An analytical solution is presented for groundwater flow to a well in an aquifer with double-porosity behavior and transient transfer between fractures and matrix. The solution is valid for fractional flow dimensions including linear, cylindrical or spherical flow to the well and for fractional inter-porosity diffusive transfer including release from storage in infinite slabs, infinite cylinders or spherical matrix blocks. Approximations are also presented for small and large times that are easy to evaluate in practice. The solution can be used to analyze pumping tests via coupling with a parameter estimation code. The utility of the method is demonstrated by a practical example using data from a pumping test performed in a fractured chalk ...
Naturally fractured reservoirs as natural stores and conductors for fluid resources occur worldwide....
Natural and anthropogenic fractured aquifers and reservoirs are dual porosity matrix-fracture system...
The aim of this work was to convert the Thiem and the Theis groundwater flow equation to the time-fr...
Abstract In this paper, a finite fractured aquifer, bounded by a stream and impervious layers on the...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
In tracer test interpretation, fissured reservoirs are commonly referred to as double porosity syste...
The spatiotemporal evolution of transients in fractured rocks often displays unusual characteristics...
Utilizing the double-porosity approach it is assumed that porous medium is constituted by two groups...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
Constant flow, rate solutions are presented for a fractured reservoir with transient interporosity f...
A multi-borehole pumping and tracer test in fractured chalk is revisited and reinterpreted in the li...
A new double porosity model for Naturally Fractured Reservoirs (NFRs) assuming fractal fracture netw...
Using fractional calculus, a dimensionally consistent governing equation of transient, saturated gr...
This work consists of a study of particular aspects of nonlinear flow equations and a non-traditiona...
We propose a generalized methodology to predictthe deliverability of wells in fractional drainage ar...
Naturally fractured reservoirs as natural stores and conductors for fluid resources occur worldwide....
Natural and anthropogenic fractured aquifers and reservoirs are dual porosity matrix-fracture system...
The aim of this work was to convert the Thiem and the Theis groundwater flow equation to the time-fr...
Abstract In this paper, a finite fractured aquifer, bounded by a stream and impervious layers on the...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
In tracer test interpretation, fissured reservoirs are commonly referred to as double porosity syste...
The spatiotemporal evolution of transients in fractured rocks often displays unusual characteristics...
Utilizing the double-porosity approach it is assumed that porous medium is constituted by two groups...
Solute transport in the fractured porous confined aquifer is modeled by the advection-dispersion equ...
Constant flow, rate solutions are presented for a fractured reservoir with transient interporosity f...
A multi-borehole pumping and tracer test in fractured chalk is revisited and reinterpreted in the li...
A new double porosity model for Naturally Fractured Reservoirs (NFRs) assuming fractal fracture netw...
Using fractional calculus, a dimensionally consistent governing equation of transient, saturated gr...
This work consists of a study of particular aspects of nonlinear flow equations and a non-traditiona...
We propose a generalized methodology to predictthe deliverability of wells in fractional drainage ar...
Naturally fractured reservoirs as natural stores and conductors for fluid resources occur worldwide....
Natural and anthropogenic fractured aquifers and reservoirs are dual porosity matrix-fracture system...
The aim of this work was to convert the Thiem and the Theis groundwater flow equation to the time-fr...