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DOI | 10.1126/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 |
ISSN | 0036-8075 |
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
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/245784 |
推荐引用方式 GB/T 7714 | 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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