Liu Xingren, Shi Yulong, Zhang Qingwen, Li Guichun
Institute of Environment and Sustainable Development in Agriculture, Chinese Academy of Agricultural Sciences, Beijing, 100081, China.
Environ Sci Pollut Res Int. 2021 Feb;28(6):6649-6663. doi: 10.1007/s11356-020-10928-4. Epub 2020 Oct 1.
Nitrous oxide (NO) is a strong greenhouse gas, and it is of great significance for NO reduction to study the effects of biochar on its production pathway. In this research, the contributions and mechanisms of biochar on autotrophic nitrification (ANF), heterotrophic nitrification (HNF), and denitrification (DF) to NO emissions were studied by using N stable isotopes and high-throughput sequencing after laboratory incubation. The results showed that biochar addition at 2% (B2) significantly reduced the NO emissions from the ANF by an average of 20.6%, while adding 5% biochar (B5) had no significant effect on the ANF. Both B2 and B5 significantly reduced the NO emissions from the HNF by 15.7% and 13.2%, respectively, and reduced the NO emissions from the DF by 40.9% and 11.7%, respectively. B2 enhanced the relative contribution rate of the ANF to NO emissions by 6.3%, while B5 had little effect on it. Biochar addition significantly changed the copy numbers of the AOA and AOB, as well as the nirK, nirS, and nosZ genes, but it had no significant effect on the community composition of the AOA and had minimal effect on the AOB community. B2 significantly increased the abundance of the genus Rhodococcus of nirK type denitrifiers and had a significant effect on the relative abundance of Cupriavidus and Pseudomonas of the nosZ type denitrifiers. These results revealed that the inhibitory effects of biochar on NO emissions from nitrification might be attributed to the direct immobilization and adsorption of inorganic N by biochar and to its promotion of the genus Rhodococcus of nirK-type denitrifiers and the genera Cupriavidus and Pseudomonas of the nosZ-type denitrifiers. The soil exchangeable NH-N and NO-N concentrations were the primary factors affecting the NO emission rates. These results help to elucidate the effects and mechanisms of biochar on NO production pathways in agricultural soil.
氧化亚氮(NO)是一种强效温室气体,研究生物炭对其产生途径的影响对于减少NO具有重要意义。在本研究中,通过实验室培养后利用氮稳定同位素和高通量测序技术,研究了生物炭对自养硝化作用(ANF)、异养硝化作用(HNF)和反硝化作用(DF)产生NO排放的贡献及机制。结果表明,添加2%的生物炭(B2)显著降低了ANF产生的NO排放,平均降低了20.6%,而添加5%的生物炭(B5)对ANF没有显著影响。B2和B5分别显著降低了HNF产生的NO排放15.7%和13.2%,并分别降低了DF产生的NO排放40.9%和11.7%。B2使ANF对NO排放的相对贡献率提高了6.3%,而B5对其影响较小。添加生物炭显著改变了氨氧化古菌(AOA)和氨氧化细菌(AOB)的拷贝数,以及nirK、nirS和nosZ基因,但对AOA的群落组成没有显著影响,对AOB群落的影响也最小。B2显著增加了nirK型反硝化细菌红球菌属的丰度,并对nosZ型反硝化细菌贪铜菌属和假单胞菌属的相对丰度有显著影响。这些结果表明,生物炭对硝化作用产生的NO排放的抑制作用可能归因于生物炭对无机氮的直接固定和吸附,以及对nirK型反硝化细菌红球菌属和nosZ型反硝化细菌贪铜菌属和假单胞菌属的促进作用。土壤交换性NH-N和NO-N浓度是影响NO排放速率的主要因素。这些结果有助于阐明生物炭对农业土壤中NO产生途径的影响及机制。