A high efficiency, low background counting setup has been made at TIFR
consisting of a special HPGe detector ($\sim$ 70%) surrounded by a low activity
copper+lead shield. Detailed measurements are performed with point and extended
geometry sources to obtain a complete response of the detector. An effective
model of the detector has been made with GEANT4 based Monte Carlo simulations
which agrees with experimental data within 5%. This setup will be used for
qualification and selection of radio-pure materials to be used in a cryogenic
bolometer for the study of Neutrinoless Double Beta Decay in $^{124}$Sn as well
as for other rare event studies. Using this setup, radio-impurities in the rock
sample from India-based Neutrino Observatory (INO) site have been estimated.Comment: 23 pages, 13 figures, re-submitted to NIM A (minor changes in text,
figures and table
Proximity of a topological insulator (TI) surface with a magnetic insulator (MI) can open an exchange gap at the Dirac point leading to exploration of surface quantum anomalous Hall effect. An important requirement to observe the above effect is to prevent the topological breakdown of the surface states (SSs) due to various interface coupling effects and to tune the Fermi level at the interface near the Dirac point. In this work, we demonstrate the growth of high-quality c-axis oriented strain-free layered films of TI, Bi2Se3, on amorphous SiO2 substrate in proximity to an MI, europium sulfide (EuS), that show stronger weak anti-localization response from the surface than previous studies with epitaxially interfaced heterostructures. Importantly, we find gate and magnetic field cooling modulated localization effects in the SSs, attributed to the position of interface Fermi level within the band gap that is also corroborated from our positron annihilation spectroscopy measurements. Furthermore, our experiments provide a direct evidence of gate-controlled enhanced interface magnetism in EuS arising from the carrier mediated Ruderman–Kittel–Kasuya–Yosida interactions across the Bi2Se3/EuS interface. These findings demonstrate the existence of complex interfacial phenomena affecting the localization response of the SSs that might be important in proximity engineering of the TI surface to observe surface quantum Hall effects.
The neutron flux at low energy (E n ≤ 15 MeV) resulting from the radioactivity of the rock in the underground cavern of the India-based Neutrino Observatory is estimated using Geant4-based Monte Carlo simulations. The neutron production rate due to the spontaneous fission of 235,238 U, 232 Th and (α, n) interactions in the rock is determined employing the actual rock composition. It is shown that the total flux is equivalent to a finite size cylindrical rock (D = L = 140 cm) element. The energy integrated neutron flux thus obtained at the center of the underground tunnel is 2.76 (0.47) ×10 −6 n cm −2 s −1 . The estimated neutron flux is of the same order (∼ 10 −6 n cm −2 s −1 ) as measured in other underground laboratories.
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