|
|
||||||||
ABSTRACT
The kinetics of Ca-montmorillonite tactoid formation and breakdown was followed by recording the changes in light transmission as a function of time when Ca-montmorillonite suspensions of 0.05% (w/v) concentration were added to Na-montmorillonite suspensions of the same concentration in a titrating vessel placed in the light path of a spectrophotometer. Tactoid formation was found to be instantaneous whereas the breakdown of Ca tactoids took about 10 min. It was suggested that the initial step upon mixing sodium and calcium montmorillonite was the redistribution of adsorbed ions. For tactoids to break, ions have to interdiffuse into the tactoids. Since the mobility of ions adsorbed on the internal surfaces is low, tactoid breakdown is slow. Ion diffusion on the single platelets of Na clay and the external surfaces of the tactoids is high; thus the formation of tactoids is instantaneous.
1 Contribution from the Department of Soil Mechanics, Negev Institute for Arid Zone Research, Beer-Sheva, Israel.
2 Senior Soil Scientist and Soil Scientist, respectively, Negev Institute for Arid Zone Research.
Received for publication December 27, 1968. Accepted for publication February 11, 1969.
| 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 |
||||