1999
DOI: 10.1007/bf00992874
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The fate of NH4NO3 added toSphagnum magettanicum carpets at five European mire sites

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Cited by 29 publications
(31 citation statements)
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“…Aerts et al (1992) concluded, based on the studies on the two Swedish sites discussed above, that high atmospheric nitrogen supply may affect the carbon balance of ombrotrophic bogs, because productivity under these circumstances is phosphorus, rather than nitrogen limited, but decomposition is probably increased by the high nitrogen loads. This hypothesis is supported by the results of the short-term experiments of Williams et al (1999a) and Williams and Silcock (2000) (for details, see above). The addition of 30 kg N ha -1 yr -1 resulted in a decrease in peat C:N ratios (Williams et al, 1999a), which could enhance rates of first-stage organic matter decomposition and nitrogen mineralization (Aerts et al, 1992).…”
Section: D) Effects On Peat and Peat Water Chemistry As Evidence Of Nsupporting
confidence: 78%
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“…Aerts et al (1992) concluded, based on the studies on the two Swedish sites discussed above, that high atmospheric nitrogen supply may affect the carbon balance of ombrotrophic bogs, because productivity under these circumstances is phosphorus, rather than nitrogen limited, but decomposition is probably increased by the high nitrogen loads. This hypothesis is supported by the results of the short-term experiments of Williams et al (1999a) and Williams and Silcock (2000) (for details, see above). The addition of 30 kg N ha -1 yr -1 resulted in a decrease in peat C:N ratios (Williams et al, 1999a), which could enhance rates of first-stage organic matter decomposition and nitrogen mineralization (Aerts et al, 1992).…”
Section: D) Effects On Peat and Peat Water Chemistry As Evidence Of Nsupporting
confidence: 78%
“…This hypothesis is supported by the results of the short-term experiments of Williams et al (1999a) and Williams and Silcock (2000) (for details, see above). The addition of 30 kg N ha -1 yr -1 resulted in a decrease in peat C:N ratios (Williams et al, 1999a), which could enhance rates of first-stage organic matter decomposition and nitrogen mineralization (Aerts et al, 1992). Furthermore, additions of nitrogen to cores of S. capillifolium and S. recurvum, although captured mainly by the moss, had significant effects on the C and N values of the microbial biomass in the underlying peat (Williams and Silcock, 2000).…”
Section: D) Effects On Peat and Peat Water Chemistry As Evidence Of Nsupporting
confidence: 78%
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“…Indeed, increasing N availability can be expected to enhance short-term Sphagnum litter decomposition through an increase of N content [Williams et al, 1999;Bragazza et al, 2006;Gerdol et al, 2007] and a decrease of (soluble) phenolics [Bragazza and Freeman, 2007], thereafter reducing the phenolics/N and the C/nutrient quotients. On the other hand, Sphagnum litter decomposition is strongly affected by its water content, and Sphagnum litter (solid circles) based on studies in which mass loss was monitored for more than 1 year.…”
Section: Litter Chemistrymentioning
confidence: 99%