Tool NameLS Factor
Tool ID22
Library IDta_hydrology
Version1.0
Author(s)O.Conrad (c) 2003

Description

Calculation of slope length (LS) factor as used by the Universal Soil Loss Equation (USLE), based on slope and specific catchment area (SCA, as substitute for slope length).

References

Böhner, J., Selige, T. (2006): Spatial Prediction of Soil Attributes Using Terrain Analysis and Climate Regionalisation. In: Böhner, J., McCloy, K.R., Strobl, J.: SAGA - Analysis and Modelling Applications. Göttinger Geographische Abhandlungen, Vol.115, p.13-27. PDF

Desmet, P.J.J. & Govers, G. (1996): A GIS Procedure for Automatically Calculating the USLE LS Factor on Topographically Complex Landscape Units. Journal of Soil and Water Conservation, 51(5), 427-433. doi:10.1080/00224561.1996.12457102

Kinnell, P.I.A. (2005): Alternative Approaches for Determining the USLE-M Slope Length Factor for Grid Cells. Soil Sci. Soc. Am. J., 69: 674-680. doi:10.2136/sssaj2004.0047

Moore, I.D., Grayson, R.B., Ladson, A.R. (1991): Digital terrain modelling: a review of hydrogical, geomorphological, and biological applications. Hydrological Processes, Vol.5, No.1. doi:10.1002/hyp.3360050103

Wischmeier, W.H., Smith, D.D. (1978): Predicting rainfall erosion losses - A guide to conservation planning. Agriculture Handbook No. 537: US Department of Agriculture, Washington DC.


Parameters

NameTypeIdentifierDescriptionConstraints
Input
Slopegrid, inputSLOPE
Catchment Areagrid, inputAREA
Output
LS Factorgrid, outputLS
Options
UnitchoiceSLOPE_UNITAvailable Choices:
[0] radians
[1] degree
Default: 0
Area to Length ConversionchoiceCONVDerivation of slope lengths from catchment areas. These are rough approximations! Applies not to Desmet & Govers' method.Available Choices:
[0] no conversion (areas already given as specific catchment area)
[1] 1 / cell size (specific catchment area)
[2] square root (catchment length)
Default: 0
Feet AdjustmentbooleanFEETNeeded if area and lengths come from coordinates measured in feet.Default: 0
Method (LS)choiceMETHODAvailable Choices:
[0] Moore et al. 1991
[1] Desmet & Govers 1996
[2] Böhner & Selige 2006
Default: 0
Rill/Interrill Erosivityfloating point numberEROSIVITYMinimum: 0.000000
Default: 1.000000
StabilitychoiceSTABILITYAvailable Choices:
[0] stable
[1] instable (thawing)
Default: 0