Limitation of the transport capacity approach in sediment transport modeling (2007)
Sander, G. C., Barry, D. A., Parlange, M. B., Hogarth, W. L.
Limitation of the transport capacity approach in sediment transport modeling (2007)
Sander, G.C., Parlange, J.Y., Barry, D.A., Parlange, M.B., Hogarth, W.L.
In a recent paper by Polyakov and Nearing (2003) it was shown experimentally that the sediment transport capacity in a rill is not unique for a given soil type, slope, and flow rate. Indeed, they...
Dynamic erosion of soil in steady sheet flow (2007)
Rose, Calvin Wyatt, Yu, Bofu, Ghadiri, Hossein, Asadi, Hossein, Parlange, J. Y., Hogarth, W.L., ...
Yes
Dynamic erosion of soil in steady sheet flow (2007)
Rose, Calvin Wyatt, Yu, Bofu, Ghadiri, Hossein, Asadi, Hossein, Parlange, J. Y., Hogarth, W.L., ...
Yes
Dynamic erosion of soil in steady sheet flow (2007)
Rose, Calvin Wyatt, Yu, Bofu, Ghadiri, Hossein, Asadi, Hossein, Parlange, J. Y., Hogarth, W.L., ...
Butler, H. J., McTainsh, G. H., Hogarth, W. L.
Spatial and temporal variations in vegetation and soil surface conditions of rangelands add a level of complexity to wind erosion processes which is often difficult to model or measure. Butler and...
Butler, H. J., McTainsh, G. H., Hogarth, W. L.
Spatial and temporal variations in vegetation and soil surface conditions of rangelands add a level of complexity to wind erosion processes which is often difficult to model or measure. Butler and...
Butler, H. J., McTainsh, G. H., Hogarth, W. L.
Spatial and temporal variations in vegetation and soil surface conditions of rangelands add a level of complexity to wind erosion processes which is often difficult to model or measure. Butler and...
Butler, H. J., McTainsh, G. H., Hogarth, W. L.
Spatial and temporal variations in vegetation and soil surface conditions of rangelands add a level of complexity to wind erosion processes which is often difficult to model or measure. Butler and...
Butler, H. J., McTainsh, G. H., Hogarth, W. L.
Spatial and temporal variations in vegetation and soil surface conditions of rangelands add a level of complexity to wind erosion processes which is often difficult to model or measure. Butler and...
Soil properties and water movement, In (2005)
Steenhuis, T. S., Haverkamp, R., Barry, D. A., Culligan, P. J., Hogarth, W. L., ...
Sudden drawdown and drainage of a horizontal aquifer. (2005)
F. Stagnitti,, A. Heilig,, J. Szilagyi,, T. S. Steenhuis., ...
Comments on “Exact solution for horizontal redistribution by general similarity” (2005)
Lockington, D., Sander, G., Hogarth, W. L., Barry, D. A., Li, L., ...
Drying front in a sloping aquifer: Nonlinear effects (2005)
Stagnitti, F., Li, L., Brutsaert, W., Lockington, D. A., Steenhuis, T. S., ...
Reply to the “Comments on ‘On an exact analytical solution of the Boussinesq equation’” (2005)
Barry, D. A., Hogarth, W. L., Govindaraju, R. S., Parlange, M. B., Lockington, D.
Butler, H. J., McTainsh, G. H., Hogarth, W. L., Leys, J. F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover are far from uniform. Field measurements taken within rangeland environments show that the shape of vertical dust...
Butler, H. J., McTainsh, G. H., Hogarth, W. L., Leys, J. F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover arefar from uniform. Field measurements taken within rangeland environments show thatthe shape of vertical dust...
Butler, H. J., McTainsh, G. H., Hogarth, W. L., Leys, J. F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover are far from uniform. Field measurements taken within rangeland environments show that the shape of vertical dust...
Butler, H. J., McTainsh, G. H., Hogarth, W. L., Leys, J. F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover arefar from uniform. Field measurements taken within rangeland environments show thatthe shape of vertical dust...
Interaction of wetting fronts with an impervious surface-longer time behavior (2005)
Hogarth, W. L., Fuentes, C., Sprintall, J., Haverkamp, R., Elrick, D., ...
Addendum to 'Interaction of wetting fronts with an impervious surface' (2005)
Hogarth, W. L., Sprintall, J., Haverkamp, R., Parlange, M. B.
Barry, D. A., Parlange, M. B., Hogarth, W. L., Haverkamp, R., Ross, P. J., ...
A general approximation for the solution to the one-dimensional Richards equation is presented. It applies to arbitrary soil properties and boundary conditions but only uniform initial conditions at...
On an exact analytical solution of the Boussinesq equation (2005)
Hogarth, W. L., Govindaraju, R. S., Parlange, M. B., Lockington, D.
A useful exact analytical solution of the Boussinesq equation is discussed and is the most general solution presently available, and in particular yields a solution for a finite aquifer. It provides...
Sudden drawdown and drainage of a horizontal aquifer (2005)
Stagnitti, F., Heilig, A., Szilagyi, J., Parlange, M. B., Steenhuis, T. S., ...
Comments on 'Exact solution for horizontal redistribution by general similarity' (2005)
Lockington, D., Sander, G., Hogarth, W. L., Barry, D. A., Li, L., ...
Drying front in a sloping aquifer: Nonlinear effects (2005)
Stagnitti, F., Li, L., Brutsaert, W., Lockington, D. A., Steenhuis, T. S., ...
Butler, H.J., McTainsh, Grant Harvey, Hogarth, W.L., Leys, J.F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover are far from uniform. Field measurements taken within rangeland environments show that the shape of vertical dust...
