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Microbial traits mediate the functional components of soil organic carbon under long-term fertilization 微生物性状对长期施肥条件下土壤有机碳功能成分的调节作用
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-13 DOI: 10.1016/j.apsoil.2026.106798
Yanhong Yuan , Jiachang Zhang , Zhanrong Feng , Qi Zhang , Zihan Zhao , Qiang Li , Shuiqing Zhang , Gehong Wei , Xinhui Han , Minggang Xu , Andong Cai , Chengjie Ren
Microbial physiological traits are key determinants of soil organic carbon (SOC) accumulation under long-term fertilization, yet their adaptability to carbon (C) and nutrient gradients, and the corresponding C feedback effects, remain largely unexplored. Here, we conducted a 33-year field experiment with mineral and mineral-organic combined fertilization (NPKM) across two contrasting soil types (nutrient-rich vs. nutrient-poor). The 18O-H2O tracer method and amino sugar biomarker approaches were used to explore the trends of microbial C use efficiency (CUE) and microbial C pump efficacy (MCP), while metagenomic analysis and environmental variables were integrated to clarify the intrinsic and extrinsic effects of long-term fertilization on these microbial traits. Our results revealed divergent responses of SOC fractions to NPKM across soil types: relative to the control (CK), NPKM increased particulate organic carbon (POC) by 130% in nutrient-rich soils, the 33.46% rise in mineral-associated organic carbon (MAOC); in contrast, only MAOC exhibited a significant increase (80.86%) in nutrient-poor soils. Further analysis confirmed that microbial physiological traits drove the changes in POC and MAOC depending on soil nutrient status under long-term fertilization. Specifically, in nutrient-poor soils, NPKM enhanced MAOC by increasing CUE (100%) and MCP (45.34%), an effect mediated by C-degradation functional genes. In nutrient-rich soils, NPKM promoted POC by improving CUE (48.48%), a process regulated by abiotic factors. These findings highlight that initial nutrient levels regulate microbial physiological traits, thereby dictating the accumulation dynamics of different C fractions, which offers a theoretical basis for targeted agricultural C management strategies.
微生物生理性状是长期施肥条件下土壤有机碳(SOC)积累的关键决定因素,但其对碳(C)和养分梯度的适应性以及相应的碳反馈效应尚未得到充分研究。在这里,我们在两种不同土壤类型(富营养型和贫营养型)上进行了为期33年的矿物和矿物-有机联合施肥(NPKM)的田间试验。采用18O-H2O示踪法和氨基糖生物标志物方法探讨了微生物C利用效率(CUE)和微生物C泵效率(MCP)的变化趋势,并结合宏基因组分析和环境变量,阐明了长期施肥对这些微生物性状的内在和外在影响。结果表明,不同土壤类型土壤有机碳组分对NPKM的响应存在差异:相对于对照(CK), NPKM使营养丰富的土壤颗粒有机碳(POC)增加了130%,矿物相关有机碳(MAOC)增加了33.46%;相反,在养分贫乏的土壤中,只有MAOC显著增加(80.86%)。进一步分析证实,长期施肥条件下,微生物生理性状驱动土壤POC和MAOC的变化,这取决于土壤养分状况。具体而言,在营养贫乏的土壤中,NPKM通过提高CUE(100%)和MCP(45.34%)来提高MAOC,这是由c降解功能基因介导的。在营养丰富的土壤中,NPKM通过提高CUE(48.48%)促进POC,这一过程受非生物因子的调控。这些研究结果表明,初始营养水平调节微生物生理性状,从而决定不同组分C的积累动态,为针对性的农业C管理策略提供理论依据。
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引用次数: 0
Soil amendment with biomass-derived carbon dots enhances rhizosphere organic matter, nutrient turnover, and microbial metabolism for maize growth 生物质碳点土壤改良提高了玉米根际有机质、养分周转和微生物代谢
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-13 DOI: 10.1016/j.apsoil.2026.106804
Yadong Li , Qianying Han , Lihaonan Chen , Shang Lei , Congli Ma , Hongjie Wang
Soil degradation necessitates reducing the application of agrochemicals, while advancements in nanotechnology present growing opportunities in agriculture. Herein, this study synthesized a calcium- and nitrogen-co-doped carbon dots (Ca,N-CDs) with a high yield of 79.97% using the biomass of a submerged plant Potamogeton crispus. The soil application of Ca,N-CDs (100 mg/kg) significantly enhanced the growth (7.27–71.69%), photosynthesis, and antioxidant activity (29.49–173.20%) of maize (Zea mays L.). In the rhizosphere microenvironment, the application of Ca,N-CDs enhanced soil pH and the turnover of organic matter and nutrients (nitrogen and phosphorus) by regulating related soil enzyme activities. Metagenome analysis revealed that Ca,N-CDs enhanced the diversity and evenness of the rhizosphere microbial community, particularly increasing the abundance of archaea, eukaryotes, and some beneficial bacterial groups (Actinomycetes, Longimicrobia, and Micrococcales). KEGG functional analysis, combined with metabolomics analysis, demonstrated that the microbial metabolic processes related to growth and reproduction were significantly enhanced by Ca,N-CDs. Changes in microbial communities and metabolism showed positive correlations with soil properties. Co-occurrence network analysis indicated that Ca,N-CDs changed the dominant microorganisms in the maize rhizosphere and strengthened their associations among themselves and with soil properties. The rhizosphere responses synergistically promoted the maize growth and development. These findings present a promising alternative for improving soil health and fertility as well as promoting sustainable agricultural production.
