A new approach to pH of point of zero charge measurement: Crystal-face specificity by scanning force microscopy (SFM)

被引:54
作者
Eggleston, CM [1 ]
Jordan, G [1 ]
机构
[1] Univ Wyoming, Dept Geol & Geophys, Laramie, WY 82071 USA
关键词
D O I
10.1016/S0016-7037(98)00119-7
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
The pH of point of zero charge (pH(pzc)) is a fundamentally important property used in modeling the interaction of solid surfaces with aqueous solutions and solutes. The pH(pzc) is normally measured by acid-base titration of solid suspensions. Here, a scanning force microscope (SFM) is used to measure forces of repulsion or attraction between chemically tailored tips and quartz (101) and hematite (001) surfaces, as a function of tip-surface separation and pH. The force at contact (FAC) is at a minimum near the expected point of pH(pzc) for a chemically similar tip and sample. The results are compared to predicted interaction forces from a simple DLVO model, which shows that the SFM technique for pH(pzc) measurement is most promising for surfaces (such as iron oxides) that have not-too-widely spaced pK(a1) and pK(a2) values for surface site deprotonation. However, improvements in precision will be necessary to fully utilize the technique. The SFM approach to pH(pzc) measurement may in future allow the measurement of crystal-face-specific pH(pzc), rather than a weighted average of all exposed surface sites, and thus allow us to ask better-defined structure-reactivity questions for mineral surfaces. The approach can in theory be extended to the single-site scale in order to probe the properties (e.g., potential and charge) of individual terrace, step, or kink sites. Copyright (C) 1998 Elsevier Science Ltd.
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页码:1919 / 1923
页数:5
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