长期施用氮肥的秸秆还田提高了土壤孔隙结构、POM积累及其正反馈

IF 6.1 1区 农林科学 Q1 SOIL SCIENCE
Tianyu Ding , Zichun Guo , Wei Li , Xinhua Peng
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引用次数: 0

摘要

土壤孔隙结构通过影响水和气体的传输来决定颗粒有机物(POM)的分解。许多研究都报道了氮肥导致的 POM 积累。然而,氮肥和秸秆管理对 POM 和孔隙的影响以及这两个因素之间的关系仍无定论。因此,我们在一个椎体土壤上进行了一项为期 15 年(2008-2023 年)的氮肥田间试验,涵盖了小麦-玉米种植系统中的三种氮肥施用量(0、360 和 540 千克/公顷-年-1,分别称为 N0、N360 和 N540)和秸秆管理(秸秆还田和秸秆清除)。利用 X 射线计算机断层扫描(CT)对孔隙结构进行量化,并根据形态特征将 POM 分为新鲜 POM 和分解 POM。研究结果表明,在 N0、N360 和 N540 速率下,秸秆还田处理使新鲜 POM 增加了 3.08-3.77 倍,与秸秆清除相比,在 N540 速率下,基于图像的孔隙率(直径 50 μm,Ø)、连通孔隙率、连通概率均有所提高(P <0.05)。在秸秆还田条件下,与 N0 处理相比,N360 处理使新鲜 POM 显著增加了 2.3 倍;N540 处理使新鲜 POM 增加了 2.94 倍,分解 POM 增加了 1.16 倍(P <0.05)。N540 处理还增加了图像孔隙度、连通孔隙度、表面积密度、平均密实度,并减少了平均孔距(P < 0.05)。此外,在秸秆还田条件下,连通孔隙被确定为新鲜 POM 的主要分布区,分布比例为 26.9 %-77.9 %。值得注意的是,在秸秆还田处理条件下,POM 与 200 μm Ø 孔隙度呈正相关(P <0.05),而在秸秆去除条件下,POM 与孔隙结构之间无显著关系(P >0.05)。总之,我们的研究结果表明,长期氮肥施用(N360 和 N540)与秸秆还田相结合可促进 POM 的积累,尤其是新鲜 POM 的积累,并改善淤积土壤的孔隙结构。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long-term straw return with nitrogen fertilization enhances soil pore structure, POM accumulation, and their positive feedback in a Vertisol
Soil pore structure determines particulate organic matter (POM) decomposition by influencing water and gas transport. The accumulation of POM due to nitrogen (N) fertilization has been reported in many studies. However, the effects of N fertilization and straw management on POM and pores as well as the relationship between these two factors remain inconclusive. Therefore, a 15-year (2008–2023) N fertilization field experiment was conducted on a Vertisol, covering three N application rates (0, 360, and 540 kg ha−1 year−1, designated as N0, N360, and N540) and straw management (straw return and straw removal) in a wheat-maize cropping system. X-ray computed tomography (CT) was utilized to quantify the pore structure, and POM was classified into fresh POM and decomposed POM based on their morphological characteristics. The findings revealed that straw return treatment increased fresh POM by 3.08–3.77-fold at N0, N360 and N540 rates, along with enhancements in image-based porosity (>50 μm in diameter, Ø), connected porosity, connection probability at the N540 rate compared to straw removal (P < 0.05). Under straw return conditions, the N360 treatment notably increased fresh POM by 2.3-fold compared to the N0 treatment; the N540 treatment led to a 2.94-fold increase in fresh POM and a 1.16-fold increase in decomposed POM (P < 0.05). The N540 treatment also increased image-based porosity, connected porosity, surface area density, mean compactness, and decreased mean pore distance (P < 0.05). Furthermore, with straw return conditions, connected pores were identified as the primary site for fresh POM distribution, accounting for a distribution proportion of 26.9 %-77.9 %. Notably, POM exhibited a positive correlation with > 200 μm Ø porosity under straw return treatment (P < 0.05), whereas no significant relationship was observed between POM and pore structure under straw removal (P > 0.05). Overall, our findings indicate that long-term N fertilization (N360 and N540) coupled with straw return facilitates POM accumulation, particularly fresh POM, and enhances soil pore structure in Vertisol.
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来源期刊
Soil & Tillage Research
Soil & Tillage Research 农林科学-土壤科学
CiteScore
13.00
自引率
6.20%
发文量
266
审稿时长
5 months
期刊介绍: Soil & Tillage Research examines the physical, chemical and biological changes in the soil caused by tillage and field traffic. Manuscripts will be considered on aspects of soil science, physics, technology, mechanization and applied engineering for a sustainable balance among productivity, environmental quality and profitability. The following are examples of suitable topics within the scope of the journal of Soil and Tillage Research: The agricultural and biosystems engineering associated with tillage (including no-tillage, reduced-tillage and direct drilling), irrigation and drainage, crops and crop rotations, fertilization, rehabilitation of mine spoils and processes used to modify soils. Soil change effects on establishment and yield of crops, growth of plants and roots, structure and erosion of soil, cycling of carbon and nutrients, greenhouse gas emissions, leaching, runoff and other processes that affect environmental quality. Characterization or modeling of tillage and field traffic responses, soil, climate, or topographic effects, soil deformation processes, tillage tools, traction devices, energy requirements, economics, surface and subsurface water quality effects, tillage effects on weed, pest and disease control, and their interactions.
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