|
|
||||||||
| ||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Soil, Water and Environmental Science Dep., Mark L. Brusseau, Hydrology and Water Resources Dep., 429 Shantz Building, #38, The Univ. of Arizona, Tucson, AZ 85721
* Corresponding author (brusseau{at}ag.arizona.edu)
Received 28 October 2004.
Gas-phase partitioning tracer tests were conducted to measure water content for several porous media with different mean particle diameters and particle-size distributions. Methane was used as the nonreactive tracer and difluoromethane was used as the water-partitioning tracer. Water contents determined from the tracer-test results were similar to values measured gravimetrically. These results support the utility of the gas-phase tracer method for measuring water content in a variety of porous media.
Abbreviations: DFM, diflouromethane U, uniformity coefficients
| HOME | HELP | FEEDBACK | SUBSCRIPTIONS | ARCHIVE | SEARCH | TABLE OF CONTENTS |