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Vertical and horizontal decreases in soil particle size distribution range along deep soil profiles (∼20 m) in Chinese loess deposits 中国黄土沉积物沿深土层剖面(~ 20 m)的土壤粒径分布范围在垂直和水平方向上呈减小趋势
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-05 DOI: 10.1016/j.still.2025.106987
Zixuan Zhou , Yunqiang Wang , Lijun Qi , Shushi Peng
Soil particle size distribution (PSD), a fundamental and vital soil physical property, influences the physical, chemical and biological processes in terrestrial ecosystems. However, the vertical and horizontal variations of soil PSD have not been fully elucidated in deep soil profiles due to observational constraints, with most knowledge gained from surface soils. Therefore, we obtained a total of 1320 soil samples from 22 soil profiles with a maximum depth of 21 m on a hillslope of the Chinese Loess Plateau, and applied fractal theory (single fractal and multifractal dimensions) to describe soil PSD. We found mean values of D (the single fractal dimension), D0 (the capacity dimension, representing the PSD's range), D1 (the information entropy dimension, representing the PSD's concentration), D2 (the correlation dimension, representing the PSD's uniformity), D1/D0, Δα (representing the distribution’s heterogeneity of the whole fractal structure) and Δf (representing the asymmetry characteristic of the singularity spectra) in loess deposits were 2.20 ± 0.06, 0.94 ± 0.02, 0.85 ± 0.01, 0.80 ± 0.02, 0.90 ± 0.02, 2.31 ± 0.45, and 0.57 ± 0.07 (mean ± standard deviation), respectively. Mean values of D, D0, D1, D2, Δα and Δf decreased with soil depth, while D1/D0 increased with depth, suggesting the overall homogeneity of PSD increased within 0–21 m soil profiles in the Loess Plateau. Additionally, D0 decreased significantly along deep soil profiles in both vertical and horizontal directions, indicating that the PSD occupied a relatively narrower range in deeper soil layers compared with the surface. In summary, our study confirms that the spatial heterogeneity of the PSD decreased with soil depth in loess deposits, mainly manifested in a reduced multifractal dimension D0 (i.e., the PSD's range decreased), which improves the fundamental knowledge for predicting deep soil properties in Earth's Critical Zone.
土壤粒度分布(PSD)是土壤的基本和重要的物理性质,影响着陆地生态系统的物理、化学和生物过程。然而,由于观测的限制,土壤PSD的垂直和水平变化尚未完全阐明深层土壤剖面,大部分知识来自表层土壤。因此,我们在黄土高原某山坡上获取了22个土壤剖面的1320个土壤样品,最大深度为21 m,并应用分形理论(单分形和多重分形维数)来描述土壤PSD。结果表明,黄土沉积层的D(单分形维数)、D0(容量维数,代表PSD的范围)、D1(信息熵维数,代表PSD的浓度)、D2(相关维数,代表PSD的均匀性)、D1/D0、Δα(代表整个分形结构的分布非均质性)和Δf(代表奇异谱的不对称特征)的平均值分别为2.20 ± 0.06、0.94 ± 0.02、0.85 ± 0.01,分别为0.80 ± 0.02、0.90 ± 0.02、2.31 ± 0.45、0.57 ± 0.07(均值±标准差)。D、D0、D1、D2、Δα和Δf的平均值随土层深度的增大而减小,而D1/D0随土层深度的增大而增大,表明黄土高原0 ~ 21 m土壤剖面内PSD的整体均匀性增强。此外,在垂直和水平方向上,D0沿深层土壤剖面均显著减小,表明PSD在深层土壤中所占范围相对较窄。综上所述,我们的研究证实了黄土沉积物PSD的空间异质性随着土壤深度的增加而降低,主要表现为多重分形维数D0的减小(即PSD的范围减小),这为预测地球临界带深部土壤性质提供了基础知识。
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引用次数: 0
Occasional tillage in no-till systems: A global meta-analysis on its frequency, causes, and agronomic implications 免耕系统中的不定期耕作:一项关于其频率、原因和农艺学意义的全球元分析
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-15 DOI: 10.1016/j.still.2025.107022
Yanfei Yan , Haoyu Li , Min Zhang , Xiwei Liu , Yaokuo Wang , Lingxin Zhang , Zhijian Ma , Yuxian Jiang , Min Yang , Ruiguo Cai
No-tillage (NT) is a crucial component of conservation tillage and an efficient approach for implementing sustainable agriculture. However, prolonged NT (≥5 years) may have negative impacts, such as soil compaction, weed control issues, and increased incidence of soil- and plant-vectored infections, which ultimately reduce crop yields, especially when NT is adopted alone and not together with the other pillars of conservation agriculture. In cases where such problems occur, occasional tillage (OT) has been proposed as a potential solution to alleviate these problems, but it is unclear how often NT systems should be tilled to optimize yields. Thus, we conducted a meta-analysis to assess how OT affects crop yields and soil properties, as well as identifying the key factors that determine yield performance and the operational time required for OT in long-term NT systems. We investigated the effects of OT versus NT on crop yields and soil properties based on 94 articles and 1079 paired comparisons from around the world. The results showed that OT significantly increased crop yields (overall effect value for all crops) by 3.2 % compared with NT. The key factors that influenced crop yields under OT included tillage practices, crop types, mean annual temperature (MAT), experimental duration (ED), mean annual precipitation (MAP), and soil type. Specifically, the yield response to OT varied significantly among subgroups. Notably higher relative increases were observed for Phaeozems (WRB classification; 26.4 %), subsoiler use (>30 cm depth; 7.1 %), wheat (Triticum aestivum L.; 6.3 %), biannual cropping (5.5 %), and under specific climatic conditions (MAT 8–16℃: 6.8 %; MAP >1200 mm: 3.6 %). Critically, a single OT operation was most effective when implemented early in the NT phase (<6 years), coinciding with the initial onset of soil compaction. Compared with NT, OT led to reductions in the soil bulk density, soil organic carbon, and total nitrogen, and improved the soil water content, soil porosity, available phosphorus and potassium. These changes in the soil properties partly explain the crop yield increases under OT. In summary, this meta-analysis demonstrates that OT is an effective strategy for mitigating the adverse effects of long-term NT under specific conditions to promote sustainable agricultural development. However, adopting OT requires a careful assessment of local conditions and system-specific constraints to ensure its efficacy and sustainability.
