Physics:Hele-Shaw flow

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Short description: Concept in fluid mechanics

Hele-Shaw flow is defined as flow taking place between two parallel flat plates separated by a narrow gap satisfying certain conditions, named after Henry Selby Hele-Shaw, who studied the problem in 1898.[1][2] Various problems in fluid mechanics can be approximated to Hele-Shaw flows and thus the research of these flows is of importance. Approximation to Hele-Shaw flow is specifically important to micro-flows. This is due to manufacturing techniques, which creates shallow planar configurations, and the typically low Reynolds numbers of micro-flows.

The conditions that needs to be satisfied are

hl1,Uhνhl1

where h is the gap width between the plates, U is the characteristic velocity scale, l is the characteristic length scale in directions parallel to the plate and ν is the kinematic viscosity. Specifically, the Reynolds number Re=Uh/ν need not always be small, but can be order unity or greater as long as it satisfies the condition Re(h/l)1. In terms of the Reynolds number Rel=Ul/ν based on l, the condition becomes Rel(h/l)21.

The governing equation of Hele-Shaw flows is identical to that of the inviscid potential flow and to the flow of fluid through a porous medium (Darcy's law). It thus permits visualization of this kind of flow in two dimensions.[3][4]Cite error: Closing </ref> missing for <ref> tag

ωx=12μpy(h2z),ωy=12μpx(h2z),ωz=0.

Since ωz=0, the streamline patterns in the xy-plane thus correspond to potential flow (irrotational flow). Unlike potential flow, here the circulation Γ around any closed contour C (parallel to the xy-plane), whether it encloses a solid object or not, is zero,

Γ=Cvxdx+vydy=12μz(hz)C(pxdx+pydy)=0

where the last integral is set to zero because p is a single-valued function and the integration is done over a closed contour.

Depth-averaged form

In a Hele-Shaw channel, one can define the depth-averaged version of any physical quantity, say φ by

φ1h0hφdz.

Then the two-dimensional depth-averaged velocity vector 𝐮𝐯xy, where 𝐯xy=(vx,vy), satisfies the Darcy's law,

12μh2𝐮=pwith𝐮=0.

Further, ω=0.

Hele-Shaw cell

The term Hele-Shaw cell is commonly used for cases in which a fluid is injected into the shallow geometry from above or below the geometry, and when the fluid is bounded by another liquid or gas.[5] For such flows the boundary conditions are defined by pressures and surface tensions.

See also

References

  1. Shaw, Henry S. H. (1898). Investigation of the nature of surface resistance of water and of stream-line motion under certain experimental conditions. Inst. N.A.. OCLC 17929897. 
  2. Hele-Shaw, H. S. (1 May 1898). "The Flow of Water". Nature 58 (1489): 34–36. doi:10.1038/058034a0. Bibcode1898Natur..58...34H. 
  3. Hermann Schlichting,Boundary Layer Theory, 7th ed. New York: McGraw-Hill, 1979.
  4. L. M. Milne-Thomson (1996). Theoretical Hydrodynamics. Dover Publications, Inc.
  5. Saffman, P. G. (21 April 2006). "Viscous fingering in Hele-Shaw cells". Journal of Fluid Mechanics 173: 73–94. doi:10.1017/s0022112086001088. https://authors.library.caltech.edu/10133/1/SAFjfm86.pdf.