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Attachment, detachment and inactivation rate coefficients were determined from fitting breakthrough curves.
Successful simulaThens of field desorption data reported by Bahr [J. Contam. Hydrol. 4 (1989) 205] further demonstrate the potential applicoefficient the developed relatinnships.
The multirate mass transfer model was capable of jointly fitting breakthrough curve behavior, showing the effectiveness and flexibility for incorporating aquifer heterogeneity and scale effects in upscaling effective mass transfer models.
Transport and degradation parameters obtained using the MOM were compared to parameters obtained by fitting breakthrough data from an advective dispersive transport model with equilibrium sorption and first-order degradation, using the nonlinear least-square curve-fitting program CXTFIT.
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We found that the MOM fitted breakthrough curves with tailing better than curve fitting.
Physical nonequilibrium models to fit breakthrough curves for tracer tests in solution conduits are now routinely employed.
We found a good agreement between observed and fitted breakthrough curves (BTCs) under both saturated and unsaturated conditions.
Using the fracture network transport model, the most probable representation and the hydrologic parameters of the fracture network can be estimated by fitting the breakthrough of uranine.
A two-dimensional porous medium approach was successfully used to fit tracer breakthrough curves measured for a dipole experiment.
Thomas and Bohart Adams models were successfully fitted with breakthrough curves obtained under different experimental conditions in a continuous column process.
An analytical solution for a model consisting of two possible cavity geometries is fit to breakthrough curves from sediment wash-off experiments.
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