OpenStax College Physics 2e — Mechanics & Fluids (Fall 2025, Prof. Raghu)
All 19 lectures | Kinematics · Dynamics · Energy · Momentum · Rotation · Gravity · Fluids
Physics is the science of how things move and why. PHYS 21 covers two big domains: mechanics (point particles and extended solids that translate, rotate, and collide) and fluids (liquids and gases that flow, push, and float things). Both are governed by a small handful of conservation laws — momentum, energy, angular momentum — applied with care to model the real world.
Every physical quantity has a numerical value and a unit. Skipping units is the #1 source of wrong answers in physics.
| Quantity | Unit | Symbol |
|---|---|---|
| Length | meter | m |
| Mass | kilogram | kg |
| Time | second | s |
| Electric current | ampere | A |
| Temperature | kelvin | K |
| Amount of substance | mole | mol |
| Luminous intensity | candela | cd |
In PHYS 21 we use kg, m, s. Every other mechanical quantity is built from these (force = kg·m/s², energy = kg·m²/s², pressure = kg/(m·s²), etc.).
| Prefix | Symbol | Factor |
|---|---|---|
| giga | G | 10⁹ |
| mega | M | 10⁶ |
| kilo | k | 10³ |
| centi | c | 10⁻² |
| milli | m | 10⁻³ |
| micro | μ | 10⁻⁶ |
| nano | n | 10⁻⁹ |
Every equation in physics must be dimensionally consistent: every term separated by + or − or = must have the same units. This is your free error checker.
Suppose you wrote v² = v0² + 2a·t. Check: left side L²/T². Right side: L²/T² + (L/T²)(T) = L²/T² + L/T. Inconsistent — the second term is wrong (it should be 2a·Δx with units L²/T²).
Position x is a coordinate on a number line; choose an origin and a positive direction first. Then:
Displacement is a signed quantity (a vector in 1-D). It is not the same as distance traveled — a runner who returns to the start has displacement 0 but distance > 0.
Sign matters: positive a means the velocity is increasing in the +x direction (could be speeding up if v > 0 or slowing down if v < 0). Decelerating just means a and v point in opposite directions.
If a is constant, integrating once gives v(t) and twice gives x(t). Memorize all four:
Near Earth's surface (and ignoring air resistance), every object falls with g = 9.80 m/s² directed downward, regardless of mass. Substitute a = ±g into the Big Four with a sign convention you choose at the start.
A ball is thrown straight up from y = 0 with v0 = +20 m/s. Take +y up, so a = −g = −9.8 m/s². Find the maximum height.
At the top, v = 0. Use v² = v0² + 2a·Δy:
Time to reach the top: t = (0 − 20)/(−9.8) ≈ 2.04 s. By symmetry, the round trip takes ~4.08 s.
A scalar has only magnitude (mass, time, temperature, energy). A vector has both magnitude and direction (displacement, velocity, force).
We write vectors with arrows: v⃗, or in bold, v. Magnitude is |v⃗| or just v (no arrow). In 2-D, a vector decomposes into components along chosen axes:
Draw the first vector. Place the tail of the second at the tip of the first. The resultant R⃗ = A⃗ + B⃗ goes from the tail of the first to the tip of the last. (Order doesn't matter — vector addition is commutative.)
Then |R| = √(Rx² + Ry²) and θ = tan⁻¹(Ry/Rx) (watching the quadrant).
Subtraction: A⃗ − B⃗ = A⃗ + (−B⃗), where −B⃗ is B⃗ flipped. Scalar multiplication: cA⃗ stretches or shrinks A⃗ by |c|, and reverses it if c < 0. Components scale: (cA)x = cAx.
The scalar product picks out the component of one vector along another:
You'll see this in Lecture 9 as work: W = F⃗·d⃗ = Fd cos φ.
In 2-D motion under constant acceleration (e.g., gravity), the x- and y-axes evolve independently. Apply the Big Four kinematic equations to each axis separately and link them only through time t.
