Nuclear Reactions
| Sitio: | Young Education |
| Curso: | Nuclear and Particle Physics |
| Libro: | Nuclear Reactions |
| Impreso por: | ゲストユーザ |
| Fecha: | viernes, 25 de septiembre de 2026, 02:37 |
1. Radioactive Decay
Learning outcomes
- I can distinguish radioactive decay from particle interactions.
- I can identify alpha, beta, and gamma decay.
- I can explain how nuclei change during decay.
- I can write nuclear decay equations.
- I can apply conservation laws to decay equations.
What Is Radioactive Decay?
Radioactive decay is the spontaneous transformation of an unstable atomic nucleus into a more stable state.
During radioactive decay, a nucleus may emit:
- an alpha particle
- a beta particle
- a gamma-ray photon
- other particles in more advanced decay processes
The original unstable nucleus is called the parent nucleus.
The nucleus formed after the decay is called the daughter nucleus.
A general decay can be represented as:
Parent nucleus → daughter nucleus + emitted radiation
Radioactive decay happens naturally and does not need to be triggered by another particle.
Radioactive Decay vs Particle Interactions
Radioactive decay is different from a particle collision or other particle interaction.
In radioactive decay:
one unstable nucleus spontaneously changes
For example:
²³⁸₉₂U → ²³⁴₉₀Th + ⁴₂He
In a particle interaction, two or more particles may interact because they meet or collide:
A + B → C + D
The key difference is:
Radioactive decay begins with an unstable nucleus on its own.
Particle interactions involve particles interacting with one another.
Comparing the Two
| Radioactive Decay | Particle Interaction |
|---|---|
| Begins with an unstable nucleus | Usually involves two or more particles |
| Occurs spontaneously | Requires particles to interact |
| Produces daughter nucleus and radiation | Can produce many different particles |
| Governed by conservation laws | Governed by conservation laws |
| Example: alpha decay | Example: high-energy collision |
Both processes obey fundamental conservation principles.
Why Do Nuclei Undergo Radioactive Decay?
Some nuclei are unstable because their arrangement of protons and neutrons has too much energy or an unfavorable balance.
Factors affecting nuclear stability include:
- neutron-to-proton ratio
- electrostatic repulsion between protons
- nuclear shell structure
- binding energy
- overall nuclear size
An unstable nucleus can transform into a lower-energy, more stable configuration.
The excess energy may be released as particles or electromagnetic radiation.
The Three Main Types of Radioactive Decay
The three radioactive processes most commonly introduced are:
alpha decay
beta decay
gamma decay
Each affects the nucleus differently.
Alpha Decay
An alpha particle consists of:
2 protons + 2 neutrons
It is the same nuclear composition as a helium-4 nucleus.
Its symbol is:
⁴₂He
or:
α
Alpha decay is common in very heavy nuclei.
Example of Alpha Decay
Uranium-238 can undergo alpha decay:
²³⁸₉₂U → ²³⁴₉₀Th + ⁴₂He
Let's examine what changed.
Mass number:
238 → 234
Difference:
−4
Atomic number:
92 → 90
Difference:
−2
Therefore, during alpha decay:
mass number decreases by 4
atomic number decreases by 2
General Alpha Decay Equation
Alpha decay can be represented generally as:
ᴬ_ZX → ᴬ⁻⁴_Z₋₂Y + ⁴₂He
where:
A = mass number
Z = atomic number
After alpha decay:
A → A − 4
Z → Z − 2
Because the atomic number changes, the nucleus becomes a different element.
Example: Completing an Alpha Decay Equation
Suppose:
²²⁶₈₈Ra → ? + ⁴₂He
Mass number of daughter:
226 − 4 = 222
Atomic number:
88 − 2 = 86
Element 86 is radon.
Therefore:
²²⁶₈₈Ra → ²²²₈₆Rn + ⁴₂He
Beta-Minus Decay
In beta-minus decay, a neutron in the nucleus changes into a proton.
At the nucleon level:
n → p + e⁻ + ν̄ₑ
The electron is emitted from the nucleus as a beta-minus particle.
An electron antineutrino is also produced.
What Changes During Beta-Minus Decay?
Because a neutron becomes a proton:
number of protons increases by 1
number of neutrons decreases by 1
The total number of nucleons does not change.
