Here is a file I made to perform case C (first-order reversible) in a simple advective transport case. The concentrations S in your table are moles per kg solid, but are in units of moles/kgw in PHREEQC, which removes the factors theta/ro from the equations. The example has a Kd of 10 (= S/C) and a forward rate constant of 1/day. The backward rate constant is found from Kd = kf/kr. You may have a problem if you have a big discrepancy between kf and the time step, for example seconds for kf and years for transport time steps. In this case, you should probably use equilibrium sorption. My example has kf = 1/day and time steps of days. David (See attached file: kinsorb.pqi) David Parkhurst (dlpark@xxxxxxxx) U.S. Geological Survey Box 25046, MS 413 Denver Federal Center Denver, CO 80225 Alan H Welch To: David L Parkhurst/WRD/USGS/DOI@xxxx 09/11/01 10:43 cc: Lawrence S Feinson/WRD/USGS/DOI@xxxx, Kenneth G AM Stollenwerk/WRD/USGS/DOI@xxxx In-Reply-To: <OF834F57B7.B3127FCD-ON88256AC4.005AC381@xxxxxxxx> Subject: Adsorption kinetics in phreeqc David, I am interested in modeling arsenic adsorption kinetics (on iron oxide) using phreeqc. Do you have an example of how to code adsorption kinetics? The rate model and symbols for the equations are in the attachments. Thanks for the help. (See attached file: rate.bmp)(See attached file: rate.symbol.bmp) Best regards, Alan Welch U.S.Geological Survey 333 W. Nye Lane Carson City, NV 89706 Office: (775) 887-7609 FAX: (775) 887-7629 ahwelch@xxxxxxxx
Attachment:
kinsorb.pqi
Description: Binary data
Attachment:
rate.bmp
Description: Binary data
Attachment:
rate.symbol.bmp
Description: Binary data
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