IGCSE Physics Notes

Examination Year: 2025–2027
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igcse Space physics

Cambridge IGCSE Physics
Syllabus: 2025–2027

6.1.1 The Earth

Basic Facts about Earth

The Earth is a planet that rotates on its axis.

  • The axis of the Earth is tilted at an angle of about 66° to its orbital plane.
  • The Earth completes one full rotation in approximately 24 hours.
  • This rotation causes the cycle of day and night.

Explanation of Day and Night

  • The Earth rotates from west to east on its axis once every 24 hours.
  • The side of the Earth facing the Sun experiences day, while the side facing away experiences night.
  • As Earth continues to rotate, the same regions alternately move into and out of sunlight.

The imaginary boundary separating the lighted part of the Earth from the dark side is called the circle of illumination.

Revolution of the Earth and Seasons

The Earth orbits the Sun once every 365 days. This revolution, combined with the tilt of its axis, causes the periodic cycle of the seasons.

  • As the Earth orbits the Sun, each hemisphere alternately tilts toward or away from the Sun.
  • The hemisphere tilted toward the Sun experiences summer (direct solar energy).
  • The hemisphere tilted away experiences winter (indirect solar energy).
  • Countries near the equator remain hotter throughout the year.

The average orbital speed of Earth is given by:

v = 2πr / T

  • where r = average orbital radius, and T = orbital period (1 year).

Variation in Earth's Tilt and Its Effects

  • The Earth's axis tilt slowly shifts between 22° and 25° over about 41,000 years.
  • Greater tilt → more extreme seasons (hotter summers, colder winters).
  • Smaller tilt → milder seasons (warmer winters, cooler summers).

The Moon and Its Motion

The Moon orbits the Earth in about one month. This causes the periodic nature of the phases of the Moon.

PhaseDescription
New Moon The Moon is between the Earth and Sun; the unlit side faces Earth. Not visible.
Waxing Crescent A thin crescent of the Moon becomes visible and increases in size (“waxes”).
First Quarter Half of the Moon’s lit portion is visible; occurs about a week after New Moon.
Waxing Gibbous More than half of the Moon’s visible surface is lit and continues increasing.
Full Moon The Moon is on the opposite side of Earth from the Sun; the full lit face is visible.
Waning Gibbous More than half the Moon is lit, but the illuminated area decreases (“wanes”).
Third Quarter Half of the lit portion is visible again after the waning gibbous phase.
Waning Crescent Less than half the Moon’s face is illuminated before returning to New Moon.

Key Astronomical Facts

  • The circle of illumination separates day and night on Earth.
  • One complete rotation gives day and night.
  • One complete revolution gives the cycle of seasons.
  • The axial tilt affects the amount of solar radiation received by each hemisphere.

Exam Focus

  • Explain why Earth experiences day and night — due to its rotation on a tilted axis.
  • Explain how seasons are caused by the tilt and revolution of Earth around the Sun.
  • List the main phases of the Moon in correct order.
  • Be able to define rotation, revolution, and circle of illumination.

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6.1.2 The Solar System

Composition of the Solar System

The Solar System consists of a variety of celestial bodies that orbit a central star — the Sun.

  • One star — the Sun.
  • Eight planets — Mercury, Venus, Earth, Mars, Jupiter, Saturn, Uranus, and Neptune.
  • Asteroids in the asteroid belt.
  • Dwarf planets such as Pluto.
  • Moons orbiting the planets.
  • Comets and other smaller Solar System bodies.

The orbits of planets and minor bodies are generally elliptical. The Sun lies at one focus of each ellipse.

Planetary Data and Observations

PropertyExample Observation
Distance from the SunMercury is closest (58 million km); Neptune is farthest (4490 million km).
Time for One OrbitMercury completes one orbit in 0.24 years; Neptune takes 164.8 years.
Diameter at EquatorJupiter has the largest (142,980 km); Mars has the smallest (6,790 km).
MassMercury is least massive (0.06 Earth masses); Jupiter is most massive (318 Earth masses).
Gravitational Field StrengthMercury and Mars: 3.8 N/kg; Neptune: 13.8 N/kg (highest).
DensitySaturn: least dense (0.7 g/cm³); Mercury: most dense (5.4 g/cm³).
Surface TemperatureVenus: hottest (460°C); Neptune: coldest (−200°C).
Number of MoonsMercury and Venus: none; Saturn: most (82).

Planet Types

  • The four planets nearest the Sun (Mercury, Venus, Earth, Mars) are rocky and small — the terrestrial planets.
  • The four outer planets (Jupiter, Saturn, Uranus, Neptune) are large and gaseous — the gas giants.