Therefore:
mass number stays the same
atomic number increases by 1
Example of Beta-Minus Decay
Carbon-14 undergoes beta-minus decay:
¹⁴₆C → ¹⁴₇N + e⁻ + ν̄ₑ
Before:
Carbon has:
6 protons
8 neutrons
After:
Nitrogen has:
7 protons
7 neutrons
The mass number remains:
14
but the atomic number changes:
6 → 7
General Beta-Minus Equation
The general form is:
ᴬ_ZX → ᴬ_Z₊₁Y + e⁻ + ν̄ₑ
Sometimes beta-minus particles are written using nuclear-style notation as:
⁰₋₁e
or:
⁰₋₁β
So the equation may also appear as:
ᴬ_ZX → ᴬ_Z₊₁Y + ⁰₋₁β + ν̄ₑ
Why Does the Mass Number Stay the Same?
Beta decay does not remove a nucleon from the nucleus.
Instead:
one neutron changes into one proton
The nucleus still contains the same total number of nucleons.
Therefore:
A remains unchanged
Beta-Plus Decay
Another type of beta decay is beta-plus decay.
In a suitable proton-rich nucleus, a proton effectively changes into a neutron:
p → n + e⁺ + νₑ
The emitted positron is called a beta-plus particle.
What Changes During Beta-Plus Decay?
A proton becomes a neutron.
Therefore:
proton number decreases by 1
neutron number increases by 1
Mass number remains unchanged.
So:
A stays the same
Z decreases by 1
Example of Beta-Plus Decay
Carbon-11 can undergo beta-plus decay:
¹¹₆C → ¹¹₅B + e⁺ + νₑ
Mass number:
11 → 11
Atomic number:
6 → 5
Carbon becomes boron.
General Beta-Plus Equation
ᴬ_ZX → ᴬ_Z₋₁Y + e⁺ + νₑ
or:
ᴬ_ZX → ᴬ_Z₋₁Y + ⁰₊₁β + νₑ
Gamma Decay
A nucleus can sometimes have the correct number of protons and neutrons but still contain excess energy.
Such a nucleus is said to be in an excited state.
The nucleus can release this energy by emitting a gamma-ray photon.
Gamma radiation is high-energy electromagnetic radiation.
A gamma photon is represented as:
γ
Gamma Decay Equation
A simple representation is:
X → X + γ*
The asterisk indicates that the original nucleus is excited.
For example:
⁹⁹ᵐTc → ⁹⁹Tc + γ
During gamma decay:
mass number does not change
atomic number does not change
Only the nuclear energy state changes.
Comparing Alpha, Beta, and Gamma Decay
| Decay | Emitted Particle/Radiation | Change in A | Change in Z |
|---|---|---|---|
| Alpha | ⁴₂He | −4 | −2 |
| Beta-minus | e⁻ + ν̄ₑ | 0 | +1 |
| Beta-plus | e⁺ + νₑ | 0 | −1 |
| Gamma | γ | 0 | 0 |
This table is extremely useful when writing nuclear equations.
A Useful Memory Pattern
Alpha
A − 4
Z − 2
Beta-minus
A unchanged
Z + 1
Beta-plus
A unchanged
Z − 1
Gamma
A unchanged
Z unchanged
Writing Nuclear Decay Equations
A nuclear decay equation must balance important quantities.
For introductory nuclear equations, always check:
mass number
and
atomic number
These reflect conservation of nucleon number and electric charge in the nuclear notation.
For more complete particle descriptions, also consider:
- electric charge
- baryon number
- lepton number
- energy
- momentum
Example: Balancing Alpha Decay
Consider:
²¹⁰₈₄Po → ? + ⁴₂He
Mass numbers must balance:
210 = A + 4
Therefore:
A = 206
Atomic numbers must balance:
84 = Z + 2
Therefore:
Z = 82
Element 82 is lead.
So:
²¹⁰₈₄Po → ²⁰⁶₈₂Pb + ⁴₂He
Checking Conservation in Alpha Decay
For:
²¹⁰₈₄Po → ²⁰⁶₈₂Pb + ⁴₂He
Mass number:
210 = 206 + 4
Atomic number:
84 = 82 + 2
Both balance.
Example: Balancing Beta-Minus Decay
Suppose:
³H → ? + e⁻ + ν̄ₑ
Tritium is hydrogen-3:
³₁H
During beta-minus decay:
A stays 3
Z increases from 1 to 2
Element 2 is helium.
