A concept-based Higher Level syllabus extending motion, matter, waves, fields, and nuclear and quantum physics through rotational mechanics, relativity, thermodynamics, induction, and quantum theory.
Course units
5
Estimated study time
180 hours
Overall completion0%
Course Overview
IB Physics HL is organized into 5 units and 24 focused topics with 299 Key Concepts sections, 0 questions, and 480 flashcards.
Each unit groups focused topics. Every topic follows the same clear rhythm: review Key Concepts, use the Question Bank, then strengthen recall.
Unit 1
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Space, Time and Motion
Theme A begins with classical mechanics and then extends the idea of motion into rotation and relativistic spacetime. The HL-only A.4 and A.5 subtopics are major additions and should be learned as conceptual extensions of familiar linear motion, momentum and energy.
42 hours estimated ·5 topics
Unit 1 progress0%
Topics in this unit
Topic A.1Not started
Kinematics
Kinematics describes motion through position, displacement, velocity and acceleration. Students connect equations with vector representations and motion graphs, then apply the same ideas to projectile motion.
Distinguish scalar distance and speed from vector displacement and velocity.
Calculate average and instantaneous velocity, speed and acceleration.
Use gradients and areas on position–time, velocity–time and acceleration–time graphs.
Apply constant-acceleration equations with a consistent sign convention.
Resolve projectile motion into independent horizontal and vertical components.
Describe qualitatively how resistance in a fluid changes a trajectory and produces terminal speed.
Key formulas
Displacement from position
Δx=xf−xi
Average acceleration
aˉ=ΔtΔv
Average speed
average speed=Δttotal distance
Average velocity
vˉ=ΔtΔx
Instantaneous velocity
v=dtdx
Instantaneous acceleration
a=dtdv
Speed from one-dimensional velocity
speed=∣v∣
Velocity from a position–time graph
v=gradient of the x-t graph
Displacement from a velocity–time graph
Δx=∫t1t2vdt
Distance from a velocity–time graph
distance=∫t1t2∣v∣dt
Velocity change from an acceleration–time graph
Δv=∫t1t2adt
Displacement from mean velocity
s=21(u+v)t
Velocity after time
v=u+at
Displacement after time
s=ut+21at2
Time-independent equation
v2=u2+2as
Vertical acceleration with upward positive
ay=−g≈−9.81ms−2
Initial velocity components
ux=ucosθ,uy=usinθ
Ideal horizontal motion
x=x0+uxt,vx=ux
Ideal vertical motion
y=y0+uyt−21gt2,vy=uy−gt
Speed from perpendicular components
v=vx2+vy2
Flight time, range and maximum rise: check the conditions
T=g2usinθ,R=gu2sin(2θ),H=2gu2sin2θ
Terminal-speed condition
Fresultant=0⇒a=0
Simplified vertical balance
Fdrag=mgat terminal speed (if buoyancy is negligible)
Topic A.2Not started
Forces and momentum
This subtopic uses Newton’s laws and momentum to explain changes in motion. It also introduces circular motion as a continuous change of velocity direction caused by a resultant inward force.
Apply Newton’s three laws and identify valid action–reaction pairs.
Draw free-body diagrams and resolve forces into useful components.
Model normal force, tension, friction, spring force, viscous drag and buoyancy.
Use momentum and impulse in collisions, explosions and force–time situations.
Apply conservation of momentum to isolated systems.
Analyse uniform circular motion using centripetal acceleration and resultant force.
Key formulas
Resultant external force
Fnet=F1+F2+⋯+Fn
Newton's second law in momentum form
Fnet=dtdp
Newton's second law for constant mass
Fnet=ma
Translational equilibrium
Fnet=0⇒a=0
Weight near Earth's surface
W=mg
Newton's second law by components
Fnet,x=max,Fnet,y=may
Newton's third law
FA→B=−FB→A
Weight components on an incline
W∥=mgsinθ,W⊥=mgcosθ
Normal force on a simple incline
N=mgcosθif a⊥=0 and no other perpendicular force acts
Static-friction range
0≤fs≤μsN
Limiting and kinetic friction
fs,max=μsN,fk=μkN
Ideal-string tension
T1=T2=T
Hooke's law
Fs=−kxandFs=k∣x∣in magnitude
Archimedes' principle
Fb=ρfluidVdisplacedg
Stokes' law
Fd=6πηrv
Terminal-motion balance
W=Fb+Fdfor steady downward motion in still fluid with no other forces
Momentum
p=mv
Net external impulse
Jnet=Δp=∫t1t2Fnetdt
Average resultant external force
Fnet,avg=ΔtΔp
Momentum conservation
Pbefore=Pafterwhen external impulse is negligible
Translational kinetic energy
K=21mv2
Speed, period and angular speed (uniform circular motion)
v=T2πr=ωr
Angular speed and period (uniform circular motion)
ω=T2π
Centripetal acceleration
ac=rv2=ω2r,ac=T24π2rfor uniform motion
Required radial resultant
Fradial=mac=rmv2
Topic A.3Not started
Work, energy and power
Energy methods provide an alternative to force-by-force analysis. Students use work, kinetic and gravitational potential energy, efficiency and power to understand how systems transfer and transform energy.
Calculate work done by a constant force, including forces at an angle to displacement.
Use the work–energy principle and conservation of energy.
Calculate kinetic and near-Earth gravitational potential energy.
Interpret force–displacement graphs as work transferred.
Calculate power from work or energy transfer rate and from force and velocity.
Analyse efficiency and Sankey-type energy-transfer representations.
