001     889363
005     20230111074312.0
024 7 _ |a 10.1080/10619127.2020.1752098
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037 _ _ |a FZJ-2021-00252
041 _ _ |a English
082 _ _ |a 530
100 1 _ |a Kumaran, S.
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245 _ _ |a A New Journey to the Center of the Earth
260 _ _ |a London
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520 _ _ |a 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.
536 _ _ |a 612 - Cosmic Matter in the Laboratory (POF3-612)
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650 2 7 |a Particle Physics
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650 1 7 |a Nuclei and Particles
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700 1 _ |a Ludhova, L.
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773 _ _ |a 10.1080/10619127.2020.1752098
|g Vol. 30, no. 4, p. 17 - 21
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|t Nuclear physics news
|v 30
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856 4 _ |u https://juser.fz-juelich.de/record/889363/files/2102.05562.pdf
|y Published on 2020-12-30. Available in OpenAccess from 2021-12-30.
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