Interaction between water, crop residue and fertilization management on the source-differentiated nitrogen uptake by rice

IF 5.1 1区 农林科学 Q1 SOIL SCIENCE
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Abstract

Alternate wetting and drying (AWD) is an effective water-saving practice for rice cultivation that may however promote nitrogen (N) losses compared to continuous flooding (CF). The interaction between water, crop residue and N fertilization management can influence the contribution of different N sources to plant uptake. We hypothesized that microbial processes driving the source-differentiated N supply for rice uptake during the early growth stages will depend on the interaction between water management, the timing of straw incorporation with respect to flooding and the temporal distribution of mineral N application. Rice was grown for 60 days in mesocosm experiment involving a factorial design with (i) two water regimes (CF vs. AWD) and (ii) three straw and fertilizer managements, during which soil N, porewater chemistry, plant growth and N uptake were evaluated. Source partitioning of plant N between fertilizer-, straw- and soil-derived N was achieved by means of a dual-stable isotope 15N tracing approach. Although AWD reduced total N uptake by about 4–25% with respect to CF, this could only be partly attributed to a lower uptake of fertilizer-N (and lower fertilizer-N use efficiency), suggesting that other N sources were affected by water management. Our findings evidence how the interaction between soil redox conditions and the availability of labile C and inorganic N strongly determined the supply of soil-derived N through microbial feedback and priming responses. Although incorporated straw contributed only minimally to rice N, it represented the primary driver controlling plant N nutrition through these microbial responses. These insights may contribute to identify suitable fertilization practices that favour plant N uptake during the early stages of rice growth under AWD.

水、作物残茬和施肥管理对水稻源差异摄氮的相互作用
摘要 干湿交替(AWD)是水稻种植的一种有效节水方法,但与连续淹水(CF)相比,可能会增加氮素(N)的损失。水、作物残留物和氮肥管理之间的相互作用会影响不同氮源对植物吸收的贡献。我们假设,在水稻生长早期阶段,驱动水稻吸收不同氮源供应的微生物过程将取决于水分管理、秸秆掺入与淹水的时间以及矿物氮施用的时间分布之间的相互作用。水稻在中型宇宙实验中生长了 60 天,该实验采用因子设计,包括 (i) 两种水分制度(CF 与 AWD)和 (ii) 三种秸秆和肥料管理,在此期间对土壤氮、孔隙水化学、植物生长和氮吸收进行了评估。通过双稳定同位素 15N 追踪方法,实现了植物氮在肥料、秸秆和土壤来源氮之间的来源分配。虽然 AWD 比 CF 降低了约 4-25% 的总氮吸收量,但这只能部分归因于肥料氮吸收量的降低(以及肥料氮利用效率的降低),这表明其他氮源也受到了水分管理的影响。我们的研究结果证明了土壤氧化还原条件与可溶性碳和无机氮的可用性之间的相互作用如何通过微生物反馈和引物反应有力地决定了土壤源氮的供应。虽然掺入的秸秆对水稻氮的贡献很小,但它是通过这些微生物反应控制植物氮营养的主要驱动力。这些见解可能有助于确定合适的施肥方法,以促进水稻在全灌溉条件下生长初期的植物氮吸收。
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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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