The coefficient of viscosity dimensional formula is [M¹ L⁻¹ T⁻¹], or [ML⁻¹T⁻¹] in short form. It tells you that the stickiness of a fluid scales with mass to the first power and falls off with one power of length and one power of time.
The coefficient η (eta) is defined by Newton's law of viscosity: the drag force between fluid layers is proportional to the layer area and to how fast the speed changes from one layer to the next (the velocity gradient). Honey has a large η, water a small one, but both carry the same bracket. Below are the derivation, the unit Pa s and the poise, a Stokes' law check and a list of slips. For numbers, see the coefficient of viscosity formula page.
Quick facts
Dimensional formula
[M¹ L⁻¹ T⁻¹], short form [ML⁻¹T⁻¹]Defining formula
SI unit
Pa s = N s m⁻² = kg m⁻¹ s⁻¹CGS unit
poise; 1 Pa s = 10 poiseCommon symbol
η (eta)Chapter
Mechanical properties of fluids, Class 11
Deriving the coefficient of viscosity dimensional formula
Start from the law that defines η, then isolate it.
- Viscous force: , so .
- Force: . Area: .
- Velocity gradient is speed per distance: .
- Area times gradient is . Flip it and multiply by the force: .
The velocity gradient step is where most errors start. It is not a velocity; it has units of s⁻¹, the same as a frequency. A minus sign sometimes appears in the force law to show the drag opposes motion, but a sign has no effect on dimensions. The velocity gradient page explains that ratio further.
Pa s, the poise and how they relate
Turn [ML⁻¹T⁻¹] into base units: kg m⁻¹ s⁻¹. Group them another way and you get N s m⁻², which is a pascal second (Pa s). Both are the SI unit of the coefficient of viscosity. Pa s is the form most answer keys print.
Convert 1 Pa s into the CGS unit, the poise
The poise is g cm⁻¹ s⁻¹. Raise each conversion factor to its own power from the bracket.
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So 1 Pa s = 10 poise, and 1 centipoise = 10⁻³ Pa s. Water near room temperature is close to 1 centipoise.
Matching brackets and a look alike
| Quantity | How it is built | Why it matches |
|---|---|---|
| Dynamic viscosity of any fluid | shear stress ÷ velocity gradient | The definition itself |
| Pressure × time | [ML⁻¹T⁻²] × [T] | |
| Stress × time | Stress has the pressure bracket |
The pressure times time row gives a neat way to remember the result: viscosity is shear stress divided by a rate, s⁻¹, so it is a stress multiplied by a time. Compare that with the dimensional formula of pressure.
Kinematic viscosity is a different quantity. It is η divided by density, ν = η/ρ, with dimensions [ML⁻¹T⁻¹] ÷ [ML⁻³] = [L²T⁻¹] and unit m²/s. Do not mix the two in an answer.
Two fluid laws put to the test
Check Stokes' law, F = 6πηrv, for a sphere falling through a fluid
Right side: .
Collect powers: M¹, L⁻¹⁺¹⁺¹ = L¹, T⁻¹⁻¹ = T⁻². Result .
That is a force, so the law is dimensionally consistent. The 6π is a number and cannot be tested.
Check the flow rate relation Q = πPr⁴/(8ηl)
Top: . Bottom: .
Ratio: , a volume per second. Here P is the pressure difference along the tube, and the result is the expected flow rate.
Errors that cost marks
- Writing [MLT⁻¹]. That is momentum. Viscosity has length to the power −1.
- Treating dv/dx as a velocity. It is [T⁻¹]; skipping the division by distance gives the wrong answer.
- Mixing up dynamic and kinematic viscosity. η is [ML⁻¹T⁻¹]; ν is [L²T⁻¹].
- Converting Pa s to poise by 100. The factor is 10, from 10³ g divided by 10² cm.
The viscosity bracket is collected with the other fluid quantities on the dimensional formulas page.
Frequently asked questions
In SI, what unit does η take?
Pa s. Written with base units that is kg m⁻¹ s⁻¹, and it can also appear as N s m⁻².
Is the dimensional formula of viscosity different from that of the coefficient?
No. When a question says viscosity it normally means the coefficient η, so the answer is [M¹ L⁻¹ T⁻¹]. Only kinematic viscosity differs, at [L²T⁻¹].
How many poise make one pascal second?
Ten. One poise is 0.1 Pa s, and one centipoise is 0.001 Pa s.
Is the coefficient of viscosity a scalar?
Yes. For ordinary fluids η is a single number that depends on the fluid and its temperature, with no direction.
Why is the velocity gradient [T⁻¹]?
It is a change in speed, [LT⁻¹], divided by the distance between layers, [L]. The lengths cancel and only one over time remains.