On the role of rock fragments and initial soil water content in the potential subsurface runoff formation
By: Hana Hlaváčiková, Viliam Novák and Ladislav Holko
References
- Allaire, S. E., Roulier, S., Cessna, A., 2009. Quantifying preferential flow in soils: A review of different techniques. J. Hydrol., 378, 179-204.
- Beven, K., German, P., 1982. Macropores and water flow in soils. Water Resour. Res., 18, 5, 1311-1325.
- Bičárová, S., Holko, L., 2013. Changes of characteristics of daily precipitation and runoff in the High Tatra Mountains, Slovakia over the last fifty years. Contributions to Geophysics and Geodesy, 43, 2, 157-177.
- Bouwer, H., Rice, R.C., 1984. Hydraulic properties of stony vadose zones. Ground Water, 22, 6, 696-705.
- Brakensiek, D.L., Rawls, W.J., Stephenson, G.R., 1986. Determining the saturated hydraulic conductivity of a soil containing rock fragments. Soil Sci. Soc. Am. J., 50, 834-835.
- Buchter, B., Hinz, C., Flűhler, H., 1994. Sample size for determination of coarse fragment content in a stony soil. Geoderma, 63, 265−275.
- Childs, S.W., Flint, A.L., 1990. Physical properties of forest soils containing rock fragments. In: Gessel, S.P., Lacate, D.S.,Weetman, G.F., Powers, R.F. (Eds.): Sustained productivity of forest soils, Proceedings of the 7th North American forest soils conference. University of British Columbia, Faculty of Forestry Publication, Vancouver, Canada, pp. 95-121.
- Coppola, A., Dragonetti, G., Comegna, A., Lamaddalena, N., Caushi, B., Haikal, M.A., Basile, A., 2013. Measuring and modeling water content in stony soils. Soil & Tillage Research, 128, 9−22.
- Cousin, I., Nicollaud, B., Coutadeur, C., 2003. Influence of rock fragments on the water retention sand and water percolation in a calcareous soil. Catena, 53, 97−114.
- Dóša, M., Holko, L., Martincová, M., Danko, M., Kostka, Z., Gomboš, M., 2012. Determination of soil hydraulic conductivity in the mountain catchment by soil texture and field measurements. Acta Hydrologica Slovaca, 13, 2, 350-357. (In Slovak.)
- Durner, W., 1994. Hydraulic conductivity estimation for soils with heterogeneous pore structure. Water Resour. Res., 30, 211-223.
- Dusek, J., Vogel, T., 2014. Modeling subsurface hillslope runoff dominated by preferential flow: One- vs. twodimensional approximation. Vadose Zone J., 13, doi:10.2136/vzj2013.05.0082.
- Fiés, J.C., De Louvigny, N., Chanzy, A., 2002. The role of stones in soil water retention. Eur. J. Soil. Sci., 53, 95-104.
- Hewlett, J.D., Hibbert, A.R., 1967. Factors affecting the response of small watersheds to precipitation in humid areas. In: Proc. International Symposium on Forest Hydrology. Pergamon, Oxford, pp. 275-290.
- Holko, L., Kostka, Z., Šanda, M., 2011. Assessment of frequency and areal extent of overland flow generation in a forested mountain catchment. Soil Water Res., 6, 1, 43-53.
- Hopp, L., McDonnell, J.J., 2009. Connectivity at the hillslope scale: Identifying interactions between storm size, bedrock permeability, slope angle and soil depth. Journal of Hydrology, 376, 378-391.
- Hraško, J., Bedrna, Z., 1988. Applied Soil Science. Priroda Publ. House, Bratislava, 474 p. (In Slovak.) Hrnčíř, M., Šanda, M., Kulasová, A., Císlerová, M., 2010. Runoff formation in a small catchment at hillslope and catchment scales. Hydrol. Process., 24, 2248-2256.
- Kostka, Z. 2009. Runoff response to rainfall event in the mountain catchment. (In Slovak with English abstract). Acta Hydrologica Slovaca, 10, 1, 130−139.
- Lin, H., 2010. Linking principles of soil formation and flow regimes. J. Hydrol., 393, 3-19.
- Lovelland, P.J., Whalley, W.R., 2001. Particle size analysis. In: Smith, K.A., Mullins, C.E. (Eds): Soil and Environmental Analysis Physical Method. Dekker Press, New York, USA.
- Ma, D.H., Shao, M., 2008. Simulating infiltration into stony soils with a dual-porosity model. Eur. J. Soil Sci., 59, 950-959.
- Ma, D. H., Shao, M. A., Zhang, J. B., Wang, Q., J., 2010. Validation of an analytical method for determining soil hydraulic properties of stony soils using experimental data. Geoderma, 159, 262-269.
