TOUGH4 User Manual
  • Quick Entry to Keywords for Data Input
  • 1️⃣INTRODUCTION
    • About TOUGH
    • TOUGH Development History
    • TOUGH4 Implementation
    • Scope and Methodology
  • 2️⃣WHAT IS NEW IN TOUGH4
  • 3️⃣CODE COMPILATION AND INSTALLATION
    • Setup for Compilation
    • Code Compilation
      • 1. Compilation of TOUGH4 using Visual Studio
      • 2. Compilation of TOUGH4 on Linux-like platform
    • Installation
    • Running the Executable for Simulations
  • 4️⃣GOVERNING EQUATIONS
    • Mass-Balance Equation
    • Accumulation Terms
    • Flux Terms
    • Sink and Source Terms
    • Virtual Node Well Treatment
    • Semi-Analytical Conductive Heat Exchange
    • Drift Model
    • Non-Darcy Flow
  • 5️⃣NUMERICAL METHOD
    • Space and Time Discretization
    • Interface Weighting Schemes
    • Initial and Boundary Conditions
      • Initial Conditions and Restarting
      • Neumann Boundary Conditions
      • Dirichlet Boundary Conditions
      • Atmospheric Boundary Conditions
      • Constant Temperature Boundary Conditions
    • Parallel computing schemes
    • Linear Solvers
    • Python Functions
      • Relative Permeability
      • Capillary Pressure
      • Initial Condition Calculation
      • Fetching Output Data
      • Fetching Thermophysical Property Data From NIST Webbook
      • Coupling With Third-Party Software
  • 6️⃣SOFTWARE ARCHITECTURE
    • Program Design
    • Data Structure
    • Linear Equation Setup
  • 7️⃣PROCESS MODELING
    • EOS1
    • EOS2
    • EOS3
    • EOS4
    • EOS6
    • EOS7
    • EOS9
    • ECO2
    • EWASG
    • TMVOC
    • Tracers/Decay Chain
    • Biodegradation Reaction
    • Wellbore Flow
    • Non-Darcy Flow
    • Enhanced Coal Bed Methane
  • 8️⃣PREPARATION OF MODEL INPUT
    • Input Formatting
    • Keywords and Input Data
      • TITLE
      • BIODG
      • CBMDA
      • CHEMP
      • COFT
      • CONNE
      • COUPL
      • DIFFU
      • ELEME
      • ENDCY
      • ENDFI
      • FLAC
      • FNIST
      • FOFT
      • FORCH
      • GASES
      • GENER
      • GOFT
      • HYSTE
      • INCON
      • INDOM
      • MESHM
      • MODDE
      • MOMOP
      • MULTI
      • OUTPU
      • PARAM
      • ROCKS
      • ROFT
      • RPCAP
      • SELEC
      • SOLVR
      • SPAVA
      • TIMBC
      • TIMES
      • TRACR
      • WELLB
    • Inputs for Initial Conditions
      • EOS1
      • EOS2
      • EOS3
      • EOS4
      • EOS6
      • EOS7
      • EOS9
      • ECO2
      • EWASG
      • TMVOC
    • Geometry Data
      • General Concepts
      • MESHMaker
      • Multiple-continuum processing
    • Inputs for MESHMaker
      • Generation of radially symmetric grids
        • RADII
        • EQUID
        • LOGAR
        • LAYER
      • Generation of rectilinear grids
      • MINC processing for fractured media
    • Adjustment of Computing Parameters at Run-time
  • 9️⃣OUTPUTS
  • 🔟VALIDATION AND APPLICATION EXAMPLES
    • EOS1
      • Problem 1 - Code Demonstration
      • Problem 2 - Heat Sweep in a Vertical Fracture (rvf)
      • Problem 3 - Five-spot Geothermal Production/Injection (rfp)
      • Problem 4 - Coupled Wellbore Flow (r1q)
      • Problem 5 - Five-Spot Geothermal Production/Injection under extremely high temperature
    • EOS2
      • Problem 1 -Five-spot Geothermal Production/Injection (rfp)
    • EOS3
      • Problem 1 - Code Demonstration (eos3p1)
      • Problem 2 - 1D TH Problem with Heating and Gas Source (by Guanlong Guo)
      • Problem 3 - Heat Pipe in Cylindrical Geometry (rhp)
      • Problem 4 - 3D Thermal Consolidation Test, Coupling with FLAC3D Simulator (by Guanlong Guo)
    • EOS4
      • Problem 1 - Code Demonstration (eos4p1)
      • Problem 2 - Heat Pipe in Cylindrical Geometry (rhp)
    • EOS6
      • Problem 1-Validation with EOS2
      • Problem 2-Noble Gas Transport
    • EOS7
      • Problem 1-Multiphase and Nonisothermal Processes in a System with Variable Salinity (rf1)