免耕是保护性耕作的重要组成部分,是实现农业可持续发展的有效途径。然而,延长NT(≥5年)可能会产生负面影响,如土壤压实、杂草控制问题以及土壤和植物媒介感染的发生率增加,最终会降低作物产量,特别是当单独采用NT而不是与保护性农业的其他支柱一起采用时。在这些问题发生的情况下,偶尔耕作(OT)已被提议作为缓解这些问题的潜在解决方案,但不清楚NT系统应多久进行一次耕作以优化产量。因此,我们进行了一项荟萃分析,以评估OT如何影响作物产量和土壤性质,以及确定长期NT系统中决定产量表现和OT所需操作时间的关键因素。我们基于来自世界各地的94篇文章和1079对比较,研究了OT和NT对作物产量和土壤性质的影响。结果表明:与NT相比,OT显著提高了作物产量(所有作物的综合效应值)3.2 %。影响OT下作物产量的关键因素包括耕作方式、作物类型、年平均温度(MAT)、试验持续时间(ED)、年平均降水量(MAP)和土壤类型。具体来说,不同亚组对OT的产量反应差异显著。稻瘟病(WRB分类;26.4 %)、深耕(>;30 cm深度;7.1 %)、小麦(Triticum aestivum L.; 6.3 %)、一年生两熟(5.5 %)和特定气候条件下(MAT 8-16℃:6.8 %;MAP >1200 mm: 3.6 %)的相对增幅显著。关键是,在NT阶段早期(6年)实施单次OT作业最有效,与土壤压实的初始开始相吻合。与NT相比,OT降低了土壤容重、土壤有机碳和全氮,提高了土壤含水量、孔隙度、速效磷和速效钾。这些土壤性质的变化在一定程度上解释了OT下作物产量的增加。综上所述,本荟萃分析表明,在特定条件下,OT是缓解长期NT不利影响、促进农业可持续发展的有效策略。然而,采用OT需要仔细评估当地条件和系统特有的限制,以确保其有效性和可持续性。
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引用次数: 0
Regenerative agriculture effects on biomass, drought resilience and 14C-photosynthate allocation in wheat drilled into ley compared to disc or ploughed arable soil 再生农业对钻地小麦生物量、抗旱性和14c -光合作用分配的影响
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2026-01-07 DOI: 10.1016/j.still.2025.107016
Nichola Austen , Elizabeth Short , Stefanie Tille , Irene Johnson , Richard Summers , Duncan D. Cameron , Jonathan R. Leake
Regenerative agriculture practices including leys and no-tillage facilitate biological reassembly of soil aggregates, increasing water, carbon and nutrient storage, but how this effects crop biomass, photosynthate partitioning, and drought resilience is unclear. To address this, we took monoliths growing semi-dwarf and taller wheat genotypes from 3-year plots that were ploughed or disc cultivated, or direct-drilled into a grass-clover ley and applied 35 kg N ha−1. Half the monoliths received a spring drought, then all were watered and the wheat 14CO2 pulse-labelled at stem elongation. The ley soil had lower bulk density, stored more water, and the taller wheat genotype maintained 8-fold higher proportion of water-stable macroaggregates despite unexpectedly having the smaller root biomass. Yields on the ley soil (3.74 t ha−1) were 77 % −123 % higher than on ploughed and disc cultivated soils, and unaffected by genotype or drought, despite its > 70 % reduction in root biomass. Of the 14C initially retained in wheat, 72 % was in shoots, with root allocation decreasing by 75–90 % in droughted ley soil, and at harvest soil retained < 1 % of the 14C, with significantly lower values for taller wheat, and ley. We conclude that soil health regeneration in the ley enhanced wheat yields, but reduced photosynthate allocation to root biomass under drought. Although taller wheat maintained better macroaggregation in ley soil, this was not explained by root biomass or photosynthate allocation and unexpectedly failed to increase soil 14C sequestration. We find no evidence that ley regeneration of macroaggregation enhances soil C sequestration under wheat, despite higher yields.
