Soil amendment and N fertilization strategies to improve C sequestration and storage in soil aggregates

Maria Gabriela de Oliveira Andrade, Carlos Felipe dos Santos Cordeiro, Juliano Carlos Calonego, Alan Franzluebbers, Ciro Antonio Rosolem
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Abstract

Management can affect soil quality through changes in carbon (C) stock, especially in protected C fractions of soil aggregates. Soil aggregation and C sequestration may be improved with soil correction (liming and gypsum) and nitrogen (N) fertilization, but it is not clear how these factors might interact to affect humic substances. The objective of the study was to evaluate the effects of calcium (Ca), magnesium (Mg), and N fertilizatilizer amendments on the accumulation of C, N, and humic substances in soil aggregates from an Oxisoil in Brazil. The production system was no-till soybean [Gycine max (L.) Merr.] double-cropped with maize (Zea mays L.) and intercropped with forage grass since 2016. Treatments were no amendment, lime only, and lime + phosphogypsum, factorially arranged with and without annual N fertilization of maize. Soil was collected at 0–10, 10–20, 20–40, and 40–60 cm 6 years after initiation of the experiment. The combination of lime, gypsum, and N led to 13% greater total C stock and 20% greater total N stock within the 0–60 cm soil profile than the control. Levels of fulvic acid (FA) and humic acid (HA) were similar among aggregate classes, but humin was greatest in larger aggregates. Liming plus N decreased FA and HA, but gypsum application mitigated this negative effect. Application of limestone, gypsum, and N increased humin, mainly in the soil surface (0–10 cm). Soil C storage and stabilization was enhanced in large soil aggregates with the combined use of lime, gypsum, and N fertilization in humid tropical soils.

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土壤改良和氮肥施用策略,提高土壤团聚体的固碳和储碳能力
管理可以通过碳(C)储量的变化影响土壤质量,尤其是土壤团聚体中受保护的 C 部分。土壤改良(石灰化和石膏)和氮(N)肥可以改善土壤团聚和固碳,但这些因素如何相互作用影响腐殖质还不清楚。本研究的目的是评估钙(Ca)、镁(Mg)和氮肥添加剂对巴西 Oxisoil 土壤团聚体中碳、氮和腐殖质积累的影响。生产系统为免耕大豆(Gycine max (L.) Merr)与玉米(Zea mays L.)复种,自 2016 年起与牧草间作。处理方式为不施肥、只施石灰和石灰+磷石膏,因地制宜地安排了每年对玉米施氮肥和不施氮肥。试验开始 6 年后,在 0-10 厘米、10-20 厘米、20-40 厘米和 40-60 厘米处采集土壤。与对照组相比,石灰、石膏和氮的组合使 0-60 厘米土壤剖面中的总碳储量增加了 13%,总氮储量增加了 20%。富勒酸(FA)和腐植酸(HA)的含量在不同等级的聚合体中相似,但腐殖质在较大的聚合体中含量最高。石灰化加氮降低了富里酸和腐殖酸的含量,但施用石膏减轻了这种负面影响。石灰石、石膏和氮的施用增加了腐殖质,主要是在土壤表面(0-10 厘米)。在潮湿的热带土壤中,结合使用石灰、石膏和氮肥,可以提高大的土壤团聚体中的土壤碳储存和稳定性。
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