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Spatial Analysis
Temporal Analysis
Arc Hydro
Conclusion
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Specific sediment
yield based on different decades for the Lower Missouri
Sediment
data behind the dams in the Missouri basin based on the last survey for
each dam is
used to develop a sediment yield map. These dams were built in
different
years and were surveyed in different years. For sub-basin 1, where most
of the
sediment originated, 85 sediment survey data behind the dams for
different
decades are used to examine the temporal pattern of sediment yield. For
this
sub-basin, survey data were available from the 1930s to the 1960s. It
can be seen
that Ks decreases by increasing the decades (Figure 13). This is due to
the
fact that the Missouri has experienced a major shift in land management
through
the implementation of soil conservation methods. Maps of unit
area yield
based on both the most recent survey data for each dam and the entire
available
data are shown in Figure 14. This Figure shows that the differences in
unit
area yield data are smoother in the most recent surveys. The standard
deviations of differences between these maps are illustrated in Figure
15. This
Figure shows that the most significant changes have occurred at
locations with very high unit area yield based on the entire available
data.

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