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![]() | README.html | 02-May-2019 17:17 | 1.4K | |
![]() | beda_corr_2may.zip | 02-May-2019 17:18 | 88K | |
![]() | beda_corr_highQ.zip | 13-May-2019 21:05 | 88K | |
![]() | beda_corr_large_sigma.zip | 13-May-2019 21:05 | 90K | |
![]() | beda_eer_inputs_oct11.zip | 11-Oct-2019 18:05 | 892K | |
![]() | jinping_tnu_nominal.out | 02-May-2019 17:10 | 10 | |
![]() | jinping_tnu_toymc.out | 02-May-2019 17:10 | 98K | |
![]() | juno_tnu_nominal.out | 02-May-2019 17:10 | 10 | |
![]() | juno_tnu_toymc.out | 02-May-2019 17:10 | 98K | |
![]() | kamland_tnu_nominal.out | 02-May-2019 17:09 | 10 | |
![]() | kamland_tnu_toymc.out | 02-May-2019 17:09 | 98K | |
![]() | obd_125E_25N_tnu_nominal.out | 02-May-2019 17:11 | 10 | |
![]() | obd_125E_25N_tnu_toymc.out | 02-May-2019 17:11 | 98K | |
Ondřej Šrámek, Charles University, 2 May 2019
Calculation following inputs from Šrámek et al. 2016 (full reference below).
A 20±4 TW Earth and other abundances as in Table 3 of paper, normally distributed except for CLM (lognormal), EM abundance calculated. Cases with negative abundances of any element (K,Th,U) in any reservoir are not included (dice were re-thrown 148 times to get 10000 cases). Here, some cases have EM < DM in terms of abundances.
Total geoneutrino signal predicted at four locations: KamLAND, JUNO, Jinping, oceanic site 125E 25N.
*_tnu_nominal.out ... nominal value, using central values of input abundances
*_tnu_toymc.out ... 10000 toyMC results, inputs fluctuated as described in Šrámek et al. 2016, total geoneutrino prediction in TNU, one per line, corresponding lines across files mean the same throw of dice
beda_corr_2may.zip ... contains all the files
Šrámek, Roskovec, Wipperfurth, Xi, McDonough (2016): "Revealing the Earth’s mantle from the tallest mountains using the Jinping Neutrino Experiment." Sci. Rep., 6:33034, doi:10.1038/srep33034