Index
Keywords and section headings of all topics.
- --json Comparison of runs
- 1. Open the example (Getting started) Getting started
- 2. Look at the project (Getting started) Getting started
- 3. Run the calculation (Getting started) Getting started
- 4. Look at the results (Getting started) Getting started
- 5. Change something and compare (Getting started) Getting started
- A_LEVEL Output files
- A_LEVEL.csv – atmospheric records (Output files) Output files
- acknowledgements Credits and license
- Activation energies (Solute transport: temperature and water-content dependence, colloids) Solute transport: temperature and water-content dependence, colloids
- activation energy Solute transport: temperature and water-content dependence, colloids
- activation energy Temperature and water-content dependence of reactions
- active uptake Root water and solute uptake
- active uptake Root solute uptake
- Active uptake (Root solute uptake) Root solute uptake
- actual evaporation Boundary fluxes, heads and cumulative quantities
- actual transpiration Boundary fluxes, heads and cumulative quantities
- add material Materials & parameters
- Additions of Rusteau (Relation to HYDRUS-1D) Relation to HYDRUS-1D
- advection dispersion equation Solute transport equations
- Aerodynamic and canopy resistance (Penman–Monteith combination equation) Penman–Monteith combination equation
- aerodynamic resistance Surface energy balance
- aerodynamic resistance Penman–Monteith combination equation
- AIC Parameter estimation results
- AIC Parameter estimation
- air entrapment Hysteresis
- air entry value Soil hydraulic property models
- albedo Meteorological data
- albedo Surface energy balance
- alpha Materials & parameters
- alpha h Scaling of the hydraulic properties
- alpha K Scaling of the hydraulic properties
- alpha theta Scaling of the hydraulic properties
- altitude Meteorological data
- Angstrom Penman–Monteith combination equation
- animation Profiles
- annotation Figure editor
- Annotations (Figure editor) Figure editor
- Arrhenius Solute transport: temperature and water-content dependence, colloids
- Arrhenius Temperature and water-content dependence of reactions
- artificial dispersion Solute transport: general
- artificial dispersion Numerical solution
- ATMOSPH.IN Time-variable boundary data
- atmospheric boundary condition Boundary conditions of water flow
- atmospheric boundary condition Water flow boundary conditions
- Atmospheric boundary condition (Boundary conditions of water flow) Boundary conditions of water flow
- atmospheric data Time-variable boundary data
- Atmospheric inputs: partitioning, daily variation, interception, snow Atmospheric inputs: partitioning, daily variation, interception, snow
- attachment Colloid, virus and bacteria transport
- Attachment from filtration theory (Colloid, virus and bacteria transport) Colloid, virus and bacteria transport
- authors Credits and license
- Axes (Figure editor) Figure editor
- axis Figure editor
- bacteria Solute transport: temperature and water-content dependence, colloids
- bacteria Colloid, virus and bacteria transport
- BALANCE Output files
- balance error Mass balance
- BALANCE.csv – mass balance (Output files) Output files
- Balance.out Mass balance
- batch Command line program
- bibliography References
- BIC Parameter estimation results
- BIC Parameter estimation
- blocking Solute transport: temperature and water-content dependence, colloids
- blocking Colloid, virus and bacteria transport
- Blocking and straining functions (Colloid, virus and bacteria transport) Colloid, virus and bacteria transport
- bootstrap Pedotransfer functions (Rosetta)
- Boundary and initial conditions (Variably saturated water flow) Variably saturated water flow
- boundary conditions Boundary conditions of water flow
- boundary conditions Water flow boundary conditions
- Boundary conditions (Heat transport) Heat transport
- Boundary conditions (Heat transport) Heat transport
- Boundary conditions (Solute transport equations) Solute transport equations
- Boundary conditions of water flow Boundary conditions of water flow
- Boundary fluxes (Dual-permeability model) Dual-permeability model
- Boundary fluxes, heads and cumulative quantities Boundary fluxes, heads and cumulative quantities
- boundary information Boundary fluxes, heads and cumulative quantities
- breakthrough curve Observation points
- Brooks and Corey (Soil hydraulic property models) Soil hydraulic property models
- Brooks Corey Soil hydraulic model
- Brooks Corey Soil hydraulic property models
- Building a figure (Figure editor) Figure editor
- bulk density Neural network prediction (Rosetta)
- bulk density Solute transport: transport parameters
- bulk density Pedotransfer functions (Rosetta)
- C(h) Soil hydraulic properties
- Campbell Heat transport
- Campbell Heat transport
- Canopy interception (Atmospheric inputs: partitioning, daily variation, interception, snow) Atmospheric inputs: partitioning, daily variation, interception, snow
- canopy resistance Penman–Monteith combination equation
- capabilities Introduction to Rusteau-1D
- caption Figure editor
- Carsel Parrish Materials & parameters
- Cauchy Solute transport: boundary conditions
- centrifugal acceleration Non-equilibrium water flow, centrifuge and density-dependent flow
- centrifuge Further options of the HYDRUS code
- centrifuge Non-equilibrium water flow, centrifuge and density-dependent flow
- Centrifuge (lCentrif) (Further options of the HYDRUS code) Further options of the HYDRUS code
- Centrifuge (Non-equilibrium water flow, centrifuge and density-dependent flow) Non-equilibrium water flow, centrifuge and density-dependent flow
- Chapters (Rusteau-1D Help) Rusteau-1D Help
- chart Figure editor
- check Check & run
- Check & run Check & run
- Checks (Check & run) Check & run
- chemical non-equilibrium Non-equilibrium solute transport
- Chung Horton Heat transport
- Chung Horton Heat transport
- citations References
- CLI Command line program
- colloid attachment Solute transport: temperature and water-content dependence, colloids
- Colloid attachment parameters (Solute transport: temperature and water-content dependence, colloids) Solute transport: temperature and water-content dependence, colloids
