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Details of Award

NERC Reference : NER/B/S/2003/00762

Chemical variations in accreted ice from Lake Vostok: artefacts of sample processing or evidence of volume change?

Grant Award

Principal Investigator:
Professor M Tranter, University of Bristol, Geographical Sciences
Co-Investigator:
Professor MJ Siegert, Imperial College London, Grantham Institute for Climate Change
Science Area:
Terrestrial
Freshwater
Earth
Overall Classification:
Freshwater
ENRIs:
Global Change
Environmental Risks and Hazards
Biodiversity
Science Topics:
Water Quality
Earth Surface Processes
Biogeochemical Cycles
Quaternary Science
Abstract:
Ice at the bottom of the Vostok ice core originates from waters of Lake Vostok, the largest of the many lakes beneath the Antarctic ice sheet. The chemical composition of this bottom ice is variable, suggesting that Lake Vostok too has had a variable chemical composition in the past. The most likely explanation for this observation is that the Lake has expanded and contracted as the Antarctic Ice Sheet grows and contracts over cycles of glaciation. However, small particles found in the bottom ice may interact with the ice during laboratory procedures. The project first assesses how much of the chemical variation is due to interactions with these particles, then examines the likely glaciological reasons for any chemical variation that cannot be explained otherwise.
Period of Award:
1 Mar 2004 - 31 Aug 2006
Value:
£20,237
Authorised funds only
NERC Reference:
NER/B/S/2003/00762
Grant Stage:
Completed
Scheme:
Small Grants Pre FEC
Grant Status:
Closed
Programme:
Small Grants

This grant award has a total value of £20,237  

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FDAB - Financial Details (Award breakdown by headings)

Total - T&STotal - Other Costs
£11,727£8,510

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