2006
DOI: 10.2136/sssaj2004.0173
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Litter Quality and Climate Decouple Nitrogen Mineralization and Productivity in Chilean Temperate Rainforests

Abstract: We measured litter quality, N mineralization, air and soil temperatures, soil moisture, and aboveground net primary production (ANPP) at 18 plots in three forest types typical of full-stature forests found on western slopes of the Cordillera de Piuchué (CP) on Isla de Chiloé in southern Chile. The primary objectives were to examine the range of net N mineralization across forest types that have different vegetation and litter composition, assess probable controls on mineral N production and leaching, and to de… Show more

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Cited by 24 publications
(15 citation statements)
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“…However, the stimulated C uptake is not enough to offset the N limitation and the net result is still an increase in atmospheric CO 2 and an overall reduction in soil C levels [70]. Some researchers have reported that increasing temperatures increase N mineralization [71][72][73], which could have a positive effect on plant growth. However, a warming study by An et al [74] showed that N mineralization was stimulated in the first year but depressed afterward.…”
Section: Influence Of Climate Change On Soil Properties and Processesmentioning
confidence: 99%
“…However, the stimulated C uptake is not enough to offset the N limitation and the net result is still an increase in atmospheric CO 2 and an overall reduction in soil C levels [70]. Some researchers have reported that increasing temperatures increase N mineralization [71][72][73], which could have a positive effect on plant growth. However, a warming study by An et al [74] showed that N mineralization was stimulated in the first year but depressed afterward.…”
Section: Influence Of Climate Change On Soil Properties and Processesmentioning
confidence: 99%
“…Plant availability of organic N in a biosolid mainly depends on soil microbial processes of mineralization and immobilization whose turnover is mainly influenced by its C : N ratio, although the soil N turnover cannot be explained by this parameter alone. Soil chemical-physical characteristics and biosolid properties such as soluble C content, N biochemical quality, and phenolic content could play a crucial role in determining N mineralization [12][13][14][15][16]. Specific studies on the mineralization dynamic of the organic N in biosolids are therefore required in order to evaluate N supply to plants and to avoid leaching of N in the environment.…”
Section: Introductionmentioning
confidence: 99%
“…Taylor et al 1991;Prescott 2002;Inagaki et al 2004;Miyamoto and Hiura 2008) and soil conditions (Bengtsson et al 2003;Booth et al 2005;Kooijman et al 2008). Distinctive differences were found between conifers and hardwood species with regard to their effects on stocks, distribution and mineralization rates of soil N (Jerabkova et al 2006;Joshi et al 2006;Inagaki et al 2004). In addition, N 2 O emissions were significantly higher in deciduous than in coniferous forests (Ambus et al 2006;Butterbach-Bahl et al 2002).…”
mentioning
confidence: 99%