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Journal of Soils and Sediments

, Volume 17, Issue 11, pp 2582–2595 | Cite as

Source ascription in bed sediments of a Mediterranean temporary stream after the first post-fire flush

  • Julián García-Comendador
  • Josep Fortesa
  • Aleix Calsamiglia
  • Francesca Garcias
  • Joan Estrany
Transfer of Sediments and Contaminants in Catchments and Rivers

Abstract

Purpose

First flushes can be crucial to sediment transport in fluvial systems of drylands, as temporary streams are a characteristic feature of Mediterranean basins. After a wildfire, storm flows may enhance runoff delivery to channels, so increasing the first-flush effect. 137Cs and 210Pbex were used as tracers for recognizing the first post-fire flush effect on the source ascription of bed sediments temporarily stored in a Mediterranean temporary stream severely affected by a wildfire.

Materials and methods

Thirty sediment source samples were collected along one of the tributaries of a catchment (4.8 km2) located in Mallorca during a field campaign some weeks after the wildfire. The sample collection took into account effects of the wildfire and distinguished between soil surface and channel bank. To measure the source contribution temporarily stored with the bed sediment, five sediment samples—deposited during the first storm, occurring 3 months after the wildfire—were collected from the bed of the main channel. The 137Cs and 210Pbex concentrations were measured by gamma spectrometry. Then, a linear mixing model was used to establish the contribution of each source type to the bed sediments along the main stream.

Results and discussion

First post-fire flush effect was generated by a torrential event with a suspended sediment concentration peak of 33,618 mg L−1, although transmission losses under a very low runoff coefficient (1%) promoted sediment deposition. Significant differences were observed in fallout radionuclide concentrations between burned surface soil and burned channel bank samples (p < 0.05), as well as between burned and unburned sources in the downstream part of the catchment (p < 0.01). The radioactivity concentrations in bed sediment samples were statistically similar (p > 0.05). Source ascription in bed sediments upstream shows that 67% was generated from burned hillslopes, reaching 75% in the downstream part, because downstream propagation of the sediment derived from the burned area.

Conclusions

Bed sediments were mostly generated on burned surface soils because of the fire’s effect on soil and sediment availability, high-intensity rainfall, and the limited contribution of channel banks, because these are fixed by dry-stone walls. This hydro-sedimentary response indicates an association between these factors driving erosion and sediment delivery, generating effective slope-to-channel sediment connectivity. The integration of the short-term response with the medium- and long-term analysis will allow for the analysis of the evolution of catchment sediment sources in future studies, determining if fire modifies the catchment sensitivity to that specific disturbance.

Keywords

Fallout radionuclides Fingerprinting technique First-flush sediment sources Mediterranean fluvial systems Wildfire disturbances 

Notes

Acknowledgements

This research was supported by the Spanish Ministry of Economy and Competitiveness (CGL2012-32446). Specifically, the study was supported by the Balearic Forest Service (Department of Environment, Agriculture and Fishery of the Balearic Autonomous Government) and by the “la Caixa” Foundation. Julián García-Comendador is in receipt of a postgraduate contract (FPU15/05239) funded by the Spanish Ministry of Education and Culture. Josep Fortesa has a contract funded by the European Commission-Directorate-General for European Civil Protection and Humanitarian Aid Operations. Aleix Calsamiglia acknowledges the support from the Spanish Ministry of Economy and Competitiveness through a postgraduate contract EEBB-I-15-10280. Meteorological data were provided by the Spanish Meteorological Agency (AEMET). The authors are grateful to the Environmental Radioactivity Laboratory at the University of the Balearic Islands for determining fallout radionuclide concentrations and Prof. Francesc Gallart at the Institute of Environmental Assessment and Water Research (IDAEA-CSIC) for determining particle size. Thanks must also be expressed to Joan Bauzà Llinàs for his assistance during the fieldwork.

Supplementary material

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Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  1. 1.Mediterranean Ecogeomorphological and Hydrological Connectivity Research Team, Department of GeographyUniversity of the Balearic IslandsMallorcaSpain
  2. 2.Institute of Agro-Environmental and Water Economy Research –INAGEAUniversity of the Balearic IslandsMallorcaSpain
  3. 3.Department of PhysicsUniversity of the Balearic IslandsMallorcaSpain

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