4 1.2 2.4 2.3 1.6 1.1 0.87 0.19 0.14 0.22 2.6 10 24 13 1.5 28 1.9 7.7 18 1.7 1.2 0.24 0.25 0.19 0.31 20 1.1 25 21 1.3 1.5 1.6 5.5 9.0 1.8 1.1 0.55 0.17 0.11 0.17 4.9 4.1 26 25 6.7 13 1.3 2.7 5.7 1.7 1.2 4.95 0.11 0.12 0.23 5.2 9.0 27 6.1 1.1 23 4.2 3.2 6.9 1.6 5.4 0.24 0.19 0.21 0.27 8.3 1.0 28 4.7 1.1 1.5 2.9 10 22 2.4 3.2 1.23 0.16 0.14 0.25 6.8 12 29 20 1.2 7.3 1.1 7.3 21 1.2 1.2 0.22 0.31 0.31 0.58 8.4 1.2 30 9.2 1.1 1.4 1.1 5.4 3.8 1.5 1.9 0.55 0.16 0.13 0.19 1.5 1.2 6 K. S. Patel et al. Table 4. Correlation matrix of elements in groundwater. F− F− NO3− SO 24− Na+ 0.18 1 − 3 0.36 0.47 1 2− 4 0.13 0.72 0.52 1 0.64 0.24 0.46 0.28 1 NO K+ Mg2+ + Na −0.26 −0.12 0.09 0.01 −0.36 1 2+ 0.51 0.27 0.52 0.39 0.68 −0.20 1 2+ 0.42 0.34 0.40 0.25 0.59 −0.28 0.83 + K Mg Ca2+ Al SiO2 Fe Mn Zn 1 Cl− SO Cl− Ca 1 Al 0.04 0.01 0.26 0.07 0.26 −0.25 0.13 0.13 1 SiO2 0.10 0.12 0.30 0.10 0.29 −0.01 0.54 0.56 0.09 1 Fe 0.37 0.44 0.69 0.70 0.57 0.01 0.74 0.58 0.29 0.48 1 Mn 0.32 0.32 0.56 0.61 0.54 0.05 0.63 0.35 0.21 0.29 0.78 1 Zn 0.16 −0.02 −0.06 −0.06 0.12 −0.10 0.09 −0.06 −0.16 −0.44 −0.05 0.14 Mo Cd La Ce 1 Table 5. Correlation matrix of trace elements in groundwater. Li Be Rb Co Ni Cu Sn Sb Pb Li 1 Be 0.11 1 Rb 0.00 0.38 1 Co −0.04 0.42 0.75 1 Ni −0.22 0.57 0.63 0.74 1 Cu −0.31 0.28 0.29 0.35 0.51 1 Sn −0.24 0.68 0.61 0.76 0.95 0.51 1 Sb 0.32 −0.25 0.39 0.48 −0.05 −0.25 −0.15 1 Mo 0.30 0.27 −0.25 −0.33 −0.29 −0.39 −0.32 0.07 1 Cd −0.12 0.41 0.30 0.44 0.65 0.64 0.66 −0.31 −0.60 1 La −0.26 0.58 0.58 0.69 0.86 0.50 0.93 −0.19 −0.37 0.67 1 Ce 0.04 0.30 0.39 0.49 0.59 0.39 0.53 0.05 −0.17 0.52 0.69 Pb −0.34 0.31 0.51 0.41 0.52 0.59 0.59 −0.27 −0.44 0.55 0.67 0.40 1 U 0.16 0.18 −0.38 −0.29 −0.24 0.12 −0.16 −0.28 0.34 −0.18 −0.23 −0.28 −0.15 U 1 1 Table 6. Physical parameter of surface water during January 2013. S. No. Location pH EC, µS/cm TDS, mg/L DO, mg/L RP, mV 1 Churri 6.7 220 430 7.8 182 2 Rumgara 7.2 331 409 6.7 202 3 Kusmunda 7.5 493 413 5.8 210 4 Balco 7.3 172 391 5.9 208 5 Manikpur 7.4 210 494 8.1 176 6 Krishi Nagar 6.8 304 437 7.8 182 7 K. S. Patel et al. Table 7. Chemical parameter of surface water during January 2013. S. No. F− Cl− NO3− SO 24− Na+ K+ Mg2+ Ca2+ Al SiO2 Fe Mn Zn 1 2.3 21 38 20 11 8.3 8.1 20 1.0 7.7 0.9 0.4 0.28 2 1.8 11 17 10 46 15 5.2 16 1.2 7.7 0.4 0.4 0.39 3 2.4 14 13 16 47 13 6.0 16 1.3 3.1 0.6 0.3 0.45 4 2.2 18 17 30 16 7.1 5.1 18 1.4 9.2 1.3 0.7 0.29 5 3.1 27 25 40 20 6.0 6.2 20 1.6 7.7 1.4 1.1 0.31 6 2.6 14 30 20 18 9.2 9.1 28 1.3 6.1 1.5 1.2 0.42 Table 8. Concentration of trace elements in surface water during January 2013. S. No. Li Rb