Ren Ning, Wang Yang, Ye Youliang, Zhao Yanan, Huang Yufang, Fu Wen, Chu Xv
Agricultural Green Development Engineering Technology Research Center, College of Resources and Environment, Henan Agricultural University, Zhengzhou, China.
Front Microbiol. 2020 Aug 21;11:1948. doi: 10.3389/fmicb.2020.01948. eCollection 2020.
Little has been reported on the effects of long-term fertilization on rhizosphere soil microbial diversity. Here, we investigated the effects of long-term continuous nitrogen (N) fertilization on the diversity and composition of soil bacteria using data from a 10-year field experiment with five N application rates (0, 120, 180, 240, and 360 kg N hm). The results revealed varying degrees of reduction in the numbers of bacterial operational taxonomic units (OTUs) in response to the different N application rates. The highest wheat yield and number of proprietary bacterial OTUs were found in the N input of 180 kg N hm. In terms of average relative richness, the top seven phyla of soil bacteria in the rhizosphere of wheat after long-term nitrogen application were Proteobacteria, . Among these, and were found to be unaffected by the nitrogen fertilizer and soil environmental factors (pH, C/N ratio, and NO concentration), whereas and showed significant positive and negative correlations, respectively, with soil pH. The richness of significantly increased in the N treatment. and showed significant positive correlations with soil NO and wheat yield, and the average relative richness of these two phyla was high under long-term application of the N treatment. These findings indicate that the relative richness of and can affect wheat yield. In conclusion, the results of our 10-year field experiments clearly show that long-term N fertilization can significantly affect most of the dominant soil bacterial species changing the soil pH. The richness of can serve as an indicator of a decreased soil pH caused by long-term N fertilization.
关于长期施肥对根际土壤微生物多样性的影响,此前报道较少。在此,我们利用一项为期10年的田间试验数据,研究了长期连续施氮对土壤细菌多样性和组成的影响,该试验设置了5个施氮量水平(0、120、180、240和360千克氮/公顷)。结果显示,不同施氮量下细菌可操作分类单元(OTU)数量出现不同程度的减少。在施氮量为180千克氮/公顷时,小麦产量和特有细菌OTU数量最高。就平均相对丰度而言,长期施氮后小麦根际土壤细菌的前七大门类为变形菌门等。其中,某些门类不受氮肥和土壤环境因素(pH值、碳氮比和硝酸根浓度)的影响,而另外一些门类分别与土壤pH值呈显著正相关和负相关。在施氮处理中,某一门类的丰度显著增加。某些门类与土壤硝酸根和小麦产量呈显著正相关,在长期施氮处理下这两个门类的平均相对丰度较高。这些发现表明,某些门类的相对丰度会影响小麦产量。总之,我们10年田间试验的结果清楚地表明,长期施氮会通过改变土壤pH值,显著影响大多数优势土壤细菌种类。某一门类的丰度可作为长期施氮导致土壤pH值下降的一个指标。