Abstract. This paper addresses an experimental and theoretical study of sorbed contaminant removal from a column (or reactor) by flushing. This removal may take place by either volatilization or rinsing, and nonlinear sorption is accounted for by employing a Freundlich relationship. A one-dimensional nonequilibrium transport model is proposed which describes the unsteady mass transfer between flushing medium and soil phases in the column, using a linear chemical transfer model. The moving boundary problem is transferred, and a perturbation method is employed to obtain an approximate solution of the governing equations for a small Merkel number Me (this dimensionless number comprises the product of fluid residence time and the mass transfer coefficient). The solution reveals the effect of the various parameters, such as the Freundlich parameter n, on the contaminant transport in fluid phase and decay in solid phase. Applying the model to various experimental data results in values for the overall mass transfer coefficients, which are useful for engineering computations. Furthermore, the model enables the prediction of the initial soil contamination level as well as the parameter n solely from the measured exit contaminant concentrations in the flushing fluid. A thorough comparison of this prediction with the measured soil concentration (prior to the experiments) yields good agreement.
IntroductionIn order to optimize real-scale soil remediation processes, conceptual models are in use and in development. As some soil parameters are very hard or nearly impossible to assess theoretically, often bench-scale experiments are performed to investigate the feasibility of a cleaning technique. For these experiments, columns are usually used; the columns are flushed in the axial direction. Relevant experimental conditions, such as flushing velocity, flushing medium, additives, etc., can be varied, and their effect can be evaluated.Current transport models often start from nonequilibrium between contaminant in the soil and flushing fluid. As a result of this nonequilibrium, contaminant is desorbed from the soil, transferred to the flushing fluid, and removed by convective transport. In an early publication, Lapidus and Amundson [1952] equilibrium between soil and fluid phases, (2) start-up phase, (3) desorption of the contaminant, using a Freundlich isotherm, and (4) convective transport and decay of soil contamination concentration. These features are typical for flushing and remediation of soil in practice. For engineering end purposes it is of major importance to derive basic models and obtain compact analytical solutions that (1) reveal the principle prevailing phenomena of the process, (2) permit a straightforward fit with experimental data, and (3) validate more advanced numerical models. Accordingly, such an analysis has been executed and is presented here in detail. C(x = x(t), t) =Equation ( and the right-hand sides of (1) and (2) remain the same (with H set equal to unity). Hence (1) and (2) are generally applica...