Radioactivity, Nuclear Reactions, and Decay Modes
Fundamentals of Atomic Structure and Radioactivity
Elements with atomic numbers of or higher usually have one or more isotopes containing unstable nuclei.
Radioactive decay (radioactivity) is defined as the spontaneous disintegration of a nucleus accompanied by the emission of particles, electromagnetic radiation, or both.
Nuclei are inherently unstable due to the relative numbers and combinations of protons and neutrons within the nucleus; unstable nuclei break apart and undergo transformations to eventually form stable nuclei.
Emission during radioactive decay involves the release of energy, physical particles, or both from the decaying atom.
Transmutation refers to the transformation of an atom of one element into an atom of a different chemical element, which occurs whenever nuclear reactions alter the proton count in the nucleus.
Decaying systems are inherently unpredictable prior to observation; regardless of the isotope, it cannot be automatically predicted beforehand what specific mode of decay an atom will undergo (e.g., whether a carbon atom will undergo alpha decay or beta decay).


Nuclear Terminology and Isotope Representation
Nucleons are defined as the subatomic particles located within the atomic nucleus, specifically comprising protons and neutrons.
A nuclide is a general term applied to any atom of a specific nuclear species, characterized by its atomic composition.
Isotope representation methods:
Nuclear Symbol Notation:
Written in the general form , where represents the mass number, represents the atomic number, and represents the chemical symbol of the element.
Mass number () is the sum of protons plus neutrons in the nucleus.
Atomic number () is the total number of protons in the nucleus.
In standard nuclear symbols, the atomic number is occasionally omitted because the chemical symbol uniquely identifies the proton count (e.g., or ).
Hyphen Notation:
Formatted by writing the element name or symbol followed by a hyphen and the mass number.
Examples include , , or .
Types of Radiation and Nuclear Decay Modes
Radioactive Decay Notation Principles:
General symbolic expression: .
Fundamental conservation law: The sum of the mass numbers () and the sum of the atomic numbers () must be equal on both sides of the arrow in all nuclear reaction equations.
Alpha () Radiation and Alpha Decay:
Involves the emission of an alpha particle, which is identical to a helium-4 nucleus (, , or ).
Physical composition: Contains protons and neutrons, giving it a mass number of and an atomic number of .
Nuclear Effect: Reduces the mass number () of the parent nucleus by and reduces the atomic number () by .
Shielding and Penetration: Alpha particles have low penetrating power and are stopped or blocked by a single sheet of paper placed in front of them.
Nuclear Reaction Example: Uranium-238 decays into Thorium-234 via alpha emission:
Mass and atomic number balance verification:
Superscript sum:
Subscript sum:

Beta () Radiation and Beta Decay:
Involves the emission of a beta particle, which is a high-energy electron (, , or ) ejected directly from the nucleus.
Nuclear Mechanism: Results from the breakdown of a neutron within an unstable nucleus into a proton and an electron.
Nuclear Effect: The generated proton remains in the nucleus, increasing the atomic number () by (add ) while decreasing the neutron count by . The overall mass number () remains unchanged because an electron has a mass number of .
Shielding and Penetration: Beta particles penetrate paper but are blocked or stopped by lead or thick glass.
Detection: Radioactivity and beta particles are detected using a Geiger counter.
Nuclear Reaction Examples:
Decay of Carbon-14 into Nitrogen-14:
Free neutron breakdown equation:
Positron Emission:
Involves the emission of a positron ( or ), which is an antimatter particle possessing the same mass as an electron (mass number ) but carrying a positive charge ().
Nuclear Mechanism: A proton inside an unstable nucleus converts into a neutron and a positron. The neutron stays in the nucleus, while the positron leaves the atom.
Nuclear Effect: Decreases the atomic number () by while leaving the mass number () unchanged.
Nuclear Reaction Examples:
Conversion of Potassium-39 to Argon-39:
Conversion of Aluminum-24 to Magnesium-24:
Electron Capture:
Occurs when an inner-shell orbital electron is captured by the nucleus of its own atom ( on the reactant side).
Nuclear Mechanism: The captured inner electron combines with a nuclear proton to form a new neutron.
Nuclear Effect: Decreases the atomic number () by while leaving the mass number () unchanged.
Nuclear Reaction Example:
Gamma () Radiation and Gamma Emission:
High-energy electromagnetic radiation ( or ) with energy levels exceeding those of X-rays.
Physical Nature: Represents pure energy emission without mass or electric charge (mass , charge ).
Nuclear Mechanism: Released when an unstable nucleus undergoes structural particle rearrangement.
Associated Emission: Frequently accompanies alpha or beta decay processes.
Nuclear Effect: Does not change the mass number () or the atomic number () of the nuclide.
Medical Application: Focused gamma radiation is utilized in medical therapies to destroy cancer cells.
Nuclear Reaction Examples:
Alpha decay of Thorium-230 with gamma emission:
Beta decay of Thorium-234 with gamma emission:
Half-Life Dynamics and Quantitative Calculations
Definition of Half-Life ():
The amount of time required for exactly one-half of the radioactive nuclei present in a sample to undergo decay.
Temporal Variation across Nuclides:
Half-lives range from tiny fractions of a second to billions of years depending on the nuclide.
Naturally occurring radioactive isotopes usually have long half-lives.
Isotopes created through nuclear processes generally have shorter half-lives.
Decay timelines for individual unstable atoms cannot be predicted.
Sequential Half-Life Decay Progression:
Starting with a sample:
After half-life (): remains.
After half-lives (): remains.
After half-lives (): remains.
After half-lives (): remains.
Starting with a sample:
.
Decay Curve:
A graphical diagram plotting the remaining quantity of a radioactive isotope against elapsed time, illustrating exponential decay.



