Dispersion and Migration of Potentially Toxic Elements in the Rock-Soil-Plant System from the Boeun Area Underlain by Black Shales, Korea

보은지역 흑색셰일 분포지역에서의 암석-토양-식물계내 잠재적 독성원소들의 분산과 이동

  • Lee, Jin-Soo (Department of Mineral and Petroleum Engineering, Seoul National University) ;
  • Chon, Hyo-Taek (Department of Mineral and Petroleum Engineering, Seoul National University) ;
  • Kim, Kyoung-Woong (Department of Environmental Science Engineering, Kwangju Institute of Science and Technology)
  • Received : 1997.12.09
  • Published : 1997.12.31

Abstract

This study had three purposes: (1) to investigate the enrichment levels and dispersion patterns of potentially toxic elements in the rock-soil-plant system; (2) to evaluate the uptake ratios of heavy metals from soils into plants and (3) to assess the chemical speciation of heavy metals in soils. Rock, surface soil and plant samples were collected in the Boeun area underlain by black shales of the Okchon Zone. These samples were analyzed for multi-elements using INAA, ICP-AES and AAS. The maximum abundance of U in black shales is 16 mg/kg and radioactivity counts up to 300 cpm. In particular, Mo, V, Ba, Cd, Pb and U are enriched in black shales. Most of soils derived from black shales show high concentrations of U, As, Mo, Ba, Cu, Cd, Pb, Zn and mean concentrations of As and Mo in soils (20 mg/kg of As and 6.6 mg/kg of Mo) are higher than the permissible level suggested by Kloke (1979). Enrichment index values of soils are calculated and higher than 1.0 in the black shale area with the highest value of 6.4. Mean concentration of Cd in plants is higher than those of Cu, Pb and Zn. The concentration of Cd in plant species decreases in the order of Chinese cabbage > red pepper > soybean=sesame > rice stalk > com > rice grain. The biological absorption coefficients (BAC) in plants are in the order of Cd > Zn=Cu > Pb, which suggests that Cd is more bioavailable to plants than Cu, Pb and Zn. From the results of sequential extraction analysis of soils, relatively high proportion of Cu, Pb and Zn are present as residual fractions whereas that of Cd as non-residual fractions. Cadmuim occurs predominantly as exchangeable/water-acid soluble phase in soils, and Cd is more mobile and bioavailable than Cu, Pb and Zn.

Keywords

Acknowledgement

Grant : 옥천대의 지질환경학적 연구 III

Supported by : 교육부