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Volatile Organic Vapor Diffusion and Adsorption in Soils
Author(s) -
Petersen L. W.,
Rolston D. E.,
Moldrup P.,
Yamaguchi T.
Publication year - 1994
Publication title -
journal of environmental quality
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.888
H-Index - 171
eISSN - 1537-2537
pISSN - 0047-2425
DOI - 10.2134/jeq1994.00472425002300040026x
Subject(s) - chemistry , soil water , partition coefficient , sorption , adsorption , diffusion , water vapor , loam , toluene , analytical chemistry (journal) , aqueous solution , environmental chemistry , thermodynamics , soil science , chromatography , organic chemistry , physics , environmental science
Knowledge of the relationship between D P / D 0 (diffusion coefficient in soil divided by diffusion coefficient in free air) and the volumetric soil‐air content, ɛ, is important when modeling gaseous movement of volatile organic compounds (VOCs) in soils. The effective diffusion (i.e., diffusion and retardation) of trichloroethylene (TCE), toluene and freon in Yolo silt loam (fine‐silty, mixed, nonacid, thermic Typic Xerorthent) were measured in a two‐chamber diffusion apparatus. The experiments were conducted on packed soil cores over a range of water contents. Vapor retardation factors were calculated from soil parameters and equilibrium partition coefficients. Partition coefficients were measured in batch experiments. It was found that for water contents higher than four molecular layers of water surface coverage, solid/vapor partition coefficients, K D ′, were consistent with values predicted by Henry's Law constants ( K H ), and aqueous/solid partition coefficients, K D . For less than four molecular layers of water, sorption increased by orders of magnitude. The vapor retardation factors, along with the measured effective diffusion, allowed a calculation of diffusion coefficients ( D P ) for the investigated species by using the analytical solution to diffusion in a two‐chamber apparatus. Values of the ratio D P / D 0 were generally higher than the values predicted by the Millington‐Quirk equation, and lower than the values predicted by the Penman equation. Compared with the nonreactive tracer freon, D P / D 0 values for TCE and toluene agreed very well for higher water contents. Values obtained for air‐dry soil, however, were under‐predicted. The experimental work for determination of the effective diffusion of reactive tracers can, therefore, for sufficiently high water contents be limited to the determination of D p / D 0 ‐ɛ relations for a nonreactive tracer and measurement of K D , K D ′, and K H values for the reactive tracers.