Key formulas
Conservation of total energy
Einitial=Efinal
Average power
Pavg=ΔtΔE=ΔtW
Efficiency
η=EinputEuseful=PinputPuseful
Work by a constant force
W=Fscosθ
Work by the parallel component
W=F∥s
Work from a variable force
W=signed area under the F∥ against s graph
Translational kinetic energy
Ek=21mv2=2mp2
Work–energy theorem
Wnet=ΔEk=21m(v2−u2)
Change in gravitational potential energy
ΔEg=mgΔh
Gravitational potential energy from a chosen zero
Eg=mgh
Work done by gravity
Wg=−ΔEg
Hooke's law
Fs=−kx
Elastic potential energy
Es=21kx2
Change in elastic potential energy
ΔEs=21k(x22−x12)
Mechanical energy
Emech=Ek+Eg+Es
Ideal mechanical-energy conservation
Ek,i+Eg,i+Es,i=Ek,f+Eg,f+Es,f
System energy change when work is the only boundary energy transfer
Wext=ΔEsystem
Thermal transfer by constant kinetic friction
ΔEth=fks
Non-conservative work
Wnc=ΔEmech
Idealized braking distance
d=2Fbmv2
Average power
Pavg=ΔtW=ΔtΔE
Instantaneous mechanical power
P=F⋅v=Fvcosθ
Parallel force form
P=F∥v
Energy efficiency
η=EinputEuseful
Power efficiency
η=PinputPuseful
Percentage efficiency
η%=100η
Overall efficiency of a simple useful-output cascade
ηoverall=η1η2η3⋯
Gravitational power of a mass flow
Pg=m˙gh
Mechanical-to-thermal balance with no external energy transfer
Emech,i=Emech,f+ΔEth
Spring constant from a graph
k=ΔxΔF
Elastic work from graph area
W=21Fx=21kx2
Useful climbing power
P=ΔtmgΔh
Topic A.4Not started
Rigid body mechanics
Rigid body mechanics is an HL-only extension from linear motion to rotation. Torque plays a role analogous to force, moment of inertia plays a role analogous to mass, and angular momentum provides a rotational conservation law.
Calculate torque from force magnitude, lever arm and angle.
Apply rotational equilibrium by setting the net torque to zero.
Use angular displacement, angular velocity and angular acceleration.
Apply constant-angular-acceleration equations in rotational motion.
Understand moment of inertia as a measure that depends on both total mass and how that mass is distributed relative to the axis.
Use τ = Iα to connect resultant torque and angular acceleration.
Calculate angular momentum and apply conservation of angular momentum when external torque is negligible.
Relate torque acting over time to angular impulse.
Calculate rotational kinetic energy.
Analyse rolling without slipping as simultaneous translation and rotation.
Key formulas
Radian definition
θ=rs
Average angular velocity
ωav=ΔtΔθ
Average angular acceleration
αav=ΔtΔω
Angular-to-linear relationships
v=r∣ω∣,at=rα,ac=rω2
Angular velocity–time
ω=ω0+αt
Angular displacement–time
Δθ=ω0t+21αt2
No-time equation
ω2=ω02+2αΔθ
Mean-angular-velocity equation
Δθ=2ω0+ωt
Torque about a chosen origin (vector extension)
τ=r×F
Planar torque magnitude about the perpendicular axis
τ=rFsinϕ=Fd⊥
Torque of a couple
τcouple=Fd
Translational equilibrium
Fnet=0
Rotational equilibrium
τnet=0
Centre of mass for discrete masses
rCM=i=1∑nmii=1∑nmiri
Discrete masses
I=i=1∑nmiri2
Continuous mass distribution
I=∫r2dm
Parallel-axis theorem
I=ICM+Md2
Thin uniform ring or hoop about its central symmetry axis
I=MR2
Uniform solid disk or cylinder about its central symmetry axis
I=21MR2
Uniform thin rod about a perpendicular axis through its centre
I=121ML2
Uniform thin rod about a perpendicular axis through one end
I=31ML2
Uniform solid sphere about an axis through its centre
I=52MR2
Rotational Newton's second law
τnet=Iα
Net external angular impulse about a fixed axis
Jangular,net=∫τext,netdt=ΔL
Constant net-torque angular impulse
τext,netΔt=ΔL
Particle angular momentum
L=r×p
Angular-momentum component about a fixed axis
L=Iω
Torque and angular momentum about a fixed inertial origin
τext,net=dtdL
Angular-momentum conservation
Lbefore=Lafter
Work by constant torque
W=τΔθ
Work by variable torque
W=∫θiθfτdθ
Fixed-axis rotational kinetic energy
Krot=21Iω2=2IL2
Rotational power
P=τω
No-slip speed constraint
vCM=R∣ω∣
No-slip acceleration constraint
aCM=αR
Total rolling kinetic energy
K=21MvCM2+21ICMω2
Free gravity-driven rolling down a fixed incline (no slip or losses)
a=1+(MR2)ICMgsinβ
Coupled linear dynamics
Fnet=ma
Coupled rotational dynamics
τnet=Iα
No-slip coupling
a=αR
Topic A.5Not started
Galilean and special relativity
This HL-only subtopic begins with classical relative motion and then shows why the invariance of the speed of light requires a new relationship between space and time. Students use Lorentz transformations and spacetime ideas quantitatively.
Describe inertial reference frames and use Galilean transformations at low speeds.
Use classical relative velocity and recognize its limitations near the speed of light.
State and apply the two postulates of special relativity.
Calculate the Lorentz factor γ.
Use Lorentz transformations for position and time in one-dimensional motion.