- Colloid, virus and bacteria transport Colloid, virus and bacteria transport
- colloids Solute transport: general
- colloids Colloid, virus and bacteria transport
- colour Figure editor
- Columns (Mass balance) Mass balance
- Columns (Time-variable boundary data) Time-variable boundary data
- command line Command line program
- Command line program Command line program
- compare runs Comparison of runs
- comparison Measured data
- comparison Comparison of runs
- Comparison of runs Comparison of runs
- compatibility Relation to HYDRUS-1D
- Compatibility (Relation to HYDRUS-1D) Relation to HYDRUS-1D
- Compensated root water uptake (Root water uptake) Root water uptake
- compensated uptake Root water uptake
- compensation Root water and solute uptake
- compensation Root solute uptake
- concentration boundary condition Solute transport: boundary conditions
- concentration flux Solute transport: boundary conditions
- Concentrations (Solute transport: boundary conditions) Solute transport: boundary conditions
- Concentrations oscillate or become negative (Questions and problems) Questions and problems
- conduction Heat transport
- conductivity function Soil hydraulic properties
- conductivity function Soil hydraulic property models
- confidence intervals Parameter estimation results
- confidence intervals Parameter estimation
- constant flux Water flow boundary conditions
- constant head Water flow boundary conditions
- constraints Parameter estimation (inverse problem)
- contents Rusteau-1D Help
- convection Heat transport
- convection dispersion Solute transport equations
- convergence Questions and problems
- convergence Iteration criteria
- correlation Parameter estimation
- correlation matrix Parameter estimation results
- coupled transport Coupled water, vapor and heat flow
- Coupled water, vapor and heat flow Coupled water, vapor and heat flow
- Coupling (Surface energy balance) Surface energy balance
- Courant number Run-time information
- Courant number Notes on spatial and temporal discretization
- Crank-Nicolson Solute transport: general
- Crank-Nicolson Numerical solution
- credits Credits and license
- Credits and license Credits and license
- crop Meteorological data
- Crop (Meteorological data) Meteorological data
- CSV Figure editor
- CSV Measured data
- CSV Output files
- Ctrl+S Keyboard and mouse
- cumulative fluxes Boundary fluxes, heads and cumulative quantities
- Curves (Materials & parameters) Materials & parameters
- daily variation Atmospheric inputs: partitioning, daily variation, interception, snow
- daily variation Time-variable boundary data
- Daily variation of evaporation and transpiration (Atmospheric inputs: partitioning, daily variation, interception, snow) Atmospheric inputs: partitioning, daily variation, interception, snow
- data file Figure editor
- Data files (Figure editor) Figure editor
- Data of Fit.in (Measured data) Measured data
- data types Parameter estimation (inverse problem)
- de Vries Heat transport
- decay Solute transport: reactions
- decay chain Solute transport: reactions
- decay chain Solute transport equations
- deep drainage Boundary conditions of water flow
- deep drainage Water flow boundary conditions
- Deep drainage (Boundary conditions of water flow) Boundary conditions of water flow
- definitions Symbols and glossary
- degradation Temperature and water-content dependence of reactions
- degree-day Atmospheric inputs: partitioning, daily variation, interception, snow
- demonstration Examples
- density-dependent flow Further options of the HYDRUS code
- density-dependent flow Non-equilibrium water flow, centrifuge and density-dependent flow
- Density-dependent flow (lDensity) (Further options of the HYDRUS code) Further options of the HYDRUS code
- Density-dependent flow (Non-equilibrium water flow, centrifuge and density-dependent flow) Non-equilibrium water flow, centrifuge and density-dependent flow
- detachment Colloid, virus and bacteria transport
- diagram Figure editor
- differences Relation to HYDRUS-1D
- diffusion coefficient Solute transport: transport parameters
- dimensions Units
- Dirichlet Solute transport: boundary conditions
- Dirichlet Boundary conditions of water flow
- disclaimer Credits and license
- discretization Soil profile
- discretization Notes on spatial and temporal discretization
- Dispersion (Solute transport equations) Solute transport equations
- dispersion coefficient Solute transport equations
- dispersivity Solute transport: transport parameters
- dpi Figure editor
- drag and drop The main window
- Drag and drop (Keyboard and mouse) Keyboard and mouse
- Drag and drop (The main window) The main window
- drains Boundary conditions of water flow
- dtMax Time & output
- dtMin Time & output
- dual non-equilibrium Non-equilibrium solute transport
- Dual non-equilibrium (Non-equilibrium solute transport) Non-equilibrium solute transport
- dual permeability Soil hydraulic model
- dual permeability Dual-permeability model
- Dual permeability (Non-equilibrium solute transport) Non-equilibrium solute transport
- dual porosity Soil hydraulic model
- dual porosity Dual-porosity models
- dual porosity Non-equilibrium solute transport
- Dual porosity inside the matrix (Dual-permeability model) Dual-permeability model
- Dual-permeability model Dual-permeability model
- Dual-permeability parameters (Soil hydraulic model) Soil hydraulic model
- Dual-porosity models Dual-porosity models
- During the run (Parameter estimation results) Parameter estimation results
- Durner Soil hydraulic model
- Durner Soil hydraulic property models
- Durner (dual porosity) (Soil hydraulic property models) Soil hydraulic property models
- Durner's model (Dual-porosity models) Dual-porosity models
- effective saturation Soil hydraulic property models
- element size Notes on spatial and temporal discretization
- emissivity Surface energy balance
- energy balance Meteorological data
- energy balance Surface energy balance
- enhancement factor Further options of the HYDRUS code
- enhancement factor Coupled water, vapor and heat flow
- Ernst Boundary conditions of water flow
- errors Questions and problems
