CMS-Flow:Sediment Fall Velocity: Difference between revisions

From CIRPwiki
Jump to navigation Jump to search
(Created page with "=Sediment Fall Velocity= The sediment fall velocity may be user-specified or is calculated using the formula by Soulsby (1997): {{Equation|<math>\omega_s = \frac{v}{d}\left ...")
 
No edit summary
Line 23: Line 23:


g = gravitational constant (9.81 m/s<sup>2</sup>).
g = gravitational constant (9.81 m/s<sup>2</sup>).
= References =
*Soulsby, R. L. 1997. Dynamics of marine sands. London, England: Thomas Telford Publications.

Revision as of 21:03, 14 January 2015

Sediment Fall Velocity

The sediment fall velocity may be user-specified or is calculated using the formula by Soulsby (1997):

  Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle \omega_s = \frac{v}{d}\left [(10.36^2 + 1.049d_* ^3)^{1/2} - 10.36 \right]} (1)

where:

v = kinematic viscosity [m2/s]

d = grain size [m]

d* = dimensionless grain size [-].


The dimensionless grain size is given by

  Failed to parse (SVG with PNG fallback (MathML can be enabled via browser plugin): Invalid response ("Math extension cannot connect to Restbase.") from server "https://en.wikipedia.org/api/rest_v1/":): {\displaystyle d_* = d \left [\frac{(s-1)g}{v^2}\right]^{1/3} } (2)

where:

s = sediment specific gravity or relative density [-]

g = gravitational constant (9.81 m/s2).

References

  • Soulsby, R. L. 1997. Dynamics of marine sands. London, England: Thomas Telford Publications.