5.8 Methods for Calculating Selected Parameters in the Mass Loss Expressions


     The first order decay/degradation coefficient is related to radioactive decay and degradation. The RAAS and MEPAS databases contain decay half lives for radionuclides and degradation half-lives for some non-radioactive contaminants. If values of half lives are available, the decay coefficient is calculated by



     For all volatilization-related calculations, the module uses the modified Henry’s Law constant (unitless). The Henry’s Law constant is obtained from the contaminant database and multiplied to obtain the unitless version by



     The Darcy water flux density may be entered by the user or calculated by the module. The user-entered value can be a single value or a piecewise-constant time series (consisting of an initial value, subsequent values, and the times at which the flux changes to those subsequent values). The module will calculate a Darcy water flux density using monthly climatology data and surface soil data as described in Section 5.1. All the other parameters in the mass flux equations for the leaching pathway are input directly by the user.

     For wind suspension, a value for the wind suspension soil removal rate, S, must be obtained. The user may enter a known constant rate, a known piecewise-constant time series (consisting of an initial value, subsequent values, and the times at which the flux changes to those subsequent values), or let the module calculate the rate. If the user does not enter any known rates, the module will calculate a rate using the methods discussed in Section 5.2.

     For surface water erosion, a value for the water erosion soil removal rate, E, must be obtained. The user may enter a known constant rate, a known piecewise-constant time series (consisting of an initial value, subsequent values, and the times at which the flux changes to those subsequent values), or let the module calculate the rate. If the user does not enter any known rates, the module will calculate a sediment removal rate using the methods discussed in Section 5.3.

     The effective vapor diffusion coefficient in soil is given by


where  is the vapor diffusion coefficient of contaminant i in air (cm2 yr-1).