CESIUM-ADSORPTION METHOD FOR MEASURING ACCESSIBLE STRUCTURAL SURFACE-CHARGE

被引:112
作者
ANDERSON, SJ [1 ]
SPOSITO, G [1 ]
机构
[1] UNIV CALIF BERKELEY, DEPT SOIL SCI, BERKELEY, CA 94720 USA
关键词
D O I
10.2136/sssaj1991.03615995005500060011x
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Measurements of the separate contributions of structural and pH-dependent charge are essential to understanding and predicting surface-chemical reactions in soils and other heterogeneous adsorbents that contain a mixture of surface functional groups. An ion-adsorption method was developed to measure the accessible structural charge density (sigma(0)) in adsorbents that comprise both structural-charge and variable-charge surface functional groups. The method is based on the preference of siloxane surface sites for Cs+ over Li+ and on the much lower selectivity of ionizable surface groups for Cs+. To estimate sigma(0), CsCl-saturated adsorbents were reacted with 0.05 mol CsCl kg-1 at pH 7, washed with ethanol to reduce the entrained CsCl concentration, dried at 65-degrees-C to promote the formation of inner-sphere surface complexes between Cs+ and permanent-charge sites, and then extracted with 0.01 mol LiCl kg-1 to displace Cs+ from variable-charge adsorption sites, which exhibit little or no preference for Cs+ over Li+. Finally, Cs+ was displaced from permanent-charge sites by repeated NH4OAc extraction until no Cs was present in the equilibrium supernatant solution. According to this method, sigma(0) represented about 85 and 70% of the accessible cation-adsorption sites at pH 7 on < 2-mu-m Wyoming montmorillonite and < 106-mu-m Silver Hill Illite, respectively; 15% and 30%, respectively, were variable-charge sites. These results were consistent with published reports of the amount of pH-dependent cation adsorption on montmorillonite and with model calculations of the relative contributions of edge and structural charge in montmorillonite and illite. When the method was used to measure Cs-accessible sigma(0) in four soils, the percentage of structural charge ranged from 1% in an Oxisol to 65% in an Alfisol. The method is appropriate for adsorbents that contain montmorillonite, illite, and repotassified (nonexpandable) vermiculite. It may be suitable for adsorbents that contain clay-sized, but probably not coarse-grained, expandable vermiculite.
引用
收藏
页码:1569 / 1576
页数:8
相关论文
共 65 条
  • [1] ANDERSON SJ, 1989, THESIS U CALIFORNIA
  • [2] STUDY OF SOME PHYSICOCHEMICAL PROPERTIES OF PILLARED MONTMORILLONITES - ACID-BASE POTENTIOMETRIC TITRATIONS AND ELECTROPHORETIC MEASUREMENTS
    AVENA, MJ
    CABROL, R
    DEPAULI, CP
    [J]. CLAYS AND CLAY MINERALS, 1990, 38 (04) : 356 - 362
  • [3] OBJECTIVE METHOD FOR FITTING MODELS OF ION ADSORPTION ON VARIABLE CHARGE SURFACES
    BARROW, NJ
    BOWDEN, JW
    POSNER, AM
    QUIRK, JP
    [J]. AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1980, 18 (01): : 37 - 47
  • [4] BARSHAD I, 1948, AM MINERAL, V33, P655
  • [5] SURFACE-CHARGE ON KAOLINITES IN AQUEOUS SUSPENSION
    BOLLAND, MDA
    POSNER, AM
    QUIRK, JP
    [J]. AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1976, 14 (02): : 197 - 216
  • [6] BOLT G. H., 1963, SOIL SCI SOC AMER PROC, V27, P294
  • [7] Brindley G.W., 1980, CRYSTAL STRUCTURES C
  • [8] CESIUM AND RUBIDIUM ION EQUILIBRIA IN ILLITE CLAY
    BROUWER, E
    BAEYENS, B
    MAES, A
    CREMERS, A
    [J]. JOURNAL OF PHYSICAL CHEMISTRY, 1983, 87 (07) : 1213 - 1219
  • [9] NEUTRON-DIFFRACTION STUDIES ON LITHIUM MONTMORILLONITE-WATER DISPERSIONS
    CEBULA, DJ
    OTTEWILL, RH
    [J]. CLAYS AND CLAY MINERALS, 1981, 29 (01) : 73 - 75
  • [10] MONO-VALENT ION ADSORPTION BY AN OXISOL
    CHARLET, L
    SPOSITO, G
    [J]. SOIL SCIENCE SOCIETY OF AMERICA JOURNAL, 1987, 51 (05) : 1155 - 1160