- Estimate (Parameter estimation (inverse problem)) Parameter estimation (inverse problem)
- evaporation Surface energy balance
- evaporation Time-variable boundary data
- example Getting started
- example projects Examples
- Examples Examples
- Examples (Projects and files) Projects and files
- export Figure editor
- export Output files
- export Projects and files
- Export (Figure editor) Figure editor
- export help Command line program
- Extensions (Variably saturated water flow) Variably saturated water flow
- extrapolation Further options of the HYDRUS code
- extraterrestrial radiation Hargreaves equation
- F1 Keyboard and mouse
- F5 Check & run
- F5 Keyboard and mouse
- FAO-56 Penman–Monteith combination equation
- FAQ Questions and problems
- features Introduction to Rusteau-1D
- Feddes Root water and solute uptake
- Feddes Root water uptake
- Feddes parameters (Root water and solute uptake) Root water and solute uptake
- Figure (Figure editor) Figure editor
- Figure editor Figure editor
- Figure editor (Keyboard and mouse) Keyboard and mouse
- figures Figure editor
- file menu Projects and files
- filtration theory Solute transport: temperature and water-content dependence, colloids
- filtration theory Colloid, virus and bacteria transport
- final time Time & output
- finite elements Numerical solution
- first simulation Getting started
- first-order Solute transport: reactions
- first-order decay Solute transport equations
- Fit.in Parameter estimation (inverse problem)
- Fit.in Projects and files
- Fit.in Parameter estimation
- Fit.in (Projects and files) Projects and files
- Fit.in data Measured data
- Fit.out Parameter estimation results
- Fit.out (Output files) Output files
- fitted parameters Parameter estimation results
- fixed points Soil profile
- font Figure editor
- Font and text sizes (Figure editor) Figure editor
- Fonts (Credits and license) Credits and license
- fraction of equilibrium sites Solute transport: transport parameters
- fractures Dual-permeability model
- free drainage Boundary conditions of water flow
- free drainage Water flow boundary conditions
- Free drainage (Boundary conditions of water flow) Boundary conditions of water flow
- Freundlich Solute transport: reactions
- Freundlich Solute transport equations
- frozen time levels Parameter estimation
- further options Further options of the HYDRUS code
- Further options of the HYDRUS code Further options of the HYDRUS code
- Galerkin Numerical solution
- Gas phase (Solute transport equations) Solute transport equations
- general solute information Solute transport: general
- Geographical and radiation parameters (Meteorological data) Meteorological data
- Gerke van Genuchten Dual-permeability model
- Getting started Getting started
- glossary Symbols and glossary
- Glossary (Symbols and glossary) Symbols and glossary
- Good practice (Parameter estimation) Parameter estimation
- goodness of fit Parameter estimation results
- governing equation Variably saturated water flow
- Governing equation (Solute transport equations) Solute transport equations
- Governing equations (Dual-permeability model) Dual-permeability model
- Governing equations (Dual-porosity models) Dual-porosity models
- GPL Credits and license
- graph Figure editor
- h1d Projects and files
- h1dr Projects and files
- Hargreaves Meteorological data
- Hargreaves Hargreaves equation
- Hargreaves equation Hargreaves equation
- Hargreaves-Samani Hargreaves equation
- hCritA Boundary conditions of water flow
- hCritA Time-variable boundary data
- hCritS Boundary conditions of water flow
- hCritS Water flow boundary conditions
- heat capacity Heat transport
- heat capacity Heat transport
- Heat capacity (Heat transport) Heat transport
- Heat transport Heat transport
- heat transport Processes & units
- Heat transport Heat transport
- heat transport parameters Heat transport
- help Rusteau-1D Help
- Help window (The main window) The main window
- Henry Solute transport: reactions
- Henry Solute transport equations
- hierarchical Pedotransfer functions (Rosetta)
- Hints (Comparison of runs) Comparison of runs
- Hints (Solute transport: reactions) Solute transport: reactions
- Hints (Time & output) Time & output
- Hooghoudt Boundary conditions of water flow
- horizontal drains Water flow boundary conditions
- Horizontal drains (Boundary conditions of water flow) Boundary conditions of water flow
- hotkeys Keyboard and mouse
- How do I cite the methods? (Questions and problems) Questions and problems
- How do I make a figure for a paper or a presentation? (Questions and problems) Questions and problems
- How to use this help (Rusteau-1D Help) Rusteau-1D Help
- hTab Iteration criteria
- humidity Meteorological data
- hydraulic conductivity Variably saturated water flow
- Hydraulic models (Soil hydraulic model) Soil hydraulic model
- hydrostatic equilibrium Soil profile
- HYDRUS 4.17 Relation to HYDRUS-1D
- HYDRUS variable names Symbols and glossary
- HYDRUS variable names (Symbols and glossary) Symbols and glossary
- HYDRUS-1D Relation to HYDRUS-1D
- HYDRUS-1D Introduction to Rusteau-1D
- HYDRUS-1D examples (Examples) Examples
- HYDRUS-1D project Projects and files
- HYDRUS-1D projects (.h1d) (Projects and files) Projects and files
- hysteresis Soil hydraulic model
- Hysteresis Hysteresis
- Hysteresis (Soil hydraulic model) Soil hydraulic model
- hysteresis curves Soil hydraulic properties
- Hysteresis.in Soil hydraulic model
- iEnhanc Further options of the HYDRUS code
- immobile water Dual-porosity models
- immobile water content Solute transport: transport parameters
- import Projects and files
- import data Measured data
- inclination Variably saturated water flow
- Inclination (Soil profile) Soil profile
- infiltration Boundary fluxes, heads and cumulative quantities
- Infiltration & evaporation with roots (Examples) Examples
- initial condition Soil profile
- Initial condition (Non-equilibrium solute transport) Non-equilibrium solute transport
- initial estimates Parameter estimation (inverse problem)
- Initial hysteresis state (Hysteresis.in) (Soil hydraulic model) Soil hydraulic model
- initial time Time & output
