We build on the model developed in Pearson et al. (2013) which describes fluid flow, solute concentration and cell distribution in a HFMB.
where 0 < η < 1, α > 0. Such a boundary condition might be more realistic in the mathematical models of thermal conductivity, groundwater flow, thermoelectric flexibility and plasma physics, because it describes the fluid properties in a certain continuous medium.
This calibration process contributes to improve the reservoir model, i.e., to make it more reliable for predictions and to better describe fluid flows within the reservoir.
From such considerations are derived the differential equations that describe fluid motion (see fluid mechanics).
A unique formulation of describing fluid motion is presented.
Helmholtz knew of Euler's and Lagrange's previous mathematical formulas describing fluid motion.
Deriving analytical expressions to describe fluid flow in porous medium is a complex task.
In this section, comparisons and a field example are presented to describe fluid flow in NFTRs.
In this paper, we use and discuss Couette equation to describe fluid flow in natural fractures.
Hence this approach unifies the two classical methods for describing fluid flows.
