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[2] [70] The island of stability for spherical nuclei may also be a "coral reef" (i.e., a broad region of increased stability without a clear "peak") around N = 184 and 114 ≤ Z ≤ 120, with half-lives rapidly decreasing at higher atomic number, due to combined effects from proton and neutron shell closures.
842 × 431 (2.28 MB) Kylegodbey: I have updated the proton numbers along the Z axis to address the issue brought forth on the talk page. See the issue here: w:Talk:Island of stability #The diagram in the beginning of the article has wrong numbers in the Z(proton number) axis: 17:07, 23 June 2012: 842 × 431 (1.93 MB) InvaderXan
The island of stability is a region outside the valley of stability where it is predicted that a set of heavy isotopes with near magic numbers of protons and neutrons will locally reverse the trend of decreasing stability in elements heavier than uranium.
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The island of stability is a hypothetical region in the top right cluster of nuclides that contains isotopes far more stable than other transuranic elements. There are no stable nuclides having an equal number of protons and neutrons in their nuclei with atomic number greater than 20 (i.e. calcium) as can be readily observed from the chart ...
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