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Nitrogen Cycling Under Conifer‐to‐Broadleaf Forest Conversion in Eastern England 英格兰东部针叶林向阔叶林转化过程中的氮循环
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-02-07 DOI: 10.1111/ejss.70281
Caitlin Lewis, Elena Vanguelova, Matthew Ascott, Lucie Jerabkova, Joshua Deakins, Martin Lukac
In the early 20th century, political focus on timber production in Europe led to extensive afforestation and replacement of broadleaves with often non‐native coniferous species. Recent interest in the reverse has risen due to recognition of the wider ecosystem services delivered by forests, such as water quality improvement. Concurrently, recognition of nitrogen saturation in forest soils driven by historically elevated atmospheric deposition has stimulated interest in management interventions aimed at mitigating deposition effects. This study investigated a pseudochronosequence of stands undergoing such conifer‐to‐broadleaf conversion to capture its effects on soil N cycling in Thetford Forest, UK. The pseudochronosequence covered (1) mature broadleaf stands ( n = 5), (2) mature Pinus sylvestris stands ( n = 5), (2) sites felled during the monitoring period ( n = 3) and clearfell sites planted with broadleaves: (3) 0–2 years ago ( n = 3), (4) 5–8 years ago ( n = 5) and (5) 10–13 years ago ( n = 5). The soil C:N ratio at 0–10 cm depth was significantly higher in mature pine sites than in all broadleaf stages. The mean total deep soil NO 3 ‐N leaching fluxes during the study period were lower in young (14.53–16.11 kg‐N ha −1 ) and mature broadleaved stands (10.72 kg‐N ha −1 ) than in mature conifers (23.81 kg‐N ha −1 year −1 ). However, soil NO 3 ‐N leaching fluxes were not significantly different between forest management stages. Net nitrification rates at 10–30 cm depth were higher under low pH conditions, but soil pH and nitrification rates were not linked to soil NO 3 ‐N leaching fluxes or forest management stages. Although no significant effects of management on NO 3 ‐N leaching were found, this study suggests the need to explore the interactive effects of site characteristics, deposition and forest management impacts on soil processes. Long‐term studies complementing observations such as those presented here are needed to capture the effects of conifer‐to‐broadleaf conversion on forest soil nitrogen dynamics.
在20世纪初,欧洲政治对木材生产的关注导致了广泛的植树造林和用非本地针叶树替代阔叶树。由于认识到森林提供的更广泛的生态系统服务,例如改善水质,最近对相反的兴趣有所增加。同时,认识到森林土壤中的氮饱和是由历史上升高的大气沉降引起的,这激发了人们对旨在减轻沉降影响的管理干预措施的兴趣。本研究调查了英国塞特福德森林发生针叶林向阔叶林转变的林分的伪时间序列,以捕捉其对土壤氮循环的影响。假时间序列包括:(1)成熟阔叶林分(n = 5),(2)成熟西洋松林分(n = 5),(2)监测期间砍伐的立地(n = 3)和已砍伐的阔叶立地:(3)0 ~ 2年前(n = 3),(4) 5 ~ 8年前(n = 5)和(5)10 ~ 13年前(n = 5)。成熟松林0 ~ 10 cm土层C:N显著高于各阔叶期。研究期间,幼林(14.53 ~ 16.11 kg‐N ha−1)和成熟阔叶林(10.72 kg‐N ha−1)深层土壤no3‐N淋溶通量平均低于成熟针叶林(23.81 kg‐N ha−1年−1)。然而,不同森林经营阶段土壤no3‐N淋溶通量差异不显著。在低pH条件下,10-30 cm深度的净硝化速率较高,但土壤pH和硝化速率与土壤no3 - N淋溶通量或森林经营阶段无关。虽然没有发现管理对no 3‐N淋溶的显著影响,但本研究表明有必要探索立地特征、沉积和森林管理对土壤过程的交互影响。需要长期的研究来补充这些观察结果,以捕捉针叶树向阔叶转化对森林土壤氮动态的影响。
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引用次数: 0
The Development of the Legend to the Provisional Soil Map of East Africa as a Case Study in Colonial Soil Science 东非临时土壤图图例的发展——以殖民地土壤学为例
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-02-05 DOI: 10.1111/ejss.70290
R. Murray Lark, Lydia M. Chabala, Clarence Chongo, Stalin Sichinga
The Provisional Soil Map of East Africa (PSMEA), published in 1936, was produced by soil scientists in what were then British East African territories. It was an innovative contribution to soil mapping, summarising available information and communicating its incomplete and patchy distribution to the user. In this paper we examine the emergence of the map legend, using proceedings from two key meetings convened for East African soil chemists in 1932 and 1934, and associated correspondence, notes and publications. We consider the international context of the map's production, focusing on attempts to coordinate the efforts of colonial soil scientists in Britain's African territories, and the emergence of an international agenda to map soils at global scale in the aftermath of the formation of the International Soil Science Society (ISSS) (now International Union of Soil Sciences). We examine evidence for the attitudes to indigenous soil knowledge among colonial scientists at the time, showing how this perspective was marginalised, even though it underpinned research in Zambia. We show how, contrary to common assumptions about colonial science, the network behind the East African map was connected to international deliberations on soil survey and made innovative contributions while critiquing proposals from key international experts. We also show the importance of exchange of ideas between the East African team and Colin G. Trapnell, in Zambia. We then outline the later influence of the East African map, and its connections to D'Hoore's Soil Map of Africa.
