Effect of fulvic acid on aggregate characteristics and humus composition in saline-alkali soil

IF 3.9 2区 农林科学 Q1 AGRONOMY
Rui Cai, Yaru Guo, Yanjie Li, Ling Li, Susu Xu, Ping Gong, Pengfei Li, Hongguang Liu
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Abstract

Background and Aims

Organic amendments rich in fulvic acid (FA) offer a way to improve the water and salt distribution in saline-alkali soils and enhance soil quality. As soil humus promotes the formation of soil aggregates and improves soil quality, exploring the effects of FA on saline-alkali soil aggregates and humification is significant to understand the potential of fulvic acid in improving soil quality.

Methods

This study examines severely saline-alkali cotton fields in Xinjiang through a two-year field experiment (2021–2022) using five FA application rates (0, 150, 300, 450, and 600 kg·ha−1) and evaluates their effects on soil structure and humus fractions through structural equation modeling (SEM).

Results

FA application increased soil moisture by 6.16–18.64% and decreased salt content and pH by 4.07–20.87% and 0.57–1.90%, respectively, compared to standard fertilization. The application of FA improved soil aggregate stability, with optimization positively correlated to the amount applied. The soil humus components rose by 5.24–60.49%, and humification improved by 6.97–20.08%. Among them, the 600 kg·ha−1 application rate yielded the most significant effects Additionally, SEM revealed that soil physical and chemical properties (path coefficient = 0.436, p < 0.001) and humus components (path coefficient = 0.442, p < 0.001) in saline-alkali cotton fields had a direct positive impact on soil humification. Additionally, soil aggregates indirectly enhanced humification by influencing humus content and soil properties.

Conclusion

FA-mediated stabilization of soil aggregates, along with salt inhibition and improved soil moisture retention, enhances saline-alkali soil structure and accelerates humification. Therefore, the results provide technical and theoretical support for reducing nutrient loss and promoting sustainable management of saline-alkali soils.

黄腐酸对盐碱土团聚体特性和腐殖质组成的影响
背景与目的富富黄腐酸的有机改良剂为改善盐碱地的水盐分布、提高土壤质量提供了一条途径。土壤腐殖质促进土壤团聚体形成,改善土壤质量,探索FA对盐碱土壤团聚体和腐殖质化的影响,对了解黄腐酸改善土壤质量的潜力具有重要意义。方法以新疆重度盐碱棉为研究对象(2021-2022年),采用5种FA施用量(0、150、300、450和600 kg·ha−1),通过结构方程模型(SEM)评价其对土壤结构和腐殖质组分的影响。结果与标准施肥相比,施用fa可使土壤含水量提高6.16 ~ 18.64%,使含盐量和pH值分别降低4.07 ~ 20.87%和0.57 ~ 1.90%。施用FA改善了土壤团聚体稳定性,且优化程度与施用量呈正相关。土壤腐殖质组分增加5.24 ~ 60.49%,腐殖质化程度提高6.97 ~ 20.08%。其中,600 kg·ha−1施用量对土壤理化性质的影响最为显著。0.001)和腐殖质成分(通径系数= 0.442,p <;0.001)对土壤腐殖质化有直接的正向影响。此外,土壤团聚体通过影响腐殖质含量和土壤性质间接促进腐殖质化。结论fa介导的土壤团聚体稳定作用,以及抑盐作用和土壤保水作用,增强了盐碱土结构,加速了腐殖质化。研究结果为减少盐碱地养分流失,促进盐碱地可持续管理提供了技术和理论支持。
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来源期刊
Plant and Soil
Plant and Soil 农林科学-农艺学
CiteScore
8.20
自引率
8.20%
发文量
543
审稿时长
2.5 months
期刊介绍: Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and that enhance our mechanistic understanding of plant-soil interactions. We focus on the interface of plant biology and soil sciences, and seek those manuscripts with a strong mechanistic component which develop and test hypotheses aimed at understanding underlying mechanisms of plant-soil interactions. Manuscripts can include both fundamental and applied aspects of mineral nutrition, plant water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics, as long as they are hypothesis-driven and enhance our mechanistic understanding. Articles including a major molecular or modelling component also fall within the scope of the journal. All contributions appear in the English language, with consistent spelling, using either American or British English.
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