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Effects of legume-cover crop rotations on soil pore characteristics and particulate organic matter distributions in Vertisol based on X-ray computed tomography 基于x射线计算机断层扫描的豆科作物轮作对versol土壤孔隙特征和颗粒有机质分布的影响
IF 6.6 1区 农林科学
Geoderma Pub Date : 2025-07-31 DOI: 10.1016/j.geoderma.2025.117464
Tianyu Ding , Zichun Guo , Keke Hua , Zizhou Yu , Jiaqi Li , Yueming Chen , Zhibin Guo , Daozhong Wang , Jianli Liu , Xinhua Peng
{"title":"Effects of legume-cover crop rotations on soil pore characteristics and particulate organic matter distributions in Vertisol based on X-ray computed tomography","authors":"Tianyu Ding ,&nbsp;Zichun Guo ,&nbsp;Keke Hua ,&nbsp;Zizhou Yu ,&nbsp;Jiaqi Li ,&nbsp;Yueming Chen ,&nbsp;Zhibin Guo ,&nbsp;Daozhong Wang ,&nbsp;Jianli Liu ,&nbsp;Xinhua Peng","doi":"10.1016/j.geoderma.2025.117464","DOIUrl":"10.1016/j.geoderma.2025.117464","url":null,"abstract":"<div><div>Cover crops have been used as an effective soil management practice to improve soil pore structure and promote particulate organic matter (POM) accumulation. However, the effects of different cover crop rotations on soil pore characteristics and the spatial distributions for POM remain poorly understood. This study examined the influence of five cropping systems (spring maize monoculture (M), wheat-maize rotation (WM), wheat-soybean rotation (WS), wheat-<em>Cassia occidentalis</em> rotation (WCo), and wheat-<em>Cassia tora</em> Linn<em>.</em> rotation (WCt)) on soil POM fractions, pore structure, and soil physical properties, and nutrient availability in a Vertisol. The results showed that, compared to M treatment, all four rotation systems significantly increased image-based porosity, 120–1000 μm porosity, pore surface area density, and connection probability (<em>P</em> &lt; 0.05). The WCo and WCt treatments led to an increase in connected porosity by 207 % and 130 % (<em>P</em> &lt; 0.05). They also significantly increased fresh POM by 90.4 % and 55.5 %, and total POM by 75.4 % and 52.4 %, respectively (<em>P</em> &lt; 0.05). These treatments also significantly increased air permeability (<em>K<sub>a</sub></em>), relative gas diffusivity (<em>D<sub>s</sub>/D<sub>0</sub></em>), and saturated hydraulic conductivity (<em>K<sub>s</sub></em>) (<em>P</em> &lt; 0.05). Strong correlations were observed between fresh POM and pore structural parameters (image-based porosity, connected porosity, 500–1000 μm porosity, hydraulic radius), as well as soil physical properties (<em>K<sub>s</sub></em>, <em>K<sub>a</sub></em>, <em>D<sub>s</sub>/D<sub>0</sub></em>). The positive feedback between pore structure and POM accumulation facilitated soil structural improvement under leguminous cover crop-based rotations (WCo, WCt). These findings suggest that integrating <em>Cassia occidentalis</em> and <em>Cassia tora</em> Linn<em>.</em> into rotation systems can effectively enhance soil structure and promote organic matter sequestration in Vertisols.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"461 ","pages":"Article 117464"},"PeriodicalIF":6.6,"publicationDate":"2025-07-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144739585","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Paleosols as indicators for late Pleistocene landscape dynamics in Crete (Greece) 古土壤作为希腊克里特岛晚更新世景观动态的指示物
IF 6.6 1区 农林科学
Geoderma Pub Date : 2025-07-31 DOI: 10.1016/j.geoderma.2025.117450
Fabian Kirsten , Daniel Moraetis , Georgios E. Christidis , Rosa Poch , Steven Forman , Kosmas Pavlopoulos
{"title":"Paleosols as indicators for late Pleistocene landscape dynamics in Crete (Greece)","authors":"Fabian Kirsten ,&nbsp;Daniel Moraetis ,&nbsp;Georgios E. Christidis ,&nbsp;Rosa Poch ,&nbsp;Steven Forman ,&nbsp;Kosmas Pavlopoulos","doi":"10.1016/j.geoderma.2025.117450","DOIUrl":"10.1016/j.geoderma.2025.117450","url":null,"abstract":"<div><div>Paleosols in different climatic zones and geomorphological settings serve as important paleoenvironmental archives. Crete (Greece) with its central location in the eastern Mediterranean area constitutes an important (paleo)climatic transition zone between northern Africa and the Eurasia. While paleosols have been commonly described and used as chronostratigraphic markers within a large number of geological