Know that the strength of the gravitational field (a) at the surface of a planet depends on the mass of the planet (b) around a planet decreases as the distance from the planet increases

IGCSE Physics 0625 – Complete Syllabus Notes (2026‑2028)

Learning Objectives (All Assessment Objectives)

  • AO1 – Knowledge & Understanding: Define terms, state laws and formulae, and explain concepts across all syllabus areas.
  • AO2 – Application: Use equations and principles to solve quantitative problems, predict outcomes and interpret data.
  • AO3 – Practical Skills: Plan, carry out and evaluate investigations; analyse uncertainties; apply safety procedures.

Contents Overview

  1. Motion, Forces & Energy
  2. Thermal Physics
  3. Waves
  4. Electricity & Magnetism
  5. Nuclear Physics
  6. Space Physics
  7. Practical Skills & Experiment Ideas
  8. Summary Checklists & Quick Reference


1. Motion, Forces & Energy

Key Concepts & Formulae

  • Scalars & Vectors: Scalars have magnitude only (e.g. speed, mass). Vectors have magnitude + direction (e.g. velocity, force). Use component method or right‑angle triangle for addition.
  • Distance, Displacement, Speed, Velocity, Acceleration

    • v = s/t, a = Δv/Δt
    • Equations of motion (constant acceleration):

      • v = u + at
      • s = ut + ½at²
      • v² = u² + 2as

  • Graphs: distance‑time, speed‑time, velocity‑time. Gradient = speed (or acceleration for v‑t); area under v‑t = displacement.
  • Forces

    • Weight: W = mg
    • Normal reaction, tension, spring force F = kx (Hooke’s law, limit of proportionality)
    • Friction:

      • Static: F ≤ μₛN
      • Kinetic: F = μₖN
      • Fluid drag (approx. F = ½ CρAv² for high speeds)

    • Resultant force: vector sum of all forces (use components or right‑angle method).
    • Torque (moment of a force): τ = Fr sinθ. Rotational equilibrium when Στ = 0.
    • Centre of gravity: point where weight can be considered to act; for uniform objects it coincides with the geometric centre.

  • Circular Motion

    • Centripetal force: F_c = mv²/r = mω²r
    • Required for any object moving in a circle; provided by tension, friction, gravity, etc.

  • Momentum & Impulse

    • Momentum: p = mv
    • Impulse: I = FΔt = Δp
    • Conservation of momentum for isolated systems.

  • Work, Energy & Power

    • Work: W = F·s cosθ (J)
    • Kinetic energy: E_k = ½mv²
    • Gravitational potential energy: E_p = mgh
    • Elastic potential energy (spring): E_s = ½kx²
    • Conservation of energy (isolated system).
    • Power: P = W/t = Fv = ΔE/Δt (W)
    • Efficiency: η = (useful energy output / total energy input) × 100 %

  • Load‑Extension Graphs

    • Linear region obeys Hooke’s law; slope = spring constant k.
    • Beyond the limit of proportionality the graph curves, indicating permanent deformation.

Worked Example (Net Force)

A 2 kg cart accelerates from rest to 5 m s⁻¹ in 4 s. Find the net force.

  1. Acceleration: a = Δv/Δt = 5/4 = 1.25 m s⁻²
  2. Force: F = ma = 2 × 1.25 = 2.5 N

Worked Example (Torque)

A force of 30 N is applied at the end of a 0.5 m wrench making a 90° angle with the wrench. Calculate the torque.

τ = Fr sinθ = 30 × 0.5 × sin90° = 15 N·m

AO Mapping (Motion, Forces & Energy)

Sub‑topicAO1AO2AO3
Kinematics (graphs, equations)✓ (graph analysis)
Forces (weight, normal, tension, friction, drag)✓ (force‑plate, air‑track)
Torque & centre of gravity✓ (lever‑balance experiment)
Circular motion & centripetal force✓ (rotating platform)
Momentum & impulse✓ (collision carts)
Work, energy, power, efficiency✓ (energy‑conservation lab)
Load‑extension & spring constant✓ (spring‑stretch experiment)


2. Thermal Physics

Fundamental Concepts

  • Particle Model: Matter consists of particles in constant motion; temperature ↔ average kinetic energy.
  • Specific Heat Capacity: Q = mcΔT
  • Latent Heat: Q = mL (fusion = Lf, vaporisation = Lv)
  • Thermal Expansion

    • Linear: ΔL = αL₀ΔT
    • Volumetric: ΔV = βV₀ΔT (β ≈ 3α for solids)

Heat Transfer – Quantitative Relationships

  • Conduction (Fourier’s law):

    \[

    Q = \frac{kA}{L}\,(ΔT)

    \]

    where k = thermal conductivity (W m⁻¹ K⁻¹), A = cross‑sectional area, L = thickness.

