淹没–出露条件下三峡水库小江消落带土壤性质变化研究
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国家水体污染与治理科技重大专项(2013ZX07104)、三峡后续工作科研项目(2013HXKY2-3)和国家自然基金面上项目(51379133)资助


Soil Property Changes Under Drain-Flooding Condition in Xiaojiang Water-level-fluctuating Belt of the Three-Gorge-Reservoir Region
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    摘要:

    以2010—2011年间采自三峡水库小江流域不同海拔消落带土壤为材料,研究了淹没前后土壤有机质、磷、氧化铁等性质的变化,以揭示消落带土壤的变化特征及其环境影响。结果表明:小江消落带土壤淹没后,土壤pH、有机质及速效磷、全磷、非晶质铁、游离氧化铁、黏粒含量增加;土壤出露后,监测点各海拔土壤的有机质、速效磷、非晶形铁、游离氧化铁及黏粒含量降低;消落带土壤经过一个“淹没–出露”周期后,双江、高阳监测点海拔170 m和165 m土壤的铁活化度降低,而海拔150 m土壤的铁活化度明显升高,增幅分别达12.4% 和94.5%。消落带土壤在经过淹没–出露过程后,磷有累积现象,其环境风险增大,应引起重视。

    Abstract:

    The soil samples were collected in Xiaojiang River Basin at different altitudes from 2010?–?2011. The changes of soil physiochemical properties, including soil pH, organic matter, phosphorus and iron oxide, were studied to reveal the variation of water-level-fluctuating belt soil and its environmental impact. The results showed that: the soil pH, organic matter, available phosphorus(P), total P, amorphous iron(Feo), free iron (Fed) and clay content increased after flooding; the soil organic matter, available P, Feo, Fed and clay content decreased after drain; the Feo/Fed of soils decreased from Shuangjiang and Gaoyang sites in 170 m and 165 m altitudes under a “drain-flooding” cycle, but the Feo/Fed increased significantly by 12.4% and 94.5%, respectively, in 150 m altitude. As the physiochemical properties of soils changed obviously change under “drain-flooding” process and P accumulated, the increasing environmental risk should be taken into consideration seriously.

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朱 强,张志永,胡红青,万成炎,胡 莲,刘 晖.淹没–出露条件下三峡水库小江消落带土壤性质变化研究[J].土壤,2014,46(5):927-932. ZHU Qiang, ZHANG Zhi-yong, HU Hong-qing, WAN Cheng-yan, HU Lian, LIU Hui. Soil Property Changes Under Drain-Flooding Condition in Xiaojiang Water-level-fluctuating Belt of the Three-Gorge-Reservoir Region[J]. Soils,2014,46(5):927-932

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  • 在线发布日期: 2014-11-18
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