秸秆还田适度减少氮肥用量可调节草甸土壤的耕地功能和微生物性状

IF 5.8 2区 农林科学 Q1 SOIL SCIENCE
Soil Pub Date : 2024-11-05 DOI:10.5194/soil-10-779-2024
Yan Duan, Minghui Cao, Wenling Zhong, Yuming Wang, Zheng Ni, Mengxia Zhang, Jiangye Li, Yumei Li, Xianghai Meng, Lifang Wu
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引用次数: 0

摘要

摘要氮(N)肥因其对土壤肥力和生产力的益处而受到全世界的关注,但过量施氮也会导致一系列生态系统退化,如温室气体排放。一般认为,土壤微生物参与维护各种土壤功能。然而,不同氮肥施用量下土壤耕地性质与微生物性状之间的联系仍不确定。为了解决这个问题,我们在东北平原秸秆还田后的草甸土壤中进行了为期 4 年的原位田间试验,并结合常规磷(P)和钾(K)施肥进行了以下处理:(i) 常规氮肥(N + PK),(ii) 减施 25% 氮肥(0.75N + PK),(iii) 减施 50% 氮肥(0.5N + PK),(IV) 不施氮肥(PK)。耕地特性和微生物性状对不同氮肥施用量的反应各不相同。0.75N + PK 处理对土壤肥力、生产力、秸秆分解、微生物丰度和功能具有全面的积极影响,并减轻了温室效应。具体而言,土壤有机碳(SOC)、全氮、全磷含量、秸秆C、氮释放量、微生物生物量C、N含量、纤维素酶和N-乙酰-D-葡萄糖苷酶活性均显著高于0.5N + PK和PK,且无明显差异。温室气体排放量随着氮输入水平的降低而减少。此外,0.75N + PK 的秸秆生物量和产量最高,明显高于 0.5N + PK 和 PK。同时,0.75N + PK 能提高地上部生物量和土壤 C:N,从而提高纤维素降解酶基因的丰度,这可能意味着潜在的 C 和 N 转化能力。此外,观察到的大多数耕地性质变化都与微生物模块和关键类群密切相关。模块-1 群落中的 Lasiosphaeriaceae 与秸秆降解率以及碳和氮的释放呈显著正相关,而模块-3 群落中的 Terrimonas 与产量呈显著正相关,这有利于土壤多功能性的实现。因此,我们的研究结果表明,秸秆还田同时减少 25% 的化肥氮用量是实现土壤功能的最佳方案。本研究强调了非生物因素和生物因素在土壤健康中的重要性,并通过优化秸秆还田后草甸土壤的氮肥用量,支持绿色农业发展。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Moderate N fertilizer reduction with straw return modulates cropland functions and microbial traits in a meadow soil
Abstract. Nitrogen (N) fertilization has received worldwide attention due to its benefits with regard to soil fertility and productivity, but excess N application also causes an array of ecosystem degenerations, such as greenhouse gas emissions. Generally, soil microorganisms are considered to be involved in upholding a variety of soil functions. However, the linkages between soil cropland properties and microbial traits under different N fertilizer application rates remain uncertain. To address this, a 4-year in situ field experiment was conducted in a meadow soil from the Northeast China Plain after straw return with the following treatments combined with regular phosphorus (P) and potassium (K) fertilization: (i) regular N fertilizer (N + PK), (ii) 25 % N fertilizer reduction (0.75N + PK), (iii) 50 % N fertilizer reduction (0.5N + PK), and (IV) no N fertilizer (PK). Cropland properties and microbial traits responded distinctly to the different N fertilizer rates. Treatment 0.75N + PK had overall positive effects on soil fertility, productivity, straw decomposition, and microbial abundance and functioning and alleviated greenhouse effects. Specifically, no significant difference was observed in soil organic carbon (SOC), total N, P content, straw C, N release amounts, microbial biomass C, N content, and cellulase and N-acetyl-D-glucosaminidase activities, which were all significantly higher than in 0.5N + PK and PK. Greenhouse gas emissions was reduced with the decreasing N input levels. Moreover, the highest straw biomass and yield were measured in 0.75N + PK, which were significantly higher than in 0.5N + PK and PK. Meanwhile, 0.75N + PK up-regulated aboveground biomass and soil C:N and thus increased the abundance of genes encoding cellulose-degrading enzymes, which may imply the potential ability of C and N turnover. In addition, most observed changes in cropland properties were strongly associated with microbial modules and keystone taxa. The Lasiosphaeriaceae within the module-1 community showed significant positive correlations with straw degradation rate and C and N release, while the Terrimonas within the module-3 community showed a significant positive correlation with production, which was conducive to soil multifunctionality. Therefore, our results suggest that straw return with 25 % chemical N fertilizer reduction is optimal for achieving soil functions. This study highlights the importance of abiotic and biotic factors in soil health and supports green agricultural development by optimizing N fertilizer rates in meadow soil after straw return.
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来源期刊
Soil
Soil Agricultural and Biological Sciences-Soil Science
CiteScore
10.80
自引率
2.90%
发文量
44
审稿时长
30 weeks
期刊介绍: SOIL is an international scientific journal dedicated to the publication and discussion of high-quality research in the field of soil system sciences. SOIL is at the interface between the atmosphere, lithosphere, hydrosphere, and biosphere. SOIL publishes scientific research that contributes to understanding the soil system and its interaction with humans and the entire Earth system. The scope of the journal includes all topics that fall within the study of soil science as a discipline, with an emphasis on studies that integrate soil science with other sciences (hydrology, agronomy, socio-economics, health sciences, atmospheric sciences, etc.).
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