  • Convection (density‑driven flow):

    \[

    Q = hAΔT

    \]

    h = convection heat‑transfer coefficient (depends on fluid velocity, viscosity, surface roughness).

  • Radiation (Stefan‑Boltzmann law):

    \[

    Q = εσAT^{4}

    \]

    ε = emissivity (0–1), σ = 5.67×10⁻⁸ W m⁻² K⁻⁴, T in kelvin.

Molecular‑Level Insight

  • In metals, free electrons transfer kinetic energy rapidly → high k.
  • In gases, energy is transferred by collisions; k is low, so conduction is weak.
  • Radiation is emission of electromagnetic waves; all bodies emit, intensity ∝ T⁴.

Worked Example – Conduction

Calculate the heat flow through a 0.02 m thick copper plate (k = 400 W m⁻¹ K⁻¹) of area 0.5 m² when the temperature difference between its faces is 30 K.

\[

Q = \frac{kA}{L}ΔT = \frac{400×0.5}{0.02}×30 = 300\,000\ \text{W}

\]

Worked Example – Radiation

A blackbody sphere (ε = 1) has a surface temperature of 500 K and a radius of 0.1 m. Find the radiated power.

\[

A = 4πr^{2}=4π(0.1)^{2}=0.126 \text{m}^{2}

\]

\[

Q = εσAT^{4}=1×5.67×10^{-8}×0.126×(500)^{4}\approx 89 \text{W}

\]

Energy‑Balance Example – Earth’s Climate (Optional Extension)

Assume the Earth receives an average solar flux of 1360 W m⁻², but only a quarter is absorbed due to albedo. Using the Stefan‑Boltzmann law, estimate the equilibrium temperature (ignore atmosphere).

\[

\frac{1360}{4}=σT^{4}\;\Rightarrow\;T=(\frac{340}{5.67×10^{-8}})^{1/4}\approx 255 \text{K}

\]

AO Mapping (Thermal Physics)

Sub‑topicAO1AO2AO3
Specific heat & latent heat✓ (calorimetry)
Thermal expansion✓ (metal‑rod experiment)
Conduction (Fourier’s law)✓ (heat‑flow apparatus)
Convection (h‑coefficient)✓ (water‑flow tank)
Radiation (Stefan‑Boltzmann)✓ (black‑body furnace)
Molecular explanation of heat transfer✓ (discussion / simulation)
Energy‑balance (climate) – extension✓ (project work)


3. Waves

Fundamental Properties

  • Wave Types: Transverse (e.g., light) vs. longitudinal (e.g., sound).
  • Speed–Frequency–Wavelength: v = fλ.
  • Reflection & Refraction: Angle of incidence = angle of reflection; Snell’s law n₁sinθ₁ = n₂sinθ₂.
  • Diffraction & Interference: Huygens’ principle; constructive when path difference = nλ, destructive when = (n + ½)λ.

Light

  • Ray optics – mirrors (concave, convex) and lenses (converging, diverging).
  • Lens formula: \(\frac{1}{f} = \frac{1}{v} + \frac{1}{u}\).
  • Dispersion → formation of a spectrum.
  • Optical instruments (microscope, telescope) – magnification formulas.

Sound

  • Production (vibrating source) → longitudinal wave.
  • Speed depends on medium (air ≈ 340 m s⁻¹, water ≈ 1500 m s⁻¹, steel ≈ 5000 m s⁻¹).
  • Pitch ↔ frequency; loudness ↔ amplitude/intensity.
  • Ultrasound applications: medical imaging, non‑destructive testing.

Worked Example – Wavelength

A sound wave has a frequency of 500 Hz and travels in air at 340 m s⁻¹. Find its wavelength.

λ = v/f = 340/500 = 0.68 m.

AO Mapping (Waves)

Sub‑topicAO1AO2AO3
Wave speed & v = fλ✓ (wave‑tank)
Reflection & refraction✓ (laser‑ray box)
Diffraction & interference✓ (single‑slit, double‑slit)
Optical instruments✓ (lens‑bench)
Sound properties & applications✓ (ultrasound lab)


4. Electricity & Magnetism

Electricity Basics

  • Charge q (C), current I = Δq/Δt (A).
  • Potential difference V (V), resistance R (Ω), Ohm’s law V = IR.
  • Power: P = VI = I²R = V²/R (W).
  • Series circuits: ΣR, same I, V splits.
  • Parallel circuits: 1/ΣR, same V, I splits.
  • Energy transferred: W = VIt = Pt (J).

