Proton Magnetic Resonance Spectrum of Polywater
- 9 January 1970
- journal article
- other
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 167 (3915), 171
- https://doi.org/10.1126/science.167.3915.171-a
Abstract
Fresh ice stalactites were observed beneath sea ice in Antarctica. They are hollow, tapering, inverted cones having a base diameter between 10 and 20 centimeters and a tip diameter of 4 to 10 centimeters extending downward about 100 centimeters. The stalactites form when dense, chilled brine drains downward from the ice sheet into seawater of norma1 salinity and near-freezing temperature.Keywords
This publication has 2 references indexed in Scilit:
- PolywaterScience, 1969
- “Anomalous” WaterNature, 1969