PHREEQC APPLICATION EXAMPLES
Most of these examples stem from Appelo and Postma, 2005. Geochemistry, groundwater
and pollution, 2nd ed. The examples can be easily run and plotted with Vincent Post's
PHREEQC for windows interface.
- Equilibrium Reactions
- Ca2+ / F- in equilibrium with
fluorite ( CaF2 )
explains high F- concentration in African Rift Valley waters.
- Dissolution of calcite ( CaCO3 )
depends on the CO2 pressure.
Mixing causes subsaturation which explains cave formation in karst areas and coastal zones.
- The Al concentration in water depends on Gibbsite
( Al(OH)3 ) equilibrium.
- Both at low and high pH, the Al concentration may exceed
the drinking water limit.
- Ca and SO4 concentrations diverge when
gypsum (CaSO4.2H2O) precipitates
from an evaporating brine.
- The series of salts that precipitate from
evaporating seawater can be computed using Pitzer equations for calculating activities.
- Ion exchange
- Surface complexation
- Zn sorption edge, % Zn sorbed as function of pH and the Zn concentration.
- CO2 sorption on oxy-hydroxides
is important in natural systems and must be included in the Dzombak and Morel database.
- Kinetic reactions
- Kinetic dissolution of quartz.
- Biodegradation of phenol with Monod kinetics.
- Biodegradation of xylene coupled with biomass growth.
- Application examples
- In situ iron removal, principles of removing iron from
groundwater by injecting oxygenated water.
- In situ iron removal, a specific case showing kinetic effects.
- Retardation of U(6) and Zn from acid mine drainage.
- Oxidation of pyrite in a column experiment.
- Modeling isotope fractionation
- Specific Conductance
NEW in PHREEQC version 2.13
(consult PHREEQC Help for details, unblock this file)
- Multicomponent diffusion
- Multicomponent diffusion can be upgradient, contrary to Fick's laws,
as explained in a column example.
- PHREEQC's multicomponent module can be checked by calculating CaCl2 diffusion profiles:
- Compare with the Nernst equation which gives the diffusion
coefficent of a salt from its constituent ions. Charge on the tracer, or diffusion in a concentrated solution
give different results!
- Compare with classic PHREEQC, which calculates with one and
the same diffusion coefficient for all species.
- Multicomponent diffusion of seawater in a fresh water sediment is
different for cations and anions.
- Multicomponent diffusion of tracers in clays is a function of the
tracer diffusion coefficient and diffuse double layer effects such as anion exclusion and enhancement of cation transport.
- Diffuse Double Layer calculations
- The membrane properties of clays depend on the extent of the diffuse double layer.
- Colloid transport
- Ferrihydrite, with sorbed Uranium, can be transported as colloid through a column.
NEW in PHREEQC version 2.16
(consult PHREEQC Help)
- Surface/interlayer diffusion of cations
- Solution density calculations