Formulas & shortcuts
Physics · 212
Every formula in this course and the easiest ways to remember them, on one page.
1Measurement and motionBeginner
What is physics? Measurement and SI units
Open lesson- athe smaller of two neighbouring numbered marks
- bthe larger of these two marks
- nthe number of divisions between them
Units of physical quantities: links between chapters
Open lesson- Nnewton — from F = m · a
- Jjoule (work and energy) — from W = F · s
- Wwatt (power) — from P = W / t
- Papascal (pressure) — from p = F / S
These four units underlie all the rest: the electrical units start from the joule and the watt.
- Ccoulomb (electric charge) — q = I · t
- Vvolt (voltage, potential, emf) — U = W / q or U = P / I
- Ωohm (resistance) — R = U / I
- Ffarad (capacitance) — C = q / U
The volt comes out two ways — joule per coulomb or watt per ampere — with the same result.
- Ttesla (magnetic induction) — from the Ampère force, B = F / (I · l)
- Wbweber (magnetic flux) — Φ = B · S; from ε = ΔΦ / Δt, Wb = V · s
- Hhenry (inductance) — L = Φ / I; from ε = L · ΔI / Δt, H = V · s/A = Ω · s
All magnetic units follow from the Ampère force and the law of electromagnetic induction: once you know the weber, the tesla and the henry follow easily.
- q · E = m · ga charged body in equilibrium in an electric field: the electric force balances gravity (E is the field strength, N/C = V/m)
- η · P · t = c · m · Δtheat balance of a heater: the share η of the energy released at power P during time t warms the water by Δt
Unit check: C · N/C = N and W · s = J — both sides match.
Speed and velocity
Open lesson- vspeed, in m/s
- sdistance travelled, in metres (m)
- ttime taken, in seconds (s)
From this, s = v · t and t = s / v.
Acceleration and uniformly accelerated motion
Open lesson- aₓacceleration projection, in m/s²
- v₀ₓ, vₓprojections of the initial and final velocity, in m/s
- ttime of the change, in s
If vₓ and aₓ have the same sign, the speed grows; if the signs are opposite, the body slows down. So a “negative acceleration” does not always mean braking!
- vₓvelocity projection at time t
Velocity depends linearly on time.
- x₀initial coordinate, in m
- xcoordinate at time t, in m
The coordinate equation of uniformly accelerated motion. The displacement is sₓ = x − x₀ = v₀ₓt + aₓt²/2; if the body does not turn back, this is also the distance.
- (v₀ₓ + vₓ) / 2(v₀ₓ + vₓ) / 2average velocity in uniformly accelerated motion
The average velocity is the mean of the initial and final velocities — only for uniformly accelerated motion!
- v₀, vinitial and final velocity, in m/s
- aacceleration (negative when braking), in m/s²
Another form: v² − v₀² = 2as. Braking distance: s = v₀² / (2|a|).
- sₙdistance covered in the n-th second by a body starting from rest, in m
- nnumber of the second
It comes from the difference sₙ = s(n) − s(n − 1).
Motion graphs
Open lesson- vₓvelocity projection, in m/s
- Δx = x₂ − x₁difference of the coordinates of two points on the graph, in m
- Δt = t₂ − t₁difference of their times, in s
The slope of the x–t graph is the velocity projection: the steeper the line, the greater the speed; a falling line means vₓ < 0.
- aₓacceleration projection, in m/s²
- Δvₓdifference of the velocities of two points on the vₓ–t graph, in m/s
The slope of the vₓ–t graph is the acceleration projection.
- sₓdisplacement projection, in m
- v₀ₓ, vₓvelocity at the start and end of the interval, in m/s
The area of the trapezium under vₓ–t. For uniform motion it is a rectangle: sₓ = vₓ · t. In the same way the rectangle under aₓ–t gives Δvₓ = aₓ · t.
- x₀initial coordinate, in m
- v₀ₓinitial velocity projection, in m/s
- aₓacceleration projection, in m/s²
The coordinate equation of uniformly accelerated motion; its graph is a parabola that opens downwards when aₓ < 0. The formula is explained in detail in the lesson «Acceleration and uniformly accelerated motion».
2Forces and Newton's lawsBeginner
Forces, inertia and interaction
Open lesson- F₁₂force exerted by object 1 on object 2
- F₂₁force exerted by object 2 on object 1
Two objects act on each other with forces that are equal in size and opposite in direction.
Newton's second law
Open lesson- Fnet force, in newtons (N)
- mmass, in kilograms (kg)
- aacceleration, in m/s²
From this, a = F / m and m = F / a.
Elastic force and friction
Open lesson- Felmagnitude of the elastic force, in N
- kstiffness (spring constant), in N/m — depends on the material, length and thickness
- Δl = |l − l₀|extension (or compression): the difference of the final and natural lengths, in m
Hooke’s law: for small elastic deformations the elastic force is proportional to the extension. In projection Fₓ = −k · x: the force opposes the deformation.
- kparstiffness in parallel: equal extensions, the forces add
- kserstiffness in series: equal force, the extensions add
Connecting springs. If you cut a spring into n equal parts, each part has stiffness n · k.
- Ffrsliding friction force (and the maximum static friction), in N
- μcoefficient of sliding friction — no unit; depends on the materials and finish of the surfaces, not on the contact area
- Nnormal (support) force, in N; on a horizontal surface with no other vertical forces N = mg
As a horizontal force F grows from 0, the Ffr(F) graph is first a 45° line (Ffr = F, the body is at rest) and then a horizontal line at μN (the body slides).
- tbbraking time, in s
- sbbraking distance, in m
- v₀speed when braking starts, in m/s
They follow from a = μg and the formulas of uniformly decelerated motion.
