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◆ Classical Mechanics Reference ◆
◆ ℒ ◆

Newton's Principia
50 Concepts of Classical Mechanics

A complete scientific reference — from the three Laws of Motion to orbital mechanics, energy, momentum, rotation, and the mathematical framework that revealed the architecture of the physical universe
Isaac Newton  ◆  Philosophiæ Naturalis Principia Mathematica, 1687  ◆  SI Units Throughout
F = ma   |   F = Gm₁m₂/r²   |   p = mv   |   Eₑ = ½mv²   |   τ = Iα
◆ Sir Isaac Newton — The Architect of Classical Physics
Isaac Newton (1643–1727) was an English mathematician, physicist, and astronomer whose Philosophiæ Naturalis Principia Mathematica (1687) stands as the most influential scientific work ever published. In three books Newton laid out the laws of motion, universal gravitation, and the mathematical methods — including his independent invention of calculus — sufficient to explain planetary orbits, tidal forces, the shape of the Earth, and the motion of comets. His framework remained the unchallenged description of physical reality for over 200 years, until Einstein's relativity (1905–1915) revealed its limits at very high speeds and strong gravitational fields. At everyday scales and speeds, Newtonian mechanics remains exact to many decimal places and is the foundation of all engineering, ballistics, orbital mechanics, and classical thermodynamics.
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◆ Index of 50 Concepts
  1. Space, Time & Absolute Frame
  2. Mass
  3. Inertia & Newton's 1st Law
  4. Force & Newton's 2nd Law
  5. Newton's 3rd Law
  6. Weight vs. Mass
  7. Universal Gravitation
  8. Gravitational Field
  9. Free Fall & g
  10. Linear Momentum
  11. Impulse
  12. Conservation of Momentum
  13. Displacement, Velocity, Acceleration
  14. Kinematic Equations
  15. Projectile Motion
  16. Relative Motion
  17. Work
  18. Kinetic Energy
  19. Potential Energy
  20. Conservation of Energy
  21. Power
  22. Elastic & Inelastic Collisions
  23. Centre of Mass
  24. Friction
  25. Normal Force
  26. Tension
  27. Circular Motion
  28. Centripetal Force
  29. Angular Displacement & Velocity
  30. Angular Acceleration
  31. Torque
  32. Moment of Inertia
  33. Angular Momentum
  34. Rotational Kinetic Energy
  35. Rolling Motion
  36. Simple Harmonic Motion
  37. The Spring — Hooke's Law
  38. The Pendulum
  39. Resonance
  40. Kepler's Laws
  41. Orbital Mechanics
  42. Escape Velocity
  43. Tidal Forces
  44. Pressure & Archimedes
  45. Fluid Dynamics — Continuity
  46. Bernoulli's Principle
  47. Dimensional Analysis
  48. Newton's Method & Calculus
  49. Superposition of Forces
  50. Limits of Newtonian Physics
◆ Section I
Foundations — Space, Time, Mass & Force
The axiomatic bedrock of Newtonian mechanics: absolute space and time, the nature of mass, and the three laws that govern all motion.
01
Absolute Space, Absolute Time & the Inertial Frame
◆ Foundations · Metaphysics of Physics
Newton's Scholium (Principia, 1687) Absolute space remains always similar and immovable. Absolute time flows equably without relation to anything external.
Newton's mechanics rests on two foundational assumptions: absolute space — a fixed, motionless backdrop against which all motion is measured — and absolute time — a universal clock ticking at the same rate everywhere in the universe simultaneously. These were not proven experimentally; they were metaphysical axioms that made his mathematics tractable. An inertial reference frame is any frame of reference in which Newton's laws hold without modification — roughly, a non-accelerating, non-rotating frame. All inertial frames are equivalent for the purposes of mechanics (Galilean relativity). Newton believed such a frame could be anchored to absolute space; in practice, the distant stars serve as its proxy.
Historical note: Einstein's Special Relativity (1905) demolished the concepts of absolute space and absolute time, replacing them with a unified spacetime in which simultaneity is observer-dependent. At everyday speeds (v ≪ c), Newton's assumptions introduce negligible error.
Dynamics
02
Mass — The Measure of Inertia and Gravitational Charge
◆ Foundations · Matter
Definitions Inertial mass: m = F / a   |   Gravitational mass: m = Fg·r²/(G·M) Unit: kilogram [kg] — the only base SI unit still defined by a physical artefact until 2019
Mass is the most fundamental property of matter in Newtonian physics, playing two distinct roles. Inertial mass measures how strongly an object resists changes in its state of motion — the greater the mass, the greater the force required to produce the same acceleration. Gravitational mass measures how strongly an object participates in gravitational attraction, acting both as a source of gravity and as a target. The extraordinary fact — confirmed to one part in 10¹² by Eötvös-type experiments — is that these two masses are exactly equal. Newton assumed this equivalence; Einstein elevated it to a foundational principle (the Equivalence Principle) from which General Relativity is derived. Mass is a Lorentz scalar: it does not depend on the reference frame (unlike relativistic energy).
Dynamics
03
Inertia & Newton's First Law — The Law of Persistence
◆ Dynamics · Laws of Motion
Newton's First Law (Lex Prima) ∑F = 0  ⇒  a = 0  ⇒  v = constant (including v = 0) Every body persists in its state of rest or uniform motion in a straight line unless compelled to change that state by forces impressed upon it.
Inertia is the intrinsic tendency of matter to resist any change in its state of motion. The First Law is both a definition (of what a force is: something that changes motion) and a statement about nature (objects don't spontaneously speed up or slow down). Before Newton, it was Aristotelian dogma that a moving object requires a continuous force to keep it moving; Newton showed that no force is needed to maintain uniform motion — only to change it. The First Law also implicitly defines inertial reference frames: frames in which a body free of net force moves in a straight line at constant speed.
Everyday manifestation: A passenger lurching forward when a car brakes; a tablecloth pulled out from under dishes; a spacecraft in deep space maintaining velocity with engines off — all are direct demonstrations of inertia.
Dynamics
04
Force & Newton's Second Law — F = ma
◆ Dynamics · Laws of Motion
Newton's Second Law (Lex Secunda) — most important equation in classical physics F = ma    |    F = dp/dt (general form) F [N = kg·m·s⁻²]   m [kg]   a [m·s⁻²]   p = mv [kg·m·s⁻¹]
The Second Law is the quantitative heart of Newtonian mechanics. Force is a vector quantity — it has both magnitude and direction. Acceleration is produced in the same direction as the net force and is proportional to that force and inversely proportional to mass. The more general form, F = dp/dt (rate of change of momentum), handles situations where mass varies (rocket propulsion). The Second Law connects three measurable quantities — force, mass, and acceleration — in a relationship that is linear, predictive, and universal. Every problem in classical mechanics reduces to identifying all forces, summing them vectorially, and applying this law.
