溶解铝在蓝宝石c和高岭石上的吸附:对粘土矿物零电荷点的影响

IF 0.9 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS Geochemical Transactions Pub Date : 2014-06-19 DOI:10.1186/1467-4866-15-9
Johannes Lützenkirchen, Ahmed Abdelmonem, Rohan Weerasooriya, Frank Heberling, Volker Metz, Remi Marsac
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引用次数: 34

摘要

研究了溶铝对刚玉和高岭石两种含铝矿物界面性能的影响。通过流动电位测量和pH值对蓝宝石基面电动势的影响,研究了有意添加溶解铝对蓝宝石基面电动势的影响,并在pH值为6时进行了二次谐波生成(SHG)研究。电动力学数据显示出与SHG数据相似的趋势,表明SHG电场与ζ电位相关。对高岭石颗粒进行了类似的研究。在这种情况下,电泳迁移率被测量为ph的函数。在两种系统中,溶解铝的加入引起了充电行为的显著变化。等电点始终向更高的pH值移动,移动的程度取决于铝的存在或添加量。实验结果表明,公布的粘土矿物等电点可能受到这一现象的影响。在实验研究中,溶解铝的存在可能是由特定的预处理方法引起的(如在酸中洗涤和随后吸附溶解铝),或者甚至仅仅是通过从极端pH值开始一系列测量(导致溶解),然后在同一批中改变pH值。这导致溶解的铝与目标表面的相互作用。对实验结果的一种可能解释是,在低铝浓度下,铝的附着原子(我们将吸附的矿物成分称为附着原子)可以在蓝宝石基面上形成,并且可以很容易地去除。同时,一旦表面暴露在足够高的铝浓度下,AFM就会看到表面的明显变化,这是由于在当前研究中使用的条件下无法去除的表面沉淀。总之,只要预处理或实验起点有利于铝的溶解,溶解的铝就可能留在实验体系中并与目标表面相互作用。系统不再是原始的,零电荷点或吸收数据是那些含铝系统。
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Adsorption of dissolved aluminum on sapphire-c and kaolinite: implications for points of zero charge of clay minerals

We have studied the impact of dissolved aluminum on interfacial properties of two aluminum bearing minerals, corundum and kaolinite. The effect of intentionally adding dissolved aluminum on electrokinetic potential of basal plane surfaces of sapphire was studied by streaming potential measurements as a function of pH and was complemented by a second harmonic generation (SHG) study at pH?6. The electrokinetic data show a similar trend as the SHG data, suggesting that the SHG electric field correlates to zeta-potential. A comparable study was carried out on kaolinite particles. In this case electrophoretic mobility was measured as a function of pH. In both systems the addition of dissolved aluminum caused significant changes in the charging behavior. The isoelectric point consistently shifted to higher pH values, the extent of the shift depending on the amount of aluminum present or added. The experimental results imply that published isoelectric points of clay minerals may have been affected by this phenomenon. The presence of dissolved aluminum in experimental studies may be caused by particular pre-treatment methods (such as washing in acids and subsequent adsorption of dissolved aluminum) or even simply by starting a series of measurements from extreme pH (causing dissolution), and subsequently varying the pH in the very same batch. This results in interactions of dissolved aluminum with the target surface.

A possible interpretation of the experimental results could be that at low aluminum concentrations adatoms of aluminum (we will refer to adsorbed mineral constituents as adatoms) can form at the sapphire basal plane, which can be rather easily removed. Simultaneously, once the surface has been exposed to sufficiently high aluminum concentration, a visible change of the surface is seen by AFM which is attributed to a surface precipitate that cannot be removed under the conditions employed in the current study.

In conclusion, whenever pre-treatment or the starting point of an experiment favor the dissolution of aluminum, dissolved Al may remain in the experimental system and interact with the target surfaces. The systems are then no longer pristine and points of zero charge or sorption data are those of aluminum-bearing systems.

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来源期刊
Geochemical Transactions
Geochemical Transactions 地学-地球化学与地球物理
CiteScore
3.70
自引率
4.30%
发文量
2
审稿时长
>12 weeks
期刊介绍: Geochemical Transactions publishes high-quality research in all areas of chemistry as it relates to materials and processes occurring in terrestrial and extraterrestrial systems.
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