Particle Terminal Velocity in Fluids Calculator

Advanced calculator for particle terminal velocity in diverse fluids with flexible inputs. Choose presets or enter fluid properties with intuitive unit switching today easily. Get velocity, Reynolds number, drag coefficient, and regime hints instantly. Export results to CSV and PDF, and save example scenarios for later. Iterative solver handles nonlaminar flows with robust stability.

White theme • Unit smart-convert • Iterative solver
Inputs Now with density models, PNG export, and φ helper
kg/m³
kg/m³
Set manually or use temperature models below.
°C
Used if viscosity or density source uses temperature.
kPa
Only used by air density model.
for time
φ
φ=1 sphere; smaller for irregular particles (Ganser uses φ).

0–0.6 typical
Results
Terminal velocity vt
Reynolds number Re
Drag coefficient Cd:
Stokes velocity vStokes
Useful when Re < 1
Settling time for H
Based on computed vt
Kinematic viscosity ν
Hindered velocity vh (R–Z)
n used: , C:
Density model status
Manual density in use.
If model selected, ρf auto-updates with T and P.
Run the solver to see regime and model hints.
Saved scenarios
# d (μm) ρₚ ρ_f μ g φ Model vt Re Load
Batch calculations
model: SN or Ganser; mode: auto or stokes; mu_unit: Pa.s or cP; C is solids fraction.
Upload CSV with header mapping
#d (μm)ρₚρ_fμgφModel vt (m/s)ReCd ν (m²/s)Cnvh (m/s)t(H) s
Example data
Case Particle Fluid d (μm) ρₚ (kg/m³) ρ_f (kg/m³) μ (Pa·s) g (m/s²) φ Action
1Silica sandWater ~20°C 30026509980.0019.806650.9
2Pollen grainAir ~20°C 3014001.2041.82e-59.806650.7
3Steel shotWater ~20°C 100078509980.0019.806651.0
Click Load to populate the inputs with the example values.
Formulas used

Stokes regime (Re ≪ 1): $$ v_{Stokes} = \frac{(\rho_p-\rho_f) g d^2}{18 \mu} $$

Force balance: $$ \frac{\pi}{6} d^3 (\rho_p-\rho_f) g = \frac{1}{2} C_d \rho_f \left(\frac{\pi}{4} d^2\right) v_t^2 $$ $$ v_t = \sqrt{ \frac{4 d (\rho_p-\rho_f) g}{3 C_d \rho_f} } $$

Sphere drag (Schiller–Naumann): $$ C_d = \begin{cases} \dfrac{24}{Re}\left(1+0.15\,Re^{0.687}\right), & Re \le 1000 \\[6pt] 0.44, & Re > 1000 \end{cases} $$

Ganser non-spherical drag (sphericity \( \phi \)): $$ Re^\* = Re \, K_1 \, K_2, \quad C_d = \frac{24}{Re^\*}\left(1+0.1118\,{Re^\*}^{0.6567}\right) + \frac{0.4305}{1 + 3305/Re^\*} $$ with $$ K_1 = \left(\tfrac{1}{3} + \tfrac{2}{3}\phi^{-0.5}\right)^{-1}, \qquad K_2 = 10^{\,1.8148\,[ -\log_{10}(\phi) ]^{0.5743}}. $$

Kinematic viscosity: \( \nu = \mu / \rho_f \).

Hindered settling (Richardson–Zaki): $$ v_h = v_t (1-C)^n, \quad \varepsilon = 1-C $$ \( n \) by Garside–Al-Dibouni: \[ n=\begin{cases} 4.65,& Re<0.2\\ 4.4\,Re^{-0.03},& 0.2\le Re<1\\ 4.4\,Re^{-0.10},& 1\le Re<500\\ 2.4,& Re\ge 500 \end{cases} \]

Air density (ideal gas): \( \rho_f = \dfrac{P}{R T} \), with \(R=287.058\) J·kg⁻¹·K⁻¹.

Water density (empirical) (°C): \( \rho_f \approx 1000\left[1 - \frac{(T-3.9863)^2(T+288.9414)}{508929.2\,(T+68.12963)}\right] \) kg/m³.

Assumptions: Newtonian carrier; ideal gas air; water fit near atmospheric pressure; no wall/slip/hindered‑bed corrections beyond R–Z.

How to use
  1. Select units and fluid preset or set properties.
  2. Choose viscosity source and density source; set temperature and pressure.
  3. Choose drag model and sphericity; enable R–Z if needed.
  4. Click Compute for v, Re, Cd, ν, and vh.
  5. Export table to CSV/PDF or capture the Results card to PNG.

Tips: φ helper suggests typical values by material/shape.

FAQs

Using the ideal gas relation ρ = P/(RT) with R=287.058 J·kg⁻¹·K⁻¹ and pressure you enter. It updates as you change T or P.

An empirical curve fit around atmospheric pressure gives fresh‑water density vs temperature. For saline water, enter ρ manually or use a seawater calculator.

It captures the Results card as an image with current outputs, perfect for reports or quick sharing.

Yes. The helper can set φ and switch the drag model to Ganser in one click.

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Important Note: All the Calculators listed in this site are for educational purpose only and we do not guarentee the accuracy of results. Please do consult with other sources as well.