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When an organism dies, it no more absorbs carbon-fourteen. the quantity of carbon-14 in the organism will start to beta decay into nitrogen. Measuring the amounts of carbon-14 from the fossilized remains of useless organisms may help ascertain the time frame when extinct species existed on the planet.
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Carbon-fourteen is produced in Earth’s higher ambiance by cosmic rays bombarding nitrogen fuel atoms. Carbon-14 is absorbed by vegetation and animals, and it appears in these organisms at the same focus degrees found in the atmosphere.
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The fusion of two scaled-down atoms to be a bigger atom involves an incredible level of activation energy to overcome the electrostatic repulsion with the protons. as opposed to much larger atoms, like uranium-235 or uranium-238, which have numerous protons shut together which makes it rather easy to induce them to break apart, bringing little atoms alongside one another to create greater types is kind of tricky. An example of a fusion reaction would be the fusion of two isotopes of hydrogen atoms right into a helium atom: