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Sammanfattning

Sulphur (S) and nitrogen (N) deposition are important drivers of the terrestrial carbon (C) and N cycling. We analyzed changes in C and N pools in soil and tree biomass at a highly acidified spruce site in the Czech Republic during a 15 year period. Total S deposition decreased from 5 to 1.1 g m(-2) yr(-1) between 1995 and 2009, whereas bulk N deposition did not change. Over the same period, C and N pools in the Oa horizon declined by 116 g C and 4.2 g N m(-2) yr(-1), a total decrease of 47% and 42%, respectively. This loss of C and N probably originated from organic matter (OM) that had accumulated during the period of high acid deposition when litter decomposition was suppressed. The loss of OM from the Oa horizon coincided with a substantial leaching (1.3 g N m(-2) yr(-1) at 90 cm) in the 1990s to almost no leaching (

Nyckelord

acidification; carbon; deposition; DOC; forest floor; leaching; nitrogen; nitrogen saturation; soil; sulphur

Publicerad i

Global Change Biology
2011, volym: 17, nummer: 10, sidor: 3115-3129
Utgivare: WILEY-BLACKWELL

SLU författare

UKÄ forskningsämne

Miljö- och naturvårdsvetenskap
Skogsvetenskap

Publikationens identifierare

  • DOI: https://doi.org/10.1111/j.1365-2486.2011.02468.x

Permanent länk till denna sida (URI)

https://res.slu.se/id/publ/57201