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Experimental studies of adsorption in bacteria-water-rock systems: Implications for heavy metal transport in the subsurface.

机译:细菌-水-岩石系统中吸附的实验研究:对地下重金属迁移的影响。

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Bacteria are ubiquitous in near-surface geologic environments, and bacteria cell walls display a high affinity for metal cations. The adsorption of metals onto bacterial surfaces can affect heavy metal contaminant transport and the effectiveness of bioremediation techniques. Quantitative prediction of the effects of bacterial adsorption on metal mobility requires an accurate knowledge of metal-bacteria and bacteria-mineral interactions. However, the effects of bacterial adsorption on metal transport are poorly understood, and with our current knowledge it is impossible to quantitatively assess the magnitude which bacteria can enhance or retard the mobility of metal contaminants.; The research presented in this dissertation thesis quantitatively describes the effects of bacterial adsorption on metal distribution and transport. Proton and Cd adsorption onto bacteria surfaces is studied for a range of gram-positive and gram-negative bacterial species. The experimental results indicate that a wide range of bacterial species adsorb nearly identical amounts of Cd as a function of pH. Metal adsorption experiments are also conducted with complex bacteria mixtures as functions of pH and bacteria:metal ratio. The adsorption behavior of bacteria mixtures is similar to that of a single bacterial species, and the extent of adsorption can be quantified using a surface complexation model.; Bacterial adsorption onto the mineral surface of corundum is studied as a function of time, pH, ionic strength and bacteria:mineral mass ratio. The data demonstrate that the adsorption of bacteria onto a mineral surface is a completely reversible process, and that the adsorption behavior is governed by the chemical speciation of the bacterial and mineral surfaces. Column and batch experiments are performed with ternary metal-bacteria-mineral systems. The results indicate that a surface complexation model can be applied to successfully quantify the distribution of Cd between the aqueous phase and the bacterial and mineral surfaces, and the model can be used to estimate the distribution of mass in systems not directly studied in the laboratory.; The experimental results underscore the need for a flexible modeling approach to quantify bacterial adsorption reactions. The surface complexation model is proposed as a quantitative means to account for the complex adsorption chemistry in bacteria-water-rock systems.
机译:细菌在近地表地质环境中无处不在,细菌细胞壁对金属阳离子显示出高亲和力。金属在细菌表面上的吸附会影响重金属污染物的运输和生物修复技术的有效性。细菌吸附对金属迁移率影响的定量预测需要对金属-细菌和细菌-矿物质相互作用的准确了解。然而,人们对细菌吸附对金属运输的影响了解甚少,以我们目前的知识,不可能定量评估细菌可以增强或阻碍金属污染物迁移的程度。本文定量研究了细菌吸附对金属分布和迁移的影响。研究了一定范围内革兰氏阳性和革兰氏阴性细菌种类的质子和Cd在细菌表面的吸附。实验结果表明,作为pH的函数,各种各样的细菌种类吸收的镉几乎相同。还根据pH和细菌:金属比率的函数,对复杂细菌混合物进行了金属吸附实验。细菌混合物的吸附行为类似于单个细菌物种的吸附行为,并且可以使用表面络合模型对吸附程度进行量化。研究了细菌在刚玉矿物表面上的吸附随时间,pH,离子强度和细菌:矿物质质量比的变化。数据表明细菌在矿物表面上的吸附是完全可逆的过程,并且吸附行为受细菌和矿物表面的化学形态控制。用三元金属-细菌-矿物质系统进行柱和分批实验。结果表明,可以使用表面络合模型成功地量化Cd在水相与细菌和矿物表面之间的分布,并且该模型可以用于估算未在实验室中直接研究的系统中的质量分布。 ;实验结果强调需要一种灵活的建模方法来量化细菌吸附反应。建议采用表面络合模型作为定量方法,以解决细菌-水-岩石系统中的复杂吸附化学反应。

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