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dc.contributor.authorLin, Guey-Linen_US
dc.contributor.authorLin, Yen-Hsunen_US
dc.contributor.authorLee, Fei-Fanen_US
dc.date.accessioned2019-04-03T06:37:14Z-
dc.date.available2019-04-03T06:37:14Z-
dc.date.issued2015-02-05en_US
dc.identifier.issn2470-0010en_US
dc.identifier.urihttp://dx.doi.org/10.1103/PhysRevD.91.033002en_US
dc.identifier.urihttp://hdl.handle.net/11536/124571-
dc.description.abstractWe argue that the detection of the neutrino signature from the Earth's core can effectively probe the coupling of heavy dark matter (m(chi) > 10(4) GeV) to nucleons. We first note that direct searches for dark matter (DM) in such a mass range provide much less stringent constraint than the constraint provided by such searches for m(chi) similar to 100 GeV. Furthermore, the energies of neutrinos arising from DM annihilation inside the Sun cannot exceed a few TeVs at the Sun's surface due to the attenuation effect. Therefore, the sensitivity to the heavy DM coupling is lost. Finally, the detection of the neutrino signature from the Galactic halo can only probe DM annihilation cross sections. We present neutrino event rates in IceCube and KM3NeT arising from the neutrino flux produced by annihilation of Earth-captured DM heavier than 10(4) GeV. The IceCube and KM3NeT sensitivities to spin-independent DM-proton scattering cross section sigma(chi p) in this mass range are presented for both isospin-symmetric and isospin-violating cases.en_US
dc.language.isoen_USen_US
dc.titleProbing the coupling of heavy dark matter to nucleons by detecting neutrino signature from the Earth's coreen_US
dc.typeArticleen_US
dc.identifier.doi10.1103/PhysRevD.91.033002en_US
dc.identifier.journalPHYSICAL REVIEW Den_US
dc.citation.volume91en_US
dc.citation.issue3en_US
dc.citation.spage0en_US
dc.citation.epage0en_US
dc.contributor.department物理研究所zh_TW
dc.contributor.departmentInstitute of Physicsen_US
dc.identifier.wosnumberWOS:000352024200002en_US
dc.citation.woscount2en_US
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