What Are Gravitational Fields?

Ever wondered why you don't float off into space? Gravitational fields are regions around massive objects where anything with mass experiences an attractive force. Think of them as invisible zones of influence that pull objects together.

Gravity might seem strong when you drop your phone, but it's actually the weakest of all forces. You only notice it between really large objects like planets and stars. The force is always attractive - there's no such thing as gravitational repulsion.

Gravitational field strength tells us how strong the pull is at any point. It's defined as force per unit mass and measured in N/kg. The formula is simple: g = F/m, where F is force and m is mass. Picture field lines radiating outward from a planet - where they're closer together, the field is stronger.

Quick Tip: Field strength decreases as you move further from the centre of mass, which is why astronauts feel weightless in space!

Newton's Law of Gravity

Newton cracked the code on how gravitational force works with his famous equation: F = Gm₁m₂/r². This tells us the force between any two masses depends on their masses and the distance between their centres.

The gravitational constant G is 6.67 × 10⁻¹¹ N/kg - a tiny number that shows how weak gravity really is. The masses (m₁ and m₂) are in kilograms, whilst r is the distance between centres in metres.

Here's the clever bit: by combining Newton's law with the definition of field strength, we get g = GM/r². This means if you know a planet's mass and radius, you can work out its gravitational field strength at the surface.

Remember: This only works for objects that are roughly spherical - Newton assumed uniform spheres, so it's brilliant for planets but rubbish for asteroids!

Working Through Examples

Let's tackle some real calculations to see how this works in practice. These examples show you exactly what examiners expect in your working.

For a minor planet with mass 2 × 10²² kg and radius 1200 km, we use g = GM/r². First convert the radius to metres (1,200,000 m), then substitute: g = (6.67 × 10⁻¹¹)(2 × 10²²)/(1.2 × 10⁶)² = 0.9 N/kg.

When comparing two stars with the same mass but different radii, you can use ratios. If star 2 has 10 times the radius of star 1, then g₂ = g₁$r₁/r₂$². So g₂ = 300(1/10)² = 3 N/kg.

The trickiest question involves showing that g = ⁴⁄₃πGρr for planets. Start with g = GM/r², substitute M = ρ × ⁴⁄₃πr³ (density times volume), and simplify. The r² cancels with one r from the volume term.

Exam Tip: Always convert units first - kilometres to metres is the most common mistake in gravitational field calculations!

Essential Equations Summary

You'll need to memorise several key equations for gravitational fields. The most important is F = Gm₁m₂/r² for the force between two masses, and g = GM/r² for field strength near a planet's surface.

For objects in orbit, velocity relates to gravitational effects through v² = GM/r. This connects orbital motion to the mass of the central body and orbital radius.

Escape velocity calculations use energy principles. The equation ½mv₁² - ½mv₂² = mΔV shows the relationship between kinetic and gravitational potential energy. For escaping a planet completely, mΔV = GMm/r.

Gravitational potential (V) represents energy per unit mass. Near a planet's surface, V = -GM/r (negative because energy is needed to escape). For small height changes, ΔV = gΔh provides a simpler approximation.

Formula Sheet Tip: These equations will be on your data sheet, but knowing when to use each one is the real skill that gets you marks!