《东非临时土壤图》(PSMEA)出版于1936年,由当时属英属东非领土的土壤科学家绘制。这是对土壤制图的创新贡献,总结了现有信息,并将其不完整和不完整的分布情况传达给用户。在本文中,我们利用1932年和1934年东非土壤化学家召开的两次重要会议的会议记录,以及相关的通信、笔记和出版物,研究了地图图例的出现。我们考虑了地图制作的国际背景,重点是协调英国非洲领土上殖民地土壤科学家的努力,以及在国际土壤科学学会(ISSS)(现为国际土壤科学联合会)成立后出现的在全球范围内绘制土壤地图的国际议程。我们研究了当时殖民地科学家对土著土壤知识态度的证据,显示了这种观点是如何被边缘化的,尽管它支撑了赞比亚的研究。我们展示了与对殖民科学的普遍假设相反,东非地图背后的网络如何与国际土壤调查的审议联系在一起,并在批评主要国际专家的建议时做出了创新贡献。我们还展示了东非团队与赞比亚的科林·g·特拉普内尔(Colin G. Trapnell)之间思想交流的重要性。然后,我们概述了东非地图的后期影响,以及它与D'Hoore的非洲土壤地图的联系。
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引用次数: 0
The Hidden Soil Carbon Turnover: Evidence From a Long‐Term C3 ‐To‐ C4 Conversion Experiment 隐藏的土壤碳周转:来自长期C3 - To - C4转化实验的证据
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-02-02 DOI: 10.1111/ejss.70283
Azhar Zhartybayeva, Bent T. Christensen, Jørgen Eriksen, Franca Giannini‐Kurina, Johannes L. Jensen
Evaluating the long‐term impact of agricultural practices on soil organic carbon (SOC) dynamics is crucial, as even small changes in SOC storage affect atmospheric CO 2 concentrations with implications for climate change. While conventional field experiments address the net effects of organic matter inputs on SOC stocks, the subsequent turnover of SOC remains hidden. We addressed this gap using soils sampled in a long‐term experiment (1996–2023) with outdoor open‐ended cylinders located at Askov Experimental Station (Denmark). Silage maize was grown every year on two soils (ASK: sandy loam; LUN: coarse sand), both with a pre‐history of C3‐crops and with different C4‐derived organic matter inputs (maize root and stubble only (M), M + additional input of aboveground maize biomass, M + additional input of maize derived sheep faeces). This allowed us to quantify the build‐up of C4‐derived SOC and the decay of C3‐derived SOC over a period of 27 years and to explore interactions between organic matter inputs and the C3‐SOC turnover. At the last sampling in 2023, C4‐SOC from maize stubbles and roots accounted for 25% and 32% of the total‐SOC in LUN and ASK soil, respectively. When soil was amended with additional inputs of maize biomass and sheep faeces, total‐SOC increased and C from these C4‐sources averaged 47%–50% and 61%–63%, respectively. In 2023, the soils retained 10% and 19% of the total C4‐C added in aboveground maize biomass and maize derived sheep faeces, respectively, throughout the 27 years. The presence of a crop accelerated the decay of the old C3‐SOC pool, as evidenced by a comparison of our results with previously published data from a long‐term bare‐fallow experiment. The addition of sheep faeces resulted in a greater loss of C3‐SOC (55%) compared to a similar C input from plant biomass (47%). This indicates that organic matter inputs of different biological quality may lead to different losses of C3‐SOC. Consequently, priming effects may influence long‐term SOC turnover, a process that is not currently represented in soil C models. Incorporating these mechanisms may therefore be necessary to improve the reliability of climate change projections and carbon accounting.
