Atoms and Isotopes — Quick Reference
Atom basics
Atoms are the basic building blocks of matter; composed of a nucleus (protons and neutrons) and electrons surrounding the nucleus.
Subatomic particles:
Protons: positive charge (+1)
Neutrons: neutral (0)
Electrons: negative charge (-1)
Atoms are electrically neutral because the number of protons equals the number of electrons in a neutral atom.
If the atom is not neutral, it forms ions.
Structure and terminology
Nucleus contains protons and neutrons (collectively called nucleons).
Electrons form an electron cloud around the nucleus.
Size: nucleus is tiny compared to the overall atom (most of the atom’s volume is empty space).
Atomic number, mass number, and isotopes
Atomic number: Z = #\text{protons}
For neutral atoms, Z = #\text{electrons}; this number uniquely identifies the element in the periodic table.
Mass number: A = Z + N where N = #\text{neutrons}.
Isotopes: atoms of the same element (same Z) with different A (different N). Examples:
Carbon-12: ^{12}_{6}\mathrm{C} (Z=6, A=12)
Carbon-13: ^{13}_{6}\mathrm{C} (Z=6, A=13)
Hydrogen isotopes: ^{1}{1}\mathrm{H}, \ ^{2}{1}\mathrm{H}, \ ^{3}_{1}\mathrm{H}
Notation: isotope symbol is ^{A}_{Z}\mathrm{X} (A on top-left, Z on bottom-left, X is element symbol).
Protons determine Z; neutrons = A − Z; electrons in neutral atom = Z.
Atomic mass unit and standard
Atomic mass unit (amu): definition
1 amu = \dfrac{m(\mathrm{C-12})}{12}
m(\mathrm{C-12}) = 12 \text{ amu}
Therefore, 1 amu = 1.6605 × 10^{-24} g
Why amu matters: converts between lab-scale masses (grams, kilograms) and atomic-scale masses.
Periodic table masses: not whole numbers; these are weighted averages of isotopic masses.
Weighted average atomic mass formula:
\overline{m} = \sumi mi fi where mi is the mass of isotope i (in amu) and f_i is its fractional abundance.
Fractional abundance: fi = \dfrac{\text{abundance}i}{100}
Natural abundances are measured by mass spectrometry (conceptual): different isotopes produce distinct signals; the peaks’ heights reflect abundances.
Practice: reading isotopes and calculating numbers
Given a symbol, read Z from the periodic table to get proton count.
If mass number A is given, neutrons N = A - Z.
For a neutral atom, electrons = Z.
Example workflow (generic): for element symbol X with mass number A, find Z from periodic table, compute N = A - Z, and electrons = Z.
When given an isotope, the element identity is fixed by Z; different isotopes share the same element but have different N and A.
Important exam reminder: you will usually be given data sheet (periodic table and isotope data); you should not memorize every numeric value beyond what is provided.
Isotope problems: quick tips
If asked to write the isotope symbol from given Z and A: use ^{A}_{Z}\mathrm{X} where X is the element.
If asked to determine neutron count from an isotope: use N = A - Z.
If asked to determine the symbol from full data (e.g., 92 protons): identify element by atomic number (e.g., Z=92 → uranium), then write ^{A}_{92}\mathrm{U} with the given A.
For weighted atomic mass problems: convert percentages to fractions, multiply by isotope masses (or mass numbers as an approximation), and sum.
Quick exam-oriented concepts
The take-home messages:
Atomic number identifies the element; mass number identifies a specific isotope via protons + neutrons.
Atoms are neutral when protons = electrons; ions occur when not equal.
Atomic mass in the periodic table is a weighted average of isotopes, not a single isotope mass.
The atomic mass unit is anchored to Carbon-12 and provides a convenient atomic-scale mass unit.
Isotopes differ in neutron number but often share chemical properties.
Key equations to remember
Protons, neutrons, electrons relationships:
Z = #\text{protons}
A = Z + N
For neutral atoms: #\text{electrons} = Z
Isotope notation:
^{A}_{Z}\mathrm{X}
Example: ^{12}_{6}\mathrm{C}
Atomic mass unit definitions:
1\ \text{amu} = \dfrac{m(\mathrm{C-12})}{12}
1\ \text{amu} = 1.6605 \times 10^{-24}\ \text{g}
Weighted average atomic mass:
\overline{m} = \sumi mi fi,\quad fi = \dfrac{\text{abundance}_i}{100}
Example relationships (conceptual, not numerical): if a given element has isotopes with masses $mi$ and fractional abundances $fi$, the periodic-table value is the weighted sum above.