Gravity, weight and weightlessness
Open lesson- Fgravitational force, in N
- m₁, m₂masses of the bodies, in kg
- rdistance between the centres, in m
- Ggravitational constant, 6.67 · 10⁻¹¹ N · m² / kg²: the pull between two 1 kg bodies 1 m apart
- mmass of the body, in kg
- g₀free-fall acceleration at the Earth’s surface
- ghfree-fall acceleration at height h
- Rradius of the Earth (≈ 6400 km)
The force of gravity and how it depends on height.
- amagnitude of the lift’s acceleration, in m/s²
- ng-load: n > 1 — weight increased, n = 0 — weightlessness
- vspeed of the car, in m/s
- Rradius of curvature of the bridge, in m
When v = √(g · R), W = 0 at the top of a convex bridge — weightlessness.
Free fall and projectile motion
Open lesson- vvelocity at time t, in m/s
- hheight fallen in time t, in m
- gfree-fall acceleration, 10 m/s²
The formulas of free fall (v₀ = 0).
- v₀initial speed, in m/s
- vyvelocity projection: positive going up, negative coming down
- yheight above the launch point, in m
Equations of motion for a body thrown straight up.
- t₁rise time (from vy = 0)
- Hmaximum height
- Ttime to return to the launch level, T = 2t₁
Symmetry: the body comes back with speed v₀.
- v₀initial downward speed, in m/s
- hheight fallen, in m
- v₀horizontal launch speed, in m/s
- hlaunch height, in m
- Rrange, in m
Horizontal throw: the time of flight does not depend on v₀. The landing speed is v = √(v₀² + (gt)²).
- αlaunch angle (between the velocity and the horizontal)
- T, Htime of flight and maximum height
- Rrange (landing at the launch level)
The range is greatest at 45°; angles that add up to 90° (30° and 60°) give the same range.
3Pressure, energy and heatIntermediate
Pressure: solids, liquids and the atmosphere
Open lesson- ppressure, in pascals (Pa)
- Fforce acting perpendicular to the surface, in N
- Sarea of the surface, in m² (often written A in English books)
- ρdensity of the liquid, in kg/m³ (1000 kg/m³ for water)
- gacceleration due to gravity, ≈ 9.8 N/kg
- hdepth below the surface, in m
Pressure at a depth in a liquid (hydrostatic pressure)
Archimedes’ principle and floating
Open lesson- FAbuoyant force, in N
- ρldensity of the liquid (gas), in kg/m³ — not of the body!
- gfree-fall acceleration, ≈ 10 m/s² (N/kg)
- Vsubvolume of the submerged part of the body, in m³ (the whole volume if fully immersed)
FA does not depend on the body’s material, its shape, or how deep a fully immersed body is. 1 cm³ = 10⁻⁶ m³, 1 L = 10⁻³ m³.
- Pweight of the body in air (P = mg), in N
- Plweight in the liquid — the reading of a dynamometer holding the fully immersed body, in N
- ρbdensity of the body, in kg/m³
The second formula follows from the first: FA = P − Pl = ρl g V and P = ρb g V; dividing them cancels g and V.
- Vsub / VVsub / Vratio of the submerged volume to the whole volume
- ρb(average) density of the body
- ρldensity of the liquid
The buoyant force on a floating body always equals its weight and does not depend on the liquid’s density: in a denser liquid the body sinks less, in a less dense one more.
- Fliftlifting force — the largest weight of load the balloon can lift, in N
- ρairdensity of air (1.29 kg/m³ at 0 °C); V is the balloon’s volume
- ρgasdensity of the gas in the balloon: helium 0.18 kg/m³, hydrogen 0.09 kg/m³
- memass of the envelope (and basket), in kg
Rafts and boats are solved the same way: water instead of air, the body’s own material instead of the gas.
Work, energy and power
Open lesson- Fforce in the direction of motion, in N
- sdistance moved in the direction of the force, in m
W — work done, in joules (J)
- Ekkinetic energy — energy of motion, in J
- mmass, in kg
- vspeed, in m/s
- Eppotential energy of an object at height h above the ground, in J
- hheight, in m
- ttime taken, in s
P — power, in watts (W); W — work done, in J
Statics: moment of force, levers, pulleys, inclined plane
Open lesson- Mmoment of the force (torque), in N · m
- Fmagnitude of the force, in N
- darm of the force, in m; if the force acts at the end of a rod of length l at an angle α to the rod, d = l · sin α
A moment that turns the body anticlockwise is taken as positive, a clockwise one as negative (this is a convention).
- ΣFvector sum (resultant) of all forces acting on the body — the first condition
- ΣMalgebraic sum of the moments of all forces about any axis — the second condition
For a body in equilibrium you may take moments about any point. The most convenient one is where an unknown force acts: its arm is zero, so it drops out of the equation.
- F₁, F₂forces that try to turn the lever in opposite directions, in N
- d₁, d₂their arms, in m
Rule of moments: a lever is in equilibrium when the clockwise moments equal the anticlockwise moments. The forces are inversely proportional to their arms. If the lever’s own weight is given, it acts at the centre of gravity (the middle of a uniform lever).
- xccoordinate of the centre of gravity
- m₁, m₂masses of the bodies
- x₁, x₂coordinates of the bodies (of their centres of gravity)
This is the rule of moments itself: about the centre of gravity the moments of the gravity forces add up to zero, so the system balances when supported at this point.
- Fforce applied to the free end of the rope, in N
- Pweight of the load (together with the movable pulleys), in N
- nnumber of rope segments holding up the load: n = 1 for a fixed pulley, n = 2 for one movable pulley
- s, hdistances moved by the rope’s end and by the load, in m
Friction and the rope’s weight are neglected. A block and tackle (a system of pulleys) reduces the force n times, while the end of the rope travels n times farther.
