Review/Journal Article FZJ-2021-00252

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A New Journey to the Center of the Earth

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2020
Taylor & Francis London

Nuclear physics news 30(4), 17 - 21 () [10.1080/10619127.2020.1752098]

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Abstract: There are still several unanswered fundamental questions concerning our planet and in particular, about the deep Earth, from where we lack direct samples. Today, due to the progress in neutrino-detection techniques, a new and unique tool to study our planet exists: geoneutrinos, antineutrinos from the decays of long-lived radioactive elements inside the Earth. In 2020, the Borexino experiment published its updated geoneutrino measurement. Thanks to the increase in acquired data and the improved analysis techniques in an enlarged fiducial volume, the final precision has significantly improved, corresponding to a total geoneutrino signal of 47.0+8.4−7.7(stat)+2.4−1.9(sys) TNU. The null-hypothesis of the geoneutrino signal from the Earth's mantle was excluded at a 99% C.L. for the first time, while exploiting the knowledge of the local crust around the detector. The article will introduce the field and describe the key elements of the updated analysis. Geological interpretation and significance of the new result will be discussed in terms of the corresponding radiogenic heat and the limits to a hypothetical georeactor.

Keyword(s): Nuclei and Particles (1st) ; Particle Physics (2nd) ; Geosciences (2nd)

Classification:

Contributing Institute(s):
  1. Experimentelle Hadrondynamik (IKP-2)
Research Program(s):
  1. 612 - Cosmic Matter in the Laboratory (POF3-612) (POF3-612)

Appears in the scientific report 2021
Database coverage:
Embargoed OpenAccess ; Ebsco Academic Search ; SCOPUS
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 Record created 2021-01-13, last modified 2023-01-11


Published on 2020-12-30. Available in OpenAccess from 2021-12-30.:
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