Download User Manual of the Multicomponent Variably - PC
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46 Table 4.8 Log K parameters for multi-site exchange complex. Yexchanger(1) HY(2) NaY KY MgY2 CaY2 CdY2 PbY2 ZnY2 -1.0 -0.3 -0.4 -0.2 -0.2 0.05 -0.2 HYa HYb HYc HYd HYe HYf 1.65 3.3 4.95 6.85 9.6 12.35 (1) The value for NaY is taken from Appelo et al. (1998). Values for the other complexes are taken from the phreeqc.dat database (Parkhurst and Appelo, 1999) and adapted relative to the K for NaY. (2) Values taken from Appelo et al. (1998). An overview of the considered aqueous equilibrium reactions is given in Table 4.7. The role of chloride as a complexing agent is described by reactions (10) through (13). Other geochemical reactions that are considered are the heterogeneous multi-site ion-exchange reactions. The exchange coefficients for major cations and heavy metals were assumed to be the same for all exchange sites. Table 4.8 gives parameters for this multi-site exchange complex. 4.3.1.2 Database and model input HP1 Chemical reactions and their equilibrium constants are stored in the database phreeqc.dat. The following keywords are used for this problem: SOLUTION_MASTER_SPECIES, SOLUTION_SPECIES, EXCHANGE_MASTER_SPECIES, and EXCHANGE_SPECIES. The input file for water flow and solute transport is relatively straightforward and can be easily created the standard way with the graphical interface of HYDRUS-1D. The problem involves 9 components that are transported, i.e., Na, K, Mg, Ca, Cl, Br, Cd, Zn, and Pb. Only parameters related to solute transport (i.e., the dispersivity and the aqueous diffusion coefficient) are defined in HYDRUS-1D. All other solute transport parameters, except for the Freundlich exponent which is equal to one, are set to zero. This information is stored in the HYDRUS-1D input files Selector.in and Profile.dat. Note that these files also contain information about the steady-state flux (0.05 cm day-1), the boundary concentrations of the nine components in the incoming water, and spatial and temporal discretization parameters of the numerical problem. The link between HYDRUS-1D and PHREEQC is defined in the Species.in input file that contains names of nine elements, the names of which must be the same as in the Phreeqc.dat database. Finally, the initial solutions and exchange complexes are defined in the Phreeqc.in input file. Since the transport problem involves variable water contents with depth, a SOLUTION-keyword needs to be defined for nearly each cell. In addition, the cation exchange complex for each soil layer must be defined using the keyword EXCHANGE, with each layer containing six exchange sites. Also included in the input file are the keywords TRANSPORT to indicate that HYDRUS-1D will be used for transport modelling, and SELECTED_OUTPUT to specify the desired output. Details about the keywords used in Phreeqc.in can be found in the PHREEQC-2 manual (Parkhurst and Appelo, 1999).