dc.contributor.advisor |
Milodowski, Antoni |
|
dc.contributor.advisor |
Kirk, Guy |
|
dc.contributor.advisor |
Ritz, K. |
|
dc.contributor.author |
Versteegen, Audrey |
|
dc.date.accessioned |
2011-05-17T09:30:59Z |
|
dc.date.available |
2011-05-17T09:30:59Z |
|
dc.date.issued |
2010 |
|
dc.identifier.uri |
http://dspace.lib.cranfield.ac.uk/handle/1826/5332 |
|
dc.description.abstract |
Over half of the carbon (C) taking part in the global C cycle is held in terrestrial systems.
Because of the sensitivity of the C cycle to changes in such soil-based pools of carbon, it is
important to understand the basic mechanisms by which soil C is stored and cycled between the
range of di erent pools which occur belowground. In the context of climate change mitigation,
it is considered that increasing soil-based stocks of C, either by reducing losses from soils, or by
actively sequestering new carbon, is a potentially important strategy . Organic carbon is the
main form of carbon in soil and as such has received most focus. Cont/d. |
en_UK |
dc.language.iso |
en |
en_UK |
dc.publisher |
Cranfield University |
en_UK |
dc.rights |
© Cranfield University, 2010. All rights reserved. No part of this publication may be reproduced
without the written permission of the copyright holder |
en_UK |
dc.title |
Biotic and Abiotic Controls on Calcium Carbonate Formation in Soils |
en_UK |
dc.type |
Thesis or dissertation |
en_UK |
dc.type.qualificationlevel |
Doctoral |
en_UK |
dc.type.qualificationname |
PhD |
en_UK |
dc.description.notes |
Milodowski, Antoni (supervisor British Geological Survey) |
|