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Compositional Data Methods and VISNIRS to Predict Soil Organic Carbon Contents 土壤有机碳成分数据方法与VISNIRS预测
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-16 DOI: 10.1111/ejss.70200
José A. Cayuela-Sánchez, Rafael López-Núñez

Soil organic carbon (SOC) content plays an important role in modulating atmospheric CO2. Visible and near-infrared spectroscopy (VISNIRS) has been proven to be a suitable method for SOC prediction in the laboratory. However, several soil properties such as soil moisture (SM), bulk density, compactness, texture, and temperature affect the near-infrared spectra obtained under field conditions. Among these factors, SM variation is the most significant challenge for SOC measurement. Soil is a composition of fractions, especially minerals and organic matter, whose contents are expressed in relative and interdependent quantities, belonging to simplex spaces. These are known as compositional data (CoDa) and require specific mathematical methods. This study proposes methods to predict SOC along with other soil components, rather than using solely one soil feature. Several predictive models using VISNIRS by considering different soil compositions were evaluated. All models included SM to mitigate its interference in SOC prediction, which would otherwise occur when using only VISNIRS-based methods. The analyzed soil components included soil organic matter (SOM, calculated as SOM = 1.724 × SOC), SM, soil inorganic carbon (SIC), and the textural fractions: “Clay,” “Silt,” and the remainder of the soil sample classified as “Other.” The 4-parts model including the clay content provided SOM prediction with Lin's concordance correlation coefficient = 0.84 and Pearson r = 0.87. Important is to note that the predictions stated with the different CoDa approaches showed similar trends, from the 6-Parts to the 2-Parts compositions, this fact highlighting the consistency of the method. The performance of all the CoDa models obtained, and in particular the 4-part “Clay” model, was superior to that obtained with the traditional PLS calibration. The results highlighted that CoDa methods for estimating SOM or SOC provided an improvement over traditional partial least square (PLS) calibration. Future software solutions could integrate routines for using these methods in the field.

土壤有机碳(SOC)含量对大气CO2具有重要的调节作用。可见和近红外光谱(VISNIRS)已被证明是一种适用于实验室SOC预测的方法。然而,一些土壤特性,如土壤湿度(SM)、容重、密实度、质地和温度会影响在野外条件下获得的近红外光谱。在这些因素中,SM的变化是对有机碳测量的最大挑战。土壤是组分的组成,特别是矿物质和有机质,其含量以相对和相互依赖的数量表示,属于单一空间。这些数据被称为组合数据(CoDa),需要特定的数学方法。本研究提出了与其他土壤组分一起预测有机碳的方法,而不是仅使用一种土壤特征。对VISNIRS在考虑不同土壤组成的情况下的几种预测模型进行了评价。所有模型都包含SM以减轻其对SOC预测的干扰,否则仅使用基于VISNIRS的方法会出现这种情况。分析的土壤成分包括土壤有机质(SOM,计算SOM = 1.724 × SOC)、SM、土壤无机碳(SIC)和质地组分:“粘土”、“淤泥”和其余土壤样品分类为“其他”。包含粘土含量的4部分模型提供SOM预测,Lin’s一致性相关系数= 0.84,Pearson r = 0.87。重要的是要注意,从6 - part到2 - part组成,不同CoDa方法的预测显示出相似的趋势,这一事实突出了方法的一致性。所获得的所有CoDa模型,特别是4 -部分“Clay”模型的性能优于传统PLS校准获得的模型。结果强调,CoDa方法估计SOM或SOC比传统的偏最小二乘(PLS)校准提供了改进。未来的软件解决方案可以集成在现场使用这些方法的例程。
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引用次数: 0
Soil Health, Crop Yield and Carbon Footprint Trade-Offs Between Conservation and Conventional Farming: A Case Study 土壤健康、作物产量和碳足迹在保护农业和传统农业之间的权衡:一个案例研究
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-12 DOI: 10.1111/ejss.70194
Christoph Rosinger, Golo Gotthalmseder, Gernot Bodner, Katharina M. Keiblinger, Stefan J. Forstner, Taru Sandén, Giacomo Ferretti, Moltinë Prebibaj, Reinhard W. Neugschwandtner, Hans-Peter Kaul

