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Within-field variation in root-to-shoot ratios and root traits in spring barley: Implications for estimating carbon inputs 春大麦根冠比和根系性状的田内变化:对估算碳输入的影响
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-07 DOI: 10.1016/j.still.2026.107103
Miyanda Chilipamushi , Claudia von Brömssen , Tino Colombi , Thomas Kätterer , Mats Larsbo
Roots are a major pathway for carbon (C) input into agricultural soils, yet field-scale measurements of belowground C inputs and associated root traits remain limited. Consequently, many soil carbon models rely on fixed root-to-shoot ratios, and root trait variability is rarely considered. In this study, we quantified within-field variation in root-to-shoot ratios and root traits (root diameter, root length density and root tissue density) in spring barley (Hordeum vulgare L.) grown in southwestern Sweden in soil classified as Stagnic Eutric Cambisol, Eutric Stagnosol or Haplic Phaeozem according to the World Reference Base system. Roots (0–40 cm) and shoots were sampled during early to mid-reproductive stage, i.e. milking/early dough development stage, in a 50 × 50 cm grid at 11 sampling locations in the same field in two consecutive years. Shoot and root biomass were not correlated, resulting in variable root-to-shoot ratios (quartile coefficients of variation 7–18 %) and no consistent spatial pattern between years. Root traits displayed clear between year and depth variation, with coarser roots in the topsoil and root tissue densities and root length densities shifting across the profile, reflecting the highly plastic nature of root systems. The spatial variation in root properties in the field could not be explained by basic soil properties. Our findings call for a more mechanistic understanding of the drivers for root-to-shoot ratios and the plastic response of root traits to improve field-scale estimates of root-derived C inputs and SOC modelling accuracy.
根系是碳(C)输入农业土壤的主要途径,但对地下碳输入和相关根系性状的田间测量仍然有限。因此,许多土壤碳模型依赖于固定的根冠比,而根系性状变异很少被考虑。本研究以瑞典西南部生长的春大麦(Hordeum vulgare L.)为研究对象,在世界参考基准系统中被划分为Stagnic Eutric Cambisol、Eutric Stagnosol和Haplic Phaeozem土壤中,对其根冠比和根系性状(根直径、根长密度和根组织密度)的田间变化进行了定量分析。根(0-40 cm)和芽在生育期早期至中期(即挤奶/面团发育早期)连续两年在同一块地的11个采样点取样,网格为50 × 50 cm。地上部生物量与根系生物量不相关,导致地上部比变化较大(四分位数变异系数为7 ~ 18 %),且年份间空间格局不一致。根系性状表现出明显的年、深差异,表层土壤根系粗化,根系组织密度和根长密度在剖面上发生变化,反映了根系的高度可塑性。田间根系性状的空间变异不能用土壤基本性状来解释。我们的研究结果要求对根冠比的驱动因素和根系性状的塑性响应进行更机械的理解,以提高根源碳输入的田间估计和土壤有机碳模型的准确性。
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引用次数: 0
Priming effect is inhibited by 12-year field nitrogen addition in a boreal forest with the extent depending on substrate carbon type 在北方针叶林中,施用12年氮肥对启动效应有抑制作用,抑制程度与底物碳类型有关
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-13 DOI: 10.1016/j.still.2026.107125
Feng Gao , Guoyong Yan , Chao Liang , Guancheng Liu , Lijiang Xu , Yajuan Xing , Liming Yin , Qinggui Wang
Plant carbon inputs can influence soil organic carbon (SOC) decomposition rate, i.e., the priming effect, which can be regulated by nitrogen (N) addition. How long-term N addition affects the priming effect remains unclear yet, especially in boreal forests with severer N limitation. Here, soils were collected from a 12-year in-situ N addition field experiment in a boreal forest, and were incubated with 13C-labeled cellulose and glucose. Further, a global data synthesis was conducted to compare the effect of N addition on priming between simple and complex C types. The results showed that cellulose-induced priming effect was inhibited by on average 150 % by 12-yr N addition. Hydrolytic enzymes were decreased, while oxidases were increased, suggesting a shift in microbial C use strategy in response to C limitation. Subsequently, microbial C use efficiency (CUE) was increased by 12-yr N addition. 68.3 % of the variation in the priming effect among all the treatments was explained by microbial CUE, hydrolytic enzymes and oxidases, reflecting the important role in regulating the priming effect. Compared to glucose, the N inhibited effect on cellulose-induced priming was greater, while the N inhibited effect on substrate-derived CO2-C was lower, broadly supporting the microbial N mining and C utilization hypotheses. Further, the N-inhibited effect on priming caused by complex C was greater than that by simple C across the globe. We highlight that substrate C type should be considered for accurately assessing SOC decomposition via the priming effect in the context of N deposition in boreal forests.
