Response Of Peat Carbon Cycle At Different Depths To Simulated Warming And Oxidizing

Warming and water table drawdown greatly reshapes peatlands carbon cycle, espcially when considering the old carbon stored under the peatland subsurface. However, little is known about the effects of warming, oxidizing by drying or their combination on carbon decomposition at different depths(0-100 cm) of peat. In this research, soil of different depths from the Zoige Plateau was incubated in four scenarios(8°C-anaerobic, 8°C-aerobic, 18°C-anaerobic and 18°C-aerobic) to detect the exported carbon.Our result showed that soil respiration(Rs) increased obviously with enhanced temperature and oxygen. The total CO2 fluxes of 2400.22 ± 57.69 mg m-2 d-1 under 8°C-anaerobic condition increased by 73.6%, 40.7% and 176.5% with warming, oxidizing and the combined effect of warming and oxidizing respectively. The average dissolved organic carbon(DOC) concentration was 74.90 ± 8.09 mg kg-1 under 8°C-anaerobic condition, but increased by 53.5%, 44% and 159.4%, respectively under the condition of warming, oxidizing and their combination. Rs and its variation under warming and oxidization differed significantly among different depths, probably caused by the differences of soil substrate, especially the variation in distribution of soil microbes and enzymes among depths of peatlands. By classifying the source of Rs as young soil(YS: 0-20 cm) and old soil(OS: 21-100 cm), this reseaerch found that OS accounted for a huge part of total Rs under 8°C-anaerobic condition(CO2: 74.2%; DOC: 60.7%). Such relative contribution of OS to total Rs did not change obviously with warming or oxidizing. Though YS and OS responded equally to warming and oxidizing, OS was responsible for a larger proportion of total increase in Rs. It is concluded that peatlands soil in our field of mid-latitude and high altitude is less sensitive to warming and oxidizing than peatlands of higher latitude, but that OS of this peatlands is more critical in predicting regional peatland carbon cycle.Our result also showed that enhanced temperature decreased CH4 emission from 4.94 ± 0.70 mg CH4-C m-2 d-1 at 8°C to 3.16 ± 0.69 mg CH4-C m-2 d-1 at 18°C. The response among the whole depth soil to warming was different. At surface, warming increased CH4 emission, but decreased it at deeper layers, which determined by soil substrate quality. The result also demonstrated that soil among the whole depth was much variation. We also found that the effect of dissolved organic carbon(DOC) on CH4 emission determined by the origin of DOC. Microbe biomass carbon(MBC) concentration increased with warming, and had a negative effect on CH4 emission.