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Typically, the hyperfine structure transition frequency of a particular isotope of caesium or rubidium atoms is used as a basis for these clocks.
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Rubidium-82, one of the element's non-natural isotopes, is produced by electron-capture decay of strontium-82 with a half-life of 25.36 days.
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O yields after 30 subsequent steps pure rubidium alum.
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Rubidium is not known to be necessary for any living organisms.
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The very short half-life of 76 seconds makes it necessary to produce the rubidium-82 from decay of strontium-82 close to the patient.
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This condensation only happens at very low temperatures: around 170 nanokelvins for rubidium atoms.
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The researchers first loaded ultracold rubidium atoms into one-dimensional tubes formed by a two-dimensional lattice (the third standing wave is off for the moment).
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Rubidium is very similar to potassium and therefore tissue with high potassium content will also accumulate the radioactive rubidium.
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Group velocities as low as 8 m/s were measured in a warm thermal rubidium vapor.
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Zone pegmatite ore bodies containing mineable quantities of caesium as pollucite or the lithium minerals lepidolite are also a source for rubidium as a by-product.
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