and archaeological studies in Crete, they have not been subject of a comparative study so far. In the present study, we analyse seven pedocomplexes in central and western Crete within different climatic, geological and geomorphological settings. Our analysis is based on geochemistry, grain size distribution, bulk and clay mineralogy, micromorphology and absolute datings (luminescence, radiocarbon). In all cases, the paleosol horizons, mainly Bt- und Bk-horizons, display strong indications for pedogenesis, such as increased clay contents or carbon accumulation, similar reddish-brown colours and abundant characteristic clay minerals, especially vermiculite, smectite and kaolinite, compared to the over- and underlying sediments. However, clay composition also reveals desequilibrium conditions indicating an allochthonous origin of at least part of the material. Furthermore, micromorphological results do not clearly confirm in-situ pedogenesis. Therefore, open questions related to the redeposition of Terra Rossa as pedosediments as well as the importance of dust inputs from long-range sources remain. Chronostratigraphically, the timing of the deposition of soil parent materials as well as the formation of petrocalcic horizons indicate that soil formation was related to climatic transition phases during the late Pleistocene in most studied cases. However, due to the limited number of profiles, datings and comparable geo-archives in Crete, these results need to be substantiated in future studies incorporating further paleosols in Crete and the surroundings areas in the Eastern Mediterranean.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"461 ","pages":"Article 117450"},"PeriodicalIF":6.6,"publicationDate":"2025-07-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144739586","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The global pedogenon map: Combining and spatialising the factors of soil formation 全球土壤分布图:土壤形成因子的组合与空间化
IF 6.6 1区 农林科学
Geoderma Pub Date : 2025-07-30 DOI: 10.1016/j.geoderma.2025.117462
Nicolas Francos, Amin Sharififar, Trevan Flynn, Quentin Styc, Sandra J. Evangelista, Jose Padarian, Wartini Ng, Damien J. Field, Budiman Minasny, Alex B. McBratney
{"title":"The global pedogenon map: Combining and spatialising the factors of soil formation","authors":"Nicolas Francos,&nbsp;Amin Sharififar,&nbsp;Trevan Flynn,&nbsp;Quentin Styc,&nbsp;Sandra J. Evangelista,&nbsp;Jose Padarian,&nbsp;Wartini Ng,&nbsp;Damien J. Field,&nbsp;Budiman Minasny,&nbsp;Alex B. McBratney","doi":"10.1016/j.geoderma.2025.117462","DOIUrl":"10.1016/j.geoderma.2025.117462","url":null,"abstract":"<div><div>This study presents the development of a global pedogenon map, which classifies soil units based on similarities in their formation processes while excluding anthropogenic effects, at a high spatial resolution of 90 m. Designed for use by scientists, land managers, and policymakers, this map classifies distinct soil units —called pedogenons—based on key soil-forming factors, including parent material, climate, soil organisms, relief, and inherent soil properties. This study employs a combination of principal component analysis (PCA), non-metric-multidimensional-scaling (NMDS), and an unsupervised classification technique (K-means clustering) to capture the full range of soil formation processes across diverse landscapes of the world yielding an unbiased, globally applicable classification. The global pedogenon map enables soil capacity and condition monitoring on a global scale. This foundation is crucial for future identification of “least disturbed soils” to serve as a reference for any soil around the globe. By integrating this dataset with broader environmental data, the global pedogenon map supports global efforts to enhance soil security and monitor environmental changes.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117462"},"PeriodicalIF":6.6,"publicationDate":"2025-07-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144724983","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Investigating the influence of soil organic carbon on pore structure within aggregates 研究土壤有机碳对团聚体孔隙结构的影响
IF 6.6 1区 农林科学
Geoderma Pub Date : 2025-07-29 DOI: 10.1016/j.geoderma.2025.117463
Jingjing Liu , Yu Tian , Chiara Pasut , Mark Farrell , Shenggao Lu
