Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, China.
Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan, 430074, China.
J Environ Manage. 2021 Aug 1;291:112579. doi: 10.1016/j.jenvman.2021.112579. Epub 2021 May 3.
Potassium (K) fertilizer additions can result in high crop yields of good quality and low nitrogen (N) loss; however, the interaction between K and N fertilizer and its effect on NO emissions and associated microbes remain unclear. We investigated this in a pot experiment with six fertilizer treatments involving K and two sources of N, using agricultural soil from the suburbs of Wuhan, central China. The aim was to determine the effects of the interaction between K and different forms of N on the NO flux and the abundance of nitrifying and denitrifying microbial communities, using static chamber-gas chromatography and high-throughput sequencing methods. Compared with no fertilizer control (CK), the addition of nitrate fertilizer (NN) or ammonia fertilizer (AN) or K fertilizer significantly increased NO emissions. However, the combined application (NNK) of K and NN significantly reduced the average NO emissions by 28.3%, while the combined application (ANK) of K and AN increased NO emissions by 22.7%. The abundance of nitrifying genes amoA in ammonia oxidizing archaea (AOA) and ammonia oxidizing bacteria (AOB) changed in response to N and/or K fertilization, but the denitrifying genes narG, nirK and norl were strongly correlated with NO emissions. This suggests that N or K fertilizer and their interaction affect NO emissions mainly by altering the abundance of functional genes of denitrifying microbes in the soil-plant system. The genera Paracoccus, Rubrivivax and Geobacter as well as Streptomyces and Hyphomicrobium play an important role in NO emissions during denitrification with the combined application of N and K.
钾(K)肥的添加可以带来高产、优质的作物和较低的氮(N)损失;然而,K 和 N 肥之间的相互作用及其对 NO 排放和相关微生物的影响仍不清楚。我们在中国中部武汉市郊区的农业土壤中进行了一项盆栽实验,使用 6 种施肥处理,涉及 K 和两种 N 源,以此来研究这一问题。本研究旨在通过静态箱-气相色谱和高通量测序方法,确定 K 和不同形式的 N 之间的相互作用对 NO 通量和硝化及反硝化微生物群落丰度的影响。与不施肥对照(CK)相比,添加硝酸盐肥料(NN)或氨肥(AN)或 K 肥均显著增加了 NO 排放。然而,K 和 NN 的联合应用(NNK)显著降低了平均 NO 排放 28.3%,而 K 和 AN 的联合应用(ANK)则增加了 22.7%的 NO 排放。氨氧化古菌(AOA)和氨氧化细菌(AOB)的氨氧化基因 amoA 的丰度对 N 和/或 K 施肥有响应,但反硝化基因 narG、nirK 和 norl 与 NO 排放强烈相关。这表明,N 或 K 肥及其相互作用主要通过改变土壤-植物系统中反硝化微生物功能基因的丰度来影响 NO 排放。在 N 和 K 的联合应用中,Paracoccus、Rubrivivax 和 Geobacter 以及 Streptomyces 和 Hyphomicrobium 等属在反硝化过程中对 NO 排放起着重要作用。