Magnetism & Electromagnetism

  • Magnetic field lines; Earth’s magnetic field (horizontal component ≈ 25 µT).
  • Force on a moving charge: F = qvB sinθ.
  • Force on a current‑carrying conductor: F = BIL sinθ.
  • Electromagnetic induction:

    • Faraday’s law: induced emf = –ΔΦ/Δt.
    • Lenz’s law: direction opposes the change producing it.

  • Transformers: \(Vs/Vp = Ns/Np\); \(Is/Ip = Np/Ns\).
  • Generators & motors – principle of rotating a coil in a magnetic field.

Worked Example – Circuit Resistance

Find the total resistance of a 4 Ω resistor in series with a parallel combination of 6 Ω and 12 Ω.

Parallel part: \(1/Rp = 1/6 + 1/12 = 3/12 ⇒ Rp = 4 Ω\).

Total \(R = 4 Ω + 4 Ω = 8 Ω\).

AO Mapping (Electricity & Magnetism)

Sub‑topicAO1AO2AO3
Current, voltage, resistance✓ (circuit‑building)
Series & parallel rules✓ (design a circuit)
Power & energy✓ (energy‑meter test)
Magnetic fields & forces✓ (magnet‑force experiment)
Electromagnetic induction✓ (moving‑magnet coil)
Transformers✓ (ratio experiment)


5. Nuclear Physics

Atomic Structure

  • Protons, neutrons, electrons; atomic number Z, mass number A.
  • Isotopes – same Z, different A.
  • Stable vs. unstable nuclei; binding energy concept (qualitative).

Radioactivity

  • α‑particles (He²⁺, +2 e, low penetration), β‑particles (electrons, moderate penetration), γ‑rays (photons, high penetration).
  • Half‑life and decay constant λ:

    \[

    N = N0 e^{-λt},\qquad t{½} = \frac{\ln2}{λ}

    \]

  • Activity A = λN (Bq).
  • Applications: medical imaging (PET, radiotherapy), carbon dating, smoke detectors.

Safety & Protection

  • Time‑distance‑shielding principle.
  • Shielding materials: α → paper, β → aluminium, γ → lead or concrete.
  • ALARA – keep exposure “as low as reasonably achievable”.

Worked Example – Half‑Life

A 80 g sample has a half‑life of 5 years. How much remains after 15 years?

Number of half‑lives = 15/5 = 3.

Remaining mass = 80 × (½)³ = 80 × 0.125 = 10 g.

AO Mapping (Nuclear Physics)

Sub‑topicAO1AO2AO3
Atomic structure & isotopes✓ (model‑building)
Radioactive decay & half‑life✓ (decay‑counter)
Radiation types & shielding✓ (shielding test)
Applications of nuclear physics✓ (research project)
Safety (ALARA)✓ (risk‑assessment)


6. Space Physics

6.1 Gravitational Field Strength

  • Definition: Gravitational field strength (g) = force per unit mass, g = F/m (units m s⁻²).
  • Surface gravity of a spherical planet:

    \[

    g_{\text{surface}} = \frac{GM}{R^{2}}

    \]

    where G = 6.67×10⁻¹¹ N m² kg⁻², M = planetary mass, R = radius.

  • Dependence on mass: For planets of similar size, a larger mass directly increases g. If radius also changes, the effect is governed by the ratio M/R².
  • Inverse‑square law for any point outside the planet:

    \[

    g(r) = \frac{GM}{r^{2}} = g_{0}\left(\frac{R}{r}\right)^{2}

    \]

    where r = distance from the planet’s centre.

  • Effect of distance: Doubling the distance reduces g to one‑quarter; tripling reduces it to one‑ninth, etc.

Worked Example – Height Above Earth

Find the gravitational field strength 400 km above Earth’s surface.