植物碳输入可以影响土壤有机碳(SOC)分解速率,即启动效应,而土壤有机碳(SOC)分解速率可通过添加氮(N)来调节。长期氮添加对启动效应的影响尚不清楚,特别是在氮限制较严重的北方森林中。在这里,从北方针叶林中收集了12年的原位氮添加试验土壤,并与13c标记的纤维素和葡萄糖孵育。此外,进行了全球数据综合,比较了N添加对简单和复杂C型之间启动的影响。结果表明,添加12年N对纤维素诱导的启动效应的抑制作用平均为150 %。水解酶减少,氧化酶增加,表明微生物对C的利用策略发生了变化,以应对C的限制。随后,添加12年N可提高微生物C利用效率(CUE)。各处理间启动效应差异的68.3% %可由微生物CUE、水解酶和氧化酶解释,反映了微生物对启动效应的重要调控作用。与葡萄糖相比,N对纤维素诱导的启动的抑制作用更大,而对底物衍生的CO2-C的抑制作用较低,广泛支持微生物N挖掘和C利用的假设。此外,在全球范围内,复合C对n的抑制作用大于简单C。我们强调,在北方针叶林氮沉降的背景下,基质C类型应该考虑通过启动效应准确评估有机碳分解。
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引用次数: 0
Contribution of Sentinel-1 radar backscatter/coherence and Sentinel-2 optical data to digital mapping of soil organic carbon in the Iberian Peninsula Sentinel-1雷达后向散射/相干和Sentinel-2光学数据对伊比利亚半岛土壤有机碳数字制图的贡献
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-09 DOI: 10.1016/j.still.2026.107106
Yajun Geng , Hongmin Zhang , Xueting Zheng , Junming Liu , Tao Zhou , Dongxu Dai , Xiaoyan Liu , Tingting Liu , Angela Lausch , Bingcheng Si , Shengxiang Xu , Feng Liu
Accurate mapping of soil organic carbon (SOC) using optical remote sensing is often constrained by persistent cloud cover, which limits data availability in many regions. While recent studies have explored the feasibility of radar sensors for SOC mapping to overcome this limitation, they have predominantly relied on backscatter features, largely overlooking the potential of interferometric coherence. To address this gap, this study assessed the potential of synergistically using backscatter/coherence observations from Sentinel-1 and optical data from Sentinel-2 for mapping SOC across the Iberian Peninsula. Backscatter, coherence, optical, and traditional auxiliary data (terrain and climate) were utilized as input features, and their various combinations were integrated with the LUCAS 2018 soil database to develop machine learning-based SOC prediction models. We evaluated how the temporal interval of backscatter composites and the temporal baseline of coherence data affected model performance. Both radar metrics showed strong predictive power for SOC, and their temporal configurations substantially affected modeling performance. Backscatter images with a monthly interval achieved the best performance, whereas longer intervals progressively decreased predictive accuracy. Models trained on coherence with shorter temporal baselines outperformed those with longer temporal baselines. The joint use of these two radar metrics improved predictive accuracy (R2 = 0.42), surpassing models that only used Sentinel-2 optical data (R2 = 0.38). Our results demonstrate promising prospects of coherence/backscatter data as substitutes or complements to optical data for SOC mapping. Integrating these three complementary and relatively independent remote sensing sources notably improved model performance, achieving accuracy no lower than models based on traditional auxiliary data. Variable importance analysis indicated that radar-derived backscatter and coherence were crucial input features for SOC mapping. The contribution of backscatter to SOC prediction was influenced by polarization modes and orbital directions, with cross-polarization and ascending-orbit backscatter showing greater importance than co-polarization and descending-orbit backscatter, respectively. The mapping results derived solely from coherence and backscatter data exhibited spatial patterns broadly consistent with those obtained from optical and traditional auxiliary data. The proposed cloud computing-based workflow utilizing freely available Sentinel optical and radar imagery provides a cost-effective and reproducible approach for large-scale SOC mapping.
