Atomic Structure and Subatomic Particles

  • Rutherford's Gold Foil Experiment and Atomic Structure:

    • Rutherford used alpha particles, which expose photographic paper (or modern mirror-based detectors), to probe the structure of atoms.

    • The experiment involved a very thin material, allowing alpha particles to pass through a few atoms.

    • Observations:

      • Most alpha particles passed through undeflected, indicating that atoms are mostly empty space.

      • Some particles were deflected at large angles (disturbing deflections).

      • A significant finding was that 11 out of every 20,00020,000 particles actually came all the way back to the emitter.

    • Conclusions:

      • This proved that atoms are not a homogeneous, light substance.

      • For an alpha particle (which is 8,0008,000 times heavier than an electron) to be reflected back, it must hit something significantly heavier than itself.

      • The core of the atom is a very dense, heavy portion called the nucleus.

      • The nucleus contains all of the positive charge, concentrated in a very small area.

      • A direct hit on this positively charged, dense nucleus would cause the alpha particle to reflect straight back.

  • Components of the Atom:

    • Nucleus:

      • The dense core of the atom, containing all protons and neutrons.

      • It is very, very small, often depicted much larger in diagrams for clarity, but in reality, it's a speck at the atom's center.

      • Contains all the positive charge of the atom.

    • Protons:

      • Located in the nucleus.

      • Carry a positive charge, represented as +1+1 in relative units.

      • Typically colored red in diagrams.

    • Neutrons:

      • Located in the nucleus.

      • Are electrically neutral, represented as 00 in relative units.

      • Typically colored white in diagrams.

      • Along with protons, they are collectively called nucleons.

    • Electron Cloud:

      • The region where electrons exist, orbiting around the nucleus.

      • Most things that do not hit the nucleus should be able to pass through the electron cloud.

      • Electrons are easily accessible and can be pulled out of the atom by an electric field because they orbit around the outside.

  • Subatomic Particle Properties (Charge and Mass):

    • Electron:

      • Relative charge: 1-1

      • Relative mass: 11 (base unit of mass)

      • Actual mass: 9.11imes10319.11 imes 10^{-31} kg

    • Proton:

      • Relative charge: +1+1

      • Relative mass: Approximately 2,0002,000 times heavier than an electron.

    • Neutron:

      • Relative charge: 00

      • Relative mass: Approximately 2,0002,000 times heavier than an electron.

      • Important Point: The neutron is slightly heavier than the proton (a difference of about 55 units in relative mass, which has a specific reason for being slightly heavier).

  • Atomic Notation and Isotopes:

    • Atomic Number (ZZ):

      • Defined as the number of protons in an atom.

      • This number uniquely identifies an element and will never change for a given element.

      • It is typically found on the periodic table.

    • Mass Number (AA):

      • Defined as the sum of protons and neutrons in an atom (A=extprotons+extneutronsA = ext{protons} + ext{neutrons}).

      • Represents the total number of nucleons.

    • Isotope Notation:

      • An element is typically represented as ZAextX_Z^A ext{X}, where (X) is the element symbol.

    • Isotopes:

      • Atoms of the same element (meaning they have the same atomic number, ZZ) but have different numbers of neutrons.

      • Since they have different numbers of neutrons, they will have different mass numbers (AA).

      • Example: Iron can have different isotopes, all with the same number of protons (characteristic of iron) but varying numbers of neutrons.

      • The number of electrons usually balances the number of protons to maintain neutrality in an atom.

  • Atomic Mass Unit (AMU):

    • Defined as 1/121/12 the mass of a carbon-1212 atom.

    • This unit provides a standard for measuring the mass of atoms, taking into account the varying weights of different atoms and their isotopes in a sample.