Worked insight: A 1 000 kg car accelerating at 2 m/s² requires a net force of 2 000 N (about 449 lbf) — the engine's thrust minus friction and air resistance. This single equation governs everything from feathers to galaxies within Newton's framework.
Dynamics
05
Newton's Third Law — Action and Reaction
◆ Dynamics · Laws of Motion
Newton's Third Law (Lex Tertia) F₁₂ = −F₂₁ For every action there is an equal and opposite reaction. Forces always occur in pairs.
The Third Law is the most misunderstood of Newton's laws. The action-reaction pair always acts on different bodies — so they never cancel each other. A book rests on a table: the book pushes down on the table (gravity + normal reaction of book on table); the table pushes up on the book (normal force). These are action-reaction pairs involving different objects. The book is also pulled down by Earth's gravity and pushed up by the table's normal force — these act on the same object and therefore can cancel (producing zero acceleration when balanced). The Third Law is the basis of rocket propulsion (exhaust pushed backward → rocket pushed forward), swimming, and walking.
Cannon-ball analogy: A cannon recoils when firing. The cannonball (small mass) acquires a large velocity; the cannon (large mass) acquires a small recoil velocity. Equal and opposite forces; equal and opposite momentum changes.
Dynamics
06
Weight vs. Mass — The Most Common Confusion in Physics
◆ Dynamics · Gravity
Definitions W = mg   |   g ≈ 9.81 m/s² (Earth surface) Weight W [N] — a force. Mass m [kg] — a scalar property. g [m/s²] — local gravitational field strength.
Mass is an intrinsic property of a body — it is the same on Earth, on the Moon, and in deep space. Weight is the gravitational force acting on that mass in a particular gravitational field. A 70 kg astronaut has a weight of 686 N on Earth (70 × 9.81), about 113 N on the Moon (70 × 1.62), and zero weight in deep space (but still 70 kg of mass). This distinction is crucial in physics and engineering: a spacecraft is designed for mass (fuel calculation, structural load); a bathroom scale reads weight. An object in free fall is weightless (zero normal force) but retains its full mass — this is precisely the condition experienced by astronauts in orbit.
Gravity
07
Universal Gravitation — The Inverse-Square Law
◆ Gravity · Long-Range Forces
Newton's Law of Universal Gravitation F = G · m₁m₂ / r² G = 6.674 × 10⁻¹¹ N·m²·kg⁻²   |   r = distance between centres [m]   |   F [N]
Newton's supreme intellectual achievement: every particle of matter in the universe attracts every other particle with a force proportional to the product of their masses and inversely proportional to the square of the distance between them. The inverse-square law (1/r²) means doubling the distance reduces the force to one-quarter; tripling it to one-ninth. This single equation explains the Moon's orbit, the tides, the trajectories of planets, and the falling of an apple — phenomena previously considered entirely unrelated. Newton was apparently inspired by the apple, but the intellectual leap was recognising that the same force that pulls the apple down also holds the Moon in orbit, merely diluted by the square of its vastly greater distance.
Gravitational constant G: Newton could not measure G directly. Henry Cavendish first determined it in 1798 using a torsion balance — 71 years after Newton's death. G is the weakest of the four fundamental forces by a factor of ~10³⁶ compared to electromagnetism.
Gravity
08
Gravitational Field — The Force-per-Unit-Mass Picture
◆ Gravity · Fields
Gravitational Field Strength g = F/m = GM/r²   [m/s² or N/kg] g at Earth surface ≈ 9.81 m/s²  |  g at Moon surface ≈ 1.62 m/s²  |  g at Sun surface ≈ 274 m/s²
The gravitational field concept — introduced conceptually by Newton but developed mathematically by Faraday and later — describes the modification of space around a massive object. Every point in space surrounding a mass M has a gravitational field strength g pointing toward M, equal to GM/r². Any mass m placed at that point experiences a force F = mg. The field picture is more powerful than the direct force picture because it decouples the source from the test body — it allows us to map the gravitational influence of any mass distribution without specifying what will be placed in that field. It is the conceptual precursor to Einstein's interpretation of gravity as spacetime curvature.
Gravity
09
Free Fall & the Acceleration due to Gravity
◆ Kinematics · Gravity
Free-fall equations (initial velocity = 0, downward positive) v = gt   |   h = ½gt²   |   v² = 2gh g = 9.80665 m/s² (standard gravity)  |  h [m] height  |  t [s] time  |  v [m/s] velocity
Free fall is motion under gravity alone, with no air resistance. Galileo established experimentally (reputedly at the Leaning Tower of Pisa) that all objects fall with the same acceleration regardless of mass — a result Newton explained via the equivalence of inertial and gravitational mass. From a height of 1 m, an object takes t = √(2h/g) ≈ 0.45 s to reach the ground. The value g varies slightly with latitude (Earth is oblate) and altitude, from 9.832 m/s² at the poles to 9.780 m/s² at the equator. Air resistance introduces a drag force F_d = ½ρv²C_dA, which eventually balances gravity to produce terminal velocity.
Kinematics Gravity
10
Linear Momentum — Quantity of Motion
◆ Dynamics · Conservation Laws
Linear Momentum p = mv   |   F = dp/dt p [kg·m/s] = momentum  |  m [kg]  |  v [m/s] — both p and v are vectors
Newton called momentum (quantitas motus) "quantity of motion" and it was, in his formulation, the primary quantity that force changes. Momentum is a vector — it has both magnitude and direction. A 1 kg ball moving at 10 m/s has the same momentum magnitude as a 10 kg ball moving at 1 m/s, but these are physically very different situations (the lighter ball hits harder per unit area; the heavier ball has 10 times more kinetic energy). Newton's Second Law in its most general form states that force equals the rate of change of momentum — this applies even when mass is not constant, as in a rocket expelling propellant. Momentum is conserved in any closed system free from external forces — one of the most powerful principles in all of physics.
Dynamics
◆ Section II
Impulse, Conservation Laws & Kinematics
How force acts over time, the foundational conservation principles, and the mathematical description of motion without regard to its causes.