利用光学遥感对土壤有机碳(SOC)进行精确制图往往受到持续云层覆盖的限制,这限制了许多地区数据的可用性。虽然最近的研究已经探索了用于SOC测绘的雷达传感器的可行性,以克服这一限制,但它们主要依赖于后向散射特征,在很大程度上忽略了干涉相干性的潜力。为了解决这一问题,本研究评估了利用Sentinel-1的后向散射/相干观测数据和Sentinel-2的光学数据协同绘制伊比利亚半岛SOC地图的潜力。利用后向散射、相干、光学和传统辅助数据(地形和气候)作为输入特征,并将它们的各种组合与LUCAS 2018土壤数据库相结合,建立基于机器学习的土壤有机碳预测模型。我们评估了后向散射复合数据的时间间隔和相干数据的时间基线对模型性能的影响。两种雷达指标都显示出很强的SOC预测能力,它们的时间配置极大地影响了建模性能。以每月为间隔的后向散射图像获得了最佳性能,而较长的间隔逐渐降低了预测精度。使用较短时间基线进行一致性训练的模型优于使用较长时间基线的模型。这两种雷达指标的联合使用提高了预测精度(R2 = 0.42),超过了仅使用Sentinel-2光学数据的模型(R2 = 0.38)。我们的研究结果表明,相干/后向散射数据作为SOC制图光学数据的替代或补充具有广阔的前景。整合这三个互补且相对独立的遥感源显著提高了模型的性能,其精度不低于基于传统辅助数据的模型。变量重要性分析表明,雷达衍生的后向散射和相干性是SOC映射的重要输入特征。后向散射对SOC预测的贡献受极化方式和轨道方向的影响,其中交叉极化和上升轨道后向散射的重要性分别大于共极化和下降轨道后向散射。仅从相干和后向散射数据获得的制图结果显示出与光学和传统辅助数据获得的空间格局大致一致。提出的基于云计算的工作流程利用免费提供的Sentinel光学和雷达图像,为大规模SOC制图提供了一种经济有效且可重复的方法。
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引用次数: 0
Multi-year comparisons of shoot and root decomposition dynamics of Italian ryegrass (Lolium multiflorum) under soybean cropping 大豆种植下意大利黑麦草(Lolium multiflorum)茎和根分解动态的多年比较
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-10 DOI: 10.1016/j.still.2026.107105
Miri Choi , Sora Lee , Chaelin Jo , Jihyeon Lee , Nayoung Choi , Jeong-Gu Lee , Chaein Na
Cover crop residue (shoot or root) decomposition regulates nutrient cycling and soil organic matter in crop rotation. This study examined the decomposition and nutrient release of Italian ryegrass (Lolium multiflorum, IRG) shoot and root residues incorporated into soil under an IRG–soybean (Glycine max L.) rotation for three years. IRG shoot and root litterbags were incorporated into the soil, and retrieved over 140 days. Dry matter, C, and N fitted asymptotic single-exponential models to residue remaining, and rise-to-maximum models to cumulative C and N release. Initial residue quality and weather covariates supported interpretation. Shoot biomass ranged from 4.43 to 6.92 t ha⁻¹ , which was approximately 2.7–5.3 times greater than root. Moreover, shoot had higher nitrogen concentrations (12.8–20.1 g kg⁻¹) and consistently exhibited lower C/N ratio and lignin/N ratios. The IRG shoot residues decomposed 2.2–2.5 times faster and released up to average 60 kg N ha⁻¹ within 40 days, matching the initial N demand of the subsequent crop. In contrast, root residues decomposed dry matter and C slowly, released negligible N, but contributed to sustained C (129 kg ha⁻¹), indicating potential for soil organic matter stabilization. These results suggest the shoot residue serves as an immediate N source for the subsequent crop and the roots contribute to long-term soil C sequestration in the field. In tilled IRG–soybean systems, incorporating both plant parts have impacts: shoot residues supply starter N and root residues add a slower, more persistent C input that supports soil organic matter accumulation.
