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Earth Surface Dynamics An interactive open-access journal of the European Geosciences Union
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Volume 1, issue 1
Earth Surf. Dynam., 1, 1-11, 2013
https://doi.org/10.5194/esurf-1-1-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
Earth Surf. Dynam., 1, 1-11, 2013
https://doi.org/10.5194/esurf-1-1-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 10 Sep 2013

Research article | 10 Sep 2013

The mass distribution of coarse particulate organic matter exported from an Alpine headwater stream

J. M. Turowski2,1, A. Badoux1, K. Bunte3, C. Rickli1, N. Federspiel4,1, and M. Jochner5,1 J. M. Turowski et al.
  • 1Swiss Federal Research Institute WSL, Zürcherstrasse 111, 8903 Birmensdorf, Switzerland
  • 2Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany
  • 3Engineering Research Center, Colorado State University, Fort Collins, CO 80523, USA
  • 4CSD Engineers SA, Hessstrasse 27d, 3097 Liebefeld (Berne), Switzerland
  • 5Institute of Geography of the University of Berne (GIUB), Hallerstrasse 12, 3012 Berne, Switzerland

Abstract. Coarse particulate organic matter (CPOM) particles span sizes from 1 mm, with a dry mass less than 1 mg, to large logs and entire trees, which can have a dry mass of several hundred kilograms. Pieces of different size and mass play different roles in stream environments, from being the prime source of energy in stream ecosystems to macroscopically determining channel morphology and local hydraulics. We show that a single scaling exponent can describe the mass distribution of CPOM heavier than 0.1 g transported in the Erlenbach, a steep mountain stream in the Swiss pre-Alps. This exponent takes an average value of −1.8, is independent of discharge and valid for particle masses spanning almost seven orders of magnitude. Similarly, the mass distribution of in-stream large woody debris (LWD) in several Swiss streams can be described by power law scaling distributions, with exponents varying between −1.8 and −2.0, if all in-stream LWD is considered, and between −1.3 and −1.8 for material locked in log jams. We found similar values for in-stream and transported material in the literature. We had expected that scaling exponents are determined by stream type, vegetation, climate, substrate properties, and the connectivity between channels and hillslopes. However, none of the descriptor variables tested here, including drainage area, channel bed slope and the percentage of forested area, show a strong control on exponent value. Together with a rating curve of CPOM transport rates with discharge, the scaling exponents can be used in the design of measuring strategies and in natural hazard mitigation.

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