SAM.aid
SAM.aid provides guidance in the selection of a sediment transport
function(s) to use with a given project, based on five screening parameters: d50,
slope, velocity, width, and depth.
General
The SAM package is a product of the Flood Damage Reduction and Stream
Restoration Research Program. The conception and initial development of the
package were the results of the efforts of William A. Thomas, Ronald R.
Copeland and Nolan Raphelt. However, many workunits and many principal
investigators have contributed to the package. The US Government is not
responsible for results obtained with this software. However, the office
supporting the package would welcome documentation of program errors and
should respond if fiscally feasible.
Files
The program operates interactively. However it saves the input data in an
ASCII files and uses these files to pass data from module to module.
Theoretical Assumptions and Limitations
SAM is not a package of one-dimensional models. SAM makes calculations
based on one cross section at one point in time. There are no provisions in any of
the modules for simulating the effects of a hydrograph nor for looking at a reach
of a river, except as it might be represented by an average. SAM is designed to
be used as a tool during reconnaissance level planning studies. Broad application
of SAM results must be made with caution.
Sediment transport functions in SAM must be used with care. Essentially,
SAM.sed applies the sediment transport functions at a point, which allows for no
variability in the size class distribution over time or space. Considering that the
size class distribution of bed material in the natural river changes with discharge,
reach, time of year, and other temporal factors, SAM's use of a fixed, non-
varying, as-prescribed size class distribution for all calculations presents the
possibility that the calculated transport rates are not truly representative of the
natural river. The procedure in HEC-6, which integrates processes over several
cross sections which describe a reach of the river and provides a continuity
equation for sediment movement, will consequently produce a more reliable
result than comes from applying a sediment transport function at a single point.
4
Chapter 1
Introduction