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Chapter 9

Nuclear Chemistry. Chapter 9. What is nuclear chemistry?. Nuclear chemistry is all about what happens in the nucleus of an atom. In nuclear chemistry, neutrons bomb bard other atoms and force them to split apart.

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Chapter 9

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  1. Nuclear Chemistry Chapter 9

  2. What is nuclear chemistry? • Nuclear chemistry is all about what happens in the nucleus of an atom. • In nuclear chemistry, neutrons bomb bard other atoms and force them to split apart. • Fission is when one atoms splits into two new atoms and releases energy in the form of heat. • Fusion is when two atoms join together.

  3. What is radiation? • In 1896, Henri Becquerel discovered radioactivity. • Radioactivity is the spontaneous emission of energy and particles by atoms of certain elements producing new elements. • Materials that emit this kind of radiation are said to be radioactive and to undergo radioactive decay.

  4. Nuclear chemistry2 • In 1899, Ernest Rutherford discovered that uranium compounds produce three different kinds of radiation. • He separated the radiations according to their penetrating abilities and named them a alpha, b beta, and g gamma radiation, after the first three letters of the Greek alphabet.

  5. Alpha Decay • In alpha decay, the nucleus emits an alpha particle; an alpha particle is essentially a helium nucleus, so it is a group of two protons and two neutrons. A helium nucleus is very stable. • Alpha radiation can be stopped by a sheet of paper.

  6. Beta Decay • A beta particle is an electron. In beta decay an electron is involved. The number of neutrons in the nucleus decreases by one and the number of protons increases by one. • Six millimeters of aluminum are needed to stop most beta particles

  7. Gamma Decay • The third class of radioactive decay is gamma decay, in which the nucleus changes from a higher-level energy state to a lower level. • Several millimeters of lead are needed to stop gamma rays.

  8. Half-Life • The time required for half of the atoms in any given quantity of a radioactive isotope to decay is the half-life of that isotope. • Each particular isotope has its own half-life.

  9. Half-Life2 • For example, the half-life of 238U is 4.5 billion years. That is, in 4.5 billion years, half of the 238U on Earth will have decayed into other elements. In another 4.5 billion years, half of the remaining 238U will have decayed. • One fourth of the original material will remain on Earth after 9 billion years.

  10. What do you know? • Positives? • Negatives?

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