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IB Physics HL/Notes/D.1 Gravitational fields

IB Physics HLD.1 Gravitational fieldsNotes

Map Kepler’s three laws of orbital motion

Kepler’s laws are observational rules that Newton’s gravitation later explains. The first law fixes the orbit geometry. The second law describes changing speed around an ellipse. The third law links orbital period to orbit size, but only when the orbiting bodies share the same central mass.

First law: an orbiting body moves in an elliptical orbit with the central mass at one focus.
Second law: a line from the central mass to the orbiting body sweeps out equal areas in equal time intervals.
The second law means the orbiting body moves faster when closer to the central mass and slower when farther away.
Third law: for bodies orbiting the same central mass, T^2 is proportional to r^3, where r is the mean orbital radius or semi-major axis.
For circular orbits around mass M, Newton’s law gives T^2 = 4π^2 r^3/(GM).

Match each Kepler law cue to the correct orbital statement.

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State Kepler’s second and third laws and explain why a comet moves faster when it is closer to the Sun.

Stating T^2 ∝ r^3 without saying that the same central mass is required.

State Kepler’s second and third laws and explain why a comet moves faster when it is closer to the Sun.

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Map Universal gravitation

Newton’s law gives the magnitude of the attractive force between two masses. For spherical bodies, treat the mass as if concentrated at the centre when calculating the external field or force. The formula gives equal force magnitudes for both bodies; the acceleration can differ because acceleration depends on mass.

Newton’s law of gravitation is F = Gm1m2/r^2.
G = 6.67 × 10^-11 N m^2 kg^-2 is the gravitational constant.
r is the centre-to-centre distance between the two masses.
The force is always attractive and acts along the line joining the centres of the masses.
Each mass exerts the same magnitude force on the other, in opposite directions.
The inverse-square relationship means increasing r reduces F by the square of the scale factor.

Build Newton’s law of gravitation and state the distance and direction conventions.

Formula
Target formula F = G m1 m2 / r^2
F
gravitational force magnitude
N
G
gravitational constant
N m^2 kg^-2
m1
mass of first body
kg
m2
mass of second body
kg
r
centre-to-centre separation
m
1Identify both masses and the centre-to-centre separation.m1, m2, r
2Multiply the masses and G, then divide by the square of separation.F = G m1 m2 / r^2
3State the direction of the force.attractive, along the line joining centres
4Check inverse-square scaling.r doubled -> F/4

Two spherical masses attract each other gravitationally. State the formula for the force and explain what distance should be used for r.

Using surface separation instead of centre-to-centre separation or omitting that the force is attractive.

Two spherical masses attract each other gravitationally. State the formula for the force and explain what distance should be used for r.

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Point-mass approximation

The point-mass approximation is a modelling step before using inverse-square gravity. For planets and stars treated as spherical, external gravitational calculations use the centre as the location of the mass. This is why orbital radius is measured from the centre of the planet, not from the surface.

A point-mass approximation replaces an extended body by a single mass located at its centre of mass.
For a spherical body, the external gravitational field is the same as if all mass were concentrated at the centre.
In Newton’s law and g = GM/r^2, r is measured from the centre of the spherical body to the external point or the other body’s centre.
The approximation is best when the separation is much larger than the size of the bodies or when the body is spherical and the point is outside it.
Do not use the simple external point-mass formula inside a planet or near an irregular body unless a model has been justified.

Match each situation to whether the point-mass approximation is valid or needs caution.

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A satellite orbits 400 km above Earth’s surface. Explain why the orbital radius used in gravitational calculations is not 400 km.

Using altitude above the surface as r instead of measuring from Earth’s centre.

A satellite orbits 400 km above Earth’s surface. Explain why the orbital radius used in gravitational calculations is not 400 km.

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Map Gravitational field strength

A gravitational field describes what force a small test mass would experience at each point. Dividing force by the test mass gives g, so the field is a property of the source masses and position, not of the particular test mass. Around a spherical planet, g points radially inward and has magnitude GM/r^2 outside the planet.

Gravitational field strength g is defined as gravitational force per unit mass: g = F/m.
The unit N kg^-1 is equivalent to m s^-2.
For a point mass or outside a spherical mass M, the magnitude is g = GM/r^2.
The direction of g is the direction of the gravitational force on a small test mass, toward the attracting mass.
g decreases with inverse-square distance and fields from multiple masses combine by vector addition.

