Syrovetnik K, Malmström M E, Neretnieks I
Department of Chemical Engineering and Technology, School of Chemical Science and Engineering, Kungliga Tekniska Högskolan, SE-10044 Stockholm, Sweden.
Environ Pollut. 2007 May;147(1):291-300. doi: 10.1016/j.envpol.2005.10.048. Epub 2007 Jan 30.
The Oostriku peat bog (central Estonia) has been exposed to metal-rich groundwater discharge over a long period of time and has accumulated high concentrations of Fe (up to 40 wt-%), heavy metals (e.g. Pb, Zn, Mn, Cu), and As. In this study, the peat was characterised with respect to composition and metal content with depth. The peat pore water was analysed and compared to a spring water emerging at the site. Sequential extraction, using a Tessier scheme optimised for iron-rich sediments, was used to understand the relative roles of binding mechanisms involved in the retention of different metals in the peat. Significant difference in depth distribution was found between different metals bound in the peat, which was partly attributed to varying compositions of the peat with depth and different dominant binding mechanisms for different metals.
奥斯特里库泥炭沼泽(爱沙尼亚中部)长期受到富含金属的地下水排放影响,积累了高浓度的铁(高达40 wt-%)、重金属(如铅、锌、锰、铜)和砷。在本研究中,对泥炭的成分和随深度变化的金属含量进行了表征。对泥炭孔隙水进行了分析,并与该地点涌出的泉水进行了比较。采用针对富铁沉积物优化的 Tessier 方案进行连续提取,以了解泥炭中不同金属保留所涉及的结合机制的相对作用。发现泥炭中结合的不同金属在深度分布上存在显著差异,这部分归因于泥炭成分随深度的变化以及不同金属的不同主导结合机制。