The Accretion Model of Solar System Formation

The accretion model explains how the Solar System formed from a rotating cloud of gas and dust approximately 4.6 billion years ago.

  • The Solar System began as a solar nebula.
  • Gravity pulled the material together, causing the nebula to spin and flatten into a rotating accretion disc.
  • The Sun formed at the centre, while the remaining material clumped to form planetesimals and protoplanets.
  • Closer to the Sun, only heavy, rocky materials condensed — forming the terrestrial planets.
  • Farther away, lighter gases like hydrogen and helium condensed — forming the gas giants.
  • Collisions outside Mars' orbit created the asteroid belt.

Gravitational Field Strength and Orbits

  • Gravitational field strength depends on a planet’s mass and decreases with distance from its centre.
  • The Sun’s gravitational field keeps planets in orbit.
  • Planets travel fastest when closest to the Sun because their kinetic energy is highest and their gravitational potential energy is lowest.
  • Total energy is conserved: KE + PE = constant.

Light Travel Time Example

Example: Calculate the time for light to travel from the Moon to Earth.

Distance between Earth and Moon = 240,000 miles
Speed of light = 186,000 miles/s

Time = Distance / Speed = 240,000 ÷ 186,000 = 1.3 s

Key Concepts to Remember

  • Planets orbit the Sun due to the Sun’s gravitational attraction.
  • Inner planets are rocky; outer planets are gaseous.
  • Orbits are elliptical, not perfectly circular.
  • Accretion theory explains how cosmic dust gathered to form planets.
  • Gravitational field strength and orbital speed both decrease with distance from the Sun.
  • Energy in an orbiting system remains constant (KE + PE = constant).

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6.2.2 Stars

What Is a Star?

A star is a huge, self-luminous sphere of hot gas that shines due to nuclear fusion. Our Sun is one such star in the Milky Way.

  • Galaxies are made of billions of stars.
  • Other stars in the Milky Way are far more distant from Earth than the Sun.
  • Astronomical distances are often measured in light-years (1 ly ≈ 9.5 × 1015 m).

Birth of a Star

  • Interstellar clouds (nebulae), mainly hydrogen, begin to collapse under gravity.
  • Collapsing clumps heat up by gravitational energy → a protostar forms.
  • A star becomes stable when inward gravitational pull balances outward gas pressure from a hot core (hydrostatic equilibrium).
  • At core temperatures > ~10 million K, hydrogen fuses to helium → the star enters the main sequence.

Old Age — Giants and Supergiants

  • When core hydrogen is mostly used up, stars leave the main sequence.
  • Lower-mass stars (up to ~1.5× Sun) expand into red giants.
  • More massive stars (≈1.5–>3× Sun and above) become red supergiants.
  • In this phase, fusion shifts to shells around the core (hydrogen-shell fusion).

Stellar “Endings” and Remnants

Initial Star TypeEnd of LifeRemnantNotes
Sun-like / lower-mass Sheds outer layers → planetary nebula white dwarf White dwarf cools over time toward a black dwarf (very long timescales).
High-mass (supergiant) supernova neutron star or black hole Supernova spreads heavy elements; debris may seed new stars and planets.

Why Stars Stay Stable (for a Time)

Stability in the main sequence is the balance of inward gravity and outward pressure from fusion-heated gas — a state called hydrostatic equilibrium. As fuel is depleted, this balance changes, driving the later life stages.

Key Takeaways

  • Stars form from collapsing hydrogen-rich nebulae; fusion “turns them on”.
  • Main sequence = hydrogen-to-helium fusion in the core; stability via hydrostatic equilibrium.
  • Fate depends on mass: giants → planetary nebula + white dwarf; supergiants → supernova → neutron star / black hole.
  • 1 light-year is a distance unit (≈ 9.5 × 1015 m), not a time unit.

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6.2.1 The Sun as a Star

What is the Sun?

The Sun is a star of medium size, composed mainly of hydrogen and helium.

Where the Sun’s Energy Appears

  • The Sun radiates most of its energy in the infrared, visible, and ultraviolet regions of the electromagnetic spectrum.

Key Terms (Quick Reminders)

TermMeaning
StarSelf-luminous sphere of hot gas powered by nuclear processes.
Hydrogen / HeliumMain elements in the Sun’s composition.
Infrared (IR)EM radiation beyond red; carries heat.
Visible lightEM band seen by the human eye.
Ultraviolet (UV)EM band beyond violet; higher energy than visible.
Electromagnetic spectrumContinuous range of EM waves from radio to gamma.

Exam Pointers

  • Identify the Sun as a medium-sized star made mostly of hydrogen and helium.
  • State that most emission is in the IR, visible, and UV bands.
  • Use correct terminology for the electromagnetic spectrum regions.

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