Apply relativistic velocity addition.
Use the spacetime interval and distinguish proper time from coordinate time.
Calculate time dilation and length contraction.
Explain the relativity of simultaneity.
Interpret basic spacetime diagrams and relate their axes to relative speed.
Use high-speed particle observations such as atmospheric muons as evidence for relativistic effects.
Key formulas
Classical relative velocity
vB/A=vB/S−vA/S
Uniform frame motion
xoriginofS′=vt
Galilean position transformation
x′=x−vt,t′=t
Inverse Galilean transformation
x=x′+vt,t=t′
Galilean velocity transformation
ux′=ux−v
Acceleration invariance classically
ax′=ax
Vacuum light speed
c≈2.998×108ms−1
Stationary light-clock path
L=2cΔτ
Moving light-clock geometry
(2cΔt)2=L2+(2vΔt)2
Dimensionless speed
β=cv
Lorentz factor
γ=1−β21=1−c2v21
Speed from Lorentz factor
cv=1−γ21
Lorentz position transformation
x′=γ(x−vt)
Lorentz time transformation
t′=γ(t−c2vx)
Transverse coordinates
y′=y,z′=z
Inverse position transformation
x=γ(x′+vt′)
Inverse time transformation
t=γ(t′+c2vx′)
Forward collinear velocity addition
u=1+c2u′vu′+v
Inverse velocity transformation
u′=1−c2uvu−v
Dimensionless velocity form
cu=1+(cu′)(cv)cu′+cv
One-dimensional spacetime interval
Δs2=c2Δt2−Δx2
Three-dimensional spacetime interval
Δs2=c2Δt2−Δx2−Δy2−Δz2
Inertial-clock proper time from a one-dimensional interval
Δτ=Δt2−c2Δx2
Interval classification
Δs2>0timelike,Δs2=0lightlike,Δs2<0spacelike
Time dilation for uniform relative motion
Δt=γΔτ
Uniform-motion proper time
Δτ=γΔt
Travel distance in a frame
d=vΔt
Length contraction
L=γL0=L01−c2v2
Proper length from contracted length
L0=γL
Simultaneous endpoint condition
Δtmeasuringframe=0
Time-separation transformation
Δt′=γ(Δt−c2vΔx)
Simultaneous in S
Δt=0⟹Δt′=−γc2vΔx
Einstein synchronization condition
tB=2tsend+treturn
Light-ray worldlines through the origin
x=±ct
Constant-velocity worldline and angle to the time axis
x=x0+vt=x0+cv(ct),tanθ=c∣v∣
Moving time axis
x=vt
Moving space axis
ct=cvx
Causal speed condition
ΔtΔx≤c
Core relativity chain
β=cv⟹γ=1−β21
One-dimensional inertial-clock proper-time check
v=ΔtΔx,Δτ=γΔt=Δt2−c2Δx2
Low-speed consistency
v≪c⟹γ≈1
Unit 2
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The Particulate Nature of Matter
Theme B connects microscopic particle models with macroscopic thermal behaviour, energy balance, gases, thermodynamic processes and electric circuits. At HL, thermodynamics formalizes heat, work, internal energy and entropy.
32 hours estimated ·5 topics
Unit 2 progress0%
Topics in this unit
Topic B.1Not started
Thermal energy transfers
Thermal physics links temperature and internal energy to microscopic particle behaviour, then examines heating, phase changes, conduction and thermal radiation.
Distinguish temperature from internal energy using a particle model.
Use the Kelvin temperature scale and convert between kelvin and degrees Celsius when appropriate.
Calculate energy transfers using specific heat capacity and specific latent heat.
Describe conduction through particle interactions.
Use black-body radiation concepts and the Stefan–Boltzmann relationship.
Connect temperature and peak wavelength using Wien’s displacement relationship.
Relate luminosity and distance to apparent brightness.
Key formulas
Energy conservation for an isolated system
Ebefore=Eafter
Average rate of energy transfer
P=ΔtΔE
Density
ρ=Vm
Mass from density
m=ρV
Celsius to Kelvin
T=θ+273.15
Equal temperature intervals
ΔT(K)=Δθ(∘C)
Mean translational kinetic energy of an ideal-gas molecule
Ek=23kBT
Internal-energy components
U=Emicroscopickinetic+Eintermolecularpotential
Simple stationary-sample energy balance
ΔU=Ein−Eout
Energy for a temperature change
Q=mcΔT
Heat capacity
C=mc
Ideal calorimetry balance
Qlost=Qgained
Magnitude of latent-heat transfer
Q=mL
Multi-stage heating
Qtotal=mc1ΔT1+mL+mc2ΔT2
Latent heat from constant power
L=mPΔt
Steady thermal conduction through a slab
P=LkAΔT
Thermal resistance of one uniform layer
Rth=kAL
Power from thermal resistance
P=RthΔT
Emissivity
ε=PblackbodyPemitted
Absorptivity
a=PincidentPabsorbed
Physical range of emissivity
0≤ε≤1
Stefan–Boltzmann law
P=εσAT4
Net radiative power to an isothermal black-body enclosure
Pnet=εσA(T4−Ts4)
Black-body stellar luminosity
L=4πR2σT4
Wien's displacement law
λmaxT=bW
Temperature from peak wavelength
T=λmaxbW
Apparent brightness
b=4πd2L
Luminosity from observations
L=4πd2b
Stellar radius from luminosity and temperature
R=4πσT4L
Electrical energy input
E=Pt=VIt
Experimental specific heat capacity
c=mΔTVIt
Experimental specific latent heat
L=mPΔt
Topic B.2Not started
Greenhouse effect
The greenhouse-effect subtopic applies radiation and energy-balance ideas to planetary atmospheres. It emphasizes modelling, absorption and emission rather than memorizing a single climate narrative.
