Published July 2008 | Version v1
Journal article

Collisions of particles advected in random flows

  • 1. Department of Physics, Goeteborg University, 41296 Gothenburg (Sweden)
  • 2. Department of Mathematics and Statistics, Open University, Walton Hall, Milton Keynes, MK7 6AA (United Kingdom)

Description

We consider collisions of particles advected in a fluid. As already pointed out by Smoluchowski (1917 Z. Phys. Chem. 92 129-68), macroscopic motion of the fluid can significantly enhance the frequency of collisions between the suspended particles. This effect was invoked by Saffman and Turner (1956 J. Fluid Mech. 1 16-30) to estimate collision rates of small water droplets in turbulent rain clouds, the macroscopic motion being caused by turbulence. Here, we show that the Saffman-Turner theory is unsatisfactory because it describes an initial transient only. The reason for this failure is that the local flow in the vicinity of a particle is treated as if it were a steady hyperbolic flow, whereas, in reality, it must fluctuate. We derive exact expressions for the steady-state collision rate for particles suspended in rapidly fluctuating random flows and compute how this steady state is approached. For incompressible flows, the Saffman-Turner expression is an upper bound

Availability note (English)

Available from http://dx.doi.org/10.1088/1367-2630/10/7/075014

Additional details

Publishing Information

Journal Title
New Journal of Physics
Journal Volume
10
Journal Issue
7
Journal Page Range
[23 p.]
ISSN
1367-2630

INIS

Country of Publication
United Kingdom
Country of Input or Organization
International Atomic Energy Agency (IAEA)
INIS RN
40024469
Subject category
S71: CLASSICAL AND QUANTUM MECHANICS, GENERAL PHYSICS;
Descriptors DEI
CLOUDS; COLLISIONS; DROPLETS; INCOMPRESSIBLE FLOW; MATHEMATICAL MODELS; RAIN; RANDOMNESS; STEADY-STATE CONDITIONS; TURBULENCE; TURBULENT FLOW; WATER
Descriptors DEC
ATMOSPHERIC PRECIPITATIONS; FLUID FLOW; HYDROGEN COMPOUNDS; OXYGEN COMPOUNDS; PARTICLES