atoms

Fundamental Structure of the Atom

An atom is the basic unit of matter that defines the structure of an element. It consists of a dense central core known as the nucleus surrounded by a cloud of negatively charged electrons.

  • Subatomic Particles:

    • Protons: Positively charged particles found within the nucleus. The relative charge is +1+1 and the relative mass is 11.

    • Neutrons: Uncharged (neutral) particles found within the nucleus. The relative charge is 00 and the relative mass is 11.

    • Electrons: Negatively charged particles orbiting the nucleus in energy levels or shells. The relative charge is −1-1 and the relative mass is 11836\frac{1}{1836}.

Atomic Notation and Key Terms
  • Atomic Number (ZZ): The number of protons in the nucleus of an atom. This defines the chemical identity of an element.

  • Mass Number (AA): The total number of protons and neutrons in the nucleus of an atom.

    • Calculation for number of neutrons: Number of neutrons=A−Z\text{Number of neutrons} = A - Z

  • Isotopes: Atoms of the same element with the same number of protons (same ZZ) but different numbers of neutrons (different AA).

    • Example: Carbon-12 (12C^{12}\text{C}) has 66 protons and 66 neutrons, while Carbon-14 (14C^{14}\text{C}) has 66 protons and 88 neutrons.

Electron Configuration

Electrons occupy specific regions around the nucleus called energy levels or electron shells.

  • Shell Capacity:

    • The maximum number of electrons that can occupy a given energy level nn is given by the formula 2n22n^2.

    • First shell (n=1n = 1): Maximum of 22 electrons.

    • Second shell (n=2n = 2): Maximum of 88 electrons.

    • Third shell (n=3n = 3): Maximum of 1818 electrons.

Relative Atomic Mass
  • Relative Atomic Mass (ArA_r): The weighted average mass of an atom of an element relative to 112th\frac{1}{12}\text{th} of the mass of an atom of Carbon-12.

  • Calculation:

    • Ar=Isotope Abundance1×Isotope Mass1+Isotope Abundance2×Isotope Mass2Total AbundanceA_r = \frac{\text{Isotope Abundance}_1 \times \text{Isotope Mass}_1 + \text{Isotope Abundance}_2 \times \text{Isotope Mass}_2}{\text{Total Abundance}}