土壤退化需要减少农用化学品的应用,而纳米技术的进步为农业提供了越来越多的机会。本研究利用沉水植物马铃薯(Potamogeton crispus)的生物量合成了钙氮共掺杂碳点(Ca,N-CDs),产率高达79.97%。土壤施钙、氮镉(100 mg/kg)显著提高了玉米(Zea mays L.)的生长(7.27 ~ 71.69%)、光合作用和抗氧化活性(29.49 ~ 173.20%)。在根际微环境中,Ca、N-CDs的施用通过调节土壤相关酶活性,提高了土壤pH值,促进了有机质和养分(氮、磷)的周转。宏基因组分析表明,Ca,N-CDs增强了根际微生物群落的多样性和均匀性,特别是增加了古细菌,真核生物和一些有益细菌群(放线菌,长微生物和微球菌)的丰度。KEGG功能分析结合代谢组学分析表明,Ca、N-CDs显著增强了与生长和繁殖相关的微生物代谢过程。微生物群落和代谢的变化与土壤性质呈正相关。共现网络分析表明,Ca、N-CDs改变了玉米根际的优势微生物,加强了它们之间的相互联系和与土壤性质的联系。根际反应协同促进玉米生长发育。这些发现为改善土壤健康和肥力以及促进可持续农业生产提供了一个有希望的替代方案。
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引用次数: 0
Biological and mineral amendments synergistically coordinate soil micro-food web to enhance multifunctionality 生物和矿物改良剂协同协调土壤微食物网,增强多功能性
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-13 DOI: 10.1016/j.apsoil.2025.106748
Baijing Zhu , Huaxiu Chen , Han Li , Qiang Zhu , Wenfeng Tan , Jiao Feng , Yu-Rong Liu
Multiple trophic groups in soil food web drive various ecosystem functions. However, it remains unclear how multitrophic interactions and associated multifunctionality respond to integrated agricultural management practices, especially the combination of mineral and biological amendments. Here, we conducted multifactor interactive experiment to explore how essential biological (microbial inoculants), mineral (fly ash addition), organic amendment, and tillage type (conventional tillage vs. deep tillage) influence soil micro-food web structure and soil multifunctionality. Our results showed that microbial inoculants and fly ash addition significantly influenced the structure of soil micro-food web and enhanced soil multifunctionality, while organic amendment and deep tillage had no significant effects. Specifically, microbial inoculants improved soil structural stability, reduced the proportion of fungal plant pathogens while enhancing the complexity of soil micro-food web. In contrast, fly ash increased soil nutrients and the relative abundance of predatory protists, and strengthened the relationship between soil food web complexity and multifunctionality. Notably, the combined application of microbial inoculants and fly ash exerted synergistic effects on both food web complexity and multifunctionality (increased by 14.6–15.7 %). These synergies were achieved predominantly by improving soil physical structure and nutrient levels, along with a reduced proportion of harmful microbes and an increase in higher trophic-level soil organisms. Overall, our findings highlight the potential of integrating biological and mineral amendments as a synergistic management strategy to enhance soil multi-trophic complexity and multifunctionality, thereby providing a novel theoretical basis for optimizing diversified soil management practices to improve soil health and support sustainable agriculture.