评估农业实践对土壤有机碳动态的长期影响至关重要,因为即使有机碳储量的微小变化也会影响大气二氧化碳浓度,从而对气候变化产生影响。虽然传统的田间试验解决了有机质投入对有机碳储量的净效应,但有机碳的后续周转仍然是隐藏的。我们利用位于阿斯科夫实验站(丹麦)的室外开放式圆柱体进行的长期实验(1996-2023年)中取样的土壤来解决这一差距。青贮玉米每年在两种土壤(ASK:沙质壤土;LUN:粗砂)上种植,这两种土壤都具有C3作物的历史,并且具有不同的C4来源的有机质输入(仅玉米根和茬(M), M +额外输入地上玉米生物量,M +额外输入玉米来源的羊粪便)。这使我们能够量化27年期间C4衍生SOC的积累和C3衍生SOC的衰减,并探索有机质输入与C3 - SOC周转之间的相互作用。在2023年的最后一次采样中,玉米残茬和根系的C4‐SOC分别占LUN和ASK土壤总SOC的25%和32%。当土壤添加玉米生物量和羊粪便时,总有机碳增加,这些C4来源的碳平均分别为47%-50%和61%-63%。在2023年的27年中,土壤分别保留了地上玉米生物量和玉米衍生绵羊粪便中添加的总C4 - C的10%和19%。作物的存在加速了旧C3 - SOC库的衰变,我们的结果与先前发表的长期裸休耕实验数据的比较证明了这一点。绵羊粪便的添加导致C3‐SOC的损失(55%)比类似的植物生物量的C输入(47%)更大。这表明不同生物质量的有机质输入会导致不同的C3‐SOC损失。因此,启动效应可能会影响长期的有机碳周转,这一过程目前尚未在土壤C模型中得到体现。因此,纳入这些机制对于提高气候变化预测和碳核算的可靠性可能是必要的。
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引用次数: 0
The Role of Aggregate Stability and Dispersed Clay in Rainfall Splash Erosion 集料稳定性和分散粘土在降雨溅蚀中的作用
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-31 DOI: 10.1111/ejss.70289
Yangbo He, Lijuan Peng, Xinran Xie, Lirong Lin, Xingsheng Song, Jiazhou Chen
While soil aggregates significantly influence splash erosion, the characteristics of clay particles released during aggregate breakdown and their impact on raindrop splash remain poorly understood. This study investigated the role of soil binding agents in controlling aggregate stability, clay classes released from aggregate, and splash erosion across three soil types (red, calcareous, purple). Red soils showed significantly smaller aggregate stability (MWD = 0.58 mm) and greater release of clay fractions from aggregate breakdown, including both water‐dispersible clay (WDC) (12.46%) and water‐reflocculable clay (WRC = 30.6%), compared to calcareous (MWD = 0.85 mm, WDC = 33.1%, WRC = 2.8%) and purple soils (MWD = 0.84 mm, WDC = 32.2%, WRC = 0.94%). This was attributed to their distinct binding agent composition: red soils were dominated by free Fe oxides (Fe d = 104 g kg −1 ), while calcareous and purple soils exhibited greater soil organic matter (SOM = 9.4–10.3 g kg −1 ) and CaCO 3 contents (0.80%–2.5%). Stepwise regression and correlation analyses revealed SOM consistently enhanced MWD and non‐dispersible clay (NDC) across all soils, whereas CaCO 3 and chelated Fe oxides (Fe p ) showed soil‐specific stabilization effects on MWD, WDC, WRC, and NDC. Total splash erosion was 29.4%–53.5% greater in red soils versus calcareous soils and purple soils, with splash loss negatively correlated to MWD and NDC but positively to WDC ( p < 0.05). These findings demonstrated that splash erosion was jointly controlled by both aggregate MWD and WDC, with soil‐specific binding mechanisms governing these aggregate properties. These findings improve mechanistic understanding of aggregate effect on splash erosion and may improve future erosion modeling.