Distinguish incoming short-wavelength solar radiation from longer-wavelength thermal radiation emitted by Earth.
Explain how atmospheric gases absorb and re-emit infrared radiation.
Use energy-balance reasoning to discuss equilibrium temperature.
Interpret absorption spectra and identify how molecular properties affect greenhouse behaviour.
Evaluate simplified greenhouse models and recognize their assumptions and limitations.
Key formulas
Top-of-atmosphere energy imbalance
Fnet=Fabsorbed−Foutgoing
Radiative equilibrium
Fabsorbed=Foutgoing
Wien's displacement law
λmaxT=bW
Peak wavelength
λmax=TbW
Projected area of a spherical planet
Aprojected=πR2
Total incident solar power
Psolar=SπR2
Global-mean incident solar flux
Fsolar=4S
Albedo
α=PincidentPreflected
Absorbed shortwave power
Pabsorbed=(1−α)Pincident
Global-mean absorbed solar flux
Fabsorbed=4(1−α)S
Stefan–Boltzmann emission
P=εσAT4
Emitted longwave flux
Femitted=εσT4
Emissivity range
0≤ε≤1
Uniform-emitter planetary equilibrium balance
(1−α)SπR2=4πR2εσT4
Uniform grey-emitter equilibrium temperature
T=[4εσ(1−α)S]41
Photon energy
Eγ=hf=λhc
Atmospheric spectral energy accounting (negligible scattering/reflection)
Pincident=Ptransmitted+Pabsorbed
Surface–effective temperature difference
ΔTgreenhouse≈Tsurface−Te
Initial enhanced-effect imbalance
Fnet=Fabsorbed−Foutgoing>0
Albedo-change forcing estimate
ΔFα=−4SΔα
Simplified climate response
ΔT=λcΔF
Stored energy per unit area
AΔE=CAΔT
Constant-imbalance response time
Δt=FnetCAΔT
Absorbed fraction from measured albedo
fabsorbed=1−α
Planetary absorbed power
Pabsorbed=(1−α)SπR2
Equilibrium test
Pabsorbed=?Poutgoing
Topic B.3Not started
Gas laws
This subtopic connects pressure, volume and temperature to a microscopic model of gas particles. Students move between empirical gas laws, the ideal-gas equation and kinetic-theory interpretations.
Use the ideal-gas equation for a fixed amount of gas.
Interpret pressure as the result of particle collisions with container walls.
Connect absolute temperature to mean random kinetic energy.
Interpret p–V and related graphs for gas processes.
Solve problems involving changes of state for an ideal gas.
Key formulas
Definition of pressure
p=AF⊥
Absolute and gauge pressure
pabsolute=pgauge+patmospheric
Normal momentum change at an elastic rebound from a stationary smooth wall
∣Δpx∣=2m∣vx∣
Average force from momentum transfer
Faverage=ΔtΔptotal
Microscopic route to pressure
p=A1ΔtΔptotal
Mean translational kinetic energy
⟨Ek⟩=21m⟨v2⟩=23kBT
Root-mean-square molecular speed
vrms=m3kBT=M3RT
Internal energy of a monatomic ideal gas
U=23NkBT=23nRT
Particle number and amount
N=nNA
Amount from mass
n=Mmsample
Boyle's law proportionality
p∝V1(T,n constant)
Boyle's law between two states
p1V1=p2V2
Constant-pressure relationship
TV=constant⇒T1V1=T2V2
Constant-volume relationship
Tp=constant⇒T1p1=T2p2
Molar form of the ideal-gas equation
pV=nRT
Particle form and constant bridge
pV=NkBT,R=NAkB
Combined gas law for fixed amount
T1p1V1=T2p2V2
Quasistatic boundary work done by a gas
Wby=∫V1V2pdV
Work sign convention and constant-pressure quasistatic work
Won=−Wby,Wby=pΔVat constant p
Kinetic-theory pressure equation
pV=31Nm⟨v2⟩
Density form of the kinetic equation
p=31ρvrms2
Mechanical meaning of temperature
21m⟨v2⟩=23kBT
Compressibility factor
Z=nRTpV
Percentage deviation from ideal behaviour
percentage deviation=∣Z−1∣×100%
First-order maximum-uncertainty estimate for a product
pVΔ(pV)≈pΔp+VΔV
Boyle-law linear form
p=(pV)(V1)
Topic B.4Not started
Thermodynamics
Thermodynamics is an HL-only treatment of energy transfer in macroscopic systems. It combines the first law, p–V work, ideal-gas internal energy, entropy, the second law and heat-engine limits.
Use the first law with a consistent sign convention for heat transferred to a system and work done by the system.
Calculate work in constant-pressure expansion or compression and interpret work as area under a p–V curve.
Calculate the internal-energy change of a monatomic ideal gas.
Analyse isovolumetric, isobaric, isothermal and adiabatic processes.
Use the monatomic ideal-gas adiabatic relationship.
Apply entropy change ΔS = ΔQ/T for reversible heat transfer at constant temperature.
Interpret entropy statistically using S = kB lnΩ.
Use the second law to explain the direction of spontaneous processes and the impossibility of complete conversion of heat into work in a cyclic engine.
Analyse cyclic heat engines and calculate efficiency.
Calculate the maximum theoretical efficiency of a Carnot engine operating between two temperatures.