Therefore:
³₁H → ³₂He + e⁻ + ν̄ₑ
Checking Charge More Carefully
For:
³₁H → ³₂He + e⁻ + ν̄ₑ
The nuclear charge before is:
+1
After:
Helium nucleus:
+2
Electron:
−1
Antineutrino:
0
Total:
+2 − 1 = +1
Charge is conserved.
Applying Lepton Number
Consider beta-minus decay:
n → p + e⁻ + ν̄ₑ
Before:
L = 0
After:
Electron:
L = +1
Antineutrino:
L = −1
Total:
L = 0
Lepton number is conserved.
This is one reason the antineutrino must appear in the complete decay equation.
Example: Why This Equation Is Incomplete
Suppose someone writes:
n → p + e⁻
Charge is conserved:
0 = +1 − 1
Baryon number is conserved:
+1 = +1
But lepton number is not.
Before:
L = 0
After:
L = +1
The missing particle is the electron antineutrino:
ν̄ₑ
Therefore the complete equation is:
n → p + e⁻ + ν̄ₑ
Conservation Laws in Alpha Decay
An alpha particle contains:
2 protons + 2 neutrons
Therefore its baryon number is:
B = 4
At the nuclear level, baryon number is equivalent to keeping track of the total number of nucleons.
For example:
²³⁸U → ²³⁴Th + ⁴He
Baryon number:
238 = 234 + 4
So baryon number is conserved.
Conservation Laws in Gamma Decay
Gamma decay:
X → X + γ*
The photon has:
charge = 0
baryon number = 0
lepton number = 0
The nucleus keeps the same number of protons and neutrons.
Energy and momentum are also conserved.
The photon carries away some of the excess energy and momentum.
Radioactive Decay Releases Energy
Radioactive decay occurs when the total mass-energy of the final state is lower than that of the initial state.
The difference appears as energy carried by:
- emitted particles
- daughter nucleus recoil
- electromagnetic radiation
The released energy can be calculated using:
Q = (minitial − mfinal)c²
If:
Q > 0
the decay is energetically allowed.
Recoil of the Daughter Nucleus
Suppose an initially stationary nucleus emits an alpha particle.
The alpha particle travels in one direction.
Momentum must remain conserved.
Therefore the daughter nucleus recoils in the opposite direction.
So:
momentum before = 0
and:
momentum after = palpha + pdaughter = 0
This is why the daughter nucleus cannot simply remain completely stationary after particle emission.
Radioactive Decay Is Random
It is impossible to predict exactly when one particular unstable nucleus will decay.
A specific nucleus might decay:
- almost immediately
- much later
- after an extremely long time
However, for a large number of identical unstable nuclei, the statistical behavior is very predictable.
This leads to the concept of half-life, which describes how quickly a radioactive sample decays.
We will treat half-life separately because it focuses on the statistical rate of radioactive decay rather than the nuclear transformations themselves.
Penetrating Ability
Alpha, beta, and gamma radiation interact with matter differently.
Alpha
Alpha particles are relatively massive and carry charge +2.
They interact strongly with matter and lose energy quickly.
They have:
- high ionizing ability
- low penetrating ability
Beta
Beta particles are electrons or positrons.
They are much lighter than alpha particles.
They typically have:
- moderate ionizing ability
- moderate penetrating ability
Gamma
Gamma rays are photons.
They carry no electric charge.
They typically have:
- lower ionizing ability per interaction
- high penetrating ability
Thick materials may be required to substantially reduce gamma radiation.
Ionizing Radiation
Alpha, beta, and gamma radiation can all ionize matter.
Ionization occurs when enough energy is transferred to remove electrons from atoms or molecules.
Ionizing radiation can therefore alter chemical structures and damage biological molecules.
The degree of biological effect depends on factors including:
- radiation type
- energy
- absorbed dose
- exposure time
- tissue exposed
Radioactive Decay Chains
Sometimes one radioactive decay does not immediately produce a stable nucleus.
The daughter nucleus may itself be radioactive.
It may then decay again.
This creates a decay chain.
For example:
unstable parent → radioactive daughter → another daughter → … → stable nucleus
Heavy radioactive elements such as uranium can undergo long decay chains containing several alpha and beta decays.
Example: Tracking Changes Through Several Decays
Suppose a nucleus undergoes:
one alpha decay
followed by:
two beta-minus decays
Start with:
A = 238
Z = 92
After alpha:
A = 234
Z = 90
After first beta-minus:
A = 234
Z = 91
After second beta-minus:
A = 234
Z = 92
Final:
A = 234
Z = 92
This method allows us to follow changes through a decay chain without memorizing every isotope.