土壤食物网中的多种营养类群驱动着不同的生态系统功能。然而,目前尚不清楚多营养相互作用和相关的多功能性如何响应综合农业管理措施,特别是矿物和生物修正的结合。在这里,我们进行了多因素交互实验,以探索必要的生物(微生物接种剂)、矿物(粉煤灰添加)、有机改进剂和耕作方式(常规耕作与深耕)对土壤微食物网结构和土壤多功能性的影响。结果表明,微生物接种剂和粉煤灰添加显著影响土壤微食物网结构,增强土壤多功能性,而有机改良剂和深耕对土壤多功能性无显著影响。具体而言,微生物接种剂改善了土壤结构稳定性,降低了真菌植物病原体的比例,同时提高了土壤微食物网的复杂性。相反,粉煤灰增加了土壤养分和掠食性原生生物的相对丰度,加强了土壤食物网复杂性和多功能性之间的关系。值得注意的是,微生物接种剂和粉煤灰的联合应用对食物网的复杂性和多功能性都产生了协同效应(提高了14.6 - 15.7%)。这些协同作用主要是通过改善土壤物理结构和营养水平,减少有害微生物的比例和增加高营养水平的土壤生物来实现的。总的来说,我们的研究结果强调了生物和矿物修正作为一种协同管理策略的潜力,以提高土壤的多营养复杂性和多功能性,从而为优化多样化的土壤管理实践提供了新的理论基础,以改善土壤健康和支持可持续农业。
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引用次数: 0
Plant-derived biochars ameliorate acidity and reshape microbial communities to enhance tea productivity and quality in acidic soils 植物来源的生物炭改善酸性和重塑微生物群落,以提高酸性土壤的茶叶产量和质量
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-12 DOI: 10.1016/j.apsoil.2026.106805
Zhangtao Li , Yu Pan , Jun Meng , Meiqi Zhao , Zhiyuan Yao , Minjun Hu , Shengdao Shan , Huaihai Chen
Chronic over-acidification (pH < 4.5) of tea garden soils induces nutrient depletion, aluminum toxicity, and suppressed microbial diversity, threatening tea productivity. To address this, we evaluated the efficacy of three plant-derived biochars (corn straw, rice straw, and bamboo; applied at 45 t·ha−1) in ameliorating soil acidity and its associated negative impacts on soil fertility, microbial communities, and plant health. Biochar application significantly increased soil pH by 0.8–1.2 units and reduced exchangeable aluminum and hydrogen by 40–79%. The effects were feedstock-dependent as corn- and rice-straw biochars enhanced nutrient availability, whereas bamboo biochar more effectively decreased the availability of certain metals. Consequently, biochar reshaped soil microbial communities, increasing bacterial and fungal diversity by 35–129% and driving taxonomic shifts, notably elevating the abundances of Bacteroidota, Verrucomicrobiota, and Tremellomycetes with significant declines in Proteobacteria, Eurotiomycetes, and Leotiomycetes. Structural equation modeling identified soil pH and nutrients as primary regulators of microbial diversity, with metal availability exerting selective pressure on fungi. These improvements led to agronomic benefits, with fresh leaf yields increasing by 13–22%. Corn-straw biochar performed the best, yielding the highest production alongside improved quality (e.g., polyphenols and free amino acids). Our findings demonstrate that selecting appropriate biochar feedstocks can effectively ameliorate soil acidity, reshape microbial communities, and enhance tea productivity and quality, providing a targeted strategy for sustainable soil management in acidic tea gardens.
茶园土壤长期过度酸化(pH < 4.5)导致养分耗竭、铝毒性和微生物多样性抑制,威胁茶叶生产力。为了解决这个问题,我们评估了三种植物来源的生物炭(玉米秸秆、稻草秸秆和竹子;施用量为45 t·ha - 1)在改善土壤酸度及其对土壤肥力、微生物群落和植物健康的负面影响方面的功效。施用生物炭可显著提高土壤pH值0.8 ~ 1.2个单位,降低交换性铝和氢40 ~ 79%。这种效应依赖于原料,玉米和水稻秸秆生物炭提高了养分有效性,而竹子生物炭更有效地降低了某些金属的有效性。因此,生物炭重塑了土壤微生物群落,使细菌和真菌多样性增加了35-129%,并推动了分类变化,特别是杆菌门、疣菌门和银耳菌门的丰度增加,而变形菌门、eurotiomyctes和leotiomyctes的丰度显著下降。结构方程模型确定土壤pH值和养分是微生物多样性的主要调节因子,金属有效性对真菌施加选择压力。这些改良带来了农艺效益,鲜叶产量提高了13-22%。玉米秸秆生物炭表现最好,产量最高,质量也有所提高(如多酚和游离氨基酸)。研究结果表明,选择合适的生物炭原料可以有效改善土壤酸度,重塑微生物群落,提高茶叶产量和品质,为酸性茶园土壤可持续管理提供了有针对性的策略。
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引用次数: 0
Solid and liquid fractions of digestate: manure or slurry just like any others? 消化液的固体和液体部分:粪肥还是泥浆?