包括轮作和免耕在内的再生农业实践促进了土壤团聚体的生物重组,增加了水分、碳和养分的储存,但这如何影响作物生物量、光合作用分配和抗旱能力尚不清楚。为了解决这一问题,我们从3年耕地、盘耕或直接钻入草-三叶草地的半矮秆和高基因型小麦中选取了大块生长体,施用35 kg N ha - 1。其中一半植株在春季干旱,然后所有植株都浇水,并在茎秆伸长时进行14CO2脉冲标记。禾草土壤容重较低,储水量较大,高基因型小麦的根系生物量较低,但水稳性大团聚体的比例却高出8倍。犁地土壤的产量(3.74 t ha - 1)比翻耕和盘耕土壤高77 % - 123 %,尽管根系生物量减少了>; 70 %,但不受基因型和干旱的影响。小麦初始保留14C的72% %在茎部,干旱麦田土壤的根系分配减少75 ~ 90% %,收获时土壤保留14C的<; 1 %,高小麦和麦田的14C值显著降低。我们认为,干旱条件下,麦田土壤健康更新提高了小麦产量,但减少了根系生物量的光合作用分配。尽管高小麦在低土壤中保持了更好的大团聚,但这不能用根系生物量或光合分配来解释,而且出乎意料地未能增加土壤的14C固存。我们没有发现证据表明,尽管小麦产量较高,但大团聚体的土壤再生增强了土壤碳的固存。
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引用次数: 0
Thickness variation of black soil on sloping farmland in northeast China from 1963 to 2023 1963 - 2023年东北坡耕地黑土厚度变化
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-06 DOI: 10.1016/j.still.2025.107005
Chang Liu , Gang Liu , Chenxi Dan , Enshuai Shen , Ya Liu , Qiong Zhang , Han Luo , Chutian Zhang , Zhen Guo , Kaishan Song
The black soil thickness (BST) serves as a critical indicator for assessing soil quality in northeast China. Nevertheless, the spatial distribution and variability of BST in sloping farmland remain inadequately understood. Especially, after many years of cultivation and erosion, this spatial variability increased. The aim of this research is to examine the variations in the BST on sloping farmland over the past semi-century. Three slopes in 150–200 m length with shapes of straight, convex, and concave in Bin County, Heilongjiang Province, were selected. The 137Cs nuclide tracing technology and ground-penetrating radar technology were utilized to analyze the distribution characteristics of soil erosion-deposition and BST on the three slopes, respectively. Furthermore, the distribution characteristics of BST on the three slopes over the past semi-century were reconstructed by using the historical soil erosion-deposition rates. The findings revealed that the soil erosion rate, arranged in descending order, are as follows: concave slope, convex slope, straight slope. The average BST in 2023 is as follows: convex slope > straight slope > concave slope, whereas in 1963 is as follows: concave slope > convex slope > straight slope. The reconstructed BST indicates notable variations in thickness across different shapes of slopes. In the past semi-century, the average soil erosion rate on three slopes were 0.17 cm a−1. However, the processes of erosion and deposition occurring on concave and convex slopes resulted solely in alterations to the local slope gradient, without influencing the overall classification of the slope type. Consequently, this study provided a precise depiction of the spatial variation characteristics and thinning rate of the black soil in past years, that can furnish a scientific foundation for forecasting soil erosion and safeguarding black soil resources.
黑土厚度(BST)是评价东北地区土壤质量的重要指标。然而,目前对坡耕地BST的空间分布和变异的认识还不够充分。特别是经过多年的种植和侵蚀,这种空间变异性增加。本研究的目的是研究过去半个世纪以来坡耕地BST的变化。选取黑龙江省宾县境内3个长度为150 ~ 200 m、形状为直、凸、凹的斜坡。利用137Cs核素示踪技术和探地雷达技术分别分析了3个坡面土壤侵蚀沉积和BST的分布特征。在此基础上,利用历史土壤侵蚀沉积速率重建了近半个世纪来3个坡面BST的分布特征。结果表明:土壤侵蚀速率由高到低依次为:凹坡、凸坡、直坡;2023年的平均BST为:凸坡>; 直坡>; 凹坡,1963年为:凹坡>; 凸坡>; 直坡。重建的BST在不同形状的斜坡上的厚度有显著的变化。在过去的半个世纪里,三个斜坡的平均土壤侵蚀速率为0.17 cm a−1。然而,凹坡和凸坡上的侵蚀和沉积过程仅导致局部坡度的变化,而不影响边坡类型的总体分类。因此,本研究准确地描述了黑土历年的空间变化特征和疏化速率,可为预测土壤侵蚀和保障黑土资源提供科学依据。
{"title":"Thickness variation of black soil on sloping farmland in northeast China from 1963 to 2023","authors":"Chang Liu ,&nbsp;Gang Liu ,&nbsp;Chenxi Dan ,&nbsp;Enshuai Shen ,&nbsp;Ya Liu ,&nbsp;Qiong Zhang ,&nbsp;Han Luo ,&nbsp;Chutian Zhang ,&nbsp;Zhen Guo ,&nbsp;Kaishan Song","doi":"10.1016/j.still.2025.107005","DOIUrl":"10.1016/j.still.2025.107005","url":null,"abstract":"<div><div>The black soil thickness (BST) serves as a critical indicator for assessing soil quality in northeast China. Nevertheless, the spatial distribution and variability of BST in sloping farmland remain inadequately understood. Especially, after many years of cultivation and erosion, this spatial variability increased. The aim of this research is to examine the variations in the BST on sloping farmland over the past semi-century. Three slopes in 150–200 m length with shapes of straight, convex, and concave in Bin County, Heilongjiang Province, were selected. The <sup>137</sup>Cs nuclide tracing technology and ground-penetrating radar technology were utilized to analyze the distribution characteristics of soil erosion-deposition and BST on the three slopes, respectively. Furthermore, the distribution characteristics of BST on the three slopes over the past semi-century were reconstructed by using the historical soil erosion-deposition rates. The findings revealed that the soil erosion rate, arranged in descending order, are as follows: concave slope, convex slope, straight slope. The average BST in 2023 is as follows: convex slope &gt; straight slope &gt; concave slope, whereas in 1963 is as follows: concave slope &gt; convex slope &gt; straight slope. The reconstructed BST indicates notable variations in thickness across different shapes of slopes. In the past semi-century, the average soil erosion rate on three slopes were 0.17 cm a<sup>−1</sup>. However, the processes of erosion and deposition occurring on concave and convex slopes resulted solely in alterations to the local slope gradient, without influencing the overall classification of the slope type. Consequently, this study provided a precise depiction of the spatial variation characteristics and thinning rate of the black soil in past years, that can furnish a scientific foundation for forecasting soil erosion and safeguarding black soil resources.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107005"},"PeriodicalIF":6.8,"publicationDate":"2026-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145685907","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Soil stoichiometric C/N and nitrogen availability jointly shape fungal and bacterial necromass carbon accumulation across ecosystems 土壤化学计量C/N和氮有效性共同决定了生态系统中真菌和细菌坏死团的碳积累
