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    中国百强科技报刊

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    Volume 39 Issue 6
    Jun.  2014
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    Article Contents
    Wang Juan, Wang Zhenghai, Geng Xin, He Fengping, Zu Yuchuan, Wang Lei, 2014. REE Biogeochemistry of Soil-Vegetation System in Dabaoshan Polymetallic Mine. Earth Science, 39(6): 733-740. doi: 10.3799/dqkx.2014.068
    Citation: Wang Juan, Wang Zhenghai, Geng Xin, He Fengping, Zu Yuchuan, Wang Lei, 2014. REE Biogeochemistry of Soil-Vegetation System in Dabaoshan Polymetallic Mine. Earth Science, 39(6): 733-740. doi: 10.3799/dqkx.2014.068

    REE Biogeochemistry of Soil-Vegetation System in Dabaoshan Polymetallic Mine

    doi: 10.3799/dqkx.2014.068
    • Received Date: 2013-11-13
    • Publish Date: 2014-06-15
    • REE biogeochemistry is important in understanding the occurrence, migration and fractionation of REE and its ecologically environmental effects. In order to explore the REE biogeochemistry of soil-vegetation system in mining affected region, Dabaoshan mine, a typical polymetallic mine, was chosen as a study area. Soils and leaves of dominant Dicranopteris Pedata and Pinus massoniana, from and outside the mine, were collected. Then REE contents were measured by using the ICP-MS. REE distribution patterns, ∑REE, δEu and δCe were analyzed. Results show that mining area, with the mean ∑REE 284.99 mg/kg, has significantly higher REE contents than outside areas., In addition, REE contents in epipedon are much higher than those in subsoil due to the effects of mining activity. What's more, the fractional degree of HREE and LREE of both soil and plant is much weaker in mining area compared with that outside the mine. The soils and plants collected are all characterized by Eu deficiency and Ce enrichment. And the accumulator Dicranopteris Pedatahas lower REE enrichment coefficient than Pinus massoniana by the presence of heavy metal. Therefore, the mining environment has negative effect on the normal migration and fractionation of REE in soil-vegetation system and growth of plants.

       

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