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Johnson and Ettinger Attenuation Factor



The attenuation factor, α, is a proportionality constant relating indoor air concentrations to soil or groundwater concentrations:

Cindoor air = αSG x Csoil gas   or   Cindoor air = αGW x Cgroundwater x H

This attenuation of vapor phase concentrations from the subsurface to indoor air can be computed by the simplified Johnson and Ettinger (1991) relationship:

A larger α indicates less attenuation and a smaller value indicates more attenuation. For example, at an α = 0.001 a subsurface concentration of 1000 [μg/m3] will attenuate to an indoor air concentration of 1 [μg/m3]. At an α = 0.1, the same subsurface concentration of 1000 [μg/m3] will only attenuate to an indoor air concentration of 100 [μg/m3]. Note that different attenuation factors will be produced for soil gas and groundwater contamination sources (because of different DTeff values as explained below).


Building Terms:



Subsurface Terms:
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Page author: Fred Tillman (National Research Council), of U.S. EPA, Office of Research and Development, Athens Georgia who last modified this content on: September 21, 2004


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