Sampson flow

Sampson flow is defined as fluid flow through an infinitely thin orifice in the viscous flow regime for low Reynolds number. It is derived from an analytical solution to the Navier-Stokes equations. The below equation can be used to calculate the total volumetric flowrate through such an orifice: ^{[1] [2] [3] [4] [5]}

${\displaystyle Q_{S}=\Delta Pd^{3}/24\mu }$

Here, ${\displaystyle Q_{S}}$ is the volumetric flowrate in ${\displaystyle m^{3}/sec}$, ${\displaystyle \Delta P}$ is the pressure difference in Pa, ${\displaystyle d}$ is the pore diameter in m, and ${\displaystyle \mu }$ is the fluid's dynamic viscosity in Pa·s. The flow can also be expressed as a molecular flux as:

${\displaystyle J_{S}=P_{ave}\Delta Pd/6\pi \mu k_{B}T}$

Here, ${\displaystyle J_{S}}$ is the molecular flux in atoms/m²·sec, ${\displaystyle P_{ave}}$ is the average of the pressures on either side of the orifice, ${\displaystyle k_{B}}$ is the Boltzmann constant, (${\displaystyle 1.38\times 10^{-23}}$ J/K), and ${\displaystyle T}$ is the absolute temperature in K.

Sampson flow is the macroscopic analog of effusion flow, which describes stochastic diffusion of molecules through an orifice much smaller than the mean-free-path of the gas molecules. For pore diameters on the order of the mean-free-path of the fluid, flow will occur with contributions from the molecular regime as well as the viscous regime, obeying the dusty gas model according to the following equation: ^[6]

${\displaystyle Q_{total}=Q_{S}+Q_{E}}$

Here, ${\displaystyle Q_{total}}$ is the total volumetric flowrate and ${\displaystyle Q_{E}}$ is the volumetric flowrate according to the law of effusion. As it turns out, for many gasses, we notice equal contributions from molecular and viscous regimes when the pore size is significantly larger than the mean-free-path of the fluid, for nitrogen this occurs at a pore diameter of 393 nm, 6.0× larger than the mean-free-path.^{[ citation needed ]}

References

1. Tio, K.-K.; Sadhal, S. S. (1994). "Boundary conditions for stokes flows near a porous membrane". Applied Scientific Research. 52: 1–20. doi:10.1007/BF00849164.
2. Sampson, R. A. (1891). "On Stokes's Current Function". Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 182: 449–518. Bibcode:1891RSPTA.182..449S. doi: 10.1098/rsta.1891.0012 .
3. Jensen, K. H.; Valente, A. X. C. N.; Stone, H. A. (2014). "Flow rate through microfilters: Influence of the pore size distribution, hydrodynamic interactions, wall slip, and inertia". Physics of Fluids. 26 (5): 052004. Bibcode:2014PhFl...26e2004J. doi:10.1063/1.4876937.
4. Roscoe, R. (1949). "XXXI. The flow of viscous fluids round plane obstacles". The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science. 40 (302): 338–351. doi:10.1080/14786444908561255.
5. Happel, J.; Brenner, H. (1983). "Low Reynolds number hydrodynamics: With special applications to particulate media". Journal of Aerosol Science. 6 (3–4): 273. Bibcode:1975JAerS...6R.273D. doi:10.1016/0021-8502(75)90096-8. ISBN   978-90-247-2877-0.
6. Petukhov, D. I.; Eliseev, A. A. (2016). "Gas permeation through nanoporous membranes in the transitional flow region". Nanotechnology. 27 (8): 085707. Bibcode:2016Nanot..27h5707P. doi:10.1088/0957-4484/27/8/085707. PMID   26821609. S2CID   32847411.