PHAST For Environmental Geosciences

PHAST is a three-dimensional simulator developed by the U.S. Geological Survey (USGS) for saturated groundwater flow, solute transport, and multicomponent geochemical reactions. It couples an HST3D-based flow and transport model with the PHREEQC geochemical engine. 

This research direction is suited to MSc students interested in hydrogeochemistry, reactive transport, hydrogeology, and environmental risk assessment. 

Core Capabilities 

  • Groundwater Flow & Transport: Three-dimensional saturated flow, advection, and dispersion under steady or transient conditions. 
  • Aqueous Geochemistry: Speciation, redox reactions, ion exchange, and surface complexation. 
  • Mineral Reactions: Equilibrium and kinetic mineral dissolution and precipitation, including carbonate reactions and silicate weathering. 
  • Environmental Applications: Simulates changes in solute concentrations, pH, and mineral reactions to assess water-quality impacts. 

Broad Research Suggestions 

PHAST serves as an efficient and robust tool for specialized environmental and geoscientific research: 

  • Shallow Aquifer CO₂ Intrusion: Modeling how dissolved carbon leakage lowers pH and mobilizes trace heavy metals from subsurface sediments. 
  • Enhanced Rock Weathering (ERW): Quantifying alkalinity generation and carbon sequestration potential when silicate dusts interact with shallow groundwater flow.
  • Water-Rock Interaction Feedbacks: Assessing long-term mineral trapping, porosity evolution, and secondary precipitation boundaries along regional flow paths. 
  • Mine Waste Geochemistry & Remediation: Examining water-rock interactions in sulfide tailings or reactive barriers, modeling acidity attenuation and pathways. 

Getting Started & Supervision 

PHAST examples cover contaminant decay and sorption, microbial reactions, ion exchange, and sewage plumes. Projects may involve model testing, reactive-transport simulations, or calibration against laboratory or field data. 

Model scope: 

Single-phase, constant-density saturated groundwater flow; not free-phase CO₂ migration. 

Contact:

Dr. Mohammad Nooraiepour (monoo@uio.no)

Published Oct. 14, 2026 11:21 AM - Last modified Oct. 14, 2026 11:32 AM

Supervisor(s)

Scope (credits)

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