Transitioning towards soil health-oriented farming systems is fundamental to mitigate future challenges such as climate change, soil degradation, and increasing global food demands. In this study, we evaluated soil health, crop yields, and greenhouse gas (GHG) emissions at a long-term experimental site in Central Europe that comprised two cropping systems: a conventional system with regular tillage, low-diversity crop rotation, and minimal cover cropping, and a conservation system with shallow tillage, diverse crop rotation, and extensive cover cropping. We assessed soil health using 13 physico-chemical and biological parameters, calculated field-scale GHG emissions, and analysed yield dynamics over an eight-year period to evaluate potential crop yield penalties under conservation farming. We observed significant soil health advances (+7%) and reductions in GHG emissions (−43%) with conservation farming, while crop yields for all cultivated crops remained stable. Improvements in soil health were particularly pronounced for nitrogen cycling and microbial-driven processes. For several measured soil health parameters, we found a larger effect of crop species compared to farming system. Further, positive management effects on soil were apparent particularly for winter wheat and to a lesser extent for maize and sugar beet, strongly emphasizing the need for standardized soil health assessments that take crop species into account. Our study demonstrates that easily implementable conservation farming measures such as reduced tillage, increased crop diversity, and enhanced cover cropping can substantially improve soil health and long-term agricultural sustainability without compromising crop yields. Conservation farming thus emerges as a viable strategy to support resilient crop production in temperate regions.

向以土壤健康为导向的农业系统过渡,对于缓解气候变化、土壤退化和全球粮食需求增加等未来挑战至关重要。在这项研究中,我们在中欧的一个长期试验点评估了土壤健康、作物产量和温室气体(GHG)排放,该试验点包括两种种植系统:常规耕作、低多样性轮作和最小覆盖种植的传统系统,以及浅耕、多样化轮作和广泛覆盖种植的保护系统。我们利用13个理化和生物学参数评估了土壤健康状况,计算了农田尺度的温室气体排放,并分析了8年期间的产量动态,以评估保护性耕作对作物产量的潜在影响。我们观察到保护性耕作显著改善了土壤健康(+7%),减少了温室气体排放(- 43%),而所有栽培作物的产量保持稳定。土壤健康的改善在氮循环和微生物驱动过程中尤为明显。对于几个测量的土壤健康参数,我们发现与耕作制度相比,作物种类的影响更大。此外,对土壤的积极管理效果很明显,特别是对冬小麦,对玉米和甜菜的影响较小,这强烈强调需要进行考虑到作物品种的标准化土壤健康评估。我们的研究表明,易于实施的保护性耕作措施,如减少耕作、增加作物多样性和增加覆盖种植,可以在不影响作物产量的情况下显著改善土壤健康和长期农业可持续性。因此,保护性耕作成为支持温带地区抗灾作物生产的一项可行战略。
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引用次数: 0
FeOx-Driven Soil Aggregation Boosts MAOC Accumulation and POC Protection in Subtropical Mixed Conifer–Broadleaf Forests feox驱动的土壤团聚促进亚热带针叶林-阔叶林MAOC积累和POC保护
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-11 DOI: 10.1111/ejss.70197
Zhengui Han, Yunchao Zhou, Yingli Guo, Han Liu, Qianbin Cao

The conversion of pure coniferous plantations to coniferous–broadleaf mixed forests increases the organic carbon (OC) content of soil and aggregates; however, the mechanisms of OC retention through soil aggregation remain inadequately understood. We selectively removed Fe oxides and OC from soil of both poorly aggregated (pure coniferous plantation) and well aggregated (mixed forest) soil systems. The mechanism of particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) sequestration in Fe oxide soil aggregation under broadleaf transformation was studied. The removal of Fe oxides broke the macroaggregates into microaggregates and < silt + clay fractions and revealed the attachment and entanglement effects of plant residues encapsulated by macroaggregates on soil particles, whereas plant residue decomposition maximised the degree of macroaggregate fragmentation (64.8%–100%). These results indicate that POC self-isolates and that the presence of Fe oxides further enhances POC physical occlusion during soil aggregation. The extent of this physical protection provided by Fe oxides follows the order: free Fe (FeD) > amorphous Fe (FeO) > complex Fe (FeP). Specifically, FeO and FeP promote macroaggregate formation through organic–inorganic complexes (MAOC formation) to enhance POC physical occlusion, whereas FeD predominantly forms inorganic–inorganic complexes. Microaggregate formation and MAOC accumulation occurred simultaneously through organic–inorganic interactions with various Fe oxide forms. These processes enhanced soil aggregation and were accompanied by significant accumulation of POC (80.2%–169.8%) and MAOC (41.1%–137.3%) after stand conversion (p < 0.05). These findings indicate that improved soil aggregation capacity mediated by Fe oxides during forest conversion promotes POC and MAOC accumulation through distinct Fe oxide-specific aggregation mechanisms.

