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DOI10.1126/science.aao0457
Response to comment on "the whole-soil carbon flux in response to warming"
Pries C.E.H.; Castanha C.; Porras R.; Phillips C.; Torn M.S.
发表日期2018
ISSN0036-8075
卷号359期号:6378
英文摘要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 prof ile, indicating that all soil depths responded to warming. © The Authors.
英文关键词carbon dioxide; climate change; heat transfer; microbial community; priority journal; Review; soil; soil analysis; soil depth; soil temperature; thermal diffusion; warming
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/245136
作者单位Climate Sciences Department, Climate and Ecosystem Sciences Division, Lawrence Berkeley National Laboratory, MS 74R316C, Berkeley, CA 94720, United States; Biological Sciences Department, Dartmouth College, Hanover, NH 03755, United States; Department of Crops and Soil Science, Oregon State University, Corvallis, OR 97331, United States
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Pries C.E.H.,Castanha C.,Porras R.,et al. Response to comment on "the whole-soil carbon flux in response to warming"[J],2018,359(6378).
APA Pries C.E.H.,Castanha C.,Porras R.,Phillips C.,&Torn M.S..(2018).Response to comment on "the whole-soil carbon flux in response to warming".Science,359(6378).
MLA Pries C.E.H.,et al."Response to comment on "the whole-soil carbon flux in response to warming"".Science 359.6378(2018).
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