Journal cover Journal topic
Natural Hazards and Earth System Sciences An interactive open-access journal of the European Geosciences Union
Nat. Hazards Earth Syst. Sci., 6, 261-270, 2006
https://doi.org/10.5194/nhess-6-261-2006
© Author(s) 2006. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
 
24 Apr 2006
Numerical simulation of debris flows triggered from the Strug rock fall source area, W Slovenia
M. Mikoš1, R. Fazarinc2, B. Majes1, R. Rajar1, D. Žagar1, M. Krzyk1, T. Hojnik3, and M. Četina1 1Faculty of Civil and Geodetic Engineering, University of Ljubljana, Ljubljana, Slovenia
2Water Engineering Ltd., Ljubljana, Slovenia
3Water Management Bureau Ltd. (Vodnogospodarski Biro Maribor d.o.o.), Glavni trg 19c, 2000 Maribor, Slovenia
Abstract. The Strug landslide was triggered in December 2001 as a rockslide, followed by a rock fall. In 2002, about 20 debris flows were registered in the Kosec village; they were initiated in the Strug rock fall source area. They all flowed through the aligned Brusnik channel, which had been finished just before the first debris flow reached the village in April 2002. Debris flow events were rainfall-induced but also governed by the availability of rock fall debris in its zone of accumulation. After 2002 there was not enough material available for further debris flows to reach the village. Nevertheless, a decision was reached to use mathematical modeling to prepare a hazard map for the village for possible new debris flows. Using the hydrological data of the Brusnik watershed and the rheological characteristics of the debris material, 5 different scenarios were defined with the debris flow volumes from 1000 m3 to a maximum of 25 000 m3. Two mathematical models were used, a one-dimensional model DEBRIF-1D, and a two-dimensional commercially available model FLO-2D. Due to the lack of other field data, data extracted from available professional films of debris flows in 2002 in the Kosec village were used for model calibration. The computational reach was put together from an 800-m long upstream reach and 380-m long regulated reach of the Brusnik channel through the village of Kosec. Both mathematical models have proved that the aligned Brusnik channel can convey debris flows of the volume up to 15 000 m3. Under the most extreme scenario a debris flow with 25 000 m3 would locally spill over the existing levees along the regulated Brusnik channel. For this reason, additional river engineering measures have been proposed, such as the raising of the levees and the construction of a right-hand side sedimentation area for debris flows at the downstream end of the regulated reach.

Citation: Mikoš, M., Fazarinc, R., Majes, B., Rajar, R., Žagar, D., Krzyk, M., Hojnik, T., and Četina, M.: Numerical simulation of debris flows triggered from the Strug rock fall source area, W Slovenia, Nat. Hazards Earth Syst. Sci., 6, 261-270, https://doi.org/10.5194/nhess-6-261-2006, 2006.
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