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-12 DOI: 10.1016/j.apsoil.2026.106788
Florian Vautrin , Mario Cannavacciuolo , Camille Chauvin , Pascal Piveteau , Pierre Barré , Cécile Villenave , Daniel Cluzeau , Kevin Hoeffner , Pierre Mulliez , Vincent Jean-Baptiste , Gregory Vrignaud , Aurélien Cottin , Julie Tripied , Samuel Dequiedt , Pierre-Alain Maron , Lionel Ranjard , Sophie Sadet-Bourgeteau
Biogas digestates are increasingly used as organic fertilizers. However, their impact on soil microbiota quality remains debated. Indeed, little is known about soil microbial communities responses to a given digestate depending on i) the fraction applied – whole (FYM_WD), liquid (FYM_LD), or solid (FYM_SD) – and/or ii) the physicochemical properties of the receiving soil. In a 42-day microcosm experiment, we applied different fractions of a same digestate to three soils with contrasting physicochemical and climatic characteristics and compared their effects on the abundance and diversity of the soil microbial communities. The experiment also included four additional treatments: cattle manure (CM), cattle slurry (CS), a mineral fertilizer, and an unfertilized control. Forty-two days after application, a significant ‘treatment’ effect was observed on soil microbial indicators for the two coarser-textured soils (P < 0.05). In the sandy loam-textured soil, FYM_SD resulted in a 40 % greater soil microbial biomass than FYM_WD or FYM_LD (P = 0.05). The effect of FYM_SD on soil microbial biomass was equivalent to that of CM or CS (P > 0.05), whereas the effect of FYM_LD more closely resembled that of CS. Moreover, FYM_SD input resulted in a significantly different prokaryotic community structure compared to FYM_LD-fertilized soil, but was equivalent to that of the CM-fertilized soil (P > 0.05). In the loam-textured soil, FYM_SD input resulted in a 20 % lower prokaryotic richness than FYM_LD. Similarly, the fungal community structure was affected the digestate fraction (P = 0.04), and the effects of FYM_SD and CM on fungal community structure were comparable (P > 0.05). Overall, these results demonstrate that digestate fraction influence soil microbial communities in a soil-type dependent manner.
沼气池越来越多地被用作有机肥料。然而,它们对土壤微生物群质量的影响仍存在争议。事实上,我们对土壤微生物群落对特定消化物的反应知之甚少,这取决于i)施用的组分——整体(FYM_WD)、液体(FYM_LD)或固体(FYM_SD)——和/或ii)接收土壤的物理化学性质。在为期42天的微观环境试验中,我们将同一消化物的不同组分施用于3种理化和气候特征截然不同的土壤中,比较了它们对土壤微生物群落丰度和多样性的影响。试验还包括4个附加处理:牛粪(CM)、牛浆(CS)、矿物肥和未施肥对照。施用42 d后,两种质地较粗的土壤的土壤微生物指标均有显著的“处理”效果(P < 0.05)。在砂壤土质地土中,FYM_SD的土壤微生物量比FYM_WD和FYM_LD高40% (P = 0.05)。FYM_SD对土壤微生物生物量的影响与CM或CS相当(P > 0.05),而FYM_LD对土壤微生物生物量的影响更接近CS。FYM_SD对土壤原核生物群落结构的影响显著高于fym_ld,但与cm肥相当(P > 0.05)。在壤土质地土中,FYM_SD输入导致原核生物丰富度比FYM_LD低20%。同样,真菌群落结构也会受到消化分数的影响(P = 0.04), FYM_SD和CM对真菌群落结构的影响具有可比性(P > 0.05)。综上所述,这些结果表明,消化物组分对土壤微生物群落的影响是土壤类型依赖的。
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引用次数: 0
Biodegradable microplastics as mediators of iron‑carbon decoupling: Enhanced soil carbon mineralization in wetland 可生物降解微塑料作为铁碳去耦的介质:增强湿地土壤碳矿化
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-12 DOI: 10.1016/j.apsoil.2026.106806
Xinyi Huang , Yuan Pan , Xiansheng Zhang , Teng Li , Ting Wu , Shanqing Tang , Yunze Wang , Junhao Chen , Juanjuan Huang , Zhifeng Liu
Wetlands, recognized as significant carbon reservoirs within ecosystems, have recently been identified as sinks for microplastics (MPs). While iron (Fe)-mediated organic carbon (OC) preservation is pivotal for soil carbon sequestration, the role of MPs in modulating Fe-OC interactions remains unclear. Here, we demonstrated that biodegradable MPs (polybutylene succinate, PBS) act as mediators to decouple Fe-OC interactions, thereby accelerating carbon mineralization in wetland soils. Through anaerobic incubation experiments with conventional (polyethylene terephthalate, PET) and biodegradable MPs (PBS), we reveal that PBS-MPs increased cumulative CO2 emissions by 25.7–39.2% compared to the control, while suppressing cumulative CH4 emissions by 62.3–75.4%. However, PET-MPs