Articles | Volume 21, issue 6
https://doi.org/10.5194/hess-21-3025-2017
https://doi.org/10.5194/hess-21-3025-2017
Research article
 | 
23 Jun 2017
Research article |  | 23 Jun 2017

Identification of runoff formation with two dyes in a mid-latitude mountain headwater

Lukáš Vlček, Kristýna Falátková, and Philipp Schneider

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Cited articles

Anderson, A. E., Weiler, M., and Alila, Y., and Hudson, R. O.: Dye staining and excavation of a lateral preferential flow network, Hydrol. Earth Syst. Sci., 13, 935–944, https://doi.org/10.5194/hess-13-935-2009, 2009.
Anderson, M. G. and Burt, T. P.: Process Studies in Hillslope Hydrology, Wiley, Winchester, UK, 1990.
Bachmair, S. and Weiler, M.: Hillslope characteristics as controls of subsurface flow variability, Hydrol. Earth Syst. Sci., 16, 3699–3715, https://doi.org/10.5194/hess-16-3699-2012, 2012.
Bachmair, S., Weiler, M., and Nützmann, G.: Controls of land use and soil structure on water movement: Lessons for pollutant transfer through the unsaturated zone, J. Hydrol., 369, 241–252, ISSN 0022-1694, 2009.
Boorman, D.B., Hollis, J.M., and Lilly, A.: Hydrology of soil types: a hydrologically-based classification of the soils of the United Kingdom, Institute of Hydrology report no. 126, 1995.
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Short summary
The role of mountain headwater area in hydrological cycle was investigated at two opposite hillslopes covered by mineral and organic soils. Similarities and differences in percolation and preferential flow paths between the hillslopes were identified by sprinkling experiments with Brilliant Blue and Fluorescein. The dye solutions infiltrated into the soil and continued either as lateral subsurface pipe flow (organic soil), or percolated vertically towards the bedrock (mineral soil).
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