Key points are not available for this paper at this time.
Global warming and the resultant increase in evapotranspiration might lead to lowered water tables in peatlands and an increase in fire frequency. The objective of this study was to investigate some of the potential effects of these changes on peat decomposition. Dry mass losses and emissions of CO 2 and CH 4 from peat samples taken from three depth layers (0—10, 10—20, and 30—40 cm) of a black spruce peatland were measured in the laboratory at 8°, 16°, and 24°C under two moisture treatments. Effects of deep peat fire on decomposition were also simulated by burning the upper layer (0—10 cm) of peat and adding the ash to peat samples from the 10—20 cm layer. CH 4 release averaged <1% of total carbon loss in flooded samples. Release of CO 2 was 4—9 times greater from the 0—10 cm layer than from the 30—40 cm layer. After 120 d, the 30—40 cm layer had lost <1% of its original dry mass in all treatments. Higher temperatures strongly promoted decomposition of samples exposed to drying cycles but had little effect on decomposition of continuously flooded samples. Ash addition had variable effects on CO 2 emissions but may have promoted CH 4 production. It is suggested that in certain situations, global warming may not cause appreciable increases in carbon loss from peat deposits. The results indicate that some deeper peats are resistant to decay even when exposed to warm, aerobic conditions. However, further experimental work is needed to predict the long—term response of peat deposits to changes in water levels in different peatland types.
Hogg et al. (Sat,) studied this question.