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Modelling metal-humic substances-surface systems: reasons for success, failure and possible routes for peace of mind

机译:对金属-腐殖质-表面系统进行建模:成功,失败的原因以及让您安心的途径

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Iron oxides and oxyhydroxides are commonly of considerable importance in the sorption of ions onto rocks, soils and sediments. They can be the controlling sorptive phases even if they are present in relatively small quantities. In common with other oxides and clay minerals, the sorption pH-edge of metals is directly linked to their hydrolysis: the higher the residual charge on the metal ion, the lower the pH-edge. Modelling of this process has been successfully carried out using different microscopic or macroscopic definitions of the interface (e.g. surface complexation or ion exchange models that may or may not include mineralogical descriptions). The influence of organic material on the sorption of many metals is of significant. This organic material includes simple organic molecules and more complex exopolymeric substances (e.g. humic substances) produced by the decay of natural organic matter. Sorption of this organic material to mineral surfaces has been the subject of a large body of work. The various types of organic substances do not share the same affinities for mineral surfaces in general, and for iron oxides and oxyhydroxides in particular. In those cases in which successful models of the component binary systems (i.e. metal-surface, metal-organic, organic-surface) have been developed, the formation of mixed surface complexes, the evolution of the surface itself, the addition order in laboratory systems, and the evolution of natural organic matter fractions during sorption, have often precluded a satisfactory description of metal-surface-organic ternary systems over a sufficiently wide range of parameter values (i.e. pH, ionic strength, concentration of humic substances). This manuscript describes the reasons for some successes and failures in the modelling of the ternary systems. Promising recent advances and possible methods of providing more complete descriptions of these intricate systems are also discussed.
机译:氧化铁和羟基氧化铁通常在将离子吸附到岩石,土壤和沉积物上时具有相当重要的意义。即使它们以相对少量存在,它们也可以是控制吸附相。与其他氧化物和粘土矿物一样,金属的吸附pH边缘直接与其水解相关:金属离子上的残留电荷越高,pH边缘越低。已使用界面的不同微观或宏观定义(例如,可能包含或不包含矿物学描述的表面络合或离子交换模型)成功地对该过程进行了建模。有机材料对许多金属吸附的影响很大。这种有机材料包括简单的有机分子和通过自然有机物的腐烂而产生的更复杂的外聚合物质(例如腐殖质)。这种有机材料对矿物表面的吸附一直是大量工作的主题。通常,各种类型的有机物质对于矿物表面,特别是对于氧化铁和羟基氧化物,不具有相同的亲和力。如果已经开发出成功的二元系统模型(即金属表面,金属有机表面,有机表面),则混合表面复合物的形成,表面本身的演变以及实验室系统中的添加顺序,以及吸附过程中天然有机物组分的演变,通常排除了在足够宽的参数值范围(即pH值,离子强度,腐殖质浓度)下对金属-表面-有机三元系统的令人满意的描述。该手稿描述了三元系统建模中某些成功和失败的原因。还讨论了有希望的最新进展以及提供对这些复杂系统的更完整描述的可能方法。

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