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Published in Soil Sci. Soc. Am. J. 67:1594-1601 (2003).
© 2003 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

SYMPOSIUM

Changes in Ecosystem Carbon and Nitrogen in a Loblolly Pine Plantation over the First 18 Years

D. W. Johnson*,a, D. E. Todd, Jr.b and V. R. Tolbertb

a Environmental and Resource Sciences, Fleischmann Agriculture Bldg/370, University of Nevada, Reno, NV 89557
b Environmental Sciences Division, Oak Ridge National Lab., P.O. Box 2008, Building 1059, Oak Ridge, TN 37831-6422

* Corresponding author (dwj{at}cabnr.unr.edu).

Eighteen years after the establishment of a loblolly pine (Pinus taeda L.) plantation, ecosystem C content had approximately tripled (from 54 to 161 Mg C ha-1) primarily because of increases in tree biomass. Ninety-three percent of the net ecosystem C accumulated in biomass (100 Mg C ha-1) and 6% of net ecosystem C accumulated in the forest floor (13 Mg C ha-1). No statistically significant changes in soil C were found. Growth responses to fertilization noted in Year 4 were no longer statistically significant in Year 18. Nitrogen accumulation in aboveground biomass and forest floor were approximately equal (averaging approximately 270 kg N ha-1 each) and could have come from a combination of atmospheric deposition, soil N mineralization, and, in the treated plots, fertilizer input. No statistically significant changes in soil N content were found. The results of this study are similar to those from a previous study in a loblolly pine plantation in South Carolina but contrast with those in nearby deciduous forests where substantial changes in soil C and N over similar time periods have been noted.

Abbreviations: DBH, diameter at breast height • GLM, General Linear Model • NERP, National Experimental Research Park • WBC, Walkley-Black C




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