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Unit C RADIOACTIVITY: NATURAL AND ARTIFICIALRADIOACTIVITY: NATURAL AND ARTIFICIAL (HANK 9:57 )
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C.1 Half-Life: A Radioactive Clock It is useful to know what the rate of decay of a radioisotope is to predict: The time a radioisotope used for medical purposes will remain in the body. the length of storage for hazardous materials. Ages of ancient organisms/civilizations.
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Carbon Dating The use of radiocarbon for dating began some 50 years ago and was based on the detection of the decay of the isotope C-14 which is formed when cosmic rays react with nitrogen gas to form a radioactive carbon dioxide molecule. There are one of these for every million million atoms of carbon 12.
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Half-Lives The rate of decay for radioisotopes is measured in half-lives. A half-life is the amount of time it takes for one-half of a radioisotopic sample to decay into something else. For instance, if H-3 has a half-life of 12.3 years, and you have a 100 gram sample of it, how many grams would be left in 36.9 years?
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Variable half-lives Half-lives can vary from a few seconds to a few billion years. After 10 half-lives, only 1/10,000 th or 0.1% will remain. If you are considering very large numbers of atoms, ie: 6.02 x 10 23, then even after 10 half-lives there is still a considerable amount of the substance left.
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C.3 Benefits of Radioisotopes Ionizing radiation given off by certain radioisotopes can be used in nuclear technology such as: Tracer studies where the radiation is used to track cellular abnormalities, locate damaged areas and aid in therapy. Irradiation, where the radiation is used as an energy source to treat medical conditions like tumors or leukemia and to sterilize medical equipment/seal plastic containers.
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Tracers Radioisotopes called tracers can be used to detect certain elements that are known to collect in specific places in the body. Cesium-137 is used as an external source to treat shallow tumors.
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Radiation Detectors Devices called scintillation counters detect entering radiation as light emitted by the excited atoms when hit with the radiation. Solid-state detectors monitor the movement of electrons through semiconductors like silicon. Liquid Scintillation Counters
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A cloud chamber is a glass filled with supersaturated water vapor. As radiation passes through the chamber, the vapor condenses on the ions formed leaving a white particulate trail.
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Artificial Radioactivity Also called transmutation, Rutherford was the first to create an element different from the original by bombarding helium with nitrogen to form oxygen and hydrogen.
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From 1940 to 1961 Glenn Seaborg and coworkers discovered 10 new element; numbers 94-103 None occur naturally. All were made by high- energy bombardments of heavy nuclei on various particles. Glenn Seaborg and John F Kennedy
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