SSSAJ Journal of Natural Resources and Life Sciences Education
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Published in Soil Sci Soc Am J 42:688-693 (1978)
© 1978 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Relation Between Rheological Properties and Dry-state b Dimension of Various Na-smectites1

J. F. Margheim and P. F. Low2

ABSTRACT

The liquid limits of pastes of five different Na-smectites were determined with the conventional liquid-limit device. In addition, the penetration rate of a Teflon cone into each paste was determined at different water contents by means of a precision penetrometer. The water content at which a curve of penetration rate versus water content showed maximal curvature was called the "critical" water content. Both the liquid limit and "critical" water content were shown to decrease as the b dimension of the Na-smectite increased. Since recent work has shown that the specific surface area of a Na-smectite depends on its dry-state b dimension, plots were made of the liquid limit and critical water content against specific surface area. They showed that both indicators of consistency increased curvilinearly with specific surface area. However, at a given state of consistency, the interparticle distance was not the same in the different smectite-water systems but depended on the b dimension. Reasons for these findings were discussed in relation to the theory of plastic flow.


NOTES

1 Journal Paper no. 6782; contribution of the Dept. of Agron., Purdue Univ., Agr. Exp. Sta., West Lafayette, IN, 47907.

2 Former Graduate Research Assistant and Professor of Agron., Purdue Univ., respectively.

Received for publication July 11, 1977. Accepted for publication May 25, 1978.







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