Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming
Abstract
Air temperatures are rising and the winter snowpack is getting thinner in many high-latitude and high-elevation ecosystems around the globe. Past studies show that soil warming accelerates microbial metabolism and stimulates soil carbon (C) and nitrogen (N) cycling. Conversely, winter snow removal to simulate loss of snow cover leads to increased soil freezing and reductions in soil microbial biomass, exoenzyme activity, and N cycling. The Climate Change Across Seasons Experiment (CCASE), located at Hubbard Brook Experimental Forest, NH (USA) is designed to evaluate the combined effects of growing season soil warming and an increased frequency of winter soil freeze-thaw cycles on a northern forest ecosystem. Soils were collected from CCASE over two years (2014 and 2015) and extractable C and N pool sizes, as well as microbial biomass, exoenzymes, and potential net N mineralization and microbial respiration were measured. Soil warming alone did not stimulate microbial activity at any sampling time. Extractable amino acid N and organic C, proteolytic and acid phosphatase activity, and microbial respiration were reduced by the combination of warming in the growing season and winter soil freeze-thaw cycles during the period following snowmelt through tree leaf out in spring. The declines in microbial activity also coincidedmore »
- Authors:
-
- Boston University, MA (United States); Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Boston University, MA (United States)
- Publication Date:
- Research Org.:
- Lawrence Berkeley National Laboratory (LBNL), Berkeley, CA (United States)
- Sponsoring Org.:
- USDOE Office of Science (SC); National Science Foundation (NSF)
- OSTI Identifier:
- 1476593
- Grant/Contract Number:
- AC02-05CH11231; DEB1149929; DEB 140621; 1114804; 1637685
- Resource Type:
- Accepted Manuscript
- Journal Name:
- Soil Biology and Biochemistry
- Additional Journal Information:
- Journal Volume: 116; Journal Issue: C; Journal ID: ISSN 0038-0717
- Publisher:
- Elsevier
- Country of Publication:
- United States
- Language:
- English
- Subject:
- 54 ENVIRONMENTAL SCIENCES; soil freeze-thaw cycle; exoenzymes; Hubbard brook experimental forest; soil warming; microbial biomass
Citation Formats
Sorensen, Patrick O., Finzi, Adrien C., Giasson, Marc-André, Reinmann, Andrew B., Sanders-DeMott, Rebecca, and Templer, Pamela H. Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming. United States: N. p., 2017.
Web. doi:10.1016/j.soilbio.2017.09.026.
Sorensen, Patrick O., Finzi, Adrien C., Giasson, Marc-André, Reinmann, Andrew B., Sanders-DeMott, Rebecca, & Templer, Pamela H. Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming. United States. https://doi.org/10.1016/j.soilbio.2017.09.026
Sorensen, Patrick O., Finzi, Adrien C., Giasson, Marc-André, Reinmann, Andrew B., Sanders-DeMott, Rebecca, and Templer, Pamela H. Tue .
"Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming". United States. https://doi.org/10.1016/j.soilbio.2017.09.026. https://www.osti.gov/servlets/purl/1476593.
@article{osti_1476593,
title = {Winter soil freeze-thaw cycles lead to reductions in soil microbial biomass and activity not compensated for by soil warming},
author = {Sorensen, Patrick O. and Finzi, Adrien C. and Giasson, Marc-André and Reinmann, Andrew B. and Sanders-DeMott, Rebecca and Templer, Pamela H.},
abstractNote = {Air temperatures are rising and the winter snowpack is getting thinner in many high-latitude and high-elevation ecosystems around the globe. Past studies show that soil warming accelerates microbial metabolism and stimulates soil carbon (C) and nitrogen (N) cycling. Conversely, winter snow removal to simulate loss of snow cover leads to increased soil freezing and reductions in soil microbial biomass, exoenzyme activity, and N cycling. The Climate Change Across Seasons Experiment (CCASE), located at Hubbard Brook Experimental Forest, NH (USA) is designed to evaluate the combined effects of growing season soil warming and an increased frequency of winter soil freeze-thaw cycles on a northern forest ecosystem. Soils were collected from CCASE over two years (2014 and 2015) and extractable C and N pool sizes, as well as microbial biomass, exoenzymes, and potential net N mineralization and microbial respiration were measured. Soil warming alone did not stimulate microbial activity at any sampling time. Extractable amino acid N and organic C, proteolytic and acid phosphatase activity, and microbial respiration were reduced by the combination of warming in the growing season and winter soil freeze-thaw cycles during the period following snowmelt through tree leaf out in spring. The declines in microbial activity also coincided with an 85% decline in microbial biomass N at that time. Growing season warming and winter soil freeze-thaw cycles also resulted in a two-fold reduction in phenol oxidase activity and a 20% reduction in peroxidase activity and these declines persisted throughout the snow-free time of the year. Finally, the results from this study suggest that positive feedbacks between warming and rates of soil C and N cycling over the next 100 years will be partially mitigated by an increased frequency of winter soil freeze-thaw cycles, which decrease microbial biomass and rates of soil microbial activity.},
doi = {10.1016/j.soilbio.2017.09.026},
journal = {Soil Biology and Biochemistry},
number = C,
volume = 116,
place = {United States},
year = {Tue Oct 10 00:00:00 EDT 2017},
month = {Tue Oct 10 00:00:00 EDT 2017}
}
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