Engineering Mechanics
10 Physics Formulas Every Engineer Should Memorize (And Why)
By Saurabh
Ten kinematics and dynamics formulas cover most of the physics an engineer actually reaches for day to day - motion, forces, energy, and the handful of special cases (falling objects, projectiles, springs) that show up constantly in coursework and real design work alike. Every one links to a calculator that runs the numbers with proper units, so you can check your own work against a real example.
Net Force: Fnet = ΣF
A tug-of-war rope that isn't moving doesn't mean nobody's pulling - it means the two teams' forces are exactly equal and opposite, so the net force is zero even though each side may be straining at hundreds of pounds.
Net force, not the size of any single individual force, is what actually determines whether - and how - something accelerates. An object can have several large forces acting on it simultaneously and still not move at all, as long as those forces sum to zero.
Try the Net Force Calculator.
Gravitational Force: F = G m1 m2 / r²
Gravity is the weakest of the four fundamental forces by an enormous margin - a small refrigerator magnet can lift a paperclip against the gravitational pull of the entire Earth, which says more about how astronomically small the gravitational constant G is than about anything unusual happening at the fridge.
Gravity only becomes the dominant force at planetary and stellar mass scales, where the sheer size of m1 and m2 finally compensates for how tiny G is - nothing else is large enough at that scale to compete with it, even though gravity loses badly to electromagnetism at everyday sizes.
Try the Gravitational Force Calculator.
Acceleration: a = (v − u) / t
In everyday language, "acceleration" means speeding up and "braking" means something else entirely - but in physics, both are exactly the same quantity with opposite signs. A car braking hard has a large negative acceleration in its direction of travel, not an absence of acceleration.
Comparing that magnitude in g's (multiples of standard gravity) is a common way engineers communicate how aggressive a deceleration actually feels - a hard stop in a car might pull under 1g, while a roller coaster drop or an ejection seat can briefly exceed 4-5g, the same formula describing wildly different real experiences.
Try the Acceleration Calculator.
Velocity: v = Δx / t
A runner who completes a full lap and returns to the exact starting point has an average velocity of exactly zero for that lap, no matter how fast they actually ran the whole way around.
Displacement, not distance traveled, is what sits in the numerator of this formula, which is why average velocity and average speed can tell completely different stories about the identical motion - speed only cares how much ground was covered, velocity only cares how far you ended up from where you started.
Try the Velocity Calculator.
Free Fall: h = ½ g t²
Free fall is one of the few formulas in physics where mass simply doesn't appear at all - a heavy object and a light one, dropped from the same height with air resistance genuinely negligible, hit the ground at exactly the same time.
That's the same demonstration Apollo 15 famously repeated on the airless Moon with a hammer and a feather, dropping both simultaneously to show live on camera that they land together once air resistance is completely out of the picture, not just reduced.
Try the Free Fall Calculator.
Projectile Motion: R = v₀² sin(2θ) / g
Range depends on sin(2θ), which peaks at exactly 45° - the reason a projectile launched at 45° travels farther than the identical launch speed sent out at any steeper or shallower angle.
That same sine relationship also produces a less obvious result: a 30° launch and a 60° launch land at the exact same range, since sin(60°) and sin(120°) are equal - two very different-looking shots, one flatter and one higher, covering identical ground.
Try the Projectile Motion Calculator.
Terminal Velocity: v = √(2mg / (Cd ρ A))
A skydiver in a spread-eagle belly-down position and the same skydiver in a head-down dive have identical mass, yet reach very different terminal velocities - spreading out increases both the cross-sectional area and the drag coefficient, slowing the fall.
That's exactly how skydivers actively control their fall rate without changing anything about their own weight: orientation alone shifts A and Cd enough to meaningfully change terminal velocity, which is also the underlying physics a parachute exploits deliberately and dramatically.
Try the Terminal Velocity Calculator.
Gravitational Potential Energy: PE = mgh
Potential energy is always measured relative to some chosen reference height - h = 0 could mean the floor, the ground outside, or sea level, and each choice gives a different absolute PE value for the exact same object sitting in the exact same place.
What's physically meaningful, and what actually determines energy available to convert into motion, is only the change in potential energy between two points, never whatever absolute number a particular reference height happens to produce - the reference point is a bookkeeping choice, not a physical fact about the object.
Try the Potential Energy Calculator.
Impact Force: Favg = ½mv² / d
A phone dropped from the same height onto a hard tile floor and onto a thick carpet experiences a dramatically different impact force despite hitting the ground at the identical speed - the carpet increases the stopping distance just enough to meaningfully reduce the average force.
That's the entire physical reason a cushioned phone case protects a phone that would otherwise crack on direct impact: it doesn't change the impact speed at all, it just extends the stopping distance over which the same kinetic energy has to be absorbed.
Try the Impact Force Calculator.
Spring Force: F = kx
Hooke's law is only exactly true within a spring's elastic limit - push or pull a real spring too far and it stops returning force proportionally, eventually deforming permanently once stretched or compressed past that point.
That's why spring specifications always include a maximum safe travel alongside the spring constant itself: k alone describes the spring's behavior only up to that limit, and using it beyond that range predicts a force the spring can no longer actually produce.
Try the Spring Force Calculator.
Quick Reference - All 10 Formulas
| Formula | Expression | Primary Use |
|---|---|---|
| Net Force | Fnet = ΣF | Combining multiple forces on one object |
| Gravitational Force | F = Gm1m2/r² | Attraction between two masses |
| Acceleration | a = (v−u)/t | Rate of change of velocity |
| Velocity | v = Δx/t | Displacement over time |
| Free Fall | h = ½gt² | Motion under gravity alone |
| Projectile Motion | R = v₀²sin(2θ)/g | Range of an angled launch |
| Terminal Velocity | v = √(2mg/(CdρA)) | Constant fall speed once drag balances weight |
| Gravitational Potential Energy | PE = mgh | Stored energy from height |
| Impact Force | Favg = ½mv²/d | Average force during a collision or stop |
| Spring Force | F = kx | Hooke's Law for an ideal spring |
Part of the Engineering Mechanics calculators collection.
Frequently Asked Questions
Why isn't Newton's second law (F = ma) or kinetic energy on this list?
Both are covered in this site's companion piece, "15 Essential Engineering Formulas Every Student Should Know" - this list deliberately covers ten different, equally fundamental Engineering Mechanics relationships instead of repeating those two.
What's the actual difference between free fall and terminal velocity?
Free fall assumes air resistance is negligible, so an object keeps accelerating at g the entire time it falls. Terminal velocity is what happens once air resistance is not negligible - drag grows with the square of speed until it exactly balances gravity, at which point acceleration stops and speed becomes constant. A real falling object transitions toward the second regime as it speeds up; which formula applies depends on how significant drag actually is for that object and speed.
Does the projectile motion formula account for air resistance?
No - the standard projectile-motion formulas assume an idealized trajectory with no drag, a very good approximation for a dense, compact object moving at moderate speed over a short range, but a poor one for a light, high-drag object or very high velocities, where air resistance meaningfully curves the actual path away from the ideal parabola.
Is gravitational potential energy (mgh) the same formula as gravitational force between two masses?
No - they're related but different. Gravitational force (F = Gm1m2/r²) is Newton's universal law, valid at any distance using the actual gravitational constant G. Potential energy (PE = mgh) is a simplified, local approximation that only holds near a planet's surface, where g is treated as a constant rather than the distance-dependent value it truly is at planetary scales.
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