BackAtoms and Radioactivity: Structure, Isotopes, and Nuclear Chemistry
Study Guide - Smart Notes
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Atoms and Their Components
Subatomic Particles
Atoms are the fundamental building blocks of matter, composed of three main subatomic particles: protons, neutrons, and electrons. Understanding their properties and arrangement is essential for studying chemical behavior.
Protons: Positively charged particles located in the nucleus. Each proton has a charge of +1.
Neutrons: Neutral particles (no charge) also found in the nucleus.
Electrons: Negatively charged particles (-1) that move in the space surrounding the nucleus, known as the electron cloud.
Atoms are electrically neutral overall because the number of protons equals the number of electrons.
Structure of the Atom
The atom consists of a dense nucleus containing protons and neutrons, surrounded by a much larger region where electrons are found.
The nucleus is the central core, containing nearly all the atom's mass.
The electron cloud is the region where electrons are likely to be found, occupying most of the atom's volume.
Most of the atom is empty space.
Relative Mass and Atomic Mass Unit (amu)
Because subatomic particles are extremely small, their masses are measured in atomic mass units (amu).
1 amu is defined as one-twelfth the mass of a carbon-12 atom (which has 6 protons and 6 neutrons).
Proton mass ≈ 1 amu; Neutron mass ≈ 1 amu; Electron mass ≈ 0.0005 amu (about 1/2000 the mass of a proton or neutron).
For most calculations, the mass of electrons is considered negligible.
Subatomic Particle | Symbol | Electrical Charge | Relative Mass (amu) | Location in Atom |
|---|---|---|---|---|
Proton | p or p+ | +1 | 1 | Nucleus |
Neutron | n or n0 | 0 | 1 | Nucleus |
Electron | e- | -1 | 0.0005 | Outside nucleus (electron cloud) |
Atomic Number and Mass Number
Definitions and Calculations
Each element is defined by its atomic number and mass number, which relate to the number of subatomic particles present.
Atomic Number (Z): The number of protons in the nucleus of an atom. This determines the element's identity.
Mass Number (A): The total number of protons and neutrons in the nucleus.
For a neutral atom: Number of electrons = Number of protons.
Symbolic notation: AZElement (e.g., 126C for carbon-12).
Formula:
Given atomic number and mass number, you can determine the number of protons, neutrons, and electrons.
Isotopes and Atomic Mass
Isotopes
Isotopes are atoms of the same element (same number of protons) that have different numbers of neutrons, and thus different mass numbers.
Isotopes are represented by their mass number (e.g., carbon-12, carbon-13, carbon-14).
All isotopes of an element have the same chemical properties but may have different physical properties (such as stability).
Atomic Mass
The atomic mass of an element is the weighted average of the masses of all its naturally occurring isotopes.
The atomic mass (as seen on the periodic table) reflects both the mass and the relative abundance of each isotope.
Formula for average atomic mass:
Isotope | Isotopic Mass (amu) | Abundance (%) |
|---|---|---|
Silicon-28 | 27.97693 | 92.223 |
Silicon-29 | 28.97649 | 4.685 |
Silicon-30 | 29.97377 | 3.092 |
Example: Chlorine has two stable isotopes: Cl-35 (75.779%) and Cl-37 (24.221%). The average atomic mass is calculated using their masses and abundances.
Radioactivity and Radioisotopes
Radioactivity
Radioactivity is the spontaneous emission of energy from the nucleus of an unstable atom. Atoms that emit radiation are called radioisotopes.
Most naturally occurring isotopes are stable; unstable isotopes undergo radioactive decay to become more stable.
Radioactive decay can emit different types of radiation: alpha particles, beta particles, gamma rays, positrons, and neutrons.
Types of Radiation
Type | Symbol | Charge | Description |
|---|---|---|---|
Alpha particle | or | 2+ | Helium nucleus (2 protons, 2 neutrons) |
Beta particle | or | -1 | High-energy electron |
Gamma ray | 0 | High-energy electromagnetic radiation | |
Positron | or | +1 | Positive electron |
Neutron | or | 0 | Neutral particle |
Alpha particles are the least penetrating; gamma rays are the most penetrating.
