Duan Chun-Jian, Wan Song, Ye Gui-Ping, Fan Jian-Bo, Wang Quan-Cheng, He Ji-Zheng, Lin Yong-Xin
Cultivation Base of State Key Laboratory for Subtropical Mountain Ecology, Fuzhou 350007, China.
School of Geographical Sciences, Fujian Normal University, Fuzhou 350007, China.
Ying Yong Sheng Tai Xue Bao. 2021 Jun;32(6):2209-2216. doi: 10.13287/j.1001-9332.202106.033.
The abundance of denitrifying functional genes plays a key role in driving the soil nitrous oxide (NO) emission potential. Nitrite reductase genes ( and ) and nitrous oxide reductase genes ( and ) are the dominant denitrifying funtional genes. In this study, real-time quantitative PCR was conducted to evaluate the effects of 32-year imbalanced fertilization and lime and gypsum additions on the abundances of , , and genes in an Ultisol at Yingtan, Jiangxi Province. We further explored the underlying driving factors The results showed that, compared with the balanced fertilization treatment, fertilization without phosphorus (P) signifi-cantly decreased the abundances of , , and genes. Fertilization without nitrogen (N) significantly reduced the abundances of , and , but did not affect the abundance of . Fertilization without potassium (K) did not affect the abundances of all denitri-fying functional genes. Results of stepwise regression analysis and random forest analysis showed that soil pH was a key environmental factor affecting the abundances of and . The application of lime or lime + gypsum significantly increased soil pH, which subsequently increased the abundances of and / by 150%-231% and 127%-155%, respectively. Our results suggested that application of lime or lime + gypsum favored more than in upland Ultisols, which might enhance the relative importance of in NO reduction. Overall, fertilization without P would reduce denitrifying gene abundances, while the application of lime or lime + gypsum enriched and increased ratio of , which might be beneficial for reducing NO emission potential in the Ultisols.
反硝化功能基因的丰度在驱动土壤一氧化二氮(N₂O)排放潜力方面起着关键作用。亚硝酸还原酶基因(nirS和nirK)和一氧化二氮还原酶基因(nosZⅠ和nosZⅡ)是主要的反硝化功能基因。在本研究中,采用实时定量PCR技术评估了32年不平衡施肥以及添加石灰和石膏对江西鹰潭一个老成土中nirS、nirK、nosZⅠ和nosZⅡ基因丰度的影响。我们进一步探究了潜在的驱动因素。结果表明,与平衡施肥处理相比,不施磷(P)显著降低了nirS、nirK、nosZⅠ和nosZⅡ基因的丰度。不施氮(N)显著降低了nirS、nirK和nosZⅡ的丰度,但对nosZⅠ的丰度没有影响。不施钾(K)对所有反硝化功能基因的丰度均无影响。逐步回归分析和随机森林分析结果表明,土壤pH是影响nirS和nosZⅡ丰度的关键环境因素。施用石灰或石灰+石膏显著提高了土壤pH,随后nirS和nosZⅠ/nosZⅡ的丰度分别增加了150% - 231%和127% - 155%。我们的结果表明,在旱地老成土中,施用石灰或石灰+石膏对nirS的促进作用大于nosZⅠ,这可能会增强nirS在N₂O还原中的相对重要性。总体而言,不施P会降低反硝化基因丰度,而施用石灰或石灰+石膏会富集nirS并提高nosZⅠ/nosZⅡ的比例,这可能有利于降低老成土中的N₂O排放潜力。