11
Impulse — Force Integrated Over Time
◆ Dynamics · Impulse-Momentum
Impulse-Momentum Theorem J = F·Δt = Δp = mΔv J [N·s = kg·m/s] impulse  |  F [N] average force  |  Δt [s] time interval
Impulse is the product of force and the time over which it acts, equal to the change in momentum it produces. The impulse-momentum theorem is a direct consequence of Newton's Second Law integrated over time. Its practical importance: to achieve the same change in momentum (e.g., bringing a car from 60 mph to zero), a longer time interval requires a smaller average force. This is the physics behind crumple zones in cars (extend collision time → reduce peak force → reduce injury), airbags, and the technique of catching a fast ball with a "giving" hand motion.
Dynamics
12
Conservation of Linear Momentum
◆ Conservation Laws
Conservation Law (closed system, no external net force) p₁ + p₂ + ... = constant   |   Δp_total = 0 Holds in all three spatial dimensions independently. Equivalent to Newton's Third Law + Second Law.
In any system where external forces sum to zero, the total vector momentum is conserved — it cannot be created or destroyed, only redistributed among parts of the system. This is not an assumption: it follows mathematically from Newton's Third Law. By Emmy Noether's theorem (1915), conservation of momentum is the consequence of the translational symmetry of space — the laws of physics are the same everywhere. Applications: collision analysis, rocket propulsion, recoil calculation, centre-of-mass motion in explosions. Conservation of momentum often allows problems to be solved even when the internal forces are complex and unknown.
Conservation
13
Displacement, Velocity & Acceleration — The Kinematic Trio
◆ Kinematics
Definitions (all vectors in 3D; shown in 1D for clarity) v = ds/dt   |   a = dv/dt = d²s/dt² s [m] displacement  |  v [m/s] velocity  |  a [m/s²] acceleration  |  t [s] time
Displacement is the change in position (a vector; unlike distance, it can be negative). Velocity is the rate of change of displacement — both instantaneous (the derivative) and average (Δs/Δt) forms are used. Speed is the magnitude of velocity (a scalar). Acceleration is the rate of change of velocity — any change in speed or direction constitutes acceleration. A car going around a curve at constant speed is accelerating (changing direction). The calculus framework Newton invented — expressing velocity and acceleration as derivatives of position — is the mathematical language in which all of classical mechanics is written.
Kinematics
14
Kinematic Equations — The SUVAT System
◆ Kinematics · Uniform Acceleration
Five SUVAT equations (constant acceleration only) v = u + at   |   s = ut + ½at²   |   v² = u² + 2as s = ½(u+v)t   |   s = vt - ½at² s [m] disp.  |  u [m/s] initial vel.  |  v [m/s] final vel.  |  a [m/s²] accel.  |  t [s] time
The five kinematic equations are valid only for constant (uniform) acceleration in a straight line. They are algebraic integrations of the definitions of velocity and acceleration. Given any three of the five variables {s, u, v, a, t}, one can solve for the remaining two. The equations are non-relativistic but exact for everyday mechanical problems. Applications: calculating stopping distance of a vehicle, range of a projectile, velocity of a falling object after a given time. For variable acceleration, the full calculus form (v = ∫a dt, s = ∫v dt) must be used.
Kinematics
15
Projectile Motion — Independence of Axes
◆ Kinematics · 2D Motion
Projectile equations (launch angle θ, initial speed v₀, no air resistance) x = v₀cos(θ)·t   |   y = v₀sin(θ)·t - ½gt² Range R = v₀²·sin(2θ)/g   |   Max height H = v₀²sin²(θ)/(2g) Maximum range at θ = 45°  |  Trajectory is a parabola
Projectile motion is the superposition of two independent motions: uniform horizontal motion (no horizontal force, so constant horizontal velocity) and uniformly accelerated vertical motion (constant downward acceleration g). Galileo established this independence of axes; Newton explained it with the Second Law applied separately to each direction. The resulting trajectory is a parabola. Maximum range is achieved at 45° launch angle; complementary angles (e.g., 30° and 60°) give the same horizontal range but different flight times. Air resistance breaks the parabolic shape and shifts the optimal angle below 45°.
Kinematics
16
Relative Motion & Galilean Relativity
◆ Kinematics · Frames of Reference
Galilean Velocity Addition v₁₃ = v₁₂ + v₂₃ v_AB = velocity of A relative to B  |  Velocities add linearly (breaks down at v ≈ c)
Motion is always measured relative to a chosen reference frame — there is no absolute velocity in Newtonian mechanics (only absolute acceleration makes physical sense). Galilean relativity states that the laws of mechanics are identical in all inertial frames. A ball thrown vertically on a smoothly moving train follows the same parabolic arc in the train frame as it would on a stationary train — the train's velocity simply adds vectorially to all velocities in the ground frame. This principle became the seed of Einstein's Special Relativity, which corrected Galilean velocity addition to remain consistent with the invariant speed of light.
Kinematics
◆ Section III
Energy, Work, Power & Collisions
The energy perspective on mechanics — scalar quantities that complement the vector force approach and reveal deep conservation principles.
17
Work — Force Acting Through Distance
◆ Energy · Work-Energy Theorem
Work definitions W = F·d·cos(θ)   |   W = ∫F·ds   [J = N·m = kg·m²·s⁻²] θ = angle between force vector and displacement vector  |  Work is a scalar
In physics, work has a precise meaning: force times displacement in the direction of the force. A force perpendicular to motion does zero work (a centripetal force does no work on an object in circular motion). A force opposing motion does negative work. The work-energy theorem states that the net work done on an object equals its change in kinetic energy. Carrying a suitcase horizontally at constant speed requires zero net work by Newton's laws — the muscles do positive work against gravity to lift it and against friction in the body, but the net work done on the suitcase in the horizontal direction is zero. Only in everyday language does "hard work" mean physical effort.
Energy
18
Kinetic Energy — Energy of Motion
◆ Energy
Kinetic Energy Eₖ = ½mv²   [J] Scales with the square of velocity — doubling speed quadruples kinetic energy. Scalar quantity.
Kinetic energy is the energy a body possesses by virtue of its motion. The dependence has profound practical consequences: a car at 100 km/h has four times the kinetic energy of the same car at 50 km/h, requiring four times the stopping distance (all else equal) — the physics behind speed limits. The work-energy theorem states W_net = ΔEₖ: net work equals the change in kinetic energy. Note that kinetic energy is frame-dependent (a stationary observer and a moving observer assign different KE values to the same object), while the work done is also frame-dependent in the same proportion.
