OPTICAL-PROPERTIES OF THE SOUTH-POLE ICE AT DEPTHS BETWEEN 0.8 AND 1 KILOMETER

被引:50
作者
ASKEBJER, P
BARWICK, SW
BERGSTROM, L
BOUCHTA, A
CARIUS, S
COULTHARD, A
ENGEL, K
ERLANDSSON, B
GOOBAR, A
GRAY, L
HALLGREN, A
HALZEN, F
HULTH, PO
JACOBSEN, J
JOHANSSON, S
KANDHADAI, V
LIUBARSKY, I
LOWDER, D
MILLER, T
MOCK, PC
MORSE, R
PORRATA, R
PRICE, PB
RICHARDS, A
RUBINSTEIN, H
SCHNEIDER, E
SUN, Q
TILAV, S
WALCK, G
YODH, G
机构
[1] UNIV STOCKHOLM, S-11385 STOCKHOLM, SWEDEN
[2] UNIV CALIF IRVINE, IRVINE, CA 92717 USA
[3] UNIV UPPSALA, S-75121 UPPSALA, SWEDEN
[4] UNIV WISCONSIN, MADISON, WI 53706 USA
[5] UNIV CALIF BERKELEY, BERKELEY, CA 94720 USA
关键词
D O I
10.1126/science.267.5201.1147
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
The optical properties of the ice at the geographical South Pole have been investigated at depths between 0.8 and 1 kilometer. The absorption and scattering lengths of visible light (similar to 515 nanometers) have been measured in situ with the use of the laser calibration setup of the Antarctic Muon and Neutrino Detector Array (AMANDA) neutrino detector. The ice is intrinsically extremely transparent. The measured absorption length is 59 +/- 3 meters, comparable with the quality of the ultrapure water used in the Irvine-Michigan-Brookhaven and Kamiokande prolon-decay and neutrino experiments and more than twice as long as the best value reported for laboratory ice. Because of a residual density of air bubbles at these depths, the trajectories of photons in the medium are randomized. If the bubbles are assumed to be smooth and spherical, the average distance between collisions at a depth of 1 kilometer is about 25 centimeters. The measured inverse scattering length on bubbles decreases linearly with increasing depth in the volume of ice investigated.
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页码:1147 / 1150
页数:4
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