虽然土壤团聚体对溅射侵蚀有显著影响,但团聚体破碎过程中释放的粘土颗粒的特征及其对雨滴溅射的影响尚不清楚。本研究探讨了土壤粘结剂在控制三种土壤类型(红色、钙质、紫色)骨料稳定性、骨料释放粘土类和飞溅侵蚀中的作用。与钙质土(MWD = 0.85 mm, WDC = 33.1%, WRC = 2.8%)和紫色土(MWD = 0.84 mm, WDC = 32.2%, WRC = 0.94%)相比,红壤表现出更小的团聚体稳定性(MWD = 0.58 mm)和更多的粘土组分释放,包括水分散粘土(WDC)(12.46%)和水可回流粘土(WRC = 30.6%)。这是由于它们的结合剂组成不同:红壤以游离铁氧化物为主(Fe d = 104 g kg - 1),而钙质和紫色土壤表现出更高的土壤有机质(SOM = 9.4-10.3 g kg - 1)和caco3含量(0.80%-2.5%)。逐步回归和相关分析显示,SOM在所有土壤中均能增强MWD和非分散性粘土(NDC),而caco3和螯合铁氧化物(Fe p)对MWD、WDC、WRC和NDC具有土壤特异性稳定作用。红壤的溅蚀总量比钙质土和紫色土高29.4% ~ 53.5%,溅蚀损失与MWD和NDC呈负相关,与WDC呈正相关(p < 0.05)。这些发现表明,飞溅侵蚀是由骨料MWD和WDC共同控制的,土壤特异性结合机制控制着这些骨料性质。这些发现提高了对骨料对飞溅侵蚀作用的机理理解,并可能改善未来的侵蚀模型。
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引用次数: 0
Seasonal Dynamics of Arbuscular Mycorrhizal Fungi and N 2 O Emissions in Danish Soils Under Long‐Term Conservation Agriculture 长期保护性农业条件下丹麦土壤丛枝菌根真菌和氮氧排放的季节动态
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-30 DOI: 10.1111/ejss.70286
Stamatios Thomopoulos, Lars Elsgaard, Lars J. Munkholm, Sabine Ravnskov
Conservation agriculture (CA), which includes reduced tillage and residue retention, has the potential to improve soil structure and support beneficial microbial communities such as arbuscular mycorrhizal fungi (AMF). At the same time, CA practices may also influence nitrous oxide (N 2 O) emissions, a potent greenhouse gas contributing to global warming through their effects on the soil environment. This study examines the effects of CA practices on AMF biomass fluctuations and on N 2 O emissions over a year. It was hypothesized that CA would promote AMF and reduce N 2 O emissions. In a field experiment under temperate climate on sandy loam soil in Denmark, AMF biomarkers and mineral N were assessed 8 times throughout the year while N 2 O fluxes were measured on 35 occasions during 2022‐2023. Signature fatty acids associated with AMF storage lipids (neutral lipid fatty acids) showed greater seasonal variation than those linked to the AMF hyphal network (phospholipid fatty acids), both of which were negatively affected by ploughing. Residue retention had no significant effect on AMF biomarkers but was associated with approximately 44% lower N 2 O emissions during late spring. No clear patterns emerged between seasonal variations in AMF biomarkers and N 2 O fluxes during a year, indicating there was no link between them. These findings highlight the importance of evaluating microbial and gaseous indicators in parallel to assess the broader impacts of CA on soil health and environmental sustainability.
保护性农业(CA),包括减少耕作和残留物保留,具有改善土壤结构和支持有益微生物群落如丛枝菌根真菌(AMF)的潜力。同时,CA的做法也可能影响一氧化二氮(n2o)的排放,这是一种强有力的温室气体,通过对土壤环境的影响导致全球变暖。本研究考察了一年多来CA做法对AMF生物量波动和氮氧化物排放的影响。假设CA可以促进AMF的发生,减少n2o的排放。在丹麦温带气候下的沙质壤土上进行了一项田间试验,在2022 - 2023年期间,全年评估了8次AMF生物标志物和矿物N,同时测量了35次n2o通量。与AMF储存脂相关的特征脂肪酸(中性脂质脂肪酸)比与AMF菌丝网络相关的特征脂肪酸(磷脂脂肪酸)表现出更大的季节性变化,两者都受到耕作的负面影响。残留物保留对AMF生物标志物没有显著影响,但与晚春期间一氧化氮排放量降低约44%相关。在一年中,AMF生物标志物的季节变化与氮氧通量之间没有明确的模式,表明它们之间没有联系。这些发现强调了同时评估微生物和气体指标以评估CA对土壤健康和环境可持续性的更广泛影响的重要性。
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引用次数: 0
Can Digital Soil Mapping Be Causal? 数字土壤制图是因果关系吗?
