ChemistryAtomic StructureMedium

Isotope

Also known as:nuclide (more specific term)

Isotopes are atoms of the same element (same atomic number Z) that have different numbers of neutrons, resulting in different mass numbers (A) but identical chemical behavior. Some isotopes are stable while others are radioactive (radioisotopes) and undergo decay, emitting radiation until they reach a stable configuration. Isotopes have widespread applications in medicine (radioactive tracers, cancer treatment), archaeology (radiocarbon dating), and nuclear energy.

Key Formula

Average atomic mass = Σ (fractional abundance × mass number) for all isotopes

LaTeX: A_{\text{avg}} = \sum_{i} (\text{abundance}_i \times A_i)

SymbolMeaningUnit
A_avgAverage atomic mass of the elementatomic mass units (u)
abundance_iFractional natural abundance of isotope idimensionless (0 to 1)
A_iMass number of isotope iu

Worked Example

Problem

Chlorine exists as two isotopes: Cl-35 (abundance 75.77%) and Cl-37 (abundance 24.23%). Calculate the average atomic mass of chlorine.

Solution

Step 1: Convert percentages to decimals: 0.7577 and 0.2423. Step 2: Apply formula: A_avg = (0.7577 × 35) + (0.2423 × 37). Step 3: A_avg = 26.520 + 8.965 = 35.485 u.

Answer

Average atomic mass of chlorine = 35.45 u (matches the periodic table value of 35.45).

Stable and Radioactive Isotopes of Carbon

IsotopeProtonsNeutronsMass NumberStabilityApplication
Carbon-126612StableStandard atomic mass reference
Carbon-136713StableNMR spectroscopy
Carbon-146814Radioactive (t½ = 5730 yr)Radiocarbon dating

Interactive Tools

PhET Isotopes and Atomic Mass

Build isotopes and calculate weighted average atomic mass interactively

Open Tool

NIST Atomic Weights and Isotopic Compositions

Official database of isotopic abundances and masses for all elements

Open Tool

Ptable – Isotope Explorer

View all known isotopes, half-lives, and decay modes for each element

Open Tool
Chart of isotopes showing stable and radioactive isotopes with mass numbers

Wikimedia Commons, CC BY-SA

Related Terms

From Greek "isos" (equal) + "topos" (place), coined by Frederick Soddy in 1913 to describe atoms that occupy the same place on the periodic table (same element) but differ in mass. Soddy received the Nobel Prize in Chemistry in 1921 partly for this concept.

isotopeatomic-structureradioactivitynuclear-chemistrymass-number