Cr Co Ni Cu Sb Pb U 1 16 13 5.1 2.7 5.2 6.6 3.8 7.4 0.92 2 22 25 4.2 3.2 5.8 9.6 3.4 6.3 0.74 3 23 18 4.6 3.9 4.8 7.5 3.4 5.7 0.89 4 15 19 4.4 4.2 6.4 7.9 4.4 6.2 0.97 5 14 14 4.8 2.5 4.0 6.4 2.4 4.5 0.68 6 18 16 8.1 5.9 7.9 14 1.4 2.8 0.32 EC and TDS of water (n = 6) in the post monsoon period was ranged from 20.8˚C - 22.2˚C, 6.7 - 7.5, 5.8 - 8.1 mg/L, 176 - 210 mV, 172 - 493 µS/cm and 391 - 494 mg/L with mean value of 21.6˚C ± 0.4˚C, 7.3 ± 0.3, 7.0 ± 0.8 mg/L, 193 ± 12 mV, 429 ± 29 µS/cm and 429 ± 29 mg/L, respectively. The concentration of F−, Cl−, NO3− , SO 24 − , Na+, K+, Mg2+, Ca2+, Al, SiO2, Fe, Mn and Zn was ranged from 1.8 - 3.1, 11 - 27, 13 - 38, 10 - 40, 11 - 47, 6.0 - 15, 5.0 - 9.0, 16 - 28, 3.1 - 9.2, 0.06 - 0.26, 0.4 - 1.5, 0.3 - 1.2 and 0.3 - 0.5 mg/L with mean value of 2.4 ± 0.3, 18 ± 4.7, 23 ± 8, 23 ± 9, 26 ± 13, 10 ± 3, 6.5 ± 1.3, 20 ± 4, 1.3 ± 0.2, 6.9 ± 1.7, 1.0 ± 0.4, 0.7 ± 0.3 and 0.4 ± 0.1 mg/L, respectively. Similarly, concentration of other metals: Li, Rb, Cr, Co, Ni, Cu, Sb, Pb and U was observed at microgram levels, ranging from 14 - 23, 13 - 25, 4.2 - 8.1, 2.5 - 5.9, 4.0 - 7.9, 6.4 - 14, 1.4 - 4.4, 2.8 7.4 and 0.3 - 1.0 µg/L with mean value of 18 ± 3, 18 ± 4, 5.2 ± 1.2, 3.7 ± 0.9, 5.7 ± 1.1, 8.7 ± 2.3, 3.1 ± 0.9, 5.5 ± 1.3 and 0.8 ± 0.2 µg/L, respectively. They were found to occur in following decreasing order: NO3− > Ca > Na+ > Cl− > SO 24 − > K+ > Mg > F− > Al > Fe > Mn > Zn > Li > Rb > Cu > Pb > Ni > Cr > Co > Sb > U. The concentration of F− in the surface water of the studied basin was found to be higher than other locations of the country [19] [20]. The factor analysis was applied and four factors were extracted. Factor-1 was accounted for 48.70% of the total variance, related to anions, Ca2+ and Mg2+. It could be correlated to complex processes such as weathering of fluoride bearing minerals (AlF3, CaF2, MgF2), gypsum, carbonate minerals and anthropogenic activities i.e. coal burning and leaching, aluminum plant effluents, etc. Factor-2 was accounted for 22.15% of the total variance, related to EC, TDS and Na+ which determined the mineralization of pond water. Factor-3 was accounted for 16.23% of the total variance having strong loadings of Fe and Mn, related to the speciation of Fe and Mn in the water. Factor-4 was accounted for 9.23% of the total variance, negatively loaded with the pH values. This factor was in the inverse relationship with the other factors. 