Module 11: Movement and change

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You should be able to (higher tier in bold):
11.01 use the following units
– second (s), metre (m), metre per second (m/s), metre per second2 (m/s2), kilogram (kg), joule (J), newton (N), newton per kilogram (N/kg), watt (W), becquerel (Bq) ()

Force and motion
You should be able to (higher tier in bold):
11.02 interpret distance-time graphs including determination of speed from the gradient of a graph
11.03 recall that velocity is speed in a stated direction
11.04 recall and use the equation
– acceleration (m/s2) = change in velocity (m/s) / time taken (s)
– a=(v-u)/t
11.05 interpret speed/time graphs
– determine the acceleration from the gradient of the graph
– determine the distance travelled from the area between the curve and the time axis
11.06
understand that the stopping distance of a vehicle is made up of
– thinking distance
– braking distance
11.07
understand the factors affecting the stopping distance of a vehicle, including
– the mass of the vehicle
– the speed of the vehicle
– the driver’s reaction time
11.08
recall a brief history of our understanding of forces and how they affect motion in a straight line including
– the Greek view – a simple force needed to sustain motion
– Galileo and Newton – balanced forces allow an object to continue in uniform motion in a straight line or to remain at rest
– Newton – gravitational attraction acts between all masses
11.09 understand that when object A pulls or pushes object B then object B pulls or pushes object A with a force that is equal in size and opposite in direction
11.10 understand that falling objects are acted on by a downward force (weight) and an upward
force (air resistance) and that at the start of the fall the forces are unbalanced and the object accelerates
11.11 understand that, when an object falls through the atmosphere, air resistance increases with
increasing speed until it is equal in size to the weight of the falling object, when terminal speed (velocity) is reached
11.12 understand that in the absence of air, all falling bodies accelerate at the same rate
11.13 describe the forces acting on a car moving in a straight line on a horizontal surface
– the driving force
– the resistive force
11.14
in the above example, understand how the balance of forces differs when the car is – accelerating
– braking
– moving at a constant speed
11.15
understand that when an unbalanced force acts on an object, the acceleration depends on
– the size of the unbalanced force
– the mass of the object
11.16 recall and use the equation
– force (N) = mass (kg)
acceleration (m/s2)
– F = m*a

Force and energy
You should be able to (higher tier in bold):
11.17recall and use the equation
– work done (J) = force (N) * distance moved in the direction of the force (m)
W = F
* d
11.18 understand that gravitational potential energy is stored positional energy, eg a swimmer on a
diving board, a person lifting weights
11.19 recall and use the equation
– gravitational potential energy (J) = mass (kg) * gravitational field strength (N/kg) * vertical height (m)
GPE = m
* g *
h
11.20 recognise the equivalence of work done and energy transfer and recall that energy transferred (J) = work done (J)
11.21 understand that power is the rate of doing work and is measured in watts (joules per second)
11.22 recall that kinetic energy is movement energy
11.23 recall and use the equation
– kinetic energy (J) = ½ * mass (kg) * velocity2 (m/s)2
KE = ½
* m *
v2

Earth waves
You should be able to (higher tier in bold):
11.24 recall that seismic waves are caused by earthquakes or ‘underground explosions’
11.25 understand that longitudinal and transverse waves are transmitted through the Earth
and that their paths and times of travel give information about the layered structure of the Earth: crust, mantle, outer (liquid) core and inner core
11.26
recall that the Earth’s outermost layer, the lithosphere, is composed of plates in relative motion and that plate tectonic processes result in the formation, deformation and recycling of rocks
11.27 understand that at plate boundaries, plates may
– slide past each other, sometimes causing earthquakes
– move towards each other, taking rock into the mantle
– move away from each other, resulting in volcanoes and forming new rocks ()

Using half-life
You should be able to (higher tier in bold):
11.28 understand that the activity of a radioactive isotope decreases over a period of time and is measured in becquerels
11.29 recall that the half-life of a radioactive isotope is the time taken for half the undecayed
nuclei to decay, and the consequent problems arising in the disposal of radioactive waste
11.30 use the concept of half-life to carry out simple calculations on the decay of a radioactive
isotope
11.31 describe the uses of radioactivity in the radioactive dating of archaeological specimens and
rocks