Oxygen-17
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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Oxygen-17 is the only stable isotope of oxygen possessing a nuclear spin. It was a product out of 14N and 42He2+ the early man-made transmutation conducted by Frederick Soddy and Ernest Rutherford in 1917-1919.The isotope was first hypothesized and subsequently imaged by Patrick Blackett in Rutherford''s lab 1924: Of the nature of the integrated nucleus little can be said without further data. It must however have a mass 17, and provided no other nuclear electrons are…mehr

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Please note that the content of this book primarily consists of articles available from Wikipedia or other free sources online. Oxygen-17 is the only stable isotope of oxygen possessing a nuclear spin. It was a product out of 14N and 42He2+ the early man-made transmutation conducted by Frederick Soddy and Ernest Rutherford in 1917-1919.The isotope was first hypothesized and subsequently imaged by Patrick Blackett in Rutherford''s lab 1924: Of the nature of the integrated nucleus little can be said without further data. It must however have a mass 17, and provided no other nuclear electrons are gained or lost in the process, an atomic number 8. It ought therefore to be an isotope of oxygen. If it is stable it should exist on the earth.