Build the gravitational field strength formulas and state the units and direction.

Formula
Target formula g = F/m; g = GM/r^2
g
gravitational field strength
N kg^-1 or m s^-2
F
gravitational force on a test mass
N
m
test mass experiencing the force
kg
G
gravitational constant
N m^2 kg^-2
M
source mass
kg
r
distance from centre of source mass to the field point
m
1Start with force per unit mass.g = F/m
2For a point or spherical source mass, substitute Newton’s law.g = GM/r^2
3State the units.N kg^-1 = m s^-2
4State the vector direction.toward the source mass

Define gravitational field strength and derive the expression for the field strength outside a spherical mass M.

Giving only g = GM/r^2 without defining g = F/m or stating the vector direction.

Define gravitational field strength and derive the expression for the field strength outside a spherical mass M.

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Map Gravitational field lines

A field-line diagram is a vector map. The arrow direction tells the direction a small mass would be pulled. Around an isolated spherical mass, all field lines point inward toward the centre. Near Earth’s surface over small distances, the radial lines are almost parallel, so the field is often drawn as uniform.

Field lines show the direction of gravitational force on a small test mass at each point.
For a point mass or spherical mass, field lines are radial and point toward the centre.
Line density represents field strength: closer lines mean larger g.
Near the surface of a large planet, the field can be approximated as uniform, with parallel equally spaced lines pointing downward.
Field lines should not cross because the field has only one direction at a point.

Label the gravitational field-line diagrams for a radial field and a uniform near-surface field.

Label
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5

Sketch the gravitational field lines around an isolated spherical planet and explain how the diagram shows field direction and strength.

Drawing arrows away from the mass or failing to state that closer lines represent stronger field.

Sketch the gravitational field lines around an isolated spherical planet and explain how the diagram shows field direction and strength.

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Map Gravitational potential energy

Because gravity is attractive, two separated masses form a bound system with less energy than the same masses infinitely far apart. Setting E_p = 0 at infinity makes every finite separation negative. Work done by an external agent to move a mass away from a planet increases E_p toward zero.

Gravitational potential energy is defined relative to a chosen zero; in fields, zero is usually set at infinite separation.
For two point masses, E_p = -Gm1m2/r.
The negative sign shows that work must be done to separate bound masses to infinity.
As r increases, E_p becomes less negative and approaches zero from below.
Near a planet surface, ΔE_p = mgΔh is only a local approximation for small height changes.

Build the gravitational potential energy expression and interpret its sign.

Formula
Target formula E_p = -G m1 m2 / r
E_p
gravitational potential energy of the two-mass system
J
G
gravitational constant
N m^2 kg^-2
m1
first mass
kg
m2
second mass
kg
r
centre-to-centre separation
m
1Set the reference level.E_p = 0 at infinite separation
2Write the two-body gravitational potential energy.E_p = -G m1 m2 / r
3Interpret the negative sign.finite separation -> bound system -> E_p < 0
4Describe what happens as separation increases.r increases -> E_p approaches 0 from below

Explain why the gravitational potential energy of a satellite-Earth system is negative when zero is set at infinity.

Writing the formula without explaining the zero at infinity and the meaning of the negative sign.

Explain why the gravitational potential energy of a satellite-Earth system is negative when zero is set at infinity.

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Two-body potential energy

Force and potential energy describe the same interaction from different viewpoints. Force tells the instantaneous pull and has a direction. Potential energy tells how much energy is associated with the separation of the two-mass system. The formulas look similar, but the distance dependence and sign are different.

Gravitational force magnitude is F = Gm1m2/r^2 and is a vector quantity with direction along the line joining centres.
Two-body gravitational potential energy is E_p = -Gm1m2/r and is a scalar quantity.
The negative sign in E_p comes from choosing zero energy at infinite separation.
Force changes with inverse-square distance; potential energy changes with inverse distance.
Potential energy belongs to the system of two masses, not to one mass alone in isolation.

Match each gravitational quantity to its correct formula or property.

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A student writes the gravitational potential energy of two masses as -Gm1m2/r^2. Identify the error and give the correct expression.