had no significant effect on the emissions of CO2 and CH4. As a material with a high carbon content, PBS-MPs directly increased soil organic carbon (SOC) and dissolved organic carbon (DOC) levels. Metagenomic and chemical analyses indicated that PBS-MPs enriched Fe-reducing bacteria and generated redox-active surface groups to facilitate electron transfer during dissimilatory Fe reduction. This process led to the uncoupling of amorphous Fe oxides and their bound organic carbon and resulted in a 54% reduction in amorphous Fe-OC. PBS-MPs enhanced humification of soil dissolved organic matter, thus providing the electron transfer capacity for the soil mineralization and dissimilatory Fe reduction. We further discovered that the competitive relationship between Fe-reducing bacteria and methanogens, as well as the promotion of anaerobic methane oxidation gene expression, led to a reduction in methane emissions. Our findings uncover a previously overlooked mechanism whereby biodegradable MPs exacerbate wetland carbon emissions via Fe-OC decoupling.
湿地被认为是生态系统中重要的碳库,最近被确定为微塑料(MPs)的汇。虽然铁(Fe)介导的有机碳(OC)保存对土壤碳固存至关重要,但MPs在调节Fe-OC相互作用中的作用尚不清楚。在这里,我们证明了可生物降解的MPs(聚丁二酸丁二酯,PBS)作为介质来解耦Fe-OC相互作用,从而加速湿地土壤中的碳矿化。通过常规(聚对苯二甲酸乙二醇酯,PET)和可生物降解MPs (PBS)的厌氧培养实验,我们发现与对照组相比,PBS-MPs的累积CO2排放量增加了25.7-39.2%,而累积CH4排放量减少了62.3-75.4%。PET-MPs对CO2和CH4的排放无显著影响。PBS-MPs作为含碳量高的材料,直接提高了土壤有机碳(SOC)和溶解有机碳(DOC)水平。宏基因组和化学分析表明,PBS-MPs富集了铁还原细菌,并产生了氧化还原活性的表面基团,以促进电子在同化铁还原过程中的转移。这一过程导致非晶态铁氧化物与其结合的有机碳解耦,导致非晶态铁oc减少54%。PBS-MPs增强了土壤溶解有机质的腐殖化作用,从而为土壤矿化和异化铁还原提供了电子传递能力。我们进一步发现,铁还原菌和产甲烷菌之间的竞争关系,以及促进厌氧甲烷氧化基因的表达,导致甲烷排放量的减少。我们的发现揭示了一个以前被忽视的机制,即可生物降解的MPs通过Fe-OC解耦加剧了湿地的碳排放。
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引用次数: 0
Maize straw-driven phosphorus mobilization in two alkaline soils: Microbial community shifts and agronomic implications 两种碱性土壤中玉米秸秆驱动的磷动员:微生物群落变化及其农艺意义
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-11 DOI: 10.1016/j.apsoil.2025.106780
Aminu Darma , Yang Jianjun , Liu Jin , Sun Meili , Chen Jiaqi , Elke Bloem , Chen Tianwen
Straw incorporation enhances soil fertility; however, a clear gap remains regarding how varying rates of maize straw incorporation simultaneously influence P mobilization and the dynamics of P-solubilizing bacterial communities in alkaline soils. Therefore, a pot trial was conducted to examine the impacts of 1 % and 2 % maize straw (MS) application on soil P availability, bacterial community composition, and uptake by wheat crops in an irrigation (XA) and industrial (XI) alkaline polluted soils. The study findings demonstrated that incorporating 2 % MS considerably (P < 0.05) increased soil P availability in both soil types, rising from 21.91 to 22.91 mg kg−1 in XIM-2 % and from 25.15 to 34.73 mg kg−1 in XAM-2 %. The 2 % MS application promoted the proliferation of key P-solubilizing bacterial groups, specifically Proteobacteria, Bacteroidota, Arthrobacter and Bacillus in both soils, indicating strong microbial shifts associated with MS decomposition. These shifts in bacterial consortium were associated with increased production of dissolved organic carbon and pH fluctuations, facilitating P solubilization. This, therefore, enhanced grain P uptake in XIM-2 % (169.42 mg kg−1) and XAM-2 % (338.82 mg kg−1), suggesting that 2 % MS application can effectively promote bacterial functions to improve P transformation and its uptake by wheat grains. These chemical and bacterial improvements produced clear agronomic gains, with the 2 MS% amendments enhancing wheat yield components compared with the control. The ranking of different MS application rates using the Technique for Order of Preference by Similarity to the Ideal Solution (TOPSIS) method (XIM-2 % = 1.00; XAM-2 % = 1.00) reinforced that 2 % MS is the optimal application rate for augmenting the bioavailability of P in these soil systems. These offer an important perspective for the emergence of viable residue management practices to optimize P availability and enhance soil fertility in alkaline agricultural systems.