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-26 DOI: 10.1016/j.still.2025.107042
Baorong Wang , Deng Ao , Chao Liang , Kate Buckeridge , Chunhui Liu , Yang Yang , Yao Li , Huijun Li , Zhongming Wen , Shaoshan An
Microbial necromass constitutes a major and stable component of soil organic carbon (SOC) in terrestrial ecosystems. However, despite plant-derived inputs largely regulate substrate quality and soil organic matter (SOM) carbon to nitrogen (C/N) ratios and shape the composition of living microbial communities, fundamental differences in resource acquisition, death pathways, and residue chemistry between fungi and bacteria decouple living biomass from necromass accumulation. Whether fungal and bacterial necromass are subject to same SOM C/N constraints across ecosystems remains an open question. Here, we combined 1600 global SOM and microbial necromass records from global ecosystems (C/N: 3.8–58) through meta-analysis and 768 field measurement samples from Loess Plateau, spanning croplands, biocrusts, grasslands, shrublands, and forests (C/N: 6–72), representing diverse SOM qualities. We found both fungal and bacterial necromass C increased with rising SOM C/N ratios, and the consistency of this pattern from the Loess Plateau to the global scale underscores a universal role of SOM C/N control in shaping microbial necromass C. Fungal necromass C increased with increasing SOM C/N ratios, reflecting fungi advantage in processing complex organic matter under relatively N-poor conditions. Its accumulation was strongly associated with SOC, total N, and particulate organic C, reinforcing its contribution to SOC accumulation. Conversely, bacterial necromass C responded primarily to dissolved N and microbial biomass C, pointing to distinct, resource-dependent pathways of microbial necromass accumulation across microbial groups. Despite increases in microbial necromass C content and SOM C/N ratios, necromass accumulation coefficient declined, suggesting that N limitation accelerates microbial necromass recycling for biomass production and constrains net storage. Overall, by revealing the dual mechanism of necromass production driven by plant-mediated SOM complexity and necromass reutilization regulated by N availability, this work provides critical insights into the stoichiometric C/N controls shaping microbial necromass dynamics, offering a foundation for strategies to optimize nutrient management and enhance SOC sequestration in future ecosystems.
微生物坏死团块是陆地生态系统土壤有机碳的主要稳定组成部分。然而,尽管植物来源的输入在很大程度上调节了基质质量和土壤有机质(SOM)碳氮比(C/N)并塑造了活微生物群落的组成,但真菌和细菌在资源获取、死亡途径和残留物化学方面的根本差异使活生物量与坏死块积累分离。真菌和细菌坏死块是否在整个生态系统中受到相同的SOM C/N限制仍然是一个悬而未决的问题。通过荟萃分析,我们将1600份全球土壤有机质和微生物坏死块记录(C/N: 3.8 ~ 58)与768份黄土高原农田、生物结皮、草原、灌丛和森林(C/N: 6 ~ 72)的野外测量样本结合起来,表明土壤有机质质量的多样性。研究发现,真菌和细菌的死质C均随有机质C/N的增加而增加,这种模式在黄土高原和全球范围内的一致性表明,有机质C/N的控制在形成微生物死质C方面具有普遍作用。真菌死质C随有机质C/N的增加而增加,反映了真菌在相对缺氮条件下处理复杂有机质的优势。其积累与有机碳、全氮和颗粒有机碳密切相关,增强了其对有机碳积累的贡献。相反,细菌坏死块C主要对溶解的氮和微生物生物量C做出反应,这表明微生物坏死块在微生物群中积累的途径不同,依赖资源。尽管微生物坏死体C含量和SOM C/N比值增加,但坏死体积累系数下降,表明限氮加速了微生物坏死体的生物量循环,限制了净储量。总的来说,通过揭示植物介导的SOM复杂性驱动的坏死物质产生和N有效性调节的坏死物质再利用的双重机制,本工作为化学计量C/N控制形成微生物坏死物质动力学提供了重要的见解,为优化养分管理和增强未来生态系统中有机碳的吸收提供了策略基础。
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引用次数: 0
Integrating soil spectral libraries with laboratory hyperspectral imaging for profile organic carbon prediction in paddy soils 结合土壤光谱库和实验室高光谱成像技术预测水稻土剖面有机碳
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-31 DOI: 10.1016/j.still.2025.107028
Shuo Li , Yuwei Zhou , Abdul Mounem Mouazen , Songchao Chen , Raphael A. Viscarra Rossel , Asim Biswas , Wenjun Ji , Zhou Shi , Shanqin Wang
To promote soil organic carbon (SOC) storage and to meet growing food demand with limited land, it is essential to understand the spatial characteristics of SOC across the entire profile of paddy soils. The establishment of soil spectral libraries (SSLs) at various geographical scales has made near-infrared (NIR: 700–1100 nm) and shortwave-infrared (SWIR: 1100–2500 nm) hyperspectral imaging (HSI) more feasible for the rapid and cost-effective estimation of SOC. This study aimed to integrate SSLs with HSI for fine-scale mapping of elemental concentrations with a high spatial resolution of 1 mm per pixel (image size: 980 × 160 pixels) with a spectral range of 900–1700 nm. We apply SOC-reflectance calibrations from Global Soil Spectral Library (GSSL) to an independent local field site for the entire profile in paddy soils to a depth of 1-m, combined with spectral similarity with continuum removal (SS-CR) analysis, three spectral matching methods (e.g., Euclidean distances [ED], Mahalanobis distances [MD], and Spectral angle mapper [SAM]) and two modeling algorithms (e.g., random forest [RF] and Cubist). Additionally, we compared the performance of different Global and Local models in characterizing the distribution of SOC across the entire profile. Results indicated that although the Cubist-Local model provided good prediction accuracy (R2 ≥ 0.77, RMSE ≤ 0.77 %, RPIQ ≥ 1.90), its ability to fine-scale mapping of the profile SOC was limited. In contrast, the RF-Local model based on the ED spectral matching method (ED-RF-Local) not only achieved the best performance (R2 = 0.80, RMSE = 0.78 %, RPIQ = 1.86), but also successfully mapped SOC across the entire soil profile. This model used two-fifths of the samples compared to the Global model. The findings of this study provide a valuable reference for SOC prediction and mapping at the field scale and across the entire soil profile using HSI techniques and GSSL, emphasizing the potential for predictions in paddy soils with high vertical resolution.
