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AGU: Water Resources Research

 
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Abstract

An Updated Model of Induced Airflow in the Unsaturated Zone

Arthur L. Baehr

U.S. Geological Survey, West Trenton, New Jersey

Craig J. Joss

Department of Civil Engineering, Drexel University, Philadelphia, Pennsylvania

Simulation of induced movement of air in the unsaturated zone provides a method to determine permeability and to design vapor extraction remediation systems. A previously published solution to the airflow equation for the case in which the unsaturated zone is separated from the atmosphere by a layer of lower permeability (such as a clay layer) has been superseded. The new solution simulates airflow through the layer of lower permeability more rigorously by defining the leakage in terms of the upper boundary condition rather than by adding a leakage term to the governing airflow equation. This note presents the derivation of the new solution. Formulas for steady state pressure, specific discharge, and mass flow in the domain are obtained for the new model and for the case in which the unsaturated zone is in direct contact with the atmosphere.

Received 10 February 1994; accepted 15 September 1994; .

Citation: Baehr, A. L., and C. J. Joss (1995), An Updated Model of Induced Airflow in the Unsaturated Zone, Water Resour. Res., 31(2), 417–421.

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