Long-term effectiveness and consequences of carbon dioxide sequestration

被引:0
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作者
Shaffer G. [1 ,2 ,3 ]
机构
[1] Department of Geophysics, University of Concepcion, Concepcion 3
[2] Niels Bohr Institute, University of Copenhagen, 2100 Copenhagen Ø
[3] Danish Center for Earth System Science, 3050 Humlebæk
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D O I
10.1038/ngeo896
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摘要
One proposal for the mitigation of ongoing global warming is the sequestration of carbon dioxide extracted at combustion sites or directly from the air. Such sequestration could help avoid a large rise in atmospheric CO 2 concentration from unchecked use of fossil fuels, and hence extreme warming in the near future. However, it is not clear how effective different types of sequestration and associated leakage are in the long term, and what their consequences might be. Here I present projections over 100,000 years for five scenarios of carbon sequestration and leakage with an Earth system model. Most of the investigated scenarios result in a large, delayed warming in the atmosphere as well as oxygen depletion, acidification and elevated CO 2 concentrations in the ocean. Specifically, deep-ocean carbon storage leads to extreme acidification and CO2 concentrations in the deep ocean, together with a return to the adverse conditions of a business-as-usual projection with no sequestration over several thousand years. Geological storage may be more effective in delaying the return to the conditions of a business-as-usual projection, especially for storage in offshore sediments. However, leakage of 1% or less per thousand years from an underground stored reservoir, or continuous resequestration far into the future, would be required to maintain conditions close to those of a low-emission projection with no sequestration. © 2010 Macmillan Publishers Limited. All rights reserved.
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页码:464 / 467
页数:3
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