Response to Comment on “The whole-soil carbon flux in response to warming”
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States); Dartmouth College, Hanover, NH (United States)
- Lawrence Berkeley National Lab. (LBNL), Berkeley, CA (United States)
- Oregon State Univ., Corvallis, OR (United States)
Temperature records and model predictions demonstrate that deep soils warm at the same rate as surface soils, contrary to Xiao et al.'s assertions. In response to Xiao et al.'s critique of our Q10 analysis, we present the results with all data points included, which show Q10 values of > 2 throughout the soil profile, indicating that all soil depths responded to warming.
- Research Organization:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Organization:
- USDOE Office of Science (SC)
- Grant/Contract Number:
- AC02-05CH11231
- OSTI ID:
- 1567116
- Journal Information:
- Science, Vol. 359, Issue 6378; ISSN 0036-8075
- Publisher:
- AAASCopyright Statement
- Country of Publication:
- United States
- Language:
- English
Sugarcane straw management for bioenergy: effects of global warming on greenhouse gas emissions and soil carbon storage
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journal | July 2019 |
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Comment on “The whole-soil carbon flux in response to warming”
The whole-soil carbon flux in response to warming
Chemistry data from soils and soil incubation experiments from the whole-soil warming experiment at Blodgett Forest, CA, 2018, from: “Metabolic capabilities mute positive response to direct and indirect impacts of warming throughout the soil profile”
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OSTI ID:1479388
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The whole-soil carbon flux in response to warming
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2017
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Chemistry data from soils and soil incubation experiments from the whole-soil warming experiment at Blodgett Forest, CA, 2018, from: “Metabolic capabilities mute positive response to direct and indirect impacts of warming throughout the soil profile”
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2022
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OSTI ID:1866269
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