Proc. Neutrino Astrophysics - MPP Theory Group
Proc. Neutrino Astrophysics - MPP Theory Group
Proc. Neutrino Astrophysics - MPP Theory Group
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could be gravitationally captured, the resulting accumulation of neutralinos continuing until<br />
balanced by χχ annihilation. Final states from χχ annihilation include many particles which<br />
subsequently decay to final states including energetic neutrinos which can be detected by<br />
ANTARES. If we assume that the dark matter in the halo of our galaxy consists of neutralinos,<br />
then a large fraction of the currently allowed SUSY parameter space predicts neutrino fluxes<br />
from χχ annihilation in the centres of the Sun and of the Earth which would be detectable [2]<br />
with exposure times of around 10 5 m 2 yr.<br />
High energy muon-neutrinos can be detected by observing long-range muons produced by<br />
charged current neutrino-nucleon interactions in the matter surrounding the detector. An<br />
array of photomultiplier tubes, placed in an optically transparent medium such as deep ocean<br />
water or antarctic ice, can be used to detect the Čerenkov photons produced along the muon<br />
tracks. Since Čerenkov radiation is emitted in a cone of fixed angle (42 degrees in water) the<br />
direction of the muon, which preserves the neutrino direction, can be reconstructed from the<br />
location and time of the PMT ‘hits’. Simulation studies of prototype ANTARES detectors<br />
show that the angular resolution for reconstructed muons could be better than 0.2◦ . Moreover,<br />
for muons with energies above 1–10 TeV, the average angle between the muon and the parent<br />
neutrino is lower than 0.1◦ . Above 1 TeV, the average number of Čerenkov photons produced<br />
per meter of muon track is proportional to the muon’s energy so that the number of detected<br />
photons can be used to measure the muon energy, albeit with poor resolution due to the<br />
stochastic nature of muon energy loss above 1 TeV.<br />
Muons from cosmic ray interactions in the Earth’s atmosphere produce a large background<br />
of down-going muons which is many orders of magnitude greater than any potential neutrino<br />
signal. Thus the aperture of the telescope is restricted to the 2π solid angle of up-going muon<br />
events where this background is negligible, provided that the detector missreconstructs less<br />
than 1 in 105 (for a detector at 2.5 km depth) down-going events as up-going events. If<br />
this is achieved then the dominant background source of up-going muons will be from upgoing<br />
atmospheric neutrinos which can interact, just like the cosmic neutrinos, in the rock<br />
or water below the detector. This background is isotropic and falls steeply with energy:<br />
angular resolution and energy resolution will therefore play a critical role in determining<br />
the detector’s ability to find point sources of neutrinos above this background. Electron<br />
and tau flavor neutrinos can also be detected via the Čerenkov photons produced from the<br />
electromagnetic and hadronic showers from neutrino interactions inside or near the detector.<br />
The pointing accuracy and event rates for these events will be significantly less favourable<br />
than for muon events but the energy resolution should be better.<br />
ANTARES is currently in an R&D phase where the technology for constructing a largearea<br />
neutrino detector in the mediterranean sea is being developed through deployments at<br />
a test site which is 30 km from the French coast near Toulon and at a depth of 2300 m.<br />
In 1998 a first prototype string will be deployed and data from 8 PMTs transmitted to<br />
shore by a 40 km long electro-optical cable which is ready to be laid in place by France<br />
Telecom. By the end of 1999 one or two fully-equipped strings and up to 100 PMTs will be<br />
deployed in an array that will be directly scalable to the large-area detector. Great emphasis<br />
is being placed on developing a reliable and cost-effective deployment strategy by using well<br />
established commercial technology from companies such as France Telecom and by involving<br />
two Oceanographics institutes (IFREMER and Centre d’Oceanologie de Marseille) directly<br />
in the collaboration. These two institutes have many years experience of deploying scientific<br />
instruments at depths relevant to ANTARES.<br />
In parallel with these activities, ANTARES has already started deploying autonomous