Dimensionless Numbers


 

The Reynolds number (Re) is a dimensionless number that gives a measure of the balance of forces, between inertial and viscous forces, that are acting on a fluid. Above a critical number, usually around 2300, a small disturbance grows and eventually leads to turbulent flow (Philpotts, 1990). The Reynolds number of a fluid is defined as:

 

.

 

 

Where r is the radius of the flow, r = density of the fluid, v is velocity, and m is the viscosity. For large viscosities encountered in normal, felsic magmas (~106 to 108 Pa s), the Re numbers could be subcritical.

 

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Rayleigh number (Ra) is a dimensionless number that is used to predict the likelihood of convection in a system. The convection can be driven by either thermal-density inversions, or compositional gradients (Sparks et al., 1984). Values for RaT (thermal convection), Prandtl number (Pr), RaS (compositional convection), and diffusivity ratio (t) can be calculated as follows:

 

 and,

 

and.

 

Where, g = gravitational acceleration, aT = coefficient of thermal expansion, DT = temperature difference across the layer, d = the layer thickness, kT = thermal diffusivity, kS = compositional diffusivity, n = kinematic viscosity, b = coefficient of expansion due to compositional changes, and bDS = fractional density change across a layer due to compositional changes (Sparks et al., 1984).

 

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Damköhler Numbers are dimensionless numbers that characterize reaction rates (Ottino, 1989),

 

, and,

 

.

 

 

Where tD is the characteristic diffusion time-scale, tR the characteristic reaction time-scale, and tF is the characteristic fluid mechanical or deformation time-scale. These numbers are useful in determining the controls on reaction rates (i.e. diffusion controlled reaction).

 

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Viscosity can be thought as the resistance to flow. More fundamentally, viscosity is defined as (Turcotte and Schubert, 2002):

 

,

 

Another type of viscosity used in the previous equations is kinematic viscosity. This is a diffusivity similar to thermal diffusivity, only it describes how momentum diffuses instead of heat.

 

,

 

 

Where n = kinematic viscosity, m = viscosity, and r = density.

 

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