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nd norbornadiene. 29. When a large excess of olefin is used, the equilibrium constant can be reduced to: K eq # (1 -- x)/(xC 0 ), where x # i c /i a for the 0/--1 couple from the CV, and C 0 is the concentration of the olefin. 30. J. W. Moore, R. G. Pearson, Kinetics and Mechanism (Wiley, New York,...
Main Authors: | , , , , , , , , , , , , , , , , , , |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.15.966 http://www.climate.unibe.ch/~blunier/Pdfs/Blunier01.pdf |
Summary: | nd norbornadiene. 29. When a large excess of olefin is used, the equilibrium constant can be reduced to: K eq # (1 -- x)/(xC 0 ), where x # i c /i a for the 0/--1 couple from the CV, and C 0 is the concentration of the olefin. 30. J. W. Moore, R. G. Pearson, Kinetics and Mechanism (Wiley, New York, ed. 3, 1981), p. 304. 31. We thank B. Cook, M. Matturro, J. Robbins, R. Espino, I. Horvath, J. McConnachie, C. Beswick, C. McConnachie, M. Greaney, R. Hall, J. Ou, M. Smith, and G. Stuntz for helpful discussions. 7 September 2000; accepted 21 November 2000 Timing of Millennial-Scale Climate Change in Antarctica and Greenland During the Last Glacial Period Thomas Blunier * and Edward J. Brook A precise relative chronology for Greenland and West Antarctic paleotemperature is extended to 90,000 years ago, based on correlation of atmospheric methane records from the Greenland Ice Sheet Project 2 and Byrd ice cores. Over this period, the onset of seven major millennial-scale warmi |
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