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-30 DOI: 10.1111/ejss.70284
Lei Zhang, Alexandre M. J.‐C. Wadoux
All too often, it is unclear whether digital soil mapping (DSM) models can support causal interpretation. A common practice in DSM studies is to interpret the importance of covariates for prediction. This carries an implicit causal assumption that is rarely stated and even more rarely justified. Because DSM relies entirely on observational data, it is widely assumed that causal inference is not possible. But is it? Here, we discuss the conditions under which causal inference with observational data is possible and two views of causality. We show that while under each of the views causal inference may be possible, a so‐called generative view is the one most capable of satisfying the conditions for causal inference in DSM. Generative causality treats causation as the system of processes that produce observed associations, rather than relying on associations themselves, as is common in current DSM studies. Realizing this perspective requires DSM to shift towards models in which soil‐forming factors influence soil properties through explicitly modelled processes, which some would call process‐informed DSM. Since these processes are ‘fully determined’ by the modeller's specification, they offer a structured means to control confounding and open the door to applying existing causal inference frameworks. While generative DSM is formally possible, we should ultimately ask whether causal inference ought to be a primary goal, since the primary strength of DSM lies not in establishing causality but in delivering accurate predictions and highlighting patterns that warrant further investigation.
通常,数字土壤制图(DSM)模型是否能支持因果解释尚不清楚。DSM研究中的一个常见做法是解释协变量对预测的重要性。这包含了一种隐含的因果假设,这种假设很少被陈述,更很少被证明是正确的。由于DSM完全依赖于观测数据,因此人们普遍认为因果推理是不可能的。但这是真的吗?在这里,我们讨论的条件下,因果推理与观测数据是可能的和因果关系的两种观点。我们表明,虽然在每种观点下因果推理都是可能的,但所谓的生成观点是最能够满足DSM因果推理条件的观点。生成因果关系将因果关系视为产生观察到的关联的过程系统,而不是依赖于关联本身,这在当前的DSM研究中很常见。实现这一观点需要DSM转向土壤形成因素通过明确建模过程影响土壤特性的模型,有些人称之为过程知情的DSM。由于这些过程是由建模者的规范“完全确定”的,因此它们提供了一种结构化的方法来控制混淆,并为应用现有的因果推理框架打开了大门。虽然生成式DSM在形式上是可能的,但我们最终应该问,因果推理是否应该成为主要目标,因为DSM的主要优势不在于建立因果关系,而在于提供准确的预测和突出值得进一步调查的模式。
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引用次数: 0
Influence of Enhanced Rock Weathering of Nepheline‐Syenite Tailings on Major and Trace Elements Accumulation in Wheat 霞石-正长岩尾矿强化岩石风化对小麦主微量元素积累的影响
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-28 DOI: 10.1111/ejss.70282
S. O. Apori, S. Flynn, D. A. C. Manning, G. Stewart, M. E. Wakefield, M. Edwards, L. Collins, K. J. Mclnnes
Soil nutrient depletion and quality are critical challenges facing agriculture and have been exacerbated by the long‐term use of chemical fertilisers. A 14‐week pot experiment was conducted, with nepheline‐syenite tailings (NST) serving as the sole non‐nitrogen nutrient source for wheat, to determine the potential of NST to improve the soil nutrient status. The impact of NST on plant health was examined at five application rates (0, 1.25, 5, 10, and 20 g/kg of artificial soil). At the end of the experiments the pH, major and trace elements (e.g., Ca, Mg, P, S, K, Fe, Mn, Zn, Si, Cu, Mo) in both the rhizosheath and the bulk soil, and wheat biomass (both above and belowground) were measured, and used to calculate nutrient uptake. These parameters generally increased with higher NST application rates. Wheat biomass increased with increasing NST doses up to 10 g/kg of artificial soil. Potentially toxic elements (PTEs) such as Al, As, Sr, Rb, and Ba increased in the soil; however, their concentrations remained 52.5% to 91.7% below the world soil average, suggesting minimal environmental risk. The P and K nutrient use efficiency (NUE) decreased with increasing application, indicating that NUE may not be effective for evaluating slow‐releasing amendments where the elemental totals do not represent the bioavailable fraction. The findings improve our understanding of how NST can be used to enhance soil fertility and agricultural yield, providing valuable insights for its effective use as soil amendments, particularly in regions with readily available silicate rocks of this type and nutrient‐depleted soils.