作物轮作中覆盖残茬(茎或根)分解调节养分循环和土壤有机质。研究了3年轮作条件下意大利黑麦草(Lolium multiflorum, IRG)茎部和根部残体在土壤中的分解和养分释放情况。将IRG的茎和根垃圾袋放入土壤中,并在140天内回收。干物质、碳和氮对残馀量拟合渐近单指数模型,对累积碳和氮释放拟合上升至最大值模型。初始残留质量和天气协变量支持解释。茎部生物量从4.43到6.92 t ha⁻¹ ,大约是根的2.7-5.3 倍。此外,茎部的氮浓度较高(12.8-20.1 g kg⁻¹),C/N比和木质素/N比始终较低。IRG苗残体分解速度快2.2-2.5 倍,在40天内平均释放出60 kg N ha⁻¹ ,与后续作物的初始N需求相匹配。相比之下,根残对干物质和碳的分解较慢,释放的氮可以忽略不计,但对持续的碳有贡献(129 kg ha⁻¹),表明土壤有机质稳定的潜力。这些结果表明,地上部残茬为后续作物提供了直接的氮源,而根系有助于田间长期的土壤碳封存。在耕作的irg -大豆系统中,将植物的两个部分结合在一起会产生影响:茎部残留物提供启动氮,根系残留物增加更慢、更持久的碳输入,支持土壤有机质积累。
{"title":"Multi-year comparisons of shoot and root decomposition dynamics of Italian ryegrass (Lolium multiflorum) under soybean cropping","authors":"Miri Choi ,&nbsp;Sora Lee ,&nbsp;Chaelin Jo ,&nbsp;Jihyeon Lee ,&nbsp;Nayoung Choi ,&nbsp;Jeong-Gu Lee ,&nbsp;Chaein Na","doi":"10.1016/j.still.2026.107105","DOIUrl":"10.1016/j.still.2026.107105","url":null,"abstract":"<div><div>Cover crop residue (shoot or root) decomposition regulates nutrient cycling and soil organic matter in crop rotation. This study examined the decomposition and nutrient release of Italian ryegrass (<em>Lolium multiflorum</em>, IRG) shoot and root residues incorporated into soil under an IRG–soybean (<em>Glycine max</em> L.) rotation for three years. IRG shoot and root litterbags were incorporated into the soil, and retrieved over 140 days. Dry matter, C, and N fitted asymptotic single-exponential models to residue remaining, and rise-to-maximum models to cumulative C and N release. Initial residue quality and weather covariates supported interpretation. Shoot biomass ranged from 4.43 to 6.92 t ha⁻¹ , which was approximately 2.7–5.3 times greater than root. Moreover, shoot had higher nitrogen concentrations (12.8–20.1 g kg⁻¹) and consistently exhibited lower C/N ratio and lignin/N ratios. The IRG shoot residues decomposed 2.2–2.5 times faster and released up to average 60 kg N ha⁻¹ within 40 days, matching the initial N demand of the subsequent crop. In contrast, root residues decomposed dry matter and C slowly, released negligible N, but contributed to sustained C (129 kg ha⁻¹), indicating potential for soil organic matter stabilization. These results suggest the shoot residue serves as an immediate N source for the subsequent crop and the roots contribute to long-term soil C sequestration in the field. In tilled IRG–soybean systems, incorporating both plant parts have impacts: shoot residues supply starter N and root residues add a slower, more persistent C input that supports soil organic matter accumulation.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"260 ","pages":"Article 107105"},"PeriodicalIF":6.8,"publicationDate":"2026-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146152897","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
Governing role of pore structure in solute transport processes in plain river network areas: Insights from CT imaging 孔隙结构在平原河网地区溶质运移过程中的控制作用:来自CT成像的见解
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-12 DOI: 10.1016/j.still.2026.107101
Sun Xiaoqin , She Dongli , Pan Yongchun , Wang Hongde , Cao Taohong , Ge Jiamin , Ju Xinni