Worked Example: Identify the Decay Type
Consider:
²¹⁴₈₂Pb → ²¹⁴₈₃Bi + ?
Compare the nuclei.
Mass number:
214 → 214
No change.
Atomic number:
82 → 83
Increase of 1.
This is beta-minus decay.
Therefore the missing products include:
e⁻ + ν̄ₑ
So:
²¹⁴₈₂Pb → ²¹⁴₈₃Bi + e⁻ + ν̄ₑ
Worked Example: Identify the Missing Daughter
Consider:
²²²₈₆Rn → X + ⁴₂He
Mass number:
222 − 4 = 218
Atomic number:
86 − 2 = 84
Element 84 is polonium.
Therefore:
²²²₈₆Rn → ²¹⁸₈₄Po + ⁴₂He
Worked Example: Gamma Emission
Suppose an excited cobalt nucleus emits gamma radiation:
⁶⁰Co → ⁶⁰Co + γ*
Mass number:
60 → 60
Atomic number:
27 → 27
No element change occurs.
Only the nuclear energy decreases.
A Reliable Method for Nuclear Decay Equations
When completing a radioactive decay equation:
Step 1: Identify the decay type.
Is it:
- alpha
- beta-minus
- beta-plus
- gamma
Step 2: Write the known particles.
Include the parent nucleus and any emitted particles.
Step 3: Balance mass number.
Check that:
total A before = total A after
Step 4: Balance atomic number.
Check that:
total Z before = total Z after
Step 5: Identify the element.
Use the atomic number to determine the daughter element.
Step 6: Check additional conservation laws.
For beta decay especially, consider:
- electric charge
- baryon number
- lepton number
Step 7: Remember energy and momentum.
Every physical decay must conserve both.
Common Mistakes
Mistake 1: Changing mass number in beta decay
Beta decay changes a neutron into a proton or vice versa.
The total number of nucleons remains the same.
So:
A does not change.
Mistake 2: Treating gamma radiation as a particle with mass number
A gamma photon has:
A = 0
Z = 0
Gamma decay does not change the element.
Mistake 3: Forgetting the neutrino
Complete beta-decay equations require the appropriate neutrino or antineutrino.
Beta-minus:
e⁻ + ν̄ₑ
Beta-plus:
e⁺ + νₑ
Mistake 4: Thinking alpha decay removes only two particles
An alpha particle contains four nucleons:
2 protons + 2 neutrons
So mass number decreases by 4.
Did You Know?
The word radioactive does not mean that an object is continuously firing out all of its nuclear energy at once.
Each unstable nucleus has a probability of decaying during a given interval.
Some radioactive isotopes decay very rapidly, while others have half-lives of millions or even billions of years.
This is why radioactive materials can be useful for very different purposes, from medical imaging to determining the age of ancient rocks.
Connecting the Ideas
Radioactive decay brings together many concepts from this course:
Unstable nucleus
↓
Nuclear transformation
↓
Alpha, beta, or gamma emission
↓
Daughter nucleus formed
↓
Mass number and atomic number balanced
↓
Charge, baryon number, and lepton number conserved
↓
Energy and momentum carried by products
↓
More stable nuclear configuration
Radioactive decay is therefore both a nuclear process and an application of the fundamental conservation laws used throughout particle physics.
Key Terms
Radioactive decay – The spontaneous transformation of an unstable atomic nucleus.
Parent nucleus – The original unstable nucleus.
Daughter nucleus – The nucleus formed after radioactive decay.
Alpha particle – A helium-4 nucleus containing two protons and two neutrons.
Beta-minus particle – An electron emitted during beta-minus decay.
Beta-plus particle – A positron emitted during beta-plus decay.
Gamma ray – A high-energy photon emitted by an excited nucleus.
Beta decay – A weak-interaction process that changes the proton-neutron balance of a nucleus.
Excited nucleus – A nucleus containing more energy than its lowest-energy state.
Decay chain – A sequence of radioactive decays leading eventually toward a stable nucleus.
Ionizing radiation – Radiation capable of removing electrons from atoms or molecules.
Key Takeaways
- Radioactive decay is a spontaneous nuclear transformation.
- It differs from a particle collision because it does not require another particle to initiate the process.