- Input data (Neural network prediction (Rosetta)) Neural network prediction (Rosetta)
- interception Atmospheric inputs: partitioning, daily variation, interception, snow
- interception Time-variable boundary data
- Interface (Credits and license) Credits and license
- Internal interpolation tables (Iteration criteria) Iteration criteria
- interpolation tables Iteration criteria
- interpolation tables Numerical solution
- Interpolation tables (Numerical solution) Numerical solution
- Interpreting the results (Parameter estimation results) Parameter estimation results
- introduction Introduction to Rusteau-1D
- Introduction to Rusteau-1D Introduction to Rusteau-1D
- inverse problem Parameter estimation (inverse problem)
- inverse problem Processes & units
- inverse problem Parameter estimation
- inverse results Parameter estimation results
- IRRIG.csv (Output files) Output files
- isothermal vapor flux Coupled water, vapor and heat flow
- Iteration (Parameter estimation (inverse problem)) Parameter estimation (inverse problem)
- Iteration criteria Iteration criteria
- iterations Parameter estimation results
- iterations Run-time information
- JSON Comparison of runs
- K(h) Soil hydraulic properties
- K(theta) Soil hydraulic properties
- Kd Solute transport: reactions
- keep results Comparison of runs
- Keeping and loading runs (Comparison of runs) Comparison of runs
- kept run Comparison of runs
- Keyboard (Keyboard and mouse) Keyboard and mouse
- Keyboard and mouse Keyboard and mouse
- keyboard shortcuts Keyboard and mouse
- kinetic sorption Non-equilibrium solute transport
- Kool and Parker model (Hysteresis) Hysteresis
- Kool Parker Hysteresis
- Kosugi Soil hydraulic model
- Kosugi Soil hydraulic property models
- Kosugi (log-normal) (Soil hydraulic property models) Soil hydraulic property models
- Ks Materials & parameters
- l Materials & parameters
- LAI Meteorological data
- LAI Atmospheric inputs: partitioning, daily variation, interception, snow
- LAI Time-variable boundary data
- Langmuir Solute transport: reactions
- Langmuir Colloid, virus and bacteria transport
- Langmuir Solute transport equations
- latent heat Surface energy balance
- latitude Meteorological data
- layer Figure editor
- lCentrif Further options of the HYDRUS code
- lDensity Further options of the HYDRUS code
- leaf area index Atmospheric inputs: partitioning, daily variation, interception, snow
- legend Figure editor
- length unit Units
- Lenhard Hysteresis
- lExtrap Further options of the HYDRUS code
- license Credits and license
- License (Credits and license) Credits and license
- Limitations (Pedotransfer functions (Rosetta)) Pedotransfer functions (Rosetta)
- linear sorption Solute transport equations
- literature References
- load run Comparison of runs
- Loading (Measured data) Measured data
- logarithmic axis Figure editor
- logistic function Root water uptake
- logistic growth Root water and solute uptake
- long-wave radiation Penman–Monteith combination equation
- look-up tables Soil hydraulic model
- Look-up tables (Soil hydraulic property models) Soil hydraulic property models
- lower boundary Water flow boundary conditions
- Lower boundary (Solute transport: boundary conditions) Solute transport: boundary conditions
- Lower boundary (Water flow boundary conditions) Water flow boundary conditions
- macropores Dual-permeability model
- main drying curve Hysteresis
- main processes Processes & units
- main wetting curve Hysteresis
- main window The main window
- markup Figure editor
- Marquardt Parameter estimation (inverse problem)
- Marquardt-Levenberg Parameter estimation
- Marquardt–Levenberg iteration (Parameter estimation) Parameter estimation
- Mass balance Mass balance
- Mass balance (Numerical solution) Numerical solution
- mass balance error Questions and problems
- mass conservative Numerical solution
- mass transfer Dual-porosity models
- mass transfer coefficient Non-equilibrium solute transport
- Mass transfer driven by the pressure head (Dual-porosity models) Dual-porosity models
- Mass transfer driven by the water content (Dual-porosity models) Dual-porosity models
- mass unit Units
- materials Soil profile
- materials Materials & parameters
- Materials & parameters Materials & parameters
- Materials (Materials & parameters) Materials & parameters
- matrix Dual-permeability model
- maximum number of iterations Iteration criteria
- Measured data Measured data
- menu The main window
- Menu bar (The main window) The main window
- mesh Notes on spatial and temporal discretization
- METEO.csv and Meteo.out (Output files) Output files
- METEO.IN Meteorological data
- Meteo.out Output files
- Meteorological data Meteorological data
- meteorological data Processes & units
- Method (Pedotransfer functions (Rosetta)) Pedotransfer functions (Rosetta)
- Michaelis-Menten Root water and solute uptake
- Michaelis-Menten Root solute uptake
- Miller Miller Scaling of the hydraulic properties
- Millington Quirk Solute transport: general
- mobile immobile Dual-porosity models
- mobile immobile Non-equilibrium solute transport
- Mobile–immobile water (physical non-equilibrium) (Non-equilibrium solute transport) Non-equilibrium solute transport
- Models (Neural network prediction (Rosetta)) Neural network prediction (Rosetta)
- modified van Genuchten Soil hydraulic property models
- Modified van Genuchten (Vogel and Císlerová) (Soil hydraulic property models) Soil hydraulic property models
- MoistDep Temperature and water-content dependence of reactions
- MoistDep.in Solute transport: temperature and water-content dependence, colloids
- moisture dependence Temperature and water-content dependence of reactions
- molecular diffusion Solute transport: transport parameters
- Molecular diffusion (Solute transport: transport parameters) Solute transport: transport parameters
- mouse Keyboard and mouse
- Moving fronts (Notes on spatial and temporal discretization) Notes on spatial and temporal discretization
- Mualem Soil hydraulic property models
- n Materials & parameters
- navigation The main window
- Navigation panel (The main window) The main window
- net radiation Penman–Monteith combination equation
- Net radiation (Surface energy balance) Surface energy balance
