Quick Search:    advanced search

GSW Home   GeoRef Home   My GSW Alerts   Contact GSW   About GSW   Journals List   Help

This Article Figures Only Full Text Full Text (PDF) Alert me when this article is cited Alert me if a correction is posted Citation Map Services Email this article to a friend Similar articles in this journal Alert me to new issues of the journal Download to citation manager Citing Articles Citing Articles via HighWire Citing Articles via Google Scholar Google Scholar Articles by Schulte, K. E. Articles by Germaine, J. T. Search for Related Content GeoRef GeoRef Citation

Testing of Intrinsic Sorptivity for Liquid Infiltration into Initially Dry, Miller- Similar Silica Sands

^a Dep. of Civil Engineering and Engineering Mechanics, Columbia Univ., New York, NY 10027
^b Dep. of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, MA 02139

Correspondence: ^* Corresponding author (culligan{at}civil.columbia.edu).

Received for publication 19 March 2008. The sorptivity (S) of a porous medium quantifies the effect of capillarity and surface forces on liquid infiltration. For infiltration into initially dry soil, S is dependent on three system attributes: the infiltrating liquid properties, the soil properties, and the maximum liquid content behind the infiltration front, _m. Through the use of scaling analyses, a singular, dimensionless value of intrinsic sorptivity (S*) and an accompanying dimensionless Boltzmann transformation (*) were previously derived that are independent of these system attributes for Miller-similar materials. The existence of S* for different infiltrating liquid properties alone were tested by performing a series of experiments that examined the infiltration of either water or the aliphatic oil Soltrol 220 into an initially dry silica sand. This study extended that work to include testing of intrinsic sorptivity for different values of _m and different Miller-similar soils. A series of 57 experiments examined the infiltration of water or Soltrol 220 into two Miller-similar dry silica sands across a range of _m values. The results of these experiments, together with the previous ones, support the existence of S* for the experimental conditions investigated. A singular value of S* can be used to estimate sorptivity values for Miller-similar media for a range of conditions. Likewise, * can be used to generate a similarity profile for normalized liquid content in Miller-similar media for different liquid types and _m values.

Abbreviations: NJFS, New Jersey fine sand • SMC, soil moisture characteristic

This article has been cited by other articles:

				J. R. Nimmo, B. J. Andraski, and R. Munoz-Carpena UZIG USGS Research: Advances through Interdisciplinary Interaction Vadose Zone J., May 21, 2009; 8(2): 411 - 413. [Abstract] [Full Text] [PDF]