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Title: Aboveground sink strength in forests controls the allocation of carbon below ground and its [CO₂]-induced enhancement.
Authors: Palmroth, S.
Oren, R.
McCarthy, H.R.
Johnsen, K.H.
Finzi, A.C.
Butnor, J.R.
Ryan, M.G.
Schlesinger, W.H.
USDA, FS
Source: Proceedings of the National Academy of Sciences of the United States of America. 2006 Dec. 19, v. 103, issue 51, p. 19362-19367.
NALT Subjects: forest plantations
Pinus taeda
deciduous forests
carbon dioxide
elevated atmospheric gases
primary productivity
leaf area index
nitrogen
nutrient availability
nitrogen fertilizers
fertilizer application
soil respiration
roots
root growth
North Carolina
Wisconsin
Tennessee
Italy
Other Subjects: total allocation to carbon below ground
free air carbon dioxide enrichment
net primary productivity
Issue Date: 19-Dec-2006
Abstract: The partitioning among carbon (C) pools of the extra C captured under elevated atmospheric CO₂ concentration ([CO₂]) determines the enhancement in C sequestration, yet no clear partitioning rules exist. Here, we used first principles and published data from four free-air CO₂ enrichment (FACE) experiments on forest tree species to conceptualize the total allocation of C to below ground (TBCA) under current [CO₂] and to predict the likely effect of elevated [CO₂]. We show that at a FACE site where leaf area index (L) of Pinus taeda L. was altered through nitrogen fertilization, ice-storm damage, and droughts, changes in L, reflecting the aboveground sink for net primary productivity, were accompanied by opposite changes in TBCA. A similar pattern emerged when data were combined from the four FACE experiments, using leaf area duration (L(D)) to account for differences in growing-season length. Moreover, elevated [CO₂]-induced enhancement of TBCA in the combined data decreased from approximately equal to 50% (700 g C m⁻² y⁻¹) at the lowest L(D) to approximately equal to 30% (200 g C m⁻² y⁻¹) at the highest L(D). The consistency of the trend in TBCA with L and its response to [CO₂] across the sites provides a norm for predictions of ecosystem C cycling, and is particularly useful for models that use L to estimate components of the terrestrial C balance.
URI: http://hdl.handle.net/10113/551
Appears in Collections:USDA Research and Information

Files in This Item:

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IND43901114.pdf935KbAdobe PDFView/Open

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