The plain river network (PRN) areas are key high-yield agricultural zones in China, but the excessive use of fertilizers and pesticides has caused severe non-point source (NPS) pollution. Soil pore structure plays a crucial role in regulating NPS generation and transport by controlling water flow and solute transport. However, conventional static fractal parameters are insufficient to capture the actual pathways of solute transport. To overcome this limitation, we introduced the spectral fractal dimension (d), a dynamic measure of pore structure derived from random walk theory. In this study, we investigated paddy fields, orchards and vegetable fields in the Jiangsu PRN region, analyzing both pore morphology, the static fractal dimension (mass fractal dimension (D) and surface fractal dimension (D)) and the dynamic pore characteristic (d) across soil depths. Solute transport parameters were determined using breakthrough curves and the continuous time random walk (CTRW) approach to assess the governing role of pore structure. Our results revealed that surface soils exhibited higher pore abundance and more complex pore structures, resulting in increased solute transport velocity (v) and dispersion coefficient (E) compared to deeper layers. Pore morphology (e.g. Volume, Surface, Mean Breadth) and heterogeneity (D and D) controlled v and E by providing fast flow paths and extensive surface interactions, whereas connectivity (d) governed anomalous transport (β) and timing (t1, t2) via tortuous, retention-enhancing pathways. Pore shape further affected solute transport indirectly through connectivity. Among land use types, paddy soils showed a less complex and poorly connected pore structure compared to orchard soils and vegetable soils. To improve the pore structure of paddy soils and mitigate the risk of agricultural non-point source (NPS) pollution in PRN areas, the adoption of water-saving irrigation combined with straw return is recommended.
平原河网(PRN)地区是中国重要的农业高产区,但化肥和农药的过度使用造成了严重的面源污染。土壤孔隙结构通过控制水流和溶质运移,对NPS的产生和运移起着至关重要的调节作用。然而,传统的静态分形参数不足以捕捉溶质输运的实际途径。为了克服这一限制,我们引入了光谱分形维数(d),这是一种来自随机游走理论的孔隙结构的动态测量。本研究以江苏PRN地区的水田、果园和菜田为研究对象,分析了土壤孔隙形态、静态分形维数(质量分形维数(D)和表面分形维数(Dₛ))和动态孔隙特征(D)。采用突破曲线和连续时间随机漫步(CTRW)方法确定溶质输运参数,以评估孔隙结构的控制作用。结果表明,表层土壤孔隙丰度更高,孔隙结构更复杂,导致溶质运移速度(v)和分散系数(E)比深层土壤高。孔隙形态(如体积、表面积、平均宽度)和异质性(D ω和D ωₛ)通过提供快速流动路径和广泛的表面相互作用来控制v和E,而连通性(D)通过扭曲的、增强保留的途径控制异常运输(β)和时间(t1, t2)。孔隙形态通过连通性进一步间接影响溶质输运。在不同的土地利用类型中,水稻土的孔隙结构较果园土和蔬菜土的孔隙结构不复杂,且连通性较差。为改善水稻土孔隙结构,降低PRN地区农业面源污染风险,建议采用节水灌溉与秸秆还田相结合的方式。
{"title":"Governing role of pore structure in solute transport processes in plain river network areas: Insights from CT imaging","authors":"Sun Xiaoqin ,&nbsp;She Dongli ,&nbsp;Pan Yongchun ,&nbsp;Wang Hongde ,&nbsp;Cao Taohong ,&nbsp;Ge Jiamin ,&nbsp;Ju Xinni","doi":"10.1016/j.still.2026.107101","DOIUrl":"10.1016/j.still.2026.107101","url":null,"abstract":"<div><div>The plain river network (PRN) areas are key high-yield agricultural zones in China, but the excessive use of fertilizers and pesticides has caused severe non-point source (NPS) pollution. Soil pore structure plays a crucial role in regulating NPS generation and transport by controlling water flow and solute transport. However, conventional static fractal parameters are insufficient to capture the actual pathways of solute transport. To overcome this limitation, we introduced the spectral fractal dimension (<span><math><mi>d</mi></math></span>), a dynamic measure of pore structure derived from random walk theory. In this study, we investigated paddy fields, orchards and vegetable fields in the Jiangsu PRN region, analyzing both pore morphology, the static fractal dimension (mass fractal dimension (<span><math><mrow><mi>D</mi><mi>ₘ</mi></mrow></math></span>) and surface fractal dimension (<span><math><mrow><mi>D</mi><mi>ₛ</mi></mrow></math></span>)) and the dynamic pore characteristic (<span><math><mi>d</mi></math></span>) across soil depths. Solute transport parameters were determined using breakthrough curves and the continuous time random walk (CTRW) approach to assess the governing role of pore structure. Our results revealed that surface