Soil respiration rates and in natural beech forest (Fagus sylvatica L.) in relation to stand structure
2011
Čater, Matjaž | Ogrinc, Nives
Soil respiration rates were studied as a function of soil type, texture and light intensity at five selected natural beech forest stands with contrasting geology: stands on silicate bedrock at Kladje and Brička in Pohorje, a stand on quartz sandstone at Vrhovo and two stands on a carbonate bedrock in the Karstic-Dinaric area in Kočevski Rog, Snežna jama and Rajhenav, Slovenia, during the growing season in 2005–2006. Soil respiration exhibited pronounced seasonal and spatial variations in the studied forest ecosystem plots. The CO₂ flux rates ranged from minimum averages of 2.3 μmol CO₂ m⁻² s⁻¹ (winter) to maximum averages of about 7 μmol CO₂ m⁻² s⁻¹ (summer) at all the investigated locations. An empirical model describing the relationship between soil respiration and soil temperature predicted seasonal variations in soil respiration reasonably well during 2006. Nevertheless, there were also some indications that soil moisture in relation to soil texture could influence the soil CO₂ efflux rates in both sampling seasons. It was shown that spatial variability of mean soil respiration at the investigated sites was high and strongly related to root biomass. Based on the data, it was shown that new photoassimilates could account for a major part of the total soil respiration under canopy conditions in forest ecosystems where no carbonate rocks are present, indicating that microbial respiration could not always dominate bulk soil CO₂ fluxes. At Snežna jama and Rajhenav, the abiotic CO₂ derived from carbonate dissolution had a pronounced influence on CO₂ efflux accounting, on average, to ∼17%. Further spatial heterogeneity of soil respiration was clearly affected by management practice. Higher respiration rates as well as higher variability in respiration rates were observed in the virgin forest (Rajhenav) than in the management forest (Snežna jama) and could be related to a higher amount of detritus and consequently to less pronounced influence of inorganic pool to CO₂ efflux, lower mixing with atmospheric CO₂ and higher sensitivity to environmental changes. Major differences in soil carbon dynamics among these five forest ecosystems can be explained by the influence of bedrock geology (particularly, the presence or absence of carbonate minerals) and soil texture (affecting gas exchange with overlying air and soil moisture).
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