Why terminal velocity helps
A small sphere falling through a viscous liquid reaches a steady speed when weight, buoyancy, and drag balance. That steady speed is terminal velocity. Under creeping flow, Stokes law links that speed to viscosity. This calculator turns measured terminal velocity into dynamic and kinematic viscosity. Kinematic viscosity is useful because it divides dynamic resistance by fluid density. It describes how quickly momentum diffuses through a fluid.
What the result means
The main result is ν, shown in square meters per second and centistokes. A lower value means the fluid lets motion spread more easily. A higher value means the fluid resists shear more strongly for its density. The tool also reports dynamic viscosity, density contrast, and Reynolds number. Reynolds number is important. Stokes law is best when it is below one. Larger values mean inertia may affect drag, so the result should be treated as an estimate.
Good measurement practice
Use a smooth, round sphere. Measure its diameter carefully, because radius is squared in the formula. Small size errors can strongly change the final value. Record terminal velocity only after the sphere is moving steadily. Use marks that are far from the release point and container bottom. Keep the fluid temperature stable. Viscosity can change quickly with temperature. Enter density values in consistent units, or use the unit selectors. For narrow tubes, enter a correction factor if you have one from your method.
When to use this calculator
This page is designed for teaching labs, quick checks, and early engineering estimates. It is suitable for dilute, Newtonian liquids with small spheres and slow motion. It is not ideal for turbulent flow, irregular particles, strong wall effects, or non Newtonian fluids. Use the exported report to attach assumptions, inputs, and results to lab notes. Always compare the Reynolds check with your course or project limits before accepting the viscosity value.
Interpreting uncertainty
The uncertainty estimate is a guide. It uses percentage errors entered for velocity, radius, density contrast, and fluid density. Because radius is squared, radius uncertainty counts twice. This helps show which measurement deserves more care. It does not replace a full experimental error analysis. Use repeated trials when high accuracy is required, and report averages.