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ORD Mine Waste Scientist to Scientist Meeting 15 June 2000, Las Vegas, NV. Mine Waste and Modeling. David G. Jewett, Ph.D. USEPA/ORD/NRMRL Subsurface Protection and Remediation Division, Ada, OK Co-Director, Center for Subsurface Modeling Support (CSMoS). Presentation Outline.
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ORD Mine Waste Scientist to Scientist Meeting15 June 2000, Las Vegas, NV Mine Waste and Modeling David G. Jewett, Ph.D. USEPA/ORD/NRMRL Subsurface Protection and Remediation Division, Ada, OK Co-Director, Center for Subsurface Modeling Support (CSMoS)
Presentation Outline • Modeling Basics • Definition • General Approach • Types of Models • Source • Flow • Reactive Transport • Other • Modeling Resources
Definition Mathematical model: simulates ground-water flow and/or solute fate and transport indirectly by means of a set of governing equations thought to representthe physical processes that occur in the system (Anderson and Woessner, 1992).
Modeling Approach • Establish purpose • Develop conceptual model • Select appropriate mathematical model • Model design (iterative process) • Calibration (including sensitivity analysis) • Verification • Prediction (including uncertainty analysis)
Types of Models • Source models • Unsaturated and saturated flow models • Reactive transport models • Other models
Source Models • Estimate mass flux from a source area • Characterize source areas in terms of source mineralogy and subsurface hydrogeological and geochemical conditions • Describe loading as steady-state or as a function of time
Source Code Example • PYROX • Univ. of Waterloo (Wunderly & Blowes, 1996) • 1-D finite element code • Sulfide mineral oxidation model • Based on conceptualization and mathematical derivation of Davis and Ritchie • Oxygen diffusion is rate-limiting factor • Simulates release of Fe, SO42-, and H+
Source Code Example • MINTEQA2 • NERL-ERD (Allison et al., 1991) • Versatile equilibrium solution chemistry code • Calculates equilibrium mass distribution of dissolved and adsorped species and multiple solid phases • Extensive thermodynamic database
Flow Models • Define water movement and variability of soil water tension or hydraulic head across domain of interest • Unsaturated versus saturated flow • Steady-state versus transient simulations
Unsaturated Flow Code Example • SOILCOVER • Univ. of Saskatchewan (Wilson, 1994) • 1-D finite element code • Simulates water flux at atmosphere-soil interface and water movement in the near surface unsaturated zone • Designed for developing soil covers for mine tailings and acid generating waste rock
Unsaturated Flow Code Example • HELP • USACE for USEPA (Schroeder et al., 1991) • Quasi-2-D layered water budget model • Rapid estimation of surface runoff, subsurface drainage, and leachate production • Extensive climate and soil characteristic databases
Unsaturated Flow Code Example • VS2DT • USGS (Healy, 1996) • 1-D or 2-D finite difference code • Simulates water and solute movement in variably saturated porous media • Distributed in VS2DI package as of 2/2000 (combined with VS2DH)
Saturated Flow Code Example • MODFLOW • USGS (McDonald and Harbaugh, 1988; Harbaugh and McDonald,1996) • 3-D finite difference ground-water flow code • Modular structure for easy adaptation • Ground-water flow model work horse • Widely used and extensively tested • GMS, Groundwater Vistas, Visual Modflow
Saturated Flow Code Example • FEMWATER • ORNL (Yeh and Ward, 1979) and Penn State (Yeh, 1990) • 3-D finite element ground-water flow code • Saturated and unsaturated flow • GMS
Reactive Transport Models • Define temporal and spatial distribution of dissolved contaminant mass in the model domain • Incorporate the physical, chemical, and biological processes controlling solute fate and transport (sorption, abiotic transformations, biologically mediated transformations)
Reactive Transport Code Example • MINTRAN • Univ. of Waterloo (Walter et al., 1994) • Couples PLUME2D (2-D finite element solute transport code; Frind et al., 1990) and MINTEQA2 • Simulates multicomponent reactive transport in spatially discrete ground-water systems • MINTOX = MINTRAN + PYROX
Reactive Transport Code Example • PHREEQC • USGS (Parkhurst and Appelo, 1999) • Low-temp aqueous geochemical model • Calculations performed: • Speciation and S.I. calculations • Batch reaction and 1-D transport calculations • Inverse modeling • PHREEQCI
Reactive Transport Code Example • MT3D • USEPA, 3-D solute transport (Zheng, 1990) • MOC, MMOC, HMOC • Runs with MODFLOW, or similar, flow output • MT3D96, MT3D99 (proprietary) • RT3D • PNNL, multi-species transport (Clement, 1997) • Based on MT3D; includes 8 rxn modules
Other Models • Surface Water Models • OTIS (USGS, 1998) simulates 1-D fate and transport of water-borne solutes in streams and rivers • EFDC (Hamerick, 1999) simulates 3-D flow, transport, and biogeochemical processes in surface water systems
Other Models (continued) • Watershed Models • BASINS (USEPA, 1998) multipurpose environmental analysis system for performing watershed- and water-quality-based studies • Dynamic System Models • STELLA (HPS, 1994) universal simulation tool to build understanding of dynamic systems and interrelationships
USEPA Modeling Resources • Center for Subsurface Modeling Support (CSMoS) • NRMRL/SPRD – Ada, OK • www.epa.gov/ada/csmos.html • On-Line Model Database: www.epa.gov/ada/mdb_form.html
USEPA Modeling Resources • Center for Exposure Assessment Modeling (CEAM) • NERL/ERD – Athens, GA • www.epa.gov/ceampubl/ceamhome.htm • EPA Scientific Model Database: athord1.ath.epa.gov:9876/Models.nsf
Other Modeling Resources • USGS Water Resources Software Page • water.usgs.gov/software • Richard B. Winston’s Home Page • www.mindspring.com/~rbwinston/rbwinsto.htm • Geotech & Geoenviron Software Directory • www.ggsd.com • Int’l Ground Water Modeling Center • www.mines.edu/igwmc
“The fascinating impressiveness of rigorous mathematical analysis, with its atmosphere of precision and elegance, should not blind us to the defects of the premises that condition the whole process.” - T.C. Chamberlin “Everything should be made as simple as possible, but not simpler.” - Albert Einstein