Introduction to Atomic Structure
The tiny constituent of an element is an atom. The word atom is a Greek word meaning indivisible, i.e., an ultimate particle which cannot be further subdivided. The idea that all matter ultimately consists of extremely small particles was conceived by ancient Indian and Greek philosophers. The old concept was put on a firm footing by John Dalton in the form of atomic theory which he developed in the years 1803-1808. This theory was a landmark in the history of chemistry.
OBJECTIVE
Towards the end of the nineteenth century, it began to appear that the atom itself might be composed of even smaller particles. In 1833, Michael Faraday showed that there is a relationship between matter and electricity. This was the first major breakthrough to suggest that an atom was not a simple indivisible particle yet smaller but was made up of particles. On the basis of Faraday’s work, Stoney proposed that units of electrical charge are associated with atoms. In 1891, he suggested that these units be called electrons. Electron is a Greek word meaning amber, a material which becomes electrically charged when rubbed with wool or silk.
It is now believed that the atom consists of several particles called sub-atomic particles like electron, proton, neutron, etc. the electron, the proton and the neutron are called Fundamental particles and are building blocks of the atoms about which we shall deal with in this chapter.
PRE-REQUISITE
Law of conservation of Mass
In a chemical reaction the weight of products is equal to the weight of reactants.
Law of definite proportions
If a compound is analysed from various sources, its elemental composition remains the same i.e., analysis of water from a river or ditch or pond either in India or in USA would always give H:O ratio as 2:1. (atom ratio)
Law of Multiple Proportions
Elements combine in simple whole number ratios to form various types of compounds e.g. The ratio of N:O is 1:1, 1:2 and 2:1 in NO, NO2 and N2O, respectively.
Atomic Number (Z)
The total number of protons present in the nucleus of an atom is called as atomic number of that atom.
Mass Number (A)
Total number of nucleons (protons + neutrons) in the nucleus of an atom is called it mass number.
Isotopes
Atoms with the same atomic number but different mass numbers are called isotopes of each other. For example the isotopes of hydrogen atom are: 1H1, 1H2, 1H3.
Isobars
Atoms with same mass number but different atomic number are called as isobars of each other. For example 15P32 and 16S32 are isobars of each other.
Isotones
Atoms having the same number of neutrons but different number of protons are called isotones. For example 6C14, 8O16, 7N15 are isotones as they all have 8 neutrons.
Isodiaphers
Atoms having the same value of (A – 2Z) but different value of A or Z are called isodiapheres. For example 11Na23, 9F19, 7N15 are isodiapheres as (A – 2Z) for all these three atoms is 1.
Nuclear Isomers
Nuclear isomers (isomeric nuclei) are the atoms with the same atomic number and same mass number but different radioactive properties are called nuclear isomers. This type of isomerism is due to the different energy states of the two isomeric nuclei. For example 30Zn69 and 30Zn69 are two atoms with their half life periods 13.8 hours and 57 minutes respectively.
Isoelectronic
Atoms, molecules or ions with same number of electrons are called isoelectronic. For example N2, CO, CN- are isoelctronic.