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The AA. compared karren formation of various slopes (3 bare slopes and 2 with a plant patch) in a glacier valley close to Tragl peak (in Totes Gebirge, Austria). It could be established that bare slopes have a larger average specific width, channel
shape and channel density. The dynamics of karren features are different on the bare slopes and slopes fed from a plant patch. Karren features tend to widen on bare slopes, while they tend to deepen on slopes with a plant patch. The specific width
2012

. It was found that natural vegetative cover reduces both runoff and erosion by approximately 36 and 7457 times over bare ground, and 16 and 1801 times over typically planted grasses, respectively. The increase in erosion associated with the replacement of native
vegetation with bare ground or grasses due to large-scale infrastructure projects in Fujian from 1999 to 2004 has implications for frequency and occurrence of landslides and other geographic hazards, the transport of chemicals into waterways, the transport
2012

Most common forms on bare slopes of high mountains are rinnenkarren or channels. The AA. aim to analyse a type of rinnenkarren, called the type A channels. The shape of the channels depends on the amount and regularity of water transport
2012

slipface deposition rate and allows vegetation to expand inward from the arms to the dune centre. The planform inversion of bare barchans dunes into vegetated parabolic dunes ultimately leads to complete stabilization.
2012

order control of the erosion resistance on conventionally tilled loess soils. For bare soils they found a strong correlation between the erosion resistance, surface roughness and clay content. These results can be used to predict the erosion resistance
2012

basin : Amala upstream; Amala downstream and Nyangores watersheds. In all of the 3 watersheds, 3 land uses (cropland, grassland and bare land) with similar slope steepness and soil types were considered. The plot scale research results indicated
2012

Soil CO2 content of areas with different vegetation coverings was investigated in alpine terrains (Totes Gebirge, Austria). Dissolution of limestone was compared on slopes with vegetation patches (grass or dwarf pine) and on bare slopes. Dissolution
2012

soil and its artificial reproduction were measured with a laser scanner in order to assess the quality of the molding method. This novel molding method was applied to get 10 footprints of the micro-topography of a loamy bare soil, at different levels
2012

on rangelands differ significantly from those of cropland rills. Concentrated flow hydraulics on rangelands are largely controlled by the amount of cover or bare soil and hillslope angle. New predictive equations for concentrated flow velocity representing
2012

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