Geo-neutrinos and Earth Models

S. T. Dye, Y. Huang, V. Lekic, W. F. McDonough, O. Šrámek

研究成果: Conference article査読

6 被引用数 (Scopus)

抄録

We present the current status of geo-neutrino measurements and their implications for radiogenic heating in the mantle. Earth models predict different levels of radiogenic heating and, therefore, different geo-neutrino fluxes from the mantle. Seismic tomography reveals features in the deep mantle possibly correlated with radiogenic heating and causing spatial variations in the mantle geo-neutrino flux at the Earth surface. An ocean-based observatory offers the greatest sensitivity to the mantle flux and potential for resolving Earth models and mantle features. Refinements to estimates of the geo-neutrino flux from continental crust reduce uncertainty in measurements of the mantle flux, especially measurements from land-based observatories. These refinements enable the resolution of Earth models using the combined measurements from multiple continental observatories.

本文言語English
ページ(範囲)310-318
ページ数9
ジャーナルPhysics Procedia
61
DOI
出版ステータスPublished - 2015
イベント13th International Conference on Topics in Astroparticle and Underground Physics, TAUP 2013 - , United States
継続期間: 2013 9 82013 9 13

ASJC Scopus subject areas

  • Physics and Astronomy(all)

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