纯针叶人工林向针叶阔叶混交林的转变增加了土壤和团聚体的有机碳含量;然而,通过土壤团聚体保持有机碳的机制仍不充分了解。我们选择性地从低团聚(纯针叶林)和高团聚(混交林)土壤系统中去除氧化铁和有机碳。研究了阔叶转化条件下颗粒有机碳(POC)和矿物伴生有机碳(MAOC)在铁氧化物土壤团聚体中的固存机制。铁氧化物的去除将大团聚体分解为微团聚体和粉土+粘土组分,揭示了被大团聚体包裹的植物残体对土壤颗粒的附着和缠结作用,而植物残体分解使大团聚体破碎程度最大化(64.8% ~ 100%)。这些结果表明,POC具有自隔离作用,铁氧化物的存在进一步增强了POC在土壤团聚过程中的物理封闭。铁氧化物提供这种物理保护的程度顺序为:自由铁(FeD) >;非晶铁(FeO) >;络合物铁(FeP)。具体而言,FeO和FeP通过有机-无机配合物(MAOC)促进大聚集体的形成,从而增强POC的物理遮挡,而FeD主要形成无机-无机配合物。微团聚体的形成和MAOC的积累是通过与各种铁氧化物形式的有机-无机相互作用同时发生的。这些过程增强了土壤团聚性,并伴随着林分转换后POC(80.2% ~ 169.8%)和MAOC(41.1% ~ 137.3%)的显著积累(p < 0.05)。这些结果表明,森林转化过程中铁氧化物介导的土壤团聚能力的提高通过不同的铁氧化物聚集机制促进了POC和MAOC的积累。
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引用次数: 0
Correction to “SoilManageR—An R Package for Deriving Soil Management Indicators to Harmonise Agricultural Practice Assessments” 更正“土壤管理器-一个获取土壤管理指标以协调农业实践评估的R包”
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-11 DOI: 10.1111/ejss.70191

Heller, O., A. Chervet, F. Durand-Maniclas, et al. 2025. “SoilManageR—An R Package for Deriving Soil Management Indicators to Harmonise Agricultural Practice Assessments.” European Journal of Soil Science 76: e70102. https://doi.org/10.1111/ejss.70102.

The error was limited to the manuscript and did not occur in the underlying calculations and the software package. Therefore, the correction of Equation (3) does not affect any of the presented data, results or interpretations.

We apologize for this error.

Heller, O., A. Chervet, F. Durand-Maniclas等,2025。“土壤管理器——一个获取土壤管理指标以协调农业实践评估的工具包。”土壤科学进展(2):1 - 4。https://doi.org/10.1111/ejss.70102.The错误仅限于稿件,并未发生在基础计算和软件包中。因此,对式(3)的修正不影响所呈现的任何数据、结果或解释。我们为这个错误道歉。
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引用次数: 0
Sustainable and Resilient Agroecosystems Need Complexity of Soil Food Webs and Multivariate Soil Health Indicators 可持续和有弹性的农业生态系统需要土壤食物网的复杂性和多元土壤健康指标
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-11 DOI: 10.1111/ejss.70192
Jennifer Michel, Iñaki Balanzategui-Guijarro, Da Cao, Philippe Hinsinger, Jacques Le Gouis, Jordi Moya-Laraño, Sara Sánchez-Moreno, Sarah Symanczik, Hervé Vanderschuren, Dominique Van Der Straeten, Matthias Waibel, Markus Weinmann, Cécile Thonar, Pierre Delaplace

We need to adapt crop species and agricultural practices to produce high quantities of quality food for a growing world population, while also reducing the negative impact of agriculture on the environment to meet the targets of the Paris Agreement. It is increasingly recognised that healthy soils are at the heart of this endeavour, sustaining global geochemical cycles and the productivity of most terrestrial ecosystems. This ability of soils to support essential ecosystem services like nutrient cycling arises from diverse communities of soil organisms. Many ecosystem services are a function of how these soil organisms interact with each other, with the aboveground plant species and with the physio-chemical soil matrix. Here, we argue that multiple ecosystem processes and climate change resilience rely on diverse plant and soil communities with complex interactions among various actors carrying out complementary functions, rather than on individual indicator species on their own. We highlight areas of research which could be expanded to advance our understanding from single-species studies to the functional complexity of soil food webs and its integration into land management strategies with the aim to improve the resilience and sustainability of essential terrestrial ecosystems and the services they provide to the human population.