- Fforce pulling the load steadily along the plane (no friction), in N
- l, hlength and height of the inclined plane, in m
- Pweight of the load, P = mg, in N
- αangle between the plane and the horizontal, sin α = h / l
The golden rule for an ideal (frictionless) inclined plane: the work F · l equals the work P · h needed to lift the load straight up. The longer (gentler) the plane, the smaller the force.
- ηefficiency
- Wuuseful work: Wu = P · h = mgh, in J
- Wintotal work: Win = F · s; s is the distance moved by the point where the force acts (l on an incline, 2h for a movable pulley), in J
Always η < 100%: the golden rule holds only for an ideal machine. For the same useful work, the lower the efficiency, the larger the force needed.
Heat and temperature
Open lesson- Ttemperature on the Kelvin scale, in K
- ttemperature on the Celsius scale, in °C
For example, 20 °C = 293 K; a temperature difference is the same on both scales.
- Qquantity of heat, in J
- cspecific heat capacity of the substance, in J/(kg · °C)
- mmass, in kg
ΔT — change in temperature (final − initial), in °C
4Electricity and magnetismIntermediate
Electric current and Ohm's law
Open lesson- Icurrent, in amperes (A)
- qcharge passing through the wire, in coulombs (C)
- ttime, in s
Current is measured with an ammeter, which is connected in series.
- Icurrent, in A
- Uvoltage (potential difference), in V — often written V in English books
- Rresistance, in Ω
From this, U = I · R and R = U / I.
Magnets, the magnetic field and electromagnets
Open lesson- μmagnetic permeability of the substance (no unit)
- Bmagnetic induction inside the substance
- B₀field of the same current in vacuum (without a core)
The permeability shows how many times a substance strengthens (or weakens) the field.
Ampère and Lorentz forces. The electric motor
Open lesson- Bmagnetic induction, T
- Fmaxforce on the wire when it is perpendicular to the field lines, N
- Icurrent, A
- llength of the part of the wire inside the field, m
1 T = 1 N / (A · m). The Earth’s field is about 5 · 10⁻⁵ T; a medical MRI scanner uses 1.5–3 T. B does not depend on the wire or the current: a larger current gives a larger Fmax, but B stays the same.
- FAAmpère force, N
- αangle between the direction of the current and the induction vector
At α = 90° the force is maximum (F = B · I · l); when the wire lies along the field lines (α = 0°) the force is zero.
- Mtorque on the frame, N · m
- Nnumber of turns
- Sarea of the frame, m²
- αangle between the normal to the frame and the induction vector
The torque is maximum when the plane of the frame is parallel to the field lines (α = 90°) and zero when it is perpendicular (α = 0°).
- FLLorentz force, N
- qcharge of the particle, C
- vspeed of the particle, m/s
- αangle between the velocity and the induction vector
The Lorentz force is always perpendicular to the velocity, so it does no work: it changes neither the particle’s speed nor its kinetic energy, only its direction of motion. Its direction is found with the left-hand rule: the four fingers point along the velocity of a positive particle, and against the velocity for a negative one (an electron).
- Rradius of the path (circle), m
- Tperiod of revolution, s
- mmass of the particle, kg
The period depends on neither the speed nor the radius: a faster particle draws a bigger circle but goes round it in the same time. Frequency ν = 1 / T = |q| · B / (2π · m).
- Uaccelerating voltage, V
- Rradius of the ion’s circle in the spectrograph, m
For ions of equal charge R ~ √m: an ion 4 times heavier moves on a circle of twice the radius.
5Waves, light and the atomAdvanced
Oscillations, waves and sound
Open lesson- Tperiod, in s
- nnumber of oscillations made in time t
f — frequency, in Hz
- llength of the pendulum, in m
- gacceleration due to gravity, in m/s²
- vwave speed, in m/s
- λwavelength, in m
Light: reflection, refraction and lenses
Open lesson- αangle of incidence (between the ray and the normal)
- βangle of reflection
- nrefractive index of the medium
- cspeed of light in a vacuum, ≈ 300 000 km/s
- vspeed of light in the medium
Water n ≈ 1.33, glass ≈ 1.5, diamond ≈ 2.42
P — lens power, in dioptres (D); f — focal length, in metres. For a diverging lens f and P are negative.
Atomic structure and radioactivity
Open lesson- N₀initial number of radioactive nuclei (or mass of the substance)
- Nnuclei remaining after time t
- nnumber of half-lives that have passed
6Upper school: mechanics and molecular physicsAdvanced
Momentum and collisions
Open lesson- pmomentum, in kg · m/s
- mmass, in kg
- vvelocity, in m/s
Momentum is a vector: it points in the same direction as the velocity.
- Faverage force, in N
- Δttime the force acts, in s
- v₁, v₂initial and final velocity (with sign), in m/s
Unit of impulse: N · s = kg · m/s
- v₁, v₂velocities before the interaction, in m/s
- v₁′, v₂′velocities after the interaction, in m/s
The total momentum of a closed system stays constant.
- vcommon velocity of the joined bodies, in m/s
Perfectly inelastic collision
- v₁velocity of the first body before the collision, in m/s
- v₁′, v₂′velocities after the collision, in m/s
Perfectly elastic head-on collision, second body initially at rest
Circular motion and gravitation
Open lesson- vlinear speed, in m/s
- Rradius of the circle, in m
- Tperiod, in s
- ωangular velocity, in rad/s
- ffrequency, in Hz (1/s)
- acentripetal acceleration, in m/s², pointing to the centre
The force that causes it is F = m · v² / R. It is not a new kind of force but the net force supplied by friction, tension, gravity and so on.
