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Explore the fascinating realm of nuclear chemistry, uncovering the mysteries of isotopes, nuclear instability, and radioactive decay. Learn about alpha and beta decay, radioactive decay reactions, decay series, and the concept of half-life. Discover the applications of nuclear fission, fusion, and radiation, including their uses in nuclear power and weaponry. Gain insight into radiocarbon dating techniques and the different types of radiation exposure.
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Nuclear Chemistry The weird world of the nucleus
Isotope Refresher • Atoms of the same element all have the same number of protons • Atoms of the same element may have different neutrons and therefore mass numbers (p+ + n0)
Nuclear Instability • Not all combinations of protons and neutrons are created equal • Some are more unstable than others. • If they are unstable they will do one of the following: • Radioactive decay • Nuclear fission • Nuclear fusion
Nuclear “Reactions” • Nuclear “reactions” must still be balanced. • Notice 238 = 4 + 234 “Mass balanced” • Notice 92 = 2 + 90 “Charge balanced”
Radioactive Decay • Radioactive decay – the nucleus of an atom undergoes a change so that it is no longer the same element • Decay is a totally random event. Nothing has an effect when an atom decays Two Main Types of Radioactive Decay • Alpha decay • Beta decay
Alpha Decay • Alpha decay – emission of an alpha particle from the nucleus • Alpha (α) particle - a helium-4 nucleus • Uranium-235, “enriched uranium,” decays by alpha decay
Beta Decay • Beta decay – emission of a beta particle from the nucleus • Beta (β) particle – electron • Thorium-231 decays by beta decay
Practice Decay Reactions • Beta decay by cesium-137 • Alpha decay by polonium-210
Decay Series • Some atoms require multiple decays to become stable • Most decay series of naturally occurring isotopes end in lead.
Half Life • Half life – the amount of time it takes for ½ of a radioactive isotope to decay into something else. • Notice the atoms don’t disappear, they just change their identity.
Half Life Problem • A 100.0g radioactive sample decays for 5 hours. Only 12.5g of the original isotope remains after 5 hours. How long is the half life? • 3 half lives = 5 hours • 5hours/3half lives = 1.67hours/halflife
Half Life Problem Selenium-72 has a half life of 8.40 days. How much of a 450.0g sample of selenium-72 will remain after 42.0 days? 25.2 days
Radiocarbon Dating Technique • Uses the known half life of C-14 to estimate death of organic matter • Based on the known ratio of C-14 to C-12
Nuclear Fission • Nuclear fission – one atom’s nucleus splits apart. • A neutron strikes a nucleus causing it to split into small pieces • Releases lots of energy. • Extra neutrons are also produced.
Nuclear Fission • The extra neutrons can cause a chain reaction
Uses of Nuclear Fission • Nuclear power • Energy produced by fission is transferred as heat to a coolant
Uses of Nuclear Fission Mushroom cloud from Nagasaki
Uses of Nuclear Fission • Nuclear weaponry • “Atomic bomb” • “A-bomb” • Runaway fission reaction resulting in an explosion.
Nuclear Fusion • Fusion – combining of nuclei • Above reactions describe fusion in the Sun. • Releases more energy than fission. • Also requires very high temperatures.
Uses of Nuclear Fusion • Fusion weapons • Hydrogen bomb • “H-bomb” • Thermonuclear bomb • Uses a fission reaction to start the fusion reaction • “A-bomb” is the detonator for an “H-bomb”
3 Primary Types of Radiation • Alpha radiation – α – alpha particles • Low energy • Result of alpha decay • Low penetration • Stop with a sheet of paper • Beta radiation – β –beta particles (electrons) • Higher energy • Result of beta decay • Some penetration ability • Stop with several sheets of aluminum foil • Gamma radiation – γ –high energy gamma rays • Very high energy • Can result from any type of decay • Very highly penetrating and damaging • Stop with several centimeters of lead or very thick concrete