Energy
19
Potential Energy — Stored Energy of Position
◆ Energy · Conservative Forces
Types of Potential Energy Gravitational: U = mgh   |   Elastic: U = ½kx² h [m] height above reference  |  k [N/m] spring constant  |  x [m] extension/compression
Potential energy is energy stored in a system by virtue of the configuration of its parts — their relative positions under the influence of a conservative force. Gravitational potential energy (mgh) depends on height above an arbitrary reference level. Elastic potential energy (½kx²) is stored in deformed springs or elastic materials. The concept of potential energy only exists for conservative forces — forces for which the work done is path-independent and depends only on initial and final positions. Friction is not conservative: it dissipates energy as heat regardless of path and has no associated potential energy.
Energy
20
Conservation of Mechanical Energy
◆ Energy · Conservation Laws
Conservation of Mechanical Energy (no non-conservative forces) E = Eₖ + U = ½mv² + mgh = constant Holds when only conservative forces do work. Add ½kx² for spring PE. Fails in presence of friction.
In the absence of friction and other dissipative forces, the total mechanical energy — kinetic plus potential — remains constant throughout motion. A roller-coaster car at the top of a hill (high PE, low KE) converts energy to speed at the bottom (low PE, high KE), with total energy conserved. This principle enormously simplifies many problems: instead of tracking forces at every instant, we simply compare energies at initial and final states. By Noether's theorem, conservation of energy follows from the time-translation symmetry of physical laws — the laws of physics are the same today as yesterday.
Pendulum example: At maximum height, all energy is potential; at the lowest point, all is kinetic. The speed at the bottom is found from ½mv² = mghv = √(2gh), independent of mass.
Energy
21
Power — Rate of Energy Transfer
◆ Energy · Power
Power P = W/t = F·v = dE/dt   [W = J/s = kg·m²·s⁻³] 1 horsepower = 745.7 W  |  Human peak power ≈ 1 kW for a few seconds
Power measures how quickly work is done or energy is transferred. The same work performed over a shorter time requires more power. The form P = Fv is particularly useful: a car engine produces a fixed maximum power output; at higher speeds, the available force for acceleration decreases. This is why cars have a maximum speed (where engine power equals drag power) and why low-gear high-torque is needed for steep hills (high force, low speed). A 100 W lightbulb consumes 100 joules per second; the human heart does roughly 1–5 W of continuous mechanical work.
Energy
22
Elastic & Inelastic Collisions
◆ Dynamics · Collisions
Collision types Elastic: p conserved AND KE conserved Inelastic: p conserved, KE NOT conserved Perfectly inelastic: objects stick together. v_f = (m₁v₁ + m₂v₂)/(m₁+m₂)
All collisions conserve momentum (assuming no external forces). They differ in kinetic energy conservation. In a perfectly elastic collision, kinetic energy is also conserved — this is an idealisation (billiard balls and molecular collisions approach it). In a perfectly inelastic collision, maximum kinetic energy is lost, converted to heat, deformation, and sound — the objects stick together after impact. Real collisions are somewhere between. The coefficient of restitution e = relative separation speed / relative approach speed quantifies this: e = 1 (elastic), e = 0 (perfectly inelastic).
Dynamics Energy
23
Centre of Mass — The Weighted Average Position
◆ Dynamics · System of Particles
Centre of Mass position (discrete particles) x_cm = (∑mᵢxᵢ) / ∑mᵢ Extends to y_cm, z_cm. For continuous bodies: replace sum with integral over mass distribution.
The centre of mass (CoM) is the unique point at which the entire mass of a system can be considered concentrated for the purpose of calculating translational motion under external forces. Newton's Second Law applied to the CoM: F_ext = M·a_cm, where M is total mass. The CoM of a system in free space moves in a straight line at constant velocity if no external force acts — even as the individual parts may be rotating, oscillating, or exploding around it. This is why a rotating hammer thrown through the air traces a parabola at its CoM while spinning. Humans locate their CoM by balance; athletes manipulate it to optimise performance.
Dynamics
24
Friction — The Force of Surface Interaction
◆ Dynamics · Contact Forces
Friction Laws (Amontons-Coulomb) f_s ≤ μ_s·N   |   f_k = μ_k·N f_s [N] static friction  |  f_k [N] kinetic friction  |  μ = coefficient (dimensionless)  |  N [N] normal force
Friction is a contact force opposing relative motion (or tendency of motion) between surfaces. Static friction can range from zero up to a maximum μ_sN — it is whatever value is needed to prevent motion, up to that maximum. Kinetic friction is approximately constant once sliding begins, slightly less than maximum static friction. Coefficients vary widely: ice on ice ≈ 0.03; rubber on dry concrete ≈ 0.7. Friction is fundamentally a macroscopic approximation of complex molecular adhesion interactions at the surface interface. It is a non-conservative force — it always dissipates mechanical energy as heat.
Dynamics
25
Normal Force & Tension — Constraint Forces
◆ Dynamics · Contact Forces
Examples Book on table: N = mg   |   Atwood machine: T = 2m₁m₂g/(m₁+m₂) Normal force N always perpendicular to surface  |  Tension T acts along a string/rope
Normal force is the contact force exerted by a surface on an object, always perpendicular (normal) to that surface. It is a reaction force: it adjusts to whatever value is needed to prevent interpenetration of surfaces — thus it is not always equal to weight. On an inclined plane, N = mg·cos(θ); in a loop-the-loop, N varies continuously. Tension is the pulling force transmitted along a rope, string, cable, or rod. For an ideal (massless, inextensible) string, tension is the same at every point. These are both examples of constraint forces — they enforce physical constraints (surfaces don't overlap; strings don't push) and are determined by Newton's Second Law applied to the complete system.
Dynamics
26
Equilibrium — Static & Dynamic Balance of Forces
◆ Dynamics · Statics
Conditions for equilibrium (translational & rotational) ∑F = 0   (translational)   |   ∑τ = 0   (rotational) Both conditions must hold simultaneously for complete static equilibrium. Choose any pivot point for the torque sum — unknown forces at that point vanish from the equation.
A body is in static equilibrium when both the net force and the net torque acting on it are zero — it is motionless and not beginning to rotate. Dynamic equilibrium occurs when the body moves at constant velocity with zero net force. Statics — the study of bodies in static equilibrium — underlies all of structural engineering: bridges, buildings, cranes, and dams are designed so that every joint and beam satisfies both equilibrium conditions simultaneously. The torque condition is the key that allows structures to resist not just translation but tipping and collapse. Choosing the pivot point cleverly eliminates unknown forces from the torque equation — a standard and powerful problem-solving technique in statics.
Classic ladder problem: A ladder leaning against a frictionless wall requires three equations: ∑F_x = 0 (wall normal = ground friction), ∑F_y = 0 (ground normal = weight), and ∑τ_base = 0 (which determines the minimum μ needed to prevent slipping). All three must hold simultaneously.