秸秆掺入提高土壤肥力;然而,不同的玉米秸秆掺入率如何同时影响碱性土壤中磷的动员和溶磷细菌群落的动态,仍然是一个明显的空白。因此,通过盆栽试验,研究了在灌溉(XA)和工业(XI)碱性污染土壤中施用1%和2%玉米秸秆(MS)对土壤磷有效性、细菌群落组成和小麦作物吸收的影响。研究结果表明,添加2% MS显著(P < 0.05)提高了两种土壤类型的土壤磷有效性,在XAM-2 %中从21.91 mg kg - 1增加到22.91 mg kg - 1,在XAM-2 %中从25.15 mg kg - 1增加到34.73 mg kg - 1。2%的质谱处理促进了两种土壤中关键p溶解菌群的增殖,特别是变形菌、拟杆菌、节杆菌和芽孢杆菌,表明与质谱分解相关的强烈微生物转移。细菌联合体的这些变化与溶解有机碳的产量增加和pH波动有关,促进了磷的溶解。因此,XAM-2 % (169.42 mg kg - 1)和XAM-2 % (338.82 mg kg - 1)提高了籽粒对磷的吸收,表明2%的质谱处理可以有效促进细菌功能,促进小麦籽粒对磷的转化和吸收。这些化学和细菌改良产生了明显的农艺收益,与对照相比,2 MS%的改良提高了小麦产量组成部分。采用理想溶液相似度优先排序技术(TOPSIS)对不同MS施用量进行排序(XAM-2 % = 1.00; XAM-2 % = 1.00),结果表明2% MS施用量是提高土壤系统磷生物利用度的最佳施用量。这为在碱性农业系统中优化磷有效性和提高土壤肥力的可行残留物管理实践的出现提供了重要的视角。
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引用次数: 0
Rhizosphere filtering drives the diversity and assembly of soil rotifer communities 根际过滤推动土壤轮虫群落的多样性和聚集
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-10 DOI: 10.1016/j.apsoil.2026.106783
Fangfang Li , Xiaoyan Jiao , Anqi Sun , Ju-Pei Shen , Yong Zheng , Ji-Zheng He , Hang-Wei Hu
Soil rotifers, a phylum of microscopic, multicellular animals, play a critical role in various important functions across global ecosystems. However, our understanding of the processes shaping the large-scale distribution of soil rotifers, particularly in relation to plants and environmental factors, remains limited. Through the analysis of 570 soil samples collected across China, we found that α-diversity of rotifers was significantly higher in rhizosphere soils than in bulk soils, and their β-diversity also exhibited significant differences, highlighting the critical role of the rhizosphere effect in shaping rotifer community structures. The β-diversity of rotifers in rhizosphere soils was primarily driven by geographical location, whereas rotifer communities in bulk soils showed weaker responses to environmental variables. Stochastic processes predominantly shaped the community assembly of rotifer communities in both rhizosphere and bulk soils. Our study provides new insights into the rotifer community assembly in agricultural ecosystems and suggests that plant hosts can have significant impacts on soil rotifer communities.
