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Results of the simulation indicate that the temporal stability of erosion rates determined from CRN concentrations in sediment decreases with increased ratios of landsliding to bedrock weathering rates within a given catchment area, and that as the frequency of landsliding increases, larger catchment areas must be sampled in order to accurately evaluate long-term erosion rates.
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In order to do that, the following characteristics of the dam must be known: (1) geotechnical stability, (2) erosion of downstream slope, (3) type of sealing of the dam, (4) overtopping probability, (5) volume of leachate stored inside the dam and (6) pollution load of leachate.
However, this can be cumbersome and prone to low stability over generations because of erosion of linkage disequilibrium between markers and QTL.
The assessment of erosion stabilities was one of the major achievements of the Sediment Management Concept of the RBC-Elbe (RBC Elbe 2013 [7]; another was the development of criteria for the prioritization of measures).
This corroborates the observation of loss of stability (lowering of the erosion threshold) during this treatment as described above.
The present Pilbara land surfaces are characterized by a long history of tectonic stability and extremely slow rates of erosion [ 8].
Geomorphic mapping and radiocarbon dating indicate synchronicity in patterns of erosion, deposition, and stability between drainage basins.
A chronology of events for two catenas, focusing on periods of landscape stability and change, establish the sequence of erosion events from pre-Hispanic to modern times.
The created system allows simultaneous analysis and evaluation of landscape from the perspective of ecological stability, erosion susceptibility, retention capacity and the economic value.
Because of their stability, erosion has had the time to flatten the topography of continental shields.
The stability of the 3rd and 4th erosion thresholds in these systems decreased in comparison to the 156 h mark (Figure 2E).
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