Field: A region where a force is exerted on objects due to a physical quantity like mass or charge.
Electric field strength, E, is the force per unit charge on a small positive test charge placed at the point
Caused by electric charges.
Can be attractive or repulsive (like charges repel, opposite charges attract).
The force between two point charges is given by:
F = 9 × 109 x Q1Q2 / r2
where 9 × 109 Fm-1 (k) is Coulomb’s constant, Q1 and Q2 are charges, and r is the separation.
The force per unit positive charge at a point:
E = F / q
Gravitational field strength, g, is the force per unit mass on a small test mass placed at the point
Caused by mass.
Always attractive.
The force between two masses is given by:
F = G x M1M2 / r2
where G is the gravitational constant, M1 and M2 are masses, and r is the separation.
The force per unit mass at a point:
g = F / m
Both electric and gravitational forces decrease with the square of the distance (1/r2).
Outside a uniform spherical mass (e.g., Earth), the gravitational field behaves as if all mass were concentrated at a single point at the centre.
g= GM / r2
where M is the total mass of the sphere and r is the radial distance from the centre.
Imaginary lines that show the direction of force in a field.
Point away from positive charges.
Point toward negative charges.
Always point toward the mass (gravity is always attractive).
Also radial for a point mass.
Indicates field strength (closer lines = stronger field).
A surface where the potential is the same at all points.
Equipotential surfaces are spheres centred around the charge or mass.
Zero, since moving along the surface does not change potential energy.
Electric and gravitational equipotentials are always at right angles to the respective field lines.
The electric potential at a point due to a charge q is:
V=kq / r
For multiple charges, add potentials algebraically (since potential is a scalar quantity).
The gravitational potential at a point due to a mass M is:
Φ = −GM / r
Always negative (gravity is always attractive).
Also follows superposition (sum of individual potentials).
The net electric field at a point:
Enet = ∑ Ei
The net gravitational field at a point:
gnet = ∑ gi
Directions must be considered when summing vectors.
ΔUP=mgΔh
where g is constant over small height changes (near Earth’s surface).
When g varies significantly, use:
UP = − GMm / r
instead of mgΔh