See more from this Session: Biochar: Environmental Uses
There were no unified trends observed in the effect of field aging on these two biochars. The first biochar was a fast-pyrolysis oak hardwood biochar (500 oC). For this fast pyrolysis biochar, both aged and fresh biochar amendments reduced N2O production compared to unamended soil, with corresponding reductions in nitrate availability. On the other hand, a slow pyrolysis oak hardwood biochar (550 oC), observed no significant impact in the N2O production or nitrate/ammonium availability in the initial soil incubations of the fresh biochar. CO2 production in the fresh biochar amended soil was suppressed. Upon field aging, this slow pyrolysis biochar stimulated both N2O and CO2 production compared to the original unamended soil as well as the fresh biochar amended soil, potentially from the increased nitrate availability in the aged biochar amended soils. Both biochars showed remarkable reductions in the presence of sorbed organic compounds due to field aging. These contrasting results in the GHG production indicate that the impact on the soil microbial GHG production is a balance of multiple factors. One of these is the role of the surface oxygen groups, since the surface oxygen groups can control the interaction of the biochar with the environment, which historically has been observed for black carbons.
See more from this Session: Biochar: Environmental Uses