{"title":"Investigating the influence of soil organic carbon on pore structure within aggregates","authors":"Jingjing Liu ,&nbsp;Yu Tian ,&nbsp;Chiara Pasut ,&nbsp;Mark Farrell ,&nbsp;Shenggao Lu","doi":"10.1016/j.geoderma.2025.117463","DOIUrl":"10.1016/j.geoderma.2025.117463","url":null,"abstract":"<div><div>Soil pore structural properties, such as porosity, size distribution and geometry, are crucial for various soil processes and are significantly influenced by soil organic carbon (SOC). SOC plays a vital role in determining soil functionality and ecosystem services and is the primary driver of pore geometry within soil aggregates, yet traditional in-situ analysis methods have fallen short in accurately describing its intricate distribution. This study employed a two-stage approach to analyze soil structure at the pore scale: a hydrogen peroxide fogging system was used to selectively remove organic carbon from soil aggregates, followed by synchrotron radiation micro-computed tomography (SR-μCT) for in-depth three-dimensional imaging. The results revealed that the hydrogen peroxide treatment variably reduced organic carbon in soil aggregates, with Cambisol samples showing a higher removal efficiency (38.58–63.31%) compared to Ultisol samples (27.33–45.74%). Mineral-associated organic carbon (MAOC) was more stable than particle organic carbon (POC). SOC depletion led to consistent changes in pore volume across soil types, but the changes in pore shape distribution varied between Cambisols and Ultisols. In Cambisols, SOC removal was associated with more pronounced shifts in pore morphology, whereas Ultisols showed more heterogeneous responses, likely due to differing mineralogical properties. These findings suggest that SOC contributes differently to pore structure depending on soil type. This study aimed to move beyond the traditional “black box” view of soil by visualizing the complex interactions between soil organic carbon (SOC) and soil structure with a new method. This approach could provide valuable insights into the mechanisms behind soil aggregate formation.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117463"},"PeriodicalIF":6.6,"publicationDate":"2025-07-29","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144721525","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Grazing-induced abiotic and resource changes drive distinct responses of soil bacterial and fungal community in temperate meadow steppe: Implications for carbon dynamics 放牧引起的非生物和资源变化驱动温带草甸草原土壤细菌和真菌群落的不同响应:对碳动态的影响
IF 6.6 1区 农林科学
Geoderma Pub Date : 2025-07-28 DOI: 10.1016/j.geoderma.2025.117451
Cuixia Jiang , Xiaoping Xin , Kai Xue , Zhigang Zhao , Weixing Liu , Haonan Guo , Feng Liu , Hui Li , Zihao Li , Yufan Si , Ruirui Yan
{"title":"Grazing-induced abiotic and resource changes drive distinct responses of soil bacterial and fungal community in temperate meadow steppe: Implications for carbon dynamics","authors":"Cuixia Jiang ,&nbsp;Xiaoping Xin ,&nbsp;Kai Xue ,&nbsp;Zhigang Zhao ,&nbsp;Weixing Liu ,&nbsp;Haonan Guo ,&nbsp;Feng Liu ,&nbsp;Hui Li ,&nbsp;Zihao Li ,&nbsp;Yufan Si ,&nbsp;Ruirui Yan","doi":"10.1016/j.geoderma.2025.117451","DOIUrl":"10.1016/j.geoderma.2025.117451","url":null,"abstract":"<div><div>Soil microbial communities play a crucial role in maintaining grassland ecosystem functions and are strongly influenced by livestock grazing. However, the long-term responses and driving mechanisms of soil microbial communities to grazing intensity gradients, remain largely unexplored. In this study, we investigated the mechanism of different grazing intensities (i.e., ungrazed, light, moderate and heavy grazing) affect the diversity and composition of soil bacteria and fungi in the Hulunbuir <em>Leymus chinensis</em> meadow steppe. Using a Bipartite network to represent indicative species shifts, bacterial community presented a clear succession along the grazing intensity gradient, likely linked to soil abiotic conditions (e.g. soil temperature, silt). In contrast, fungal community exhibited a more discrete shift along the grazing intensity gradient, challenging the traditional view that fungal community is more stable under disturbance. The shifts in fungal community were closely related to the vegetation composition