Many scientists have performed experiments to study the properties, size and nature of an atom, all the measurements have been indirect and manipulation of large scale to fit the microscopic world.
Einstein’s work on theoretical Brownian motion, additionally confirmed the hypothesis and improved the values of Avogadro’s number in the early 1900s.
The composition of an atom, a heavy positive nucleus and negatively charged particles revolving around it, was proved by multiple discoveries.
The discovery of the law of electrolysis by Michael Faraday, 1833.
The identification of cathode rays as electrons and measurement of e/m by Joseph John, 1897.
Precise measurement of e by Robert Millikan, 1909.
Faraday’s law of electrolysis
J.J. Thompsons Experiment
Millikan’s Value of the Elementary Charge
By balancing the electric and gravitational force on individual oil drops, Millikan was able to determine the fundamental electric charge and to show that charges always occur in multiples of e.
The quantum charge of an electron is given by
where n is an integer, m is the mass of the drop, E is the magnitude of the electric field, v is the terminal speed of the drop with field off (falling), and v 1 is the terminal speed of the drop with field on (rising).
Rutherford’s scattering of alpha particles from gold atoms
Bohr’s postulates
These postulates explained the motion of electrons within the atom from the diffraction experiment and the rich and elaborate series of spectral lines emitted by the atom.
Electrons move about the nucleus in circular orbits determined by Coulomb’s and Newton’s laws.
Only certain orbits are stable. The electron does not radiate electromagnetic energy in these special orbits, and because the energy is constant with time these are called stationary states.
A spectral line of frequency f is emitted when an electron jumps from an initial orbit of energy Ei to a final orbit of energy Ef, where,
hf=Ei-Ef
The sizes of the stable electron orbits are determined by requiring the electron’s angular momentum to be an integral multiple of h.
These postulates lead to quantized orbits and quantized energies for a single electron orbiting a nucleus with charge Ze, given by Correspondence principle
As a bridge between the familiar domain of classical physics and the more uncertain domain of atomic systems and quantum theory, Bohr provided the correspondence principle.
Direct confirmation of atomics energy levels: the Frank-Hertz experiment