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.
{"title":"Nitrogen Cycling Under Conifer‐to‐Broadleaf Forest Conversion in Eastern England","authors":"Caitlin Lewis, Elena Vanguelova, Matthew Ascott, Lucie Jerabkova, Joshua Deakins, Martin Lukac","doi":"10.1111/ejss.70281","DOIUrl":"https://doi.org/10.1111/ejss.70281","url":null,"abstract":"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 ( <jats:italic>n</jats:italic> = 5), (2) mature <jats:styled-content style=\"fixed-case\"> <jats:italic>Pinus sylvestris</jats:italic> </jats:styled-content> stands ( <jats:italic>n</jats:italic> = 5), (2) sites felled during the monitoring period ( <jats:italic>n</jats:italic> = 3) and clearfell sites planted with broadleaves: (3) 0–2 years ago ( <jats:italic>n</jats:italic> = 3), (4) 5–8 years ago ( <jats:italic>n</jats:italic> = 5) and (5) 10–13 years ago ( <jats:italic>n</jats:italic> = 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 <jats:sub>3</jats:sub> ‐N leaching fluxes during the study period were lower in young (14.53–16.11 kg‐N ha <jats:sup>−1</jats:sup> ) and mature broadleaved stands (10.72 kg‐N ha <jats:sup>−1</jats:sup> ) than in mature conifers (23.81 kg‐N ha <jats:sup>−1</jats:sup> year <jats:sup>−1</jats:sup> ). However, soil NO <jats:sub>3</jats:sub> ‐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 <jats:sub>3</jats:sub> ‐N leaching fluxes or forest management stages. Although no significant effects of management on NO <jats:sub>3</jats:sub> ‐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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"58 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-02-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146134158","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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。
{"title":"The Development of the Legend to the Provisional Soil Map of East Africa as a Case Study in Colonial Soil Science","authors":"R. Murray Lark, Lydia M. Chabala, Clarence Chongo, Stalin Sichinga","doi":"10.1111/ejss.70290","DOIUrl":"https://doi.org/10.1111/ejss.70290","url":null,"abstract":"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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"160 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-02-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146122169","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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。
{"title":"The Hidden Soil Carbon Turnover: Evidence From a Long‐Term C3 ‐To‐ C4 Conversion Experiment","authors":"Azhar Zhartybayeva, Bent T. Christensen, Jørgen Eriksen, Franca Giannini‐Kurina, Johannes L. Jensen","doi":"10.1111/ejss.70283","DOIUrl":"https://doi.org/10.1111/ejss.70283","url":null,"abstract":"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 <jats:sub>2</jats:sub> 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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"66 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-02-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146098264","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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。
{"title":"The Role of Aggregate Stability and Dispersed Clay in Rainfall Splash Erosion","authors":"Yangbo He, Lijuan Peng, Xinran Xie, Lirong Lin, Xingsheng Song, Jiazhou Chen","doi":"10.1111/ejss.70289","DOIUrl":"https://doi.org/10.1111/ejss.70289","url":null,"abstract":"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 <jats:sub>d</jats:sub> = 104 g kg <jats:sup>−1</jats:sup> ), while calcareous and purple soils exhibited greater soil organic matter (SOM = 9.4–10.3 g kg <jats:sup>−1</jats:sup> ) and CaCO <jats:sub>3</jats:sub> 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 <jats:sub>3</jats:sub> and chelated Fe oxides (Fe <jats:sub>p</jats:sub> ) 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 ( <jats:italic>p</jats:italic> < 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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"79 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-01-31","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146098266","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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.
{"title":"Seasonal Dynamics of Arbuscular Mycorrhizal Fungi and N 2 O Emissions in Danish Soils Under Long‐Term Conservation Agriculture","authors":"Stamatios Thomopoulos, Lars Elsgaard, Lars J. Munkholm, Sabine Ravnskov","doi":"10.1111/ejss.70286","DOIUrl":"https://doi.org/10.1111/ejss.70286","url":null,"abstract":"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 <jats:sub>2</jats:sub> 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 <jats:sub>2</jats:sub> O emissions over a year. It was hypothesized that CA would promote AMF and reduce N <jats:sub>2</jats:sub> 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 <jats:sub>2</jats:sub> 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 <jats:sub>2</jats:sub> O emissions during late spring. No clear patterns emerged between seasonal variations in AMF biomarkers and N <jats:sub>2</jats:sub> 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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"43 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146071662","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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.
{"title":"Can Digital Soil Mapping Be Causal?","authors":"Lei Zhang, Alexandre M. J.‐C. Wadoux","doi":"10.1111/ejss.70284","DOIUrl":"https://doi.org/10.1111/ejss.70284","url":null,"abstract":"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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"76 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-01-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146071659","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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.
{"title":"Influence of Enhanced Rock Weathering of Nepheline‐Syenite Tailings on Major and Trace Elements Accumulation in Wheat","authors":"S. O. Apori, S. Flynn, D. A. C. Manning, G. Stewart, M. E. Wakefield, M. Edwards, L. Collins, K. J. Mclnnes","doi":"10.1111/ejss.70282","DOIUrl":"https://doi.org/10.1111/ejss.70282","url":null,"abstract":"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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"103 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-01-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146070591","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
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.
{"title":"Divergent Shifts in Soil Nutrient Stoichiometry and Microbial Quotient From Topsoil to Subsoil After Forest Conversion","authors":"Rui Zhang, Lingling Zhang, Rufeng Guo, Dazhi Wen, Xianzhen Luo","doi":"10.1111/ejss.70287","DOIUrl":"https://doi.org/10.1111/ejss.70287","url":null,"abstract":"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 <jats:sub>imbalance</jats:sub> (stoichiometric imbalance between soil C:P and MBC:MBP) and the N:P <jats:sub>imbalance</jats:sub> (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.","PeriodicalId":12043,"journal":{"name":"European Journal of Soil Science","volume":"16 1","pages":""},"PeriodicalIF":4.2,"publicationDate":"2026-01-27","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146056034","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}