# SMS:SRH-2D Boundary Conditions

This contains information about functionality available starting at SMS version 13.1.The content may not apply to other versions. |

SRH-2D supports a variety of boundary conditions for hydraulic computation. The boundary conditions for the model are defined on the arcs in an SRH-2D boundary conditions coverage by selecting an arc or by selecting a nodestring in the mesh. Once the arc or nodestring has been selected, double-clicking, or right-clicking and using the **Assign BC...** command, will bring up a dialog where the boundaries can be assigned.

The type of boundary conditions are specified on the SRH-2D boundary condition coverage.

All currently supported inflow and outflow boundary types are exterior boundaries with the exception of a monitor line. Other boundary types include the following: Inlet-Q, Inlet-SC, Exit-EX, Exit-H, Exit-Q, Wall, and Symmetry. For the Inlet-Q and Inlet-SC boundary condition types, additional information is required on sediment inflow when a sediment transport simulation is selected.

## SRH-2D Assign BC Dialog

The *SRH-2D Assign BC* dialog contains multiple boundary condition types. Selecting a type for an arc will determine what boundary conditions can be assigned to the arc.

### Inflow and Outflow Boundary Conditions Options

SMS provides options for the following boundary conditions options:

#### Inlet-Q

A subcritical inlet boundary that may be given as a constant discharge or as a variable discharge hydrograph. The velocity distribution type may be selected from the boundary condition menu.

*Discharge (Q)*– Specify as either a "Constant" or a "Time Series".- "Constant" – Use for a steady state simulation.
*Constant Q*– Enter a real positive value along with the units as either "cfs" or "cms".

- "Time Series" – Use for unsteady flow.
*Time Series Files*– Clicking the button will bring up the*XY Series Editor*. Units must be specified as either "cfs" or "cms".

- "Constant" – Use for a steady state simulation.
*Distribution at Inlet*– The lateral distribution of the velocity. Options include:- "Conveyance" – Calculates the conveyance parameter first then the velocity. The flow direction is assumed to be normal.
- "Profile" – Uses a depth average velocity profile.
- "Q" – A constant unit discharge, q=vh, is assumed with flow direction normal to the inlet boundary.
- "Velocity" – A constant velocity magnitude is imposed at the inlet with flow direction normal to the inlet boundary.

*Sediment Inflow*– This input becomes available when "Mobile" is selected as the*Run Type*in the*BC Type Parameters*dialog in the SRH-2D boundary condition coverage.*Sediment Discharge Type*– Has the following two options:- "Capacity" – Calculates the sediment transport capacity based on the element hydraulics, bed material gradation, and selected transport function.
- "File" – An input file containing a rating curve of sediment load (by size fraction in cfs or cms) versus total water discharge is provided. The format for this file is shown in the
*SRH-2D Files*article.

Note: Most bridge hydraulics and sour problems are intended to evaluate conditions during an extreme event (hours to days) rather than for degradation studies of long-term bed changes over decades. Therefore, the capacity option is often an appealing choice because it is intended to produce a model in general equilibrium. The capacity option, however, is very sensitive to the velocities and depths at the upstream boundary, so it may not accurately represent a balanced sediment transport condition throughout the modeled reach. Therefore, the results should be reviewed for reasonableness and adjustments made to the inflowing transport rates. This can be done using the file option, where inflowing rates are specified by size fraction.

#### Inlet-SC

A supercritical inlet boundary that may be given as a constant discharge or as a variable discharge hydrograph. Inlet-SC also requires information about depth. Within the boundary condition menu, the velocity distribution type may be specified.

*Supercritical Inflow Options*– Specify the discharge type and water surface elevation units.*Discharge (Q)*– Set as one of the following:- "Constant" – Use for a steady state simulation.
- "Time Series" – Use for unsteady flow.

*Units*– Can be set as "U.S. Customary" or "Metric".

*Supercritical Constant Inflow Options*– Enter values for a steady state simulation.*Discharge (Q)*– Enter a real positive value for the flow.*Water Elevation (WSE)*– Enter a real positive value for the water surface elevation.

*Supercritical Varied Inflow Options*– Use for unsteady flow.*Time Series Discharge File*– Clicking the button will bring up the*XY Series Editor*for entering the varied discharge values.*Water Elevation (WSE)*– Can be entered as either a "Time Series" or a "Rating Curve".*Time Series vs. WSE File*– Clicking the button will bring up the*XY Series Editor*for entering the time versus elevation values.*Q vs. WSE Files*– Clicking the button will bring up the*XY Series Editor*for entering the flow versus elevation rating curve values.

