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Roberts, P. , Goltz, M. , and MacKay, D. , “A Natural Gradient Experiment on Solute Transport in a Sand Aquifer 3. Retardation Estimates and Mass Balances for Organic Solutes,” Water Resources Research, 2047, 1986. Sims, R. , “Soil Remediation Techniques at Uncontrolled Hazardous Waste Sites, A Critical Review,” J. Air & Waste Management Association, 40, 5, 1990. E. , Journal of Contaminant Hydrogeology, 4, 181, 1989. C01 Page 40 Thursday, November 2, 2000 3:29 PM C02 Page 41 Tuesday, October 31, 2000 4:29 AM CHAPTER 2 Lifecycle Design Evan K.
26 M). (Roberts, Goltz, and MacKay, 1986. ) The tails in this study were created in a homogeneous, sand aquifer over a 5meter sampling area. Due to the nature of the aquifer and the short distances, the effect from diffusion will be minor compared to retardation. As the aquifer becomes less homogeneous, the tails of concentration will lengthen. One final note before we leave retardation. The same properties that can slow the movement of contaminants in an aquifer can also combine to speed the movement of the contaminants.
Soluble constituents dissolved in the groundwater. Volatile constituents in the soil pore space of the vadose zone. All four phases are in equilibrium. Air or water as the carrier must interact with these phases in order to remove the mass from the ground. The air can come into direct contact with NAPL when it is in the free phase or adsorbed to the soil. The organic compounds can directly volatilize into the air from the NAPL. If the NAPL is located in one of the main flow paths of the air, then the organic will be directly removed from the ground.