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Equations to predict the mean erosion rate are proposed.
The mean erosion rate increases with deposit height, deposit width, and decreasing grain size.
The upper estimate of 90 t/km2/y is comparable to the mean erosion rate estimated using the radionuclide method for uncultivated sites in Australia and is significantly lower than that measured at sites were vegetation cover was disturbed by livestock grazing prior to its exclusion from the alpine area in the 1940s CE.
The length, depth and width of the linear erosion features were recorded every 5-m from their headcuts to their outlets in order to estimate the total catchment LE. 52 linear features, mainly rills, were formed or developed within the study area with a mean erosion rate of 1.3 Mg ha− 1 y− 1.
Results show that this group indeed has a low mean erosion rate, but it is not the lowest.
Then, we grouped them in all possible combinations and calculated the mean erosion rate for each group.
Similar(48)
The temporal evolution of the deposit geometry and the corresponding mean erosion rates were studied.
For MatIV, we also investigated the evolution of mean erosion rates and stream power erosion law exponents in 1D as a function of slope.
Catchment mean erosion rates contrast sharply along strike: ca. 300 m/Myr in the Ejia section and ca. 100 m/Myr in the Nansha section.
We use fluvial longitudinal profiles, catchment slopes, and catchment mean erosion rates derived from in-situ cosmogenic 10Be and 26Al to examine the late Cenozoic landscape evolution of the Ailao Shan Shear Zone (ASSZ) in the southeastern Tibetan Plateau.
Table 3 shows the mean erosion rates of the remaining 17 groups, arranged from low to high mean erosion rates.
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