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DOI10.1126/science.272.5260.393
Rapid exchange between soil carbon and atmospheric carbon dioxide driven by temperature change
Trumbore S.E.; Chadwick O.A.; Amundson R.
发表日期1996
ISSN0036-8075
起始页码393
结束页码396
卷号272期号:5260
英文摘要Comparison of 14C (carbon-14) in archived (pre-1963) and contemporary soils taken along an elevation gradient in the Sierra Nevada, California, demonstrates rapid (7 to 65 years) turnover for 50 to 90 percent of carbon in the upper 20 centimeters of soil (A horizon soil carbon). Carbon turnover times increased with elevation (decreasing temperature) along the Sierra transect. This trend was consistent with results from other locations, which indicates that temperature is a dominant control of soil carbon dynamics. When extrapolated to large regions, the observed relation between carbon turnover and temperature suggests that soils should act as significant sources or sinks of atmospheric carbon dioxide in response to global temperature changes.
英文关键词carbon cycle; carbon dioxide; decomposition rate; resident time; soil organic matter; temperature; USA, California, Sierra Nevada
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/245784
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Trumbore S.E.,Chadwick O.A.,Amundson R.. Rapid exchange between soil carbon and atmospheric carbon dioxide driven by temperature change[J],1996,272(5260).
APA Trumbore S.E.,Chadwick O.A.,&Amundson R..(1996).Rapid exchange between soil carbon and atmospheric carbon dioxide driven by temperature change.Science,272(5260).
MLA Trumbore S.E.,et al."Rapid exchange between soil carbon and atmospheric carbon dioxide driven by temperature change".Science 272.5260(1996).
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