为了促进土壤有机碳(SOC)的储存,在有限的土地条件下满足日益增长的粮食需求,有必要了解水稻土全剖面有机碳的空间特征。不同地理尺度土壤光谱库(SSLs)的建立,使得近红外(NIR: 700-1100 nm)和短波红外(SWIR: 1100-2500 nm)高光谱成像(HSI)技术更有可能实现土壤有机碳的快速、经济估算。本研究旨在将SSLs与HSI相结合,在光谱范围为900-1700 nm的情况下,以1 mm /像素(图像尺寸:980 × 160像素)的高空间分辨率进行元素浓度的精细制图。我们将全球土壤光谱库(GSSL)的soc反射率校准应用于水稻土中1 m深度的独立局部现场,结合光谱相似性与连续体去除(SS-CR)分析,三种光谱匹配方法(例如欧几里得距离[ED],马氏距离[MD]和光谱角度映射[SAM])和两种建模算法(例如随机森林[RF]和Cubist)。此外,我们还比较了不同的Global和Local模型在整个剖面中表征SOC分布的性能。结果表明,虽然cuist - local模型具有较好的预测精度(R2≥0.77,RMSE≤0.77 %,RPIQ≥1.90),但其对剖面SOC的精细映射能力有限。相比之下,基于ED光谱匹配方法的RF-Local模型(ED-RF-Local)不仅表现最佳(R2 = 0.80, RMSE = 0.78 %,RPIQ = 1.86),而且成功地绘制了整个土壤剖面的SOC。与全球模型相比,该模型使用了五分之二的样本。本研究结果为利用HSI技术和GSSL在农田尺度和整个土壤剖面上进行有机碳预测和制图提供了有价值的参考,并强调了高垂直分辨率水稻土的预测潜力。
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引用次数: 0
High-resolution mapping of soil mechanical properties by integrating geophysical sensors and terrain attributes 结合地球物理传感器和地形属性的土壤力学特性高分辨率制图
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2026-01-05 DOI: 10.1016/j.still.2025.107019
Ameesh Khatkar, Triven Koganti, Amélie Beucher, Alvaro Calleja-Huerta, Lars Juhl Munkholm, Mathieu Lamandé
Soil mechanical properties are essential for evaluating its strength and stability when subjected to stress from farm machinery. Conventional methods for measuring these properties are often slow, labour-intensive, and destructive. This study presents a novel approach that utilizes on-the-go proximal soil sensors (PSS), specifically electromagnetic induction (EMI) and gamma-ray spectroscopy (GRS), alongside terrain attributes, to evaluate their effectiveness in estimating three key soil mechanical properties: (1) precompression stress (σpc), (2) compression index (CC), and (3) strain at 100 kPa (Ɛ100kPa). For this, a geophysical survey and soil sampling were conducted across three arable fields, yielding 129 bulk soil samples and 516 intact soil cores (100 cm3) collected from 69 sampling points at two depths (0.15 and 0.40 m). Uniaxial confined compression tests (UCCT) were conducted to measure these mechanical properties, with multiple linear regression (MLR) applied for their estimation and cross-validation with the leave-one-out method (LOOCV). Both site-specific and unified datasets were analyzed, revealing higher prediction accuracy at 0.15 m compared to 0.40 m depth. Among the examined soil mechanical properties, CC was estimated most accurately, followed by σpc and Ɛ100kPa. Estimates of σpc derived from on-the-go PSS combined with terrain attributes substantially outperformed those obtained from the existing pedotransfer function. Furthermore, digital maps of these properties were successfully generated to visualize their spatial variability at the field scale. This study shows that on-the-go PSS provide a rapid, field-scale and non-destructive framework for estimating soil mechanical properties, supporting improved soil compaction assessment and monitoring.
