2004 Denver Annual Meeting (November 7–10, 2004)
Paper No. 169-10
Presentation Time: 4:10 PM-4:25 PM

CALCULATION OF FIRST-ORDER RATE COEFFICIENTS FROM SINGLE-WELL PUSH-PULL TEST DATA

PALMER, Carl D., Geosciences Research, Idaho National Engineering and Environmental Lab, P.O. Box 1625, Idaho Falls, ID 83415-2107, palmcd@inel.gov and STARR, Robert C., North Wind, Inc, P.O. Box 51174, Idaho Falls, ID 83415, bstarr@nwindenv.com

A method for obtaining first-order rate coefficients from push-pull tests is derived. It is more general than previous methods that assume instantaneous injection or use the average concentration in the aquifer at the end of the injection stage. Both the injection and extraction phases are directly incorporated into the solution. A rest phase can be included if there is no significant advection of the slug during the rest stage. The effect of wellbore storage is included by assuming immiscible displacement of the water in the well by the injected or recovered fluid. The decay coefficient within well bore can differ from the decay coefficient in the aquifer. The effects of dispersion are reasonably included by plotting ln[Cd/Cd,0]-ln[Ctr/Ctr,0] versus the time since initiation of extraction where Cd and Cd,0 are the time dependent concentration and the injected concentration of the decaying solute and Ctr and Ctr,0 are the time dependent concentration and the injected concentration of the conservative tracer. There is good agreement between the approximate solution and numerical simulations.

2004 Denver Annual Meeting (November 7–10, 2004)
General Information for this Meeting
Session No. 169
Innovative Tracer Applications in Hydrogeology: New Techniques, Design and Interpretation Methods, and Case Studies II
Colorado Convention Center: 205
1:30 PM-5:30 PM, Tuesday, November 9, 2004

Geological Society of America Abstracts with Programs, Vol. 36, No. 5, p. 396

© Copyright 2004 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.