David-- Thank you, I appreciate your taking time to answer my questions. A final one (hopefully) -- QUESTION: I appreciate the role of kinetics. However, assuming that kinetics are not an issue, how can I best apply PHREEQC to determine, at equlibirum, what remains in solution and what (eventually) precipitates - for a given a water quality? Thank you, Mike ------------------------- Mickley & Associates 752 Gapter Road Boulder, Colorado 80303 303-499-3133 fax 303-499-5305 www.mickleyassoc.com ----- Original Message ----- From: "David L Parkhurst" <dlpark@xxxxxxxx> To: "Mike Mickley" <michael@xxxxxxxxxxxxxxxx> Sent: Monday, August 18, 2003 8:18 AM Subject: Re: trouble downloading PHREEQC for Windows > > > > > QUESTION 1: would you recommend software to use at higher salinities? > EQ3/6 or something else? > > You need a program that includes the Pitzer formulation for activities to > run at higher ionic strengths. EQ3/6, Geochemists Workbench, and TEQUIL > (though I have never successfully downloaded this code) include or are > based on the Pitzer formulation. Note that as far as I know, the Pitzer > formulation does not include any redox reactions, aluminum, or silica. > > > Example 1 of PHREEQC determines the speciation of seawater. The data > input > corresponds to standard water quality for seawater. I have always > assumed > that this 'standard' WQ for seawater refers to the common elements in their > dissolved state. In this instance calcium at 412.3 ppm would be assumed to > be nearly all in ionic form. Yet the results of the simulation suggest > that about 10% of the calcium is present as CaSO4. While nucleation of > CaSO4 can be such that initially it is dissolved I would assume that here > CaSO4 implies solids that are precipitated. > > > QUESTION 2: Is this correct? OR am I missing something? > > You are missing something. The CaSO4 in the distribution of species is a > dissolved ion pair or complex. All species listed in the distribution of > species are dissolved and concentrations defined in SOLUTION refer to total > dissolved concentrations (free ion + complexes). Saturation indices show > the saturation state of the solution relative to minerals. Mineral > equilibria are defined with EQUILIBRIUM_PHASES; KINETICS can be used to > define kinetic reaction of minerals. > > David > > David Parkhurst (dlpark@xxxxxxxx) > U.S. Geological Survey > Box 25046, MS 413 > Denver Federal Center > Denver, CO 80225 > > Project web page: https://wwwbrr.cr.usgs.gov/projects/GWC_coupled > >
Please note that some U.S. Geological Survey (USGS) information accessed through this page may be preliminary in nature and presented prior to final review and approval by the Director of the USGS. This information is provided with the understanding that it is not guaranteed to be correct or complete and conclusions drawn from such information are the sole responsibility of the user.
Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government.
The URL of this page is:
Last modified: $Date: 2005-09-13 21:04:21 -0600 (Tue, 13 Sep 2005) $
Visitor number 2234 since Jan 22, 1998.