Initial speed v0 at angle θ above horizontal: v0x = v0 cos θ, v0y = v0 sin θ. Take +y up, +x in launch direction; ax = 0, ay = −g.
A diver leaves a 30-m cliff horizontally at v0 = 6 m/s. How far from the base does she hit the water?
Vertical: y = h − ½ g t² = 0 ⇒ t = √(2h/g) = √(60/9.8) ≈ 2.47 s. Horizontal: x = v0 t = 6(2.47) ≈ 14.8 m.
Notice you never need to mix x and y in the algebra — they're independent until you read off "at the same time."
The single most useful tool in mechanics. Steps:
| Force | Direction | Magnitude |
|---|---|---|
| Weight (gravity) | Toward Earth's center | W = mg, g ≈ 9.80 m/s² |
| Normal N | ⊥ to contact surface | Whatever the surface needs (constraint) |
| Tension T | Along the rope | Whatever the rope needs (massless, inextensible) |
| Spring | Toward equilibrium | F = −kx (Hooke's law) |
| Friction f | Opposes relative slip / impending slip | Static: f ≤ μsN. Kinetic: fk = μkN |
For a block of mass m on a frictionless incline of angle θ:
With friction (block sliding down): a = g(sin θ − μk cos θ). The block won't slide at all if μs ≥ tan θ.
A massless, frictionless pulley simply redirects the tension — magnitude is the same on both sides. A massless, inextensible rope means both ends share the same |a|.
Two masses m1 and m2 (m2 > m1) over a pulley. Let a be the acceleration of m2 downward. Newton on each mass:
Add: a = (m2 − m1)g/(m1 + m2). Then T = 2 m1 m2 g / (m1 + m2). Limits: m1 = m2 → a = 0 ✓. m2 ≫ m1 → a → g ✓.
Measure angles in radians: a full circle is 2π rad, and arc length s = r θ only in radians. Angular velocity ω is rate of change of angle:
An object moving in a circle at constant speed is still accelerating — its velocity vector keeps turning. The acceleration points toward the center (centripetal):
A car of mass m rounds a curve of radius r at speed v on a road banked at angle θ. Without friction: tan θ = v²/(rg). For larger v, friction must supply the extra inward force.
Every pair of point masses attracts along the line joining them with a force:
For a circular orbit at radius r around a body of mass M, gravity supplies the centripetal force:
Altitude 400 km above Earth, so r = 6.37 × 10⁶ + 4 × 10⁵ = 6.77 × 10⁶ m. v ≈ √[(6.67×10⁻¹¹)(5.97×10²⁴)/(6.77×10⁶)] ≈ 7.67 km/s; T ≈ 5550 s ≈ 92 minutes. Matches reality.
If speed is changing in addition to direction, total acceleration has two components:
|a| = √(ac² + at²), and a points inward and forward/backward by the angle tan⁻¹(at/ac).
The total work done by every force adds up to the change in kinetic energy. This is one of the most important and reliable problem-solving tools in mechanics.
For a position-dependent force, work is the area under the F-vs-x curve:
For a spring (Hooke's law F = −kx) stretched from 0 to x:
A 1-horsepower motor delivers 746 W. A bright LED bulb consumes ~10 W; a treadmill at jogging speed dissipates ~600 W; a Tesla Model S can pull ~500 kW for a few seconds.
A force is conservative if the work it does between two points is path-independent (equivalently: the work around any closed loop is zero). Gravity and springs are conservative; friction and air drag are not.
The zero of potential energy is your choice; only differences matter.
If only conservative forces act:
If non-conservative forces (friction, drag, applied push) also act:
A ball starts at rest at height h on a frictionless track that curves into a vertical loop of radius R. Minimum h for the ball to complete the loop: at the top, gravity supplies the entire centripetal force, so vtop² = gR. Energy conservation between start and top:
For constant mass this reduces to F⃗ = ma⃗. But the momentum form survives even when mass changes (rockets, raindrops collecting water).
