150 likes | 274 Views
Comparison of OM Responses at Different Sites. Zh.-A. Dzhilkibaev, A. Gazizov and Ch. Spiering. N = N + N. g. m. d. Response of OM to Muon Tracks. Uniform track. N – muon’s light. m. d. N – -el. light (8% N ). d. m. Sites. Lake Baikal (BAIKAL)
E N D
Comparison of OM Responses at Different Sites Zh.-A. Dzhilkibaev, A. Gazizov and Ch. Spiering
N = N + N g m d Response of OM to Muon Tracks Uniformtrack N – muon’s light m d N – -el. light (8% N ) d m Sites Lake Baikal (BAIKAL) Mediterranean (ANTARES) Antarctic ice (AMANDA)
Optical Parameters Light wave-length: 350 nm – 600 nm BAIKALAMANDAANTARES Absorption - Scattering - Scattering Function - Inverse light velocity, ns/m - ~20 m ~100 m ~60 m 30–50 m ~3 m 50-70 m 0.85-0.9 0.9-0.95 ~0.85 4.68-4.5 4.59-4.44 4.73-4.55
absorption scattering
Time differences (350 nm – 600 nm) Refraction index
Characteristics of OM angular sensitivity quantum efficiency
Influence of light velocity and absorption on OM time response (without scattering)
FWHM of the time distribution (without scattering)
Time distributions BAIKAL AMANDA ANTARES r = 10 m r = 10 m r = 25 m r = 25 m
Integral time distributions N(<t) r=10 m, cos(q)=-1 r=25 m, cos(q)=-1 r=60 m, cos(q)=-1
r=10 m, cos(q)=1 r=25 m, cos(q)=1 r=60 m, cos(q)=1