*Distribution at Inlet*– The lateral distribution of the velocity. Options include:- "Conveyance" – Calculates the conveyance parameter first then the velocity. The flow direction is assumed to be normal.
- "Profile" – Uses a depth average velocity profile.
- "Q" – A constant unit discharge, q=vh, is assumed with flow direction normal to the inlet boundary.
- "Velocity" – A constant velocity magnitude is imposed at the inlet with flow direction normal to the inlet boundary.

*Sediment Inflow*– This input becomes available when "Mobile" is selected as the*Run Type*in the*BC Type Parameters*dialog in the SRH-2D boundary condition coverage.*Sediment Discharge Type*– Has the following two options:- "Capacity" – Calculates the sediment transport capacity based on the element hydraulics, bed material gradation, and selected transport function.
- "File" – An input file containing a rating curve of sediment load (by size fraction in cfs or cms) versus total water discharge is provided. The format for this file is shown in the
*SRH-2D Files*article.

#### Exit-H

A stage type exit boundary where water surface elevation may be given as a constant number or as a stage-discharge or rating curve.

*Water Elevation(WSE)*– Set as either a constant, a time series, or a rating curve.- "Constant" – Use for a steady state simulation.
*Constant WSE*– Enter a positive value for the water surface elevation.**Populate**– Launches the*Populate*dialog to automatically generate an estimated constant.

- "Time Series" – Use for unsteady flow.
*Time Series vs. WSE file*– Clicking the button will bring up the*XY Series Editor*for entering the time versus elevation values.

- "Rating Curve" – Use for unsteady flow.
*Q vs. WSE file*– Clicking the button will bring up the*XY Series Editor*for entering the discharge versus elevation rating curve values. The*Populate*dialog can be accessed from the*XY Series Editor*to automatically generate an estimated rating curve.

- "Constant" – Use for a steady state simulation.

#### Exit-Q

An exit boundary with a discharge given as a constant number or as a hydrograph.

*Discharge (Q)*– Specify as either a "Constant" or a "Time Series".- "Constant" – Use for a steady state simulation.
*Constant Q*– Enter a real positive value along with the units as either "cfs" or "cms".

- "Time Series" – Use for unsteady flow.
*Time Series Files*– Clicking the button will bring up the*XY Series Editor*. Units must be specified as either "hrs-vs-cfs" or "hrs-vs-cms".

- "Constant" – Use for a steady state simulation.

#### Wall

Solid wall boundaries may represent banks and islands. No-slip condition is assumed at solid walls for the dynamic wave solver.

*Add Extra Roughness at Wall Boundary*– Can be turned "On" or "Off".*Roughness Height in mm*– Only available with the "On" option.

### Boundary Conditions Without Additional Options

The following boundary conditions do not have additional options.

- "Exit-EX" – A supercritical exit boundary condition.
- "Symmetry" – Defined as a boundary where all dependent variables are extrapolated assuming the gradient of the variable in a direction normal to the boundary is zero except the velocity component normal to the boundary.
- "Monitor-Line" – Not a real boundary at all; it is an internal polyline which may be used to monitor the total flow discharge through it. Monitor lines are applied the model to determine the flow and sediment flux across the lines at specified locations in the model. SRH-2D creates a *_LN#.DAT file (where * indicates the run name and # is the monitor line number) for each monitor line that details the bed and water-surface elevations, the flow, and the sediment flux across the lines. The monitor lines can be used to determine when the model reaches steady state conditions. For example, by comparing the predicted water-surface elevations over time and at various locations along the reach, the user can determine when the water-surface elevation reaches a steady state condition.

### Structure Boundary Conditions

In general, two arcs must be selected before assigning arcs a structure boundary condition.

- Weir – See the SRH-2D Structures article for more information.
- Culvert – See the SRH-2D Structures article for more information.
- Pressure zone – See the SRH-2D Structures article for more information.
- Gate – See the SRH-2D Structures article for more information.
- Internal Sink – See the SRH-2D Structures article for more information.
- Link – See the SRH-2D Structures article for more information.

- Note: 1D hydraulic structures (e.g. culverts and 1D weir over topping) do not work with sediment transport options in SRH-2D.

## Related Topics

SMS – Surface-water Modeling System | ||
---|---|---|

Modules: | 1D Grid • Cartesian Grid • Curvilinear Grid • GIS • Map • Mesh • Particle • Quadtree • Raster • Scatter | |

General Models: | FVCOM • Generic • PTM • TUFLOW FV | |

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Riverine/Estuarine Models: | ADH • FESWMS • HEC-RAS • HYDRO AS-2D • RMA2 • RMA4 • SRH-2D • Steering • TUFLOW | |

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