If the net external force on a system is zero, the total momentum of the system is conserved:
Momentum conservation holds even when energy isn't conserved. Collisions, explosions, and even sticky bumps all conserve momentum as long as you can ignore external forces during the brief impact.
| Type | Momentum? | Kinetic Energy? | Example |
|---|---|---|---|
| Elastic | Conserved | Conserved | Billiard balls (approx.); atomic-scale |
| Inelastic | Conserved | Decreases | Most everyday bumps |
| Perfectly inelastic | Conserved | Maximum loss; objects stick together | Clay hits wall; rail-car coupling |
m1 hits m2 (initially at rest). Conservation of p and KE gives:
Maximum KE is lost (consistent with momentum conservation). The lost KE goes to deformation, heat, and sound.
In 2-D, momentum is conserved component-wise (two scalar equations). For a system of particles, define:
The CM moves as if all the mass were concentrated there and all external forces acted on it: Mtot a⃗CM = F⃗ext, net. Internal forces shift particles relative to the CM but never move the CM itself.
For a rigid body to be in translational equilibrium, the net external force must vanish: ΣF⃗ = 0. This gives two scalar equations in 2-D.
A force can cause an object to rotate. The rotational analog of force is torque τ:
A child of mass m1 = 25 kg sits 1.6 m left of the pivot. A larger child of mass m2 sits 1.0 m right. Find m2 for balance.
Στ = 0 about pivot: m1 g (1.6) − m2 g (1.0) = 0 ⇒ m2 = 1.6 × 25 = 40 kg.
Uniform ladder of length L, mass M, leaning at angle θ against a frictionless vertical wall. The ground has coefficient of static friction μs. Find the minimum θ before slipping.
Forces: weight Mg (down at center), normal N from ground (up), normal Nw from wall (horizontal toward ladder), friction fs at base (horizontal toward wall).
ΣFx: fs = Nw. ΣFy: N = Mg. Στ about base: Nw L sin θ − Mg (L/2) cos θ = 0 ⇒ Nw = (Mg/2) cot θ. At slip: fs = μs N = μs Mg, so:
An object is stable if its center of gravity, when slightly displaced, returns toward the original position (lower CM). A simple machine (lever, pulley, wheel-and-axle) trades distance for force; ideal mechanical advantage = (effort arm)/(load arm).
| Linear | Angular | Connection (point at radius r) |
|---|---|---|
| x (m) | θ (rad) | s = r θ |
| v (m/s) | ω (rad/s) | v = r ω |
| a (m/s²) | α (rad/s²) | at = r α; ac = r ω² |
| F (N) | τ (N·m) | τ = r F⊥ |
| m (kg) | I (kg·m²) | I = Σ mi ri² |
| p = m v | L = I ω | L = m v r (point particle) |
Identical structure to the linear Big Four — same problem-solving recipe, different letters.
The moment of inertia I measures how the mass is distributed about the rotation axis. More mass farther from the axis → larger I → harder to spin up. Same mass closer in → smaller I → easier to spin.
| Object (mass M) | Axis | I |
|---|---|---|
| Point particle at distance r | Through pivot, ⊥ to r | M r² |
| Hoop / thin ring (radius R) | Through center, ⊥ to plane | M R² |
| Solid disk / cylinder (R) | Through center, along axis | ½ M R² |
| Solid sphere (R) | Through center | (2/5) M R² |
| Hollow sphere (R) | Through center | (2/3) M R² |
| Rod (length L) | Through center, ⊥ rod | (1/12) M L² |
| Rod (length L) | Through end, ⊥ rod | (1/3) M L² |
Same form as ½ m v², with mass replaced by moment of inertia and speed replaced by angular speed.
An object rolling without slipping has total kinetic energy equal to translational + rotational:
This explains the racing-down-a-ramp puzzle of Lec 13: more I means more rotational KE for the same total energy, so less goes into translation, so smaller vCM.
A solid sphere (I = (2/5)MR²) rolls without slipping down a ramp of height h. Find vCM at the bottom.
Mgh = ½ M v² + ½ (2/5)MR² (v/R)² = ½ M v²(1 + 2/5) = (7/10) M v². So v = √(10gh/7) ≈ 0.845 √(2gh) — slower than a frictionless slide (v = √(2gh)).
