Hostname: page-component-848d4c4894-hfldf Total loading time: 0 Render date: 2024-05-23T09:54:06.693Z Has data issue: false hasContentIssue false

Current research work on the clay minerals at the University of Granada, Spain

Published online by Cambridge University Press:  14 March 2018

Get access

Extract

These authors are studying the influence of pH and particle size on sedimentation volume, and on the velocity with which it is reached. They are using fractions from > 1.2 μ to < 0.3 μ, obtained by sedimentation, and buffer solutions of pH 1, 3, 5, 7, 8, 9, 10, as well as distilled water. For all pH's the volume of sedimentation and the time taken to attain it rise with decreasing particle size. For a given fraction the volume of sedimentation rises in the pH's near neutrality (7 and 8) and in distilled water, depending partly on the ions present, their nature and concentration, in the buffering solutions employed. The thixotropy and the base exchange capacity rise parallel with the sedimentation volume.

Type
Research Article
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1947

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)