The classical Darcy law is generalised by regarding the water flow as a function of a non-integer order derivative of the piezometric head. This generalised law and the law of conservation of mass are then used to derive a new equation for groundwater flow. Numerical solutions of this equation for various fractional orders of the derivatives are compared with experimental data and the Barker generalised radial flow model for which a fractal dimension for the flow is assumed. Water SA Vol.32 (1) 2005: pp.1-
The purposes of this paper are primarily to research on behavior of groundwater flow in saturated an...
The purpose of this thesis is to use basic ideas of Mathematics and Physics, such as Darcy's Law and...
Groundwater flow in saturated geological porous media is described step by step. The representative ...
Formulations of natural phenomena are derived, sometimes, from experimentation and observation. Math...
This paper presents a set of fractional Boussinesq equations (fBEs) for groundwater flow in confined...
This work consists of a study of particular aspects of nonlinear flow equations and a non-traditiona...
The first part of the slide show consists of reminders about the basic concepts and equations of sat...
The sustainable exploitation of groundwater resources is a multifaceted and complex problem, which i...
A new model of groundwater flowing within a confined aquifer was proposed using the concept of local...
AbstractTraditional groundwater flow modelling is based on the Darcy's law which is valid when the f...
In fractured rock systems, ground water flow is not as simple and as methodical as in a porous mediu...
Darcy’s law is the basic law of flow, and it produces a partial differential equation is similar to ...
In this chapter, the differential groundwater flow equation that governs the distribution of the flo...
ABSTRACTThe Theis solution is the most widely used solution for determination of confined aquifer pa...
Non-Darcian flow in a finite fractured aquifer is studied in this thesis. A stream bounds the aquife...
The purposes of this paper are primarily to research on behavior of groundwater flow in saturated an...
The purpose of this thesis is to use basic ideas of Mathematics and Physics, such as Darcy's Law and...
Groundwater flow in saturated geological porous media is described step by step. The representative ...
Formulations of natural phenomena are derived, sometimes, from experimentation and observation. Math...
This paper presents a set of fractional Boussinesq equations (fBEs) for groundwater flow in confined...
This work consists of a study of particular aspects of nonlinear flow equations and a non-traditiona...
The first part of the slide show consists of reminders about the basic concepts and equations of sat...
The sustainable exploitation of groundwater resources is a multifaceted and complex problem, which i...
A new model of groundwater flowing within a confined aquifer was proposed using the concept of local...
AbstractTraditional groundwater flow modelling is based on the Darcy's law which is valid when the f...
In fractured rock systems, ground water flow is not as simple and as methodical as in a porous mediu...
Darcy’s law is the basic law of flow, and it produces a partial differential equation is similar to ...
In this chapter, the differential groundwater flow equation that governs the distribution of the flo...
ABSTRACTThe Theis solution is the most widely used solution for determination of confined aquifer pa...
Non-Darcian flow in a finite fractured aquifer is studied in this thesis. A stream bounds the aquife...
The purposes of this paper are primarily to research on behavior of groundwater flow in saturated an...
The purpose of this thesis is to use basic ideas of Mathematics and Physics, such as Darcy's Law and...
Groundwater flow in saturated geological porous media is described step by step. The representative ...