Dynamics
◆ Section IV
Rotational Mechanics — The Angular World
The complete rotational analogue of linear mechanics: every linear quantity has a rotational counterpart connected by a precise mathematical correspondence.
The linear ↔ rotational analogy: m ↔ I  |  v ↔ ω  |  a ↔ α  |  F ↔ τ  |  p ↔ L  |  KE = ½mv² ↔ ½Iω² Every law of linear mechanics has an exact rotational counterpart. Learning one set transfers directly to the other.
27
Circular Motion — Kinematics of Revolution
◆ Kinematics · Rotation
Circular Motion Relations v = rω   |   a_c = v²/r = rω²   |   T = 2πr/v = 2π/ω r [m] radius  |  ω [rad/s] angular velocity  |  a_c [m/s²] centripetal acceleration  |  T [s] period
An object moving in a circle at constant speed undergoes uniform circular motion. Despite constant speed, it is accelerating — the direction of velocity changes continuously. The acceleration (centripetal, pointing toward the centre) has magnitude v²/r. The linear speed v = rω connects the rotational description (angular velocity ω) to the linear description. The period T is the time for one complete revolution. Non-uniform circular motion (changing speed) adds a tangential component of acceleration a_t = rα alongside the centripetal component.
Rotation
28
Centripetal Force — The Inward-Pointing Requirement
◆ Dynamics · Circular Motion
Centripetal Force (not a new force — provided by existing forces) F_c = mv²/r = mrω² Provided by: gravity (satellite), tension (ball on string), normal force (car on curve), friction (car tyres)
Centripetal force is not a new type of force — it is the net inward force required to maintain circular motion, provided by whatever real forces are available. The Moon's centripetal force is provided by Earth's gravity; a car rounding a curve uses static friction from the road; a ball on a string uses tension. The centrifugal force felt by a passenger in a turning car is not a real force — it is a fictitious (pseudo) force that arises only in the non-inertial rotating reference frame. In the inertial frame, the passenger's body tends to continue in a straight line (inertia) while the car floor pushes inward — the net effect is circular motion, not an outward force.
Rotation
29
Angular Displacement, Velocity & the Radian
◆ Kinematics · Rotation
Angular kinematic quantities θ [rad]   |   ω = dθ/dt [rad/s]   |   arc length s = rθ 1 revolution = 2π rad = 360°  |  ω = 2πf = 2π/T  |  v_tangential = rω
Just as linear kinematics uses displacement, velocity, and acceleration, rotational kinematics uses their angular counterparts. Angular displacement θ (theta) is measured in radians — the ratio of arc length to radius, making it dimensionless. The radian is the natural unit for circular motion because it eliminates conversion factors in all rotational equations. Angular velocity ω (omega) is the rate of change of angular displacement; for uniform circular motion it is constant. The tangential (linear) speed of any point on a rotating body is v = rω — points farther from the axis move faster. A vinyl record at 33⅓ rpm has ω = 33.33/60 × 2π ≈ 3.49 rad/s; a point on the outer edge (r = 0.15 m) moves at v = 0.524 m/s while the label area (r = 0.025 m) moves at only 0.087 m/s — same ω, very different v.
Rotation Kinematics
30
Angular Acceleration & Rotational Kinematics
◆ Kinematics · Rotation
Rotational SUVAT (constant angular acceleration α) α = dω/dt   [rad/s²] ω = ω₀ + αt   |   θ = ω₀t + ½αt²   |   ω² = ω₀² + 2αθ Exact rotational analogues of the linear SUVAT equations: s↔θ, u↔ω₀, v↔ω, a↔α
Angular acceleration α (alpha) is the rate of change of angular velocity — the rotational analogue of linear acceleration. When a motor spins up from rest, α is positive; when a spinning top slows, α is negative (angular deceleration). The rotational kinematic equations are structurally identical to the linear SUVAT equations with every quantity replaced by its angular counterpart. A point on a body undergoing angular acceleration experiences two components of linear acceleration: the centripetal (a_c = rω², toward the axis) and the tangential (a_t = rα, tangent to the circular path). The total linear acceleration is their vector sum: a = √(a_c² + a_t²).
Example: A grinding wheel accelerates from rest to 3 000 rpm (314 rad/s) in 10 s. Angular acceleration: α = 314/10 = 31.4 rad/s². Total angle turned: θ = ½ × 31.4 × 100 = 1 570 rad ≈ 250 full revolutions during spin-up.
Rotation Kinematics
31
Torque — The Rotational Analogue of Force
◆ Dynamics · Rotation
Torque (moment of force) τ = r × F = r·F·sin(θ)   [N·m] r [m] moment arm (perpendicular distance from axis to line of force)  |  θ = angle between r and F vectors
Torque (τ, "tau") is the rotational effectiveness of a force — it depends not only on the magnitude of the force but on where and at what angle it is applied. A force applied at a greater distance from the rotation axis (larger r) produces more torque for the same force magnitude. A force directed radially toward the axis (θ = 0) produces zero torque. Newton's Second Law for rotation: τ = Iα (net torque = moment of inertia × angular acceleration). Torque is a vector (its direction is along the rotation axis, determined by the right-hand rule). Everyday examples: door hinges (apply force far from hinge), wrenches (long handle = more torque), seesaws (balanced when torques are equal).
Rotation
32
Moment of Inertia — Rotational Mass
◆ Dynamics · Rotation
Moment of Inertia (discrete & continuous) I = ∑mᵢrᵢ²   |   I = ∫r²dm   [kg·m²] Solid sphere: I = 2/5·mr²  |  Thin ring: I = mr²  |  Solid cylinder: I = ½mr²
The moment of inertia (I) is the rotational analogue of mass — it measures resistance to angular acceleration. Unlike mass, I depends on the distribution of mass relative to the rotation axis: mass far from the axis contributes more ( dependence). A solid sphere and a thin spherical shell of the same mass and radius have different moments of inertia (2/5 mr² vs. 2/3 mr²) because the shell has all its mass at maximum distance from the centre. The parallel axis theorem allows I to be calculated for any axis: I = I_cm + md², where d is the distance from the centre of mass to the new axis.
