Using fractional calculus, a dimensionally consistent governing equation of transient, saturated groundwater flow in fractional time in a multi-fractional confined aquifer is developed. First, a dimensionally consistent continuity equation for transient saturated groundwater flow in fractional time and in a multi-fractional, multidimensional confined aquifer is developed. For the equation of water flux within a multi-fractional multidimensional confined aquifer, a dimensionally consistent equation is also developed. The governing equation of transient saturated groundwater flow in a multi-fractional, multidimensional confined aquifer in fractional time is then obtained by combining the fractional continuity and water flux equations. ...
ABSTRACTThe Theis solution is the most widely used solution for determination of confined aquifer pa...
We report on generic relations between fractional flow and pressure in steady two-phase flow in poro...
The medium through which the groundwater moves varies in time and space. The Hantush equation descri...
In this study dimensionally consistent governing equations of continuity and motion for transient so...
The aim of this work was to convert the Thiem and the Theis groundwater flow equation to the time-fr...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
This work consists of a study of particular aspects of nonlinear flow equations and a non-traditiona...
Upscaling groundwater flow is a fundamental challenge in hydrogeology. This study proposed time-frac...
Abstract In this paper, a finite fractured aquifer, bounded by a stream and impervious layers on the...
An analytical solution is presented for groundwater flow to a well in an aquifer with double-porosit...
A new model of groundwater flowing within a confined aquifer was proposed using the concept of local...
We present a distributed-order fractional diffusion-wave equation (dofDWE) to describe radial ground...
This paper presents a set of fractional Boussinesq equations (fBEs) for groundwater flow in confined...
This book is an unique integrated treatise, on the concepts of fractional calculus as models with ap...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
ABSTRACTThe Theis solution is the most widely used solution for determination of confined aquifer pa...
We report on generic relations between fractional flow and pressure in steady two-phase flow in poro...
The medium through which the groundwater moves varies in time and space. The Hantush equation descri...
In this study dimensionally consistent governing equations of continuity and motion for transient so...
The aim of this work was to convert the Thiem and the Theis groundwater flow equation to the time-fr...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
This work consists of a study of particular aspects of nonlinear flow equations and a non-traditiona...
Upscaling groundwater flow is a fundamental challenge in hydrogeology. This study proposed time-frac...
Abstract In this paper, a finite fractured aquifer, bounded by a stream and impervious layers on the...
An analytical solution is presented for groundwater flow to a well in an aquifer with double-porosit...
A new model of groundwater flowing within a confined aquifer was proposed using the concept of local...
We present a distributed-order fractional diffusion-wave equation (dofDWE) to describe radial ground...
This paper presents a set of fractional Boussinesq equations (fBEs) for groundwater flow in confined...
This book is an unique integrated treatise, on the concepts of fractional calculus as models with ap...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
ABSTRACTThe Theis solution is the most widely used solution for determination of confined aquifer pa...
We report on generic relations between fractional flow and pressure in steady two-phase flow in poro...
The medium through which the groundwater moves varies in time and space. The Hantush equation descri...