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Phast Version 2 - A Program for Simulating Groundwater Flow, Solute Transport, and Multicomponent Geochemical Reactions (Paperback)
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Phast Version 2 - A Program for Simulating Groundwater Flow, Solute Transport, and Multicomponent Geochemical Reactions (Paperback)
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The computer program PHAST (PHREEQC And HST3D) simulates
multicomponent, reactive solute transport in three-dimensional
saturated groundwater flow systems. PHAST is a versatile
groundwater flow and solute-transport simulator with capabilities
to model a wide range of equilibrium and kinetic geochemical
reactions. The flow and transport calculations are based on a
modified version of HST3D that is restricted to constant fluid
density and constant temperature. The geochemical reactions are
simulated with the geochemical model PHREEQC, which is embedded in
PHAST. Major enhancements in PHAST Version 2 allow spatial data to
be defined in a combination of map and grid coordinate systems,
independent of a specific model grid (without node-by-node input).
At run time, aquifer properties are interpolated from the spatial
data to the model grid; regridding requires only redefinition of
the grid without modification of the spatial data. PHAST is
applicable to the study of natural and contaminated groundwater
systems at a variety of scales ranging from laboratory experiments
to local and regional field scales. PHAST can be used in studies of
migration of nutrients, inorganic and organic contaminants, and
radionuclides; in projects such as aquifer storage and recovery or
engineered remediation; and in investigations of the natural
rock/water interactions in aquifers. PHAST is not appropriate for
unsaturated-zone flow, multiphase flow, or density-dependent flow.
A variety of boundary conditions are available in PHAST to simulate
flow and transport, including specified-head, flux
(specified-flux), and leaky (head-dependent) conditions, as well as
the special cases of rivers, drains, and wells. Chemical reactions
in PHAST include (1) homogeneous equilibria using an
ion-association or Pitzer specific interaction thermodynamic model;
(2) heterogeneous equilibria between the aqueous solution and
minerals, ion exchange sites, surface complexation sites, solid
solutions, and gases; and
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