- Ggravitational constant, 6.67 · 10⁻¹¹ N · m²/kg²
- m₁, m₂masses of the bodies, in kg
- rdistance between the centres, in m
- Mmass of the planet, in kg
- rorbit radius (from the planet's centre), in m
- v₁first cosmic velocity for the Earth
- Torbital period, in s
- rorbit radius (semi-major axis for an ellipse), in m
For a circular orbit this follows from T = 2πr / v and v² = G · M / r.
Basics of molecular-kinetic theory
Open lesson- namount of substance, in mol
- mmass of the substance, in kg
- Mmolar mass, in kg/mol
- Nnumber of particles (molecules)
- NAAvogadro constant, 6.02 · 10²³ mol⁻¹
Amount of substance. It gives the number of molecules N = (m / M) · NA.
- m₀mass of one molecule, in kg
Mass of one molecule. The volume per molecule is V₀ = V / N, and the molecule’s size is estimated as d ≈ ∛V₀.
- ppressure of the gas, in Pa
- N/VN/Vnumber density, in m⁻³
- vroot-mean-square speed of the molecules, in m/s
- Ēmean translational kinetic energy of a molecule, Ē = m₀v²/2, in J
The basic equation of the kinetic theory of an ideal gas. Since (N/V) · m₀ = ρ, it can also be written p = (1/3) · ρ · v².
- kBoltzmann constant, 1.38 · 10⁻²³ J/K (k = R / NA)
- Tabsolute temperature, in K
The mean kinetic energy of a molecule of any ideal gas depends only on temperature. At the same p and T all gases have the same number density.
- vrms speed, in m/s
- Runiversal gas constant, 8.31 J/(mol · K)
The speed grows as √T and falls as √M: at the same temperature lighter molecules are faster.
- ttemperature in degrees Celsius, °C
- Tabsolute temperature, in K; ΔT = Δt
- tFtemperature in degrees Fahrenheit, °F
Links between the temperature scales. Backwards: t = (tF − 32) / 1.8.
The ideal-gas law and isoprocesses
Open lesson- ppressure, in Pa
- Vvolume, in m³ (1 L = 10⁻³ m³, 1 cm³ = 10⁻⁶ m³)
- namount of substance, in mol
- m, Mmass (kg) and molar mass (kg/mol) of the gas
- Runiversal gas constant, 8.31 J/(mol · K)
- Tabsolute temperature, in K
The Mendeleev–Clapeyron equation (ideal-gas law). It gives the density of a gas: ρ = m / V = p · M / (R · T).
- p₁, V₁, T₁initial state of the gas
- p₂, V₂, T₂final state of the gas (same mass)
Clapeyron’s equation (the combined gas law), m = const.
- T = constisothermal process: pressure is inversely proportional to volume
- p = constisobaric process: volume is directly proportional to absolute temperature
- V = constisochoric process: pressure is directly proportional to absolute temperature
The three isoprocess laws (m = const).
- ppressure of the mixture
- p₁, p₂, …partial pressures of the components: pᵢ = nᵢRT / V
Dalton’s law: the pressure of a mixture equals the sum of the partial pressures.
Thermodynamics
Open lesson- ΔUchange in internal energy of a monatomic ideal gas, in J
- namount of substance, in mol
- ΔTchange in temperature, in K
- Wwork done by the gas at constant pressure, in J
- ΔVchange in volume, in m³
The work is positive when the gas expands and negative when it is compressed. In any process it equals the area under the p–V graph.
- Qheat supplied to the gas, in J (Q < 0 if the gas gives off heat)
- ΔUchange in internal energy, in J
- Wwork done by the gas, in J
Heat given to a gas goes into raising its internal energy and into the work the gas does — this is conservation of energy.
- ηefficiency
- Q₁, Q₂heat taken from the hot reservoir and given to the cold one, in J
- T₁, T₂absolute temperatures of the hot and cold reservoirs, in K
ηmax is the efficiency of an ideal (Carnot) engine; no real engine working between the same temperatures can do better.
Saturated and unsaturated vapour. Air humidity
Open lesson- p(partial) pressure of the vapour, in Pa
- ρdensity of the vapour, in kg/m³
- Mmolar mass (0.018 kg/mol for water)
The Mendeleev–Clapeyron equation for a vapour; for saturated vapour p = ps, ρ = ρs. Boyle’s law cannot be applied to saturated vapour — its mass changes when it is compressed.
- φrelative humidity, %
- ρ, pdensity (absolute humidity) and partial pressure of the vapour in the air
- ρs, psdensity and pressure of saturated vapour at the same temperature
Relative humidity. A comfortable humidity for people is about 40–60 %.
Properties of solids and liquids
Open lesson- εstrain, the relative elongation (no unit, often in %)
- σstress, in Pa
- Scross-sectional area, in m² (1 mm² = 10⁻⁶ m²)
Strain and stress — the elastic force per unit cross-sectional area.
- EYoung’s modulus, in Pa: steel ≈ 2 · 10¹¹, copper ≈ 1.2 · 10¹¹, aluminium ≈ 7 · 10¹⁰, lead ≈ 1.6 · 10¹⁰
Hooke’s law: for small deformations stress is proportional to strain. E depends only on the material, not on the size of the rod.
- kstiffness of the rod (wire), in N/m
- l₀length of the undeformed rod, in m
Stiffness depends on the material, the cross-section and the length, not on the applied force.
- Eppotential energy of an elastically deformed body, in J
The area of the triangle under the F(Δl) graph. When the force is given, the form F² / (2k) is handiest.
- σcoefficient of surface tension, in N/m (= J/m²): water ≈ 0.073, soap solution ≈ 0.04, alcohol ≈ 0.022, mercury ≈ 0.49 (20 °C)
- llength of the boundary line of the surface, in m
The surface tension force. σ decreases as the temperature rises and when surfactants (soap) are added.
