While there have been many studies of gravity-driven rivulet flow over an external surface, treatment of internal rivulets has been sparse. A notable exception is the analytical and experimental study by Anand and Bejan 1; they derived an approximate solution for a laminar rivulet developing between two parallel vertical planes and employed it to examine the transition to a meandering flow.
For rivulets flowing between closely spaced plates, the velocity becomes “slow” (i.e., “low” Reynolds number) and an approximately fully-developed flow at its terminal velocity can be reached in a short distance. Conceptually, this value can be derived from the analysis of Anand and Bejan. However, for cases where the inlet volumetric flow rate Q is sufficiently high that the rivulet becomes wide relative to the plate spacing, a simple treatment can describe the resulting flow.
For this treatment, we orient the coordinates as and to the vertical plates and assume:
• an incompressible fluid with constant properties
• steady, laminar flow (except at the leading edge outside the region of interest)
• fluid density much greater than density of its surroundings (so
• negligible interface shear with surroundings at edges
• fully-developed flow away from the inlet
• rivulet width in spanwise direction (W) considerably larger than edge region formed by curvature of free surfaces at the edges
Provided that the assumptions and approximations above are approached so that this treatment is valid, the results offer the possibilities of employing this configuration as a viscometer or flowmeter by measuring the appropriate quantities. For such applications the sensitivity to plate spacing makes its accurate measurement important. Alternatively, the measurement of the rivulet width, flow rate and viscosity can be used to estimate the plate spacing and, as a first approximation, its variation or the degree to which the plates are parallel.
Acknowledgments
The study reported was partly supported by the Environmental Management Science program through DoE Idaho Operations Office contract DE-AC07-99ID13727. The encouragement and advice of Dr. Paul Meakin, the Principal Investigator of the project, is appreciated.
Nomenclature
= hydraulic diameter,
- f
= Fanning friction factor,
- g
= acceleration of gravity
= units conversion factor, e.g., 1 kg m/(N s2)
= mass flow rate
= static pressure of surroundings (typically air)
- Q
= volumetric flow rate
- Re
= Reynolds number,
- s
= spacing between plates
- u
= vertical velocity component
= bulk or mixed mean vertical velocity
- W
= rivulet width
- x
= vertical coordinate
- y
= spanwise coordinate
- z
= normal coordinate
- μ
= absolute viscosity
- ν
= kinematic viscosity, μ/ρ
- ρ
= fluid density
= wall shear stress