Comparison of isoelectric points of single-crystal and polycrystalline α-Al2O3 and α-Fe2O3 surfaces

被引:19
|
作者
Wang, Yingge [1 ]
Persson, Per [2 ,3 ]
Michel, F. Marc [4 ,5 ,6 ]
Brown, Gordon E., Jr. [1 ,4 ,5 ]
机构
[1] Stanford Univ, Sch Earth Energy & Environm Sci, Dept Geol Sci, Surface & Aqueous Geochem Grp, Stanford, CA 94305 USA
[2] Lund Univ, Ctr Environm & Climate Res, SE-22362 Lund, Sweden
[3] Lund Univ, Dept Biol, SE-22362 Lund, Sweden
[4] SLAC Natl Accelerator Lab, Dept Photon Sci, 2575 Sand Hill Rd,MS 69, Menlo Pk, CA 94025 USA
[5] SLAC Natl Accelerator Lab, Stanford Synchrotron Radiat Lightsource, 2575 Sand Hill Rd,MS 69, Menlo Pk, CA 94025 USA
[6] Virginia Tech, Dept Geosci, Blacksburg, VA 24061 USA
基金
瑞典研究理事会;
关键词
Isoelectric point (IEP); pH point of zero charge (pH(PZC)); Fe- and Al-oxides; single crystal; polycrystalline; surface; defects; OPTICAL 2ND-HARMONIC GENERATION; ATOMIC-FORCE MICROSCOPY; IRON-OXIDE; WATER INTERFACE; ALPHA-ALUMINA; ZERO CHARGE; COMPETITIVE ADSORPTION; ELECTROLYTE INTERFACE; AMBIENT CONDITIONS; ORGANIC-MATTER;
D O I
10.2138/am-2016-5531
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 surface charging behavior as a function of pH and isoelectric points (IEPs) of single-crystal alpha-Al2O3 (0001) and (1 (1) over bar 02) and alpha-Fe2O3 (0001) was determined by streaming potential measurements using an electrokinetic analyzer. The IEPs of alpha-Al2O3 (0001) and (1 (1) over bar 02) and alpha-Fe2O3 (0001) were found to be 4.5, 5.1, and 6.5, respectively. These IEP values for oriented single crystals of alpha-Al2O3 are in good agreement with literature values, whereas the new IEP value for alpha-Fe2O3 (0001) is significantly lower than four reported values (IEP = 8-8.5) for single-crystal alpha-Fe2O3 (0001) (Eggleston and Jordan 1998; Zarzycki et al. 2011; Chatman et al. 2013; Ltitzenkirchen et al. 2013) and significantly higher than one (IEP = 4) recently measured by Lfltzenkirchen et al. (2015) on a fresh alpha-Fe2O3 (0001) surface. Most of the single-crystal IEP values measured recently are lower than IEP values reported for polycrystalline alpha-Al2O3 and alpha-Fe2O3, which are generally in the pH range of 8 to 10. Calculations of the IEP values based on estimated K-a values of alpha-Fe2O3 and alpha-Al2O3 surfaces in contact with water as a function of defect type and concentration suggest that highly reactive surface defect sites (primarily singly coordinated aquo groups) on the Fe- and Al-oxide powders are possibly a major source of the surface charge differences between polycrystalline samples and their oriented single-crystal counterparts studied here. The results of this study provide a better understanding of the surface charging behavior of Fe and Al-oxides, which is essential for predicting complex processes such as metal-ion sorption occurring at mineral/water interfaces.
引用
收藏
页码:2248 / 2259
页数:12
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