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Net primary production and light use efficiency in a mixed coniferous forest in Sweden
FREDERIK LAGERGREN 1 , LARS EKLUNDH 1 , ACHIM GRELLE 2 , MATTIAS LUNDBLAD 3 , MEELIS MÖLDER 1 , HARRY LANKREIJER 1 & ANDERS LINDROTH 1
  1 Physical Geography and Ecosystems Analysis, Geobiosphere Science Centre, Lund University, Sölvegatan 12, SE-223 62 Lund, Sweden,
  2 Department for Ecology and Environmental Research, Swedish University of Agricultural Sciences, PO Box 7042, SE-750 07 Uppsala, Sweden and
  3 Swedish Environmental Protection Agency, Blekholmsterrassen 36, SE-106 48 Stockholm, Sweden
Correspondence to  Fredrik.Lagergren. Fax: +46 46 2220321; e-mail: Fredrik.Lagergren@nateko.lu.se
Copyright 2005 Blackwell Publishing Ltd
KEYWORDS
light saturation • meteorological dependency • Norway spruce • Scots pine • seasonal variation

ABSTRACT

AbstractINTRODUCTIONMATERIALS AND METHODSRESULTS AND DISCUSSIONCONCLUSIONSACKNOWLEDGMENTSREFERENCES

Simple light use efficiency (ɛ) models of net primary production (NPP) have recently been given great attention (NPP = ɛ × absorbed photosynthetically active radiation). The underlying relationships have, however, not been much studied on a time step less than a month. In this study daily NPP was estimated as the sum of net ecosystem exchange (NEE) and heterotrophic respiration (Rh) of a mixed pine and spruce forest in Sweden. NEE was measured by eddy correlation technique and Rh was estimated from measurements of forest floor respiration (Rf) and the root share of Rf. The total yearly NPP was on average 810 g C m−2 year−1 for 3 years and yearly ɛ was between 0.58 and 0.71 g C MJ−1, which is high in comparison with other studies. There was a seasonal trend in ɛ with a relatively constant level of approximately 0.90 g C MJ−1 from April to September Daily NPP did not increase for daily intercepted radiation above 6 MJ m−2 d−1, indicating that between-years variation in NPP is not directly dependent on total Qi. The light was most efficiently used at an average daytime temperature of around 15 °C. At daytime vapour pressure deficit above 1400 Pa ɛ was reduced by approximately 50%.


Received: 25 June 2001; Accepted: 27 September 2004;
DIGITAL OBJECT IDENTIFIER (DOI)
10.1111/j.1365-3040.2004.01280.x About DOI

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