- Neumann Boundary conditions of water flow
- neural network Neural network prediction (Rosetta)
- neural network Pedotransfer functions (Rosetta)
- Neural network prediction (Rosetta) Neural network prediction (Rosetta)
- Neural network prediction (Rosetta) (Materials & parameters) Materials & parameters
- new project Workflow of a project
- Next steps (Getting started) Getting started
- No file dialog appears (Linux) (Questions and problems) Questions and problems
- NOD_INF Output files
- Nod_Inf Profiles
- NOD_INF.csv – profiles at the print times (Output files) Output files
- node spacing Notes on spatial and temporal discretization
- nodes Soil profile
- non-convergence Questions and problems
- non-equilibrium Solute transport: general
- non-equilibrium flow Dual-porosity models
- non-equilibrium rate Solute transport: reactions
- Non-equilibrium solute transport Non-equilibrium solute transport
- non-equilibrium transport Non-equilibrium solute transport
- Non-equilibrium transport (Solute transport equations) Solute transport equations
- non-equilibrium water flow Further options of the HYDRUS code
- non-equilibrium water flow Non-equilibrium water flow, centrifuge and density-dependent flow
- Non-equilibrium water flow (Non-equilibrium water flow, centrifuge and density-dependent flow) Non-equilibrium water flow, centrifuge and density-dependent flow
- Non-equilibrium water flow, centrifuge and density-dependent flow Non-equilibrium water flow, centrifuge and density-dependent flow
- non-isothermal flow Coupled water, vapor and heat flow
- Not included (Introduction to Rusteau-1D) Introduction to Rusteau-1D
- Not supported (Relation to HYDRUS-1D) Relation to HYDRUS-1D
- notation Symbols and glossary
- Notes on spatial and temporal discretization Notes on spatial and temporal discretization
- Noto Sans Figure editor
- Number fields (Keyboard and mouse) Keyboard and mouse
- number of solutes Solute transport: general
- numerical dispersion Notes on spatial and temporal discretization
- Numerical methods (Credits and license) Credits and license
- numerical oscillations Notes on spatial and temporal discretization
- Numerical scheme (Solute transport: general) Solute transport: general
- Numerical solution Numerical solution
- Numerical solution (Heat transport) Heat transport
- Numerical solution (Solute transport equations) Solute transport equations
- nutrient uptake Root solute uptake
- objective function Parameter estimation (inverse problem)
- objective function Parameter estimation
- Objective function (Parameter estimation) Parameter estimation
- OBS_NODE Output files
- Obs_Node Observation points
- OBS_NODE.csv – observation nodes (Output files) Output files
- observation nodes Soil profile
- observation nodes Observation points
- Observation nodes (Soil profile) Soil profile
- Observation points Observation points
- observations Parameter estimation (inverse problem)
- observations Measured data
- Observations (Parameter estimation (inverse problem)) Parameter estimation (inverse problem)
- omega c Root water and solute uptake
- open Projects and files
- optimization Parameter estimation (inverse problem)
- Options (Time-variable boundary data) Time-variable boundary data
- Options.in Further options of the HYDRUS code
- Options.in Non-equilibrium water flow, centrifuge and density-dependent flow
- oscillations Questions and problems
- Osmotic (salinity) stress (Root water uptake) Root water uptake
- osmotic stress Root water and solute uptake
- osmotic stress Root water uptake
- output Output files
- output Time & output
- Output files Output files
- overview Rusteau-1D Help
- overview Introduction to Rusteau-1D
- Overview (Check & run) Check & run
- Pages (The main window) The main window
- palette Figure editor
- panel Figure editor
- Panels and layers (Figure editor) Figure editor
- parameter estimation Parameter estimation (inverse problem)
- Parameter estimation Parameter estimation
- Parameter estimation (inverse problem) Parameter estimation (inverse problem)
- Parameter estimation (Relation to HYDRUS-1D) Relation to HYDRUS-1D
- Parameter estimation (Workflow of a project) Workflow of a project
- Parameter estimation results Parameter estimation results
- Parameter estimation: one-step outflow (Examples) Examples
- Parameter estimation: soil temperature (Examples) Examples
- Parameters (Colloid, virus and bacteria transport) Colloid, virus and bacteria transport
- Parameters (Hysteresis) Hysteresis
- Parameters (Materials & parameters) Materials & parameters
- Parameters (Parameter estimation (inverse problem)) Parameter estimation (inverse problem)
- Parameters (Solute transport: reactions) Solute transport: reactions
- Parameters per material (Heat transport) Heat transport
- partitioning Atmospheric inputs: partitioning, daily variation, interception, snow
- Partitioning (Penman–Monteith combination equation) Penman–Monteith combination equation
- Partitioning of the potential evapotranspiration (Atmospheric inputs: partitioning, daily variation, interception, snow) Atmospheric inputs: partitioning, daily variation, interception, snow
- passive uptake Root water and solute uptake
- passive uptake Root solute uptake
- Passive uptake (Root solute uptake) Root solute uptake
- Peclet Solute transport: general
- Peclet number Run-time information
- Peclet number Notes on spatial and temporal discretization
- pedotransfer functions Neural network prediction (Rosetta)
- pedotransfer functions Pedotransfer functions (Rosetta)
- Pedotransfer functions (Credits and license) Credits and license
- Pedotransfer functions (Rosetta) Pedotransfer functions (Rosetta)
- Penman-Monteith Meteorological data
- Penman-Monteith Penman–Monteith combination equation
- Penman–Monteith combination equation Penman–Monteith combination equation
- Per material (Solute transport: transport parameters) Solute transport: transport parameters
- performance Run-time information
- Philip de Vries Coupled water, vapor and heat flow
- physical non-equilibrium Non-equilibrium solute transport
- Picard iteration Numerical solution
- plot Figure editor
- plots Keyboard and mouse
