Understand the historical development of atomic theory.
Identify and describe the atomic structure and the role of electron shells.
Comprehend radioactivity and the properties of alpha and beta particles.
Differentiate between particulate and electromagnetic ionizing radiation.
History of the Atom
Centuries of Discovery
Greek Atom Theory
Dalton’s Atomic Theory
Thomson's Plum Pudding Model
Rutherford’s Nuclear Model
Bohr’s Model
Atomic Structure
Fundamental Particles
Electron Arrangements
Electron Binding Energy
Radioactivity
Types of Ionizing Radiation
Properties of Alpha and Beta Particles
Radioactive Half-life
Greek Atom: Proposed by early philosophers, where matter was believed to be made of four elements (earth, water, air, fire) combined with essences (wet, dry, hot, cold).
John Dalton (1808): Introduced the idea that each element has identical atoms differing from those of other elements, leading to atomic theory based on atomic mass.
J.J. Thomson (1897): Discovered electrons and proposed the Plum Pudding Model, describing atoms as a mix of positive charge with embedded electrons.
Ernest Rutherford (1911): Conducted gold foil experiment, leading to the nuclear model of the atom, which has a small, dense positively charged nucleus and electrons surrounding it.
Niels Bohr (1913): Enhanced Rutherford's model by introducing quantized electron orbits or shells around the nucleus, forming the Bohr model, which describes the atom like a small solar system.
Fundamental Particles
Protons: Positively charged, located in the nucleus, ~1 amu.
Neutrons: Neutrally charged, also in the nucleus, ~1 amu.
Electrons: Negatively charged, located in orbitals around the nucleus, negligible mass (~0.000549 amu).
Electron Arrangement
Electrons occupy specific energy shells (K, L, M, N)
Maximum electrons per shell given by the formula: 2n², where n is the shell number.
Electron Binding Energy
The amount of energy required to remove an electron from the atom. K-shell electrons are tightly bound, more energy is required to ionize them compared to those in outer shells.
Types of Ionizing Radiation
Particulate Radiation:
Alpha Particles: Composed of 2 protons and 2 neutrons; not significantly penetrating but highly ionizing; emitted from heavy radioactive nuclei.
Beta Particles: Electrons or positrons emitted from nuclei; lighter than alpha particles and can penetrate deeper into tissue.
Electromagnetic Radiation:
Includes X-rays and gamma rays; photon-based, no mass or charge, can penetrate various materials depending on energy.
Radioactive Half-life
Time required for half of the radioactive substance to decay; unique for each isotope; utilized in various applications like radiometric dating.
Atoms are the smallest unit of elements and compounds are formed by atoms combining through either ionic (electrons transferred) or covalent (electrons shared) bonds.
Nucleons (protons and neutrons) are found within the nucleus; electrons orbit the nucleus in defined shells or energy levels.
Nuclear stability is dictated by the balance of protons and neutrons, leading to concepts of isotopes, isobars, and isotones.
Radioactivity describes the decay of unstable atomic nuclei, releasing particles and energy, characterized primarily through beta and alpha emissions.
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