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首页> 外文期刊>Fresenius environmental bulletin >AN INVESTIGATION IN DYNAMIC PROCESSES AND ITS INFLUENCES OF IRON AND MANGANESE RELEASES FROM RESERVOIR SEDIMENT
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AN INVESTIGATION IN DYNAMIC PROCESSES AND ITS INFLUENCES OF IRON AND MANGANESE RELEASES FROM RESERVOIR SEDIMENT

机译:储层沉积物中铁,锰释放动力学过程及其影响研究。

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To control the emission of iron (Fe) and manganese (Mn) from reservoir sediment, fluxes of Fe and Mn across the sediment-water interface were tested in the laboratory to study the dynamic release properties of Fe and Mn from the sediment and to investigate the influences of dissolved oxygen (DO), biological effect and light on their release processes. The results showed that dissolved Fe (DFe) in the pore water was mainly microbially caused and its release resulted from diffusion and exchange with solid phase of the top sediment. Whereas, microbes activities was not the only reason for dissolved Mn (DMn) in pore water, and its release was mainly influenced by the concentration difference between pore water and overlying water. Moreover, the release of Fe from sediment was significantly influenced by DO, biological effects, while Mn release was greatly affected by DO and temperature.
机译:为了控制储层沉积物中铁(Fe)和锰(Mn)的排放,在实验室中测试了穿过沉积物-水界面的Fe和Mn的通量,以研究Fe和Mn从沉积物中的动态释放特性,并进行了研究。溶解氧(DO),生物效应和光对其释放过程的影响。结果表明,孔隙水中溶解的Fe(DFe)主要是微生物引起的,其释放是由于顶部沉积物与固相的扩散和交换所致。微生物活性并不是孔水中溶解的Mn(DMn)的唯一原因,其释放主要受孔水与上覆水之间浓度差异的影响。此外,沉积物中铁的​​释放受DO,生物学效应的显着影响,而Mn的释放则受DO和温度的显着影响。

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