Rotation
33
Angular Momentum & its Conservation
◆ Rotation · Conservation Laws
Angular Momentum L = Iω   |   L = r × p   [kg·m²/s] Conservation: τ_net = 0 ⇒ L = constant  |  By Noether: conserved due to rotational symmetry of space
Angular momentum (L) is the rotational analogue of linear momentum. It is conserved whenever the net external torque on a system is zero. The spinning ice-skater who pulls in their arms reduces I (mass closer to axis), so ω must increase to keep L = Iω constant — they spin faster. A gyroscope resists changes in orientation because its large angular momentum makes the required torque to change L enormous. The Earth's axial tilt remains stable over thousands of years for the same reason. Like energy conservation and momentum conservation, conservation of angular momentum is a deep consequence of the symmetry structure of space itself.
Rotation Conservation
34
Rotational Kinetic Energy — Energy of Spinning Bodies
◆ Rotation · Energy
Rotational Kinetic Energy Eₖ_rot = ½Iω² I [kg·m²] moment of inertia  |  ω [rad/s] angular velocity  |  Compare: Eₖ_linear = ½mv²
A spinning body possesses kinetic energy by virtue of its rotation, entirely analogous to the translational kinetic energy ½mv². The formula ½Iω² replaces mass with moment of inertia and linear speed with angular speed. This energy is real and can do work — a flywheel stores energy as rotational KE and releases it on demand. The total kinetic energy of a body that is both translating and rotating (like a rolling ball) is the sum of both: E_total = ½mv²_cm + ½Iω². This has important consequences: two objects of the same mass but different mass distributions (solid vs. hollow cylinder) accelerate at different rates down an incline because a larger fraction of available energy must go into rotational KE for the object with higher I.
Flywheel energy storage: A 100 kg steel flywheel of radius 0.5 m (I = ½mr² = 12.5 kg·m²) spinning at 3 000 rpm (ω = 314 rad/s) stores E = ½ × 12.5 × 314² ≈ 617 000 J — enough to accelerate a car from 0 to 60 mph several times. Flywheel KERS systems in Formula 1 cars exploit exactly this principle.
Rotation Energy
35
Rolling Motion — Translation Plus Rotation Combined
◆ Rotation · Kinematics
Rolling without slipping (contact point instantaneously at rest) v_cm = rω   |   a_cm = rα E_total = ½mv²_cm + ½Iω² = ½mv²_cm(1 + I/mr²) For solid sphere: I = 2/5·mr² → E_total = 7/10·mv²_cm  |  For hollow cylinder: E_total = mv²_cm
Rolling without slipping is a combined motion where translation and rotation are linked by the constraint v_cm = rω. The contact point between a rolling body and the surface is momentarily at rest — if it weren't, the body would be sliding, not rolling. This constraint means friction does no work on a purely rolling object (no relative motion at contact), yet friction is essential: without it, the body would slip. When a ball or cylinder rolls down an incline of height h, energy conservation gives its speed at the bottom: v = √(2gh/(1 + I/mr²)). A solid sphere (I = 2/5 mr²) reaches the bottom faster than a hollow sphere (I = 2/3 mr²) of the same mass and radius — a result that can be verified by a simple ramp experiment and depends entirely on mass distribution, not mass or size.
Rotation Kinematics
◆ Section V
Oscillations — Periodic Motion
Simple harmonic motion, springs, pendulums, and the universal phenomenon of resonance — the mathematics of anything that oscillates.
36
Simple Harmonic Motion — The Universal Oscillator
◆ Oscillations · SHM
SHM equations x(t) = A·cos(ωt + φ)   |   a = -ω²x ω = 2πf = 2π/T   |   E_total = ½mω²A² = constant A [m] amplitude  |  ω [rad/s] angular frequency  |  T [s] period  |  φ [rad] phase constant
Simple harmonic motion (SHM) occurs whenever a restoring force is proportional to and directed opposite to displacement from equilibrium (F = -kx). The resulting acceleration a = -(k/m)x leads to sinusoidal position variation. SHM is the most important type of periodic motion because any small-amplitude oscillation about a stable equilibrium is approximately SHM — regardless of the exact shape of the potential well. This is why the same mathematics describes springs, pendulums, molecular vibrations, electrical LC circuits, sound waves, and quantum harmonic oscillators. The total energy continuously converts between kinetic (maximum at centre) and potential (maximum at turning points).
Oscillations
37
Hooke's Law — The Ideal Spring
◆ Oscillations · Elasticity
Hooke's Law (Robert Hooke, 1678) F = -kx   |   T = 2π√(m/k) k [N/m] spring constant (stiffness)  |  x [m] displacement from equilibrium  |  T [s] period
Hooke's Law states that the restoring force of a spring is proportional to its extension or compression. The negative sign indicates the force always opposes the displacement — this is what makes it a restoring force and gives rise to oscillatory motion. The spring constant k characterises stiffness: a car suspension spring might have k ≈ 20 000 N/m; a watch spring, a few N/m. Critically, the period T = 2π√(m/k) is independent of amplitude (for ideal springs and small oscillations). Stiffer springs oscillate faster; heavier masses oscillate slower. Hooke's Law breaks down at large deformations (elastic limit exceeded).
Oscillations
38
The Simple Pendulum — Gravity's Oscillator
◆ Oscillations · Gravity
Simple Pendulum (small angle approximation: θ < ~15°) T = 2π√(L/g) L [m] pendulum length  |  g [m/s²] local gravitational acceleration  |  Independent of mass and amplitude (for small θ)
The simple pendulum — a mass on a massless string swinging through small arcs — exhibits SHM because the restoring force component (mg·sinθ ≈ mgθ for small θ) is proportional to displacement. The remarkable result: the period depends only on length and local gravity, not on mass or amplitude. Galileo first noted this isochronism (allegedly by timing his pulse against a swinging chandelier in Pisa Cathedral). The pendulum clock, accurate to seconds per day, exploited this property and was the most precise timekeeping device for over 200 years. The period formula also enables measurement of local g: measure T and L, solve for g = 4π²L/T².
Oscillations Gravity
39
Resonance — When Driving Frequency Meets Natural Frequency
◆ Oscillations · Resonance
Resonance condition ω_drive = ω_0 = √(k/m)  ⇒  amplitude → maximum (damping limited) Q-factor = ω_0 / Δω = resonance sharpness  |  High Q = sharp resonance, slow decay
Resonance occurs when a periodic driving force is applied at a system's natural frequency. Energy is added constructively each cycle and amplitude builds dramatically — limited only by damping. Resonance is simultaneously one of the most useful and most dangerous phenomena in engineering. Useful: radio tuning circuits select signals by resonance; MRI scanners use nuclear magnetic resonance; musical instrument bodies amplify specific frequencies. Dangerous: the Tacoma Narrows Bridge collapse (1940) was caused by aerodynamic forcing at the bridge's structural resonance frequency; soldiers break step crossing bridges to avoid resonant forcing; earthquake damage is amplified when building natural frequencies match seismic frequencies.
