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Mobility of Metals in the Soil Environment
 

Here's another example: A soil system that contains a certain amount of naturally occurring lead. The question is whether the lead is going to remain on-site or dissolve and gradually move with the groundwater into surrounding streams and wells. Generally this would be answered by placing monitoring wells throughout an area and measuring the chemical concentration of lead. If, in addition to this monitoring, one were to apply the principles of chemical equilibrium, it would be possible to develop deeper insight into the chemical mechanisms controlling the system. A monitoring program answers what is happening in the system. Chemical equilibrium answers why.

For instance, if in the course of your monitoring program you were to notice that the concentration of lead was decreasing as you moved farther down a watershed, it would be useful to know what happened to the lead. The chemical equilibrium approach would tell you if lead solids were forming or if an observed change in pH was due to the addition of a new ion to solution. If most of the lead is calculated to form a particular solid phase, if might be interesting to see how small perturbations in the system effects the dissolution of lead. The net effect of applying chemical equilibrium modeling is that the  underlying mechanism is clearer , and the ability to make decisions about this system is improved.




 
 
 
  Sept-2007 Vista compatible, 32-bit, version 4.6 is released.

May - 2002 Version 4.5: Thermodynamic database is upgraded, documented and conforms to USEPA standards.  All reaction data is referenced.

Sept - 1998 Version 4.0: Windows, 16-bit version released.  Numerical stability locked in for wide range of chemical conditions.  New report writing features. Titrations, sensitivity analysis, processing of huge datasets now possible.

June - 1992 Version 3.0: DOS, 8-bit version is released. First spatial user interface for MINEQL. Tableau view of input data.  Object oriented management of output data to fit any application. MINTEQ data is included.

Prior to our work:

Late 1980's USEPA combines MINEQL numerical code and the USGS's WATEQ thermodynamic  data to produce MINTEQ.

1987 At MIT, Dave Dzombak collects Two Layer surface complexation data for a wide range of aqueous ions on FeO

Early 1980's The USGS develops a chemical equilibrium program called WATEQ. Their work continues throughout the decade to provide critical review of thermodynamic data.

1980 MINEQL "+Stanford" (because of the work at Stanford University) provides electrostatic surface complexation reactions within MINEQL.

1975 MINEQL is developed at MIT, by John Westall and Francois Morel. The FORTRAN program uses a generic tableau approach to describe equilibria and mass balance in aqueoous systems.

1972 REDEQL is developed by James Morgan and Francois Morel.  First chemical equilibrium program with a vast scope of application. Becomes the prototype for MINEQL.