SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 39:1049-1053 (1975)
© 1975 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 Philip, J. R.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Philip, J. R.
Agricola
Right arrow Articles by Philip, J. R.

The Growth of Disturbances in Unstable Infiltration Flows1

J. R. Philip2

ABSTRACT

The stability analysis of the delta-function model of infiltration yields a maximum wave-number for unstable disturbances, Mcrit, and a wave-number for maximum amplification, M*. The "column effect," i.e. the suppression of instability in laboratory columns, depends on Mcrit; and the dimensions of fingers in unstable flows can be expected to depend on M*. When instability is induced by a sudden jump of G, the water pressure gradient behind the wetting front, Mcrit and M* may be evaluated simply and directly. When, on the other hand, instability emerges during gradual increase of G, it is necessary to study the amplification of disturbances during the whole course of increase of G through positive values.

Such a study is made for one example of instability induced by air compression and for one where it is induced by increase of conductivity with depth. Both exhibit qualitatively similar patterns of amplification: disturbances of small M (wave-number) begin to be amplified sooner, but are ultimately overtaken by some disturbances of larger M starting later. Definite values of M* are found, and the results discussed with special reference to fingering and to the column effect.


NOTES

1 Contribution from CSIRO, Australia.

2 Chief, CSIRO Division of Environmental Mechanics, P.O. Box 821, Canberra City, A.C.T. 2601, Australia.

Received for publication March 21, 1975. Accepted for publication June 20, 1975.







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
Copyright © 1975 by the Soil Science Society of America.