Stefan Wirtz Vom Fachbereich VI (Geographie/Geowissenschaften ...
Stefan Wirtz Vom Fachbereich VI (Geographie/Geowissenschaften ...
Stefan Wirtz Vom Fachbereich VI (Geographie/Geowissenschaften ...
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Experimentelle Rinnenerosionsforschung vs. Modellkonzepte – Quantifizierung der hydraulischen und erosiven Wirksamkeit von Rinnen<br />
The rill experiment as a method to approach a quantification of rill erosion process<br />
activity<br />
<strong>Wirtz</strong> S. (1), Seeger M. (1,2) & Ries J.B. (1)<br />
(1) Dep. of Physical Geography, Trier University (2) Dep. of Land Degradation and<br />
Development, Wageningen University<br />
with 9 figures and 6 tables<br />
Summary<br />
Within this paper a standardized method to quantify sediment transport and runoff in natural<br />
rills is described. In order to achieve this, several rill experiments (RE) were accomplished in<br />
March 2007 in the Arnás catchment in the Spanish Pyrenees. Both, anthropogenically<br />
initiated and naturally developed rills were flushed with a total water quantity of 72 l in 8<br />
minutes (equivalent to 9 l min -1 ). Following the developed experimental routine flow<br />
velocities are recorded along the whole flushed rill, sediment concentrations are measured at<br />
different points and different times during the experiment and runoff values are measured<br />
after 25 m. For the characterisation of the rill, slope is measured and micromorphological<br />
features like scours are registered.<br />
By means of the developed rill experiments it becomes possible to assess the effectivity of<br />
single rills in a catchment. However, the assessments can not be generalized because it is<br />
impossible to project the behaviour of one rill to other rills, even if the spatial distance in<br />
between is small. But it gets possible to detect the qualitative process activity in a rill.<br />
The average slopes oscillated between 7.6° and 11.3°, the highest slope was 16°. The<br />
sediment concentrations reached average values between 0.69 and 2.21 g l -1 , the maximum<br />
values ranged between 1.59 and 6.31 g l -1 . Comparing the sediment concentrations measured<br />
in the rills to the sediment concentrations in the runoff of the river Arnás, it can be stated that<br />
the concentrations in the rills are usually higher.<br />
Keywords: soil erosion, rill erosion, field experiments, quantification of process activity,<br />
Arnás catchment<br />
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