Microbial ammonium immobilization promoted soil nitrogen retention under high moisture conditions in intensively managed fluvo-aquic soils

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE Biology and Fertility of Soils Pub Date : 2024-05-14 DOI:10.1007/s00374-024-01831-y
Hui Wang, Zhifeng Yan, Zengming Chen, Xiaotong Song, Jinbo Zhang, Si-Liang Li, Christoph Müller, Xiaotang Ju, Xia Zhu-Barker
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Abstract

Quantifying the gross rates of individual nitrogen (N) processes is critical for understanding the availability, retention and loss of N and its eco-environmental impacts in agricultural ecosystems. Here, we carried out a 15N tracing study to quantify the influence of soil moisture on the gross rates of ten different N processes in two intensively managed fluvo-aquic soils. Results showed that the gross N mineralization rates were insensitive to changes in soil moisture, ranging from 40 to 120% water-filled pore space (WFPS). Contrarily, the gross ammonium (NH4+) immobilization rates increased exponentially with elevated soil moisture. Specifically, under high soil moisture conditions (i.e., 90–120%WFPS), the gross NH4+ immobilization rates (4.04 ± 0.83 and 0.88 ± 0.28 mg N kg− 1d− 1 for the two soils, respectively) were nearly four times higher than those under medium or low moisture conditions (i.e., 40–80%WFPS). Meanwhile, the high WFPS reduced the gross autotrophic nitrification rates (5.92 ± 2.15 and 12.31 ± 3.83 mg-N kg− 1d− 1 for the two soils, respectively) to only one-third to one-half of those that were observed under medium or low WFPS. By contrast, the rates of nitrate (NO3) immobilization increased in one soil whereas they decreased in another under high moisture conditions, and the other N processes (including heterotrophic nitrification and dissimilatory nitrate reduction to ammonium (DNRA)) were negligible throughout the different WFPS. Overall, our results suggest that under highly saturated conditions, the increase in microbial NH4+ immobilization and decrease in autotrophic nitrification are critical for N retention in the fluvo-aquic soils. These findings provide valuable insights into potential alterations in soil N retention or loss under future climate change scenarios, where more intensive irrigation and extreme rainfall events are anticipated.

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在高湿度条件下,微生物固定铵促进了集中管理的氟水土中的土壤固氮作用
量化各个氮(N)过程的总速率对于了解农业生态系统中氮(N)的可用性、保留和流失及其对生态环境的影响至关重要。在此,我们开展了一项 15N 追踪研究,以量化土壤水分对两种集中管理的氟水土中 10 种不同氮过程总速率的影响。结果表明,氮的总矿化率对土壤水分的变化不敏感,范围从 40% 到 120% 的充满水的孔隙空间(WFPS)不等。相反,铵(NH4+)总固定率随着土壤湿度的升高呈指数增长。具体来说,在高土壤湿度条件下(即 90-120% WFPS),两种土壤的 NH4+ 总固定率(分别为 4.04 ± 0.83 和 0.88 ± 0.28 mg N kg- 1d-1)比中或低湿度条件下(即 40-80%WFPS)高出近四倍。同时,高 WFPS 使总自养硝化率(两种土壤分别为 5.92 ± 2.15 和 12.31 ± 3.83 mg-N kg- 1d-1)降低到中或低 WFPS 条件下的三分之一到二分之一。相比之下,在高湿度条件下,一种土壤的硝酸盐(NO3-)固定化速率增加,而另一种土壤的固定化速率降低,其他氮过程(包括异养硝化和硝酸盐异养还原成铵(DNRA))在不同的 WFPS 条件下均可忽略不计。总之,我们的研究结果表明,在高饱和度条件下,微生物 NH4+ 固定化的增加和自养硝化作用的减少对于氟质土壤中的氮保持至关重要。在未来气候变化的情况下,预计会出现更密集的灌溉和极端降雨事件,这些发现为了解土壤氮保留或流失的潜在变化提供了宝贵的见解。
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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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