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首页> 外文期刊>Soil Science >CdEDTA2- adsorption to weathered shale-limestone saprolite: modeling the adsorption mechanism and effect of Al-oxide co-dissolution on Fe-oxide dissolution dynamics.
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CdEDTA2- adsorption to weathered shale-limestone saprolite: modeling the adsorption mechanism and effect of Al-oxide co-dissolution on Fe-oxide dissolution dynamics.

机译:CdEDTA2-对风化的页岩-石灰石腐泥土的吸附:模拟Al-氧化物共溶解对Fe-氧化物溶解动力学的吸附机理和影响。

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Partially weathered bedrocks that retain the fabric and structure of the parent rocks, commonly known as saprolite, exist extensively in the subsurface. A large quantity of Fe-, Al- and Mn-oxides is often present in saprolite soils. These surface oxides are very important in promoting and regulating geochemical reactions in the subsurface. The objective of this research is to identify and characterize the mechanisms of CdEDTA2- surface complexation in a saprolite derived from a shale-limestone bedrock on the Oak Ridge Reservation of the US Department of Energy. CdEDTA2- is a compound of two widely used industrial chemicals. As a result of the complexation of Cd and EDTA, the mobility of Cd is largely increased. This has had grave implications to the environment and the industrial facilities that use EDTA as a chelating agent for various purposes. The existence of Fe- and Al-oxides in the saprolite with highly pH-buffered soil solutions may result in the co-dissolution of Fe and Al oxides under the influences of pH and EDTA. In this research, a series of laboratory batch experiments was conducted with varying initial concentrations of CdEDTA2- in the presence of the saprolite. Three surface complexation mechanisms were evaluated in terms of their likelihood of describing the dynamics of CdEDTA2- adsorption and oxide dissolution. The modelling results verified a previous hypothesis that the formation rate of AlEDTA- was faster than that of FeEDTA-, largely because of the much larger initial concentration of Al ions in the soil solution. The subsequent CdEDTA2- dissociation and acid-promoted Al-oxide dissolution was thus identified as mechanisms that may interfere or inhibit the transformation of a surface CdEDTA2- ternary complex to FeEDTA- and explain the slower formation rate of FeEDTA-. It was concluded that acid-promoted dissolution of amorphous Al-oxide may exert certain degree of control on the dissolution dynamics of amorphous Fe-oxide..
机译:保留母体岩石结构和结构的部分风化基岩(通常称为腐泥土)广泛存在于地下。腐泥土中经常存在大量的Fe,Al和Mn氧化物。这些表面氧化物对于促进和调节地下的地球化学反应非常重要。这项研究的目的是鉴定和表征美国能源部橡树岭保留地页岩-石灰岩基岩衍生的腐泥土中CdEDTA2-表面络合的机理。 CdEDTA2-是两种广泛使用的工业化学品的化合物。由于Cd和EDTA络合,Cd的迁移率大大提高。这对使用EDTA作为多种螯合剂的环境和工业设施产生了严重影响。在腐泥土中,pH值较高的土壤溶液中铁和铝的氧化物的存在可能会导致铁和铝的氧化物在pH和EDTA的影响下共同溶解。在这项研究中,在腐泥土存在下,使用不同的CdEDTA2-初始浓度进行了一系列实验室批量实验。根据描述CdEDTA2-吸附和氧化物溶解动力学的可能性,对三种表面络合机理进行了评估。模拟结果证实了先前的假设,即AlEDTA-的形成速度比FeEDTA-的形成速度要快,这在很大程度上是由于土壤溶液中Al离子的初始浓度大得多。因此,随后的CdEDTA2-解离和酸促进的Al溶解被确定为可能干扰或抑制表面CdEDTA2-三元络合物向FeEDTA-转化的机制,并解释了FeEDTA-的形成速度较慢。结论是酸促进非晶态氧化铝的溶解可对非晶态Fe的溶解动力学产生一定程度的控制。

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