r.sim.sediment(1)
r.sim.sediment π
okay bestie, gather round, because this is the GRASS GIS User's Manual page for r.sim.sediment β yes, the (1) one, section 1, we're in the big leagues. Sit down, hydrate, we're simulating sediment transport with path sampling and it's gonna be iconic. β¨
πΈ NAME πΈ
r.sim.sediment β Sediment transport and erosion/deposition simulation using path sampling method (SIMWE).
π¦ KEYWORDS π¦
raster, hydrology, soil, sediment flow, erosion, deposition, model, parallel
β¨ SYNOPSIS β¨
r.sim.sediment
r.sim.sediment --help
r.sim.sediment [-s] elevation=name water_depth=name dx=name dy=name
detachment_coeff=name transport_coeff=name shear_stress=name [man=name]
[man_value=float] [observation=name] [transport_capacity=name]
[tlimit_erosion_deposition=name] [sediment_concentration=name]
[sediment_flux=name] [erosion_deposition=name] [logfile=name]
[walkers_output=name] [nwalkers=integer] [niterations=integer]
[mintimestep=float] [output_step=integer] [diffusion_coeff=float]
[random_seed=integer] [nprocs=integer] [--overwrite] [--help]
[--verbose] [--quiet] [--ui]
Flags:
-sβ Generate random seed. Automatically generates random seed for random number generator (use when you don't want to provide the seed option) π²--overwriteβ Allow output files to overwrite existing files. yes she will bulldoze your old files, that's the deal π--helpβ Print usage summary--verboseβ Verbose module output. she will yap (affectionately)--quietβ Quiet module output. she will NOT yap--uiβ Force launching GUI dialog
Parameters:
elevation=name[required] β Name of input elevation raster mapwater_depth=name[required] β Name of water depth raster map [m]dx=name[required] β Name of x-derivatives raster map [m/m]dy=name[required] β Name of y-derivatives raster map [m/m]detachment_coeff=name[required] β Name of detachment capacity coefficient raster map [s/m]transport_coeff=name[required] β Name of transport capacity coefficient raster map [s]shear_stress=name[required] β Name of critical shear stress raster map [Pa]man=nameβ Name of Manning's n raster mapman_value=floatβ Manning's n unique value. Default:0.1observation=nameβ Name of sampling locations vector points map. Or data source for direct OGR accesstransport_capacity=nameβ Name for output transport capacity raster map [kg/ms]tlimit_erosion_deposition=nameβ Name for output transport limited erosion-deposition raster map [kg/m2s]sediment_concentration=nameβ Name for output sediment concentration raster map [particle/m3]sediment_flux=nameβ Name for output sediment flux raster map [kg/ms]erosion_deposition=nameβ Name for output erosion-deposition raster map [kg/m2s]logfile=nameβ Name for sampling points output text file. For each observation vector point the time series of sediment transport is stored.walkers_output=nameβ Base name of the output walkers vector points mapnwalkers=integerβ Number of walkersniterations=integerβ Time used for iterations [minutes]. Default:10mintimestep=floatβ Minimum time step for the simulation [seconds]. A larger minimum time step substantially reduces processing time, but at the cost of accuracy. Default:0.0output_step=integerβ Time interval for creating output maps [minutes]. Default:2diffusion_coeff=floatβ Water diffusion constant. Default:0.8random_seed=integerβ Seed for random number generator. The same seed can be used to obtain same results or random seed can be generated by other means.nprocs=integerβ Number of threads which will be used for parallel computation. Default:1
π DESCRIPTION π
So r.sim.sediment is a landscape scale, simulation model of soil erosion, sediment transport and deposition caused by flowing water, and it's designed for spatially variable terrain, soil, cover and rainfall excess conditions. Basically she eats variable conditions for breakfast. π
The soil erosion model is based on the theory used in the USDA WEPP hillslope erosion model, but it has been generalized to 2D flow. The solution is based on the concept of duality between fields and particles and the underlying equations are solved by Green's function Monte Carlo method, to provide robustness necessary for spatially variable conditions and high resolutions (Mitas and Mitasova 1998). no cap, that's the actual technique.
