radioactive decay of uranium

Where the Earth’s Heat Comes From

By Guest PostJuly 18, 2011Scienceanti electron, berkeley lab, borexino experiment, brian fujikawa, bse, bulk silicate earth, department of physics, earth crust and mantle, earth interior, earth magnetic field, geo antineutrinos, geologists, geoneutrinos, gran sasso, heat, heat energy, italy, itaru shimizu, Japan, kamioka liquid-scintillator antineutrino detector, kamland, kamland collaboration, ke han, lawrence berkeley national laboratory, lithophiles, muon neutrinos, neutrinos, partial radiogenic heat model for earth, photomultiplier, potassium, radioactive decay of uranium, radioactive isotopes decay, rock loving elements, sea floors, siderophiles, stuart freedman, study antineutrinos, sunken layer, tau neutrinos, thomas banks, thorium, tohoku university, university of california

*Berkeley Lab scientists join their KamLAND colleagues to measure the radioactive sources of Earth’s heat flow*

What spreads the sea floors and moves the continents? What melts iron in the outer core and enables the Earth’s magnetic field? Heat. Geologists have used temperature measurements from more than 20,000 boreholes around the world to estimate that some 44 terawatts (44 trillion watts) of heat continually flow from Earth’s interior into space. Where does it come from?

Radioactive decay of uranium, thorium, and potassium in Earth’s crust and mantle is a principal source, and in 2005 scientists in the KamLAND collaboration, based in Japan, first showed that there was a way to measure the contribution directly. The trick was to catch what KamLAND dubbed geoneutrinos – more precisely, geo-antineutrinos – emitted when radioactive isotopes decay. (KamLAND stands for Kamioka Liquid-scintillator Antineutrino Detector.) (more…)

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Where the Earth’s Heat Comes From