我们需要调整作物品种和农业做法,为不断增长的世界人口生产大量优质粮食,同时减少农业对环境的负面影响,以实现《巴黎协定》的目标。人们日益认识到,健康的土壤是这一努力的核心,它维持着全球地球化学循环和大多数陆地生态系统的生产力。土壤支持养分循环等基本生态系统服务的能力来自土壤生物的不同群落。许多生态系统服务是这些土壤生物如何相互作用的功能,与地上植物物种和理化土壤基质。本文认为,多种生态系统过程和气候变化恢复力依赖于多种植物和土壤群落,这些群落之间存在着相互作用的互补功能,而不是单独依赖于单个指示物种。我们强调了可以扩展的研究领域,以促进我们从单一物种研究到土壤食物网功能复杂性的理解,并将其纳入土地管理战略,以提高基本陆地生态系统的恢复力和可持续性及其为人类提供的服务。
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引用次数: 0
Scientific Indicators and Stakeholders' Perceptions on Soil Threats in France: How Do They Compare? 科学指标和利益相关者对法国土壤威胁的看法:它们如何比较?
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-10 DOI: 10.1111/ejss.70190
Eloise Mason, Sophie Cornu, Claire Froger, Nicolas P. A. Saby, Claire Chenu

Soils are under multiple threats, with varying levels of intensity and nature across different areas. It is therefore important to assess the soil threat level. To do so, scientific indicators have been developed, but their implementation at the country level can be challenging. As stakeholders have good knowledge of soil conditions, stakeholders' perceptions on soil threats could be used as a complementary indicator. The objective of this paper is to explore this possibility focusing on the five soil threats considered by stakeholders as the most important at the European level: erosion, artificialisation, compaction, soil organic carbon (SOC) loss and contamination. A participatory stakeholder consultation conducted in France in 2021 yielded 1444 responses. We elaborated stakeholders' perception maps at the departmental scale, which we compared with scientific indicator maps per soil threat. Our findings indicate that stakeholders consider artificialisation the most important soil threat in France. The spatial distribution of soil threats based on stakeholders' perceptions and scientific indicators matches in 43% of the departments for SOC loss, and in over half of the departments for erosion (50%), compaction (51%), artificialisation (63%) and contamination (74%). The differences can be attributed to higher stakeholders' perception compared to scientific indicators for erosion, SOC loss and contamination. Conversely, for artificialisation and compaction, these differences can be attributed to lower stakeholders' perception than the scientific indicators. Moreover, certain scientific indicators assess the threat only partially, whereas stakeholders may perceive the threat differently or as a whole. When biases in the scientific assessment, stakeholders' perception or comparison are taken into consideration, stakeholders' perceptions can be used as a tool to complement existing scientific indicators.

土壤面临多重威胁,不同地区的威胁程度和性质各不相同。因此,评估土壤威胁程度是很重要的。为此,已经制定了科学指标,但在国家一级实施这些指标可能具有挑战性。由于利益相关者对土壤状况有很好的了解,利益相关者对土壤威胁的看法可以作为一个补充指标。本文的目的是探讨这种可能性,重点关注利益相关者认为在欧洲层面上最重要的五种土壤威胁:侵蚀、人工、压实、土壤有机碳(SOC)损失和污染。2021年在法国进行的参与性利益相关者协商收到了1444份答复。我们在部门尺度上详细阐述了利益相关者的感知图,并将其与每个土壤威胁的科学指标图进行了比较。我们的研究结果表明,利益相关者认为法国最重要的土壤威胁是人工。基于利益相关者的认知和科学指标的土壤威胁的空间分布在43%的部门中与有机碳损失相匹配,在一半以上的部门中与侵蚀(50%)、压实(51%)、人工(63%)和污染(74%)相匹配。与侵蚀、有机碳损失和污染的科学指标相比,这种差异可归因于更高的利益相关者认知。相反,对于人为化和压缩,这些差异可归因于利益相关者的感知低于科学指标。此外,某些科学指标只能对威胁进行部分评估,而利益相关者可能会以不同的方式或整体地看待威胁。当考虑到科学评估中的偏差、利益相关者的感知或比较时,利益相关者的感知可以作为补充现有科学指标的工具。
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引用次数: 0
Effects of Physicochemical Properties on Soil Water Vapour Sorption Kinetics 理化性质对土壤水蒸气吸附动力学的影响
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-10 DOI: 10.1111/ejss.70195
Zizheng Deng, Chong Chen, Xue Song, Jianying Shang, Hu Zhou