Key formulas
Ideal-gas equation
pV=nRT
Particle form of the ideal-gas equation
pV=NkBT
Change in a state function
ΔU=Uf−Ui
First law
ΔU=Q−W
Heat from the first law
Q=ΔU+W
Complete-cycle condition
ΔUcycle=0
Quasi-static p–V work
W=∫ViVfpdV
Constant-pressure work
W=p(Vf−Vi)
Straight-path graph area
W=2pi+pf(Vf−Vi)
Monatomic internal energy
U=23nRT
Particle form
U=23NkBT
Monatomic internal-energy change
ΔU=23nRΔT
State-point form
U=23pV
Isochoric work
WV=0
Isochoric first law
QV=ΔU
Isobaric work for an ideal gas
Wp=pΔV=nRΔT
Isobaric heat for a monatomic ideal gas
Qp=25nRΔT
Isothermal state relation
piVi=pfVf
Isothermal internal-energy change
ΔU=0
Reversible isothermal work
W=nRTln(ViVf)
Isothermal energy balance
Q=W
Adiabatic first law
Q=0⇒ΔU=−W
Reversible adiabatic pressure relation
pVγ=constant
Reversible adiabatic temperature relation
TVγ−1=constant
Monatomic heat-capacity ratio
γ=35
Reversible adiabatic work
W=γ−1piVi−pfVf
Cycle internal-energy change
ΔUcycle=0
Cycle energy balance
Qnet=Wnet
Rectangular-cycle work
∣Wnet∣=(phigh−plow)(Vhigh−Vlow)
Reversible constant-temperature entropy change
ΔS=TQrev
General reversible entropy change
ΔS=∫ifTdQrev
Total entropy change
ΔStotal=ΔSsystem+ΔSsurroundings
Boltzmann entropy
S=kBlnΩ
Entropy change from multiplicity
ΔS=kBln(ΩiΩf)
Boltzmann constant
kB=1.380649×10−23JK−1
Second-law inequality
ΔStotal≥0
Reversible limit
ΔStotal=0
Irreversible spontaneous process
ΔStotal>0
Heat-engine energy balance
W=QH−QC
Thermal efficiency
η=QHW=1−QHQC
Carnot efficiency
ηC=1−THTC
Real-engine limit
0<ηreal<ηC<1
Topic B.5Not started
Current and circuits
Circuit physics models the movement of charge and the transfer of electrical energy. Students use potential difference, current, resistance, power and Kirchhoff-type reasoning in direct-current networks.
Define current as rate of flow of charge and potential difference as energy transferred per unit charge.
Use resistance and Ohm’s law for ohmic components.
Interpret current–voltage characteristics for common components.
Combine resistors in series and parallel.
Use conservation of charge at junctions and energy around closed loops.
Calculate electrical power and energy transfer.
Include electromotive force and internal resistance in simple source models.
Key formulas
Average current (or steady current)
I=ΔtΔQ
Quantization of charge
Q=Ne
Current in a conductor
I=nqAvd
Potential difference with specified polarity
VAB=QWtransferred
Electromotive force
ε=QEsupplied
Resistance at an operating point
R=IV
Ohm's law
V=IR(constant physical conditions)
Resistance of a uniform conductor
R=ρAL
Area of a circular wire
A=4πd2
Linear temperature approximation
ρ=ρ0[1+α(T−T0)]
Electrical power
P=VI
Power in a resistor
P=I2R=RV2
Energy transferred at constant voltage and current
E=PΔt=VIΔt
Kirchhoff's junction rule
j=1∑mIj,in=k=1∑nIk,out
Kirchhoff's loop rule
k=1∑nΔVk=0
Equivalent series resistance
Req=R1+R2+⋯
Common voltage across a parallel group
Vgroup=V1=V2=⋯
Total current in parallel
Itotal=I1+I2+⋯
Equivalent parallel resistance
Req1=R11+R21+⋯
Terminal voltage while delivering current
Vterminal=ε−Ir
Current from a real cell
I=R+rε
Internal power transfer
Pinternal=I2r
Unloaded potential divider
Vout=VinR1+R2R2
Uniform potentiometer ratio
VinVout=Lx
Unloaded divider output measured across a sensor
Vout=VinRfixed+RsensorRsensor
Qualitative sensor trends
T↑⇒RNTC↓,L↑⇒RLDR↓
Parallel loading by a voltmeter
Rloaded=R+RVRRV
First-order maximum fractional uncertainty in resistance
RΔR≈VΔV+IΔI
Two resistors in parallel
Rp=R1+R2R1R2
Steady dc operating current from electrical input power
I=VP
Unit 3
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Wave Behaviour
Theme C moves from oscillation to wave propagation, interference, diffraction, standing waves, resonance and Doppler shifts. Higher Level adds a fully quantitative treatment of SHM, diffraction patterns and moving-source/observer Doppler effects.
29 hours estimated ·5 topics
Unit 3 progress0%
Topics in this unit
Topic C.1Not started
Simple harmonic motion
Simple harmonic motion combines the shared SL model with HL phase constants, trigonometric state equations, signed velocity-displacement analysis and quantitative energy through the cycle.
The wave model describes how oscillations transfer energy without net transport of matter. Students work with transverse and longitudinal waves, wave speed, intensity and graphical representations.
Use the laws of reflection and qualitative/quantitative refraction.
Apply Snell’s law and discuss refractive index.
Explain diffraction and how it depends on wavelength relative to aperture size.
Use the principle of superposition.
Analyse two-source interference and Young double-slit fringes.
Analyse the angular structure of a single-slit diffraction pattern and use the first-minimum approximation.