An ice skater spins with arms extended at ω0, then pulls them in. With no external torque, L is conserved: I0 ω0 = If ωf. Since I drops, ω rises.
Where does the KE come from? KErot = ½ I ω² = ½ L²/I. Smaller I → larger KE. The skater does work pulling the arms in against the centrifugal pseudo-force; that work shows up as added rotational KE.
When a free particle strikes an extended object, both linear and angular momentum are conserved (assuming no external impulsive forces).
A bullet of mass m at velocity v hits a vertical door (mass M, width L, hinged at one side) at distance d from the hinge and embeds. Find the angular velocity of door + bullet just after impact.
Conservation of L about the hinge: m v d = (Idoor + m d²) ω. With Idoor = (1/3) M L²:
Linear momentum is not conserved because the hinge exerts an impulsive horizontal force. Angular momentum about the hinge is conserved because the hinge force has zero torque about itself.
A fluid is a substance that flows — it has no fixed shape and conforms to its container. Liquids (nearly incompressible) and gases (highly compressible) are both fluids.
Water: ρ ≈ 1000 kg/m³ at 4 °C. Air at sea level: ρ ≈ 1.29 kg/m³. Mercury: ρ ≈ 13,600 kg/m³. Specific gravity = ρ/ρwater (a dimensionless ratio).
Where h is depth below a free surface at pressure P0. Two consequences:
Volume conservation requires F1 · d1 = F2 · d2: you trade distance for force, with no free lunch in energy.
Most pressure gauges (tire, blood pressure cuff) read pressure above atmospheric:
A "32 psi" tire has absolute pressure ~46.7 psi. A flat tire has gauge 0, absolute 1 atm.
A U-tube manometer measures gauge pressure as a height difference: ΔP = ρ g Δh. A mercury barometer reads atmospheric pressure: 1 atm pushes up a column of Hg by 760 mm.
Mathematically, FB arises because the pressure on the bottom of the submerged volume is greater than the pressure on the top — that pressure difference times the cross-section area equals ρ V g.
ρice = 920 kg/m³, ρseawater = 1025 kg/m³. Submerged fraction = 920/1025 ≈ 0.898 → about 10% above water. (Hence "tip of the iceberg.")
For an incompressible fluid in steady flow, the same mass passes every cross-section per unit time. With Q = volume flow rate (m³/s):
Pinch a hose: smaller A → larger v. The water comes out faster.
Conservation of energy per unit volume along a streamline of an incompressible, non-viscous, steady flow:
Three energy densities, each with units of pressure (Pa = J/m³):
A large tank has a small hole at depth h below the water surface. Apply Bernoulli between the surface (large area, v ≈ 0, P = Patm) and the exit (P = Patm):
Same as a free-fall from height h. Deep water exits faster.
Horizontal pipe narrows from A1 to A2. Continuity: v2 = (A1/A2) v1. Bernoulli (h1 = h2):
Pressure drops at the constriction. Carburetors and atomizers exploit this to draw fuel into the airflow.
A cambered (curved) airfoil shape forces air over the top to travel a longer path, increasing v above the wing. Bernoulli says P drops there, and the resulting pressure imbalance lifts the wing. (Reality is more subtle than the "equal-time" simplification, but Bernoulli + Newton's 3rd law is the right starting picture.)
Real fluids resist relative motion of adjacent layers — that resistance is viscosity η, measured in Pa·s. Honey is more viscous than water; air is even less viscous.
Two parallel plates separated by fluid: the force per unit area to slide one plate relative to the other is proportional to the velocity gradient. Honey is η ≈ 10 Pa·s; water is ~0.001 Pa·s; air is ~10⁻⁵ Pa·s.
At low speeds, fluid layers slide smoothly past each other (laminar); at high speeds, swirling chaos sets in (turbulent). The dimensionless Reynolds number tells you which regime:
Volume flow rate through a pipe of radius r and length L driven by pressure difference ΔP. The dramatic r⁴ dependence means a small change in pipe radius has a huge effect on flow.
