二氧化碳生物地球化学循环研究的进展

doi:10.11867/j.issn.1001-8166.1995.04.0367

综述了对二氧化碳生物地球化学循环的研究现状，着重介绍了大气二氧化碳的源和汇的研究资料，并简要介绍了有关碳循环模式。

关键词: 碳循环, 大气二氧化碳, 海洋二氧化碳, 碳循环模式

A large amount of carbon dioxide is released into the atmosphere by human activities, one part of which remains in the atmosphere and the other is taken up by the other carbon reservoirs on the Earth. The oceans are a significant sink of atmospheric carbon dioxide. Because of lack of temporal and spatial variations of observed data, there is some controversy over the exact figure. Research on oceanic carbon cycle often uses models, either one-dimensional box models or three-dimensional circulation models. As some parameters for some physical and biochemical processes of carbon dioxide in the oceans are not clearly known, for example, exchange coefficient of CO₂ vertical eddy diffusivity, the role of biological web, etc., the obtained results still have large uncertainties. The interaction of CO₂between the atmosphere and terrestrial ecosystems is not sufficiently known. According to the current data and oceanic carbon cycle model, a missing sink is often attributed to the terrestrial biosphere. The so called CO₂ fertilization effect is currenly a major hypothesis. Another possible fate of missing sink is soil.

Key words: Carboncycle, Atmospheric CO₂, Oceanic CO₂, Terrestrial biosphere.

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摘要

ON THE STUDY OF THEBIOGEOCHEMICAL CYCLE OF CARBON DIOXIDE