Oscillations
◆ Section VI
Orbital Mechanics, Escape & Celestial Dynamics
Newton's gravitation applied to planetary motion — unifying terrestrial and celestial physics for the first time in history.
40
Kepler's Three Laws — The Empirical Foundation
◆ Orbital Mechanics · History
Kepler's Laws (1609–1619) — derived by Newton from F = GMm/r² I. Orbits are ellipses with Sun at one focus. II. Equal areas swept in equal times (conserves angular momentum). III. T² ∝ a³   exact: T² = 4π²a³/(GM) T [s] orbital period  |  a [m] semi-major axis  |  M [kg] central body mass
Johannes Kepler (1609–1619) derived his three laws empirically from Tycho Brahe's meticulous observational data. Newton's supreme achievement was deriving all three laws mathematically from his Law of Universal Gravitation and Second Law — demonstrating that they are not independent facts but consequences of a single force law. Kepler's Second Law (equal areas in equal times) is equivalent to conservation of angular momentum; the Third Law (T² ∝ a³) follows from equating centripetal force to gravitational force. This unification of terrestrial physics (falling apple) with celestial mechanics (planetary orbits) was the scientific revolution's defining moment.
Gravity
41
Orbital Mechanics — Circular & Elliptical Orbits
◆ Orbital Mechanics
Circular orbit (radius r, central mass M) v_orbit = √(GM/r)   |   T = 2πr/v = 2π√(r³/GM) LEO (r ≈ 6 571 km): v ≈ 7.8 km/s, T ≈ 90 min  |  GEO (r ≈ 42 164 km): v ≈ 3.1 km/s, T = 24 h
A circular orbit exists when gravitational force exactly provides the centripetal acceleration: GMm/r² = mv²/r. The orbital speed is entirely determined by the altitude — higher orbits are slower. At geostationary orbit (35 786 km above Earth's equator), the orbital period matches Earth's rotation, so the satellite appears stationary — the basis of communication and GPS satellites. Elliptical orbits generalise this: at periapsis (closest approach) speed is maximum; at apoapsis (farthest point) speed is minimum, consistent with conservation of energy and angular momentum. The total energy of an orbit: E = -GMm/(2a), negative indicating a bound system.
Gravity
42
Escape Velocity — Breaking Free from Gravity
◆ Orbital Mechanics · Gravity
Escape Velocity (from radius r, central mass M) v_esc = √(2GM/r) Earth: 11.2 km/s  |  Moon: 2.4 km/s  |  Sun: 617 km/s  |  Black hole (Schwarzschild): v_esc = c
Escape velocity is the minimum speed at which an object must be launched to escape a gravitational field without further propulsion. Derived by setting total mechanical energy to zero: ½mv² - GMm/r = 0. Notably, v_esc = √2 · v_orbit — escape velocity is always √2 ≈ 1.414 times the circular orbital speed at the same radius. A black hole is formally defined (in classical terms) as an object for which the escape velocity at the surface equals or exceeds the speed of light — the Schwarzschild radius is r_s = 2GM/c². For Earth, r_s ≈ 9 mm; Earth would need to be compressed to a marble to become a black hole.
Gravity
43
Tidal Forces — Gravity's Differential Effect
◆ Gravity · Tides
Tidal acceleration (difference in gravity across object of size d, at distance r from mass M) Δg ≈ 2GMd/r³ Scales as 1/r³ — falls off faster than gravity itself (1/r²). Moon dominates Earth's tides despite Sun being far more massive.
Tidal forces arise because gravity follows an inverse-square law: the near side of a body is pulled more strongly toward a massive object than the far side, stretching the body along the radial direction and squeezing it sideways. Earth's ocean tides are caused by the Moon's tidal force — the near-side ocean is pulled toward the Moon, the far-side ocean is "left behind," creating two tidal bulges. The Sun also contributes tides; spring tides (Moon and Sun aligned) and neap tides (90° apart) result from their combination. Tidal forces also cause orbital decay of nearby moons, the synchronous rotation of the Moon (same face always toward Earth), and the eventual destruction of objects inside the Roche limit.
Gravity
◆ Section VII
Fluids, Mathematics & The Limits of Newton
Classical fluid mechanics, the mathematical foundations Newton invented, and an honest account of where his framework breaks down.
44
Pressure & Archimedes' Principle
◆ Fluids · Statics
Pressure & Buoyancy P = F/A   [Pa = N/m²]   |   P = P_0 + ρgh Archimedes: F_buoy = ρ_fluid · g · V_displaced ρ [kg/m³] fluid density  |  h [m] depth  |  V [m³] submerged volume
Pressure is force per unit area, transmitted equally in all directions within a static fluid (Pascal's principle). Hydrostatic pressure increases linearly with depth. Archimedes' Principle (287–212 BC, predating Newton): the upward buoyant force on a submerged object equals the weight of the fluid it displaces. An object floats when its average density is less than the fluid; sinks when greater. Newton's contribution was explaining buoyancy quantitatively via pressure differences: the higher pressure on the bottom face minus the lower pressure on the top face yields the net upward buoyant force. This explains ships, hot-air balloons, submarines, and the hydrometer.
Fluids
45
Fluid Dynamics — The Continuity Equation
◆ Fluids · Flow
Continuity Equation (incompressible fluid) A₁v₁ = A₂v₂ = Q = constant A [m²] cross-sectional area  |  v [m/s] fluid velocity  |  Q [m³/s] volumetric flow rate
The continuity equation expresses conservation of mass for fluid flow: the volume flow rate (volume per unit time) is constant in a pipe of varying cross-section (for incompressible fluids). Where the pipe is narrow (A small), the fluid moves faster (v large), and vice versa. This is why a river speeds up at a narrow gorge and slows in a wide delta; why squeezing a garden hose end increases jet speed. For compressible fluids (gases), the mass flow rate ρAv = constant must be used instead. Continuity is the foundation of all fluid mechanics and is conservation of mass in differential form (the advection equation).
Fluids
46
Bernoulli's Principle — Energy Conservation for Fluids
◆ Fluids · Flow
Bernoulli's Equation (Daniel Bernoulli, 1738 — derived from Newton's laws) P + ½ρv² + ρgh = constant along a streamline P [Pa] static pressure  |  ½ρv² [Pa] dynamic pressure  |  ρgh [Pa] hydrostatic pressure
Bernoulli's equation is the energy conservation equation for an ideal (inviscid, incompressible, steady) fluid: along a streamline, the sum of static pressure, dynamic pressure, and hydrostatic pressure is constant. Where fluid speeds up, pressure drops. This explains: aircraft lift (faster flow over curved upper wing surface → lower pressure above → net upward force); the carburetor (fast airflow → low pressure → fuel drawn in); the Venturi meter; the curveball in baseball; the Coandă effect. Real fluids deviate from Bernoulli due to viscosity — addressed by the Navier-Stokes equations, one of the unsolved Millennium Prize Problems.
