Abstract

This study investigates the importance of various geoenvironmental conditions such as depth to water table, gas permeability, water-table fluctuations, moisture content, and temperature on the advection and diffusion fluxes of volatile organic compounds (VOCs) from the unsaturated zone to the atmosphere under natural conditions. A one-dimensional gas-flow and organic-vapor transport model was used to simulate vapor fluxes under sinusoidal atmospheric pressure changes with an amplitude of 300 N m-2. The diffusion fluxes were generally greater than the advection fluxes by several orders of magnitude. The thickness of the vadose zone and gas permeability have a relatively significant effect on the advection fluxes at land surface compared to their effect on diffusion fluxes. Increasing the thickness of the vadose zone up to 30 m causes advection fluxes to increase. Increasing the gas permeability of the vadose zone up to 10-12 m2 also increases the advection flux. Further increases of vadose-zone thickness o...

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