- The three main introductory forms are alpha, beta, and gamma decay.
- Alpha decay emits a helium-4 nucleus.
- In alpha decay, A decreases by 4 and Z decreases by 2.
- In beta-minus decay, a neutron changes into a proton, so A stays constant and Z increases by 1.
- In beta-plus decay, a proton effectively changes into a neutron, so A stays constant and Z decreases by 1.
- Gamma decay releases excess nuclear energy without changing A or Z.
- Nuclear equations must conserve mass number and electric charge.
- Complete beta-decay equations also conserve lepton number through the production of neutrinos or antineutrinos.
- Energy and momentum are conserved in every radioactive decay.
- The daughter nucleus may also be radioactive, creating a decay chain.
- Radioactive decay allows an unstable nucleus to move toward a lower-energy, more stable configuration.
2. Nuclear Fission
Learning outcomes
- I can describe nuclear fission.
- I can explain chain reactions.
- I can calculate simple energy changes.
- I can describe how nuclear reactors control fission.
- I can evaluate the advantages and disadvantages of fission.
What Is Nuclear Fission?
Nuclear fission is the splitting of a heavy atomic nucleus into two smaller nuclei.
This process usually also releases:
- neutrons
- gamma radiation
- a large amount of energy
A common example involves uranium-235.
One possible reaction is:
²³⁵₉₂U + ¹₀n → ¹⁴¹₅₆Ba + ⁹²₃₆Kr + 3¹₀n + energy
The exact fission products can vary, but the general pattern is:
heavy nucleus + neutron → two smaller nuclei + neutrons + energy
Why Can Heavy Nuclei Undergo Fission?
Very heavy nuclei contain many protons.
All protons repel one another because of the electromagnetic force.
The strong nuclear interaction holds nucleons together, but it acts only over very short distances.
As nuclei become very large:
- proton-proton repulsion becomes increasingly important
- the nucleus can become easier to deform
- some heavy nuclei become susceptible to splitting
A nucleus such as uranium-235 can absorb a neutron and become highly excited.
That excitation can cause the nucleus to stretch and split.
Fission of Uranium-235
Uranium-235 is especially important because it can undergo fission after absorbing a slow neutron.
The first step can be represented as:
²³⁵U + n → ²³⁶U*
The asterisk means that uranium-236 is in an excited state.
The excited nucleus can then split:
²³⁶U → fission fragments + neutrons + energy*
For example:
²³⁵₉₂U + ¹₀n → ¹⁴¹₅₆Ba + ⁹²₃₆Kr + 3¹₀n + energy
Checking the Nuclear Equation
Mass numbers:
235 + 1 = 141 + 92 + 3
236 = 236
Atomic numbers:
92 = 56 + 36
92 = 92
So nucleon number and charge are conserved.
Where Does the Energy Come From?
The energy released during fission comes from a difference in nuclear binding energy.
Very heavy nuclei generally have a lower binding energy per nucleon than medium-mass nuclei.
When a heavy nucleus splits, the products move toward the more tightly bound middle region of the binding-energy curve.
Therefore:
fission products have greater binding energy per nucleon than the original heavy nucleus
The total mass of the products is slightly less than the total mass of the starting system.
This mass defect appears as released energy.
Mass-Energy in Fission
The energy released is calculated using:
E = Δmc²
where:
Δm = mass before − mass after
Even a very small mass difference can produce a large amount of energy because:
c² ≈ 9 × 10¹⁶ m²/s²
Example 1: Energy from a Mass Change
Suppose a fission reaction has a mass defect of:
3.5 × 10⁻²⁸ kg
Use:
E = Δmc²
E = (3.5 × 10⁻²⁸)(3.0 × 10⁸)²
E = (3.5 × 10⁻²⁸)(9.0 × 10¹⁶)
E = 3.15 × 10⁻¹¹ J
This is the energy from only one reaction.
That may seem tiny, but an enormous number of nuclei can undergo fission in a macroscopic sample.
Using Atomic Mass Units
Particle and nuclear masses are often given in atomic mass units.
Recall:
1 u c² ≈ 931.5 MeV
So:
Energy released in MeV = mass defect in u × 931.5
Example 2: Energy in MeV
Suppose the mass defect is:
0.210 u
Then:
E = 0.210 × 931.5
E ≈ 196 MeV
A single uranium-235 fission typically releases energy on the order of about 200 MeV.