土壤养分枯竭和土壤质量是农业面临的重大挑战,长期使用化肥加剧了这一问题。以霞石正长岩尾矿(NST)作为小麦唯一的非氮营养源,进行了为期14周的盆栽试验,以确定NST改善土壤养分状况的潜力。在5种施用量(0、1.25、5、10和20 g/kg人工土壤)下,研究了NST对植物健康的影响。在试验结束时,测量根鞘和块土中的pH、主微量元素(如Ca、Mg、P、S、K、Fe、Mn、Zn、Si、Cu、Mo)和小麦生物量(地上和地下),并用于计算养分吸收。这些参数通常随着NST施用量的增加而增加。小麦生物量随着NST用量的增加而增加,最高可达10 g/kg人工土壤。土壤中Al、as、Sr、Rb、Ba等潜在有毒元素(pte)增加;然而,它们的浓度仍比世界土壤平均水平低52.5%至91.7%,表明环境风险最小。磷和钾养分利用效率(NUE)随着施用量的增加而下降,表明在元素总量不代表生物可利用部分的情况下,NUE可能对评估缓释修正剂无效。这些发现提高了我们对NST如何用于提高土壤肥力和农业产量的理解,为其作为土壤改良剂的有效利用提供了有价值的见解,特别是在具有这种类型的硅酸盐岩石和养分枯竭土壤的地区。
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引用次数: 0
Divergent Shifts in Soil Nutrient Stoichiometry and Microbial Quotient From Topsoil to Subsoil After Forest Conversion 森林转化后表层土壤养分化学计量学和微生物商的差异变化
IF 4.2 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-27 DOI: 10.1111/ejss.70287
Rui Zhang, Lingling Zhang, Rufeng Guo, Dazhi Wen, Xianzhen Luo
Soil microbial quotient (qMB), representing the proportion of soil elements contained within microbial biomass, is a critical indicator of microbial community efficiency in regulating soil quality and nutrient cycling. Changes in qMB are vital for ecosystem functioning and maintenance of soil fertility. However, the effects of converting primary natural broadleaf forests (NF) to plantation and broad‐leaved mixed forests (PNF) or plantation forests (PF) on qMB dynamics remain poorly understood, especially in phosphorus (P)‐limited subtropical ecosystems. We analyzed litter, soil, and microbial biomass carbon (C), nitrogen (N), P across three typical subtropical forests to assess stoichiometric characteristics and qMB changes. Forest conversion significantly decreased the concentrations of soil C, N, P and microbial biomass C (MBC), N (MBN), P (MBP), and these reductions were more pronounced in the topsoil (0–10 cm) than in the subsoil (10–30 cm). However, in the subsoil, soil C, N, and P decreased more steeply than MBC, MBN, and MBP by 117.4%, 351.9%, and 111.5%, respectively, which disrupted the stoichiometric balance between soil nutrients and microbial biomass. The C:P imbalance (stoichiometric imbalance between soil C:P and MBC:MBP) and the N:P imbalance (stoichiometric imbalance between soil N:P and MBN:MBP) increased by 78.3% and 46.7%, respectively, in the subsoil after NF‐to‐PF conversion, respectively. Concurrently, these changes in stoichiometric imbalance significantly remained stable in the topsoil but increased microbial quotient P by 114.3% in the subsoil, indicating microbial adaptation aimed at enhancing P acquisition and retention in response to soil P scarcity. Redundancy analysis and structural equation modeling further confirmed that qMB shifts were driven mainly by stoichiometric imbalances resulting from reduced resource availability, suggesting the stoichiometric imbalances induced by forest conversion compel microbial communities to adapt to nutrient constraints, especially under P‐deficient conditions. Overall, our findings highlight adaptive management strategies should be developed to prioritize the preservation of soil fertility in primary forests, while considering soil P nutrition to maintain C, N, and P balance and stability of soil microorganisms during afforestation.
