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  • methane emission  (4)
  • AGE; AWI Arctic Land Expedition; Barium 2+; Bicarbonate ion; Bromide; CA-Land_2009_YukonLakes; Calcium; Chloride; Conductivity, electrical; DEPTH, sediment/rock; Iron; Lithologic unit/sequence; Magnesium; Manganese; Nitrate; PCUWI; PG1967; pH; Piston corer, UWITEC; Potassium; Sodium; Strontium 2+; Sulfate; Yukon_Lakes_2009  (1)
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  • 1
    Electronic Resource
    Electronic Resource
    Springer
    Plant and soil 202 (1998), S. 27-32 
    ISSN: 1573-5036
    Keywords: gas transport ; methane emission ; methane oxidation ; peatland
    Source: Springer Online Journal Archives 1860-2000
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
    Notes: Abstract The importance of plant-mediated CH4 transport was studied in a northern wetland. CH4 transport through Eriophorum, a dominant sedge, was found to be the major pathway for CH4 fluxes. Mean emission from Sphagnum lawns was low (34 μg CH4 m-2 h-1) and significantly higher from tussocks of Eriophorum vaginatum (974 μg CH4 m-2 h-1; U-test, p 〈 0.05). Mean flux from single tillers of Eriophorum angustifolium was 92 μg CH4 h-1. In contrast to other ecosystems, no CH4 oxidation was associated with Eriophorum. Hence, the lack of oxidation is one reason for the high emission rates from these ecosystems. This finding is a caveat for models of CH4 emission and may also have consequences for carbon flow models of northern wetlands.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 41 (1998), S. 199-214 
    ISSN: 1573-515X
    Keywords: methane balance ; methane emission ; methane oxidation ; methane production ; paddy soil
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract In rice microcosms (Oryza sativa, var. Roma, type japonica),CH4 emission, CH4 production, CH4oxidation and CH4 accumulation were measured over an entirevegetation period. Diffusive CH4 emission was measured inclosed chambers, CH4 production was measured in soil samples,CH4 oxidation was determined from the difference between oxicand anoxic emissions, and CH4 accumulation was measured byanalysis of porewater and gas bubbles. The sum of diffusiveCH4 emission, CH4 oxidation, andCH4 accumulation was only 60% of the cumulativeCH4 production. The two values diverged during the first 50days (vegetative phase) and then again during the last 50 days (latereproductive phase and senescence) of the 150 day vegetation period. Duringthe period of day 50–100 (early reproductive phase/flowering), theprocesses were balanced. Most likely, gas bubbles and diffusion limitationare responsible for the divergence in the early and late phases. The effectof rice on CH4 production rates and CH4concentrations was studied by measuring these processes also in unplantedmicrocosms. Presence of rice plants lowered the CH4concentrations, but had no net effect on the CH4 productionrates.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 51 (2000), S. 91-112 
    ISSN: 1573-515X
    Keywords: bog ; methane emission ; methane oxidation ; microtopography
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The aim of this study was to correlate magnitude andcontrols of CH4 fluxes with the microtopographyand the vegetation in a hollow-ridge complex of araised bog. High CH4 emission rates were measuredfrom hollows and mud-bottom hollows, while hummocksconsumed atmospheric CH4 at a low rate. Thehighest emissions were measured from plots with Eriophorum vaginatum and Scheuchzeriapalustris. CH4 emission ceased after Scheuchzeria had been clipped below the water table,indicating the importance of this aerenchymatic plantas a conduit for CH4. Peat in the upper catotelm of hollows was younger andless decomposed than in hummocks. Potential CH4production in vitro was higher and themethanogenic association was better adapted to highertemperatures in hollow than in hummock peat. Highertemperatures in hollows resulted in a strongerCH4 source in hollows than in hummocks. Negativefluxes from hummocks indicated that even in wetlandsmethanotrophic bacteria exist that are able to oxidizeCH4 at atmospheric mixing ratios, and thatoxidation controls CH4 emission completely. TheCH4 mixing ratio was low in the acrotelm, but itincreased within the catotelm. Comparing fluxesmeasured in static chambers with fluxes calculatedfrom the porewater CH4 profiles it was deducedthat the zone of methane oxidation was located closeto the water table. In hollows, CH4 production at in situtemperature was far higher than emission into theatmosphere, corresponding to an oxidation rate ofnearly 99%. The CH4 flux between the catotelmand the acrotelm of hollows was also higher than theemission, indicating the importance of CH4oxidation in the aerobic acrotelm, too. CH4microprofiles showed that CH4 oxidation inmud-bottom hollows was confined to the topmost 2 mm,and that in Sphagnum-covered hollows CH4oxidation occurred at the lower edge of green Sphagnum-parts.
    Type of Medium: Electronic Resource
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  • 4
    ISSN: 1573-515X
    Keywords: fertiliser ; methane emission ; methane oxidation ; microcosm ; rice
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract The emission of the greenhouse gas CH4 from ricepaddies is strongly influenced by management practicessuch as the input of ammonium-based fertilisers. Weassessed the impact of different levels (200 and 400kgN.ha−1) of urea and (NH4)2HPO4on the microbial processes involved in production andconsumption of CH4 in rice field soil. We usedcompartmented microcosms which received fertilisertwice weekly. Potential CH4 production rates weresubstantially higher in the rice rhizosphere than inunrooted soil, but were not affected by fertilisation.However, CH4 emission was reduced by the additionof fertiliser and was negatively correlated with porewater NH 4 plus concentration, probably as theconsequence of elevated CH4 oxidation due tofertilisation. CH4 oxidation as well as numbersof methanotrophs was distinctly stimulated by theaddition of fertiliser and by the presence of the riceplant. Without fertiliser addition,nitrogen-limitation of the methanotrophs will restrictthe consumption of CH4. This may have a majorimpact on the global CH4 budget, asnitrogen-limiting conditions will be the normalsituation in the rice rhizosphere. Elevated potentialnitrifying activities and numbers were only detectedin microcosms fertilised with urea. However, asubstantial part of the nitrification potential in therhizosphere of rice was attributed to the activity ofmethanotrophs, as was demonstrated using theinhibitors CH3F and C2H2.
    Type of Medium: Electronic Resource
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  • 5
    Publication Date: 2023-06-27
    Keywords: AGE; AWI Arctic Land Expedition; Barium 2+; Bicarbonate ion; Bromide; CA-Land_2009_YukonLakes; Calcium; Chloride; Conductivity, electrical; DEPTH, sediment/rock; Iron; Lithologic unit/sequence; Magnesium; Manganese; Nitrate; PCUWI; PG1967; pH; Piston corer, UWITEC; Potassium; Sodium; Strontium 2+; Sulfate; Yukon_Lakes_2009
    Type: Dataset
    Format: text/tab-separated-values, 714 data points
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