Key inputs of the model include the following raster maps, and bestie, we're listing ALL of them:
- elevation (
elevation[m]) β the terrain itself, main character energy - flow gradient given by the first-order partial derivatives of elevation field (
dxanddy) - overland flow water depth (
water_depth[m]) - detachment capacity coefficient (
detachment_coeff[s/m]) - transport capacity coefficient (
transport_coeff[s]) - critical shear stress (
shear_stress[Pa]) - surface roughness coefficient called Manning's n (
manraster map)
Partial derivatives can be computed by v.surf.rst or r.slope.aspect module. π«Ά
The data are automatically converted from feet to metric system using database/projection information, so the elevation always should be in meters. The water depth file can be computed using r.sim.water module. Other parameters must be determined using field measurements or reference literature (see suggested values in Notes and References).
Now, the outputs, because she's giving range:
- transport capacity raster map
transport_capacityin [kg/ms] - transport capacity limited erosion/deposition raster map
tlimit_erosion_deposition[kg/m2s]
Those two are output almost immediately and can be viewed while the simulation continues. lowkey the best part.
- Sediment flow rate raster map
sediment_flux[kg/ms] - net erosion/deposition raster map [kg/m2s]
Those can take longer time depending on time step and simulation time. Simulation time is controlled by niterations [minutes] parameter.
If the resulting erosion/deposition map is noisy, higher number of walkers, given by nwalkers should be used. π«Ά
Also, heads up: increasing the number of threads with nprocs does not really speed up the simulation. like, at all. it's giving placebo π
π REFERENCES π
- Mitasova, H., Thaxton, C., Hofierka, J., McLaughlin, R., Moore, A., Mitas L., 2004, Path sampling method for modeling overland water flow, sediment transport and short term terrain evolution in Open Source GIS. In: C.T. Miller, M.W. Farthing, V.G. Gray, G.F. Pinder eds., Proceedings of the XVth International Conference on Computational Methods in Water Resources (CMWR XV), June 13-17 2004, Chapel Hill, NC, USA, Elsevier, pp. 1479-1490.
- Mitasova H, Mitas, L., 2000, Modeling spatial processes in multiscale framework: exploring duality between particles and fields, plenary talk at GIScience2000 conference, Savannah, GA.
- Mitas, L., and Mitasova, H., 1998, Distributed soil erosion simulation for effective erosion prevention. Water Resources Research, 34(3), 505-516.
- Mitasova, H., Mitas, L., 2001, Multiscale soil erosion simulations for land use management, In: Landscape erosion and landscape evolution modeling, Harmon R. and Doe W. eds., Kluwer Academic/Plenum Publishers, pp. 321-347.
- Neteler, M. and Mitasova, H., 2008, Open Source GIS: A GRASS GIS Approach. Third Edition. The International Series in Engineering and Computer Science: Volume 773. Springer New York Inc, p. 406.
π SEE ALSO π
v.surf.rst, r.slope.aspect, r.sim.water
π AUTHORS π
- Helena Mitasova, Lubos Mitas β North Carolina State University β
hmitaso@unity.ncsu.edu - Jaroslav Hofierka β GeoModel, s.r.o. Bratislava, Slovakia β
hofierka@geomodel.sk - Chris Thaxton β North Carolina State University β
csthaxto@unity.ncsu.eduβcsthaxto@unity.ncsu.edu
(yes, that last email is listed twice in the original, and I am NOT about to erase a single character of it, that's her lore π)
πΎ SOURCE CODE πΎ
Available at: r.sim.sediment source code (history)
Accessed: Saturday Jan 17 05:41:00 2026
Main index | Raster index | Topics index | Keywords index | Graphical index | Full index
okay that's the whole page, every flag, every default, every reference, every email, periodt. πβ¨
And a lil sign-off for the girlies: this is GRASS GIS 8.4.2, Β© 2003-2025 GRASS Development Team, straight out of the GRASS GIS 8.4.2 Reference Manual, and the page itself signs off as GRASS 8.4.2 with r.sim.sediment(1). slay, go simulate some erosion, bestie πΈπ¦π
π¦ where this page comes from
- fedora 44: grass 8.4.2-4.fc44 Β· GPL-2.0-or-later
- π girlified by deepseek-ai/DeepSeek-V4.1-Flash on : a language model's rewrite of the original, under its terms