- Plots (Keyboard and mouse) Keyboard and mouse
- PNG Figure editor
- ponding Boundary conditions of water flow
- ponding Water flow boundary conditions
- pore connectivity Materials & parameters
- port Relation to HYDRUS-1D
- potential evapotranspiration Atmospheric inputs: partitioning, daily variation, interception, snow
- potential evapotranspiration Hargreaves equation
- potential evapotranspiration Penman–Monteith combination equation
- precipitation Time-variable boundary data
- precision Relation to HYDRUS-1D
- Precision (Relation to HYDRUS-1D) Relation to HYDRUS-1D
- preferential flow Dual-permeability model
- preferential flow Dual-porosity models
- pressure head Variably saturated water flow
- Pressure head and flux conditions (Boundary conditions of water flow) Boundary conditions of water flow
- pressure head profile Profiles
- pressure head tolerance Iteration criteria
- print times Profiles
- print times Time & output
- Printing (Time & output) Time & output
- problems Check & run
- problems Questions and problems
- procedure Workflow of a project
- Processes & units Processes & units
- Processes (Processes & units) Processes & units
- production Solute transport: reactions
- Profile depth and discretization (Soil profile) Soil profile
- profile editor Soil profile
- profile editor Keyboard and mouse
- profile information Profiles
- PROFILE.DAT Soil profile
- Profiles Profiles
- project Projects and files
- Project and units (Processes & units) Processes & units
- project title Processes & units
- Projects and files Projects and files
- psychrometric constant Penman–Monteith combination equation
- PTF Neural network prediction (Rosetta)
- PTF Pedotransfer functions (Rosetta)
- publication figure Figure editor
- pulse duration Solute transport: boundary conditions
- pumping effect Hysteresis
- Quantities (Soil profile) Soil profile
- Questions and problems Questions and problems
- quick start Getting started
- R2 Parameter estimation results
- radiation Meteorological data
- Radiation (Penman–Monteith combination equation) Penman–Monteith combination equation
- Radiation and cloudiness (Meteorological data) Meteorological data
- random sequential adsorption Colloid, virus and bacteria transport
- reaction parameters Solute transport: reactions
- records Time-variable boundary data
- Records (Meteorological data) Meteorological data
- References References
- Related topics (Processes & units) Processes & units
- Relation to HYDRUS-1D Relation to HYDRUS-1D
- resolution Figure editor
- restart Soil hydraulic model
- Result (Neural network prediction (Rosetta)) Neural network prediction (Rosetta)
- Results (Parameter estimation results) Parameter estimation results
- Results (Projects and files) Projects and files
- results file Comparison of runs
- results files Output files
- retardation Solute transport equations
- retention curve Soil hydraulic properties
- retention curve Soil hydraulic property models
- reversal point Hysteresis
- Richards equation Variably saturated water flow
- ripening Colloid, virus and bacteria transport
- root distribution Soil profile
- root distribution Root water uptake
- Root distribution (Root water uptake) Root water uptake
- Root distribution and growth (Root water and solute uptake) Root water and solute uptake
- root growth Processes & units
- root growth Root water and solute uptake
- root growth Root water uptake
- Root growth (Root water uptake) Root water uptake
- Root solute uptake Root solute uptake
- Root solute uptake (Root water and solute uptake) Root water and solute uptake
- Root water and solute uptake Root water and solute uptake
- root water uptake Processes & units
- root water uptake Root water and solute uptake
- Root water uptake Root water uptake
- Root water uptake model (Root water and solute uptake) Root water and solute uptake
- Rosetta Neural network prediction (Rosetta)
- Rosetta Materials & parameters
- Rosetta Pedotransfer functions (Rosetta)
- Rosetta 3 Neural network prediction (Rosetta)
- Rosetta Lite Neural network prediction (Rosetta)
- Ross Smettem Non-equilibrium water flow, centrifuge and density-dependent flow
- RSA Colloid, virus and bacteria transport
- run Check & run
- run time information Run-time information
- Run-time information Run-time information
- Run_Inf Run-time information
- Running (Check & run) Check & run
- runoff Boundary fluxes, heads and cumulative quantities
- runoff Boundary conditions of water flow
- runoff Water flow boundary conditions
- Rusteau iteration (Parameter estimation) Parameter estimation
- Rusteau projects (.h1dr) (Projects and files) Projects and files
- Rusteau-1D Help Rusteau-1D Help
- rusteau-cli Command line program
- S-shape Root water and solute uptake
- S-shape Root water uptake
- salinity Root water uptake
- sand silt clay Neural network prediction (Rosetta)
- save Projects and files
- save run Comparison of runs
- scaling factors Soil profile
- scaling factors Scaling of the hydraulic properties
- Scaling of the hydraulic properties Scaling of the hydraulic properties
- scanning curves Hysteresis
- scenario Comparison of runs
- scripting Command line program
- See also (Figure editor) Figure editor
- seepage face Boundary conditions of water flow
- seepage face Water flow boundary conditions
- Seepage face (Boundary conditions of water flow) Boundary conditions of water flow
- Selecting nodes (Soil profile) Soil profile
- Sensible and latent heat (Surface energy balance) Surface energy balance
- sensible heat Surface energy balance
- sensitivity Comparison of runs
- setting up a model Workflow of a project
- Setting values in the selection (Soil profile) Soil profile
- Showing runs in a figure (Comparison of runs) Comparison of runs
- similar media Scaling of the hydraulic properties
- sink term Variably saturated water flow
- sink term Root water uptake
- Sink term (Root water uptake) Root water uptake
- Sinusoidal precipitation (Atmospheric inputs: partitioning, daily variation, interception, snow) Atmospheric inputs: partitioning, daily variation, interception, snow
- slow simulation Questions and problems
- snow Atmospheric inputs: partitioning, daily variation, interception, snow
