Role of CH(4) oxidation, production and transport in forest soil CH(4) flux

MA Bradford; P Ineson; PA Wookey; HM Lappin-Scott

doi:10.1016/S0038-0717(01)00078-5

Role of CH(4) oxidation, production and transport in forest soil CH(4) flux

MA Bradford^*, P Ineson, PA Wookey, HM Lappin-Scott

^*Corresponding author for this work

Research output: Contribution to journal › Article › peer-review

41 Citations (Scopus)

Abstract

Forest soils are an important sink for atmospheric CH(4) but the contribution of CH(4) oxidation, production and transport to the overall CH(4) flux is difficult to quantify. It is important to understand the role these processes play in CH(4) dynamics of forest soils, to enable prediction of how the size of this sink will respond to future environmental change. Methane oxidation, production and transport were investigated for a temperate forest soil, previously shown to be a net CH(4) consumer, to determine the extent to which physical and biological processes contributed to the not flux. The sum of oxidation rates for soil layers were significantly greater (P

Original language	English
Pages (from-to)	1625-1631
Number of pages	7
Journal	Soil Biology and Biochemistry
Volume	33
Issue number	12-13
DOIs	https://doi.org/10.1016/S0038-0717(01)00078-5
Publication status	Published - Oct 2001

Keywords

methane oxidation
methane consumption
forest soil
methane transport
kinetics
METHANE OXIDATION
TEMPERATE FOREST
ATMOSPHERIC METHANE
NITROGEN
CONSUMPTION
KINETICS
DEPOSITION
SAMPLES
WATER
PEAT

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Cite this

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title = "Role of CH(4) oxidation, production and transport in forest soil CH(4) flux",

abstract = "Forest soils are an important sink for atmospheric CH(4) but the contribution of CH(4) oxidation, production and transport to the overall CH(4) flux is difficult to quantify. It is important to understand the role these processes play in CH(4) dynamics of forest soils, to enable prediction of how the size of this sink will respond to future environmental change. Methane oxidation, production and transport were investigated for a temperate forest soil, previously shown to be a net CH(4) consumer, to determine the extent to which physical and biological processes contributed to the not flux. The sum of oxidation rates for soil layers were significantly greater (P",

keywords = "methane oxidation, methane consumption, forest soil, methane transport, kinetics, METHANE OXIDATION, TEMPERATE FOREST, ATMOSPHERIC METHANE, NITROGEN, CONSUMPTION, KINETICS, DEPOSITION, SAMPLES, WATER, PEAT",

author = "MA Bradford and P Ineson and PA Wookey and HM Lappin-Scott",

year = "2001",

month = oct,

doi = "10.1016/S0038-0717(01)00078-5",

language = "English",

volume = "33",

pages = "1625--1631",

journal = "Soil Biology and Biochemistry",

issn = "0038-0717",

publisher = "Elsevier",

number = "12-13",

}

TY - JOUR

T1 - Role of CH(4) oxidation, production and transport in forest soil CH(4) flux

AU - Bradford, MA

AU - Ineson, P

AU - Wookey, PA

AU - Lappin-Scott, HM

PY - 2001/10

Y1 - 2001/10

N2 - Forest soils are an important sink for atmospheric CH(4) but the contribution of CH(4) oxidation, production and transport to the overall CH(4) flux is difficult to quantify. It is important to understand the role these processes play in CH(4) dynamics of forest soils, to enable prediction of how the size of this sink will respond to future environmental change. Methane oxidation, production and transport were investigated for a temperate forest soil, previously shown to be a net CH(4) consumer, to determine the extent to which physical and biological processes contributed to the not flux. The sum of oxidation rates for soil layers were significantly greater (P

AB - Forest soils are an important sink for atmospheric CH(4) but the contribution of CH(4) oxidation, production and transport to the overall CH(4) flux is difficult to quantify. It is important to understand the role these processes play in CH(4) dynamics of forest soils, to enable prediction of how the size of this sink will respond to future environmental change. Methane oxidation, production and transport were investigated for a temperate forest soil, previously shown to be a net CH(4) consumer, to determine the extent to which physical and biological processes contributed to the not flux. The sum of oxidation rates for soil layers were significantly greater (P

KW - methane oxidation

KW - methane consumption

KW - forest soil

KW - methane transport

KW - kinetics

KW - METHANE OXIDATION

KW - TEMPERATE FOREST

KW - ATMOSPHERIC METHANE

KW - NITROGEN

KW - CONSUMPTION

KW - KINETICS

KW - DEPOSITION

KW - SAMPLES

KW - WATER

KW - PEAT

U2 - 10.1016/S0038-0717(01)00078-5

DO - 10.1016/S0038-0717(01)00078-5

M3 - Article

SN - 0038-0717

VL - 33

SP - 1625

EP - 1631

JO - Soil Biology and Biochemistry

JF - Soil Biology and Biochemistry

IS - 12-13

ER -

Role of CH(4) oxidation, production and transport in forest soil CH(4) flux

Abstract

Keywords

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