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The soil erosion data produced compared well with the published local and regional data.
Three-year measurements of hydrological and soil erosion data from a series of nested experimental watersheds in a semi-arid area of SE Spain are discussed.
Traditional approaches, such as runoff plots and water weirs in a watershed, provide reliable spatially averaged soil erosion data but cannot validate process-based erosion prediction models for dynamic soil erosion evaluation.
Our erosion data from 20 small catchments in the Betic range are lower than the results of previous erosion studies in southeast Spain that were conducted in the Neogene intramontane basins.
Equations using an aggregate stability index As to replace the erodibility factor of interrill and rill erosion in the Water Erosion Prediction Project (WEPP) model were constructed after analysing the relationships between estimated and measured rill and interrill erosion data.
In this study, Mahleran (Model for Assessing Hillslope to Landscape Erosion Runoff, And Nutrients) is extensively evaluated against runoff and erosion data from four plots (representative of different stages of land degradation) over a transition from grassland to shrubland, at the Sevilleta National Wildlife Refuge in New Mexico, USA.
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However, there was no statistically significant difference between YORA and LORA patients in terms of progression of the Larsen scores or the presence of erosions (data not shown).
No significant relationships were observed between FCGR3B CN and RF, anti-CCP antibodies (Table 2) or radiographic erosions (data not shown) within RA patients.
We found no associations between the frequent haplotypes and RA susceptibility in the overall group or in subgroups defined by the presence of RF, anti-CCP antibodies, or joint erosions (data not shown).
Comparison of clinical and demographic features in PTPN22 1858T allele positive and negative RA cases showed no differences in the frequency of SE carriership, the concentrations of anti-CCP antibodies, the concentrations of IgM RF, the concentrations of IgA RF or the presence of erosions (data not shown).
We use previously published erosion rate data obtained mainly using 10Be and sediment yield and sediment yield data published by the United States Geological Survey.
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