Rozalén Marisa, Brady Patrick V, Huertas F Javier
Geochemistry Research, Sandia National Laboratories, Albuquerque, MS-0754, NM 87185, USA.
J Colloid Interface Sci. 2009 May 15;333(2):474-84. doi: 10.1016/j.jcis.2009.01.059. Epub 2009 Jan 31.
The surface chemistry of K-montmorillonite was investigated by potentiometric titrations conducted at 25, 50 and 70 degrees C and at ionic strengths of 0.001, 0.01 and 0.1 M KNO(3). Proton adsorption decreases with electrolyte concentration at all pHs. The pH of zero net proton charge (PZNPC) decreases from 8.1 to 7.6 when the ionic strength increases from 0.001 to 0.1 M. Temperature has a very small effect on surface charge. A constant capacitance model that accounts for protonation/deprotonation of aluminol and silanol edge sites and basal plane H(+)/K(+) exchange is used to fit the experimental data. H(+) and OH(-) adsorption to specific surface sites appear to account for the pH-dependence of the K-montmorillonite dissolution.
通过在25、50和70摄氏度以及0.001、0.01和0.1 M硝酸钾离子强度下进行的电位滴定,研究了钾蒙脱石的表面化学性质。在所有pH值下,质子吸附量随电解质浓度的增加而降低。当离子强度从0.001 M增加到0.1 M时,零净质子电荷(PZNPC)的pH值从8.1降至7.6。温度对表面电荷的影响非常小。使用一个考虑了铝醇和硅醇边缘位点的质子化/去质子化以及基面H(+)/K(+)交换的恒电容模型来拟合实验数据。H(+)和OH(-)在特定表面位点的吸附似乎解释了钾蒙脱石溶解的pH依赖性。