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Dissolved gases in the bottom of liquid lakes of the McMurdo oasis area
Entry ID: K094_1991_1992_NZ_1

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Summary
Abstract: The lakes in the McMurdo Dry Valleys have a density gradient which in turn prevents the usual vertical convection seen in other lakes. Consequently the basal layers of the lakes remain stagnant. Crustal gases permeate through the permafrost into the deep layers of the lake where they become trapped, and the hydrostatic pressure increases the solubility of these gases. By sampling these layers it ... View entire text
Geographic Coverage
Spatial coordinates   
  N: -77.52   S: -77.52   E: 161.67   W: 161.67
Max Depth: 70

Temporal Coverage
Start Date: 1991-11-25
Stop Date: 1991-12-09
ISO Topic Category
Data Set Progress
COMPLETE
Originating Center
Data Center
Antarctica New Zealand, New Zealand Antarctic Institute, New Zealand Supplemental Info
Data Center URL: http://www.antarcticanz.govt.nz/

Data Center Personnel
Name: SHULAMIT GORDON
Phone: +64 3 358 0200
Fax: +64 3 358 0211
Email: s.gordon at antarcticanz.govt.nz
Contact Address:
Antarctica New Zealand
Private Bag 4745
City: Christchurch
Country: New Zealand
Personnel
Role: INVESTIGATOR
Phone: +64 9 373 7599 Extn 87374
Email: j.webster at auckland.ac.nz
Contact Address:
Department of Chemistry
University of Auckland
Private Bag 92019
City: Auckland
Country: New Zealand
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Publications/References
Brown, K.L., Webster, J.G., Giggenbach, W.F. and Lyon, G.L. 1991. A note on gases dissolved in the deep waters of Lake Vanda. New Zealand Antarctic Record 11(1): 14-18.
Extended Metadata Properties
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Creation and Review Dates
DIF Creation Date: 2005-11-01
Last DIF Revision Date: 2009-03-27

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