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Nuclear Physics 243 NMT. Dr. Abdo Mansour Assistant Professor of radiology E-mail : a_mansour@inaya.edu.sa. بسم الله الرحمن الرحيم Lecture No. 1 Introduction to Nuclear Physics. The Atom.
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Nuclear Physics243 NMT Dr. AbdoMansour Assistant Professor of radiology E-mail : a_mansour@inaya.edu.sa
بسم الله الرحمن الرحيم Lecture No. 1 Introduction to Nuclear Physics
The Atom • The word “atom” derives from the Greek word “atom” which means indivisible particle; an atom was the smallest component of matter. • However, we now know that atoms are actually composed of subatomic particles: Protonsand neutrons in the nucleus of the atom, and electrons orbiting that nucleus.
The total number of Protons and Neutrons in a nucleus p + n is the mass number , symbolized by A. • The total number of Protons is called the atomic number and is symbolized by Z. The atomic number and the mass number of an element X are usually presented in the form
Example 9.1 Natural Radioactivity Mass Number number of protons and neutrons atomic symbol boron Atomic Number number of protons
Radiation • The transmission of energy can take the form of electromagnetic radiation (i.e., electromagnetic waves, non-ionizing). • X-rays and γ-rays, are grouped together under the terms “electromagnetic radiation, ionizing” .
Radiation Structure • If the smallest unit of an element is considered to be its atom, the photon is the smallest unit of electromagnetic radiation. • Photon properties: • It have no mass. • It propagates in a straight line. • It travels at the speed of light (300,000 km/s). • It transfers energy to the medium via it passes through the medium.
The energy of the radiation decreases as it passes through a material, due to absorption and scattering .
Radioactivity Process • Radioactivity process means, the nucleus emit energetic particles or rays (α and β particles as well as γ ray).
Types of radioactivity 1- Natural radioactivity: Nuclear reactions occur spontaneously 2- Artificial radioactivity: The artificial radioactivity produced by particle bombardment the nucleus.
Isotopesof an atom have the same number of protons, but a different number of neutrons. • Example: • Carbon atommeans, number of protons = number of neutrons (6 = 6) is carbon-12. * But carbon isotopemeans number of protons ≠ number of neutrons (6 ≠ 8) is carbon-14.
Three Isotopes of Carbon • Each nucleus contains the same number of protons. • Only the number of neutrons is different. • With different numbers of neutrons the mass of each isotope is different. 9.1 Natural Radioactivity
Properties of emission radiations • Radiation refers to particles or waves coming from the nucleus of the atom (radioisotope or radionuclide).
Alpha Particles • Alpha particle (a) is 2 protons and 2 neutrons. • Same as He nucleus (He2+) • Slowmoving, and stopped by small barriers, such as paper. 9.1 Natural Radioactivity
Alpha Decay 238 = 234 + 4 Mass number 92 = 90 + 2 Atomic number
Beta Particles • Beta particles (b) is fast-moving electron, Emitted from the nucleus as a neutron is converted to a proton. • Higher speed particles, more penetrating than alpha particles. • Symbolized by: 9.1 Natural Radioactivity
Beta Decay • Upon decomposition, isotope of nitrogen-16 produces oxygen-16 and a beta particle. • In beta decay, one neutron in nitrogen-16 is converted to a proton and the electron, the beta particle is released.
Gamma Rays • Gamma rays (g) - pure energy or electromagnetic radiation. • High energy. • The most penetrating form of radiation • Symbol is 9.1 Natural Radioactivity g
Gamma Production • Gamma radiation occurs to increase the stability of an isotope. • The atomic mass and number do not change. • Usually gamma rays are emitted along with alpha or beta particles.
In General • The penetrating power of the radiation determines the ionizing damage that can be caused. • Alpha particle < beta particle < gamma rays. 9.1 Natural Radioactivity
Alpha particles are easy to stop, gamma rays are hard to stop.
Half-Life • Half-life (t1/2) is the time required for a given substance to reach half quantity (half initial value). • Each radioactive isotope has its own half-life. • Ranges from a fraction of a second to a billion years. 9.3 Properties of Radioisotopes
Half-Lives of Selected Radioisotopes 9.3 Properties of Radioisotopes
Units of Radiation Measurement The Curie is the amount of radioactive material that produces 3.7 x 1010atomic disintegrations per second. The Roentgenis used for very high energy ionizing radiation only. The Radis used for radiation absorbed dose. 9.8 Measurement of Radiation