How to Make a Physics Equation Dimensionless
At a glance
- 1. List the dimensions
Write the dimensions of every variable, parameter, and constant in the equation.
- 2. Choose reference scales
Select characteristic scales for length, time, mass, temperature, or another relevant quantity.
- 3. Define dimensionless variables
Divide each dimensional variable by its corresponding reference scale.
- 4. Substitute and simplify
Replace the original variables and divide through by a common dimensional factor.
- 5. Interpret the groups
Identify the remaining dimensionless combinations as ratios controlling the system.
A dimensional equation contains quantities such as metres, seconds, kilograms, or pascals. A dimensionless equation is written in terms of variables and parameters that have no units. This process is called nondimensionalization or dimensionless scaling.
The essential idea is to divide each variable by a suitable characteristic value. For example, if is a position and is a characteristic length, define
Both and have dimensions of length, so is dimensionless. You do the same for time, velocity, pressure, temperature, and other quantities.
Dimensional homogeneity comes first
Before nondimensionalizing, check that the original equation is dimensionally consistent. Terms that are added or subtracted must have the same dimensions. For example,
would not generally be valid because is a force, while and have different dimensions unless and are defined appropriately.
For a damped, driven spring–mass oscillator, a dimensionally consistent equation is
where:
- is mass,
- is the damping coefficient,
- is the spring constant,
- is the driving-force amplitude, and
- is the driving angular frequency.
Dimensional consistency does not by itself make the equation dimensionless. It only ensures that the equation is physically meaningful.
Choose characteristic scales
Introduce a characteristic displacement and a characteristic time . Define
Here, and are dimensionless. Equivalently,
Using the chain rule,
and
The scales and are not unique. A good choice makes important coefficients equal to one and leaves only the physically meaningful ratios.
Worked example: a driven oscillator
Start with
Choose the natural oscillator scales
The time scale is the inverse natural frequency, and is the static displacement that a force would produce.
Substitute and :
Since and , divide the entire equation by . The result is
Define the damping ratio and dimensionless driving frequency by
Then the dimensionless equation becomes
Every quantity in this final equation is dimensionless: , , , and . The original five parameters have been reduced to two controlling ratios, and .
Numerical substitution
Suppose
m=2\ \mathrm{kg},\qquad c=2\ \mathrm{N\,s/m},\qquad k=8\ \mathrm{N/m},$$ with $F_0=4\ \mathrm{N}$ and $\omega=3\ \mathrm{s}^{-1}$. Thenx_0=\frac{F_0}{k}=0.5\ \mathrm{m}, \qquad t_0=\sqrt{\frac{m}{k}}=0.5\ \mathrm{s}.
\zeta=\frac{2}{2\sqrt{2\cdot8}}=0.25, \qquad \Omega=3\sqrt{\frac{2}{8}}=1.5.
\frac{d^2X}{d\tau^2}+0.5\frac{dX}{d\tau}+X=\cos(1.5\tau).
The units have disappeared, but the physical content has not. The numbers $0.25$ and $1.5$ describe damping and forcing relative to the oscillator's natural scales. ## General recipe for any equation For a more complicated model, use this sequence: 1. List every dimensional variable and parameter. 2. Choose characteristic scales such as length $L$, time $T$, velocity $U$, pressure $P$, or temperature difference $\Delta T$. 3. Define dimensionless variables, for example $X=x/L$, $\tau=t/T$, and $\Theta=(T-T_\mathrm{ref})/\Delta T$. 4. Rewrite derivatives using the new variables. 5. Substitute into the original equation. 6. Divide by one common dimensional coefficient. 7. Collect the remaining dimensionless parameter combinations. For example, in fluid mechanics, choosing a length scale $L$ and speed scale $U$ often produces the Reynolds number\operatorname{Re}=\frac{\rho UL}{\mu},
which compares inertial effects with viscous effects. Such groups are often more informative than the original dimensional constants. ## Common mistakes ### Dividing variables by numbers instead of scales Writing $X=x/2$ does not make $X$ dimensionless unless the $2$ carries the same units as $x$. Use a dimensional reference quantity, such as $x_0=2\ \mathrm{m}$. ### Forgetting derivative factors If $t=t_0\tau$, then $d/dt=(1/t_0)d/d\tau$. A second derivative introduces $1/t_0^2$, not merely $1/t_0$. ### Mixing dimensional and dimensionless variables After defining $X=x/x_0$, use $X$ consistently. Writing $\cos(\omega\tau)$ is usually wrong if $\tau$ is dimensionless, because $\omega$ still has units. The correct argument is typically $\omega t_0\tau$. ### Assuming there is only one correct scaling Different choices of reference scales produce different-looking dimensionless equations. They are equivalent when the variables are related correctly. Choose scales that reflect the regime or simplify the terms you want to study. ### Confusing “dimensionless” with “equal to one” A dimensionless quantity can be $0.2$, $15$, or $\pi$. Dimensionless means it has no units, not that its numerical value is one.References
- Dimensional Analysis and Scale-Up in Chemical Engineering, H. L. Langhaar
- Scaling, Self-similarity, and Intermediate Asymptotics, G. I. Barenblatt
- An Introduction to Fluid Dynamics, G. K. Batchelor
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