The possible sources analyzed up to now for the neutron flux background at the Gran Sasso National Laboratory are the natural radioactivity in the rock, the concrete, as well as the induced part coming from interaction of cosmic ray muons with the rock or the detector material itself. Water was considered only as moderator in concrete, due to its variable concentration and its radioactivity as additional source for neutron flux modulation. Therefore, the water-rock interaction and its spatial-temporal variation induced by hydrological pattern of the Gran Sasso aquifer are taken into account.

Plastino, W., Nisi, S., De Luca, G., Balata, M., Laubenstein, M., Bella, F. (2009). Environmental radioactivity in the ground water at the Gran Sasso National Laboratory (Italy): a possible contribution to the variation of the neutron flux background. JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY, 282(3), 809-813 [10.1007/s10967-009-0151-2].

Environmental radioactivity in the ground water at the Gran Sasso National Laboratory (Italy): a possible contribution to the variation of the neutron flux background

PLASTINO, Wolfango;
2009-01-01

Abstract

The possible sources analyzed up to now for the neutron flux background at the Gran Sasso National Laboratory are the natural radioactivity in the rock, the concrete, as well as the induced part coming from interaction of cosmic ray muons with the rock or the detector material itself. Water was considered only as moderator in concrete, due to its variable concentration and its radioactivity as additional source for neutron flux modulation. Therefore, the water-rock interaction and its spatial-temporal variation induced by hydrological pattern of the Gran Sasso aquifer are taken into account.
2009
Plastino, W., Nisi, S., De Luca, G., Balata, M., Laubenstein, M., Bella, F. (2009). Environmental radioactivity in the ground water at the Gran Sasso National Laboratory (Italy): a possible contribution to the variation of the neutron flux background. JOURNAL OF RADIOANALYTICAL AND NUCLEAR CHEMISTRY, 282(3), 809-813 [10.1007/s10967-009-0151-2].
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11590/136142
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