Encyclopedia of Hydrological Sciences 2005
DOI: 10.1002/0470848944.hsa157
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Numerical Models of Groundwater Flow and Transport

Abstract: The article gives an introduction to numerical modeling of flow and transport problems and to software tools that are currently in use for modeling such phenomena. Details are explained on numerical approximations leading to different numerical models. Extensions for reactive transport are mentioned. Basic guidelines and criteria are given that should be taken into account by the modeler in order to improve the accuracy of results. Inverse modeling is presented as an advanced feature. Some examples of pre‐ and… Show more

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Cited by 15 publications
(9 citation statements)
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“…Numerical stability of the combined flow and biodegradation system simulation was ensured by applying the Peclet and Courant convergence and stability criteria to the model. These criteria affect the time step Δt and the space discretization of the grid Δx in RT3D, respectively, and minimize the numerical errors due to round off and truncation of derivatives that occur when replaced by finite differences [ Holzbecher and Sorek , 2005]. The criteria are Peclet number criterion Courant number criterion where P e is the Peclet stability number (dimensionless), C r is the Courant stability number (dimensionless), is the average linear flow velocity (m/d), Δ t is the time step difference (d), Δ x is the spatial step difference (m) and D is the coefficient of hydrodynamic dispersion (m 2 /d).…”
Section: Model Developmentmentioning
confidence: 99%
See 1 more Smart Citation
“…Numerical stability of the combined flow and biodegradation system simulation was ensured by applying the Peclet and Courant convergence and stability criteria to the model. These criteria affect the time step Δt and the space discretization of the grid Δx in RT3D, respectively, and minimize the numerical errors due to round off and truncation of derivatives that occur when replaced by finite differences [ Holzbecher and Sorek , 2005]. The criteria are Peclet number criterion Courant number criterion where P e is the Peclet stability number (dimensionless), C r is the Courant stability number (dimensionless), is the average linear flow velocity (m/d), Δ t is the time step difference (d), Δ x is the spatial step difference (m) and D is the coefficient of hydrodynamic dispersion (m 2 /d).…”
Section: Model Developmentmentioning
confidence: 99%
“…[21] Numerical stability of the combined flow and biodegradation system simulation was ensured by applying the Peclet and Courant convergence and stability criteria to the model. These criteria affect the time step Dt and the space discretization of the grid Dx in RT3D, respectively, and minimize the numerical errors due to round off and truncation of derivatives that occur when replaced by finite differences [Holzbecher and Sorek, 2005]. The criteria are Peclet number criterion…”
Section: General Substrate Interaction Modulementioning
confidence: 99%
“…The coefficient, which appears in front of the brackets, the parameter combination DÁDt Dx 2 is also known as Neumann-number 3 (abbreviation: Neu), (see Holzbecher and Sorek 2005). It is the given explicit formula for c i,new that is computed in the m-file 'diffusion.m'.…”
Section: A Simple Numerical Modelmentioning
confidence: 99%
“…Such models simulate the groundwater dynamics in an aquifer by translating its physical, chemical, and biological characteristics into mathematical equations by simplifying assumptions (Holzbecher and Sorek 2006). Such models simulate the groundwater dynamics in an aquifer by translating its physical, chemical, and biological characteristics into mathematical equations by simplifying assumptions (Holzbecher and Sorek 2006).…”
Section: Introductionmentioning
confidence: 99%
“…Groundwater models are commonly used in conjunction with field monitoring to assess the physical processes representing subsurface flow and solute transport. Such models simulate the groundwater dynamics in an aquifer by translating its physical, chemical, and biological characteristics into mathematical equations by simplifying assumptions (Holzbecher and Sorek 2006). These equations require data about aquifer characteristics-such as hydraulic properties, geological borders, boundary conditions, and sources and sinks-that will sufficiently aid in understanding groundwater dynamics (Bakalowicz 2005).…”
Section: Introductionmentioning
confidence: 99%