Sedimentation Coefficient Calculator

Turn centrifugation readings into a clear sedimentation coefficient. Choose velocity or buoyancy workflows. Get Svedberg outputs, then download your results fast.

Visualization

If no calculation is shown, the chart displays the example S values.

Calculator

Pick a method, enter inputs, and compute the sedimentation coefficient. Required fields are marked *.

Switching method refreshes visible fields.
Both units are always computed.
Quick reference
1 S = 10−13 s • ω = 2π·RPM/60
Use the measured boundary speed in the radial direction.
Distance from rotor axis to the boundary position.
Choose rotor speed input format.
Converted internally to ω using 2π·RPM/60.
Use this if you already computed ω.
Sanity checks
  • Typical protein s values: ~2–20 S.
  • Very large assemblies can exceed 100 S.
  • Negative s suggests inconsistent inputs.

Example data table

These sample rows show typical inputs and the resulting coefficient in seconds and S units.

Case Method v (m/s) RPM r (m) s (s) s (S)
A Velocity 2.0e-6 45000 0.070 1.006e-13 1.006
B Velocity 3.5e-6 55000 0.065 1.716e-13 1.716
C Buoyancy 1.2e-19 1.1e-11 1000 7.3e-4 7.636e-13 7.636
Note: Example results are rounded for readability.

Formula used

Velocity-based definition
For a particle moving radially at speed v in a field ω²r:
s = v / (ω² r)
Where ω is angular velocity (rad/s) and r is radial distance (m).
Convert RPM to ω with ω = 2π·RPM/60.
Buoyancy/friction form
For mass m with friction coefficient f in solvent (ρ, v̄):
s = m(1 − ρv̄) / f
The term (1 − ρv̄) accounts for buoyant mass reduction.
Report in Svedberg: 1 S = 10⁻¹³ s.

How to use this calculator

  1. Choose a method: velocity-based for measured boundary speed, or buoyancy-based for material parameters.
  2. Enter required inputs using consistent SI units (m, s, kg, and kg/m³).
  3. Click Calculate. Your result appears above the form, just under the header.
  4. Use Download CSV for spreadsheets, or Download PDF for printing and sharing.
  5. Compare S values across samples to infer size, shape, and assembly state.

What the coefficient represents

Sedimentation coefficient s links radial motion to centrifugal acceleration and reflects size, shape, and hydration. In velocity form, s = v/(ω²r). If ω doubles, ω² rises fourfold and s drops 75% when v is unchanged. The unit is time; 1 Svedberg (1 S) equals 10⁻¹³ s, keeping values readable. Higher s generally indicates faster sedimentation under identical solvent and temperature conditions.

Typical ranges and scale

Many soluble proteins fall near 2–20 S, while large ribonucleoprotein complexes often exceed 50 S. A 10 S species corresponds to 1.0×10⁻¹² s. If your result is 0.2 S (2.0×10⁻¹⁴ s), re-check units: r must be meters, and v must be m/s. Also confirm that v is radial, not tangential stage motion.

Uncertainty propagation

The velocity method is sensitive to ω and r because they appear in the denominator as ω²r. A 2% RPM error becomes about a 4% ω² error, shifting s by roughly 4%. A 1 mm radius error at r = 70 mm is ~1.4% and directly changes s by the same proportion. When averaging frames, report the time window used.

Velocity workflow checkpoints

Use measured boundary speed v in m/s and boundary radius r in meters. At 45,000 RPM, ω ≈ 4,712 rad/s. With v = 2.0×10⁻⁶ m/s and r = 0.070 m, s ≈ 1.01×10⁻¹³ s, or about 1.01 S, matching the example table. At 55,000 RPM with v = 3.5×10⁻⁶ m/s and r = 0.065 m, s is about 1.72 S.

Buoyancy workflow checkpoints

In buoyancy form, s = m(1 − ρv̄)/f, where (1 − ρv̄) captures buoyant mass reduction. For ρ ≈ 1000 kg/m³ and v̄ ≈ 7.3×10⁻⁴ m³/kg, (1 − ρv̄) ≈ 0.27. With m = 1.2×10⁻¹⁹ kg and f = 1.1×10⁻¹¹ N·s/m, s ≈ 7.6×10⁻¹³ s (7.6 S).

Reporting and comparison

Report s in seconds and S, and record temperature, solvent composition, and the method because viscosity and density shift results. Use CSV exports to compare replicates; for example, three runs at 9.8, 10.1, and 10.0 S average to 9.97 S with 0.15 S spread. PDFs are best for sign-off and sharing. If you publish, state rotor type, speed, and r reference.

FAQs

What does a larger S value usually imply?

Under the same solvent and temperature, a larger S typically indicates faster sedimentation, often due to greater mass or a more compact shape. Compare only under matched experimental conditions.

Why can my result be negative?

Negative s commonly occurs when v is negative due to direction choice, or when (1 − ρv̄) becomes negative in the buoyancy method. Re-check signs, units, and whether the particle is less dense than solvent.

Should I enter radius in centimeters?

No. Enter r in meters to match SI units in the formula. If you have centimeters, divide by 100 before entering. Unit mistakes can change s by orders of magnitude.

Do I need RPM or angular velocity?

Either works. If you enter RPM, the calculator converts it to ω using ω = 2π·RPM/60. If you already know ω in rad/s, select the ω option and enter it directly.

What friction coefficient f should I use?

Use the translational friction coefficient appropriate to your particle and solvent, often derived from hydrodynamic models or experimental diffusion/viscosity data. Ensure units are N·s/m for consistency.

How should I report the final value?

Report s in S and seconds, plus temperature, solvent composition, rotor speed, and the radius reference. If averaging replicates, include mean and spread, and keep significant figures consistent with measurement precision.

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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.