Predicting subsurface stormflow response of a forested hillslope - the role of connected flow paths
暂无分享,去创建一个
[1] Keith Beven,et al. Macropores and water flow in soils revisited , 2013 .
[2] Markus Weiler,et al. Hillslope characteristics as controls of subsurface flow variability , 2012 .
[3] R. Helmig,et al. Modeling Macroporous Soils with a Two-Phase Dual-Permeability Model , 2012, Transport in Porous Media.
[4] D. Jongmans,et al. Application of geophysical measurements for assessing the role of fissures in water infiltration within a clay landslide (Trièves area, French Alps) , 2012 .
[5] Rabi H. Mohtar,et al. Field method for separating the contribution of surface‐connected preferential flow pathways from flow through the soil matrix , 2012 .
[6] Shahar Baram,et al. Water percolation through a clayey vadose zone , 2012 .
[7] Aldo Fiori,et al. On Preferential Flow, Channeling and Connectivity in Heterogeneous Porous Formations , 2012, Mathematical Geosciences.
[8] Thom Bogaard,et al. A conceptual model of the hydrological influence of fissures on landslide activity , 2011 .
[9] Jeffrey J. McDonnell,et al. Examining the role of throughfall patterns on subsurface stormflow generation , 2011 .
[10] Giuseppe Perale,et al. Diffusion and aggregation of sodium fluorescein in aqueous solutions. , 2011, The journal of physical chemistry. B.
[11] Erwin Zehe,et al. A novel explicit approach to model bromide and pesticide transport in connected soil structures , 2011 .
[12] Erwin Zehe,et al. Challenges in Understanding the Hydrologic Controls on the Mobility of Slow‐Moving Landslides , 2011 .
[13] Jeffrey J. McDonnell,et al. Gypsies in the palace: experimentalist's view on the use of 3‐D physics‐based simulation of hillslope hydrological response , 2010 .
[14] B. Kelly,et al. Detection of subsurface soil cracks by vertical anisotropy profiles of apparent electrical resistivity , 2010 .
[15] Julian Klaus,et al. Modelling rapid flow response of a tile‐drained field site using a 2D physically based model: assessment of ‘equifinal’ model setups , 2010 .
[16] S. R. Hencher,et al. Preferential flow paths through soil and rock and their association with landslides , 2010 .
[17] John L. Nieber,et al. How do disconnected macropores in sloping soils facilitate preferential flow? , 2010 .
[18] J. A. Jones,et al. Soil piping and catchment response , 2010 .
[19] Erwin Zehe,et al. The principle of ‘maximum energy dissipation’: a novel thermodynamic perspective on rapid water flow in connected soil structures , 2010, Philosophical Transactions of the Royal Society B: Biological Sciences.
[20] Rabi H. Mohtar,et al. New method for the characterization of three‐dimensional preferential flow paths in the field , 2010 .
[21] Erwin Zehe,et al. Plot and field scale soil moisture dynamics and subsurface wetness control on runoff generation in a headwater in the Ore Mountains , 2009 .
[22] Younes Alila,et al. Subsurface flow velocities in a hillslope with lateral preferential flow , 2009 .
[23] Jeffrey J. McDonnell,et al. Connectivity at the hillslope scale: identifying interactions between storm size, bedrock permeability, slope angle and soil depth. , 2009 .
[24] Hervé Andrieu,et al. Modeling the influence of an artificial macropore in sandy columns on flow and solute transfer , 2009 .
[25] M. Sivapalan,et al. Threshold behaviour in hydrological systems as (human) geo-ecosystems: Manifestations, controls, implications , 2009 .
[26] Erwin Zehe,et al. Applied tracers for the observation of subsurface stormflow at the hillslope scale , 2009 .
[27] Erwin Zehe,et al. Process identification through rejection of model structures in a mid‐mountainous rural catchment: observations of rainfall–runoff response, geophysical conditions and model inter‐comparison , 2009 .
[28] John Maximilian Köhne,et al. A review of model applications for structured soils: a) Water flow and tracer transport. , 2009, Journal of contaminant hydrology.
[29] S. Barbour,et al. Fracture‐Dominated Subsurface Flow and Transport in a Sloping Reclamation Cover , 2009 .
[30] Younes Alila,et al. Dye staining and excavation of a lateral preferential flow network. , 2008 .
[31] Stephen R. Green,et al. Preferential flow and transport in soil: progress and prognosis , 2007 .
[32] Isabelle Cousin,et al. Numerical modelling of direct current electrical resistivity for the characterisation of cracks in soils , 2007 .
[33] Richard P. Hooper,et al. Moving beyond heterogeneity and process complexity: A new vision for watershed hydrology , 2007 .
[34] N. Jarvis. A review of non‐equilibrium water flow and solute transport in soil macropores: principles, controlling factors and consequences for water quality , 2007 .
[35] Markus Weiler,et al. Conceptualizing lateral preferential flow and flow networks and simulating the effects on gauged and ungauged hillslopes , 2007 .
[36] Horst H. Gerke,et al. Preferential flow descriptions for structured soils , 2006 .
[37] J. McDonnell,et al. 112 Subsurface Stormflow , 2006 .
[38] S. Attinger,et al. Importance of spatial structures in advancing hydrological sciences , 2006 .
[39] Jeffrey J. McDonnell,et al. Threshold relations in subsurface stormflow: 1. A 147‐storm analysis of the Panola hillslope , 2006 .
