Surface charge of variable porosity Al2O3(s) and SiO2(s) adsorbents

被引:79
作者
Goyne, KW [1 ]
Zimmerman, AR
Newalkar, BL
Komarneni, S
Brantley, SL
Chorover, J
机构
[1] Penn State Univ, Dept Crop & Soil Sci, University Pk, PA 16802 USA
[2] Univ Arizona, Dept Soil Water & Environm Sci, Tucson, AZ 85721 USA
[3] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA
[4] Penn State Univ, Mat Res Lab, University Pk, PA 16802 USA
基金
美国国家科学基金会;
关键词
surface charge; proton adsorption; ion adsorption; site density; alumina; silica; p.z.n.p.c;
D O I
10.1023/A:1021631827398
中图分类号
O69 [应用化学];
学科分类号
081704 ;
摘要
The surface charge properties of two SiO2 and three Al2O3 mineral adsorbents with varying degrees of framework porosity were investigated using discontinuous titration and ion adsorption methodologies. Points of zero net charge (p.z.n.c) for porous and non-porous SiO2 were < 2.82 and for Al2O3 minerals ranged from 6.47-6.87. Silica surfaces possessed very slight negative charge in the acid pH range (pH < 7) and significant dissociation of silanol groups occurred at pH > 7. Variation of surface charge density with aqueous proton concentration was nearly identical within a mineral type (i.e., SiO2 or Al2O3) irrespective of the degree of framework porosity, indicating that the densities of dissociable surface sites are equivalent, when normalized to surface area. The results suggest that the use of titration methods alone may be insufficient for thorough surface charge characterization, particularly at low and high pH. Proton titrations should be coupled with concurrent ion adsorption measurements to confirm surface charge development. Discontinuous proton titration and ion adsorption data, which were in agreement in the slightly acidic through slightly basic pH range, both indicated that p.z.n.c. was equal to the point of zero net proton charge (p.z.n.p.c.) for the variable charge minerals investigated.
引用
收藏
页码:243 / 256
页数:14
相关论文
共 40 条
[1]  
[Anonymous], 2022, INFRARED SPECTRA MIN, DOI DOI 10.1180/MONO-4.16
[2]   THE DETERMINATION OF PORE VOLUME AND AREA DISTRIBUTIONS IN POROUS SUBSTANCES .1. COMPUTATIONS FROM NITROGEN ISOTHERMS [J].
BARRETT, EP ;
JOYNER, LG ;
HALENDA, PP .
JOURNAL OF THE AMERICAN CHEMICAL SOCIETY, 1951, 73 (01) :373-380
[3]   CONTROLS ON SILICATE DISSOLUTION RATES IN NEUTRAL AND BASIC PH SOLUTIONS AT 25-DEGREES-C [J].
BRADY, PV ;
WALTHER, JV .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1989, 53 (11) :2823-2830
[4]  
Brunauer S., 1943, ADSORPTION GASES VAP, V1
[5]   SURFACE-CHARGE CHARACTERISTICS OF KAOLINITIC TROPICAL SOILS [J].
CHOROVER, J ;
SPOSITO, G .
GEOCHIMICA ET COSMOCHIMICA ACTA, 1995, 59 (05) :875-884
[6]   STRUCTURE OF OXIDE GELS AND GLASSES BY INFRARED AND RAMAN-SCATTERING .1. ALUMINA [J].
COLOMBAN, P .
JOURNAL OF MATERIALS SCIENCE, 1989, 24 (08) :3002-3010
[7]  
Conway J. H., 1993, SPHERE PACKINGS LATT
[8]  
Goldberg S., 1996, The environmental chemistry of aluminum, V2nd, P271
[9]  
GOYNE KW, 2001, 11 ANN VM GOLDSCHM C
[10]   PHYSICAL ADSORPTION ON NON-UNIFORM SURFACES [J].
HALSEY, G .
JOURNAL OF CHEMICAL PHYSICS, 1948, 16 (10) :931-937