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Source Identification and Speciation of Metals in the Topsoil of the Khli Ti Watershed, Thailand
Authors:Paweena Panichayapichet  Suwanchai Nitisoravut  Wijarn Simachaya  Arpa Wangkiat
Institution:1. The Joint Graduate School of Energy and Environment, King Mongkut’s University of Technology Thonburi, 126 Pracha-Uthit Road, Bangmod, Tungkru, Bangkok, 10140, Thailand
2. Sirindhorn International Institute of Technology, Thammasat University, P.O. Box 22, Thammasat-Rangsit Post Office, Klong Luang, Pathumthani, 12121, Thailand
3. Pollution Control Department, Ministry of Natural Resources and Environment, 92 Soi Phahon Yothin 7, Phahon Yothin Road, Sam Sen Nai, Phayathai District Bangkok, 10400, Thailand
4. Department of Civil and Environmental Engineering, Rangsit University, 52/347 Paholyothin Rd., Lakhok, Muang, Pathumthani, 12000, Thailand
Abstract:The enrichment factor, multivariate analysis and metal speciation studies were used to identify degree, source and dispersal of metal contamination in Khli Ti watershed, Thailand. Topsoil samples were collected throughout the watershed, analyzed for total metal concentration. Sequential extraction was also carried out to determine geochemical phases of metals which were identified as exchangeable and bound to carbonates, Fe–Mn oxides, organic matter and residuals. Soil characteristics including pH, total organic carbon, redox potential, cation exchange capacity and texture were also analyzed. Principal component analysis yielded three metal groups which explained 83% of the variance. The concentrations of metals which were derived from lithogenic origin, such as Co, Cr, Fe, Ni and V were in natural background levels and were mostly bound to the residual phase. The remaining elements (i.e. Ba, Cd, Cu, Pb, Sb and Zn) were associated with the contamination from previous activities of the Pb-ore concentrator and Zn–Pb mining. Anthropogenic contamination mainly increased Pb and Zn bound to Fe–Mn oxides at the expense of residual fraction. Even though low exchangeable Pb contents in Khli Ti soils indicated low availability to plants, Pb bound to Fe–Mn oxides fraction might increase its mobility under reducing conditions.
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