Abstract
AbstractBiochar–bioenergy coproduction from biomass pyrolysis has the potential to contribute to climate change mitigation. Biochar produced at various pyrolysis temperatures (<600°C) has been widely studied. However, the effect of biochars, produced at high pyrolysis temperature (≥600°C), on soil nitrogen (N) dynamics and nitrous oxide (N2O) emission is largely unknown. A pot trial was performed to examine the effect of high pyrolysis temperature (600, 700, 850 and 950°C) woody biochars on soil N dynamics, microbial gene abundance and N2O emissions with (+N) and without N (−N) fertilization from an acid soil. Results showed that all biochar treatments significantly lowered the N2O emissions in both fertilized and unfertilized regimes. However, the suppressive effect on N2O emission among different high pyrolysis temperatures was not statistically different. Biochar amendment significantly decreased the concentration of soil NH4+, and lower levels of soil NO3− were observed at the later stage of experiment. Under −N, plant biomass and N uptake were significantly lowered in all biochar treatments. Under +N, biochar addition significantly increased plant biomass, while only the 700°C biochar significantly increased N uptake. This suggests that single application of biochar could limit soil mineral N bioavailability and further decrease plant growth and N uptake in the plant–soil system. Biochar amendments tended to increase nitrous oxide reductase (nosZ) gene abundance, but this effect was only significant for biochar produced at 950°C under +N. In conclusion, high pyrolysis temperature biochars can be effectively used to reduce N2O emission, while increases in nosZ gene abundance and decreases in NH4+ and NO3− concentrations in the acid soil are likely to be responsible for the reduction in N2O emission. Thus, woody biochars as a by‐product produced at high pyrolysis temperature have the potential to mitigate soil N2O emission via modifying N transformation and further affect climate change.
Highlights
Global climate change and the increasing use of fossil fuels have become a severe challenge in the 21st century (Crombie & Mašek, 2015)
Mitigating climate change can be achieved by renewable energy sources and reducing greenhouse gas (GHG) emissions (Nelissen, Rütting, Huygens, Ruysschaert, & Boeckx, 2015)
The biochar amendment to soil has been recently proposed as a promising strategy to mitigate soil N loss and N2O emissions from fertilized systems (Cayuela et al, 2013; Van Zwieten et al, 2009)
Summary
Global climate change and the increasing use of fossil fuels have become a severe challenge in the 21st century (Crombie & Mašek, 2015). Pyrolysis temperature may affect biochar's physicochemical properties such as pH, bioavailable carbon (C) and N contents, composition of functional groups (e.g., C–O and C–H) and porosity and pore size distribution This may affect soil and plant nutrient status after biochar incorporation to agroecosystems (Lehmann & Joseph, 2012; Lehmann et al, 2011). This study aimed to investigate the effect of high pyrolysis temperature woody biochars on soil N dynamics, the abundance of microbial functional genes, plant biomass and N2O emissions in an acid soil under conditions with and without N fertilization. It was hypothesized that soil amendment of biochars with high pyrolysis temperatures would (a) modify plant N uptake and biomass via changing soil biochemical properties; (b) alter microbial functional gene abundance involved in nitrification and denitrification processes; and (c) suppress N2O emissions via limiting the bioavailability of soil N sources for soil nitrifiers and denitrifiers
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