gravitational fields Flashcards
gravitational field
area in which objects with mass experience a non contact force
gravitational field strength
the force per unit mass exerted by a gravitational field
g=F/m
newtons law of gravitation
shows that the magnitude of the gravitational force between two masses is directly proportional to the product of the masses, and is inversely proportional to the square of the distance between them
F=GMm/r^2
gravitational field strength in a radial field
F=GMm/r^2 g=F/m
gm=GMm/r^2 g=GM/r^2
gravitational potential
the work done per unit mass when moving an object from infinity to that point. At infinity, it is 0, and as it moves away from infinity to a point, energy is released as gravitational potential energy is reduced. therefore it is always negative
gravitational potential difference (∆v)
the energy needed to move a unit mass between two points, and therefore can be used to find the work done when moving an object in a gravitational field.
workdone=m∆v
velocity of an object with a change in Potential
E1-E2=0.5v^2
similarities between electric and gravitational fields
-forces both follow inverse square law
-uses field lines to represent and can both be either uniform or radial
-use equations of a similar form to find the force exerted and field strength
differences between electric and gravitational fields
-grav fields are always attractive, whilst electric fields can repel
-electric forces acts on charge, whilst gravity acts on mass
orbital motion
Keplers third law is that the square of the orbital period is dire try proportional to the cube of the radius
derive the equation !
gravitational potential energy
GPE=Gmm/r
how to calculate a new time period if distance from the centre is changed
due to Keplers law T^2 is proportional to r^3, and so T1^2/T2^2=r1^3/r2^3
kinetic energy during orbit
the closer the orbit to the surface, the greater the kinetic energy as it will have a greater velocity due to the shorter time period.
geostationary orbit
time period of 24 hours and so stays above the same point of the equator