soils exhibited higher pore abundance and more complex pore structures, resulting in increased solute transport velocity (<span><math><mi>v</mi></math></span>) and dispersion coefficient (<span><math><mi>E</mi></math></span>) compared to deeper layers. Pore morphology (e.g. Volume, Surface, Mean Breadth) and heterogeneity (<span><math><mrow><mi>D</mi><mi>ₘ</mi></mrow></math></span> and <span><math><mrow><mi>D</mi><mi>ₛ</mi></mrow></math></span>) controlled <span><math><mi>v</mi></math></span> and <span><math><mi>E</mi></math></span> by providing fast flow paths and extensive surface interactions, whereas connectivity (<span><math><mi>d</mi></math></span>) governed anomalous transport (<span><math><mi>β</mi></math></span>) and timing (<span><math><msub><mrow><mi>t</mi></mrow><mrow><mn>1</mn></mrow></msub></math></span>, <span><math><msub><mrow><mi>t</mi></mrow><mrow><mn>2</mn></mrow></msub></math></span>) via tortuous, retention-enhancing pathways. Pore shape further affected solute transport indirectly through connectivity. Among land use types, paddy soils showed a less complex and poorly connected pore structure compared to orchard soils and vegetable soils. To improve the pore structure of paddy soils and mitigate the risk of agricultural non-point source (NPS) pollution in PRN areas, the adoption of water-saving irrigation combined with straw return is recommended.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"260 ","pages":"Article 107101"},"PeriodicalIF":6.8,"publicationDate":"2026-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146161052","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
Effects of Alhagi sparsifolia root content and soil moisture content on soil deformation and strength under different freeze-thaw temperature conditions 不同冻融温度条件下疏叶alhagi根系含量和土壤含水量对土壤变形和强度的影响
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-09 DOI: 10.1016/j.still.2026.107110
Meixue Zhang , Qinglin Li , Xuanbing Luo , Wenjuan Chen , Rui Wang , Shuailong Yu , Guang Yang
This study focuses on cold arid regions in Xinjiang, China, and investigates the reinforcement effect of Alhagi sparsifolia roots on sandy soil under freeze-thaw conditions. Freeze-thaw cycle and direct shear tests, combined with environmental scanning electron microscopy (ESEM), were conducted to analyze the effects of root reinforcement on the deformation and strength characteristics of sandy soil under varying soil water contents (8–14 %) and freezing temperatures (−5 to −20 ℃). The results revealed that soil deformation during freeze-thaw cycle underwent five distinct stages and was strongly controlled by soil water content and temperature. Root incorporation reduced the maximum soil deformation by more than 30 %, and the suppressive effect exceeded 51 % at high soil water content (14 %). In low-water-content soils (8 %), excessive root content (>0.35 %) induced deformation rebound, which was attributed to root clustering and the development of interfacial voids. At the optimal root content (0.28–0.35 %), the maximum shear stress of the root-soil composite increased by 5–45 %, with the specific magnitude depending on soil water content and freezing temperature. Moreover, the optimal root content (η) decreased with increasing soil water content. The results demonstrate the effectiveness of A. sparsifolia in enhancing soil stability under freeze-thaw conditions and highlight the nonlinear and moisture-sensitive characteristics of root reinforcement. This study provides a theoretical basis for optimizing vegetation-based slope stabilization strategies in cold arid environments.
