납 안정동위원소를 이용한 아연제련시설 인근지역의 납 오염 특성
Characterization of Lead Pollution Near Zinc Smelter Facility in South Korea using Lead Stable Isotopes
2
조회
0
다운로드
0
인용
0
참고문헌
키워드
초록
This study was conducted to evaluate lead(Pb) pollution near a zinc smelter using Pb stable isotopes as environmental tracers. Environmental samples such as air particles, precipitation, soils, conifer leaves, and tree rings were analyzed; input and output materials were also collected from the zinc smelter. The 207Pb/206Pb ratios of the output materials from the zinc smelter were in the range of 0.865-0.881, and plotted on a mixing line with zinc ores from South America and Australia as the two end-members. The 207Pb/206Pb ratios of air particles, precipitation, and conifer leaves were in the ranges of 0.822-0.887, 0.853-0.882, and 0.866-0.877, respectively, and fall within the line attributed to the smelter. In contrast, the 207Pb/206Pb ratios of soils fell within a broader range of 0.694-0.893. Soils with a higher 207Pb/206Pb ratio of 0.850 were plotted on the smelter line and showed high Pb concentrations of 207.5±141.9 mg/kg. Soils with a lower 207Pb/206Pb ratio of 0.850 were plotted on the Korean ore line and showed low Pb concentrations of 60.5±44.2 mg/kg. The 207Pb/206Pb ratios of tree rings showed an increasing trend toward the isotopic composition of emission gases, implying that the source of Pb pollution changed from the local mine to the zinc smelter.
Abstract
This study was conducted to evaluate lead(Pb) pollution near a zinc smelter using Pb stable isotopes as environmental tracers. Environmental samples such as air particles, precipitation, soils, conifer leaves, and tree rings were analyzed; input and output materials were also collected from the zinc smelter. The 207Pb/206Pb ratios of the output materials from the zinc smelter were in the range of 0.865-0.881, and plotted on a mixing line with zinc ores from South America and Australia as the two end-members. The 207Pb/206Pb ratios of air particles, precipitation, and conifer leaves were in the ranges of 0.822-0.887, 0.853-0.882, and 0.866-0.877, respectively, and fall within the line attributed to the smelter. In contrast, the 207Pb/206Pb ratios of soils fell within a broader range of 0.694-0.893. Soils with a higher 207Pb/206Pb ratio of 0.850 were plotted on the smelter line and showed high Pb concentrations of 207.5±141.9 mg/kg. Soils with a lower 207Pb/206Pb ratio of 0.850 were plotted on the Korean ore line and showed low Pb concentrations of 60.5±44.2 mg/kg. The 207Pb/206Pb ratios of tree rings showed an increasing trend toward the isotopic composition of emission gases, implying that the source of Pb pollution changed from the local mine to the zinc smelter.
참고문헌 (15)
- B. L. Murphy., "Introduction to Environmental Forensics" (2007), Academic Press
- 국립환경과학원, "환경오염원 추적기법-중금속 동위원소편(I)", 31~42 (2012)
- "International lead and zinc study group, press release" (2011)[URL]
- Final review of scientific information on lead, "United nations environment programme.", 60~72 (2010)
- M. Komarek, "Lead isotopes in environmental sciences : A review", Environment International, 34, pp.562~577 (2008)
- H. Cheng, "Lead (Pb) isotopic fingerprinting and its applications in lead pollution studies in China:a review", Environmental Pollution, 158, pp.1134~1146 (2010)
- L. Qian, "The estimated atmospheric lead emissions in China, 1990-2009", Atmospheric Environment, 60, pp.1~8 (2012)
- 박진주, "납 동위원소를 이용한 안동호 퇴적물 중의 납 오염 기원", 분석과학, 25(6), pp.429~434 (2012), 한국분석과학회
- E. -J. Yoo., "Tracing lead pollution sources in abandoned mine area using stable Pb isotope ratios", Environmental Monitoring and Assessment, 186, pp.781~789 (2014)
- F. Albarède, "Analytical Methods for Non-Traditional Isotopes", Reviews in Mineralogy & Geochemistry, 55, pp.113~152 (2004)
- A. E. Shiel., "Evaluation of zinc, cadmium and lead isotope fractionation during smelting and refining", Science of the Total environment, 408, pp.2357~2368 (2010)
- M. E. Kylander., "Tow high resolution terrestrial records of atmospheric Pb deposition from New Brunswick, Canada, and Loch Laxford, Scotland", Science of the Total Environment, 407, pp.1644~1657 (2009)
- 환경부, "대기환경연보(2012)", 64~65 (2013)
- 박계헌, "연화 및 장군 연-아연 광상의 Pb 동위원소 조성 및 Pb의 근원 : 선캠브리아 기저 지각 및 중생대 화성암의 역할", 한국암석학회지, 14, pp.141~148 (2005)