- hheight of rise (fall, for a non-wetting liquid) in a capillary, in m
- ρdensity of the liquid, in kg/m³
- rradius of the capillary, in m
For complete wetting: the surface tension force σ · 2πr holds up the weight of the column ρgπr²h. h is inversely proportional to the radius.
7Upper school: electrodynamicsAdvanced
Electric charge, Coulomb’s law and the electric field
Open lesson- qcharge of the body, C
- Nnumber of extra (or missing) electrons — a whole number
- eelementary charge, 1.6 · 10⁻¹⁹ C
Extra electrons mean a negative charge, missing electrons a positive one. Conservation of charge: in a closed system the algebraic sum of charges does not change: q₁ + q₂ + … = const.
- q₁, q₂charges before contact (with their signs)
- q₁′, q₂′charges after contact
Only for conducting balls of the same size and shape. Mind the signs: +8 and −2 → (8 − 2) / 2 = +3.
- Fforce of interaction, N
- k9 · 10⁹ N · m²/C² (k = 1 / (4π · ε₀))
- εrelative permittivity of the medium (1 for vacuum and air, 81 for water)
- rdistance between the charges, m
For point charges (bodies much smaller than the distance between them). By Newton’s third law F₁₂ = F₂₁ — even when the charges differ, they act on each other with the same force.
- Efield strength, N/C (= V/m)
- q₀test charge placed in the field, C
- qpoint charge creating the field, C
The field strength is a vector: it points away from a positive charge and towards a negative one. A charge q in the field feels F = q · E; the force on a negative charge (an electron) points opposite to E.
- E⃗₁, E⃗₂field strengths created by each charge alone
Along one line: vectors in the same direction add, opposite ones subtract. When they are perpendicular, E = √(E₁² + E₂²).
Electric potential and potential difference
Open lesson- Awork done by the field, J
- qcharge moved (with its sign), C
- Estrength of the uniform field, V/m
- dprojection of the displacement onto the direction of the field lines, m
- αangle between the displacement and the field lines
For a positive charge moving along the field lines A > 0, against them A < 0, perpendicular to them A = 0. For a negative charge (an electron) the signs are reversed.
- Wp₁, Wp₂potential energy of the charge at the start and at the end, J
- q₁, q₂point charges (with their signs), C
- k9 · 10⁹ N · m²/C²
- εrelative permittivity of the medium (1 for air)
- rdistance between the charges, m
When the field does positive work, the potential energy decreases. For like charges Wp > 0 (an external force must do work to bring them closer), for unlike charges Wp < 0. The zero level is at infinity.
- φpotential at the given point, V
- q₀charge brought into the field, C
- qpoint charge that creates the field (with its sign), C
- rdistance from the charge to the point, m
φ = 0 at infinity. In the field of a positive charge the potential is positive and grows towards the charge; in the field of a negative charge it is negative. φ ~ 1/r while E ~ 1/r²: when the distance doubles, the potential halves and the field strength drops 4 times. At the same point |φ| = E · r.
- φ₁, φ₂potential created by each charge alone (with its sign), V
- r₁, r₂distance from the point to the corresponding charge, m
The potential of a negative charge is taken as negative. Where the potential is zero the field strength need not be zero, and vice versa — see Example 4.
- Upotential difference (voltage) between points 1 and 2, V
- φ₁, φ₂potentials of the start and end points, V
- Awork of the field when the charge moves from 1 to 2, J
- qcharge moved (with its sign), C
1 V is the voltage between two points when the field does 1 J of work moving 1 C of charge. A positive charge released in a field moves from high to low potential, a negative charge (an electron) from low to high potential — in both cases the field does positive work.
- eVelectronvolt, a unit of energy
- eelementary charge, 1.6 · 10⁻¹⁹ C
A particle with charge e starting from rest gains U eV after passing through a voltage U: 100 V → 100 eV. An α-particle with charge 2e gains twice as much at the same voltage — 2U eV.
- Estrength of the uniform field, V/m
- Uvoltage between two points (for example, two plates), V
- ddistance between these points along the field lines, m
For a uniform field only. The field points in the direction in which the potential decreases. Using this formula in a capacitor is covered in the lesson «Capacitance and capacitors».
- qcharge of the sphere, C
- Rradius of the conducting sphere, m
- rdistance from the centre of the sphere to the point, m
For a charged conducting sphere in air. Outside the sphere the field is as if all the charge sat at the centre. Inside E = 0, and the potential is the same as on the surface. The field strength is greatest just outside the surface: E = k · q / R².
- εrelative permittivity (dielectric constant) of the substance, no unit
- E₀field strength the same charges create in a vacuum, V/m
- Efield strength in the dielectric, V/m
ε = 1 for a vacuum, ≈ 1 for air, ≈ 2 for kerosene and paraffin, ≈ 7 for glass, 81 for water. In a dielectric the field strength and potential of a point charge, and the force between charges, are ε times smaller than in a vacuum.
- |q|magnitude of the particle’s charge, C (e for an electron)
- Uaccelerating potential difference the particle passes through, V
- mmass of the particle, kg (electron 9.1 · 10⁻³¹ kg, proton 1.67 · 10⁻²⁷ kg)
- v₀, vinitial and final speed, m/s; the second formula is for v₀ = 0
The speed is proportional to √U: four times the voltage gives twice the speed and four times the kinetic energy. If the field slows the particle down, the voltage that stops it is U = m · v₀² / (2 · |q|).