Explain how the single-slit diffraction envelope modifies a two-slit interference pattern.
Use the diffraction-grating equation for multiple-slit interference.
Interpret how changing slit width, spacing, wavelength or number of slits changes observed intensity patterns.
Key formulas
Ray-wavefront geometry
v⊥wavefront
Wave speed from wavefront spacing
v=fλ
Law of reflection
θi=θr
Frequency continuity at a stationary boundary
fi=fr=ft
Power balance at a passive boundary in steady state
Pi=Pr+Pt+Pabs
Refractive index
n=vc
Snell’s law
n1sinθ1=n2sinθ2
Speed–angle–wavelength ratio: nonzero ray angles; use undivided Snell at normal incidence
sinθ2sinθ1=v2v1=λ2λ1=n1n2
Wavelength in a refractive medium
λ=nλ0
Critical-angle form of Snell’s law
n1sinc=n2sin90∘
Critical-angle equation
sinc=n1n2
Total-internal-reflection conditions
n1>n2andθi>c
Diffraction-control ratio
D=aλ
Strong-spreading condition
a≲λ
Same-medium wave relation
v=fλ=constant
Principle of superposition
yresultant=i=1∑Nyi
In-phase amplitude addition
Amax=A1+A2
Opposite-phase resultant amplitude
Amin=∣A1−A2∣
Path difference
Δr=∣r2−r1∣
Constructive and destructive conditions
Δr=mλorΔr=(m+21)λ
Path-induced unwrapped phase-lag magnitude
Δϕ=λ2πΔr
Double-slit path difference
Δr≈s∣sinθ∣≈Ds∣y∣
Bright-fringe position: far field, small angles
ym=smλD
Fringe spacing: far field, small angles
w=sλD
Wavelength from a near-axis fringe pattern
λ=Dws
Far-field rectangular-slit first-minimum condition at normal incidence
bsinθ1=λ
Small-angle first-minimum approximation
θ1≈bλ
First-minimum screen position
y1≈bλD
Central-maximum screen width
W≈b2λD
Interference-factor maxima: normal incidence, far field
dsinθ=mλ
Single-slit envelope minima
bsinθ=pλ
Missing-order condition
m=pbd
Grating phase-matching equation at normal incidence
mλ=dsinθ
Spacing from line density
d=q1
Wavelength from a nonzero grating order at normal incidence
λ=mdsinθ
Highest possible grating-order bound
mmax≤λd
Envelope angular scale
θenv∼bλ
Interference angular spacing near the centre
Δθfringe≈dλ
Angular-to-linear conversion
y≈Dθ
Principal intensity for equal slit amplitudes
Imax=N2I1
Mean fringe spacing
w=NL
Double-slit graph gradient
ΔDΔw=sλ
Percentage uncertainty
%u=∣q∣Δq×100%
Topic C.4Not started
Standing waves and resonance
Standing waves arise from superposition of waves travelling in opposite directions. Resonance occurs when a system is driven near one of its natural frequencies.
Equal ideal length and sound speed: pipe first-harmonic ratio
fclosed−openfopen−open=2
Percentage difference from a model
%difference=∣qmodel∣∣qmeasured−qmodel∣×100%
Topic C.5Not started
Doppler effect
The Doppler effect is the change in observed frequency caused by relative motion between source, observer and wave medium or by relative motion in electromagnetic-wave contexts.
Optional quantitative application: Blood speed inferred from shift
u≈2f0∣cosθ∣∣Δf∣vw,∣cosθ∣>0
Wavelength change from radial velocity
Δλ≈cλ0vr
Signed radial velocity component
ur=ucosθ
Percentage wavelength shift
percentage shift=100λ0λobs−λ0
Approaching-source frequency
fo=fsvw−vsvw
Source speed from observed frequency
vs=vw(1−fofs)
First-order light shift: total relative speed much smaller than c
f0Δf≈cvr≪1
Unit 4
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Fields
Theme D develops gravitational, electric and magnetic field models and then studies charged-particle motion and electromagnetic induction. Higher Level introduces potential-energy and potential-field descriptions as well as induction.
38 hours estimated ·4 topics
Unit 4 progress0%
Topics in this unit
Topic D.1Not started
Gravitational fields
Gravitational fields describe how masses interact at a distance. HL extends force and field strength into gravitational potential, potential energy, orbital energy and escape conditions.
Calculate gravitational field strength around a point or spherical mass.
Interpret gravitational field lines.
Use Kepler’s laws qualitatively and quantitatively in orbital contexts.
Calculate gravitational potential energy and gravitational potential.
Connect field strength to the spatial gradient of potential.
Use equipotential surfaces to reason about work and field direction.
Calculate work done in moving a mass through a potential difference.
Derive or use orbital speed for a circular orbit.
Calculate escape speed from a spherical body.
Analyse energy changes in satellites and other gravitational systems.