      • Problem 2-Thermal and Tracer Diffusion (EOS7R/rdif7)
      • Problem 3-Contamination of an Aquifer from VOC Vapors in the Vadose Zone (EOS7R/rdica)
      • Problem 4-Density, Viscosity, Solubility, and Enthalpy of Real Gas Mixtures (EOS7C/SAM7C1)
      • Problem 5-CO2 Injection into a Depleted Gas Reservoir (EOS7C2/SAM7C2)
      • Problem 6- CO2 Injection into a Saturated System (EOS7C/SAM7C3)
      • Problem 7-Density, Viscosity, and Enthalpy of Real Gas Mixtures (EOS7CA/SAM7CA1)
      • Problem 8-CO2 Injection into a Shallow Vadose Zone (EOS7CA/SAM7CA2)
      • Problem 9-Non-Isothermal Compressed Air Energy Storage in Reservoir (by Julien Mouli-Castillo)
    • EOS9
      • Page 1
    • ECO2
      • Problem 1-Demonstration of Initialization Options (ECO2N/rtab)
      • Problem 2-Radial Flow from a CO2 Injection Well (ECO2N/rcc3)
      • Problem 3-CO2 Discharge Along a Fault Zone (ECO2N/r1dv)
      • Problem 4-CO2 Injection into a 2-D Layered Brine Formation (ECO2N/rtp7)
      • Problem 5-Upflow of CO2 along a Deep Fault Zone (ECO2M/r1d)
      • Problem 6-Migration of a CO2 Plume in a Sloping Aquifer, Intersected by a Fault (ECO2M/rwaf)
      • Problem 7-GCS/GHE with a double-porosity reservoir (Case6_50kg_DP/ECO2NV2)
    • EWASG
      • Problem 1 - Brine Density Calculation (dnh)
      • Problem 2 - Production from a Geothermal Reservoir with Hypersaline Brine and CO2 (rhbc)
    • TMVOC
      • Problem 1-Initialization of Different Phase Conditions (r7c)
      • Problem 2-1-D Buckley-Leverett Flow (rblm)
      • Problem 3-Diffusion of components (rdif2)
      • Problem 4-Steam Displacement of a NAPL in a Laboratory Column (rtcem)
      • Problem 5-Steam Displacement of a Benzene-Toluene Mixture in a Laboratory Column (rbt)
      • Problem 6 -Air Displacement of a NAPL from a Laboratory Column (rad)
      • Problem 7-NAPL Spill in the Unsaturated Zone (r2dl)
    • T4.Well
      • Problem 1-Steady-state two-phase flow upward
      • Problem 2-Non-isothermal CO2 flow through a wellbore initially full of water
  • CONCLUSION REMARKS
  • REFERENCES
  • ACKNOWLEDGEMENT
  • Appendix
    • ☑️A: RELATIVE PERMEABILITY FUNCTIONS
      • IRP=1 Linear function
      • IRP=2 Power function
      • IRP=3 Corey's curves
      • IRP=4 Grant's curve
      • IRP=5 Perfectly mobile
      • IRP=6 Fatt and Klikoff function
      • IRP=7 van Genuchten-Mualem Model
      • IRP=8 Verma function
      • IRP=10 Modified Brooks-Corey Model
      • IRP=11 Modified van Genuchten Model
      • IRP=12 Regular hysteresis
      • IRP=13 Simple hysteresis
      • IRP=31 Three phase perfectly mobile
      • IRP=32 Modified Stone's first 3-phase method
      • IRP=33 Three-phase Parker's function
      • IRP=34 Alternative Stone 3-phase
      • IRP=35 Power-law function
      • IRP=36 Faust for two-phase Buckley-Leverett problem
      • IRP=37 Another alternative to Stone function
      • IRP=40 Table lookup
      • IRP=41 User-Defined relative permeability function
    • ☑️B: CAPILLARY PRESSURE FUNCTIONS
      • ICP=1 Linear function
      • ICP=2 Function of Pickens
      • ICP=3 TRUST capillary pressure
      • ICP=4 Milly’s function
      • ICP=6 Leverett’s function
      • ICP=7 van Genuchten function
      • ICP=8 No capillary pressure
      • ICP=10 Modified Brooks-Corey Model
      • ICP=11 Modified van Genuchten Model
      • ICP=12 Regular hysteresis
      • ICP=13 Simple hysteresis
      • ICP=31 Parker et al 3-phase function
      • ICP=32 Parker 3-phase function, alternative 1
      • ICP=33 Parker 3-phase function, alternative 2
      • ICP=34 Parker 3-phase function, alternative 3
      • ICP=40 Table lookup
      • ICP=41 User-Defined capillary pressure function
    • ☑️C: ADDITIONAL PROGRAM OPTIONS
    • ☑️D: DESCRIPTION OF FRACTURED FLOW
      • Multiple Continuum Approaches
      • Active Fracture Modle
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  1. NUMERICAL METHOD
  2. Initial and Boundary Conditions