Mixing the inverse-square force law with the inverse-distance potential energy expression.

A student writes the gravitational potential energy of two masses as -Gm1m2/r^2. Identify the error and give the correct expression.

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Map Gravitational potential

Potential strips away the test mass from potential energy. Instead of asking how much energy a particular mass has, V describes the field’s energy-per-kilogram value at a point. Around a single mass, V is negative because work must be supplied to move a test mass from that point to infinity.

Gravitational potential is the work done per unit mass in bringing a small test mass from infinity to a point in the field.
For a point or spherical mass M, V = -GM/r when zero is chosen at infinity.
Potential is a scalar quantity with unit J kg^-1.
Potential energy of mass m at that point is E_p = mV.
At finite distance from an attracting mass, V is negative and approaches zero as r approaches infinity.

Build the gravitational potential formula and connect it to potential energy.

Formula
Target formula V = -GM/r; E_p = mV
V
gravitational potential at a point
J kg^-1
G
gravitational constant
N m^2 kg^-2
M
source mass
kg
r
distance from source centre to point
m
m
test mass placed at the point
kg
E_p
gravitational potential energy
J
1Start from energy per unit mass.V = E_p/m
2Use the point-mass potential.V = -GM/r
3Recover potential energy for a test mass.E_p = mV
4State scalar unit and sign.J kg^-1, negative at finite r

Define gravitational potential and state the expression for potential at distance r from an isolated mass M.

Giving the potential energy formula instead of potential per unit mass, or using units of joules.

Define gravitational potential and state the expression for potential at distance r from an isolated mass M.

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Potential gradient

A potential graph stores field information in its slope. Close to a mass, the potential changes rapidly with distance, so the field is strong. Far away, the graph flattens and the field is weak. The minus sign is a direction statement: an object accelerates in the direction of decreasing gravitational potential.

Gravitational potential is scalar, but changes in potential with position determine the vector field strength.
For a radial coordinate r directed away from the mass, g = -dV/dr.
The magnitude of g is the magnitude of the gradient of the V-r graph.
The negative sign means the field points toward decreasing potential, which is inward for an attractive mass.
For V = -GM/r, differentiating gives dV/dr = GM/r^2, so the field points inward with magnitude GM/r^2.

Build the link between gravitational potential gradient and field strength.

Formula
Target formula g = -dV/dr; |g| = |gradient of V-r graph|
g
radial gravitational field strength
N kg^-1
V
gravitational potential
J kg^-1
r
radial distance from source mass
m
G
gravitational constant
N m^2 kg^-2
M
source mass
kg
1Start with the point-mass potential.V = -GM/r
2Differentiate potential with respect to r.dV/dr = GM/r^2
3Apply the negative-gradient relation.g = -dV/dr
4State the magnitude and direction.|g| = GM/r^2, directed inward

The gravitational potential V becomes less negative as distance r from a planet increases. Explain how the V-r graph can be used to find gravitational field strength.

Using the value of V instead of the gradient of the V-r graph.

The gravitational potential V becomes less negative as distance r from a planet increases. Explain how the V-r graph can be used to find gravitational field strength.

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Map Work in gravitational fields

Potential is energy per unit mass, so multiplying potential difference by mass gives the potential energy change. The sign depends on who does the work. If an external agent slowly lifts a mass away from a planet, it does positive work and gravitational potential energy increases. Gravity does negative work for that same displacement.

A mass m moved through potential difference ΔV has potential energy change ΔE_p = mΔV.
If an external agent moves the mass slowly without changing kinetic energy, W_external = ΔE_p.
The work done by the gravitational field is W_gravity = -ΔE_p.
Moving farther from a planet increases gravitational potential and potential energy toward zero, so external work is positive.
Moving along an equipotential has ΔV = 0 and no gravitational work is required for the move.

Spot and repair the sign or concept errors in work-potential statements.

Spot Errors

A 500 kg spacecraft is moved slowly between two points where the gravitational potential changes from -8.0 MJ kg^-1 to -6.0 MJ kg^-1. Calculate the external work done.

Using the sign for work done by gravity when the question asks for external work.

A 500 kg spacecraft is moved slowly between two points where the gravitational potential changes from -8.0 MJ kg^-1 to -6.0 MJ kg^-1. Calculate the external work done.