- aacceleration perpendicular to the plates, m/s²
- Uvoltage between the plates, V
- ddistance between the plates, m
- llength of the plates, m
- v₀initial speed of the particle parallel to the plates, m/s
- ydeflection at the exit from the plates (displacement along the field), m
A particle entering midway between the plates misses them if y < d / 2. At the exit the velocity component perpendicular to the plates is a · t, and the deflection angle of the velocity is given by tan β = a · t / v₀.
Capacitance and capacitors
Open lesson- Ccapacitance, F (farad)
- qmagnitude of the charge on one plate, C
- Uvoltage (potential difference) between the plates, V
1 F = 1 C/V. The farad is a very large unit, so µF (10⁻⁶ F), nF (10⁻⁹ F) and pF (10⁻¹² F) are used. Capacitance depends neither on the charge nor on the voltage: when q grows, U grows by the same factor and the ratio stays the same.
- εrelative permittivity (dielectric constant) of the medium between the plates, no unit (1 for vacuum and air)
- ε₀electric constant, 8.85 · 10⁻¹² F/m
- Sarea of one plate, m²
- ddistance between the plates, m
The capacitance of a parallel-plate capacitor is directly proportional to the plate area and inversely proportional to the gap; it depends only on the geometry and the dielectric.
- Cparequivalent capacitance in parallel: same voltage, charges add
- Cserequivalent capacitance in series: same charge, voltages add
For two capacitors in series C = C₁ · C₂ / (C₁ + C₂) — “product over sum”.
- Wenergy of the capacitor (of its electric field), J
- qcharge of the capacitor, C
- Uvoltage between the plates, V
- Ccapacitance, F
The three forms are the same formula (substitute q = C · U). Which one to use depends on what stays constant: if U is constant, use C · U² / 2; if q is constant, use q² / (2C).
- Estrength of the uniform field between the plates, V/m
- ddistance between the plates, m
- wenergy density of the electric field, J/m³; the capacitor’s energy is W = w · S · d
The energy density grows as the square of the field strength: double the field and every cubic metre holds four times the energy.
Circuits: EMF, power and Kirchhoff's rules
Open lesson- ℰEMF of the source, in V
- Rexternal (load) resistance, in Ω
- rinternal resistance of the source, in Ω
- Uterminal voltage of the source, in V
Ohm's law for a complete circuit. With R = 0 you get the short-circuit current I = ℰ / r.
- Pelectrical power, in W
- Qheat produced in the conductor in time t, in J (Joule's law)
Electricity meters measure energy in kilowatt-hours: 1 kW · h = 3.6 · 10⁶ J.
Semiconductors and semiconductor devices
Open lesson- Rresistance of a metal conductor at t °C, Ω
- R₀resistance at 0 °C, Ω
- αtemperature coefficient of resistance, K⁻¹; for metals α > 0 (about 4 · 10⁻³ K⁻¹ for pure metals)
For metals the resistance grows linearly with temperature. The formula does not apply to semiconductors: their resistance falls sharply and non-linearly when heated.
- Icurrent in the circuit (ammeter reading), A
- Uconstant source voltage, V
- R, Rₜresistance of the fixed resistor and of the thermistor (photoresistor), Ω
- U₁, U₂readings of V₁ (across the resistor) and V₂ (across the thermistor), V
In a series circuit the voltage is shared in proportion to the resistances: U₂ / U₁ = Rₜ / R. The element whose resistance drops gets a smaller share of the voltage.
Electromagnetic induction
Open lesson- Φmagnetic flux, in webers (Wb)
- Bmagnetic flux density, in T
- Sarea of the loop, in m²
- αangle between B and the normal (perpendicular) to the surface
Magnetic flux measures “how many field lines” pass through the loop. Its unit is 1 Wb = 1 T · 1 m²; from Faraday’s law also 1 Wb = 1 V · s.
- ℰinduced EMF, in V
- Nnumber of turns in the coil
- ΔΦ / ΔtΔΦ / Δtrate of change of flux, in Wb/s
The minus sign expresses Lenz’s rule: the induced current creates a magnetic field that opposes the change in flux that caused it.
- qcharge passing through the loop, in C
- Nnumber of turns
- ΔΦchange in flux through one turn, in Wb
- Rresistance of the loop, in Ω
- Nenumber of electrons passing through the loop
- eelementary charge, 1.6 · 10⁻¹⁹ C
The charge does not depend on how fast the flux changes: push the magnet in quickly and the current is larger but lasts a shorter time — the same charge passes through the galvanometer. If Φ is given as the total flux through all the turns, N is not written separately: q = ΔΦ / R.
- llength of the moving conductor, in m
- vspeed of the conductor, in m/s
- αangle between v and B
Induced EMF in a conductor moving through a magnetic field. If the conductor moves along the field lines (α = 0), no EMF appears.
Self-induction. Inductance. Magnetic-field energy
Open lesson- Φmagnetic flux created by the circuit’s own current, in Wb (for a coil of N turns, the total flux through all turns)
- Linductance, in H (henry)
- Icurrent, in A
1 H is the inductance of a circuit in which a current of 1 A creates a flux of 1 Wb: 1 H = 1 Wb/A = 1 V·s/A = 1 Ω·s.
- μrelative permeability of the core (μ ≈ 1 for air, hundreds or thousands for iron)
- μ₀magnetic constant, 4π · 10⁻⁷ H/m
- Nnumber of turns
- Scross-sectional area of the coil, in m²
- llength of the coil, in m
For a long coil (solenoid). Inductance grows as the square of the number of turns, and an iron core increases it hundreds of times.
- ℰ_siself-induced EMF, in V
- Linductance of the coil, in H
- ΔI / ΔtΔI / Δtrate of change of the current, in A/s
The minus sign is Lenz’s rule: when the current grows (ΔI > 0) the EMF acts against the source, when it falls the EMF acts along the current. This gives a second definition: 1 H is the inductance of a circuit in which an EMF of 1 V appears when the current changes steadily by 1 A every second.