Dirichlet Boundary Conditions

PreviousNeumann Boundary ConditionsNextAtmospheric Boundary Conditions

Dirichlet conditions prescribe fixed thermodynamic conditions, such as pressure, temperature, or saturation. Dirichlet conditions can be implemented by assigning very large volumes (e.g., V = 105010^{50}1050 m3m^3m3) to grid blocks adjacent to the boundary, so that their thermodynamic conditions do not change at all from fluid or heat exchange with finite-size blocks in the flow domain. For those elements with very large volumes, no mass or energy balance equations are set up, and their primary thermodynamic variables are not included in the list of unknowns. In addition, a small value (such as D = 10−910^{-9}10−9m) should be specified for the nodal distance of such blocks, so that boundary conditions are in fact maintained in close proximity to the surface where they are desired, and not at some distance from it.

The Dirichlet conditions for each element can also be specified through the last parameter (named "Activity") of input record or MESH file. "Activity" is element activity indicator. It can be “A”-active element, “I”-inactive element, “V”-time-dependent first-type boundary element, and “T”-constant temperature element. In addition, an element with a zero or negative volume is used to indicate that the element and all subsequent elements are to be used for Dirichlet boundary conditions. The code will internally assign a very large volume for this element and all subsequent elements (to be backward compatible with TOUGH2) and print out a warning message. In TOUGH4, the user must specify a material name or material number for every element.

Time-dependent Dirichlet conditions can be implemented using two different approaches. The first method consists of placing appropriate, large sinks or sources in boundary elements with large volumes (Moridis and Pruess, 1992). As an example, consider a laboratory experiment reported by Kruger and Ramey (1974) that involved flashing (vaporizing) flow from a sandstone core, with a time-dependent gas pressure boundary condition

Pb=P0+P1t+P2t2P_b=P_0+P_1t+P_2t^2Pb​=P0​+P1​t+P2​t2 (5-12)

maintained at the outflow end. According to the ideal gas law, the pressure behavior of Eq. (5-12) can be associated with a time-dependent gas inventory of mass MbM_bMb​ in a volume V as follows.

Mb=Pb(mV/RT)M_b=P_b(mV/RT)Mb​=Pb​(mV/RT) (5-13)

where m is the molar weight of the gas, R the universal gas constant, and T absolute temperature. The required time dependence of MbM_bMb​ can be realized by means of a sink/source rate of

Qb=dMb/dt=(mVRT)dPb/dt=(mVRT)(P1+2P2t)Q_b=dM_b/dt=\left(\frac{mV}{RT}\right)dP_b/dt=\left(\frac{mV}{RT}\right)\left(P_1+2P_2t\right)Qb​=dMb​/dt=(RTmV​)dPb​/dt=(RTmV​)(P1​+2P2​t) (5-14)

Therefore, the desired boundary condition can be implemented by means of a grid block with volume V that is initialized in single-phase gas (e.g., air) conditions, with pressure P0, and with a time-dependent sink/source term given by Eq. (5-14) that would be specified through tabular generation data in data block GENER. In order for the pressure conditions in this block to be negligibly affected by heat and mass exchange with the flow domain, the volume V should be made very large, e.g., V = 105010^{50}1050 m3m^3m3, just as for time-independent Dirichlet boundary conditions. The time-dependent generation rates from Eq. (5-14) will then also be very large. The same approach as just outlined for a time-dependent gas pressure boundary can be used to realize other time-dependent Dirichlet conditions, such as prescribed temporal variation of temperature, capillary pressure, and others.

The second, users can use "" keyword to realize time-dependent Dirichlet boundary conditions by reading a set of time and primary variable data at boundary elements from the main input file or a data file named "timvsp.dat". Boundary values will be linearly interpolated between table entries. The volume for these elements should be made very large as well.

5️⃣
ELEME.1
TIMBC