Huang Rong, Gao Ming, Wang Ying-Yan, Li Jia-Cheng, Xu Guo-Xin, Luo Mei, Xu Chang
College of Resources and Environment, Southwest University, Chongqing 400715, China.
Chongqing Municipal Tobacco Company, Chongqing 400023, China.
Huan Jing Ke Xue. 2019 Jan 8;40(1):401-411. doi: 10.13227/j.hjkx.201805125.
Crop straw is an important agricultural source, which can replace chemical fertilizers. A field experiment with six different amounts of fertilization combined with maize straw residues was carried out in purple soil, including the control (CK), conventional fertilizing (F), straw return with conventional fertilizing (100FS), straw return with 70% conventional fertilizing (70FS), straw return with 60% conventional fertilizing (60FS), and straw return with 50% regular fertilizing (50FS), to determine the response of the soil NO emission and ammonia-oxidizing microorganism community distribution to straw return with reducing fertilizer. The dynamic characteristics of the NO emission in purple soil were observed using an closed chamber and gas chromatography-based system. The ammonia-oxidizing microorganism community distribution was analyzed with multiple molecular techniques (DNA-based clone library and qPCR) linked to physical-chemical soil properties. The results show that the combination of straw with fertilizer increases the NO emission and cumulative NO emission. The highest NO emission[57.59-6238.02 μg·(m·h)]and cumulative NO emission (60.76 kg·hm) were observed for the 100FS treatment. Compared with the F treatment, the soil ammonium nitrogen and nitrate nitrogen contents are reduced and the soil organic matter increases after crop straw return with chemical fertilizer. However, significant changes of the soil total nitrogen and pH were not observed. The bacterial ammonia oxidizer (AOB) gene abundance is higher than that of the archaeal ammonia oxidizer (AOA). The AOA gene abundance during F treatment (50.9×10 copies·g) is significantly higher than that of others, while the AOB abundance gene of the F treatment is the lowest (1.36×10 copies·g). The 100FS reduces the community diversity and Pielou index of AOA and AOB gene. Their gene abundance significantly declines during 100FS treatment. However, the increment of the AOA and AOB gene diversity and dominant increment of AOB gene abundance are significant when applying straw with reducing fertilizer. The specific AOA indicator OTU1 may be most important with respect to the direct and indirect production of NO in purple soil. The redundancy analysis (RDA) shows that the community structure of AOA is remarkably relevant to the soil ammonium nitrogen, organic matter, and available phosphorus (<0.05) and that the community structure of AOB is remarkably relevant to the soil dissolved organic nitrogen, total nitrogen, available potassium, and available phosphorus (<0.05). The tolerance to different environments and ecological niches of AOB is weaker than that of AOA. Our results illustrate that the maize straw return with 60%-70% regular fertilizing dramatically increases the community diversity and abundance of the AOA and AOB genes and partly mitigates the soil NO emission without significantly decreasing the vegetable yields.
作物秸秆是一种重要的农业资源,可替代化肥。在紫色土上进行了一项田间试验,设置了六种不同施肥量并结合玉米秸秆残茬,包括对照(CK)、常规施肥(F)、常规施肥并秸秆还田(100FS)、70%常规施肥并秸秆还田(70FS)、60%常规施肥并秸秆还田(60FS)以及50%常规施肥并秸秆还田(50FS),以确定土壤NO排放和氨氧化微生物群落分布对减量化施肥秸秆还田的响应。使用基于密闭箱和气相色谱的系统观测紫色土中NO排放的动态特征。通过多种与土壤理化性质相关的分子技术(基于DNA的克隆文库和qPCR)分析氨氧化微生物群落分布。结果表明,秸秆与肥料结合增加了NO排放和累积NO排放量。100FS处理的NO排放最高[57.59 - 6238.02 μg·(m²·h)],累积NO排放量为60.76 kg·hm²。与F处理相比,化肥配施作物秸秆还田后土壤铵态氮和硝态氮含量降低,土壤有机质增加。然而,土壤全氮和pH未观察到显著变化。细菌氨氧化菌(AOB)基因丰度高于古菌氨氧化菌(AOA)。F处理期间AOA基因丰度(50.9×10⁶拷贝·g⁻¹)显著高于其他处理,而F处理的AOB丰度基因最低(1.36×10⁶拷贝·g⁻¹)。100FS降低了AOA和AOB基因的群落多样性和Pielou指数。在100FS处理期间它们的基因丰度显著下降。然而,减量化施肥配施秸秆时AOA和AOB基因多样性增加且AOB基因丰度优势增加显著。特定的AOA指示OTU1对于紫色土中NO的直接和间接产生可能最为重要。冗余分析(RDA)表明,AOA的群落结构与土壤铵态氮、有机质和有效磷显著相关(<0.05),AOB的群落结构与土壤溶解有机氮、全氮、速效钾和有效磷显著相关(<0.05)。AOB对不同环境和生态位的耐受性弱于AOA。我们的结果表明,60% - 70%常规施肥量配施玉米秸秆还田显著增加了AOA和AOB基因的群落多样性和丰度,并在不显著降低蔬菜产量的情况下部分缓解了土壤NO排放。