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Subdecks (4)
quantum+particles AS
physics AS
37 cards
mechanics AS
physics AS
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Electricity AS
physics AS
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Waves AS
physics AS
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Cards (282)
Waves
Transfer energy
without
transferring
matter
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Types of waves
Transverse
Longitudinal
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Transverse waves
Particles oscillate
perpendicular
to the direction of
energy
transfer. example is
seismic S
waves
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Longitudinal waves
Particles oscillate parallel
to the direction of
energy transfer
, made up of compressions and rarefactions. example of this are
sound waves
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Time period
Time taken for one complete
wave
to pass a
point
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Frequency
Number of complete
waves
passing a point every second, calculated as 1 /
time period
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Wave
speed
Equals
frequency
times
wavelength
(V = f * Lambda)
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Polarization
Transverse waves can be polarized by a
filter
that only transmits waves oscillating in a particular
direction
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Interference
/
Superposition
When displacements of
individual waves sum
at each point, can be constructive or
destructive
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Harmonics
Occur when wavelength is equal to
2x
or
1x
the length of the string
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Nodes and antinodes
Nodes have
destructive interference
and no energy transfer, antinodes have both constructive and destructive interference with
energy transfer
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Young's
double
slit experiment
Uses coherent sources (in phase) at the double slit to produce a
diffraction
pattern, fringe width W =
Lambda
* D / s where D is distance and s is slit separation
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Single slit diffraction
Has a
large central
maximum that falls away
quickly
, with smaller secondary maxima
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Diffraction grating
Equation: n * Lambda = d * sin(Theta), where n is order,
Lambda
is
wavelength
, d is line spacing
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Refraction
Equation: n1 * sin(Theta1) = n2 * sin(Theta2), where n1 and n2 are
refractive indices
of the
two media
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Total internal reflection
(
TIR
)
Occurs when
angle
of incidence is greater than the critical angle, and the
refractive index
of the first medium is greater than the second
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Average speed
Distance
/
time
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SUVAT equations
Equations
of motion for
accelerating objects
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Projectile motion
Vertical motion uses
SUVAT
, horizontal motion uses
constant speed
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Newton's laws
1st: Constant
motion
if no external force, 2nd:
F=ma
, 3rd: Action-reaction pairs
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Weight
Force = mass *
gravitational field strength
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Equilibrium
No
resultant force
and
no resultant moment
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Friction
Increases with speed, force parallel to slope =
mg
*
sin
(Theta)
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Energy
Kinetic =
1/2*mv^2
, Gravitational potential =
mgh
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Hooke's
law
Force =
spring constant
*
extension
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Stress and strain
Stress = force/area, Strain = extension/original length, Young's modulus =
stress
/
strain
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Stress-strain graph
Limit
of proportionality,
Elastic
limit, Ultimate tensile stress
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Equilibrium
Sum of clockwise moments = sum of
anticlockwise
moments
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Scalars
and
vectors
Scalars have
magnitude only
, vectors have
magnitude
and direction
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Momentum
p =
mv
, F = rate of change of
momentum
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Conservation of momentum
Total momentum
before
= total momentum
after
in closed systems
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Braking distance
Quadruples
if
speed doubles
due to kinetic energy
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Elastic and inelastic collisions
Elastic conserves
kinetic energy
,
inelastic
does not
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Fundamental
particles
Leptons
are fundamental, hadrons are made of quarks (
baryons 3 quarks
, mesons quark-antiquark)
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Strong nuclear force
Keeps
nucleus
together,
attractive
up to 0.5 cm then repulsive, range 3-4 cm
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Mass-energy
equivalence
E =
mc^2
, mass can be converted to energy in
annihilation
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Graviton
Exchange particle for the
gravitational force
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Strong nuclear force
Force that keeps the
nucleus
of an atom together, overcoming the
electrostatic repulsion
of protons
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Strong nuclear force
Attractive up to
0.5
cm, then becomes
repulsive
Range of attraction is
3-4
cm
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Mass-energy equivalence
Mass
can be converted into
energy
, and vice versa, according to the equation E = mc^2
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