Neutrino geophysics : proceedings of Neutrino Sciences 2005 by Stephen T. Dye

By Stephen T. Dye

Those pages current a set of contemporary papers essentially documenting the nascent technology of neutrino geophysics. lots of the papers from talks given at 1 Neutrino Sciences 2005: Neutrino Geophysics held on the college of Hawaii in December 2005. numerous papers have been solicited later in an e?ort to make the gathering as accomplished as attainable. each paper was once scrutinized via an exterior reviewer to guarantee the standard of scienti?c content material. those reviewers are thanked for lending their scienti?c services via their many considerate reviews and recommendations. All authors are recommended for supplying very good manuscripts in their very important paintings whereas retaining a spirit of cooperative collaboration all through. even though each test used to be made to provide a completely exact quantity, it's the authorised accountability of the affiliate editor for any errors, error, or omissions within the p- sented fabric. The innovations, suggestion, and knowledge of John realized and Sandip Pakvasa have been essential in organizing and finishing this undertaking. P- duction fees have been generously supplied by means of the college of Hawaii. The help of Hawaii Paci?c collage, which contributed educating unlock time, is gratefully - knowledged. Stephen T. Dye affiliate Editor November 28, 2006 Stephen T. Dye is an affiliate professor of physics at Hawaii Paci?c college and an a?liate to the graduate college of the dept of Physics and Astronomy on the collage of Hawaii at Manoa. 1 See www. phys. hawaii. edu/ sdye/hnsc. html Earth, Moon, and Planets (2006) 99:1 15 Springer 2006 DOI 10."

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It is is thus not useful to hold on to the rigid classification of elements as lihtophile, chalcophile or siderophile. Rather, to evaluate realistically whether or not there is radioactivity in the core, we need to investigate the geochemical behavior of these radioactive elements at the high P and T conditions relevant to core–mantle segregation in the earth. Such investigations are emerging just now. Of the three main radioactive elements in the earth, K, U and Th, potassium is the only element for which there is some basis both in theory and experiment calling for its presence in the core.

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