Quantitative Half-Life Worked Examples:
Sample Problem 1:
Question: A radioactive isotope has a half-life of . How much remains of a sample after ?
Calculation:
Calculate total half-life cycles elapsed:
Halve the original sample three times sequentially:
Result: Exactly remains after .
Sample Problem 2:
Question: In , a sample of a radioactive isotope decays to leave . What is the half-life of this nuclide?
Calculation:
Count the number of half-life decay cycles from to :
Total cycles elapsed =
Calculate the duration of one half-life cycle:
Result: The half-life is .
Nuclear Fission and Chain Reactions
Definition of Nuclear Fission:
A reaction process in which heavy nuclei split into lighter, stable, medium-mass nuclei.
Energy and Neutrons Released:
Fission releases massive amounts of energy (atomic energy) alongside fast-moving neutrons.
Occurrence and Initiation:
Fission occurs naturally or can be artificially induced by bombarding heavy target nuclei with small particles such as neutrons.
Primary Example — Fission of Uranium-235:
Neutron bombardment of Uranium-235 ():
An unstable Uranium-236 intermediate nucleus briefly forms before splitting into Krypton-92, Barium-141, three high-speed neutrons, and energy.
Chain Reaction Dynamics:
The fast-moving neutrons released during initial fission hit adjacent heavy nuclei, causing them to split in turn.
Applications:
Uncontrolled Chain Reactions: Lead to nuclear weapon explosions (atomic bomb).
Controlled Chain Reactions: Utilized in nuclear reactors, which are equipped with containment and control systems designed to prevent runaway chain reactions.



Nuclear Fusion
Definition of Nuclear Fusion:
A process where two or more low-mass nuclei (such as hydrogen or helium nuclei) combine or fuse together to form a heavier, stable nucleus.
Energy Yield:
Releases extraordinarily large amounts of energy, surpassing the energy yield per unit mass of nuclear fission.
Temperature Requirements:
Requires extremely high temperatures (around ) to overcome electrostatic repulsion between positively charged hydrogen nuclei.
Astrophysical Context:
Powers the Sun and other stars, supplying their thermal and light output.
Stellar Multistep Fusion Chain Reactions:
Reaction 1:
Reaction 2:
Reaction 3:
Alternative Reaction Path:
Practical Applications and Summaries of Radioactivity


Radiocarbon Dating & Age Determination:
Carbon dating uses the known half-life of Carbon-14 () to determine the age of ancient organic remnants, fossils, and human artifacts based on remaining radiation levels.
Medical Cancer Treatments:
Targeted radiation therapy utilizes gamma rays and beta decay to selectively destroy malignant cancer cells.
Diagnostic Medical Radiotracers:
Short-lived radioactive isotopes serve as diagnostic tracers inside the human body for medical imaging procedures.
Electrical Energy Production:
Nuclear power plants convert energy from controlled fission into electricity. Fission remnants have super long half-lives, providing continuous electrical generation over long spans.
Medical Instrument Sterilization:
Radiation kills pathogens and sterilizes surgical instruments and medical supplies safely.
Space Exploration Power:
Nuclear power units supply long-duration power for space travel and extraterrestrial exploration equipment, such as Mars rovers.