2001
DOI: 10.2307/2680063
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Effects of Temperature, and Nitrogen and Sulfur Deposition, on Methane Emission from a Boreal Mire

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Cited by 63 publications
(133 citation statements)
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“…The linear r 2 and the nonlinear R 2 are neither appropriate measures of regression model correctness (often used for checking linearity) nor appropriate filter criteria for measurement performance (Granberg et al, 2001;Huber, 2004;Hibbert, 2005). The expressions (1−r 2 ) and (1−R 2 ) are measures of the unexplained variance normalized to the total variance.…”
Section: Discussionmentioning
confidence: 99%
“…The linear r 2 and the nonlinear R 2 are neither appropriate measures of regression model correctness (often used for checking linearity) nor appropriate filter criteria for measurement performance (Granberg et al, 2001;Huber, 2004;Hibbert, 2005). The expressions (1−r 2 ) and (1−R 2 ) are measures of the unexplained variance normalized to the total variance.…”
Section: Discussionmentioning
confidence: 99%
“…Granberg et al (2001) evaluated CH 4 emissions from a fen in response to crossed treatments of elevated air temperature, nitrogen deposition, and sulfur deposition. They found that SO|~ additions depressed CH 4 emissions at ambient temperature, but not at elevated temperature.…”
Section: Wetland Methane Emissions Andmentioning
confidence: 99%
“…The authors were interested in possible effects of climate change on CH 4 emission, and they expected (and confirmed) sedges to be an important pathway for CH 4 release into the atmosphere. Similar to effects found in ombrotrophic bogs (see section 6.2), sedge cover was significantly increased with an increasing amount of nitrogen addition (Granberg et al, 2001). Unfortunately, the regression analysis used did not permit a distinction between effects found at 15 or at 30 kg N ha -1 yr -1 .…”
Section: Valley Mires Poor Fens and Transition Mires (D2)mentioning
confidence: 63%
“…When sedge cover was accounted for, the effect of nitrogen addition on CH 4 emission changed over the two years of addition from nonsignificant in the first year (1995) to a significant negative effect during the last year (1997). This cumulative effect was probably linked to the significant accumulation of total nitrogen in the upper 5 (15 kg N ha -1 yr -1 treatment) or 10 (30 kg N ha -1 yr -1 treatment) cm of the soil (Granberg et al, 2001). This accumulation corroborated the results found by Francez and Loiseau (1999), who added 5 kg N ha -1 yr -1 labelled with 15 N to a poor fen in Côte de Braveix, Central France (background deposition 10 kg N ha -1 yr -1 ).…”
Section: Valley Mires Poor Fens and Transition Mires (D2)mentioning
confidence: 99%
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