Key formulas
Definition of gravitational field strength
g=mF
Weight
W=mg
Equivalent field-strength units
1Nkg−1=1ms−2
Newton's law of gravitation
F=Gr2m1m2
Gravitational constant
G≈6.67×10−11Nm2kg−2
Inverse-square force ratio
F1F2=m1,1m2,1m1,2m2,2(r2r1)2
Radial gravitational field strength
g=Gr2M
Force on a mass in a field
F=mg
Source mass from field data
M=Ggr2
Inverse-square field ratio
g1g2=(r2r1)2
Radial vector direction
g=−r2GMr^
Area of a sphere
A=4πr2
Field strength at altitude
g(h)=(R+h)2GM
Altitude-to-surface field ratio
g0g(h)=(R+hR)2
Optional first-order estimate of small-height fractional change
g0Δg≈−R2h(h≪R)
Superposition of gravitational fields
gnet=i=1∑Ngi
Two-mass cancellation condition
x2GM1=(d−x)2GM2
Zero-field position between two masses
x=M1+M2dM1
Gravitational potential energy
Ep=−rGMm
Gravitational potential
Vg=−rGM
Energy-potential relation
Ep=mVg
Radial field-potential relation
gr=−drdVg
Finite-difference estimate
gr≈−ΔrΔVg
Spherical-mass radial field
gr=−r2GM
Potential-energy change
ΔEp=mΔVg=m(VB−VA)
Work done by gravity
Wgravity=−ΔEp=−mΔVg
External transfer with no kinetic-energy change or other losses
Wexternal=ΔEp=mΔVg
Optional ellipse geometry: periapsis and apoapsis distances
rp=a(1−e),ra=a(1+e)
Kepler's equal-area statement
ΔtΔA=constant
Optional small-sector area approximation
ΔA≈21r2Δθ
Kepler's third-law ratio
a13T12=a23T22
Newton–Kepler orbital relationship
T2=GM4π2a3
Central mass from an orbit
M=GT24π2a3
Circular-orbit speed
vorbit=rGM
Circular-orbit force balance
r2GMm=rmv2
Circular-orbit period
T=2πGMr3
Circular-orbit kinetic energy
Ek=2rGMm
Circular-orbit potential energy
Ep=−rGMm=−2Ek
Circular-orbit total energy
E=−2rGMm=−Ek
Escape-energy condition
21mvescape2−rGMm=0
Escape speed
vescape=r2GM
Escape-orbit relation
vescape=2vorbit
Circular-orbit energy change
ΔE=2GMm(r11−r21)
Mechanical energy: gravity alone, fixed source and no drag
Ek+Ep=constant
Bound-or-escape test
E<0bound,E≥0escape possible
Orbital period from central mass
T=2πGMa3
Gradient of T squared against a cubed
S=GM4π2
Small-angle simple-pendulum estimate of g (SHM link)
g=Tp24π2L
Inverse-square scaling check
g∝r2M
Orbital-period scaling
T1T2=(a1a2)23
Percentage difference from surface g
percentage change=100g0g(h)−g0
Topic D.2Not started
Electric and magnetic fields
This subtopic treats electrostatic and magnetic interactions through force and field models. HL adds electric potential and potential energy, allowing direct comparison with gravitational fields.
Optional long-wire exterior model: Two-condition field ratio
B1B2=I1r2I2r1
Turn density
n=LN
Optional long air-core model: Solenoid field scaling
B∝nI
Optional long air-core model: Solenoid comparison
B1B2≈n1I1n2I2
Electrostatic-force scaling
F∝r2∣q1q2∣
Field-force connection
F=qE
Combined-source rule
Xnet=i=1∑NXi(X=F,E,B)
Topic D.3Not started
Motion in electromagnetic fields
This subtopic applies electric and magnetic forces to moving charges and current-carrying conductors. It includes circular particle motion, velocity selection and forces between currents.
Calculate the force on a charge in a uniform electric field.
Calculate magnetic force on a moving charge and determine its direction.
Analyse circular motion of charged particles in a uniform magnetic field.
Use crossed electric and magnetic fields as a velocity selector.
Calculate force on a current-carrying conductor in a magnetic field.
Analyse the force per unit length between parallel current-carrying wires.
Key formulas
Electric force
FE=qE
Magnetic force
FB=qv×B
Combined Lorentz force
F=q(E+v×B)
Electric acceleration
a=mqE
Velocity under constant electric acceleration
v=u+mqEt
Displacement under constant electric acceleration
s=ut+21mqEt2
Transit time through plates
t=vxL
Transverse deflection
y=21mqEt2
Electric-field trajectory
y=2mvx2qEx2
Magnetic-force magnitude
FB=∣q∣vBsinθ
Perpendicular speed
v⊥=vsinθ
Magnetic power
PB=FB⋅v=0
Magnetic centripetal balance
∣q∣vB=rmv2
Magnetic orbit radius
r=∣q∣Bmv
Magnetic orbit period
T=∣q∣B2πm
Velocity components
v∥=vcosθ,v⊥=vsinθ
Helix radius
r=∣q∣Bmv⊥
Helix pitch
p=∣v∥∣T=∣q∣B2πm∣v∥∣
Selector force balance
∣q∣E=∣q∣vB
Selected speed
v=BE
Initial transverse force magnitude in the standard selector geometry
Fnet=∣q∣∣E−vB∣
Charge-to-mass ratio from a magnetic orbit
m∣q∣=Brv
Selector plus analyser
m∣q∣=BsBarE
Mass-to-radius comparison
r1r2=m1∣q2∣m2∣q1∣
Conductor-force magnitude
F=BILsinθ
Vector conductor force
F=IL×B
Force per unit active length
LF=BIsinθ
Field of wire 1 at wire 2
B1=2πdμ0I1
Parallel-wire force per length
LF=2πdμ0I1I2
Permeability of free space
μ0≈4π×10−7TmA−1
Field from current balance: nonzero current, length and sine of angle
B=ILsinθF
Current-balance gradient
ΔIΔF=BL(θ=90∘)
Force reversal checks
I→−I⇒F→−F,B→−B⇒F→−F
Electromagnetic decision equation
F=q(E+v×B)
Magnetic-radius scaling
r∝∣q∣Bmv⊥
Parallel-wire scaling
LF∝dI1I2
Topic D.4Not started
Induction
Electromagnetic induction is an HL-only subtopic describing how changing magnetic flux produces an emf. It links generators, moving conductors and energy conservation through Faraday’s and Lenz’s laws.
