Economic and Environmental Geology (자원환경지질)
- Volume 30 Issue 4
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- Pages.341-352
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- 1997
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- 1225-7281(pISSN)
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- 2288-7962(eISSN)
The Geochemical Behaviour and Environmental Pollution of Pb, Zn, Mn and Cd in Interstitial Waters and Sediments from a Retention Pond along the A-71 Highway, France
프랑스 A-71고속도로변에 설치된 침전조에서 채취된 간극수와 퇴적물에 함유된 Pb, Zn, Mn 및 Cd의 지화학적 행동 및 오염에 관한 연구
- Lee, Pyeong-Koo (Korea Institute of Geology, Mining and Materials)
- 이평구 (한국자원연구소 환경지질연구부)
- Received : 1997.07.09
- Published : 1997.08.30
Abstract
Retention ponds have been dug along some of the motorways in France to minimize environmental pollution by keeping pollutants from spreading over the surrounding area. In order to study heavy metal pollution and diagenetic behaviour of sediments, eight core samples were collected from the bottom of a retention pond located along the A-71 motorway in Sologne. The metal concentrations in interstitial waters and extractable metal concentrations in sediment layers using sequential chemical extraction method were determined. The depth distributions of Pb, Zn and Cd concentrations in interstitial water and particulate sediments were studied, and distribution coefficients (KD) were also determined to investigate the environmental mobility of these elements. In addition. the index of geoaccumulation and the Fe-normalized enrichment factor were calculated to differentiate the natural accumulation from the anthropogenic pollution. The vertical concentration profiles of heavy metals in core sediments indicate that surface enrichments (0~2 cm) of Pb, Zn, Cd and organic carbon were always observed at each core sample, due to the early diagenesis. However, the major factor contributing to the accumulation of Cd at the sediment surface is attributed to the dissolution of Cd from polluted roadside soil during periods of rainstorms and its subsequent redeposition on the sediment surface after being carried to the retention pond. A comparison of the KD values indiactes that a decrease in the KD values for Pb and Zn was observed with depth while KD values for Cd increase. According to the KD values. the relative mobility of studied metals was determined as following: Mn>Zn>Cd>Pb, for the upper layer, and Mn>Cd>Zn>Pb, for the lower layers.
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