Assessing the global C budget requires a better understanding of the effect
of temperature on soil CO2 efflux both from experiments and developments i
n theory. intact soil cores (ca. 31 cm in diameter and 45 cm in depth) were
collected from a farmland and a sitka spruce site near Edinburgh. Scotland
, and incubated in a growth chamber with varying temperature and soil moist
ure contents. There was no influence of incubation time on the measured soi
l respiration rate found in this study and this is different from previous
studies that commonly use a reconstructed soil sample. Both soils showed an
exponential increase in respiration rate with temperature. No optimal temp
erature for soil respiration was found with soil temperature up to 32 degre
esC. The influence of soil moisture content, varying between 20 and 50 vol%
, on soil respiration and its response to temperature was not obvious. Most
equations describing the relationship between soil respiration and tempera
ture fitted the observed data well. However, based on model and Q(10) analy
sis, the Arrhenius model may be better than the others in its performance a
nd theoretical basis, despite a tendency to underestimate somewhat the resp
onse of soil respiration at low temperature. A simple empirical equation, R
-s = a(T - T-min)(b), is presented, which is more responsive at low tempera
ture than the Arrhenius and exponential models. (C) 2001 Elsevier Science L
td. All rights reserved.