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 develops the mechanics foundation of Physics SL. It moves from describing motion to explaining it with forces and momentum, then to analysing systems through work, energy and power.
27 hours estimated ·3 topics
Unit 1 progress0%
Topics in this unit
Topic A.1Not started
Kinematics
Kinematics describes motion without initially asking what causes it. Students work in one and two dimensions and move fluently among words, equations, vectors and motion graphs.
Distinguish distance from displacement and speed from velocity.
Calculate average and instantaneous velocity, speed and acceleration.
Interpret position–time, velocity–time and acceleration–time graphs using gradients and areas.
Apply the constant-acceleration equations with a consistent sign convention.
Resolve projectile motion into independent horizontal and vertical components.
Describe qualitatively how fluid resistance changes projectile trajectories and leads to 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 topic links interactions to changes in motion. Students use Newton’s laws, free-body diagrams, contact forces, momentum and circular motion to model real systems.
Apply Newton’s three laws and identify action–reaction pairs correctly.
Draw and analyse free-body diagrams, resolving forces into useful components.
Model normal force, friction, tension, Hooke’s-law spring forces, viscous drag and buoyancy.
Use momentum and impulse, including conservation of momentum in collisions and explosions.
Relate resultant force to acceleration and to rate of change of momentum.
Analyse uniform circular motion using centripetal acceleration and resultant inward 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 often provide a shorter route than force-and-acceleration methods. Students learn to track transfers among kinetic, gravitational, elastic and other energy stores and to quantify efficiency and power.
Apply conservation of energy to mechanical and mixed-energy systems.
Calculate work done by a constant force at an angle to displacement.
Read energy transfers from Sankey diagrams and distinguish useful from dissipated energy.
Use kinetic, gravitational potential and elastic potential energy relationships.
Interpret force–displacement graphs through the area under the graph.
Calculate power as rate of energy transfer and evaluate efficiency.
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
Unit 2
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The Particulate Nature of Matter
Theme B connects microscopic particle models with thermal behaviour, radiation, climate, gases and electric circuits. It is one of the most varied parts of Physics SL.
24 hours estimated ·4 topics
Unit 2 progress0%
Topics in this unit
Topic B.1Not started
Thermal energy transfers
Students connect temperature and internal energy to molecular motion, then quantify heating, phase change, conduction and radiation. The topic also introduces the radiation laws used later in stellar physics.
Use the molecular model to distinguish solids, liquids and gases.
Relate Kelvin temperature to average molecular kinetic energy and convert between Kelvin and Celsius.
Calculate density, specific heat energy and latent heat energy.
Explain conduction and convection and calculate steady thermal conduction through a material.
Apply the Stefan–Boltzmann law to black-body radiation.
Use luminosity, apparent brightness and Wien’s displacement law to infer stellar properties.
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
This topic applies radiation physics and energy balance to the Earth–atmosphere system. Students quantify albedo, emissivity and incoming solar power and explain how greenhouse gases absorb and re-emit infrared radiation.
Apply conservation of energy to planetary energy-balance models.
Use emissivity to compare real surfaces with ideal black-body radiation.
Use albedo to describe the fraction of incident energy reflected or scattered.
Use the solar constant and projected area to estimate mean incoming intensity.
Explain the role of major greenhouse gases and why molecular energy levels allow infrared absorption.
Distinguish the natural greenhouse effect from the enhanced greenhouse effect caused by human activity.
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
Gas laws connect macroscopic pressure, volume and temperature to a microscopic model of moving particles. Students use both empirical gas relationships and kinetic-theory ideas.
Define pressure and amount of substance and distinguish particle number N from amount n in moles.
Use constant-pressure, constant-volume and constant-temperature gas relationships.
Apply the ideal gas equation in different forms.
Interpret pressure–volume diagrams for changes of state.
Explain gas pressure through molecular collisions and momentum change.
Relate pressure and internal energy to molecular speeds and temperature.
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.5Not started
Current and circuits
Electric circuits are treated through charge flow, energy transfer, resistance and source behaviour. Students analyse both series and parallel combinations and connect macroscopic circuit quantities to a particle model.
Define current as charge flow per unit time and potential difference as energy transferred per unit charge.
Use Ohm’s law for ohmic conductors and interpret current–voltage characteristics.
Relate resistance to resistivity, conductor length and cross-sectional area.
Calculate electrical power and energy transfer.
Analyse current, voltage and equivalent resistance in series and parallel circuits.
Model real cells using emf and internal resistance.
Interpret the behaviour of thermistors, light-dependent resistors and potentiometers.
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 develops oscillations and waves as models for systems that transfer energy and information. Students study simple harmonic motion, travelling waves, interference, diffraction, standing waves, resonance and the Doppler effect.
17 hours estimated ·5 topics
Unit 3 progress0%
Topics in this unit
Topic C.1Not started
Simple harmonic motion
Simple harmonic motion (SHM) is a model for oscillations in which acceleration is proportional to displacement and directed back toward equilibrium. At SL, the emphasis is on the defining relation, period and qualitative energy changes.
