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Pages in category "Isotopes of titanium"
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The isotopes of titanium range in atomic mass from 38.01 u (38Ti) to 62.99 u (63Ti).
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Main article: Isotopes of titanium
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The calcium in some presolar grains is composed primarily of Ca-44, which is presumably the remains of the extinct radionuclide Ti-44, a titanium isotope which is formed in abundance in Type II supernovae such as SN 1987A after rapid capture of eight alpha particles by Si-28, after the process of silicon burning normally begins, and prior to the supernova explosion.
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Despite its rarity among supernova, this species is able to generate huge amounts of radioactive isotope, known as titanium-44.
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Two kinds of basaltic flood basalts can be distinguished : those poor in P2O5 and in TiO2, called low phosphorus and titanium those rich in P2O5 and in TiO2, called high phosphorus and titanium The isotopic ratios 87Sr/86Sr and 206Pb/204Pb are different from that observed in general, which shows that the basalt flood magma was contaminated as it passed through the continental crust.
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Naturally occurring titanium is composed of five stable isotopes: 46Ti, 47Ti, 48Ti, 49Ti, and 50Ti, with 48Ti being the most abundant (73.8% natural abundance).
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Naturally occurring titanium is composed of 5 stable isotopes: 46Ti, 47Ti, 48Ti, 49Ti, and 50Ti, with 48Ti being the most abundant (73.8% natural abundance).
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Naturally occurring titanium (22Ti) is composed of five stable isotopes; 46Ti, 47Ti, 48Ti, 49Ti and 50Ti with 48Ti being the most abundant (73.8% natural abundance).
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