- Mosley, M. P., 1979. Streamflow generation in a forested watershed. Water Resour. Res., 15, 795-806.
- Novák, V., Kňava, K., Šimůnek, J., 2011. Determining the influence of stones on hydraulic conductivity of saturated soils using numerical method. Geoderma, 161, 177-181.
- Pavelková, H., Dohnal, M., Vogel, T., 2012. Hillslope runoff generation - comparing different modeling approaches. J. Hydrol. Hydromech., 60, 2, 73-86.
- Peck, A.J., Watson, J.D., 1979. Hydraulic conductivity and flow in non-uniform soil. Workshop on soil physics and soil heterogeneity. CSIRO Division of Environmental Mechanics, Canberra, Australia.
- Poesen, J., Lavee, H., 1994. Rock fragments in top soils: significance and processes. Catena, 23, 1-28.
- Ravina, I., Magier, J., 1984. Hydraulic conductivity and water retention of clay soils containing coarse fragments. Soil Sci. Soc. Am. J., 48, 736-740.
- Šály, R., 1978. Soil − Basic Component of Forest Production. Priroda Publ. House, Bratislava, 235 p. (In Slovak.) Šanda, M., Císlerová, M., 2009. Transforming hydrographs in the hillslope subsurface. J. Hydrol. Hydromech., 57, 4, 264-275.
- Sauer, T.J., Logsdon, S.D., 2002. Hydraulic and physical properties of stony soils in a small watershed. Soil. Sci. Soc. Am. J., 66, 1947-1956.
- Schaap, M.G., van Genuchten, M.Th., 2005. A modified Mualem-van Genuchten formulation for improved description of the hydraulic conductivity near saturation. Vadose Zone J., 5, 27-34.
- Shi, Z., Wang, Y., Yu, P., Xu, L., Xiong, W., Guo, H., 2008. Effect of rock fragments on the percolation and evaporation of forest soil in Liupan Mountains, China. Acta Ecologica Sinica, 28, 12, 6090-6098.
- Šimůnek, J., Šejna, M., 2007. HYDRUS (2D/3D), Software Package for Simulating Two- and Three-Dimensional Movement of Water, Heat, and Multiple Solutes in Variably- Saturated Media. User Manual, Version 1.02. PC Progress, Prague, Czech Republic, 203 p.
- Šimůnek, J., Šejna, M., Saito, H., Sakai, M., van Genuchten, M.Th., 2008. The HYDRUS-1D Software Package for Simulating the One-dimensional Movement of Water, Heat, and Multiple Solutes in Variably-Saturated Media. Version 4.0, Hydrus Series 3. Department of Environmental Sciences, University of California Riverside, Riverside, CA, USA, 281 p.
- Tani, M., 1997. Runoff generation processes estimated from hydrological observations on a steep forested hillslope with a thin soil layer. J. Hydrol., 200, 84-109.
- Tromp-van Meerveld, H.J., McDonnell, J.J., 2006. Threshold relations in subsurface stormflow: 1. A 147-storm analysis of the Panola hillslope. Water Resour. Res., 42, W02410, doi: 10.1029/2004WR003778.
- van Genuchten, M.Th., 1980. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Sci.Soc.A.J., 44, 987-996.
- Verbist, K., Baetens, J., Cornelis, W.M., Gabriels, D., Torres, C., Soto, G., 2009. Hydraulic Conductivity as Influenced by Stoniness in Degraded Drylands of Chile. Soil Sci. Soc. Am. J., 73, 2, 471-484.
- Vogel, T., van Genuchten, M.Th., Cislerová, M., 2001. Effect of the shape of the soil hydraulic functions near saturation on variably-saturated flow predictions. Advances in Water Res., 24, 133-144.
- Whipkey, R.Z., 1965. Subsurface stormflow from forested slopes. Bull. Int. Assoc. Sci. Hydrol., 10, 2, 74-85.
- Zhou, B., Shao, M., Shao, H., 2009. Effects of rock fragments on water movement and solute transport in a Loess Plateau soil. C.R. Geoscience, 341, 462-472.
DOI: https://doi.org/10.1515/johh-2015-0002 | Journal eISSN: 1338-4333 (formerly 0042-790X) | Journal ISSN: 0042-790X
Language: English
Page range: 71 - 81
Submitted on: Oct 21, 2013
Accepted on: Sep 4, 2014
Published on: Jan 28, 2015
Published by: Slovak Academy of Sciences, Institute of Hydrology
In partnership with: Paradigm Publishing Services
Related subjects:
© 2015 Hana Hlaváčiková, Viliam Novák, Ladislav Holko, published by Slovak Academy of Sciences, Institute of Hydrology
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.