Soil water vapour sorption kinetics is of great significance to understanding the soil water cycle and soil water vapour movement in arid areas. However, the differences and influencing factors of soil water vapour sorption kinetics in different adsorption processes are still not completely clear. Thus, this study aimed to investigate the soil water vapour adsorption/desorption rates (Ra/Rd) for various water activity (aw) levels and to identify the key factors affecting these rates. In this study, we determined the change of Ra and Rd with aw and the Ra and Rd during the monolayer adsorption (aw = 0.05–0.02, Ra0 and Rd0), multilayer adsorption (aw = 0.2–0.6, Ram and Rdm), and condensation (aw = 0.6–0.93, Rac and Rdc) processes for eight mineral soils with different clay contents and mineralogies using a fully-automated AquaLab Vapour Sorption Analyser in dynamic dewpoint isotherm (DDI) mode. Across the entire aw range, the Ra varied from 2.18 × 10−5 to 1.85 × 10−4 g g−1 min−1, and the Rd varied from 2.23 × 10−5 to 3.93 × 10−4 g g−1 min−1. The adsorption rate was in the order of Ra0 > Ram>Rac, and the desorption rate was in the order of Rdc>Rdm > Rd0. The ratios of adsorption and desorption rates Ra0/Rd0, Ram/Rdm, and Rac/Rdc are 2.82, 0.97, and 0.48, respectively. The monolayer adsorption rate exceeded its desorption rate, while multilayer adsorption exhibited comparable kinetics to desorption. Adsorption kinetics during capillary condensation exhibited significant retardation compared to desorption dynamics. Cation exchange capacity (CEC) and total specific surface area (SSA) were significant determinants of adsorption–desorption kinetic parameters (Ra0, Rd0, Ram, Rdm, and Rac), whereas pore volume (PV) and clay content showed no statistically significant correlation with these kinetic metrics. In contrast, clay content, external SSA, and PV emerged as key factors affecting the Rac, while CEC and total SSA exhibited negligible influence on this parameter.

土壤水蒸气吸附动力学对认识干旱区土壤水循环和土壤水蒸气运动具有重要意义。然而,不同吸附过程中土壤水蒸气吸附动力学的差异及影响因素尚不完全清楚。因此,本研究旨在研究不同水活度(aw)水平下土壤水蒸气吸附/解吸速率(Ra/Rd),并确定影响这些速率的关键因素。在本研究中,我们使用全自动AquaLab蒸汽吸附分析仪在动态露点等温线(DDI)模式下,测定了8种不同粘土含量和矿物学的矿质土在单层吸附(aw = 0.05 ~ 0.02, Ra0和Rd0)、多层吸附(aw = 0.2 ~ 0.6, Ram和Rdm)和冷凝(aw = 0.6 ~ 0.93, Rac和Rdc)过程中Ra和Rd随aw的变化,以及Ra和Rd随aw的变化。在整个光谱范围内,Ra在2.18 × 10−5到1.85 × 10−4 g g−1 min−1之间变化,Rd在2.23 × 10−5到3.93 × 10−4 g g−1 min−1之间变化。吸附速率为Ra0 >; Ram>Rac,解吸速率为Rdc>;Rdm > Rd0。吸附速率Ra0/Rd0、Ram/Rdm和Rac/Rdc分别为2.82、0.97和0.48。单层吸附速率大于脱附速率,多层吸附速率与脱附速率相当。与脱附动力学相比,毛细冷凝过程中的吸附动力学表现出明显的延迟。阳离子交换容量(CEC)和总比表面积(SSA)是吸附-解吸动力学参数(Ra0、Rd0、Ram、Rdm和Rac)的重要决定因素,而孔隙体积(PV)和粘土含量与这些动力学参数没有统计学上的显著相关性。粘土含量、外部SSA和PV是影响Rac的关键因素,而CEC和总SSA对Rac的影响可以忽略不计。
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引用次数: 0
Effect of Manual Sample Dosing Techniques on Soil Particle Size Distribution Measured via Laser Diffraction 人工加样技术对激光衍射测量土壤粒度分布的影响
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-10 DOI: 10.1111/ejss.70196
Stanislav Paseka