Fluids
47
Dimensional Analysis — Physics as a Language
◆ Mathematics · Method
Fundamental dimensions (SI) Length [L]   Mass [M]   Time [T]   Current [I]   Temperature [Θ] Force: [MLT⁻²]  |  Energy: [ML²T⁻²]  |  Power: [ML²T⁻³]
Dimensional analysis is the technique of tracking the physical dimensions of every quantity in an equation to verify consistency and derive relationships. Every valid physical equation must be dimensionally homogeneous — each term must have the same dimensions. Dimensional analysis can: check the consistency of derived equations; predict the form of unknown relationships (Buckingham π theorem); convert between unit systems; and catch algebraic errors instantly. The pendulum period must involve L (length), g (acceleration, [LT⁻²]) and possibly m (mass) — only T = f(L/g)^{1/2} gives the right dimensions of time, and experiment confirms the coefficient is 2π.
Mathematics
48
Newton's Calculus — The Mathematics of Change
◆ Mathematics · Calculus
Fundamental Theorem of Calculus (Newton's "method of fluxions") d/dt[x(t)] = v(t)   |   ∫v(t)dt = x(t) + C F = ma = m·d²x/dt²  →  Second-order ODE governs all motion
Newton invented calculus ("method of fluxions") between 1665–1666, simultaneously and independently with Leibniz (who published first, 1684). Without calculus, the Principia could not have been written — the laws of motion are inherently differential equations. Velocity is the derivative of position; acceleration is the derivative of velocity (or second derivative of position). Newton's Second Law becomes a second-order ordinary differential equation whose solution gives position as a function of time. The integral of a force over time gives impulse; over distance gives work. Modern physics — from quantum mechanics to general relativity — is entirely written in the language Newton invented to describe motion.
Mathematics
49
Superposition of Forces — The Vector Sum
◆ Dynamics · Vector Methods
Principle of Superposition F_net = F₁ + F₂ + F₃ + ... = ∑Fᵢ Vector addition; each force acts independently. Resolving into components: F_x = ∑Fᵢcosθᵢ, F_y = ∑Fᵢsinθᵢ
The principle of superposition states that when multiple forces act on a body, each force acts independently, and the net effect is the vector sum of all forces. This is Newton's implicit assumption that forces are additive — a body simultaneously experiencing gravity, normal force, friction, and tension simply experiences the vector resultant of all four. This linear principle fails for strong gravitational fields (General Relativity is nonlinear) and in nonlinear mechanical systems, but holds exactly within Newtonian mechanics. The practical method: resolve all forces into orthogonal components (typically x and y), sum each component independently, then find the resultant magnitude and direction.
Dynamics
50
The Limits of Newtonian Physics — Where Newton Ends
◆ Foundations · Modern Physics
Breakdown conditions and their replacements v ≈ c  ⇒  Special Relativity: E = γmc², p = γmv Strong gravity  ⇒  General Relativity: G_μν = 8πG/c⁴ · T_μν Atomic scale  ⇒  Quantum Mechanics: HΨ = iℏ∂Ψ/∂t
Newtonian mechanics is not wrong — it is a limiting case of more complete theories, accurate when: speeds are much less than light (v ≪ c ≈ 3×10⁸ m/s); gravitational fields are weak; and the action of the system is much larger than Planck's constant (ℏ ≈ 10⁻³⁴ J·s). Special Relativity (Einstein, 1905) governs high-speed motion: mass increases with velocity, time dilates, lengths contract, and the speed of light is invariant. General Relativity (Einstein, 1915) replaces Newton's gravity with spacetime curvature — required for GPS satellites (gravitational and velocity time dilation corrections of ~38 microseconds/day). Quantum Mechanics governs atoms and subatomic particles: energy is quantised, particles have wave nature, and the Heisenberg uncertainty principle sets fundamental limits on simultaneous knowledge of position and momentum. For all engineering, ballistics, orbital mechanics, and most of everyday physics, Newton is exact to many decimal places.
The measure of Newton's achievement: The equations Newton wrote in 1687 are used unchanged today to navigate spacecraft to Pluto (3 billion km from Earth, arriving within seconds of schedule), to design bridges, to model ocean currents, and to calculate the trajectories of billions of tonnes of steel and concrete in motion daily. No other intellectual product of the 17th century remains so operationally current.
Dynamics Mathematics
◆ Appendix
Quick Reference — Key Equations
ConceptEquationSI Units
Newton's 2nd LawF = ma = dp/dtN = kg·m·s⁻²
Universal GravitationF = Gm₁m₂/r²N
Kinetic EnergyE_k = ½mv²J = kg·m²·s⁻²
Gravitational PEU = mghJ
Momentump = mvkg·m·s⁻¹
ImpulseJ = FΔt = ΔpN·s
WorkW = Fd·cosθJ
PowerP = W/t = FvW = J·s⁻¹
Centripetal Acc.a_c = v²/r = rω²m·s⁻²
Torqueτ = rF·sinθ = IαN·m
Angular MomentumL = Iω = r × pkg·m²·s⁻¹
Hooke's LawF = -kxN
SHM Period (spring)T = 2π√(m/k)s
Pendulum PeriodT = 2π√(L/g)s
Orbital Speedv = √(GM/r)m·s⁻¹
Escape Velocityv_esc = √(2GM/r)m·s⁻¹
Kepler's 3rd LawT² = 4π²a³/(GM)s² / m³
Bernoulli's EquationP + ½ρv² + ρgh = constPa
ArchimedesF_b = ρ_fluid·g·VN
Friction (kinetic)f_k = μ_k·NN

"If I have seen further it is by standing on the shoulders of Giants."

◆ Isaac Newton, Letter to Robert Hooke, 1675

"Nature and Nature's laws lay hid in night: God said, Let Newton be! and all was light."

◆ Alexander Pope, epitaph proposed for Newton's tomb, 1727

"I do not know what I may appear to the world, but to myself I seem to have been only like a boy playing on the seashore... whilst the great ocean of truth lay all undiscovered before me."

◆ Isaac Newton, recalled by David Brewster, Memoirs of Newton (1855)