土壤轮虫是一门微小的多细胞动物,在全球生态系统的各种重要功能中发挥着关键作用。然而,我们对土壤轮虫大规模分布的形成过程,特别是与植物和环境因素的关系的理解仍然有限。通过对全国570个土壤样品的分析,我们发现根际土壤中轮虫α-多样性显著高于块状土壤,它们的β-多样性也表现出显著差异,凸显了根际效应在轮虫群落结构塑造中的关键作用。根际土壤轮虫群落β-多样性主要受地理位置的驱动,而散装土壤轮虫群落对环境变量的响应较弱。根际和块状土壤中轮虫群落的组成主要由随机过程决定。本研究为农业生态系统中轮虫群落的组成提供了新的认识,表明植物寄主对土壤轮虫群落有重要影响。
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引用次数: 0
Microbial carbon-cycling processes drives soil organic carbon accumulation during afforestation in hyper-arid regions 超干旱区造林过程中微生物碳循环过程驱动土壤有机碳积累
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-09 DOI: 10.1016/j.apsoil.2025.106647
Xinping Dong , Yanju Gao , Akash Tariq , Corina Graciano , Zhihao Zhang , Mengfei Cong , Guangxing Zhao , Taotao Wang , Weiqi Wang , Jordi Sardans , Josep Peñuelas , Fanjiang Zeng
Soil microbes represent an important driving force of biogeochemical cycles and are closely related to the soil carbon (C) cycle during afforestation process. Despite their ecological significance, the paucity characterized the mechanistic role of soil microbial C-cycling processes (MCCPs) in hyper-arid regionslimits our ability to assess soil organic carbon (SOC) dynamics and terrestrial C feedbacks to climate change. The present study integrates metagenomics to quantitatively evaluate the MCCPs dynamics across soil profiles (topsoil vs subsoil) in both uncultivated land (0 Y) and Populus alba var. pyramidalis Bunge shelterbelts of different afforestation years (7-, 12-, 22-years-old) along the Taklimakan Desert periphery. Results showed that C fixation was the predominant MCCPs, influenced by afforestation years and soil depth. Shelterbelt establishment significantly increased the concentration of SOC (+57.57 %), the relative abundance of microbial C fixation process (+16.35 %) and methanogenic process (+11.00 %) across both soil layers compared to 0Y, while exhibiting depth-dependent C decomposition patterns (topsoil +12.83 % vs subsoil −8.92 %). Microbial communities demonstrated increased Simpson diversity in topsoil but maintained subsoil stability post-afforestation. Interestingly, network analysis revealed an intensification of positive edges in C fixation process (+127.44 %) and a reduction in negative edges in C decomposition process (−28.47 %). Energy optimization strategies emerged, with microbial communities preferentially utilizing low-energy C fixation pathways under nutrient-deficient conditions. Crucially, afforestation-induced modifications in key edaphic parameters (soil nutrient condition (−49.96 %) and electrical conductivity (−74.42 %)) were identified as primary drivers of MCCPs enhancement and subsequent SOC accumulation. However, despite sustained SOC accumulation in late afforestation stages (22-year period), the marked EC elevation underscores the critical need to integrate secondary salinization control into plantation management frameworks. This study establishes MCCPs as pivotal biological mediators of C sink formation during ecological restoration. We recommend that future afforestation projects in hyper-arid regions simultaneously enhance microbial C fixation pathways and soil nutrient availability to maximize C sequestration.