Optional extension: motional emf along a specified directed path
E=∫(v×B)⋅dℓ
Rotating-coil flux linkage
NΦ=NBAcos(ωt)
Sinusoidal generator emf
E=NBAωsin(ωt)
Peak generator emf
E0=NBAω
Frequency and angular speed
ω=2πf
Period–frequency relation
T=f1
Adjacent extrema time separation: sinusoidal linkage and emf
Δt=4T
Peak-emf proportionality
E0∝f
Magnitude of sinusoidal linkage–emf phase separation
Δφ=2π
Optional: fixed linear inductor flux–current relation
NΦ=LI
Optional: self-induced emf for constant inductance
EL=−LdtdI
Optional: magnetic energy of a linear lossless inductor
UB=21LI2
Optional: henry unit equivalence
1H=1VsA−1
Core induction chain
Φ=BAcosθ⟶NΦ⟶E=−dtd(NΦ)
Current magnitude: passive resistive circuit, negligible self-inductance
I=R∣E∣
Rotating-coil maximum
E0=2πfNBA
Unit 5
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Nuclear and Quantum Physics
Theme E follows the development of atomic and nuclear models, then extends into wave–particle duality, radioactive decay, fission, fusion and stellar physics. The HL-only quantum subtopic is one of the most conceptually distinctive parts of the course.
39 hours estimated ·5 topics
Unit 5 progress0%
Topics in this unit
Topic E.1Not started
Structure of the atom
This subtopic traces evidence for atomic structure from scattering and spectra to photons and quantized energy levels. HL adds quantitative nuclear-size and Bohr-model relationships.
Percentage deviation from a positive reference wavelength
percentage difference=100λref∣λmeas−λref∣%
Particle-count checklist
p=Z,n=A−Z,Q=(Z−Ne)e
One-photon bound-bound energy checklist: consistent units, vacuum wavelength
Eγ=∣Ei−Ef∣=hf=λhc
Energy-wavelength scaling
Eγ∝f∝λ1
Topic E.2Not started
Quantum physics
Quantum physics is HL-only. It uses experimental evidence to show that electromagnetic radiation and matter each display both wave-like and particle-like behaviour, depending on the measurement context.
Radioactive decay links nuclear stability, random decay processes and radiation to energy and conservation laws. HL adds the exponential-decay model and a deeper treatment of nuclear stability and spectra.
Alpha/beta energy balance: Q referenced to ground-state products
Q=Kproducts+Eexcitation
Beta energy sharing: selected daughter state and negligible neutrino rest energy
Q=Kβ+Kν+Krecoil
Electric force
F=qE
Magnetic-path radius
r=∣q∣Bp
Steady isotropic point source: negligible attenuation and background
I∝r21
Average activity
A=ΔtΔNdecays
Measured count rate
C=ΔtNcounts
Idealized net detection: one relevant emission per decay
Csource=εgA
Parents after integer half-lives
N=N0(21)n
Activity after integer half-lives
A=A0(21)n
Elapsed complete half-lives
n=T21t
Rate equation for undecayed nuclei
dtdN=−λN
Exponential decay law
N=N0e−λt
Time from population ratio
t=λ1ln(NN0)
Activity and undecayed nuclei
A=−dtdN=λN
Exponential activity law
A=A0e−λt
Common remaining fraction
A0A=N0N=e−λt
Half-life and decay constant
T21=λln2
Decay constant from half-life
λ=T21ln2
Repeated-halving exponential form
N=N0(21)T21t
Background correction
Cnet=Cmeasured−Cbackground
Supporting counting statistics: independent raw Poisson counts
σN≈N
Supporting fractional uncertainty: sufficiently many raw counts
NσN≈N1
Steady isotropic point source, negligible attenuation: distance trend
I1I2=(r2r1)2
Time after complete half-lives
t=nT21
Single parent, fixed response: integer-half-life net count model
Cnet=(Cmeasured−Cbackground)=C0(21)n
Topic E.4Not started
Fission
Nuclear fission releases energy when a heavy nucleus splits into more tightly bound products. The subtopic connects binding energy, neutron multiplication, chain reactions and reactor control.
Same nonrelativistic neutron: positive initial energy
KiKf=(vivf)2
Supporting toy model: extra fractional loss, all other effects fixed
kafter=k0(1−fabs)
Control change
Δk=kafter−kbefore
Mean absorption rate over a positive interval
Rabs=ΔtNabsorbed
Mean thermal-energy transfer over a positive interval
P=ΔtQ
Steady single-phase coolant: constant heat capacity, negligible other changes
P=m˙cΔT
Power-station efficiency
η=PthermalPelectrical
Supporting model: steady isotropic point source, negligible attenuation/background
I1I2=(r2r1)2
Supporting concept: mean absorbed dose in the stated mass
D=mEabsorbed
Supporting concept: equivalent dose to one tissue, one radiation type
H=wRD
Single isolated parent, no replenishment: integer-half-life activity
A=A0(21)n
Elapsed whole half-lives, not a universal safe-storage duration
t=nT21
Electrical-energy audit: Q is mean recoverable heat per fission here
Eelectrical=ηNfQ
Topic E.5Not started
Fusion and stars
This subtopic applies nuclear physics and radiation to stars. Students connect fusion, stellar equilibrium, luminosity, temperature, distance and stellar evolution.