Interpolation between Darcy-Weisbach and Darcy for laminar and turbulent flows (2005)
Hogarth, W.L., Rose, Calvin Wyatt, Fuentes, C., Haverkamp, R., Walker, M.T.
An equation describing flow in an open channel with obstacles is derived, following the conservation of momentum approach used by Bélanger and St. Venant. When the obstacles are all submerged the...
Gao, B., Walter, M.T., Steenhuis, T.S., Richards, B.K., Hogarth, W.L., ...
A simple modeling and laboratory investigation was carried out to investigate the raindrop effects on both sediment detachment and chemical transport from soil water into runoff. Solute movement...
Butler, H.J., McTainsh, Grant Harvey, Hogarth, W.L., Leys, J.F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover are far from uniform. Field measurements taken within rangeland environments show that the shape of vertical dust...
Interpolation between Darcy-Weisbach and Darcy for laminar and turbulent flows (2005)
Hogarth, W.L., Rose, Calvin Wyatt, Fuentes, C., Haverkamp, R., Walker, M.T.
An equation describing flow in an open channel with obstacles is derived, following the conservation of momentum approach used by Bélanger and St. Venant. When the obstacles are all submerged the...
Gao, B., Walter, M.T., Steenhuis, T.S., Richards, B.K., Hogarth, W.L., ...
A simple modeling and laboratory investigation was carried out to investigate the raindrop effects on both sediment detachment and chemical transport from soil water into runoff. Solute movement...
Butler, H. J., McTainsh, G. H., Hogarth, W. L., Leys, J. F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover are far from uniform. Field measurements taken within rangeland environments show that the shape of vertical dust...
Butler, H.J., McTainsh, Grant Harvey, Hogarth, W.L., Leys, J.F.
In rangelands, unlike cultivated fields, soil surface conditions and vegetation cover are far from uniform. Field measurements taken within rangeland environments show that the shape of vertical dust...
Interpolation between Darcy-Weisbach and Darcy for laminar and turbulent flows (2005)
Hogarth, W.L., Rose, Calvin Wyatt, Fuentes, C., Haverkamp, R., Walker, M.T.
An equation describing flow in an open channel with obstacles is derived, following the conservation of momentum approach used by Bélanger and St. Venant. When the obstacles are all submerged the...
Gao, B., Walter, M.T., Steenhuis, T.S., Richards, B.K., Hogarth, W.L., ...
A simple modeling and laboratory investigation was carried out to investigate the raindrop effects on both sediment detachment and chemical transport from soil water into runoff. Solute movement...
Hogarth, W.L., Rose, Calvin Wyatt, Parlange, J.Y., Sander, G.C., Carey, G.
Dynamic changes take place in the nature of sediment eroded from bare soil at low slopes by rainfall impact when there is no inflow of water at the top of the eroding slope. This relates initially to...
Hogarth, W.L., Rose, Calvin Wyatt, Sander, G.C., Steenhuis, T.S., Barry, Andrew, ...
An approximate analytical solution is obtained for a physically based model of soil erosion on a gentle slope driven by rainfall impact in which there is inflow of clear or nearly clear water to the...
Rose, Calvin Wyatt, Gao, Bin, Walter, M.T., Steenhuis, T.S., Nakano, K., ...
No
Hogarth, W.L., Rose, Calvin Wyatt, Parlange, J.Y., Sander, G.C., Carey, G.
Dynamic changes take place in the nature of sediment eroded from bare soil at low slopes by rainfall impact when there is no inflow of water at the top of the eroding slope. This relates initially to...
Hogarth, W.L., Rose, Calvin Wyatt, Sander, G.C., Steenhuis, T.S., Barry, Andrew
An approximate analytical solution is obtained for a physically based model of soil erosion on a gentle slope driven by rainfall impact in which there is inflow of clear or nearly clear water to the...
Rose, Calvin Wyatt, Gao, Bin, Walter, M.T., Steenhuis, T.S., Nakano, K., ...
No
Hogarth, W.L., Rose, Calvin Wyatt, Parlange, J.Y., Sander, G.C., Carey, G.
Dynamic changes take place in the nature of sediment eroded from bare soil at low slopes by rainfall impact when there is no inflow of water at the top of the eroding slope. This relates initially to...
Hogarth, W.L., Rose, Calvin Wyatt, Sander, G.C., Steenhuis, T.S., Barry, Andrew
An approximate analytical solution is obtained for a physically based model of soil erosion on a gentle slope driven by rainfall impact in which there is inflow of clear or nearly clear water to the...
Hogarth, W. L., Rose, C. W., Sander, G. C., Steenhuis, T. S., Barry, Andrew
An approximate analytical solution is obtained for a physically based model of soil erosion on a gentle slope driven by rainfall impact in which there is inflow of clear or nearly clear water to the...
Hogarth, W. L., Rose, C. W., Parlange, J. Y., Sander, G. C., Carey, G.
Dynamic changes take place in the nature of sediment eroded from bare soil at low slopes by rainfall impact when there is no inflow of water at the top of the eroding slope. This relates initially to...
Gao, Bin, Walter, M. T., Steenhuis, T. S., Nakano, K., Rose, Calvin Wyatt, ...
This work extends the simple experimental studies initiated by Heilig et al. [J. Hydrol. 244(2001) 9] to study erosion processes inherent to a mechanistic soil erosion model (the Rose model) that...
Addendum to overland flow to and through a segment of uniform resistance (2003)
Hogarth, W. L., Rose, Calvin Wyatt
The St Venant equation is used to model the steady flow of water on a low slope through a grass buffer strip represented by beds of nails of various densities. The analytical solution is obtained...