以新疆寒冷干旱区为研究对象,研究冻融条件下阿拉木图根系对沙质土壤的加固作用。通过冻融循环和直剪试验,结合环境扫描电镜(ESEM),分析了不同土壤含水量(8 ~ 14% %)和冻结温度(−5 ~−20℃)下根系加固对沙土变形和强度特性的影响。结果表明,冻融循环过程中土壤变形经历了5个不同的阶段,且受土壤含水量和温度的强烈控制。在土壤含水量较高时(14 %),根系掺入对土壤最大变形的抑制作用超过51 %。在低含水量(8 %)土壤中,过多的根含量(>0.35 %)引起变形回弹,这主要归因于根系聚集和界面空隙的形成。在最佳根含量(0.28 ~ 0.35 %)下,根土复合材料的最大剪应力增加了5 ~ 45 %,具体幅度取决于土壤含水量和冻结温度。最佳根含量(η)随土壤含水量的增加而减小。结果表明,疏叶松对冻融条件下土壤稳定性具有增强作用,根系加固具有非线性和水分敏感性。该研究为在寒冷干旱环境下优化基于植被的边坡稳定策略提供了理论依据。
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引用次数: 0
Nitrogen fertilization drives bacterial turnover versus fungal persistence for straw-derived C and N stabilization in a wheat-maize rotation 在小麦-玉米轮作中,氮肥驱动细菌周转与真菌持久性,以稳定秸秆来源的碳和氮
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-09 DOI: 10.1016/j.still.2026.107111
Guocui Ren , Xiuli Xin , Haowei Ni , Xianfeng Zhang , Lan Mu , Wenliang Yang , Shuchun Ge , Shaopu Pang , Anning Zhu
Nitrogen (N) fertilization is a critical management practice for enhancing soil organic matter (SOM) sequestration, yet its efficacy often varies unpredictably within intensive annual rotation systems. To unravel the phase-specific mechanisms regulating stabilization outcomes of straw-derived C and N, we conducted two in situ dual-labeled (13C and 15N) wheat and maize straw tracing studies nested within a 5-year field experiment under contrasting N rates (0, 150, and 250 kg N ha−1). We found that SOM stabilization outcomes were strictly regulated by the distinct biochemical environments inherent to each rotation phase. In the wheat straw phase, high N input (N250) primed an oxidative enzyme-bacterial pathway. Although this pathway generated substantial bacterial necromass (contributing up to 56.9 % of 13C-SOC), it was characterized by rapid turnover. Path analysis revealed that this intense bacterial cycling negatively impacted stable C retention (r = -0.83, P < 0.001), ultimately leading to a 17.6 % reduction in straw-derived mineral-associated organic carbon (13C-MAOC) content compared to N0. In contrast, the maize straw phase exhibited a distinct C and N decoupling, with 13C preferentially retained in particulate organic matter (POM) and 15N in MAOM. High N input activated a hydrolytic enzyme-fungal pathway, boosting fungal PLFAs by 70.8 % and necromass contribution to 31.7 %. Crucially, unlike the bacterial pathway in wheat, this fungal-mediated process acted as a strong positive driver of MAOM formation (r = 0.84, P < 0.001), facilitating the persistence of straw-derived C and N via physical and chemical protection. These findings demonstrate that N fertilization primes a leaky “bacterial turnover” pump in the wheat straw phase but a conservative “fungal persistence” pathway in the maize straw phase. Consequently, we propose a phase-specific N management strategy that combines moderate N inputs for wheat straw to minimize turnover losses with higher N inputs for maize to leverage fungal stabilization, thereby optimizing system-level C storage.
