Soil respiration contributes substantially to urban carbon fluxes in the greater Boston area
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- 作者：Stephen M. Decinaa ; sdecina@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Lucy R. Hutyrab ; lrhutyra@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Conor K. Gatelyb ; gately@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Jackie M. Getsonb ; getsonj@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Andrew B. Reinmannb ; reinmann@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Anne G. Short Gianottib ; agshort@bu.edu" class="auth_mail" title="E-mail the corresponding author ; Pamela H. Templera ; ptempler@bu.edu" class="auth_mail" title="E-mail the corresponding author
- 关键词：Urban ecology ; Biogeochemistry ; Fossil fuels ; CO2 flux
- 刊名：Environmental Pollution
- 出版年：2016
- 出版时间：May 2016
- 年：2016
- 卷：212
- 期：Complete
- 页码：433-439
- 全文大小：1750 K
文摘
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Growing season soil respiration produces a significant amount of urban CO2.
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Soil CO2 efflux is spatially and temporally variable across urban areas.
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Areas with high pervious residential land cover are dominant areas of soil CO2 efflux.
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Soil amendments by homeowners may be responsible for high urban soil CO2 efflux.
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Assessing and attributing urban CO2 fluxes requires quantifying biological CO2 efflux.