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Abstract
Forest floor C0
2 efflux (F
ff) depends on vegetation type, climate, and soil physical properties. We assessed the effects of biological factors on F
ff by comparing a maturing pine plantation (PP) and a nearby mature Oak-Hickory-type hardwood forest (HW). F
ff was measured continuously with soil chambers connected to an IRGA during 2001-2002. At both sites, F
ff depended on soil temperature at 5cm (T
5) when soil was moist (soil moisture, 0> 0.20 m3mm-3)a, nd on both T5 and 0 when soil was drier. A model (F
ff( T
5,0 )) explained 292% of the variation in the daily mean F
ff at both sites. Higher radiation reaching the ground during the leafless period, and a thinner litter layer because of faster decomposition, probably caused higher soil temperature at HW compared with PP. The annual Frt was estimated at 1330 and 1464 g Cm
Citation
Palmroth, S.; Maier, Chris A.; McCarthy, Heather R.; Oishi, A. C.; Kim, H. S.; Johnsen, Kurt H.; Katul, Gabrial G.; Oren, Ram. 2005. Contrasting responses to drought of forest floor CO
2 efflux in a loblolly pine plantation and a nearby Oak-Hickory forest. Global Change Biology 11: 421-434