Where Does the Fission Energy Go?
The released energy appears mainly as:
- kinetic energy of the fission fragments
- kinetic energy of emitted neutrons
- gamma radiation
- later radioactive decay energy from unstable fission products
Most of the immediate energy is carried by the two large fission fragments.
As these fragments move through surrounding material, collisions convert their kinetic energy into thermal energy.
Chain Reactions
One of the most important features of nuclear fission is that it can produce additional neutrons.
Suppose one fission produces three neutrons.
Those neutrons may strike other uranium-235 nuclei.
Each of those nuclei may also split.
This can produce still more neutrons.
The result is a chain reaction.
A Simple Chain Reaction
Imagine:
Generation 1
One fission produces:
3 neutrons
Generation 2
If all three cause fission:
3 fissions
Suppose each produces 3 more neutrons:
9 neutrons
Generation 3
Those could cause:
9 fissions
and produce:
27 neutrons
The number of reactions could increase very rapidly.
In reality, not every neutron causes another fission.
Some:
- escape
- are absorbed without causing fission
- lose energy
- interact with other nuclei
Criticality
A chain reaction can behave in three general ways.
Subcritical
On average, fewer than one neutron from each fission causes another fission.
The reaction gradually dies out.
Critical
On average, exactly one neutron from each fission causes another fission.
The reaction continues at a steady rate.
Supercritical
On average, more than one neutron from each fission causes another fission.
The reaction rate increases.
A power reactor is designed to operate close to a controlled critical condition.
The Multiplication Factor
Nuclear engineers often describe chain reactions using a multiplication factor called k.
Very simply:
k < 1 → subcritical
k = 1 → critical
k > 1 → supercritical
A reactor operating steadily aims for approximately:
k = 1
This means the fission rate remains roughly constant.
How a Nuclear Reactor Uses Fission
A nuclear reactor uses a controlled fission chain reaction to produce thermal energy.
The basic sequence is:
fission
↓
kinetic energy of fission products
↓
thermal energy in reactor fuel
↓
heat transferred to coolant
↓
steam produced, directly or indirectly
↓
turbine turns
↓
generator produces electricity
The reactor is therefore primarily a heat source.
Main Parts of a Nuclear Reactor
A simplified reactor includes:
- nuclear fuel
- moderator in many reactor designs
- control rods
- coolant
- reactor vessel/core
- heat exchanger or steam generator in many designs
- turbine
- generator
- containment structures
Nuclear Fuel
The fuel contains fissile material.
Common examples include fuels containing uranium, especially uranium-235.
The fuel is commonly formed into ceramic pellets and arranged in fuel rods.
The fuel rods are grouped into assemblies inside the reactor core.
The Moderator
In many thermal reactors, a moderator slows fast neutrons.
Why is this useful?
For uranium-235, slow or thermal neutrons are particularly effective at causing further fission.
Common moderator materials include:
- ordinary water
- heavy water
- graphite
The moderator does not stop the reaction. It changes neutron energies so that the chain reaction can be sustained efficiently.
Control Rods
Control rods absorb neutrons.
They can be inserted into or withdrawn from the reactor core.
If control rods are inserted farther:
more neutrons are absorbed
↓
fewer neutrons cause fission
↓
fission rate decreases
If control rods are withdrawn:
fewer neutrons are absorbed
↓
more neutrons remain available
↓
fission rate can increase
Control rods therefore help regulate reactor power.
Common Control-Rod Materials
Control rods use materials that absorb neutrons efficiently.
Examples include materials containing:
- boron
- cadmium
- hafnium
The exact materials depend on reactor design.
The Coolant
The coolant removes thermal energy from the reactor core.
Depending on reactor type, coolants may include:
- water
- heavy water
- gases
- liquid metals
- molten salts in some designs
The coolant transports energy from the core to another part of the power-generation system.
From Heat to Electricity
A nuclear power station does not generate electricity directly from the nucleus.
Instead:
nuclear energy → thermal energy → mechanical energy → electrical energy
The heat from fission ultimately produces steam or another working fluid.
The steam turns a turbine.
The turbine turns a generator.
The generator produces electrical energy.
Why Reactors Need Continuous Control
The power output of a reactor depends strongly on the neutron population.
If too many neutrons cause new fissions:
power rises
If too few do:
power falls
Reactor systems use:
- control rods
- neutron measurements
- temperature feedback
- coolant systems
- shutdown systems
to maintain safe operation.
