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arXiv · 1405.0192

Geo-neutrinos and Earth Models

S. T. Dye·Y. Huang·V. Lekic·W. F. McDonough·O. Sramek
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Abstract

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.

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S. T. Dye, Y. Huang, V. Lekic, W. F. McDonough, O. Sramek. 2014-05-01. Geo-neutrinos and Earth Models. https://arxiv.org/abs/1405.0192

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