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Flashcards · 9630 · A Level Topic 7
Gravitational fields and satellites (A Level) flashcards
19 cards on A Level Topic 7, subtopics 3.7.1 to 3.7.4. Pick a subtopic or study them all.
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3.7.1 Newton's gravitational law
- Newton's law of gravitation
- Two point masses attract each other with a force proportional to the product of their masses and inversely proportional to the square of their separation: F = Gm₁m₂/r².
- Value and unit of the gravitational constant G
- G = 6.67 × 10⁻¹¹ N m² kg⁻² (use the value given in the question).
- The distance between two masses is tripled. What happens to the gravitational force?
- F ∝ 1/r², so it falls to (1/3)² = 1/9 of its original value.
- In F = Gm₁m₂/r² for a satellite, what is r?
- The distance between the centres of mass: planet radius + height above the surface (r = R + h).
3.7.2 Gravitational field strength
- Gravitational field strength g
- The force per unit mass acting on a small mass placed at that point in the field: g = F/m. Unit N kg⁻¹ (equivalent to m s⁻²).
- Field strength in a radial field
- g = GM/r², where M is the mass creating the field and r the distance from its centre.
- Derive g = GM/r²
- Force on a small mass m: F = GMm/r². Field strength g = F/m = GM/r²; the test mass cancels.
- Field lines around a planet and near its surface
- Around the planet: radial, pointing inwards, spreading out as the field weakens. In a small region near the surface: parallel and equally spaced (approximately uniform).
- G vs g
- G is a universal constant, the same everywhere. g is a field strength that depends on the source mass and the position.
3.7.3 Gravitational potential
- Gravitational potential V
- The work done per unit mass by an external agent in moving a small mass from infinity to the point. Zero at infinity, so negative everywhere else. Unit J kg⁻¹.
- Potential in a radial field, and work done moving a mass
- V = −GM/r. ΔW = mΔV, where ΔV = V(final) − V(initial).
- Equipotential surface (gravitational)
- A surface on which V is constant. The field is at right angles to it, and no work is done moving a mass along it.
- Field strength from a graph of V against r
- g = −ΔV/Δr: the magnitude of g is the gradient of the tangent to the V–r graph at that point.
- Gravitational potential difference
- The work done per unit mass in moving a mass between two points.
3.7.4 Orbits of planets and satellites
- Orbital speed and period of a satellite in a circular orbit
- GMm/r² = mv²/r gives v = √(GM/r), independent of the satellite's mass. T² = 4π²r³/(GM), so T² ∝ r³.
- Kinetic, potential and total energy of an orbiting satellite
- Ek = GMm/(2r) Ep = −GMm/r E = −GMm/(2r), so E = −Ek.
- Geosynchronous orbit
- An orbit whose period equals the planet's rotation period (23 h 56 min for the Earth).
- Geostationary orbit
- A geosynchronous orbit above the equator in the same direction as the planet's rotation, so the satellite stays above one point and a fixed ground antenna can point at it.
- Why does a satellite speed up when drag makes it fall to a lower orbit?
- Drag removes total energy, so the orbit radius falls. Potential energy falls by twice the gain in kinetic energy, so the speed increases (v = √(GM/r)).
Revise Gravitational fields and satellites further
- Study guideOxfordAQA International AS and A-level Physics: Gravitational potential and orbits of planets and satellites (9630)
- Revision notesOxfordAQA International AS and A-level Physics: Gravitational potential and orbits of planets and satellites (9630) – Revision Notes
- Practice questionsOxfordAQA International AS and A-level Physics: Gravitational potential and orbits of planets and satellites (9630) – Practice Questions