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贵州东风水库中不同形态汞迁移转化规律的初步探讨
其他题名The Primary Study on Distributions and Transformations of Mercury in Dongfeng Reservoir, Guizhou, China
刘凯
2009-05-26
学位授予单位中国科学院地球化学研究所
学位授予地点地球化学研究所
学位名称博士
关键词 甲基汞 沉积物 水库 季节变化
摘要北欧和北美的研究发现水库是典型的汞敏感生态系统,新建水库而引起的鱼的甲基汞污染问题已经受到科学家的高度重视,而我国在这方面的研究比较薄弱。本论文以乌江流域上游的东风水库为研究对象,于夏季(2007 年8月)、冬季(2007 年12 月)和春季(2008年4月)分别对水库不同深度分层水体、沉积物间隙水、沉积柱剖面中不同形态汞的含量、分布特征以及迁移转化规律进行了详细的研究。研究结果发现: 1.东风水库水体中各种形态汞浓度均表现出季节性变化。总汞(THg)浓度变化范 围为1.1-2.3ng/L,平均为1.6ng/L;溶解态汞(THg)浓度变化范围为0.3-1.3ng/L,平均为0.6ng/L;颗粒态汞(PHg)浓度范围为0.3-1.5ng/L,平均为0.8ng/L;活性汞(RHg)浓度范围为0.2-0.6ng/L,平均为0.4ng/L;总甲基汞(TMHg)浓度变化范 围为0.04-1.01ng/L,平均为0.27ng/L;溶解态甲基汞(DMHg)浓度变化范围为0.03-0.48ng/L,平均为0.12ng/L;颗粒态甲基汞汞(PMHg)浓度范围为0.01-0.7ng/L,平均为0.16ng/L。 2.东风水库水体颗粒态总汞与总汞呈极显著相关,说明东风水库水体的颗粒态汞强烈影响着总汞迁移和分布。水库水体总甲基汞与溶解态甲基汞汞和颗粒态甲基汞之间存在极显著正线性相关,证明水库水体中的甲基汞的产生和迁移与溶解态甲基汞和颗粒态甲基汞均有着密切的关系。但是,水体甲基汞与总汞之间并不存在相关性。 3.东风水库水体夏季溶解态汞、活性汞、溶解态甲基汞浓度均远高于冬春两季,除了外源异重径流输入的影响外,很大程度与夏季水库底部缺氧环境密不可分。沉积物释放大量吸附的汞进入水体,造成水体溶解态汞、活性汞、溶解态甲基汞的升高。 4.东风水库沉积物间隙水中总汞和甲基汞浓度出现明显的季节性变化,夏季大于冬春两季。沉积物甲基汞的浓度分布与沉积物中有机质含量相关性明显(r=0.219*,n=133)。东风水库沉积物中甲基汞的含量随沉积物深度增加浓度梯度不明显。 5.东风水库沉积物总汞含量基本没有季节变化,浓度变化范围为97-354ng/g,平均为180ng/g。东风水库沉积物中总汞含量大大高于其他未受污染地区水库沉积物中总汞含量。甲基汞含量变化范围为0.1-5.5ng/g,平均为2.1ng/g 。 6.东风水库沉积物间隙水中总汞、甲基汞浓度均显著高于其上覆水体的总汞和甲基汞的浓度,二者之间存在显著的浓度梯度,沉积物中总汞和甲基汞的释放是水库水体的重要来源。
其他摘要Some studies have revealed that reservoir is one of the typical Hg-sensitive ecosystems in northern Europe and North America, and sepecial attention has been paid to methylmercury pollution in fishes in newly constructed reservoirs. In this thesis, we present a comprehensively study on the distribution and transformation of mercury species the Dongfeng reservoir. In August 2007, December 2007, and April 2008, samples from water columns, sediment profiles, and inflow and outflow streams of Dongfeng reservoir were collected and analyzed to study the influence of man-made reservoir on the environmental biogeochemistry of Hg. some main conclusions were obtained as follows: 1. Discernible seasonal change of different mercury in water body were obtained in Dongfeng Reservoir. The concentrations of total mercury(THg) were 1.1-2.3ng/L, the average is 1.6ng/L ; The concentrations of dissolved (DHg) ranged from 0.3-1.3ng/L, the average is 0.6ng/L ;The concentrations of particulate mercury (PHg) were 0.3-1.5 ng/L, the average is 0.8ng/L; The concentrations of reactive mercury (RHg) were 0.2-0.6ng/L , the average is 0.4ng/L; The concentrations of methylmercury(TMHg) were 0.04-1.01ng/L , the average is 0.27ng/L; The concentrations of dissoved methylmercury (DMHg) were 0.03-0.48ng/L , the average is 0.12ng/L; The concentrations of particulate methylmercury (PMHg) were 0.01- 0.7ng/L , the average is 0.16ng/L. 2. With regards to the whole sampling periods, the concentrations of HgP in Dongfeng Reservoir water body were evidently correlated to the concentrations of total mercury, it shows that total mercury was mostly associated with particles mercury. The concentrations of methylmercury in water body were also evidently correlated to the concentrations of dissolved mercury. The dissolved mercury evidently effects the distribution and transportation of methylmercury. However, there is no correlated between methylmercury and total mercury. 3. The dissolved mercury, reactive mercury, dissolved methylmercury levels in the water body in summer were much higher than those in winter and spring .The distribution, speciation and levels of mercury in Dongfeng Reservoir water body were governed by several factors, such as the output of river, the release ofsediment . 4. Discernible seasonal change of total mercury and methylmercury in porewater were obtained during the sampling periods, with the concentrations in summer were generally higher than those in winter and sping. The methylmercury in pore water column were correlated to organic materials in the sediment (r=0.219*,n=133). Maximum levels of methylmercury in sediment profiles changed greatly, with no distinct concentration grads. 5. Total mercury levels in the whole sediments in Dongfeng Reservoir were 97-354ng/g , the average is 180ng/g, without significant variations between different seasons. The total mercury levels in Dongfeng Reservoir were higher compared to data reported in other uncontaminated reservoirs. The levels of methylmercury were 0.1-5.5ng/g, the average is 2.1ng/g. 6. The concentrations of HgD and MeHgD in porewater were higher than that obtained in the underlying water, with a great concentration grads, which suggested that the sediment was a dominant Hg source to the reservoir.
页数72
语种中文
文献类型学位论文
条目标识符http://ir.gyig.ac.cn/handle/352002/3508
专题研究生_研究生_学位论文
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GB/T 7714
刘凯. 贵州东风水库中不同形态汞迁移转化规律的初步探讨[D]. 地球化学研究所. 中国科学院地球化学研究所,2009.
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