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Source and remediation for heavy metals of soils at an iron mine of Ulsan City,Korea
Authors:Sang Yong Chung  Venkatramanan Senapathi  Kye Hyun Park  Joo Hyeong Son  Selvam Sekar
Institution:1.Department of Earth and Environmental Sciences,Pukyong National University,Busan,South Korea;2.Department for Management of Science and Technology Development,Ton Duc Thang University,Ho Chi Minh City,Vietnam;3.Faculty of Applied Sciences,Ton Duc Thang University,Ho Chi Minh City,Vietnam;4.Department of Groundwater and Geology,Korea Rural Community Corporation,Uichang-gu Changwon-si,South Korea;5.Department of Geology,V. O Chidambaram College,Tuticorin,India
Abstract:Ulsan mine produced the iron ore minerals of magnetite, arsenopyrite, and scheelite in 1992, and serpentine was developed from 1977 to 2002. The soils of the mine were contaminated by heavy metals such as As, Zn, Ni, and Cd. Heavy metals of Ni and Zn came mostly from serpentinite, and As was derived mainly from arsenopyrite in the scan-type iron ore body. As, Zn, and Ni were major contaminants, but Cd was a minor contaminant on a basis of Korean standard. The heavy metals in the deep depth (>?5 m) came from the host rocks, and those in the shallow depth (<?5 m) were derived from the organic–mineral complexation soil. The remediation plan was a soil washing for highly contaminated soils and the containment of clay materials for less contaminated soils. Even though the remediation methods were successful, the continuous monitoring and the analysis of monitoring data are still necessary for the conservation of soil and groundwater around the study area.
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