and aboveground biomass, reflecting a typical bottom-up resource-related regulation, which were more dynamic than changes caused by abiotic conditions along the grazing intensity gradient. Interestingly, indicator analysis showed that higher grazing intensity shifted bacterial and fungal composition towards more oligotrophic (e.g. Dothideomycetes, Sordariomycetes, Leotiomycetes, and Chloroflexi, Thermoleophilia) and less copiotrophic (e.g. Saprotrophs, Bacteroides and subgroup_6). This shift reflects the depleted substrate and is consistent with the observed inhibition of ecosystem respiration, implying lower organic matter decomposition. The distinct patterns of bacteria and fungi responses provides novel insights into the mechanisms, through which grazing alters soil bacterial and fungal communities with potential long-term consequences, including future growth-limiting resource and soil environment conditions to withstand future disturbances, which affect soil bacterial and fungal communities differently and consequently modulate soil organic carbon turnover. Moreover, the different substrate affinity of copiotrophic and oligotrophic groups altered available and recalcitrant C decomposition, which may change soil carbon cycling and stocks.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117451"},"PeriodicalIF":6.6,"publicationDate":"2025-07-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144721524","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Denitrification in the deep vadose zone: implications for nitrate leaching under agricultural managed aquifer recharge 深层渗透带的反硝化作用:农业管理含水层补给下硝酸盐淋滤的影响
IF 5.6 1区 农林科学
Geoderma Pub Date : 2025-07-27 DOI: 10.1016/j.geoderma.2025.117457
Hannah Waterhouse, Helen E. Dahlke, William R. Horwath
{"title":"Denitrification in the deep vadose zone: implications for nitrate leaching under agricultural managed aquifer recharge","authors":"Hannah Waterhouse,&nbsp;Helen E. Dahlke,&nbsp;William R. Horwath","doi":"10.1016/j.geoderma.2025.117457","DOIUrl":"10.1016/j.geoderma.2025.117457","url":null,"abstract":"<div><div>Managed aquifer recharge on agricultural lands (AgMAR) is an inexpensive and extensive form of recharge compared to dedicated recharge basins and injections wells. However, uncertain nitrogen cycling outcomes concerning nitrate (NO<sub>3</sub><sup>–</sup>) transport and fate in the unsaturated zone remain. A combination of laboratory and field experiments were conducted to assess biogeochemical controls on denitrification in surface soils and subsurface sediments during AgMAR. Acetylene block assays were conducted in anaerobic conditions to determine dentification potential rates in the root zone and subsurface sediments collected from an almond orchard down to nine meters in the Central Valley of California. Samples were either amended with carbon (C) and NO<sub>3</sub><sup>–</sup> additions (potential assays) or no substrates were added (control) and nitrous oxide (N<sub>2</sub>O) was measured over three days. Denitrification potential assays resulted in four times more N<sub>2</sub>O production near the surface, and 49x more N<sub>2</sub>O production in the subsurface compared to the control. However, even without additions of C, sediments were able to denitrify ∼ 40 % of the NO<sub>3</sub><sup>–</sup> present in the subsurface during the incubation. Additionally, δ<sup>15</sup>N of NO<sub>3</sub><sup>–</sup> was measured in the field before and after AgMAR, showing an average absolute increase of 4.0 ‰ in δ<sup>15</sup>N across 4 m depth suggesting denitrification following AgMAR. Statistical analysis suggests N<sub>2</sub>O production in assays depends on environmental controls or geochemistry of the soils/sediments when C concentrations are low, with iron significantly influencing denitrification in the control, but not in denitrification potential assays. These results from both laboratory incubations and the field demonstrate initial indications that the vadose zone has the potential to attenuate NO<sub>3</sub><sup>–</sup> via denitrification, however, our results do not allow exact quantification of denitrified N mass under AgMAR, and more work is needed to determine denitrification rates in-situ. Future studies should focus on quantifying denitrification rates in-situ during and immediately following AgMAR events.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117457"},"PeriodicalIF":5.6,"publicationDate":"2025-07-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144713283","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Increasing ECM tree dominance enhances soil lignin phenols but suppresses microbial necromass contribution to soil organic carbon in a subtropical mountainous forest 增加ECM树优势增加了土壤木质素酚,但抑制了亚热带山地森林微生物坏死团对土壤有机碳的贡献