土壤微生物商(qMB)代表了微生物生物量中所含土壤元素的比例,是衡量微生物群落调节土壤质量和养分循环效率的重要指标。qMB的变化对生态系统功能和土壤肥力的维持至关重要。然而,将原始天然阔叶林(NF)转化为人工林和阔叶混交林(PNF)或人工林(PF)对qMB动态的影响尚不清楚,特别是在磷(P)限制的亚热带生态系统中。本文分析了3种典型亚热带森林凋落物、土壤和微生物生物量碳(C)、氮(N)、磷的化学计量特征和qMB的变化。森林转化显著降低了土壤C、N、P和微生物生物量C (MBC)、N (MBN)、P (MBP)的浓度,且表层土壤(0 ~ 10 cm)的降低幅度大于底土(10 ~ 30 cm)。土壤C、N、P分别比MBC、MBN和MBP降低117.4%、351.9%和111.5%,破坏了土壤养分与微生物生物量之间的化学计量平衡。土壤C:P失衡(土壤C:P与MBC:MBP之间的化学计量失衡)和N:P失衡(土壤N:P与MBN:MBP之间的化学计量失衡)在NF - to - PF转化后分别增加了78.3%和46.7%。同时,这些化学计量失衡的变化在表层土壤中保持稳定,但在底土中增加了114.3%的微生物商P,表明微生物适应旨在提高磷的获取和保留,以应对土壤磷稀缺。冗余分析和结构方程模型进一步证实,qMB的变化主要是由资源可用性降低导致的化学计量失衡驱动的,这表明森林转换引起的化学计量失衡迫使微生物群落适应营养约束,特别是在缺磷条件下。总体而言,我们的研究结果强调应制定适应性管理策略,以优先保护原生林的土壤肥力,同时考虑土壤P营养,以维持造林过程中土壤C、N、P的平衡和土壤微生物的稳定性。
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引用次数: 0
Microbial Driven C-P Coupled Coordination Facilitates Soil Health 微生物驱动的C - P耦合协调促进土壤健康
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-26 DOI: 10.1111/ejss.70288
Shudong Ding, Hechuan Liu, Ruirui Chen, Xiangui Lin, Xin Zhou, Youzhi Feng

The global decline in soil phosphorus (P) availability presents a significant threat to food security, necessitating a re-evaluation of phosphorus deficiency in soils and an urgent focus on activating legacy phosphorus reservoirs. Phosphorus deficiency is typically addressed through two main strategies: the Limiting Factor Principle, which emphasizes direct mineral P supplementation, and Systems Theory, which advocates for soil elemental stoichiometry driven by microorganisms. However, it remains unclear which strategy is more effective in improving P availability and long-term soil health, a gap that may impact soil management practices. To address this, we conducted an incubation experiment with soil subjected to 23 years of localized fertilization management. Our results showed that P amendment alone did not resolve phosphorus deficiency, while C amendment, either alone or in combination with P, effectively promoted P activation and enhanced microbial functionality. Microcalorimetric analyses indicated that exogenous organic carbon increased microbial biomass and stimulated metabolic activity and alkaline phosphatase activity, particularly in P-deficient soils, thereby enhancing organic P mineralization and mobilization. Additionally, shifts in soil microbial communities were observed, characterized by increased relative abundances of Comamonadaceae and Bacillus. Both taxa are known for their strong responsiveness to carbon availability, suggesting their potential role in coupled carbon-phosphorus phosphate cycling. These findings indicate that Systems Theory, improving the soil health of P-deficient soils through both soil functions and soil life, provides a complementary strategy to traditional fertilization for improving P-deficient soils.

全球土壤磷(P)有效性下降对粮食安全构成重大威胁,需要重新评估土壤磷缺乏症,并迫切关注激活遗留磷库。磷缺乏通常通过两种主要策略来解决:限制因子原则,强调直接补充矿物磷;系统理论,主张由微生物驱动的土壤元素化学计量学。然而,目前尚不清楚哪种策略在改善磷有效性和长期土壤健康方面更有效,这一差距可能会影响土壤管理实践。为了解决这个问题,我们对土壤进行了23年局部施肥管理的培养试验。我们的研究结果表明,单独添加P不能解决缺磷问题,而单独添加C或与P联合添加C都能有效地促进P的活化,增强微生物功能。微量热分析表明,外源有机碳增加了微生物生物量,刺激了代谢活性和碱性磷酸酶活性,从而增强了有机磷的矿化和动员,特别是在缺磷土壤中。此外,土壤微生物群落发生了变化,其特征是共生菌科和芽孢杆菌的相对丰度增加。这两个类群都以其对碳可用性的强烈响应而闻名,这表明它们在碳-磷耦合磷酸盐循环中的潜在作用。这些发现表明,系统理论通过土壤功能和土壤生命改善缺磷土壤的土壤健康,为改善缺磷土壤提供了传统施肥的补充策略。
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引用次数: 0
Time-Dependent Effects of Subsoil Chiselling on Soil Physical Resilience in a Semi-Arid Soybean-Wheat Cropping System 半干旱大豆-小麦种植系统中底土凿凿对土壤物理恢复力的时间依赖性影响
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-01-21 DOI: 10.1111/ejss.70258
