GRAVITATIONAL FIELDS
- Created by: CPev3
- Created on: 06-11-20 18:48
Define gravitational field:
- A field created around any object with mass
.
- Extends all the way to infinity
.
- Diminishes as the distance from the centre of mass of the object increases
Define gravitational field strength:
The gravitational force exerted per unit mass at a point within a gravitational field
Define weight:
- The gravitational force on an object
.
- An attractive force towards the centre of mass of the object producing the gravitational field
Equation for gravitational field strength:
g = F / m
.
F = ma and F = mg
∴ gravitational field strength at a point = acceleration of free fall of an object at that point
g on the Earth's surface:
9.81 Nkg-1
Define gravitational field lines:
- Lines of force used to map the gravitational field pattern around an object having mass
Properties of gravitational field lines:
- Do not cross
.
- The arrows show the direction of the force on an object at that point in the field
- Gravitational force is always attractive
- The direction of the field is always towards the centre of mass of the object producing the field
- Gravitational force is always attractive
.
- Closer together = stronger field
Define radial field:
- A symmetrical field
.
- Diminishes with distance from the centre of mass of the object producing the field
.
- Shown by the field lines getting further apart
Define point mass:
A mass with negligible volume
Define uniform gravitational field:
- The field lines are parallel
.
- The value for gravitational field strength remains constant
.
- The gravitational field close to the surface of a planet is approximately uniform
Newton's law of gravitation:
The force between two point masses is:
- Directly proportional to the product of the masses, F ∝ Mm
- Inverseley proportional to the square of their separation, F ∝ 1 / r2
.
F = - GMm / r2
G = 6.67e-11 Nm2kg-2
Equation for g in a radial field:
g = F / m and F = - GMm / r2
g = - GMm / mr2
g = - GM / r2
.
The negative sign shows that g at that point is in the opposite direction to r from the centre of mass of the object producing the gravitational field- a gravitational field is an attractive field.
Kepler's first law of planetary motion:
The orbit of a planet is an ellipse with the Sun at one of the two foci
.
Ellipse = an elongated 'circle' with two foci
Eccentricity = a measure of the elongation of an ellipse
Aphelion = the furthest point from the Sun in an orbit
Perihelion = the closest point to the Sun in an orbit
Kepler's second law of planetary motion:
- A line segment connecting a planet to the Sun sweeps out equal areas during equal intervals of time
.
- As a planet moves on its elliptical orbit around the Sun, its speed is not constant
.
- When it is closer to the Sun it moves faster
Kepler's third law of planetary motion:
mv2 / r = GMm / r2
v2 = GM / r
v = 2πr / T so 4π2r2 / T2 = GM / r
T2 = (4π2 / GM) r3
∴ T2 ∝ r3 or T2 / r3 = k
k is a constant for the planets orbiting the Sun approximately equal to 1 y2AU-3
F for any satellite in orbit:
F = mv2 / r = centripetal force on the satellite
F = GMm / r2 = gravitational force between the satellite and the Earth
.
Only force acting on a satellite is the gravitational attraction between it and the Earth
∴ always falling towards the Earth
↑ speed and ↑ distance
∴ as it falls the Earth curves away beneath it
∴ its height above the Earth's surface remains constant
v for any satellite in orbit:
- v = √ GM / r
.
- All satellites placed in a given orbit at a given height will be travelling at the same speed, even if their mass varies
.
- Once launched they are normally above the atmosphere
There is no air resistance to slow them down
Their speed remains constant
Uses of satellites:
- Communications (e.g. satellite phones)
.
- Military uses (e.g. reconnaissance)
.
- Scientific research (e.g. looking down onto the Earth to monitor pollution)
.
- Weather and climate (e.g. monitoring long-term changes in climate)
.
- Global positioning
Types of orbit:
Polar orbit
- Circles the poles
- Offers a complete view of the Earth over a given time period as the Earth rotates beneath the path of the satellite
- Useful for reconnaissance
Low Earth orbit
- In orbit close to the Earth
- T2 ∝ r 3 so takes less than 2 hours for the satellite to orbit the Earth
Equatorial orbit
- In orbit above the equator
Geostationary satellites...
- Are in a geostationary orbit
.
- Are in orbit above the equator
.
- Rotate in the same direction as the Earth's rotation
.
- Have an orbital period of 24 hours
.
- ∴ Remain above the same point of the Earth whilst the Earth rotates
.
- Are used for satellite television
Define gravitational potential:
- The work done per unit mass to bring an object from infinity to a point in the gravitational field
.
- All masses attract each other
External work must be done to move masses apart
Gravitational potential is a maximum at infinity
= 0 Jkg-1
∴ all values of gravitational potential are negative
Define infinity:
A distance so far from the object producing the gravitational field that the gravitational field strength is zero
Equation for Vg in a radial field:
Vg = - (GM / r)
- All values of Vg within the region of the gravitational field are negative
- When r = ∞ then Vg = 0
Changes in gravitational potential:
- Moving towards a point mass results in a decrease in gravitational potential
∴ the change in gravitational potential would be negative
.
- Moving away from a point mass (towards infinity) results in an increase in gravitational potential
∴ the change in gravitational potential would be positive
Define gravitational potential energy:
The capacity for doing work as a result of an object's position in a gravitational field
Equation for gravitational potential energy:
E = mVg
E in a uniform gravitational field:
↑ r
= ↑ Vg
= ↑ E
E in a radial field:
E = mVg and Vg = - (GM / r)
∴ E = - (GMm / r)
Equation for escape velocity:
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