In this chapter, we will study various atomic models. Initially, J.J. Thomson proposed an atomic model in which he thought of as electrons embedded in between protons. In 1911, his student Earnest Rutherford proposed a nuclear model, on the basis of a scattering experiment. In spite of strong experimental evidence, Rutherford’s model of the atom was rejected on the ground of the classical theory of electromagnetism.
So in order to rectify the shortcomings of Rutherford’s model, in 1913, Niels Bohr combined the classical and early quantum concepts of Einstein and Plank to explain the stability of an atom.
According to Thomson, “An atom consists of positively charged matter, into which negatively charged particles are embedded randomly”. But this model did not last long as it could not explain the observations of Rutherford’s alpha-particle scattering experiment.
In 1911, Rutherford, along with his assistants, H. Geiger and E. Marsden, performed the Alpha Particle scattering experiment, which led to the birth of the ‘nuclear model of an atom’.
They took a thin gold foil having a thickness of 2.1×10-7 m and placed it in the center of a rotatable detector made of zinc sulfide and a microscope. Then, they directed a beam of 5.5MeV alpha particles emitted from a radioactive source at the foil. Lead bricks collimated these alpha particles as they passed through them.

After hitting the foil, the scattering of these alpha particles could be studied by the brief flashes on the screen. Rutherford and his team expected to learn more about the structure of the atom from the results of this experiment.
Here is what they found:
In 1912, Rutherford proposed his nuclear model of the atom. It is also known as Rutherford’s planetary model of the atom. Salient features of Rutherford’s atom model are as follows :
It was Niels Bohr (1885-1962) who used the concept of quantized energy and explained the model of a hydrogen atom in 1913. Bohr combined classical and early quantum concepts and proposed a theory in the form of three postulates. These postulates are:
The lowest energy level of an atom is called the “ground state” and higher levels are called “excited states”. The H-atom has the lowest energy in the state for the principal quantum number n = 1. and all other states (i.e, for n = 2, 3, 4…) are excited states. Thus E2, E3, E4 …are called the first, the second, and the third …excited states respectively.
The minimum energy needed to ionize an atom is called “ionisation energy”. The potential difference through which an electron should be accelerated to acquire this much energy is called “ionisation potential”. Hence, ionisation energy of H-atom in the ground state is 13.6 eV and ionisation potential is 13.6 V.
The binding energy of a system is defined as the minimum energy needed to separate its constituents over large distances. This may also be defined as the energy released when its constituents are brought from infinity to form the system. The binding energy of H-atom in the ground state is 13.6 eV which is the same as its ionization energy.
The energy needed to take an atom from its ground state to an excited state is called the “excitation energy” of that excited state. The potential through which an electron should be accelerated to acquire this energy is called the “excitation potential”.
Bohr’s model explains the spectral lines of the hydrogen atomic emission spectrum. While the electron of the atom remains in the ground state, its energy is unchanged. When the atom absorbs one or more quanta of energy, the electron moves from the ground state orbit to an excited state orbit that is further away. When the atom relaxes back to a lower energy state, it releases energy that is again equal to the difference in energy of the two orbits.
Based on the wavelengths of the spectral lines, Bohr was able to calculate the energies that the hydrogen electron would have in each of its allowed energy levels. He then mathematically showed which energy level transitions corresponded to the spectral lines in the atomic emission spectrum.
The general formula for wavelength of emitted radiation is given by
1λ=R(1n21−1n22)1λ=R(1n12-1n22)
where n2 = 2, 3, 4, …. and n2 > n1
R = 1.01 x 107 m-1 = Rydberg constant

He found that the four visible spectral lines corresponded to transitions from higher energy levels down to the second energy level (n = 2). This is called the Balmer series. Transitions ending in the ground state (n = 1) are called the Lyman series, but the energies released are so large that the spectral lines are all in the ultraviolet region of the spectrum. The transitions called the Paschen series and the Brackett series both result in spectral lines in the infrared region because the energies are too small.
de-Broglie explained the second postulate of Bohr’s atomic model by assuming an electron to be a particle wave. Therefore, it should form standing waves under resonance conditions.

According to de-Broglie, for an electron moving in nth circular orbit of radius r,
2πr = nλ n = 1, 2, 3, …..
i.e., the circumference of the orbit should be an integral multiple of the de-Broglie wavelength of an electron moving in nth orbit. As we know that de-Broglie wavelength,
λ=hmvλ=hmv
2πr=nhmv2πr=nhmv
mvr=nh2π