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Flashcards · 9702 · A Level Topic 13
Gravitational fields (A Level) flashcards
19 cards on A Level Topic 13, subtopics 13.1 to 13.4. Pick a subtopic or study them all.
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13.1 Gravitational field
- Gravitational field
- A region of space in which a mass experiences a force due to another mass. A field of force.
- What do gravitational field lines show?
- The direction of the force on a small test mass. They are drawn closer together where the field is stronger.
- Field-line pattern around an isolated spherical mass
- Radial lines pointing in towards the centre of the mass, getting further apart with distance (the field weakens).
- Field-line pattern close to the Earth’s surface
- Parallel, equally spaced lines pointing vertically down: the field is approximately uniform over small height changes.
13.2 Gravitational force between point masses
- Newton’s law of gravitation
- F = Gm₁m₂ ÷ r², an attractive force between two point masses, where r is the distance between their centres. G = 6.67 × 10⁻¹¹ N m² kg⁻².
- The separation of two masses doubles. What happens to the gravitational force?
- It falls to a quarter: an inverse square law, F ∝ 1/r².
- Derive the orbital speed of a satellite in a circular orbit
- Gravity provides the centripetal force: GMm ÷ r² = mv² ÷ r, so v = √(GM ÷ r). The satellite’s mass m cancels.
- Derive T² ∝ r³ for a circular orbit
- v² = GM ÷ r and v = 2πr ÷ T, so 4π²r² ÷ T² = GM ÷ r, giving T² = (4π² ÷ GM) r³.
- Three conditions for a geostationary orbit
- Period of 24 hours; orbiting west to east (the same direction as the Earth spins); directly above the Equator. Radius about 42 000 km from the Earth’s centre.
13.3 Gravitational field of a point mass
- Gravitational field strength
- The force per unit mass on a small test mass placed at that point: g = F ÷ m. Unit N kg⁻¹. A vector.
- Field strength of a point mass M
- g = GM ÷ r², with r measured from the centre of the mass. For a satellite at height h above a planet of radius R, r = R + h.
- Why can g = GM/r² be used for the field at the Earth’s surface?
- Outside a uniform sphere, the mass acts as if concentrated at its centre. Near the surface r ≈ R, so g is roughly constant.
- Earth: M = 5.97 × 10²⁴ kg, R = 6.37 × 10⁶ m. Find g at the surface.
- g = GM ÷ R² = (6.67 × 10⁻¹¹ × 5.97 × 10²⁴) ÷ (6.37 × 10⁶)² = 9.8 N kg⁻¹.
- A planet has mass 6.4 × 10²³ kg and radius 3.4 × 10⁶ m. Find g at its surface.
- g = (6.67 × 10⁻¹¹ × 6.4 × 10²³) ÷ (3.4 × 10⁶)² = 3.7 N kg⁻¹.
13.4 Gravitational potential
- Gravitational potential
- The work done per unit mass in bringing a small test mass from infinity to that point. φ = −GM ÷ r. Unit J kg⁻¹. A scalar.
- Why is gravitational potential always negative?
- It is defined as zero at infinity, and gravity is attractive: work must be done on a mass to move it out to infinity, so at any finite distance the potential is below zero.
- Gravitational potential energy of a mass m at distance r from M
- Ep = mφ = −GMm ÷ r.
- How does gravitational potential change as r increases?
- It increases (becomes less negative), approaching zero at infinity.
- Field strength vs potential for a point mass
- g = GM/r²: a vector, falls off as 1/r². φ = −GM/r: a scalar, falls off as 1/r. g = −dφ/dr: field strength is minus the potential gradient.