土壤的力学特性是评估其强度和稳定性的关键,当受到农业机械的应力。测量这些特性的传统方法通常是缓慢的、劳动密集型的和破坏性的。本研究提出了一种新颖的方法,利用即时近端土壤传感器(PSS),特别是电磁感应(EMI)和伽马射线能谱(GRS),以及地形属性,来评估它们在估计三个关键土壤力学特性方面的有效性:(1)预压缩应力(σpc),(2)压缩指数(CC)和(3)100kPa应变(Ɛ100kPa)。为此,在三个耕地上进行了地球物理调查和土壤取样,从两个深度(0.15和0.40 m)的69个采样点收集了129个散装土壤样品和516个完整土壤岩心(100 cm3)。采用单轴密闭压缩试验(UCCT)来测量这些力学性能,并采用多元线性回归(MLR)进行估计,并用留一法(LOOCV)进行交叉验证。对特定站点和统一数据集进行了分析,发现0.15 m深度的预测精度高于0.40 m深度。所测土壤力学性质中,CC最准确,σpc次之,Ɛ100kPa次之。结合地形属性的动态PSS估算的σpc值明显优于现有土壤传递函数估算的σpc值。此外,成功地生成了这些属性的数字地图,以可视化它们在野外尺度上的空间变异性。该研究表明,移动PSS为估算土壤力学特性提供了快速、现场规模和非破坏性的框架,支持改进的土壤压实评估和监测。
{"title":"High-resolution mapping of soil mechanical properties by integrating geophysical sensors and terrain attributes","authors":"Ameesh Khatkar,&nbsp;Triven Koganti,&nbsp;Amélie Beucher,&nbsp;Alvaro Calleja-Huerta,&nbsp;Lars Juhl Munkholm,&nbsp;Mathieu Lamandé","doi":"10.1016/j.still.2025.107019","DOIUrl":"10.1016/j.still.2025.107019","url":null,"abstract":"<div><div>Soil mechanical properties are essential for evaluating its strength and stability when subjected to stress from farm machinery. Conventional methods for measuring these properties are often slow, labour-intensive, and destructive. This study presents a novel approach that utilizes on-the-go proximal soil sensors (PSS), specifically electromagnetic induction (EMI) and gamma-ray spectroscopy (GRS), alongside terrain attributes, to evaluate their effectiveness in estimating three key soil mechanical properties: (1) precompression stress (σ<sub>pc</sub>), (2) compression index (C<sub>C</sub>), and (3) strain at 100 kPa (Ɛ<sub>100kPa</sub>). For this, a geophysical survey and soil sampling were conducted across three arable fields, yielding 129 bulk soil samples and 516 intact soil cores (100 cm<sup>3</sup>) collected from 69 sampling points at two depths (0.15 and 0.40 m). Uniaxial confined compression tests (UCCT) were conducted to measure these mechanical properties, with multiple linear regression (MLR) applied for their estimation and cross-validation with the leave-one-out method (LOOCV). Both site-specific and unified datasets were analyzed, revealing higher prediction accuracy at 0.15 m compared to 0.40 m depth. Among the examined soil mechanical properties, C<sub>C</sub> was estimated most accurately, followed by σ<sub>pc</sub> and Ɛ<sub>100kPa</sub>. Estimates of σ<sub>pc</sub> derived from on-the-go PSS combined with terrain attributes substantially outperformed those obtained from the existing pedotransfer function. Furthermore, digital maps of these properties were successfully generated to visualize their spatial variability at the field scale. This study shows that on-the-go PSS provide a rapid, field-scale and non-destructive framework for estimating soil mechanical properties, supporting improved soil compaction assessment and monitoring.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107019"},"PeriodicalIF":6.8,"publicationDate":"2026-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145902300","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
While legume-based rotation influences the chemical composition of mineral-associated organic matter, tillage has little effect on its persistence 以豆科植物为基础的轮作影响矿物相关有机质的化学组成,而耕作对其持久性影响不大
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-11 DOI: 10.1016/j.still.2025.107014
Paulina B. Ramírez , Surendra Singh , Stephen Machado , Roser Matamala , Shikha Singh , Francisco Calderón
Legume-based rotations are key to enhancing soil carbon (C) storage in stable forms such as mineral-associated organic matter (MAOM), improving soil health, and helping maintain long-term C stock. This study investigates how plant inputs and tillage practices influence the distribution, composition, and persistence of MAOM in wheat cropping systems when legumes are incorporated into the rotation. Soil samples were collected from Walla Walla silty loam of northeast Oregon, including conventional tillage (CT) and no-till (NT) treatments in a long-term dryland winter wheat (Triticum aestivum L.) and spring pea (Pisum sativum L.) rotation experiment, with an adjacent grass pasture (GP) plot serving as the baseline. Bulk soil, particulate organic matter (POM), and MAOM fractions were scanned using mid-infrared (Mid-IR) spectroscopy and analyzed for total C and nitrogen (N) as well as radiocarbon age, aggregate stability, and mineralizable C. In WP systems, NT promoted greater C accumulation and stabilization in MAOM than CT, reaching levels similar to those under native GP conditions. Furthermore, our findings indicate that decades of continuous legume-based rotation were insufficient to restore total bulk C content to levels observed in the undisturbed reference site (GP) in the 0–30 cm layer, with increases limited to the surface layer. The Mid-IR data provided insights into how cultivation may alter the chemical composition of MAOM. An increase in amide bands was observed in GP, while legume-based rotation systems favored an abundance of aliphatic (C-H) components in the MAOM fraction. In cultivated soils, C in MAOM exhibited longer residence times under arable conditions than in grassland, while POM remained an actively cycled pool across all treatments. Despite variations in the chemical composition of MAOM across treatments, mineralizable C emissions from MAOM fractions remained statistically unchanged during the 96-hour incubation period. Our findings suggest that soil physical protection, enhanced by reduced tillage, is the primary factor influencing MAOM cycling.
