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Nitrous oxide consumption potentials of well-drained forest soils in Southern Québec, Canada.

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Nitrous oxide consumption potentials of well-drained forest soils in Southern Québec, Canada. / Frasier, Rebeccah; Ullah, Sami; Moore, Tim R.
In: Geomicrobiology Journal, Vol. 27, No. 1, 18.01.2010, p. 53-60.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

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Frasier R, Ullah S, Moore TR. Nitrous oxide consumption potentials of well-drained forest soils in Southern Québec, Canada. Geomicrobiology Journal. 2010 Jan 18;27(1):53-60. doi: 10.1080/01490450903232199

Author

Frasier, Rebeccah ; Ullah, Sami ; Moore, Tim R. / Nitrous oxide consumption potentials of well-drained forest soils in Southern Québec, Canada. In: Geomicrobiology Journal. 2010 ; Vol. 27, No. 1. pp. 53-60.

Bibtex

@article{7eea4bbeee6e47d8bba6a6c26f57a2c2,
title = "Nitrous oxide consumption potentials of well-drained forest soils in Southern Qu{\'e}bec, Canada.",
abstract = "To establish the major controls on N2O consumption by forest soils, we conducted laboratory incubations of 16 samples from four soil types, two organic and two mineral, varying in overlying forest vegetation (sugar maple, American beech and eastern hemlock). The fastest potential consumption of N2O occurred under anoxic conditionswith little soil nitrate and under elevated headspaceN2O concentration. Potential N2O consumption rates were fastest in organic soils under hemlock and beech trees (111 and 75 ng N2O-Ng−1 d−1, respectively) compared to mineral soils under beech and maple trees (45 and 41 ng N2O-N g−1 d−1). Organic soils showed faster N2O consumption rates than mineral soils, possibly due to larger organic C levels and higher C:N ratios. Acetylene treatment confirmed that denitrification was the process underlyingN2Oconsumption. These results suggest that soils regularly consume N2O with varying magnitude, most likely in anoxic microsites throughout the soil profile and that the potential for N2O consumption is larger in organic than in mineral forest soils.",
keywords = "denitrification, forest soils, nitrification, N cycling, N2O consumption, N2O fluxes, N2O production",
author = "Rebeccah Frasier and Sami Ullah and Moore, {Tim R.}",
note = "The final, definitive version of this article has been published in the Journal, Geomicrobiology Journal, 27 (1), 2010, {\textcopyright} Informa Plc",
year = "2010",
month = jan,
day = "18",
doi = "10.1080/01490450903232199",
language = "English",
volume = "27",
pages = "53--60",
journal = "Geomicrobiology Journal",
issn = "0149-0451",
publisher = "Taylor and Francis Ltd.",
number = "1",

}

RIS

TY - JOUR

T1 - Nitrous oxide consumption potentials of well-drained forest soils in Southern Québec, Canada.

AU - Frasier, Rebeccah

AU - Ullah, Sami

AU - Moore, Tim R.

N1 - The final, definitive version of this article has been published in the Journal, Geomicrobiology Journal, 27 (1), 2010, © Informa Plc

PY - 2010/1/18

Y1 - 2010/1/18

N2 - To establish the major controls on N2O consumption by forest soils, we conducted laboratory incubations of 16 samples from four soil types, two organic and two mineral, varying in overlying forest vegetation (sugar maple, American beech and eastern hemlock). The fastest potential consumption of N2O occurred under anoxic conditionswith little soil nitrate and under elevated headspaceN2O concentration. Potential N2O consumption rates were fastest in organic soils under hemlock and beech trees (111 and 75 ng N2O-Ng−1 d−1, respectively) compared to mineral soils under beech and maple trees (45 and 41 ng N2O-N g−1 d−1). Organic soils showed faster N2O consumption rates than mineral soils, possibly due to larger organic C levels and higher C:N ratios. Acetylene treatment confirmed that denitrification was the process underlyingN2Oconsumption. These results suggest that soils regularly consume N2O with varying magnitude, most likely in anoxic microsites throughout the soil profile and that the potential for N2O consumption is larger in organic than in mineral forest soils.

AB - To establish the major controls on N2O consumption by forest soils, we conducted laboratory incubations of 16 samples from four soil types, two organic and two mineral, varying in overlying forest vegetation (sugar maple, American beech and eastern hemlock). The fastest potential consumption of N2O occurred under anoxic conditionswith little soil nitrate and under elevated headspaceN2O concentration. Potential N2O consumption rates were fastest in organic soils under hemlock and beech trees (111 and 75 ng N2O-Ng−1 d−1, respectively) compared to mineral soils under beech and maple trees (45 and 41 ng N2O-N g−1 d−1). Organic soils showed faster N2O consumption rates than mineral soils, possibly due to larger organic C levels and higher C:N ratios. Acetylene treatment confirmed that denitrification was the process underlyingN2Oconsumption. These results suggest that soils regularly consume N2O with varying magnitude, most likely in anoxic microsites throughout the soil profile and that the potential for N2O consumption is larger in organic than in mineral forest soils.

KW - denitrification

KW - forest soils

KW - nitrification

KW - N cycling

KW - N2O consumption

KW - N2O fluxes

KW - N2O production

U2 - 10.1080/01490450903232199

DO - 10.1080/01490450903232199

M3 - Journal article

VL - 27

SP - 53

EP - 60

JO - Geomicrobiology Journal

JF - Geomicrobiology Journal

SN - 0149-0451

IS - 1

ER -