Nuclear Composition and Notation:
An atom consists of a dense positively charged nucleus containing nucleons (protons and neutrons) surrounded by orbiting electrons. Standard nuclear representation: $\mathbf{_Z^A X}$, where $Z$ is the Atomic Number (number of protons) and $A$ is the Mass Number (total number of nucleons = protons + neutrons). Neutron number $N = A - Z$.
- Isotopes: Atoms of the same element having the same atomic number $Z$ but different mass numbers $A$ (e.g. $_1^1\text{H}, _1^2\text{H}, _1^3\text{H}$ or $_{17}^{35}\text{Cl}, _{17}^{37}\text{Cl}$). They possess identical chemical properties but different physical weights.
- Isobars: Atoms of different elements having the same mass number $A$ but different atomic numbers $Z$ (e.g. $_{18}^{40}\text{Ar}$ and $_{20}^{40}\text{Ca}$).
- Isotones: Nuclei having the same number of neutrons $N$ but different $Z$ and $A$ (e.g. $_6^{14}\text{C}$ and $_8^{16}\text{O}$, both having $N = 8$).
Radioactivity as a Purely Nuclear Phenomenon:
Radioactivity is the spontaneous disintegration of an unstable atomic nucleus accompanied by the emission of ionizing radiations ($lpha, eta, \gamma$). Crucially, radioactivity is entirely independent of all external physical conditions (temperature, pressure, magnetic or electric fields) and chemical combinations (whether uranium is elemental or bonded as uranium oxide, its radioactive decay rate remains strictly unchanged). This proves that radioactivity is an intrinsic nuclear process, completely independent of orbital valence electrons!