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The decay of 40 K in Earth's mantle ranks third, after 232 Th and 238 U, in the list of sources of radiogenic heat. Less is known about the amount of radiogenic sources in Earth's outer and inner core, which lie below the mantle. It has been proposed, though, that significant core radioactivity (1–2 TW) may be caused by high levels of U, Th ...
19 K) has 25 known isotopes from 34 K to 57 K as well as 31 K, as well as an unconfirmed report of 59 K. [3] Three of those isotopes occur naturally: the two stable forms 39 K (93.3%) and 41 K (6.7%), and a very long-lived radioisotope 40 K (0.012%) Naturally occurring radioactive 40 K decays with a half-life of 1.248×10 9 years. 89% of those ...
The compounds produced using stable isotopes are either specified by the percentage of labeled isotopes (that is, 30% uniformly labeled 13 C glucose contains a mixture that is 30% labeled with 13 carbon isotope and 70% naturally labeled carbon) or by the specifically labeled carbon positions on the compound (that is, 1-13 C glucose which is ...
The darker more stable isotope region departs from the line of protons (Z) = neutrons (N), as the element number Z becomes larger. Isotopes are nuclides with the same number of protons but differing numbers of neutrons; that is, they have the same atomic number and are therefore the same chemical element. Isotopes neighbor each other vertically.
List: 86 Ru 87 Ru 88 Ru 89 Ru 90 Ru 91 Ru 92 Ru 93 Ru 94 Ru 95 Ru 96 Ru 97 Ru 98 Ru 99 Ru 100 Ru 101 Ru 102 Ru 103 Ru 104 Ru 105 Ru 106 Ru 107 Ru 108 Ru 109 Ru 110 Ru 111 Ru 112 Ru 113 Ru 114 Ru 115 Ru
The column labeled "energy" denotes the energy equivalent of the mass of a neutron minus the mass per nucleon of this nuclide (so all nuclides get a positive value) in MeV, formally: m n − m nuclide / A, where A = Z + N is the mass number. Note that this means that a higher "energy" value actually means that the nuclide has a lower energy.
This is a list of positron emission tomography (PET) radiotracers. These are chemical compounds in which one or more atoms have been replaced by a short-lived, positron emitting radioisotope. Cardiology
40 Zirconium: List: 74 Zr 75 Zr 76 Zr 77 Zr 78 Zr 79 Zr 80 Zr 81 Zr 82 Zr 83 Zr 84 Zr 85 Zr 86 Zr 87 Zr 88 Zr 89 Zr 90 Zr 91 Zr 92 Zr 93 Zr 94 Zr 95 Zr 96 Zr 97 Zr 98 Zr 99 Zr 100 Zr 101 Zr 102 Zr 103 Zr