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Published online 1 January 2007
Published in Soil Sci Soc Am J 71:140-144 (2007)
DOI: 10.2136/sssaj2006.0110
© 2007 Soil Science Society of America
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Carbon Dioxide Effects on Heterotrophic Dinitrogen Fixation in a Temperate Pine Forest

Kirsten S. Hofmockel*

Nicholas School of the Environ. and Earth Sci., Duke Univ., Durham, NC 27708
current address: School of Natural Resources & Environment, Univ. of Michigan, Dana Building, Room G530, 440 Church St., Ann Arbor, MI 48109-1041

William H. Schlesinger

Nicholas School of the Environ. and Earth Sci., Duke Univ., Durham, NC 27708


Figure 1
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Fig. 1. Acetylene reduction assays in (A) homogenized forest floor and (B) mineral soil with nutrient additions (30% gravimetric soil moisture content). Bars represent average ± SE N2 fixation rates. Treatments consisted of combinations of P, Mo, Fe, and glucose (C).

 

Figure 2
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Fig. 2. Average (± SE) monthly rates of total N2 fixation (forest floor + mineral soil horizons). Open bars represent ambient conditions, closed bars represent elevated CO2 (+200 µL L–1).

 

Figure 3
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Fig. 3. Measurements of potential heterotrophic N2 fixation rates as a function of gravimetric soil moisture content in forest floor and mineral soil horizons.

 





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