土壤微生物是生物地球化学循环的重要驱动力,与造林过程中土壤碳(C)循环密切相关。尽管极干旱区土壤微生物碳循环过程(MCCPs)具有重要的生态意义,但其缺乏特征限制了我们评估土壤有机碳(SOC)动态和陆地碳对气候变化反馈的能力。本研究采用宏基因组学方法,对塔克拉玛干沙漠周边不同造林年限(7年、12年、22年)的无耕地(0年)和白胡杨(Populus alba vara . pyramidalis Bunge)防护林不同土壤剖面(表土与底土)的MCCPs动态进行了定量评价。结果表明,固碳是主要的mccp,受造林年限和土壤深度的影响。与2010年相比,防护林的建立显著提高了两层土壤有机碳浓度(+ 57.57%)、微生物固碳过程的相对丰度(+ 16.35%)和产甲烷过程的相对丰度(+ 11.00%),同时呈现出深度依赖的碳分解模式(表层+ 12.83% vs底层- 8.92%)。造林后表层土壤微生物群落Simpson多样性增加,底土保持稳定。有趣的是,网络分析显示,碳固定过程中的正边增强(+ 127.44%),碳分解过程中的负边减少(- 28.47%)。能量优化策略出现了,微生物群落在营养缺乏条件下优先利用低能量的碳固定途径。重要的是,植树造林引起的关键土壤参数(土壤养分状况(- 49.96%)和电导率(- 74.42%))的改变被确定为MCCPs增强和随后SOC积累的主要驱动因素。然而,尽管有机碳在造林后期(22年)持续积累,但显著的欧共体升高强调了将次生盐渍化控制纳入人工林管理框架的迫切需要。本研究确定MCCPs是生态恢复过程中碳汇形成的关键生物介质。我们建议未来在极度干旱地区的造林项目同时加强微生物固碳途径和土壤养分有效性,以最大限度地提高碳固存。
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引用次数: 0
Higher density of earthworms (Pheretima guillelmi) enhances soil carbon sequestration and carbon pool management index in a subtropical forest 较高的蚯蚓密度提高了亚热带森林土壤固碳和碳库管理指数
IF 5 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-01-09 DOI: 10.1016/j.apsoil.2026.106787
Yufeng Qiu , Yue Zhuang , Tanja Trakić , Ronggui Tang , Yihong Liu , Youchao Chen , Xie Wang , Yanjiang Cai , Scott X. Chang
Earthworms play a crucial role in maintaining soil health by influencing biological and ecological processes, particularly in soil organic carbon (SOC) and soil quality restoration. However, many studies on soil quality focus on the impacts of land management practices while overlooking the role of earthworms. This study conducted a one-year field experiment in a subtropical Moso bamboo forest located in Anji, Zhejiang province, China, using homogenized soil (Ferrisol) to investigate the effects of different endogeic earthworm (Pheretima guillelmi) densities, including CK (control, removal of earthworms), OE (original density), DE (double original density), on soil organic carbon stock (SOCS) and carbon pool management index (CPMI, an indicator of soil restoration and the quality of soil carbon pools) in the 0–15 cm and 15–30 cm layers. The results showed that earthworms significantly promoted litter decomposition, leading to increased carbon input into the soil. The SOC and labile organic carbon (LOC) were markedly higher in the 0–15 cm layer compared to the 15–30 cm layer, along with more pronounced earthworm effects. Specifically, in the 0–15 cm layer, SOC concentrations increased by 15.0 % and 19.5 % for the OE and DE treatments, respectively, while SOCS rose by 2.3 % and 7.5 %. Furthermore, earthworms significantly increased the CPMI of the 0–15 cm layer, with increases of 35.9 % in the OE treatment and 62.9 % in the DE treatment. This study highlights the critical role of earthworms in regulating soil carbon inputs and carbon management in both 0–15 cm and 15–30 cm layers, providing valuable insights into the potential of managing earthworm density to enhance sustainable soil carbon management, support long-term soil health, and promote the sustainability of the forest ecosystem.
蚯蚓通过影响生物和生态过程,特别是土壤有机碳(SOC)和土壤质量恢复,在维持土壤健康方面发挥着至关重要的作用。然而,许多关于土壤质量的研究侧重于土地管理措施的影响,而忽视了蚯蚓的作用。本研究在浙江安吉的亚热带毛梭竹林进行了为期一年的田间试验,采用均质土(Ferrisol),研究了不同内源蚯蚓密度(CK(对照,去除蚯蚓)、OE(原始密度)、DE(双原始密度)对土壤有机碳储量(SOCS)和碳库管理指数(CPMI)的影响。0 ~ 15 cm和15 ~ 30 cm土层土壤恢复和土壤碳库质量指标。结果表明:蚯蚓显著促进凋落物分解,导致土壤碳输入增加;土壤有机碳和挥发性有机碳(LOC)在0 ~ 15 cm土层显著高于15 ~ 30 cm土层,且蚯蚓效应更为明显。在0 ~ 15 cm土层,OE和DE处理的有机碳浓度分别提高了15.0%和19.5%,而SOCS分别提高了2.3%和7.5%。蚯蚓显著提高了0 ~ 15 cm土层的CPMI, OE处理提高了35.9%,DE处理提高了62.9%。本研究强调了蚯蚓在0-15 cm和15-30 cm土层中调节土壤碳输入和碳管理的关键作用,为管理蚯蚓密度在加强可持续土壤碳管理、支持土壤长期健康和促进森林生态系统可持续性方面的潜力提供了有价值的见解。
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引用次数: 0
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Applied Soil Ecology
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