Delayed Neutrons
Most neutrons from fission are emitted almost immediately.
However, a small fraction appear later from radioactive fission products.
These are called delayed neutrons.
Although they represent only a small fraction of the neutron population, they are extremely important because they make reactor chain reactions much easier to control over human and mechanical timescales.
Fission Products Are Often Radioactive
The smaller nuclei produced by fission are usually neutron-rich.
Many are unstable.
They undergo radioactive decay, often through beta decay.
Therefore, even after the chain reaction is stopped, radioactive fission products continue to release energy.
This is called decay heat.
Why Cooling Must Continue After Shutdown
Stopping the chain reaction does not instantly eliminate all heat production.
Radioactive fission products continue to decay.
Therefore:
reactor shutdown ≠ immediate zero heat
Cooling systems must continue removing decay heat.
This is one of the most important safety considerations in reactor design.
Advantages of Nuclear Fission
Nuclear fission has several major advantages as an energy source.
High Energy Density
A small amount of nuclear fuel can release a very large amount of energy.
This is because nuclear energy changes are much larger than ordinary chemical energy changes.
Low Direct Carbon Dioxide Emissions During Operation
A nuclear reactor does not burn fossil fuel during normal operation.
Therefore, direct carbon dioxide emissions from electricity generation are very low.
There are still lifecycle emissions from:
- construction
- mining
- fuel processing
- transport
- decommissioning
but overall lifecycle greenhouse-gas emissions are generally low compared with fossil-fuel generation.
Reliable Power Production
Nuclear power stations can produce large amounts of electricity continuously.
They are not directly dependent on:
- sunshine
- wind speed
- daily weather changes
This makes them useful for steady electricity generation.
Small Fuel Mass
Because nuclear fuel has very high energy density, relatively little fuel is required compared with coal, oil, or gas for the same amount of energy.
Disadvantages of Nuclear Fission
Fission also presents significant challenges.
Radioactive Waste
Fission produces radioactive materials.
Some waste remains hazardous for long periods.
It must be:
- contained
- shielded
- transported safely
- stored or disposed of securely
Accident Risk
Modern reactors include many safety systems, but severe accidents can have significant environmental, economic, and social consequences.
Safe reactor design therefore requires multiple independent protective systems.
High Construction Cost
Nuclear power stations are complex.
They require:
- extensive safety systems
- radiation shielding
- highly engineered components
- strict regulation
As a result, construction costs can be high.
Long Construction and Decommissioning Times
Large reactors can take years to plan and build.
At the end of their useful life, they must also be safely decommissioned.
This can be expensive and time-consuming.
Nuclear Material Security
Some nuclear materials and technologies can raise concerns involving:
- security
- theft
- diversion of nuclear material
- weapons proliferation
Civil nuclear programs therefore require strong safeguards and international oversight.
Evaluating Fission Fairly
Whether nuclear fission is considered a good energy option depends on several factors.
These include:
- electricity demand
- available alternatives
- local geography
- cost
- climate goals
- grid reliability
- waste-management plans
- reactor technology
- public acceptance
A strong evaluation considers both advantages and disadvantages rather than treating nuclear power as simply "good" or "bad."
Comparing Fission with Fossil Fuels
| Nuclear Fission | Fossil Fuels |
|---|---|
| Very high energy density | Lower energy density |
| Low direct CO₂ during operation | Large CO₂ emissions when burned |
| Produces radioactive waste | Produces greenhouse gases and air pollutants |
| High construction cost | Often lower initial construction cost |
| Requires radioactive-material management | Requires continuous fuel extraction and combustion |
| Can provide steady output | Can also provide controllable steady output |
Fission and Renewable Energy
Nuclear and renewable technologies are not necessarily direct opposites.
A low-carbon electricity system can potentially combine:
- nuclear power
- solar
- wind
- hydroelectricity
- storage
- other low-carbon technologies
The best mixture depends on the needs and resources of a particular region.
Example 3: Chain Reaction Reasoning
Suppose each fission produces an average of:
2.5 neutrons
But only:
40%
of those neutrons cause another fission.
Average successful neutrons per fission:
2.5 × 0.40 = 1.0
So:
k ≈ 1
The chain reaction would be approximately critical and could continue at a steady rate.
Example 4: Subcritical Reaction
Suppose each fission produces:
2.4 neutrons
and only:
30%
cause another fission.