Mukhtar Ahmad, Pramila Aggarwal, R. N. Garg, Surajit Mondal, Sunayan Saha, Debasish Roy, Ravender Singh, Debashis Chakraborty

Sub-surface soil compaction restricts root growth and water movement in intensively cultivated semi-arid croplands. Chiselling is commonly used to alleviate compaction, but its effects are often short-lived under variable rainfall conditions. We evaluated the time-variable effects of chiselling on soil hydro-mechanical properties (penetration resistance [PR], bulk density [BD], hydraulic function [steady-state infiltration, IR; field-saturated hydraulic conductivity, Kfs] and soil moisture dynamics), root traits (length, volume, surface area and diameter), yield and water use efficiency (WUE) in a soybean-wheat rotation on a sandy loam soil over 2 years. Four treatments were evaluated: residual chisel (RS; May 2011), repeated chisel (RC; May 2011 and May 2013), fresh chisel (FC; May 2013), and no chisel (NC). At early soybean 2013, the compact layer (15–30 cm) showed 20%–22% lesser PR in RS and RC than NC (p = 0.019); BD reductions mirrored this pattern. Despite greater PR, NC initially exhibited the highest IR (1.36 cm h−1 vs. RS 0.79, RC 1.08, FC 0.90 cm h−1) and Kfs (1.10–1.19 cm h−1, 31%–82% above chiselled plots at 15–30 cm), consistent with a dual-porosity mechanism in which a few continuous biopores govern near-saturated flow while the surrounding matrix remains strong. Root responses concentrated at 15–30 cm. RS/RC increased root length, volume and surface area and moderately enlarged mean diameter relative to NC/FC (p < 0.05). Yield gains and improved WUE were observed in soybean in year 1 under RS (21% and 10%) and RC (32% and 17%) versus NC, whereas wheat yield did not differ; WUE was modest. Rainfall timing explained the short-lived FC gains. The first 14 days after chiselling (20 May 2013) were dry, followed by two storm clusters within days 15–60 totaling ~330 mm, including ≥ 50–100 mm single-day events. These high-load, antecedently wet events plausibly collapsed freshly created voids in FC, truncating hydraulic gains, while RS/RC retained some storage advantages. The findings highlight that the effectiveness of chiselling is strongly time- and rainfall-dependent, and their persistence depends on pore-network continuity. Results suggest site-specific, rainfall-informed tillage decisions to enhance soil structural resilience and sustainable productivity in semi-arid systems.

在精耕细作的半干旱农田中,地下土壤压实限制了根系生长和水分流动。凿凿通常用于缓解压实,但在多变的降雨条件下,其效果往往是短暂的。我们评估了凿凿对砂壤土2年大豆-小麦轮作中土壤水力学特性(渗透阻力[PR]、体积密度[BD]、水力功能[稳态入渗,IR;田间饱和水力电导率,kfs]和土壤水分动力学)、根系性状(长度、体积、表面积和直径)、产量和水分利用效率(WUE)的时变效应。评估四种处理:残余凿(RS; 2011年5月)、重复凿(RC; 2011年5月和2013年5月)、新鲜凿(FC; 2013年5月)和无凿(NC)。早熟大豆15 ~ 30 cm密实层的PR在对照和对照中较对照低20% ~ 22% (p = 0.019);BD减少反映了这种模式。尽管PR较高,但NC最初表现出最高的IR (1.36 cm h - 1, RS为0.79,RC为1.08,FC为0.90 cm h - 1)和kfs (1.10-1.19 cm h - 1,高于15-30 cm的楔形图的31%-82%),这与双孔隙机制一致,其中少数连续的生物孔控制着接近饱和的流动,而周围的基质仍然很强。根系反应集中在15 ~ 30 cm处。与NC/FC相比,RS/RC增加了根长、体积和表面积,并适度扩大了平均直径(p < 0.05)。对照(21%和10%)和对照(32%和17%)处理第1年大豆的产量和水分利用效率均较对照提高,而小麦产量无显著差异;WUE是适度的。降雨时间解释了短期的FC增长。凿凿后的前14天(2013年5月20日)是干燥的,随后在15-60天内出现了两个风暴群,总计约330毫米,其中包括≥50-100毫米的单日事件。这些高负荷、事先潮湿的事件可能会破坏FC中新形成的空隙,从而截断水力增益,而RS/RC保留了一些存储优势。研究结果强调,凿凿的有效性强烈依赖于时间和降雨,其持久性取决于孔隙网络的连续性。研究结果表明,在半干旱系统中,基于特定地点、降雨信息的耕作决策可以提高土壤结构弹性和可持续生产力。
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引用次数: 0
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European Journal of Soil Science
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