Abstract

Biochar application to agricultural soil is an appealing approach to mitigate nitrous oxide (N2O) and methane (CH4) emissions. However, the underlying microbial mechanisms are unclear. In this study, a paddy soil slurry was incubated anaerobically for 14d with biochar amendments produced from rice straw at 300, 500, or 700°C (B300, B500, and B700) to study their influences on greenhouse gas emissions. Illumina sequencing was used to characterize shift of soil bacterial and archaeal community composition. After peaking at day 1, N2O emission then sharply decreased to low levels while CH4 started to emit at day 3 then continually increased with incubation. Compared to control soil (57.9mgkg-1 soil), B300, B500, and B700 amendments decreased N2O peak emission to 17.9, 1.28, and 0.59mgkg-1, mainly due to increased soil pH. In contrast, the amendments enhanced CH4 production from 58.2 to 93.4, 62.6, and 63.4mgkg-1 at day 14 due to increased soil dissolved organic carbon. Abundance of denitrifying bacteria (e.g., Bacilli, 7.07-13.6 vs. 16.9%) was reduced with biochar amendments, especially with B500 and B700, contributing to the decreased N2O emissions. However, larger pore size of B500 and B700 (surface area of 68.1 and 161m2g-1) than B300 (4.40m2g-1) favored electron transfer between bacteria and iron minerals, leading to increased abundance of iron-reducing bacteria, (e.g., Clostridia, 48.2-50.6 vs. 33.3%), which competed with methanogens to produce CH4, thereby leading to lower increase in CH4 emission. Biochar amendments with high pH and surface area might be effective to mitigate emission of both N2O and CH4 from paddy soil.

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