Liming enhances the abundance and stability of nitrogen-cycling microbes: the buffering effect of long-term lime application

IF 5.6 1区 农林科学 Q1 SOIL SCIENCE Biology and Fertility of Soils Pub Date : 2025-01-24 DOI:10.1007/s00374-025-01889-2
Akari Mitsuta, Késia Silva Lourenço, Jingjing Chang, Mart Ros, René Schils, Yoshitaka Uchida, Eiko Eurya Kuramae
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Abstract

Lime application (liming) has historically been used to ameliorate soil acidity in grasslands. Liming effectively improves soil pH, plant productivity, and soil physicochemical properties, but the long-term impact of acidity control by liming on key microbial nitrogen (N)-cycling genes in semi-natural grasslands is unknown. We investigated the effect of 65 years of liming on N-cycling processes in the limed and control plots of the Ossekampen long-term grassland experiment in the Netherlands. These plots have not received any other fertilizers for 65 years. Soil sampling and nitrous oxide (N2O) emission measurements were conducted three times in spring and four times in summer, and quantitative real-time PCR was performed to determine the absolute abundances of N-cycling genes, including ammonia-oxidation (amoA-AOB, amoA-AOA, amoA-comammox), denitrification (nirS, nirK, nosZ), nitrate ammonification (nrfA), and N-fixation (nifH) genes. Long-term liming increased the absolute abundances of nitrifiers, denitrifiers, and nitrate ammonifiers. Soil N2O emissions did not differ significantly between liming and control treatments. Additionally, liming had a buffering effect that maintained the population of N-cycling microbes against seasonal variations in abundance. Our results indicate that improving soil acidity through liming potentially facilitates microbial N-cycling processes without increasing N2O emissions.

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石灰增强了氮循环微生物的丰度和稳定性:长期施用石灰的缓冲作用
石灰施用(石灰化)历来用于改善草地土壤酸度。石灰能有效改善土壤pH值、植物生产力和土壤理化性质,但石灰控制酸度对半自然草地关键微生物氮循环基因的长期影响尚不清楚。摘要研究了荷兰奥塞坎本长期草地试验石灰样地和对照样地65年石灰化对氮循环过程的影响。这些地块65年来没有施用过任何其他肥料。在春季和夏季分别进行3次土壤采样和4次氧化亚氮(N2O)排放测量,并采用实时荧光定量PCR技术测定氮循环基因的绝对丰度,包括氨氧化基因(amoA-AOB、amoA-AOA、amoA-comammox)、反硝化基因(nirS、nirK、nosZ)、硝态氨化基因(nrfA)和固氮基因(nifH)。长期石灰化增加了硝化菌、反硝化菌和硝酸盐氨化菌的绝对丰度。土壤N2O排放量在石灰处理和对照处理之间无显著差异。此外,石灰还具有缓冲作用,使氮循环微生物的数量不受季节变化的影响。我们的研究结果表明,通过石灰化改善土壤酸度可能会促进微生物n -循环过程,而不会增加N2O排放。
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来源期刊
Biology and Fertility of Soils
Biology and Fertility of Soils 农林科学-土壤科学
CiteScore
11.80
自引率
10.80%
发文量
62
审稿时长
2.2 months
期刊介绍: Biology and Fertility of Soils publishes in English original papers, reviews and short communications on all fundamental and applied aspects of biology – microflora and microfauna - and fertility of soils. It offers a forum for research aimed at broadening the understanding of biological functions, processes and interactions in soils, particularly concerning the increasing demands of agriculture, deforestation and industrialization. The journal includes articles on techniques and methods that evaluate processes, biogeochemical interactions and ecological stresses, and sometimes presents special issues on relevant topics.
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