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Filters: Extensions: Citation (X) > Types: Journal Citation (X) > partyWithName: Dirk Goossens (X)

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Field data are reported for the horizontal and vertical flux of wind-eroded sediment on an agricultural field in northern Germany. Measurements were made during a windstorm that hit the region on 18 May 1999. The magnitude of both fluxes was significantly affected by the presence of a surface crust covering the test field. Measuring the physical crust strength at 45 locations with a torvane, the relationships between crust strength (Ï„) and the horizontal (Fh) and vertical (Fv) sediment fluxes were investigated. Both fluxes decreased as the surface crust became stronger. The decay behaved as an exponential function for both types of flux. The horizontal sediment flux over a crusted surface can be accurately predicted...
This article presents a simple physical concept of aeolian dust accumulation, based on the behaviour of the subprocesses of dust deposition and dust erosion. The concept is tested in an aeolian dust wind tunnel. The agreement between the accumulation curve predicted by the model and the accumulation curve obtained in the experiments is close to perfect and shows that it is necessary to discriminate between the processes of aeolian dust deposition and aeolian dust accumulation. Two important thresholds determine the accumulation process. For wind speeds below the deflation threshold, the aeolian accumulation of dust increases linearly with the wind speed. For wind velocities between the deflation threshold and the...
Aeolian erosion of natural dust on two types of hills located in a rocky desert was investigated by means of wind tunnel simulations and field measurements. The first hill showed an elongated, nearly symmetric shape and was oriented perpendicular to the wind, whereas the second hill was almost perfectly conical. Erosion was measured along three transects: one across the elongated hill (transect parallel to the wind) and two across the conical hill (transects perpendicular to each other and crossing at the summit). In the field, erosion was measured on erosion plots during two wind storms. In the wind tunnel, erosion was measured on topographic scale models. The wind tunnel experiments and field experiments showed...
This study investigates how dust deposition samplers affect the grain size characteristics of the sediment they catch. Sediment samplers act as obstacles in the flow and their collection efficiency varies with the grain size and other factors. Some particle fractions are collected more efficiently than others, resulting in a modification of the original grain size distribution of the sediment. This paper presents wind tunnel results for five dust deposition samplers and five wind velocities ranging from 1 to 5 m s− 1. The catcher's effect on the grain size was apparent in all experiments. Dust accumulated in a catcher is finer than undisturbed dust. For the dust used in the tests the difference (in median grain...