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Effects of nitrogen deposition rates and frequencies on the abundance of soil nitrogen-related functional genes in temperate grassland of northern China

机译:氮沉降速率和频率对北方温带草原土壤氮相关功能基因丰度的影响

摘要

Microbial processes driving nitrogen (N) cycling are hot topics in terms of increasing N deposition. Abundances of N-related functional genes (NFG) can be most responsive to N deposition and commonly used to represent N transformation rates. However, empirically simulated N deposition has been exclusively conducted through large and infrequent N fertilization, which may have caused contrasting effects on NFGs. Therefore, experiments with small and frequent N additions closed to natural deposition are necessary. Independently manipulated N addition rates (i.e., 0, 5, 10, 15, 20, and 50 g N m(-2) year(-1)) and two frequencies (2 times per year addition as conventional large and infrequent N fertilization (2 N), and 12 times per year addition simulating small and frequent N deposition (12 N), respectively) were conducted in a long-term field experiment of a semiarid grassland in northern China. Quantification analysis using real-time PCR were carried out for NFGs, including nifH for N fixation, chiA for N mineralization, archaeal (AOA) and bacterial (AOB) amoA for nitrification, and narG, nirS, nirK, and nosZ for denitrification. NFG abundances showed distinct sensitivities to N addition rates. The nifH, AOA-amoA, nirS, and nosZ gene abundances increased due to improved available N at low N rates, but suppressed by salt toxicity and acidification at high N rates. Large changes of chiA and AOB-amoA gene abundances highlighted their great sensitivities to the N enrichment. The abundance of AOB-amoA was more sensitive to N addition than AOA-amoA, but AOA-amoA dominated in absolute numbers and they predominated the ammonia-oxidation under different conditions. The N addition frequencies caused significant lower gene abundances of nifH, nirS, and nosZ under the 2-N frequency due to stronger suppression of acidification and salt toxicity and resulted in significant higher AOB-amoA gene abundances in response to higher N availability under the 2-N frequency. The NFGs abundances responded to N addition rates distinctly, highlighting that the driven processes involved in N cycling were altered by the N addition rates. The different effects of two N addition frequencies on NFG abundances demonstrated that conventional large and infrequent N fertilization cannot represent N deposition, and small and frequent N addition should be employed to project the effects of N deposition on microbial functional groups as well as on N transformations.
机译:就增加氮沉积而言,驱动氮(N)循环的微生物过程是热门话题。 N相关功能基因(NFG)的丰度可能对N沉积最敏感,通常用于表示N转化率。但是,经验性模拟的氮沉积仅通过大量且不频繁的氮肥施肥来进行,这可能对NFG产生了对比作用。因此,需要进行少量且频繁的N添加以接近自然沉积的实验。独立操作的氮添加量(即0、5、10、15、20和50 g N m(-2)年(-1))和两种频率(每年添加2次,是常规的大氮肥和少氮肥的施用量)在中国北方半干旱草原的长期田间试验中,分别进行了2 N)和每年12次的添加,分别模拟了少量和频繁的N沉积(分别为12 N)。使用实时PCR对NFG进行了定量分析,包括用于固氮的nifH,用于氮矿化的chiA,用于硝化的古细菌(AOA)和细菌(AOB)amoA以及用于反硝化的narG,nirS,nirK和nosZ。 NFG的丰度显示出对氮添加速率的不同敏感性。 nifH,AOA-amoA,nirS和nosZ基因的丰度由于在低氮水平下有效氮的提高而增加,但在高氮水平下被盐毒性和酸化所抑制。 chiA和AOB-amoA基因丰度的巨大变化突出了它们对N富集的高度敏感性。 AOB-amoA的丰度比AOA-amoA对N的添加更为敏感,但是AOA-amoA在绝对数上占主导地位,并且它们在不同条件下占主导地位。在2-N频率下,N的添加频率导致nifH,nirS和nosZ的基因丰度显着较低,这是由于更强的酸化和盐毒性抑制作用,并且在2下,由于较高的N利用率,导致AOB-amoA基因的丰度显着较高。 -N频率。 NFGs的丰度对氮的添加率有明显的响应,这表明氮的添加率改变了参与氮循环的驱动过程。两个不同的氮添加频率对NFG丰度的不同影响表明,常规的大量施氮和不频繁施氮不能代表氮的沉积,应采用少量和频繁的氮添加来预测氮沉积对微生物官能团以及氮转化的影响。 。

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