Then:
2.4 × 0.30 = 0.72
Since:
k < 1
the reaction is subcritical.
The chain reaction will decrease.
Example 5: Supercritical Reaction
Suppose each fission produces:
3 neutrons
and:
50%
cause another fission.
Then:
3 × 0.50 = 1.5
Since:
k > 1
the neutron population increases.
The reaction is supercritical.
Nuclear Fission and Conservation Laws
A fission reaction must conserve:
- electric charge
- nucleon number
- energy
- momentum
- angular momentum
Consider:
²³⁵₉₂U + ¹₀n → ¹⁴¹₅₆Ba + ⁹²₃₆Kr + 3¹₀n
Nucleon number:
235 + 1 = 141 + 92 + 3
Charge:
92 = 56 + 36
Both are conserved.
The small difference in rest mass appears as released energy.
Did You Know?
Most of the energy released in a fission event does not come directly from the emitted neutrons.
A large fraction appears as kinetic energy of the two heavy fission fragments.
These positively charged fragments move rapidly through the surrounding fuel and collide with other atoms.
Their motion is converted into thermal energy.
This is how microscopic nuclear energy ultimately becomes the heat used to generate electricity.
Connecting the Ideas
Nuclear fission links several ideas from this course:
Heavy nucleus absorbs neutron
↓
Excited compound nucleus forms
↓
Nucleus splits
↓
Smaller nuclei + neutrons produced
↓
Products have greater binding energy per nucleon
↓
Mass decreases slightly
↓
E = Δmc²
↓
Energy released
↓
Released neutrons can trigger more fissions
↓
Chain reaction
↓
Control rods and reactor systems regulate the process
Fission is therefore a direct application of nuclear stability, binding energy, mass defect, mass-energy equivalence, and conservation laws.
Key Terms
Nuclear fission – The splitting of a heavy nucleus into smaller nuclei, usually with the release of neutrons and energy.
Fission fragment – One of the smaller nuclei produced during fission.
Chain reaction – A sequence in which neutrons from one fission cause additional fissions.
Critical – A condition in which the chain reaction continues at a steady rate.
Subcritical – A condition in which the chain reaction decreases.
Supercritical – A condition in which the chain reaction increases.
Moderator – Material used in many reactors to slow neutrons.
Control rod – A neutron-absorbing component used to regulate a reactor.
Coolant – Material that transfers heat away from a reactor core.
Fissile material – Material capable of sustaining fission after absorbing appropriate neutrons.
Decay heat – Heat produced by radioactive decay of fission products after the main chain reaction has stopped.
Key Takeaways
- Nuclear fission is the splitting of a heavy nucleus into smaller nuclei.
- Fission typically releases neutrons and a large amount of energy.
- Uranium-235 can undergo fission after absorbing a neutron.
- Fission releases energy because the products are generally more tightly bound per nucleon than the original heavy nucleus.
- The small loss of rest mass is converted to energy according to E = Δmc².
- One fission releases energy on the order of hundreds of MeV.
- Neutrons released by fission can trigger further fissions, producing a chain reaction.
- A steady reactor aims to maintain approximately k = 1.
- Control rods absorb neutrons and help regulate the reaction.
- A moderator slows neutrons in many reactor designs.
- A coolant transfers thermal energy away from the reactor core.
- Radioactive fission products continue producing decay heat even after shutdown.
- Fission offers very high energy density and low direct operational carbon emissions, but it also produces radioactive waste and requires strict safety and security systems.
- A fair evaluation of nuclear fission must consider both its benefits and limitations.
3. Nuclear Fusion
Learning outcomes
- I can describe nuclear fusion.
- I can explain why fusion releases energy.
- I can compare fusion with fission.
- I can describe fusion in stars.
- I can explain challenges in producing controlled fusion.
4. Stellar Nucleosynthesis
Learning outcomes
- I can explain how stars produce heavier elements.
- I can describe hydrogen fusion.
- I can explain the formation of elements beyond iron.
- I can relate stellar evolution to element formation.
- I can explain why supernovae are important.
5. Energy from Nuclear Reactions
Learning outcomes
- I can compare energy released in chemical and nuclear reactions.
- I can explain why nuclear reactions release large amounts of energy.
- I can interpret nuclear reaction energy diagrams.
- I can compare different nuclear energy sources.
- I can evaluate the efficiency of nuclear energy.