3.4. Water Quality The concentration of F−, Al, Mn and Fe was found to be several folds higher than recommended value of 1.0, 0.03, 0.10 and 0.30 mg/L, respectively. The higher values of EC, TDS, RP, F−, Cl−, NO3− , Mg2+, Ca2+, SiO2, Al, Fe, Ni, Zn, Sb, Pb and U in the groundwater than the surface water was observed, may be due to leaching from the coal (Figure 2, Figure 3). The main sources of the contaminants in the water of the studied area expected are 8 K. S. Patel et al. 8 mg/L 6 4 2 0 pH FF− DO Parameter SW GW mg/L (a) 700 600 500 400 300 200 100 0 RP EC TDS Parameter SW GW mg/L (b) 40 35 30 25 20 15 10 5 0 Al Mg2+ Mg2+ Cl Cl-− SiO2 SiO2 2+ Ca Ca2+ NO3− NO3- 2− SO 4 SO42- Na+ Na+ Element SW GW (c) Figure 2. Distribution of pH and elements in ground and surface water in the post monsoon period, January, 2013. coal mine leachates and the Aluminum and Thermal power plant effluents discharged into the environment. 3.5. Exposure Assessment The toxic elements i.e. F−, Al, Mn, Fe, Cu, Cd, Pb and U are exposed to human and animals through the contaminated water. Among them, the concentration of F− is dominated in ground and surface water. The stool and urine samples were reported as good indicator for the exposure assessment. In this study, the F− content was analyzed in stool and urine samples of domestic animals i.e. cattle, buffalo, sheep and goat (Table 9). The F− concentration in the urine and stool samples (5 × 4 × 2 = 40) was ranged from 32 - 63 mg/L and 186 - 356 mg/kg with mean value of 44 mg/L and 266 mg/kg (dried mass), respectively. The highest F− concentration was observed in the goat clinical samples, which might be due to higher intake of the contaminated biomass and water (Figure 4). Several cases of fluorosis diseases in the domestic animals of the basin was observed and shown in Figure 5. 4. Conclusion The water of the Korba basin is contaminated with elements (i.e. F−, Al, Fe and Mn) by multiple sources (i.e. coal 9 K. S. Patel et al. A 12 SW GW 10 mg/L 8 6 4 2 0 Mn + K K+ Fe Metal (a) 20 SW GW µ g/L 15 10 5 0 Ni Cu Li Rb Metal µ g/L (b) 8 7 6 5 4 3 2 1 0 SW GW U Sb Pb Element (c) Figure 3. Distribution trace elementsin ground and surface water in the post monsoon period, January, 2013. 700 600 mg/L 500 400 300 200 100 0 Cattle Buffalo Sheep Sample Urine − Stool Ash Figure 4. Comparison of F concentration in clinical samples. 10 Goat K. S. Patel et al. (a) (b) Figure 5. Dental (a) and hair (b) fluorosis in buffalo. Table 9. Concentration of F− in clinical samples during January 2013. S. No. Sample Cattle Buffalo Sheep Goat 1 Urine 32 38 42 63 2 Stool 186 233 287 356 3 Ash 324 516 567 602 burning, Aluminum plant effluent, mine leachate, etc.). 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