Literature DB >> 20502855

A possible in situ 3H and 3He source in Earth's interior: an alternative explanation of origin of 3He in deep Earth.

Songsheng Jiang1, Jing Liu, Ming He.   

Abstract

Origin of (3)He in the Earth is a mystery. Lacking a production mechanism, scientists assume (3)He was trapped in the Earth, when the Earth was formed. In contrast to this assumption, we have found (3)He and (3)H concentrations in excess of the atmospheric values in the deep waters of the volcanic Lakes Pavin (France), Laacher (Germany) and Nemrut (Turkey). This paper reports the result of finding (3)H in these three volcanic lakes that appear to originate from the mantle. Because (3)H has a half-life of 12.3 years, this (3)H and the resulting (3)He must have formed recently in the mantle and not be part of a primordial reservoir. The nuclear reactions that generate tritium might be a source of "missing" energy in the interior of the Earth.

Entities:  

Mesh:

Substances:

Year:  2010        PMID: 20502855     DOI: 10.1007/s00114-010-0681-z

Source DB:  PubMed          Journal:  Naturwissenschaften        ISSN: 0028-1042


  5 in total

1.  Nuclear georeactor origin of oceanic basalt 3He/4He, evidence, and implications.

Authors:  J Marvin Herndon
Journal:  Proc Natl Acad Sci U S A       Date:  2003-03-03       Impact factor: 11.205

2.  Helium-3 from the mantle: primordial signal or cosmic dust?

Authors:  D L Anderson
Journal:  Science       Date:  1993-07-09       Impact factor: 47.728

3.  High 3He/4He ratios in picritic basalts from Baffin Island and the role of a mixed reservoir in mantle plumes.

Authors:  Finlay M Stuart; Solveigh Lass-Evans; J Godfrey Fitton; Robert M Ellam
Journal:  Nature       Date:  2003-07-03       Impact factor: 49.962

4.  Rogue mantle helium and neon.

Authors:  Francis Albarède
Journal:  Science       Date:  2008-01-17       Impact factor: 47.728

5.  Theory of Bose-Einstein condensation mechanism for deuteron-induced nuclear reactions in micro/nano-scale metal grains and particles.

Authors:  Yeong E Kim
Journal:  Naturwissenschaften       Date:  2009-05-14
  5 in total

北京卡尤迪生物科技股份有限公司 © 2022-2023.