- snow Time-variable boundary data
- Snow (Atmospheric inputs: partitioning, daily variation, interception, snow) Atmospheric inputs: partitioning, daily variation, interception, snow
- snow melt Atmospheric inputs: partitioning, daily variation, interception, snow
- soil catalog Materials & parameters
- Soil catalog (Materials & parameters) Materials & parameters
- soil cover fraction Atmospheric inputs: partitioning, daily variation, interception, snow
- soil heat flux Surface energy balance
- Soil hydraulic model Soil hydraulic model
- soil hydraulic parameters Materials & parameters
- Soil hydraulic properties Soil hydraulic properties
- Soil hydraulic property models Soil hydraulic property models
- Soil profile Soil profile
- Soil profile editor (Keyboard and mouse) Keyboard and mouse
- soil surface resistance Surface energy balance
- Solute and heat transport (Notes on spatial and temporal discretization) Notes on spatial and temporal discretization
- Solute and heat transport (Numerical solution) Numerical solution
- solute boundary conditions Solute transport: boundary conditions
- solute fluxes Boundary fluxes, heads and cumulative quantities
- solute front Notes on spatial and temporal discretization
- solute mass balance Mass balance
- Solute pulse with sorption and decay (Examples) Examples
- solute stress Root water and solute uptake
- Solute stress parameters (Root water and solute uptake) Root water and solute uptake
- solute transfer Dual-permeability model
- solute transport Processes & units
- solute transport Solute transport: general
- Solute transport (Dual-permeability model) Dual-permeability model
- Solute transport (Dual-porosity models) Dual-porosity models
- Solute transport equations Solute transport equations
- solute transport parameters Solute transport: transport parameters
- Solute transport: boundary conditions Solute transport: boundary conditions
- Solute transport: general Solute transport: general
- Solute transport: reactions Solute transport: reactions
- Solute transport: temperature and water-content dependence, colloids Solute transport: temperature and water-content dependence, colloids
- Solute transport: transport parameters Solute transport: transport parameters
- Solutes (Solute transport: general) Solute transport: general
- sorption Solute transport: reactions
- sorption Solute transport equations
- Sorption (Solute transport equations) Solute transport equations
- sources References
- spatial variability Scaling of the hydraulic properties
- standard error Parameter estimation results
- start calculation Check & run
- start page Rusteau-1D Help
- starting points Parameter estimation results
- starting points Parameter estimation
- Statistics (Parameter estimation) Parameter estimation
- status bar The main window
- Step 1 – Project (Workflow of a project) Workflow of a project
- Step 2 – Soil (Workflow of a project) Workflow of a project
- Step 3 – Boundary conditions (Workflow of a project) Workflow of a project
- Step 4 – Uptake and transport (Workflow of a project) Workflow of a project
- Step 5 – Run (Workflow of a project) Workflow of a project
- step by step Getting started
- steps Workflow of a project
- stop Check & run
- straining Solute transport: temperature and water-content dependence, colloids
- straining Colloid, virus and bacteria transport
- structured soils Dual-porosity models
- sub-regions Soil profile
- sub-regions Mass balance
- Sub-regions (Mass balance) Mass balance
- subtitle Figure editor
- summary Check & run
- sunshine Meteorological data
- Surface energy balance Surface energy balance
- surface temperature Surface energy balance
- SVG Figure editor
- symbols Figure editor
- symbols Symbols and glossary
- Symbols (Symbols and glossary) Symbols and glossary
- Symbols and glossary Symbols and glossary
- T_LEVEL Output files
- T_Level Boundary fluxes, heads and cumulative quantities
- T_LEVEL.csv – time-level information (Output files) Output files
- T_LEVEL1.csv – extended fluxes (Output files) Output files
- TauW Further options of the HYDRUS code
- TauW Non-equilibrium water flow, centrifuge and density-dependent flow
- temperature Heat transport
- Temperature and water-content dependence of reactions Temperature and water-content dependence of reactions
- temperature boundary conditions Heat transport
- temperature dependence Soil hydraulic model
- temperature dependence Solute transport: temperature and water-content dependence, colloids
- temperature dependence Soil hydraulic property models
- temperature dependence Temperature and water-content dependence of reactions
- Temperature dependence (Soil hydraulic model) Soil hydraulic model
- Temperature dependence (Soil hydraulic property models) Soil hydraulic property models
- Temperature dependence (Temperature and water-content dependence of reactions) Temperature and water-content dependence of reactions
- temperature-based Hargreaves equation
- template Figure editor
- text file Measured data
- Text: markup and symbols (Figure editor) Figure editor
- texture Neural network prediction (Rosetta)
- texture Pedotransfer functions (Rosetta)
- The actual transpiration is smaller than the potential one (Questions and problems) Questions and problems
- The calculation stops: the iteration does not converge (Questions and problems) Questions and problems
- The interface (Introduction to Rusteau-1D) Introduction to Rusteau-1D
- The main window The main window
- The mass balance error is large (Questions and problems) Questions and problems
- The parameter l (Materials & parameters) Materials & parameters
- The program stopped unexpectedly (Questions and problems) Questions and problems
- The pumping effect and the model of Lenhard et al. (Hysteresis) Hysteresis
- The results differ from HYDRUS-1D (Questions and problems) Questions and problems
- The run is slow (Questions and problems) Questions and problems
- The window (Figure editor) Figure editor
- theme Figure editor
- themes The main window
- Themes (The main window) The main window
- thermal conductivity Heat transport
- thermal conductivity Heat transport
- Thermal conductivity (Heat transport) Heat transport
