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Variation in N2O emission and N2O related microbial functional genes in straw- and biochar-amended and non-amended soils

生物炭 稻草 土壤水分 一氧化二氮 修正案 肥料 环境化学 农学 中观 化学 硝化作用 微生物种群生物学 环境科学 氮气 土壤科学 生物 营养物 热解 细菌 遗传学 有机化学 法学 政治学
作者
Rong Huang,Yingyan Wang,Jiang Liu,Jiacheng Li,Guo-Xin Xu,Mei Luo,Chang Xu,En Ci,Ming Gao
出处
期刊:Applied Soil Ecology [Elsevier BV]
卷期号:137: 57-68 被引量:101
标识
DOI:10.1016/j.apsoil.2019.01.010
摘要

Abstract Reducing mineral fertilizer application is an important management practice for mitigating nitrous oxide (N2O) emissions. Crop straw and biochar are two farmer-friendly residues that can be used for reducing the application of mineral fertilizers. However, different effect of straw- and biochar-amended and non-amended soils on N2O emissions is not well understood. Here, we conducted a mesocosm experiment in a vegetable field in Southwestern China using four treatments: control (CT, no addition), solely mineral fertilizers at the recommended dosage (F), maize straw with mineral fertilizers (SF), and biochar with mineral fertilizers (BF), based on the same total nitrogen, phosphorus and potassium contents. Soil N2O fluxes, cumulative N2O emission, soil chemical parameters, the abundance of N2O related microbial functional genes (amoA, nirS, nirK and nosZ) and microbial community structure were monitored and analyzed. Compared to F, the SF treatment increased the cumulative N2O emission. However, no significant difference was observed in cumulative N2O emission between F and BF treatments. Covariation in cumulative N2O emission and soil dissolved organic nitrogen (DON) content indicated that heterotrophic ammonia oxidation fueled by soil DON might be the driving force for N2O production. Compared to F, both SF and BF treatments increased the amoA gene copy numbers of ammonia oxidizing bacteria (AOB) but reduced those of ammonia oxidizing archaea (AOA); nirS and nosZ gene copy numbers were also reduced under SF and BF treatments. Compared to SF, the diversity of nirK and nosZ communities under the BF treatment was increased, whereas the diversity of nirS community was decreased. Lower cumulative N2O emission under BF than that under SF may be attributed to lower N2O production from heterotrophic ammonia oxidation fueled by soil DON and increased N2O consumption mediated by nosZ-harboring denitrifiers.
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