经 20 年施肥处理的超土壤土壤团粒中有机碳保存的驱动因素

IF 3.4 3区 农林科学 Q2 ENVIRONMENTAL SCIENCES
Peidong Xu, Rundong Wang, Likai Yi
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引用次数: 0

摘要

目的:土壤团聚体对土壤结构和有机碳(OC)保存至关重要。施肥是提高作物产量和有机碳储存的有效模式。本研究旨在探讨土壤团聚体中施肥诱导有机碳保存的驱动因素。研究方法从一个经过二十年不施肥(CK)、化肥(CF)和有机肥(OF)处理的超土壤中获得了 LM(大型团聚体,> 2 mm)、SM(小型团聚体,0.25-2 mm)和 MI(微型团聚体,< 0.25 mm)土壤团聚体。研究了每种集料的集料质量比例、OC 成分和铁/铝氧化物,以评估它们在集料相关 OC 保存中的作用。结果发现CF仅使LM中的OC含量(g kg- 1土壤)提高了27.4%,OF使所有集料中的OC含量提高了14.2%-60.8%。施肥有利于形成大粒径团聚体,促进土壤团聚体的稳定。在每个团聚体中,可溶性和难溶性 OC 的浓度(g kg- 1 团聚体)顺序为 OF > CF > CK。施肥,尤其是 OF,显著提高了螯合铁和氧化铝的浓度(g kg- 1),提高幅度在 5.9-117.6% 之间。在每个土壤团聚体中,团聚体的质量比例、OC 成分和铁/铝氧化物对 OC 的保存起着不同的作用。此外,在所有土壤团聚体中,OC 的保存主要由难降解 OC 控制。结论施肥促进了 OC 的保存,而这主要是由 Ultisol 土壤团聚体中的难降解 OC 驱动的。这项研究从机理上揭示了长期化学肥料和有机肥料作用下土壤团聚体中 OC 的保存机理。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Drivers of Organic Carbon Preservation Within Soil Aggregates from An Ultisol Treated with Twenty-Year Fertilizations

Drivers of Organic Carbon Preservation Within Soil Aggregates from An Ultisol Treated with Twenty-Year Fertilizations

Purpose: Soil aggregates are crucial for soil structure and organic carbon (OC) preservation. Fertilizations are an efficient pattern to improve crop productivity and OC storage. This study aimed to explore the driving factors regulating fertilization-induced OC conservation within soil aggregates. Methods: Soil aggregates of LM (large macro-aggregates, > 2 mm), SM (small macro-aggregates, 0.25–2 mm), and MI (micro-aggregates, < 0.25 mm) were obtained from an Ultisol treated with twenty-year no (CK), chemical (CF), and organic (OF) fertilizations. Aggregate mass proportions, OC components, and iron/aluminum oxides of each aggregate were investigated to evaluate their roles in aggregate-associated OC preservation. Results: The CF only enhanced the OC content (g kg− 1 soil) in LM by 27.4%, and the OF increased the OC contents in all aggregates by 14.2-60.8%. The fertilizations were conducive to the formation of large-size aggregates and the stimulation of soil aggregate stabilization. The order OF > CF > CK was observed in the concentrations (g kg− 1 aggregate) of labile and recalcitrant OC within each aggregate. The fertilizations, particularly the OF, significantly improved the concentrations (g kg− 1 aggregate) of chelated iron and aluminum oxides by 5.9-117.6%. The aggregate mass proportions, OC components, and iron/aluminum oxides displayed various roles in the OC preservation within every individual soil aggregate. Furthermore, the OC conservation was dominantly controlled by the recalcitrant OC within all soil aggregates. Conclusions: Fertilizations stimulated the OC preservation mostly driven by the recalcitrant OC within soil aggregates from an Ultisol. This study provided a mechanistic understanding of OC preservation within soil aggregates under long-term chemical and organic fertilizations.

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来源期刊
Journal of Soil Science and Plant Nutrition
Journal of Soil Science and Plant Nutrition Agricultural and Biological Sciences-Soil Science
CiteScore
5.90
自引率
10.30%
发文量
331
审稿时长
9 months
期刊介绍: The Journal of Soil Science and Plant Nutrition is an international, peer reviewed journal devoted to publishing original research findings in the areas of soil science, plant nutrition, agriculture and environmental science. Soil sciences submissions may cover physics, chemistry, biology, microbiology, mineralogy, ecology, pedology, soil classification and amelioration. Plant nutrition and agriculture submissions may include plant production, physiology and metabolism of plants, plant ecology, diversity and sustainability of agricultural systems, organic and inorganic fertilization in relation to their impact on yields, quality of plants and ecological systems, and agroecosystems studies. Submissions covering soil degradation, environmental pollution, nature conservation, and environmental protection are also welcome. The journal considers for publication original research articles, technical notes, short communication, and reviews (both voluntary and by invitation), and letters to the editor.
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