- thermal dispersivity Heat transport
- thermal dispersivity Heat transport
- thermal vapor flux Coupled water, vapor and heat flow
- theta r Materials & parameters
- theta s Materials & parameters
- theta(h) Soil hydraulic properties
- Thomas algorithm Numerical solution
- Time & output Time & output
- time discretization Time & output
- Time discretization (Time & output) Time & output
- time information Time & output
- time series Observation points
- time slider Profiles
- time step Time & output
- time step control Numerical solution
- Time step control (Numerical solution) Numerical solution
- time steps Run-time information
- time unit Units
- time weighting Solute transport: general
- time-variable boundary conditions Time-variable boundary data
- Time-variable boundary data Time-variable boundary data
- Time-variable conditions (Boundary conditions of water flow) Boundary conditions of water flow
- Tips (Workflow of a project) Workflow of a project
- title Figure editor
- tolerance Iteration criteria
- tooltips The main window
- tortuosity Solute transport: general
- tortuosity Solute transport equations
- transpiration Root water uptake
- transpiration Time-variable boundary data
- Transport model (Solute transport: general) Solute transport: general
- triggered irrigation Water flow boundary conditions
- Triggered irrigation (Water flow boundary conditions) Water flow boundary conditions
- troubleshooting Questions and problems
- tutorial Getting started
- tutorial projects Examples
- two-region Non-equilibrium solute transport
- two-site sorption Non-equilibrium solute transport
- Two-site sorption (chemical non-equilibrium) (Non-equilibrium solute transport) Non-equilibrium solute transport
- Typical behaviour (Non-equilibrium solute transport) Non-equilibrium solute transport
- Typical values (Soil hydraulic property models) Soil hydraulic property models
- unit conversion Units
- Unit conversion (Units) Units
- units Processes & units
- Units Units
- Units of the heat parameters (Units) Units
- unsaturated flow Variably saturated water flow
- UNSODA Pedotransfer functions (Rosetta)
- upper boundary Water flow boundary conditions
- Upper boundary (Solute transport: boundary conditions) Solute transport: boundary conditions
- Upper boundary (Water flow boundary conditions) Water flow boundary conditions
- upstream weighting Solute transport: general
- upstream weighting Numerical solution
- vadose zone Introduction to Rusteau-1D
- validation Check & run
- van Genuchten Soil hydraulic model
- van Genuchten Soil hydraulic property models
- van Genuchten with an air-entry value of −2 cm (Soil hydraulic property models) Soil hydraulic property models
- van Genuchten – Mualem (Soil hydraulic property models) Soil hydraulic property models
- vapor flow Processes & units
- vapor flow Coupled water, vapor and heat flow
- Vapor flow (Further options of the HYDRUS code) Further options of the HYDRUS code
- Vapor pressure (Penman–Monteith combination equation) Penman–Monteith combination equation
- vapor pressure deficit Penman–Monteith combination equation
- variables Symbols and glossary
- Variably saturated water flow Variably saturated water flow
- verification Relation to HYDRUS-1D
- Verification (Introduction to Rusteau-1D) Introduction to Rusteau-1D
- Verification against HYDRUS 4.17 (Relation to HYDRUS-1D) Relation to HYDRUS-1D
- Views (Soil profile) Soil profile
- virus Solute transport: temperature and water-content dependence, colloids
- viruses Colloid, virus and bacteria transport
- viscosity Non-equilibrium water flow, centrifuge and density-dependent flow
- volatilization Solute transport: boundary conditions
- volatilization Solute transport equations
- Walker Solute transport: temperature and water-content dependence, colloids
- Walker Temperature and water-content dependence of reactions
- WatBalR Mass balance
- WatBalT Mass balance
- water balance Mass balance
- water capacity Soil hydraulic properties
- water content Variably saturated water flow
- water content dependence Solute transport: temperature and water-content dependence, colloids
- water content dependence Temperature and water-content dependence of reactions
- water content profile Profiles
- water content tolerance Iteration criteria
- water flow Processes & units
- water flow Variably saturated water flow
- Water flow (Further options of the HYDRUS code) Further options of the HYDRUS code
- Water flow (Notes on spatial and temporal discretization) Notes on spatial and temporal discretization
- Water flow (Numerical solution) Numerical solution
- Water flow boundary conditions Water flow boundary conditions
- water fluxes Boundary fluxes, heads and cumulative quantities
- water stress Root water and solute uptake
- water stress Root water uptake
- Water stress response functions (Root water uptake) Root water uptake
- water transfer Dual-permeability model
- Water transfer (Dual-permeability model) Dual-permeability model
- water vapor Coupled water, vapor and heat flow
- Water-content dependence (Solute transport: temperature and water-content dependence, colloids) Solute transport: temperature and water-content dependence, colloids
- Water-content dependence (Temperature and water-content dependence of reactions) Temperature and water-content dependence of reactions
- weighting Parameter estimation (inverse problem)
- weighting Parameter estimation
- Weighting of the measurement sets (Parameter estimation (inverse problem)) Parameter estimation (inverse problem)
- wetting front Notes on spatial and temporal discretization
- What the program computes (Introduction to Rusteau-1D) Introduction to Rusteau-1D
- Where are the results stored? (Questions and problems) Questions and problems
- wind Meteorological data
- workflow Workflow of a project
- workflow bar The main window
- Workflow bar and status bar (The main window) The main window
- Workflow of a project Workflow of a project
- Writing the HTML help (Command line program) Command line program
- zero gradient Solute transport: boundary conditions
- zero-order Solute transport: reactions
- zero-order production Solute transport equations
- zoom Keyboard and mouse