Sentence examples for analytical inflow from inspiring English sources

The analytical inflow performance relationships (IPRs) of horizontal gas wells are presented in this paper for different reservoir boundary conditions.

To avoid extensive analytical efforts to measure inflow and outflow fluxes at each time interval, the users can use an empirical or a kinetic model to estimate the time-dependent inflow/outflow fluxes for the mini-FBAs through an entire growth period based on limited measurement data.

This paper provides analytical methods for estimating groundwater inflow rate taking into account the groundwater table drawdown.

The significance of this variable is discussed in the 1st part of the paper which presents an analytical solution assessing ground water inflow rate into a tunnel using a mathematical derivation that takes into account the excavation-induced rock permeability reduction in the vicinity of a tunnel based on hydro-mechanical coupling effect.

It is based on approximate analytical solutions for the 2D inflow performance of an infinite-conductivity fracture in a rectangular drainage area and the near-well pressure drop for flow to a circular well in a vertical cross-section of the reservoir.

In this paper, the groundwater assessment modelling of mine pits was discussed in predicting of groundwater inflows and reviewing analytical and numerical approaches.

Analytical solutions exist to calculate tunnel inflow, and, increasingly, numerical groundwater models are used to this end.

In the 2nd part of the paper, results from numerical analysis are presented to verify the proposed analytical solution for estimating ground water inflow rate into a tunnel.

In this work, a new semi-analytical model that couples the reservoir inflow to the downhole flow is developed for predicting the performance of horizontal wells with inflow control devices in a box-shaped reservoir with bottom-water drive.

Current practice for estimating water inflow rate relies mostly on analytical solutions which assume a homogeneous, isotropic porous medium around a tunnel.

At outflow points the boundary values at the upper time-level are obtained from data at the present time-level within and on the boundary via the analytical solutions, while the boundary values at inflow points remain constant in time.