- WMenergy of the coil’s magnetic field, in J
- Linductance, in H
- Icurrent, in A
- Φmagnetic flux of the coil, in Wb
It looks like kinetic energy mv²/2: inductance plays the role of “electrical mass” and current the role of “velocity”. Its partner for a capacitor is WE = CU²/2 (see “Capacitance and capacitors”).
- wenergy density of the magnetic field, in J/m³
- Vvolume occupied by the field, in m³
- Bmagnetic flux density, in T
The energy density is proportional to B²: a field twice as strong holds 4 times more energy in every cubic metre.
Alternating current and the transformer
Open lesson- einstantaneous EMF, in V
- ℰ_mamplitude (peak value) of the EMF, in V
- N, B, Snumber of turns, flux density (T), area of the coil (m²)
- ωangular frequency, in rad/s: ω = 2πf = 2π / T
The voltage u = Um · sin ωt and the current i = Im · sin(ωt + φ) follow the same law (φ is the phase shift). The mains frequency in Azerbaijan is 50 Hz: T = 0.02 s, ω = 100π ≈ 314 rad/s; the current changes direction 100 times a second.
- I, U, ℰeffective values of current, voltage and EMF — what meters show
- Im, Um, ℰ_mamplitudes (peak values)
√2 ≈ 1.41, 1/√2 ≈ 0.71. The mains has U = 220 V, so Um = 220 · √2 ≈ 311 V.
- XLinductive reactance, in Ω
- XCcapacitive reactance, in Ω
- ffrequency, in Hz
- L, Cinductance (H) and capacitance (F)
As f grows, XL grows in proportion and XC falls in inverse proportion; R does not depend on frequency.
- Zimpedance (total resistance) of the circuit, in Ω
- U, Ieffective (or peak) values of voltage and current
With only a resistor Z = R, only a coil Z = XL, only a capacitor Z = XC. When XL = XC, Z = R is smallest and the current is largest — this is resonance (see “Electromagnetic oscillations and waves”).
- Paverage (active) power of the AC circuit, in W
- cos φpower factor; φ is the phase shift between current and voltage
Power is released only in the resistance. With only a resistor cos φ = 1 and P = U · I; for an ideal coil or capacitor cos φ = 0 and P = 0.
- kturns ratio (transformation ratio): k > 1 — step-down, k < 1 — step-up transformer
- U₁, N₁voltage and number of turns of the primary winding
- U₂, N₂voltage and number of turns of the secondary winding
A transformer works only with alternating current: direct current gives a constant flux, and no EMF appears in the secondary.
- ηefficiency of the transformer
- P₁power taken from the mains, in W
- P₂power delivered to the load, in W
Large transformers reach an efficiency of 99 %. In an ideal transformer (η = 1), U₁I₁ = U₂I₂, so I₁ / I₂ = N₂ / N₁: it lowers the current by the same factor as it raises the voltage.
- ΔPpower lost in the line, in W
- Ppower transmitted, in W
- Utransmission voltage, in V
- Rresistance of the line wires, in Ω
Raising the voltage n times cuts the loss n² times. That is why a step-up transformer raises the voltage at the power station and step-down transformers lower it again near the consumers.
Electromagnetic oscillations and waves
Open lesson- Wtotal energy of the circuit, in J
- q, iinstantaneous charge and current
- qm, Imamplitudes of charge and current
- C, Lcapacitance (F) and inductance (H)
In an ideal circuit (no resistance) the total energy is conserved. So the WM(WE) graph is the straight line WM = W − WE: it cuts the same length W off both axes. Since qm = C · Um, we can also write W = C · Um² / 2.
- Tnatural period of the circuit, in s
- fnatural frequency, in Hz
- ωangular frequency, in rad/s
- L, Cinductance (H) and capacitance (F)
Thomson’s formula: the period depends only on L and C, not on the amplitude of the charge. The charge changes as q = qm · cos ωt and the current as i = −Im · sin ωt; Im = ω · qm, Um = qm / C. The current reaches its maximum a quarter of a period after the charge.
- cspeed of light in a vacuum, ≈ 3 · 10⁸ m/s
- λwavelength, in m
- ffrequency, in Hz
- Tperiod, in s
When a wave passes into another medium its frequency stays the same, while its speed and wavelength change. The wavelength radiated (or received) by an LC circuit is λ = c · T = 2πc · √(L · C).
- Rdistance to the object, in m
- ttime for the pulse to travel to the object and back, in s
Radar is based on the reflection of radio waves. The radar sends short pulses; the next pulse must be sent only after the reflected signal has come back.
- Iintensity of the radiation (electromagnetic energy flux density), in W/m²
- Wenergy passing through area S in time Δt, in J
- Ppower of the radiation through the surface, in W
- rdistance from a point source, in m
Moving away from a point source, the energy spreads over a sphere of area 4πr²: twice the distance means a quarter of the intensity. The radiated intensity is proportional to the fourth power of the frequency — that is why radio needs high-frequency carrier waves.
8University physicsUniversity
Vectors and kinematics with calculus
Open lesson- rposition vector, in m
- vinstantaneous velocity vector, in m/s; tangent to the path
- aacceleration vector, in m/s²
In components: vₓ = dx/dt, ax = dvₓ/dt = d²x/dt², etc.; the speed is |v| = √(vₓ² + vy² + vz²).
- v₀, r₀initial velocity and position (at t = 0) — they fix the constants of integration
- τintegration variable, in s
- θlaunch angle above the horizontal
- v₀launch speed, in m/s
Trajectory equation: solve x = v₀ cos θ · t for t and substitute into y(t) — the result is a parabola.