Most "hard" problems on the final yield to one of these. Always ask: what is conserved here, and between which two instants?
A bullet (m, v) embeds in a hanging block (M, at rest). The combined mass swings up to height h. Find v.
During impact (very fast): momentum conservation, mv = (m+M)V.
After impact (slow swing): energy conservation, ½(m+M)V² = (m+M)gh, so V = √(2gh).
Combine: v = (1 + M/m) √(2gh). You can't use energy through the impact (some KE went to heat) and you can't use momentum through the swing (gravity is external) — pick the right tool for each phase.
You sit on a frictionless rotating stool holding a spinning bicycle wheel horizontally with Lwheel = +L0. You flip the wheel over so its L is now −L0. Total system L is conserved → you and the stool spin in the +direction with L = 2L0.
Hot air at temperature T inside the balloon has lower density ρ' = ρair(T0/T). The buoyant force (ρair V g) exceeds the gas weight (ρ' V g), and the balloon rises until ρ' equals the local atmospheric density.
A solid sphere released from rest down a frictionless ramp of height h reaches v = √(2gh). Released as rolling-without-slipping down the same ramp, it reaches v = √(10gh/7) ≈ 0.85√(2gh) — slower because some PE went into rotational KE.
| Cluster | Lectures | OpenStax |
|---|---|---|
| Units, dimensions, kinematics | 1, 2, 4 | Ch. 1, 2, 3 |
| Vectors | 3 | §3.2, 3.3 |
| Newton's laws, friction, inclines | 5, 6 | Ch. 4, 5 |
| Circular motion & gravity | 7, 8 | Ch. 6 |
| Work, energy, conservation | 9, 10 | Ch. 7 |
| Momentum & collisions | 10, 11 | Ch. 8 |
| Torque & static equilibrium | 12 | Ch. 9 |
| Rotational motion & angular momentum | 13, 14, 15 | Ch. 10 |
| Fluid statics | 15, 16 | Ch. 11 |
| Fluid dynamics & viscosity | 17, 18 | Ch. 12 |
| Constant | Symbol | Value |
|---|---|---|
| Surface gravity (Earth) | g | 9.80 m/s² (sometimes rounded to 9.81 or 10) |
| Universal gravitation | G | 6.674 × 10⁻¹¹ N·m²/kg² |
| Earth mass | M⊕ | 5.97 × 10²⁴ kg |
| Earth radius | R⊕ | 6.37 × 10⁶ m |
| Sun mass | M☉ | 1.99 × 10³⁰ kg |
| Sun–Earth distance (1 AU) | — | 1.50 × 10¹¹ m |
| Speed of sound (air, 20 °C) | vs | 343 m/s |
| Density of water | ρwater | 1000 kg/m³ |
| Density of air (sea level) | ρair | 1.29 kg/m³ |
| Density of mercury | ρHg | 13,600 kg/m³ |
| Atmospheric pressure | Patm | 1.013 × 10⁵ Pa = 1 atm = 760 mmHg |
| Viscosity of water (20 °C) | η | 1.00 × 10⁻³ Pa·s |
| Quantity | Conversion |
|---|---|
| Length | 1 mile = 1.609 km; 1 ft = 0.3048 m; 1 inch = 2.54 cm |
| Mass | 1 lb-mass ≈ 0.4536 kg; 1 ton (metric) = 1000 kg |
| Speed | 1 mph = 0.447 m/s; 1 km/h = 0.278 m/s |
| Force | 1 lb-force = 4.448 N |
| Energy | 1 cal = 4.186 J; 1 Cal (food) = 4186 J; 1 kWh = 3.6 × 10⁶ J |
| Pressure | 1 atm = 1.013 × 10⁵ Pa = 14.7 psi = 760 torr |
| Volume | 1 L = 10⁻³ m³; 1 gallon (US) = 3.785 L |
| Angle | 1 rev = 2π rad = 360°; 1 rad = 57.30° |
| Power | 1 hp = 746 W |