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Map Gravitational equipotentials

Equipotentials are contour lines for gravitational potential. Just as height contours connect equal altitude on a map, equipotentials connect equal potential in a field diagram. Moving along a contour does not change potential energy, but moving between contours does.

An equipotential surface is a surface where gravitational potential V has the same value everywhere.
Moving a mass along an equipotential has ΔV = 0, so ΔE_p = mΔV = 0 and no gravitational work is done.
Around an isolated spherical mass, equipotential surfaces are concentric spheres; in a 2D diagram they appear as concentric circles.
Potential values are more negative closer to the mass and increase toward zero outward.
Equipotentials are closer together where the potential changes more rapidly, meaning the field is stronger.

Label the gravitational equipotential diagram around a spherical mass.

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5

Explain why no work is done moving a satellite along a gravitational equipotential surface.

Saying no work is done because there is no gravitational field, instead of because potential is constant along the path.

Explain why no work is done moving a satellite along a gravitational equipotential surface.

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Map Equipotentials and field lines

Equipotentials and field lines are two views of the same field. The equipotentials show scalar values of V, while field lines show the direction of force. A field line cannot have any component along an equipotential, because then the field would do work without a change in potential. Therefore the field line crosses the equipotential at right angles.

Gravitational field lines are always perpendicular to equipotential surfaces.
The field points in the direction of decreasing potential; around a mass this is inward toward more negative potential.
Moving along an equipotential requires no gravitational work because ΔV = 0.
Moving between equipotentials changes potential energy by ΔE_p = mΔV.
Closer equipotentials mean a larger potential gradient and therefore a stronger gravitational field.

Label the relationship between gravitational field lines and equipotentials.

Label
Labels
5

On a diagram of gravitational equipotential lines around a planet, add field lines and explain their direction.

Drawing field lines tangent to equipotentials or failing to state that they point toward decreasing potential.

On a diagram of gravitational equipotential lines around a planet, add field lines and explain their direction.

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Map Escape speed

At escape threshold, the object just reaches infinity with no kinetic energy left. Its initial kinetic energy must therefore equal the magnitude of its negative gravitational potential energy. This gives the escape-speed formula and explains why escape speed from a planet depends on planet mass and starting radius, not on the launched object’s mass.

Escape speed is the minimum initial speed needed to escape a gravitational field without further propulsion.
For the minimum case, final kinetic energy at infinity is zero and gravitational potential energy at infinity is zero.
Energy conservation gives 1/2 mv_esc^2 - GMm/r = 0.
Solving gives v_esc = sqrt(2GM/r).
The escaping object’s mass cancels, but the central mass M and starting radius r matter.
The model ignores air resistance and assumes r is measured from the centre of the source mass.

Build the escape speed formula from the energy balance.

Formula
Target formula v_esc = sqrt(2GM/r)
v_esc
escape speed
m s^-1
G
gravitational constant
N m^2 kg^-2
M
central mass
kg
r
starting distance from centre of central mass
m
m
mass of escaping object, cancels
kg
1Write total mechanical energy at the escape threshold.1/2 m v_esc^2 - GMm/r = 0
2Move the potential energy term to the other side.1/2 m v_esc^2 = GMm/r
3Cancel the escaping object’s mass.v_esc^2 = 2GM/r
4Take the square root.v_esc = sqrt(2GM/r)

Derive the escape speed from the surface of a planet of mass M and radius R, ignoring air resistance.

Using centripetal force or orbital speed instead of an energy argument.

Derive the escape speed from the surface of a planet of mass M and radius R, ignoring air resistance.

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Map Orbital speed

A circular orbit is continuous free fall around the central mass. Gravity provides the inward acceleration needed to keep the satellite moving in a circle. Equating gravitational force with centripetal force gives orbital speed. The force direction is inward while the velocity is tangential.

For a circular orbit, the gravitational force acts as the centripetal force.
Set GMm/r^2 = mv^2/r to derive v = sqrt(GM/r).
The mass of the orbiting object cancels; orbital speed depends on central mass M and orbital radius r.
Higher circular orbits have smaller orbital speed.
The period is T = 2πr/v, so T^2 = 4π^2r^3/(GM), consistent with Kepler’s third law.
Escape speed at the same radius is sqrt(2GM/r), which is larger than circular orbital speed.

