Author:
Ramírez García D.,Baur D.,Grigat J.,Hofmann B.A.,Lindemann S.,Masson D.,Schumann M.,von Sivers M.,Toschi F.
Abstract
Abstract
The GeMSE (Germanium Material and meteorite Screening
Experiment) facility operates a low-background HPGe crystal in an
underground laboratory with a moderate rock overburden of
620 m.w.e. in Switzerland. It has been optimized for continuous
remote operation. A multi-layer passive shielding, a muon veto, and
a boil-off nitrogen purge line inside the measurement cavity
minimize the instrument's background rate, which decreased by 33%
to (164 ± 2) counts/day (100 – 2700 keV) after five years of
underground operation. This agrees with the prediction based on the
expected decay of short-lived isotopes. A fit to the known
background components, modeled via a precise simulation of the
detector, shows that the GeMSE background is now muon-dominated. We
also present updates towards a more accurate detection efficiency
calculation for the screened samples: the thickness of the crystal's
outer dead-layer is precisely determined and the efficiency can now
be easily calculated for any sample geometry. The advantage of this
feature is showcased via the determination of the 40K content
in the screening of a complex-shaped object: a banana.
Subject
Mathematical Physics,Instrumentation
Cited by
8 articles.
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