豆类轮作是提高土壤碳(C)以矿物相关有机质(MAOM)等稳定形式储存、改善土壤健康和帮助维持长期碳储量的关键。本研究调查了当豆类轮作时,植物投入和耕作方式如何影响小麦种植系统中MAOM的分布、组成和持久性。在美国俄勒冈州东北部的Walla Walla粉质壤土上采集土壤样品,采用常规耕作(CT)和免耕(NT)处理,以相邻草地(GP)小区为基准,进行旱地冬小麦(Triticum aestivum L.)和春豌豆(Pisum sativum L.)长期轮作试验。利用中红外(Mid-IR)光谱扫描土壤、颗粒有机质(POM)和MAOM组分,并分析总C和氮(N)、放射性碳年龄、团聚体稳定性和可矿化C。在WP系统中,NT比CT促进MAOM中更多的C积累和稳定,达到与原生GP条件相似的水平。此外,我们的研究结果表明,连续数十年的豆科植物轮作不足以将0-30 cm层未受干扰的参考点(GP)的总体积C含量恢复到观测到的水平,增加仅限于表层。中红外数据提供了培养如何改变MAOM化学成分的见解。在GP中观察到酰胺带的增加,而豆科植物为基础的旋转系统有利于MAOM部分中脂肪族(C-H)成分的丰富。在耕地土壤中,土壤中碳在耕地条件下的停留时间比在草地条件下更长,而POM在所有处理下都是一个活跃的循环池。尽管不同处理的MAOM的化学成分有所不同,但在96小时的孵育期间,MAOM馏分的可矿化C排放量在统计上保持不变。研究结果表明,减少耕作所增强的土壤物理保护是影响MAOM循环的主要因素。
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引用次数: 0
Long-term green manure incorporation increases soil carbon sequestration and improves aggregate stability by changing organic carbon components 长期施用绿肥可通过改变有机碳组分增加土壤固碳,提高团聚体稳定性
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-23 DOI: 10.1016/j.still.2025.107024
Yulu Chen , Li Huang , Shaomin Huang , Tengfei Guo , Shuiqing Zhang , Doudou Guo , Xiao Song , Shijie Ding , Muhammad Mehran , Yongqiang Yang , Ke Yue , Sumiao Su , Mingjian Geng , Huimin Zhang
Dissolved organic carbon (DOC), the most labile fraction of soil organic carbon (SOC), plays a vital role in ecosystem functioning and soil productivity. However, the influence of long-term green manure application on DOC composition and its role in soil aggregate formation and carbon stabilization remains unclear. This study investigated changes in DOC composition and their effects on aggregate stability and carbon sequestration in two rice-green manure rotation trials long-5 years in Jingzhou (JZ) and 36 years in Qiyang (QY), China. Treatments included rice-winter fallow (WF), rice-Chinese milk vetch (MV), rice-oilseed rape (RP), and rice-ryegrass (RG). At the JZ test site, 5-year MV incorporation slightly improved aggregate stability, measured by mean weight diameter (MWD) and geometric mean diameter (GMD), but without significant changes. In contrast, at QY, 36-year MV and RG incorporation significantly enhanced both MWD and GMD. Green manure addition increased SOC and DOC contents and enhanced the molecular complexity of DOC, reflected by higher molecular weight, aromaticity, and humification degree. DOC was primarily derived from plant residues and microbial metabolites, with green manure application enhancing microbial contributions. Fluorescence spectroscopy identified three DOC components: bioavailable, humic-like, and protein-like. While DOC composition at JZ remained largely unchanged after 5 years of MV incorporation, 36 years of MV and RG incorporation at QY facilitated the transformation of protein-like into humic-like components. SOC, humic-like DOC, and the humification index (HIX), were the key drivers of aggregate stability, showing direct positive effects on aggregate MWD. Humic-like DOC indirectly promoted SOC accumulation through increased DOC aromaticity and enhanced humification. Our findings highlight the central role of humic-like DOC in enhancing SOC sequestration and soil aggregate stabilization, underscoring the long-term benefits of green manure in sustainable agriculture.