  • Given: g₀ = 9.81 m s⁻², R = 6.37×10⁶ m, h = 4.0×10⁵ m.
  • r = R + h = 6.77×10⁶ m
  • \[

    g = g_{0}\left(\frac{R}{R+h}\right)^{2}

    = 9.81\left(\frac{6.37×10^{6}}{6.77×10^{6}}\right)^{2}

    \approx 8.7\ \text{m s}^{-2}

    \]

6.2 Earth’s Rotation & Orbit

  • Rotation period = 24 h → apparent daily motion, Coriolis effect on moving objects.
  • Orbit period = 365.25 days; axial tilt = 23.5° gives seasons.
  • Escape velocity:

    \[

    v_{\text{esc}} = \sqrt{\frac{2GM}{R}}

    \]

    (≈ 11.2 km s⁻¹ for Earth).

6.3 Additional Space Topics (Extended)

  • Kepler’s Laws (qualitative) – elliptical orbits, equal areas in equal times, period‑radius relationship.
  • Satellite motion – balance of gravitational force and centripetal force:

    \[

    \frac{GMm}{r^{2}} = \frac{mv^{2}}{r}

    \]

    leading to \(v = \sqrt{GM/r}\).

  • Energy in orbital motion – total mechanical energy \(E = -\frac{GMm}{2r}\).

AO Mapping (Space Physics)

Sub‑topicAO1AO2AO3
Gravitational field strength (surface & distance)✓ (gravity‑probe experiment)
Mass‑radius relationship for planets✓ (model‑planet comparison)
Earth’s rotation & Coriolis effect✓ (deflection of falling objects)
Orbit, seasons & axial tilt✓ (solar‑angle investigation)
Escape velocity & satellite motion✓ (launch‑simulation)
Kepler’s laws & orbital energy (extension)✓ (planet‑model activity)


7. Practical Skills & Experiment Ideas

  • Design and analyse a force‑plate experiment to determine the coefficient of static friction for different surfaces.
  • Investigate torque using a lever and varying load distances – verify τ = Fr sinθ.
  • Measure spring constant from load‑extension graphs; identify the limit of proportionality.
  • Quantify conduction through metal, wood and plastic rods using a heat‑flow apparatus; calculate thermal conductivity k.
  • Determine convection coefficient by heating water in a beaker with and without stirring; use Q = hAΔT.
  • Use a black‑body furnace and a thermopile to verify the Stefan‑Boltzmann law.
  • Set up a simple pendulum to explore circular motion and centripetal force concepts.
  • Carry out a radioactive decay measurement with a Geiger‑Müller tube; plot activity versus time and extract half‑life.
  • Build a small satellite model (mass on string) to demonstrate balance of gravitational and centripetal forces.
  • Perform a laser‑diffraction experiment to observe interference patterns and calculate wavelength.

Data‑handling & Uncertainty

  • Use percentage uncertainty: \(\%Δ = (Δx/x)×100\).
  • Propagation of uncertainties for multiplication/division: add percentage uncertainties.
  • Graphical determination of gradients (e.g., g from a falling‑ball distance‑time graph).


8. Summary Checklists & Quick Reference

Motion, Forces & Energy – Quick Formulas

QuantityFormula
WeightW = mg
Spring forceF = kx
Friction (static)F ≤ μₛN
Friction (kinetic)F = μₖN
Torqueτ = Fr sinθ
Centripetal forceF_c = mv²/r
Momentump = mv
ImpulseI = FΔt = Δp
WorkW = F s cosθ
Kinetic energyE_k = ½mv²
Gravitational PEE_p = mgh
Elastic PEE_s = ½kx²
PowerP = Fv = VI
Efficiencyη = (output / input) × 100 %

Thermal Physics – Quick Formulas

QuantityFormula
Specific heatQ = mcΔT
Latent heatQ = mL
Linear expansionΔL = αL₀ΔT
Volumetric expansionΔV = βV₀ΔT
ConductionQ = (kA/L)ΔT
ConvectionQ = hAΔT
RadiationQ = εσAT⁴

Space Physics – Quick Formulas

QuantityFormula
Surface gravityg = GM/R²
Gravity at distance rg(r) = GM/r² = g₀(R/r)²
Escape velocityvₑₛc = √(2GM/R)
Orbital speedv = √(GM/r)
Orbital energyE = ‑GMm/(2r)

AO Checklist – What to Remember for the Exam

  • Identify which formula applies (e.g., choose between kinetic and potential energy).
  • Check units and convert where necessary (e.g., km → m, °C → K).
  • State assumptions clearly (e.g., neglect air resistance, treat planet as a perfect sphere).
  • Show all steps – marks are awarded for method as well as final answer.
  • For practical questions, include a brief description of the set‑up, variables measured, and how uncertainties are evaluated.