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Aerosol Stokes Relaxation Time Term Tool

Calculate aerosol stokes relaxation time term from explicit caller-supplied inputs.

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Description

Return Stokes particle relaxation time with a supplied slip factor.

Particle and droplet terms depend on size representation, weights, density, drag and logarithmic-bin conventions. A spherical growth or low-Reynolds approximation is a local model term rather than a measured size distribution, composition or health/exposure assessment.

Return Stokes particle relaxation time with a supplied slip factor.

When to use this tool

Use Aerosol Stokes Relaxation Time Term when checking the stated particle, droplet, drag, growth or bin-basis convention.

How to use the tool and how it works

  1. Enter particleDensity, diameter, slipCorrection, viscosity. Use the units and conventions below.
  2. Run the tool. Correct any format, range, or cross-field input error before interpreting the output.
  3. Read relaxationTime. Use the output convention below.

Return Stokes particle relaxation time with a supplied slip factor. Require density/diameter >= 0, viscosity/slipCorrection > 0; tau = density*diameter²*slipCorrection/(18*viscosity).1

Stokes drag describes a sphere in an appropriate viscous-flow regime. The low-Reynolds assumption must be checked separately before using a derived transport scale.2

Input fieldMeaning and unitsAccepted input
particleDensityParticle DensityRequired. Finite number; minimum 0.
diameterDiameterRequired. Finite number; minimum 0.
slipCorrectionSlip CorrectionRequired. Finite number; strictly above 0.
viscosityViscosityRequired. Finite number; strictly above 0.
Output fieldInterpretationReturned shape
relaxationTimeRelaxation TimeRequired. Finite number.
json
{
  "input": {
    "particleDensity": 1800,
    "diameter": 0.00001,
    "slipCorrection": 1,
    "viscosity": 0.00002
  },
  "output": {
    "relaxationTime": 0.0005
  }
}

Limitations and assumptions

  • This assumes an appropriate spherical low-Reynolds drag model; slip correction, actual particle properties and transport conditions are not derived.
  • Inputs must satisfy both the field types and the cross-field conditions above. Invalid input causes an error; a successful false flag or documented placeholder is a different result.
  • Numeric calculations use binary floating point unless exact decimal-integer arithmetic is explicitly stated. No hidden measurement tolerance or decimal rounding is added; nonfinite or out-of-contract results are rejected. Numeric signed-zero results are exported as zero.

Alternative or Complementary methods

Use verified particle measurements and an appropriate complete distribution/transport model with justified material, shape and flow assumptions for atmospheric inference.

References

  1. Calculation and input contract: atmospheric-physics/aerosol-stokes-relaxation-time-term — tool.io

  2. Motion of an object in a viscous fluid — OpenStax

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