IF 5.6 1区 农林科学
Geoderma Pub Date : 2025-07-26 DOI: 10.1016/j.geoderma.2025.117456
Mengzhen Lu , Long Chen , Qiuxiang Tian , Qing He , Mi Yang , Zhiyang Feng , Feng Liu
{"title":"Increasing ECM tree dominance enhances soil lignin phenols but suppresses microbial necromass contribution to soil organic carbon in a subtropical mountainous forest","authors":"Mengzhen Lu ,&nbsp;Long Chen ,&nbsp;Qiuxiang Tian ,&nbsp;Qing He ,&nbsp;Mi Yang ,&nbsp;Zhiyang Feng ,&nbsp;Feng Liu","doi":"10.1016/j.geoderma.2025.117456","DOIUrl":"10.1016/j.geoderma.2025.117456","url":null,"abstract":"<div><div>Arbuscular mycorrhizal (AM) and ectomycorrhizal (ECM) plants exhibit distinct litter quality characteristics and nutrient uptake strategies that critically influence soil carbon and nitrogen cycling. However, the effect of mycorrhizal type on soil organic carbon (SOC) accumulation remains unclear, particularly in tropical and subtropical forests in China. To address this knowledge gap, this study quantified the SOC content and its components across a gradient of ECM tree dominance (ECM%, defined as the proportion of ECM tree basal area relative to the all trees) in a subtropical mountainous forest. Lignin phenols and amino sugars were used as indicators of plant- and microbial-derived C in the soil, respectively. Plant, soil, and microbial properties were analyzed to explore the underlying mechanisms influencing SOC components across different mycorrhizal types. Our results indicated that ECM% did not affect SOC content but significantly altered SOC composition. Specifically, a higher ECM% promoted plant-derived C accumulation and reduced microbial-derived C. The increase in plant-derived C accumulation with ECM% was primarily owing to lower litter quality and higher C inputs from litter and fine roots. Conversely, microbial-derived C accumulation decreased with ECM%, primarily because of the lower metabolic efficiency and higher degradation rate of microbial necromass, as indicated by metabolic quotient and extracellular enzyme activities, respectively. Overall, these findings improve existing understanding of the mechanisms underlying SOC formation and decomposition along the gradient of ECM tree dominance, providing valuable insights into how shifts in tree mycorrhizal dominance under global change may alter the pathways and composition of SOC accumulation in forest soils.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117456"},"PeriodicalIF":5.6,"publicationDate":"2025-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144711249","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Soil microbial C:N:P stoichiometry across environmental transects in China’s typical ecologically fragile regions 中国典型生态脆弱区环境样带土壤微生物C:N:P化学计量特征
IF 5.6 1区 农林科学
Geoderma Pub Date : 2025-07-26 DOI: 10.1016/j.geoderma.2025.117454
Wenjie Cao , Yun Chen , Yuqiang Li , Lilong Wang , Yulong Duan , Xiaohui Li
{"title":"Soil microbial C:N:P stoichiometry across environmental transects in China’s typical ecologically fragile regions","authors":"Wenjie Cao ,&nbsp;Yun Chen ,&nbsp;Yuqiang Li ,&nbsp;Lilong Wang ,&nbsp;Yulong Duan ,&nbsp;Xiaohui Li","doi":"10.1016/j.geoderma.2025.117454","DOIUrl":"10.1016/j.geoderma.2025.117454","url":null,"abstract":"<div><div>The stoichiometry of soil microbial biomass is closely tied to the terrestrial cycling of carbon (C) and nutrients. Those stoichiometry influences not only soil fertility but also global change mitigation efforts. Ecologically fragile areas are commonly located in the ecotones between different ecosystems, with poor stability, weak ability to resist disturbance, and easy degradation. Yet the biogeographical patterns and potential mechanistic drivers of soil microbial biomass stoichiometry and its homeostasis in fragile ecosystems remain