|
|
||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Dep. of Soil Science, Univ. of California, Berkeley, CA 94720
*Corresponding author.
ABSTRACT
Recent theoretical and experimental studies of the effect of Cl– ions on Na-Ca and Na-Mg exchange reactions with montmorillonite have produced conflicting data and conceptual models. A discussion is given of three of the key issues involved in this controversy with the objective of posing them more precisely as a guide to future research. The importance of clay mineral suspension characteristics (mineral purification, particle-size fraction, suspension density) is emphasized, and a charge balance condition on the surface excesses of Na+ and CaCl+ or MgCl+ species is pointed out. The role of anion exclusion in generating differences of adsorbed metal charge between Na- and either Ca- or Mg-montmorillonite also is clarified as it relates to exchange reactions in Cl– vs. ClO–4 ionic media.
Received for publication October 18, 1990.
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |
| The SCI Journals | Agronomy Journal | Crop Science | |||
| Vadose Zone Journal | Journal of Plant Registrations | ||||
| Journal of Natural Resources and Life Sciences Education |
Journal of Environmental Quality |
||||