溶解有机碳(DOC)是土壤有机碳(SOC)中最不稳定的部分,在生态系统功能和土壤生产力中起着至关重要的作用。然而,长期施用绿肥对土壤DOC组成的影响及其在土壤团聚体形成和碳稳定中的作用尚不清楚。研究了荆州5年和祁阳36年两个水稻-绿肥轮作试验中DOC组成的变化及其对团聚体稳定性和固碳的影响。处理包括水稻-冬休(WF)、水稻-豇豆(MV)、水稻-油菜(RP)和水稻-黑麦草(RG)。在JZ试验场,通过平均重量直径(MWD)和几何平均直径(GMD)测量,5年MV掺入略微改善了骨料稳定性,但没有显著变化。相比之下,在QY, 36年的MV和RG结合显著提高了MWD和GMD。添加绿肥增加了有机碳和DOC含量,提高了DOC的分子复杂性,表现为分子量、芳香性和腐殖化程度的提高。DOC主要来源于植物残体和微生物代谢产物,绿肥的施用增强了微生物的贡献。荧光光谱鉴定出三种DOC成分:生物可利用性、腐殖质样和蛋白质样。经过5年的MV掺入,JZ处的DOC成分基本保持不变,而QY处36年的MV和RG掺入促进了蛋白样成分向腐殖质样成分的转化。SOC、类腐殖质DOC和腐殖质化指数(HIX)是骨料稳定性的关键驱动因素,对骨料MWD有直接的正向影响。腐殖质样DOC通过增加DOC芳香性和增强腐殖化间接促进有机碳积累。我们的研究结果强调了腐殖质类DOC在增强有机碳固存和土壤团聚体稳定方面的核心作用,强调了绿肥在可持续农业中的长期效益。
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引用次数: 0
Crop planting promotes the stabilization of straw-derived carbon in fertilized soil by regulating soil stoichiometry 作物种植通过调节土壤化学计量来促进施肥土壤中秸秆碳的稳定
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-05-01 Epub Date: 2025-12-09 DOI: 10.1016/j.still.2025.107008
Tengxiao Zhu , Xiuwen Mei , Yuping Li , Shuangyi Li , Tingting An , Jingkuan Wang
Straw returning to cropland is a sustainable management practices to enhance soil organic carbon (SOC) sequestration. The dynamics of straw C transformation in soils have been widely studied, however, it is less clear how crop planting regulates the incorporation of added straw C into SOC pools via soil - microbial nutrients status. We designed two sub- treatments, including single application of 13C-labeled straw (S) and its combination with crop planting (SR) in each fertilization treatment, and then conducted a field micro- experiment for 510 days. Regardless of fertilization, the SR treatments increased the content of straw derived mineral associated organic C (13C-MAOC) by 53.19 % and that of straw- derived particulate organic C (13C-POC) by 27.45 % compared with S treatments on the 510th day. And the SR treatments averagely increased the contribution percentage of straw-derived C in total MAOC by 39.44 %, especially under NP soil. Structure equation modeling results indicated crop planting promotes the formation of straw-derived SOC by reducing soil nutrients (r = −0.141, P < 0.05) and soil nutrients stoichiometry (r = −0.232, P < 0.01); fertilization alleviates nutrient limitations by reducing soil nutrients stoichiometry (r = −0.432, P < 0.001), microbial biomass stoichiometry (r = −0.701, P < 0.001), and increasing soil nutrients (r = 0.584, P < 0.001), thereby regulating the formation of straw C. Our results imply that crop planting contributes long-term incorporation of straw C to stable SOC pool via optimizing nutrients within soil-microbial system.
秸秆还田是加强土壤有机碳固存的一种可持续管理措施。秸秆C在土壤中的转化动力学已经得到了广泛的研究,然而,作物种植如何通过土壤微生物养分状态调节添加的秸秆C进入有机碳库的机制尚不清楚。设计了两个亚处理,分别在每个施肥处理中单独施用13c标记秸秆(S)和与作物种植(SR)相结合,并进行了510 d的田间微试验。在不施肥的情况下,与S处理相比,SR处理第510天秸秆源矿物伴生有机C (13C-MAOC)含量提高了53.19 %,秸秆源颗粒有机C (13C-POC)含量提高了27.45 %。SR处理使秸秆源C对总MAOC的贡献率平均提高了39.44 %,特别是NP土壤下。结构方程建模结果表明,作物种植通过降低土壤养分(r = −0.141,P <; 0.05)和土壤养分化学计量(r = −0.232,P <; 0.01)促进秸秆源有机碳的形成;受精减轻营养限制通过减少土壤养分化学计量学(r = −0.432,P & lt; 0.001),微生物生物量化学计量学(r = −0.701,P & lt; 0.001),并增加土壤养分(r = 0.584,P & lt; 0.001),从而调节的形成秸秆C。我们的研究结果表明,作物种植长期秸秆C整合有助于稳定SOC池通过优化养分在土壤微生物系统。
{"title":"Crop planting promotes the stabilization of straw-derived carbon in fertilized soil by regulating soil stoichiometry","authors":"Tengxiao Zhu ,&nbsp;Xiuwen Mei ,&nbsp;Yuping Li ,&nbsp;Shuangyi Li ,&nbsp;Tingting An ,&nbsp;Jingkuan Wang","doi":"10.1016/j.still.2025.107008","DOIUrl":"10.1016/j.still.2025.107008","url":null,"abstract":"<div><div>Straw returning to cropland is a sustainable management practices to enhance soil organic carbon (SOC) sequestration. The dynamics of straw C transformation in soils have been widely studied, however, it is less clear how crop planting regulates the incorporation of added straw C into SOC pools via soil - microbial nutrients status. We designed two sub- treatments, including single application of <sup>13</sup>C-labeled straw (S) and its combination with crop planting (SR) in each fertilization treatment, and then conducted a field micro- experiment for 510 days. Regardless of fertilization, the SR treatments increased the content of straw derived mineral associated organic C (<sup>13</sup>C-MAOC) by 53.19 % and that of straw- derived particulate organic C (<sup>13</sup>C-POC) by 27.45 % compared with S treatments on the 510th day. And the SR treatments averagely increased the contribution percentage of straw-derived C in total MAOC by 39.44 %, especially under NP soil. Structure equation modeling results indicated crop planting promotes the formation of straw-derived SOC by reducing soil nutrients (<em>r</em> = −0.141, <em>P</em> &lt; 0.05) and soil nutrients stoichiometry (<em>r</em> = −0.232, <em>P</em> &lt; 0.01); fertilization alleviates nutrient limitations by reducing soil nutrients stoichiometry (<em>r</em> = −0.432, <em>P</em> &lt; 0.001), microbial biomass stoichiometry (<em>r</em> = −0.701, <em>P</em> &lt; 0.001), and increasing soil nutrients (<em>r</em> = 0.584, <em>P</em> &lt; 0.001), thereby regulating the formation of straw C. Our results imply that crop planting contributes long-term incorporation of straw C to stable SOC pool via optimizing nutrients within soil-microbial system.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107008"},"PeriodicalIF":6.8,"publicationDate":"2026-05-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145731635","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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