Derive circular orbital speed by equating gravity and centripetal force.

Formula
Target formula v = sqrt(GM/r)
v
circular orbital speed
m s^-1
G
gravitational constant
N m^2 kg^-2
M
central mass
kg
m
orbiting mass, cancels
kg
r
orbital radius from centre of central mass
m
1Write gravitational force on the satellite.F_g = GMm/r^2
2Write required centripetal force.F_c = mv^2/r
3Set gravity equal to centripetal force and cancel m.GM/r^2 = v^2/r
4Solve for orbital speed.v = sqrt(GM/r)

Derive the speed of a satellite in a circular orbit of radius r around a planet of mass M.

Starting from energy or escape speed instead of centripetal force for a circular orbit.

Derive the speed of a satellite in a circular orbit of radius r around a planet of mass M.

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Atmospheric drag on orbits

Drag acts opposite the satellite’s motion and removes mechanical energy. The satellite drops to a lower orbit with more negative gravitational potential energy. For a circular orbit around the same planet, smaller radius requires a larger orbital speed. The apparent paradox is resolved by remembering that total mechanical energy decreases even though kinetic energy can increase in the lower orbit.

Atmospheric drag is a non-conservative force that dissipates mechanical energy as thermal energy.
As energy is lost, the satellite cannot remain in the same high orbit, so its orbital radius and height decrease.
For a circular orbit, v = sqrt(GM/r), so a smaller orbital radius corresponds to a larger orbital speed.
This means a satellite can lose total mechanical energy while moving faster in the lower orbit.
Continued drag causes orbital decay and can lead to re-entry.

Repair the incorrect statements about atmospheric drag on an orbiting satellite.

Spot Errors

Describe the qualitative effect of a small atmospheric drag force on the height and speed of a satellite in low Earth orbit.

Stating only that the satellite slows down, without explaining orbital decay and the higher speed of the lower circular orbit.

Describe the qualitative effect of a small atmospheric drag force on the height and speed of a satellite in low Earth orbit.

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Retrieve the Core D.1 Gravitational fields Model

Review

Core D.1 is secure when the student chooses the correct gravitational representation. Kepler describes observed orbit patterns. Newton explains the attractive inverse-square force. Field strength describes force per kilogram and field lines show direction and relative strength. Circular orbit questions use centripetal force, not escape-energy arguments.

Kepler’s laws describe elliptical orbits, equal areas in equal times, and T^2 proportional to r^3 for the same central mass.
Newton’s law of gravitation is F = Gm1m2/r^2, attractive and along the line joining centres.
For spherical bodies outside the mass, use the point-mass model and measure r from centre to centre.
Gravitational field strength is g = F/m = GM/r^2 and points toward the source mass; multiple fields add vectorially.
Field lines point in the force direction, are denser where the field is stronger, and are radial around a spherical mass.
For circular orbits, gravity provides centripetal force and v = sqrt(GM/r).

Match each core D.1 cue to the response it should trigger.

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Retrieve the HL D.1 Gravitational fields Model

Review

HL D.1 is an energy-field extension. The key move is separating scalar quantities from vector quantities. Potential and potential energy are scalar and negative near an attracting mass. Field strength is a vector found from the negative potential gradient. Work depends on potential difference. Escape speed uses total energy, while drag reduces total mechanical energy and drives orbital decay.

With zero at infinity, gravitational potential energy is E_p = -Gm1m2/r and gravitational potential is V = -GM/r.
Potential is scalar with unit J kg^-1; potential energy for mass m is E_p = mV.
The gravitational field is the negative gradient of potential: g = -dV/dr, with magnitude equal to the slope magnitude of a V-r graph.
Work and potential are linked by ΔE_p = mΔV; work done by gravity is -ΔE_p.
Equipotential surfaces have constant V, field lines cross them at right angles, and no work is done along them.
Escape speed follows from energy conservation: v_esc = sqrt(2GM/r).
Small atmospheric drag removes mechanical energy, lowers orbital height, and can lead to a lower orbit with greater circular orbital speed.

Match each HL D.1 cue to the formula, graph, or physical interpretation it should trigger.

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