Accurate determination of the soil particle size distribution (PSD) is critical for a wide range of environmental, agronomic, and geotechnical applications. Laser diffraction method (LDM) has gained popularity because of its speed and reproducibility; however, it remains sensitive to sample preparation and introduction methods. This study evaluated the impact of three manual dosing techniques on PSD results obtained via laser diffraction for seven USDA-classified soil types, with the pipette method used as a reference. Each technique (A: pipetted suspension; B: semiliquid paste; C: dried material) was applied to 1050 measurements. The results revealed a systematic underestimation of clay and overestimation of silt fractions across all LDM techniques, with Technique A yielding the highest relative standard deviation (average RSD for clay: 16.8%; sand: 26.9%). Techniques B and C showed markedly better repeatability (clay RSDs: 7.1% and 10.2%, respectively), with silt exhibiting the highest measurement precision overall (mean RSD: 6.7%). One-way analysis of variance (ANOVA) confirmed that the choice of dosing technique significantly affected the measured clay fraction (p < 0.001), whereas no statistically significant differences were found for silt or sand. All the laser-based techniques misclassified the soil texture in the USDA triangle, with most samples shifting to silt-dominated groups regardless of the true origin. These findings highlight that while LDM itself introduces systematic biases in PSD estimation, the choice of manual dosing technique—particularly uncontrolled suspension pipetting (Technique A)—further amplifies measurement variability, rendering it unsuitable for high-precision applications. These findings highlight the strong influence of manual dosing on LDM outcomes and confirm the unsuitability of uncontrolled suspension pipetting (Technique A) in precision analysis. Recommendations are provided for standardized manual procedures that can improve reproducibility and classification accuracy in soil laboratories.

准确测定土壤粒度分布(PSD)对于广泛的环境、农艺和岩土工程应用至关重要。激光衍射法(LDM)因其速度快、重现性好而得到广泛应用;然而,它仍然对样品制备和引入方法敏感。本研究以移液法为参照,评估了三种人工给药技术对7种美国农业部分类土壤类型激光衍射所得PSD结果的影响。每种技术(A:移液悬浮液;B:半液体膏状;C:干燥材料)应用于1050次测量。结果显示,在所有的LDM技术中,对粘土组分的系统性低估和对粉砂组分的系统性高估,其中技术a产生的相对标准偏差最高(粘土的平均RSD为16.8%,砂的平均RSD为26.9%)。方法B和方法C具有较好的重复性(粘土RSD分别为7.1%和10.2%),其中粉土的测量精度最高(平均RSD为6.7%)。单因素方差分析(ANOVA)证实,给药技术的选择显著影响了测量的粘土含量(p < 0.001),而在淤泥或沙子中没有发现统计学上的显著差异。所有基于激光的技术都错误地分类了美国农业部三角地区的土壤质地,大多数样本都转移到淤泥为主的群体,而不管真正的来源。这些发现强调,虽然LDM本身在PSD估计中引入了系统偏差,但手动给药技术的选择——特别是不受控制的悬液移液(技术A)——进一步放大了测量的可变性,使其不适合高精度应用。这些发现强调了人工给药对LDM结果的强烈影响,并证实了不受控制的悬浮移液(技术A)在精度分析中的不适用性。为标准化的手工程序提供了建议,这些程序可以提高土壤实验室的可重复性和分类准确性。
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引用次数: 0
The Language of Soil: Learning the Lessons From Climate Change 土壤的语言:从气候变化中吸取教训
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-09 DOI: 10.1111/ejss.70188
Karolina Trdlicova, Roy Neilson

The issues of both soil health and climate change can be characterised as a so called ‘wicked problem’. We adopt this shared characteristic as a rationale for applying lessons from climate change communications to suggest an appropriate ‘language of soil’ that should be deployed to effectively communicate the pertinent issue(s) of soil health. Using six recognised examples of climate change communication pitfalls, we illustrate why inciting a sense of dread around soil and why setting ‘soil health’ deadlines are not helpful strategies to promote positive action on soils. We also discuss the value-action gap and the way in which it applies to soil communication and why it is important to avoid the ‘trap’ of the knowledge deficit model. Finally, we stress the importance of communicating actions rather than knowledge as well as the importance of ‘credible’ soil health communicators.

