The divergent response of fungal and bacterial necromass carbon in soil aggregates under biochar amendment in paddy soil

IF 4.1 2区 农林科学 Q1 AGRONOMY Plant and Soil Pub Date : 2025-01-24 DOI:10.1007/s11104-025-07228-6
Mengtao Zhu, Zhiwei Liu, Qi Yi, Ruiling Ma, Man Xu, Kaiyue Song, Rongjun Bian, Jufeng Zheng, Xuhui Zhang
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Abstract

Background and aims

Microbial necromass carbon (C) significantly contributes to soil organic carbon (SOC) sequestration. However, there is limited information on how biochar amendment affects the accumulation and allocation of microbial necromass C in soil aggregates in paddy soil remains scarce, particularly with regard to changes in microbial life strategies.

Methods

From a 2-year field experiment, topsoil samples with biochar (C15) and without biochar amendment (C0) treatments were collected and fractionated into macroaggregate (2000–250 μm), microaggregate (250–53 μm), and silt–clay (< 53 μm) fractions. We investigated the impact of maize straw-derived biochar amendment on microbial community structure, SOC, and microbial necromass C in paddy soil aggregates.

Results

Biochar amendment significantly increased SOC and microbial biomass C but reduced microbial necromass C concentration. The microbial community shifted towards K-strategists under biochar amendment. Compared with the C0 treatment, total necromass C concentration in the C15 treatment decreased by 14.9% in the bulk soil, primarily due to reductions in fungal and bacterial necromass C concentrations of 14.7% and 16.1%, respectively. The decrease in total necromass C was primarily observed in macroaggregate and microaggregate. Specially, fungal necromass C primarily decreased in macroaggregate, while bacterial necromass C decreased in microaggregate. Biochar amendment did not significantly reduce microbial necromass C in silt–clay fraction, indicating its greater stabilization due to strong binding with soil minerals under biochar amendment, thereby protects it from microbial decomposition.

Conclusions

The results offer new insights into the role of soil aggregates in microbial-mediated SOC sequestration following biochar amendment in paddy soil.

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生物炭改良水稻土土壤团聚体中真菌和细菌坏死团碳的差异响应
背景与目的微生物坏死物碳(C)对土壤有机碳(SOC)的固存起着重要作用。然而,关于生物炭改性如何影响水稻土土壤团聚体中微生物死亡物质C的积累和分配的信息仍然有限,特别是关于微生物生命策略的变化。方法通过2年的田间试验,收集了经过生物炭(C15)和未经过生物炭改性(C0)处理的表土样品,并将其分馏为大团聚体(2000 ~ 250 μm)、微团聚体(250 ~ 53 μm)和粉砂粘土(53 μm)组分。研究了玉米秸秆生物炭对水稻土团聚体微生物群落结构、有机碳和微生物坏死物C的影响。结果生物炭改性显著提高了土壤有机碳和微生物生物量C,降低了微生物坏死块C浓度。生物炭处理下微生物群落向k -战略型转变。与C0处理相比,C15处理块状土壤中总坏死团C浓度下降了14.9%,主要原因是真菌和细菌坏死团C浓度分别下降了14.7%和16.1%。总坏死团C的减少主要见于大聚集体和微聚集体。特别是,真菌坏死团C主要在大聚集体中减少,而细菌坏死团C在微聚集体中减少。生物炭对粉质粘土组分中微生物坏死团C的降低不显著,说明在生物炭的作用下,粉质粘土组分与土壤矿物质结合较强,具有较强的稳定性,从而保护其不被微生物分解。结论土壤团聚体在水稻土生物炭改良后微生物介导的有机碳固存中的作用有了新的认识。
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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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