FeOx-Driven Soil Aggregation Boosts MAOC Accumulation and POC Protection in Subtropical Mixed Conifer–Broadleaf Forests

IF 3.8 2区 农林科学 Q2 SOIL SCIENCE
Zhengui Han, Yunchao Zhou, Yingli Guo, Han Liu, Qianbin Cao
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引用次数: 0

Abstract

The conversion of pure coniferous plantations to coniferous–broadleaf mixed forests increases the organic carbon (OC) content of soil and aggregates; however, the mechanisms of OC retention through soil aggregation remain inadequately understood. We selectively removed Fe oxides and OC from soil of both poorly aggregated (pure coniferous plantation) and well aggregated (mixed forest) soil systems. The mechanism of particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) sequestration in Fe oxide soil aggregation under broadleaf transformation was studied. The removal of Fe oxides broke the macroaggregates into microaggregates and < silt + clay fractions and revealed the attachment and entanglement effects of plant residues encapsulated by macroaggregates on soil particles, whereas plant residue decomposition maximised the degree of macroaggregate fragmentation (64.8%–100%). These results indicate that POC self-isolates and that the presence of Fe oxides further enhances POC physical occlusion during soil aggregation. The extent of this physical protection provided by Fe oxides follows the order: free Fe (FeD) > amorphous Fe (FeO) > complex Fe (FeP). Specifically, FeO and FeP promote macroaggregate formation through organic–inorganic complexes (MAOC formation) to enhance POC physical occlusion, whereas FeD predominantly forms inorganic–inorganic complexes. Microaggregate formation and MAOC accumulation occurred simultaneously through organic–inorganic interactions with various Fe oxide forms. These processes enhanced soil aggregation and were accompanied by significant accumulation of POC (80.2%–169.8%) and MAOC (41.1%–137.3%) after stand conversion (p < 0.05). These findings indicate that improved soil aggregation capacity mediated by Fe oxides during forest conversion promotes POC and MAOC accumulation through distinct Fe oxide-specific aggregation mechanisms.

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feox驱动的土壤团聚促进亚热带针叶林-阔叶林MAOC积累和POC保护
纯针叶人工林向针叶阔叶混交林的转变增加了土壤和团聚体的有机碳含量;然而,通过土壤团聚体保持有机碳的机制仍不充分了解。我们选择性地从低团聚(纯针叶林)和高团聚(混交林)土壤系统中去除氧化铁和有机碳。研究了阔叶转化条件下颗粒有机碳(POC)和矿物伴生有机碳(MAOC)在铁氧化物土壤团聚体中的固存机制。铁氧化物的去除将大团聚体分解为微团聚体和粉土+粘土组分,揭示了被大团聚体包裹的植物残体对土壤颗粒的附着和缠结作用,而植物残体分解使大团聚体破碎程度最大化(64.8% ~ 100%)。这些结果表明,POC具有自隔离作用,铁氧化物的存在进一步增强了POC在土壤团聚过程中的物理封闭。铁氧化物提供这种物理保护的程度顺序为:自由铁(FeD) >;非晶铁(FeO) >;络合物铁(FeP)。具体而言,FeO和FeP通过有机-无机配合物(MAOC)促进大聚集体的形成,从而增强POC的物理遮挡,而FeD主要形成无机-无机配合物。微团聚体的形成和MAOC的积累是通过与各种铁氧化物形式的有机-无机相互作用同时发生的。这些过程增强了土壤团聚性,并伴随着林分转换后POC(80.2% ~ 169.8%)和MAOC(41.1% ~ 137.3%)的显著积累(p < 0.05)。这些结果表明,森林转化过程中铁氧化物介导的土壤团聚能力的提高通过不同的铁氧化物聚集机制促进了POC和MAOC的积累。
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来源期刊
European Journal of Soil Science
European Journal of Soil Science 农林科学-土壤科学
CiteScore
8.20
自引率
4.80%
发文量
117
审稿时长
5 months
期刊介绍: The EJSS is an international journal that publishes outstanding papers in soil science that advance the theoretical and mechanistic understanding of physical, chemical and biological processes and their interactions in soils acting from molecular to continental scales in natural and managed environments.
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