Penetration and Shielding
Radiation Type | Penetration | Shielding Material |
|---|---|---|
Alpha () | Few centimeters; stopped by paper or skin | Paper, clothing |
Beta () | Few meters; penetrates skin | Plastic, aluminum foil, gloves |
Gamma (), X-rays | Fully penetrates body; several meters | Lead, concrete |
Neutron | Fully penetrates body; thousands of meters | Concrete, water |
Biological Effects of Radiation
Ionizing radiation can remove electrons from atoms, making them more reactive and potentially damaging biological tissues.
High doses can cause radiation sickness, cancer, or death; rapidly dividing cells are most susceptible.
Exposure is measured in sieverts (Sv) or millisieverts (mSv).
Nuclear Equations and Radioactive Decay
Writing Nuclear Equations
Nuclear equations represent the changes that occur during radioactive decay. The sum of mass numbers and atomic numbers must be equal on both sides of the equation.
Alpha decay:
Beta decay:
Gamma emission:
Positron emission:
Neutron emission:
Example: (Alpha decay of americium-241)
Producing Radioisotopes
Radioisotopes can be produced by bombarding stable isotopes with particles (e.g., neutrons, protons, alpha particles).
In these reactions, the incoming particle appears on the reactant side of the equation.
Example:
Radiation Units and Half-Lives
Units of Radioactivity
Becquerel (Bq): 1 disintegration per second (SI unit).
Curie (Ci): disintegrations per second.
Other units: millicurie (mCi), microcurie (μCi).
Unit | Relationship |
|---|---|
1 Bq | 1 disintegration/second |
1 Ci | disintegrations/second |
1 mCi | 1/1000 Ci |
1 μCi | 1/1,000,000 Ci |
Half-Life
The half-life () of a radioactive isotope is the time required for half of the atoms in a sample to decay.
Each isotope has a characteristic half-life, ranging from fractions of a second to billions of years.
Medical isotopes are chosen for short half-lives to minimize patient exposure.
Formula for remaining isotope:
where = number of half-lives elapsed.
Radioisotope | Symbol | Physical Half-Life |
|---|---|---|
Hydrogen-3 | 12.3 years | |
Carbon-14 | 5730 years | |
Radium-226 | 1600 years | |
Uranium-238 | 4.5 billion years |
Medical Applications for Radioisotopes
Diagnostic Uses
Radioisotopes are widely used in medicine for both diagnosis and treatment. Diagnostic procedures often use small amounts of radioisotopes (tracers) with short half-lives to minimize radiation exposure.
Tracers are radioisotopes that concentrate in specific organs or tissues, allowing imaging of physiological processes.
Technetium-99m is commonly used to assess blood flow in the lungs.
Areas with abnormal tracer distribution appear as "cold" (no uptake) or "hot" (increased uptake) spots in scans.
Therapeutic Uses
Radioisotopes can be used to destroy diseased or cancerous tissues (e.g., iodine-131 for thyroid cancer).
External beam radiation therapy uses gamma rays (e.g., from cobalt-60) to target tumors.
Brachytherapy involves implanting radioactive seeds directly into tumors.
Positron Emission Tomography (PET)
PET scans use positron-emitting isotopes (e.g., fluorine-18) to image metabolic activity in tissues, especially the brain.
When a positron meets an electron, gamma radiation is produced and detected by the scanner.
Summary Table: Key Concepts
Concept | Definition/Key Point |
|---|---|
Atom | Smallest unit of an element, composed of protons, neutrons, and electrons |
Isotope | Atoms of the same element with different numbers of neutrons |
Radioactivity | Spontaneous emission of energy from an unstable nucleus |
Half-life | Time for half the atoms in a sample to decay |
Tracer | Radioisotope used in small amounts for diagnostic imaging |