Optional HL link: grating principal maxima at normal incidence
dsinθ=mλ
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 the superposition of identical waves travelling in opposite directions. Boundary conditions determine the allowed modes in strings and pipes, while resonance describes large responses near a system’s natural frequency.
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 describes the observed change in frequency or wavelength caused by relative motion between a source and an observer. At SL, students study qualitative sound-wave cases and the small-speed approximation for light.
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
Optional HL link: Approaching-source frequency
fo=fsvw−vsvw
Optional HL link: 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 fields as models of interactions at a distance. Students then study the motion and forces of charged particles and current-carrying conductors in electromagnetic fields.
19 hours estimated ·3 topics
Unit 4 progress0%
Topics in this unit
Topic D.1Not started
Gravitational fields
Students model gravitational interactions using Newton’s law and field strength, and connect these ideas to orbital motion through Kepler’s laws.
State and apply Kepler’s three laws of orbital motion qualitatively and quantitatively where appropriate.
Apply Newton’s universal law of gravitation to point masses and suitable spherical bodies.
Define gravitational field strength as force per unit mass.
Calculate gravitational field strength around a spherical mass.
Sketch and interpret gravitational field lines.
Recognize when the near-Earth approximation g ≈ constant is appropriate and when an inverse-square model is required.
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
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
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 topic introduces electric charge, electrostatic forces, electric field strength and magnetic-field patterns. SL students focus on forces and field representations rather than electric potential energy and potential, which are HL extensions.
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
Students combine field ideas with mechanics to analyse charged particles and currents in electric and magnetic fields. Magnetic forces often produce circular motion because they act perpendicular to velocity.
Describe charged-particle motion in uniform electric fields.
Describe charged-particle motion in uniform magnetic fields.
Analyse motion in crossed perpendicular electric and magnetic fields.
Calculate the magnetic force on a moving charge.
Calculate the force on a current-carrying conductor in a magnetic field.
Use the force per unit length between parallel current-carrying wires.
Determine magnetic-field direction from current and force directions.
Use circular-motion ideas to determine or compare charge-to-mass ratios.
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
Unit 5
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Nuclear and Quantum Physics
Theme E moves from atomic evidence and spectra to nuclear stability, radioactive decay, fission, fusion and stellar evolution. It links microscopic physics with some of the largest scales in the universe.
23 hours estimated ·4 topics
Unit 5 progress0%
Topics in this unit
Topic E.1Not started
Structure of the atom
Students use experimental evidence to develop the nuclear model of the atom and connect discrete atomic energy levels to line spectra and photons.
Optional grating support: spacing from line density
d=ng1
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.3Not started
Radioactive decay
This topic combines nuclear structure, mass–energy, stability and the statistical nature of radioactive decay. At SL, students use half-life through discrete repeated-halving reasoning rather than the full exponential decay equations used at HL.
Explain mass defect and binding energy and interpret the binding-energy-per-nucleon curve.
Apply mass–energy equivalence to nuclear reactions.
Describe the strong nuclear force as a short-range attractive interaction between nucleons.
Describe alpha, beta-minus, beta-plus and gamma decay and balance nuclear equations.
Explain the role of neutrinos and antineutrinos in beta processes.
Compare penetration and ionizing ability of alpha, beta and gamma radiation.
Use activity, count rate and half-life for integer numbers of half-lives.
Correct measured count rates for background radiation.
Key formulas
Neutron number
N=A−Z
Nucleon count
A=Z+N
Ion charge
Q=(Z−Ne)e
Mass–energy equivalence
ΔE=Δmc2
Atomic mass unit
1u≈1.66054×10−27kg
Energy equivalent of u
1uc2≈931.5MeV
Nuclear-mass defect
Δm=Zmp+(A−Z)mn−mnucleus
Atomic-mass defect
Δm≈ZmH+(A−Z)mn−matom
Binding energy
Eb=Δmc2
Binding energy per nucleon
Eb=AEb
Total binding from average
Eb=AEb
Binding-energy change: unchanged total proton and neutron counts
Q=Eb,final−Eb,initial
Nuclear length scale
1fm=10−15m
Neutron-to-proton ratio
Rnp=ZN
Proton-pair count
Npp=2Z(Z−1)
Nucleon-number conservation
Aparent=Adaughters+Aemitted
Charge-number conservation
Zparent=Zdaughters+Zemitted
Nuclear reaction energy
Q=(minitial−mfinal)c2
General alpha decay
ZAX→Z−2A−4Y+24He
Momentum conservation from rest
pα+pd=0
Released kinetic energy
Q=Kα+Kd
Beta-minus decay
ZAX→Z+1AY+−10e+νˉe
Beta-plus decay
ZAX→Z−1AY++10e+νe
Nucleon changes in energetically allowed beta decays
n→p+e−+νˉe,p→n+e++νe
Gamma transition
ZAX∗→ZAX+γ
Gamma photon energy
Eγ=hf=λhc
Photon momentum
pγ=cEγ
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
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. Students connect binding energy, chain reactions and reactor design to the production of electrical energy and the management of radioactive products.
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
Fusion powers stars and provides the link between nuclear physics and stellar evolution. Students use equilibrium, HR diagrams, parallax and radiation relationships to interpret stars.