- Lrange for landing at the launch height, in m
- Hmaximum height, in m
- Ttime of flight, in s
T comes from y(t) = 0, H from vy = 0, and L = vₓ · T.
- aτtangential acceleration — changes the speed, in m/s²
- annormal (centripetal) acceleration — changes the direction, in m/s²
Rotational dynamics
Open lesson- τtorque (a vector along the rotation axis), in N · m
- rposition vector from the axis to the point where the force acts, in m
- dlever arm — shortest distance from the axis to the line of action of the force, in m
- Icmoment of inertia about a parallel axis through the centre of mass, in kg · m²
- adistance between the two axes, in m
Parallel-axis (Steiner) theorem. Check: for the rod, mL²/12 + m(L/2)² = mL²/3 — the value in the table.
- Imoment of inertia, in kg · m²
- αangular acceleration, in rad/s²
- ωangular velocity, in rad/s
- Wwork done by a torque during rotation, in J
- Ppower, in W
- Erotational kinetic energy, in J
- Langular momentum, in kg · m²/s
If the external torque is zero, L = const: I₁ω₁ = I₂ω₂.
- kI / (mR²): sphere 2/5, cylinder 1/2, hoop 1; 0 for a block sliding without friction
- θangle of the slope
The answer depends on neither mass nor radius — only on the shape (k).
Oscillations and waves: the differential equations
Open lesson- ω₀natural angular frequency, in rad/s
- Aamplitude, in m
- φ₀initial phase, in rad
- kspring constant, in N/m
Velocity v = −Aω₀ sin(ω₀t + φ₀), acceleration a = −ω₀²x; the total energy E = kA²/2 is constant.
- βdamping coefficient, in s⁻¹
- ωangular frequency of the damped motion, in rad/s (slightly below ω₀)
- Qquality factor: the larger it is, the weaker the damping
- F₀amplitude of the driving force, in N
- ωangular frequency of the driving force, in rad/s
The maximum is at ωres = √(ω₀² − 2β²) ≈ ω₀; for weak damping Amax ≈ F₀ / (2mβω₀), which is Q times the static displacement.
- Ftension in the string, in N
- μlinear density (mass per unit length), in kg/m
- kwave number, k = 2π/λ, in rad/m
Maxwell's equations and electromagnetic waves
Open lesson- Qenctotal charge enclosed by the closed surface, in C
- ε₀electric constant, 8.85 · 10⁻¹² F/m
- Eelectric field (vector), in V/m
- dAsurface element — its size is the area, its direction the outward normal, in m²
I. Gauss's law: charges are the sources of the electric field.
- Bmagnetic field (vector), in T
- ∮ … dAintegral over any closed surface
II. Gauss's law for magnetism: there are no magnetic charges (monopoles); B field lines are closed.
- ΦBmagnetic flux through a surface bounded by the loop, in Wb
- dlelement of the closed loop (vector), in m; the left side is the EMF around the loop, in V
III. Faraday's law: a changing magnetic field creates a circulating electric field.
- μ₀magnetic constant, 4π · 10⁻⁷ H/m
- Iconduction current through the loop, in A
- ε₀ · dΦE / dtε₀ · dΦE / dtMaxwell's displacement current, in A
IV. Ampère–Maxwell law: currents and changing electric fields create a circulating magnetic field.
- cspeed of electromagnetic waves in vacuum — the speed of light
- E, Binstantaneous field values; E ⊥ B ⊥ direction of travel, in phase
Wave intensity: I = c · ε₀ · E₀² / 2 (W/m²).
Special relativity
Open lesson- γLorentz factor (γ ≥ 1)
- Δt₀proper time — the interval measured in the clock's own rest frame, in s
- L₀proper length — measured in the frame where the object is at rest, in m
Lengths contract only along the direction of motion; perpendicular dimensions are unchanged.
- x′, t′coordinates of an event in frame S′, which moves along x at speed v relative to S
- u′, uvelocity of a body in S′ and in S
For v ≪ c they reduce to the Galilean ones: x′ = x − vt, t′ = t, u = u′ + v.
- mmass of the body (rest mass — invariant), in kg
- Etotal energy, in J
- E₀rest energy, in J
Foundations of quantum physics
Open lesson- hPlanck constant, 6.63 · 10⁻³⁴ J · s
- ffrequency of the light, in Hz
- λwavelength, in m
In atomic physics energy is measured in electronvolts: 1 eV = 1.6 · 10⁻¹⁹ J.
- Awork function of the metal, in eV or J
- U₀stopping voltage — the voltage that stops the photocurrent, in V
- f₀threshold frequency, in Hz
- λde Broglie wavelength, in m
- Δx, Δpuncertainties in position and momentum
- ħreduced Planck constant, ≈ 1.055 · 10⁻³⁴ J · s
- ψwave function; |ψ|² is the probability density
- U(x)potential energy, in J
- nquantum number, n = 1, 2, 3, …
- Lwidth of the well, in m
- Eₙenergy of level n in hydrogen (negative — the electron is bound)
- Em, Enenergies of the upper and lower levels in the transition
Each element emits only photons matching differences between its own levels — its spectral “fingerprint”.
Nuclear and particle physics
Open lesson- Z, Nnumbers of protons and neutrons (A = Z + N)
- mp, mnproton and neutron masses: 1.007276 u and 1.008665 u
- Ebbinding energy; Eb / A is the binding energy per nucleon
- λdecay constant, in s⁻¹
- Thalf-life
- Aactivity — decays per second, in becquerels (Bq)
Mean lifetime τ = 1/λ = T / ln 2 ≈ 1.44 T.
- Qenergy released by the reaction; Q > 0 means energy is given out
In a reaction the totals of charge number (Z) and mass number (A) are conserved.