unclear. In this study we set three transects in typical ecologically fragile areas of China from which topsoil (0 − 20 cm depth) samples were collected to measure their microbial biomass carbon (MBC), nitrogen (MBN), and phosphorus (MBP). The results revealed much lower MBC (190.1 mg kg<sup>−1</sup>), MBN (20.5 mg kg<sup>−1</sup>), and MBP (7.1 mg kg<sup>−1</sup>) concentrations than their corresponding global and Chinese averages, but higher MBC:MBN (9.7), MBC:MBP (48.4), and MBN:MBP (4.3) ratios. The stoichiometric homeostasis (<em>H</em>, calculated by nonlinear fitting of microbial and soil stoichiometry) of MBC, MBN, and MBP concentrations ranged from 1.4 to 2.3, being weakly plastic to weakly homeostatic, while their ratios were generally homeostatic (with <em>H</em> ranged from 4.2 to 45.5). The MBC:MBN:MBP ratio was approximately 48:4:1. Overall, soil microbes were vulnerable to soil nitrogen and phosphorus limitations, compared to soil carbon. Soil MBC:MBN:MBP stoichiometry changed nonlinearly along the latitudinal gradient. Soil chemical and vegetation properties contributed the majority of variance explanations (&gt; 62 %) to microbial biomass stoichiometry. Altogether, these findings provide new insight into the patterns and homeostasis of soil MBC:MBN:MBP stoichiometry in fragile ecosystems.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117454"},"PeriodicalIF":5.6,"publicationDate":"2025-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144711283","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Relict charcoal hearth magnetic fingerprints in the forest topsoil 森林表层土壤中残留木炭炉磁指纹
IF 5.6 1区 农林科学
Geoderma Pub Date : 2025-07-26 DOI: 10.1016/j.geoderma.2025.117458
Marcin Szuszkiewicz , Jarosław Lasota , Maria Magdalena Szuszkiewicz , Ewa Błońska
{"title":"Relict charcoal hearth magnetic fingerprints in the forest topsoil","authors":"Marcin Szuszkiewicz ,&nbsp;Jarosław Lasota ,&nbsp;Maria Magdalena Szuszkiewicz ,&nbsp;Ewa Błońska","doi":"10.1016/j.geoderma.2025.117458","DOIUrl":"10.1016/j.geoderma.2025.117458","url":null,"abstract":"<div><div>The relationship between the magnetic properties and fire-affected soil is crucial for environmental inference, especially in the case of soil magnetic enhancement by thermal transformation of iron minerals. Generally, there are no studies reporting relict charcoal hearths using magnetic analyses. This gap is addressed in our work. Moreover, we also fill the gap regarding how long fire-related magnetic enhancement may persist in soils. Hence, the data may also influence the development of research on pyrogenic magnetic enhancement of soils. The preliminary research was aimed at verifying the possibility of using some environmental magnetism parameters to detect differences in the soil magnetic signal with and without relict charcoal hearth (RCH). Consequently, to understand and describe the mechanism of pyrogenic magnetic enhancement in charcoal-enriched horizon (CEH), research into its magnetic features was initiated. This work was carried out on three soil profiles <em>(Albic Brunic Arenosols</em>), both RCHs and reference. The magnetic data obtained during the study showed variable contribution of magnetic particles in soil horizons, which indicates pyrogenic magnetic enhancement related to the presence of superparamagnetic (SP) grains in the charcoal particles from CEH in the RCHs soil profile. Despite the oxidation of SP grains of ferrimagnetic minerals over time (200–250 years) superparamagnetic magnetite and/or maghemite are still responsible for the pyrogenic magnetic enhancement in soil.</div></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":"460 ","pages":"Article 117458"},"PeriodicalIF":5.6,"publicationDate":"2025-07-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144711282","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Moisture-driven shifts in microbial nitrogen limitation under biochar and nitrification inhibitors co-application in tropical soils 热带土壤生物炭与硝化抑制剂共同施用时微生物氮限制的水分驱动变化
IF 5.6 1区 农林科学
Geoderma Pub Date : 2025-07-25 DOI: 10.1016/j.geoderma.2025.117455
Lijun Liu , Qilin Zhu , Xiaoqian Dan , Huanyu Bao , Tongbin Zhu , Lei Meng , Ahmed S. Elrys , Christoph Müller , Jinbo Zhang
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