SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 20:453-458 (1956)
© 1956 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Swartzendruber, D.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Swartzendruber, D.
Agricola
Right arrow Articles by Swartzendruber, D.

Anomalies in Capillary Intake as Explained by Capillary Rise Experiments1

Dale Swartzendruber2

ABSTRACT

In an earlier study of soil structure, an attempt was made to utilize as a soil structure index, the proportionality constant in the square-root-of-time equation of horizontal capillary flow. In the present paper, anomalous variations of this constant—the capillary absorption coefficient—are considered in greater detail.

As a starting point, the movement of the meniscus in a single round capillary tube was assumed amenable to treatment on the basis of Poiseuille's law. Using data from the literature, it was found that there is validity in the Poiseuille analysis. However, quantitiative agreement with the experiments depended somewhat on the conductivity K of the capillary tube.

The Poiseuille analysis was then utilized in a theoretical treatment of the capillary absorption coefficient, assuming an idealized soil model consisting of parallel, non-interconnected capillary tubes. From the intersection behavior of capillary rise curves, it was found possible to predict within limits the behavior of the capillary absorption coefficient as affected by changes in pore radius, surface tension, wetting angle, and viscosity.

Experimental curves of capillary rise versus time were then obtained for the soils of the previous structure study for which values of capillary absorption coefficient had already been measured. The observed behavior of the coefficient, especially when a large variation was induced in it by a given structure treatment, was found to be consistent with the behavior predicted on the basis of capillary rise curves.

The favorable qualitative comparisons of the capillary tube theory with the experimental data for the soils tested, suggest that the theory can be refined for determining more simply the now difficulty determinable soil physical property—the wetting angle.


NOTES

1 Journal paper No. J-2817 of the Iowa Agr. Exp. Sta., Ames, Iowa, Project No. 1235. Presented before Div. I, Soil Science Society of America, Davis, Calif., August 17, 1955.

2 Formerly Graduate Assistant, Iowa State College, and Assistant Soil Scientist, Agr. Exp. Sta., Univ. of California, Los Angeles, where paper was prepared. Presently Associate Professor of Soils, Purdue University, Lafayette, Indiana.

Received for publication October 17, 1955.





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1956 by the Soil Science Society of America.