Methane production in laboratory incubations of Arctic soil at three temperatures, 2018
When wet Arctic tundra soils begin to freeze in the fall, an unfrozen layer remains between the frozen surface and deeper permafrost layers. This period is known as the zero curtain, as liquid water keeps the temperature of this soil layer near 0 Celsius (C) while latent heat is gradually dissipated...
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NSF Arctic Data Center
2021
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Online Access: | https://dx.doi.org/10.18739/a29882p2h https://arcticdata.io/catalog/view/doi:10.18739/A29882P2H |
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ftdatacite:10.18739/a29882p2h 2023-05-15T14:52:19+02:00 Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 Lipson, David 2021 text/xml https://dx.doi.org/10.18739/a29882p2h https://arcticdata.io/catalog/view/doi:10.18739/A29882P2H en eng NSF Arctic Data Center Q10 zero curtain methanogenesis tundra Dataset dataset 2021 ftdatacite https://doi.org/10.18739/a29882p2h 2022-04-01T18:11:40Z When wet Arctic tundra soils begin to freeze in the fall, an unfrozen layer remains between the frozen surface and deeper permafrost layers. This period is known as the zero curtain, as liquid water keeps the temperature of this soil layer near 0 Celsius (C) while latent heat is gradually dissipated. This experiment compares the temperature response of the methanogenic community in the zero curtain period with that of the summer community to test whether the zero curtain methanogenic community is especially cold adapted. This dataset includes methane production rates measured in anaerobic laboratory incubations of soils collected from two dates (July and Nov 2018) at temperatures around 0, 4 and 10C. Dataset Arctic permafrost Tundra DataCite Metadata Store (German National Library of Science and Technology) Arctic |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Q10 zero curtain methanogenesis tundra |
spellingShingle |
Q10 zero curtain methanogenesis tundra Lipson, David Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 |
topic_facet |
Q10 zero curtain methanogenesis tundra |
description |
When wet Arctic tundra soils begin to freeze in the fall, an unfrozen layer remains between the frozen surface and deeper permafrost layers. This period is known as the zero curtain, as liquid water keeps the temperature of this soil layer near 0 Celsius (C) while latent heat is gradually dissipated. This experiment compares the temperature response of the methanogenic community in the zero curtain period with that of the summer community to test whether the zero curtain methanogenic community is especially cold adapted. This dataset includes methane production rates measured in anaerobic laboratory incubations of soils collected from two dates (July and Nov 2018) at temperatures around 0, 4 and 10C. |
format |
Dataset |
author |
Lipson, David |
author_facet |
Lipson, David |
author_sort |
Lipson, David |
title |
Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 |
title_short |
Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 |
title_full |
Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 |
title_fullStr |
Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 |
title_full_unstemmed |
Methane production in laboratory incubations of Arctic soil at three temperatures, 2018 |
title_sort |
methane production in laboratory incubations of arctic soil at three temperatures, 2018 |
publisher |
NSF Arctic Data Center |
publishDate |
2021 |
url |
https://dx.doi.org/10.18739/a29882p2h https://arcticdata.io/catalog/view/doi:10.18739/A29882P2H |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic permafrost Tundra |
genre_facet |
Arctic permafrost Tundra |
op_doi |
https://doi.org/10.18739/a29882p2h |
_version_ |
1766323539548307456 |