recordValidityResult

Result of the validity analysis of the ATES_L4 model

Extends from TransiEnt.Basics.Icons.Record (Icon for records).

Information

1. Purpose of model

Record returned by the validity analysis function ValidityAnalysis. It contains one status per criterion and the key figures on which the status is based.

2. Level of detail, physical effects considered, and physical insight

(Purely technical component without physical modeling.)

3. Limits of validity

- Status values: 0 = criterion fulfilled, 1 = warning, 2 = criterion violated.

- The key figures are pre-simulation estimates; see ValidityAnalysis for their definitions and limits.

4. Interfaces

(no elements)

5. Nomenclature

s statusDarcy, statusLTE, statusNRGF, statusBuoyancy status of the criteria on Darcy's law, local thermal equilibrium, natural regional groundwater flow and buoyancy switch (0 fulfilled, 1 warning, 2 violated) [-]
s statusOverall maximum of all status values [-]
R_\mathrm{th} R_th thermal radius of the stored volume [m]
d d_grain grain diameter used for the criteria on Darcy's law and local thermal equilibrium [m]
dGrainEstimated true if the grain diameter was estimated from permeability and porosity [-]
\mathrm{Re}_\mathrm{d} Re_well grain Reynolds number at the well screen [-]
E E_well non-Darcy share of the pressure gradient at the well screen [-]
r_E r_E radius up to which the non-Darcy share exceeds E_Darcy_max [m]
r_\mathrm{LTE} r_LTE radius up to which the seepage velocity exceeds v_s_LTE [m]
f_\mathrm{V} fV_LTE fraction of the thermal plume volume in which the seepage velocity exceeds v_s_LTE [-]
r_\mathrm{LTNE} r_LTNE radius up to which the Darcy velocity exceeds q_LTNE [m]
M M_mobility mobility ratio of the injected to the ambient water [-]
N_0 N_0 displacement number without high-temperature correction [-]
N_\mathrm{lo} N_lo lower bound of the displacement number with high-temperature correction [-]
N_\mathrm{hi} N_hi upper bound of the displacement number with high-temperature correction [-]
\mathrm{Ra} Ra Rayleigh-Darcy number of the aquifer [-]
q_0 q_0 characteristic buoyancy flow velocity [m/s]

6. Governing Equations

(no equations)

7. Remarks for Usage

Returned by ValidityAnalysis; the definitions of all key figures are given in the documentation of ValidityAnalysis. Bind the result to a parameter record, e.g. parameter Records.ValidityResult validity = Function.ValidityAnalysis(...), to access the values in a model.

8. Validation

(no validation or testing necessary)

9. References

(no remarks)

10. Version History

Model created by Markus Gillner (markus.gillner@tuhh.de) on 01.10.2026

Components

TypeNameDefaultDescription
IntegerstatusDarcyValidity of Darcy's law (creeping flow)
IntegerstatusLTELocal thermal equilibrium between fluid and solid
IntegerstatusNRGFNegligible natural regional groundwater flow
IntegerstatusBuoyancyConsistency of the buoyancy switch
IntegerstatusOverallMaximum of all status values
SI.LengthR_thThermal radius of the stored volume
SI.Lengthd_grainGrain diameter used for the criteria on Darcy's law and local thermal equilibrium
BooleandGrainEstimatedTrue if the grain diameter was estimated from permeability and porosity
RealRe_wellGrain Reynolds number at the well screen
RealE_wellNon-Darcy share of the pressure gradient at the well screen
SI.Lengthr_ERadius up to which the non-Darcy share exceeds E_Darcy_max
SI.Lengthr_LTERadius up to which the seepage velocity exceeds v_s_LTE
RealfV_LTEFraction of the thermal plume volume in which the seepage velocity exceeds v_s_LTE
SI.Lengthr_LTNERadius up to which the Darcy velocity exceeds q_LTNE
RealM_mobilityMobility ratio of the injected to the ambient water (viscosity ratio)
RealN_0Displacement number without high-temperature correction
RealN_loLower bound of the displacement number with high-temperature correction
RealN_hiUpper bound of the displacement number with high-temperature correction
RealRaRayleigh-Darcy number of the aquifer
SI.Velocityq_0Characteristic buoyancy flow velocity