[40] Jeffrey J. McDonnell,et al. Threshold relations in subsurface stormflow: 2. The fill and spill hypothesis , 2006 .
[41] Erwin Zehe,et al. Uncertainty of simulated catchment runoff response in the presence of threshold processes: Role of initial soil moisture and precipitation , 2005 .
[42] Roy C. Sidle,et al. Development of a simple lateral preferential flow model with steady state application in hillslope soils , 2005 .
[43] H. Vogel,et al. The dominant role of structure for solute transport in soil: Experimental evidence and modelling of structure and transport in a field experiment , 2005 .
[44] Jeffrey J. McDonnell,et al. The role of lateral pipe flow in hillslope runoff response: an intercomparison of non-linear hillslope response , 2005 .
[45] Erwin Zehe,et al. Process identification at a slow‐moving landslide in the Vorarlberg Alps , 2005 .
[46] Erwin Zehe,et al. Predictability of hydrologic response at the plot and catchment scales: Role of initial conditions , 2004 .
[47] Takahisa Mizuyama,et al. Numerical calculation of soil pipe flow and its effect on water dynamics in a slope , 2004 .
[48] Jeffrey J. McDonnell,et al. Virtual experiments: a new approach for improving process conceptualization in hillslope hydrology , 2004 .
[49] H. Elsenbeer,et al. Scale dependency in spatial patterns of saturated hydraulic conductivity , 2004 .
[50] G. Richard,et al. Electrical Resistivity Imaging for Detecting Soil Cracking at the Centimetric Scale , 2003 .
[51] Peter J. Shouse,et al. Lateral Water Diffusion in an Artificial Macroporous System: Modeling and Experimental Evidence , 2003 .
[52] Hans-Jörg Vogel,et al. Moving through scales of flow and transport in soil , 2003 .
[53] M. V. Genuchten,et al. Review and comparison of models for describing non-equilibrium and preferential flow and transport in the vadose zone , 2003 .
[54] Keith Beven,et al. The role of bedrock topography on subsurface storm flow , 2002 .
[55] J. Moncrief,et al. Role of macropore continuity and tortuosity on solute transport in soils: 2. Interactions with model assumptions for macropore description. , 2002, Journal of contaminant hydrology.
[56] J. Moncrief,et al. Role of macropore continuity and tortuosity on solute transport in soils: 1. Effects of initial and boundary conditions. , 2002, Journal of contaminant hydrology.
[57] J. A. A. Jones,et al. A semi-distributed simulation model for natural pipeflow , 2002 .
[58] James M. Buttle,et al. Coupled vertical and lateral preferential flow on a forested slope , 2002 .
[59] Takahisa Mizuyama,et al. Effects of pipeflow on hydrological process and its relation to landslide: a review of pipeflow studies in forested headwater catchments , 2001 .
[60] Karin Laursen,et al. A conceptual model of preferential flow systems in forested hillslopes: evidence of self‐organization , 2001 .
[61] Erwin Zehe,et al. Preferential transport of isoproturon at a plot scale and a field scale tile-drained site , 2001 .
[62] Takahisa Mizuyama,et al. Runoff characteristics of pipeflow and effects of pipeflow on rainfall-runoff phenomena in a mountainous watershed , 1999 .
[63] Shoji Noguchi,et al. Morphological Characteristics of Macropores and the Distribution of Preferential Flow Pathways in a Forested Slope Segment , 1999 .
[64] Kurt Roth,et al. Transport of conservative chemical through an unsaturated two‐dimensional Miller‐similar medium with steady state flow , 1996 .
[65] Graham E. Fogg,et al. Random-Walk Simulation of Transport in Heterogeneous Porous Media: Local Mass-Conservation Problem and Implementation Methods , 1996 .
[66] J. Buttle,et al. Runoff Production in a Forested, Shallow Soil, Canadian Shield Basin , 1995 .
[67] Hannes Flühler,et al. Transport of Anions and Herbicides in a Loamy and a Sandy Field Soil , 1995 .
[68] Hannes Flühler,et al. SUSCEPTIBILITY OF SOILS TO PREFERENTIAL FLOW OF WATER : A FIELD STUDY , 1994 .
[69] W. Durner. Hydraulic conductivity estimation for soils with heterogeneous pore structure , 1994 .
[70] M. Bonell. Progress in the understanding of runoff generation dynamics in forests , 1993 .
[71] M. V. Genuchten,et al. A dual-porosity model for simulating the preferential movement of water and solutes in structured porous media , 1993 .
[72] J. Nieber,et al. Soil pipe contribution to steady subsurface stormflow , 1991 .
[73] M. Celia,et al. A General Mass-Conservative Numerical Solution for the Unsaturated Flow Equation , 1990 .
[74] Glenn V. Wilson,et al. Physical and chemical controls of preferred path flow through a forested hillslope , 1990 .
[75] K. Beven,et al. Macropores and water flow in soils , 1982 .
[76] Van Genuchten,et al. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils , 1980 .
[77] Y. Mualem. A New Model for Predicting the Hydraulic Conductivity , 1976 .
[78] S. Moysey,et al. Can the Onset of Macropore Flow be Detected using Electrical Resistivity Measurements , 2012 .
[79] J. Ihringer,et al. Characterization of soil hydraulic properties on a creeping alpine slope. , 2009 .
[80] Felix Naef,et al. Subsurface storm flow formation at different hillslopes and implications for the ‘old water paradox’ , 2008 .
[81] J. Ihringer,et al. Modeling water flow and mass transport in a loess catchment , 2001 .