土壤健康和气候变化的问题可以被描述为所谓的“邪恶问题”。我们采用这一共同特征作为应用气候变化沟通经验教训的基本原理,提出一种适当的“土壤语言”,应用于有效沟通土壤健康的相关问题。通过六个公认的气候变化传播陷阱的例子,我们说明了为什么煽动对土壤的恐惧感以及为什么设定“土壤健康”的最后期限并不是促进土壤积极行动的有益策略。我们还讨论了价值-行动差距及其应用于土壤沟通的方式,以及为什么避免知识赤字模型的“陷阱”很重要。最后,我们强调传播行动而不是知识的重要性,以及“可靠的”土壤健康传播者的重要性。
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引用次数: 0
Using Digital Soil Mapping to Create Spatial Off-Road Driving Guidelines and Optimal Road Networks in the Phinda Reserve 利用数字土壤制图在Phinda保护区创建空间越野驾驶指南和最优道路网络
IF 3.8 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2025-09-03 DOI: 10.1111/ejss.70182
G. M. van Zijl, G. P. Nortjé, P. J. Fourie

Protected areas are often thought of as pristine natural environments. Practically however, protected areas are often degraded. In Africa, protected areas are mostly funded through game viewing tourism, where development of the road network to enable game viewing often leads to land degradation. Furthermore, off-road driving is common in such game parks, leading to soil compaction and crusting. Guidelines for sustainable road network development and off-road driving exist but are impossible to apply without a soil map of the game reserve. This paper shows how a digital soil map can be used to create spatial off-road driving guidelines for the Phinda Game Reserve in South Africa. Phinda has a very high road density and therefore an additional aim was to designate roads for closure and rehabilitation, without decreasing the opportunity to view predators. A soil class map with a Kappa value of 0.8 was created using the multinomial logistic regression algorithm and 133 soil observations. A soil sensitivity rating was assigned to each soil class based on the soil properties of the class. The off-driving guideline map showed that off-road driving should be prohibited on 6.7% of the area and can only be practised on 41% of the area when not bare or overgrazed. Using the soil sensitivity map and the locations of accommodation camps and predator sighting hotspots, roads were designated for closure and rehabilitation. In total, 207 km of 17% of roads were designated for closure. These roads were outside of predator hotspot areas and would therefore not negatively affect the touristic experience. This paper gives a blueprint to develop spatial off-road driving guidelines and sustainable road network design in game reserves using digital soil mapping and could be applied to similar game parks throughout Africa.

保护区通常被认为是原始的自然环境。然而,实际上,保护区往往会退化。在非洲,保护区的资金主要来自观赏野生动物旅游,在那里,为了观赏野生动物而开发道路网络往往会导致土地退化。此外,越野驾驶在这些野生动物公园很常见,导致土壤压实和结壳。虽然有可持续道路网络发展和越野驾驶的指导方针,但如果没有野生动物保护区的土壤地图,就不可能适用。本文展示了如何使用数字土壤地图为南非的菲达野生动物保护区创建空间越野驾驶指南。Phinda的道路密度非常高,因此另一个目标是指定道路关闭和修复,而不减少观察捕食者的机会。利用多项logistic回归算法和133份土壤观测资料,建立Kappa值为0.8的土壤类图。根据每个土壤类别的土壤性质,对每个土壤类别进行土壤敏感性评级。越野驾驶指南地图显示,6.7%的区域应禁止越野驾驶,只有41%的区域在没有裸露或过度放牧的情况下才能进行越野驾驶。利用土壤敏感性图和住宿营地和捕食者观察热点的位置,指定道路关闭和修复。总共有207公里,占17%的道路被指定封闭。这些道路位于食肉动物热点地区之外,因此不会对旅游体验产生负面影响。本文为利用数字土壤制图技术在野生动物保护区制定空间越野驾驶指南和可持续道路网络设计提供了蓝图,并可应用于整个非洲的类似野生动物公园。
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引用次数: 0
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European Journal of Soil Science
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