氮(N)施肥是提高土壤有机质(SOM)固存的关键管理措施,但在集约轮作系统中,其效果往往发生不可预测的变化。为了揭示调节秸秆碳氮稳定结果的阶段性机制,我们在5年的田间试验中进行了两项原位双标记(13C和15N)小麦和玉米秸秆追踪研究,分别在不同的施氮量(0、150和250 kg N ha−1)下进行。我们发现SOM稳定结果受到每个旋转阶段固有的不同生化环境的严格调节。在麦秸期,高N输入(N250)启动了一个氧化酶-细菌途径。尽管这一途径产生了大量的细菌坏死块(占13C-SOC的56.9% %),但其特点是快速转换。通径分析显示,这种强烈的细菌循环对稳定的碳保留产生了负面影响(r = -0.83,P <; 0.001),最终导致秸秆衍生矿物相关有机碳(13C-MAOC)含量与N0相比降低了17.6 %。相反,玉米秸秆阶段表现出明显的碳氮解耦,13C优先保留在颗粒有机质(POM)中,15N优先保留在MAOM中。高氮输入激活了水解酶-真菌途径,使真菌PLFAs提高了70.8% %,坏死团贡献提高了31.7% %。关键的是,与小麦中的细菌途径不同,真菌介导的这一过程是MAOM形成的一个强大的正驱动因素(r = 0.84,P <; 0.001),通过物理和化学保护促进秸秆来源的C和N的持续存在。这些发现表明,氮肥在小麦秸秆期启动了一个渗漏的“细菌周转”泵,而在玉米秸秆期启动了一个保守的“真菌持续”途径。因此,我们提出了一种阶段性氮素管理策略,将小麦秸秆的适度氮素投入与玉米的高氮素投入相结合,以最大限度地减少周转损失,从而利用真菌稳定,从而优化系统级碳储存。
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引用次数: 0
Network analysis and machine learning-aided soil quality index prediction: Insights from a wind-eroded region in northeastern China 网络分析和机器学习辅助土壤质量指数预测:来自中国东北风蚀区的启示
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-14 DOI: 10.1016/j.still.2026.107109
Xue Zhang , Shuren Wang , Meng Li , Wei Hu
Soil quality degradation threatens food and ecological security on 33 % of global terrestrial land, and there is an urgent need for effective evaluation systems. The objective was to clarify the multifactorial interactions driving soil-quality degradation and develop an accurate evaluation framework. In a typical wind-eroded region in northeastern China, 316 surface soil samples (0–20 cm) were collected using the grid sampling method, with 20 physicochemical and biological indicators tested. Core indicators for the minimum data set were identified via network analysis, and four machine learning algorithms—support vector machine, random forest, light gradient boosting machine (LightGBM), and extreme gradient boosting—were combined with 14 high-resolution environmental factors to predict the soil quality index (SQI). Results showed that soil water content, soil organic carbon, and field water holding capacity were core indicators for constructing SQI. LightGBM had the highest prediction accuracy (mean absolute error = 0.10, root mean square error = 0.12, coefficient of determination = 0.72, concordance correlation coefficient = 0.81) and was optimal for removing redundant environmental factors. Latitude (19.5 %–40.6 %), mean annual temperature (12.8 %–19.1 %), and near-surface wind speed (10.1 %–12.5 %) were dominant drivers of SQI spatial variability. Soil quality exhibited a decreasing trend from northeast to southwest, with low SQI values (<0.4, 27.2 %) prevalent in low-latitude, high-temperature, and strong-wind-speed areas. The integration of network analysis, high-resolution environmental factors, and machine learning provides an effective framework for evaluating soil quality. Notably, soil quality in low-latitude, high-temperature, and strong-wind-speed regions should be emphasized in the context of future global warming.
土壤质量退化威胁着全球33% %陆地土地的粮食和生态安全,迫切需要有效的评价系统。目的是澄清驱动土壤质量退化的多因素相互作用,并制定准确的评价框架。在东北典型风蚀区,采用栅格采样法采集了316份表层土壤样品(0 ~ 20 cm),并对20项理化和生物指标进行了测试。通过网络分析确定最小数据集的核心指标,并将支持向量机、随机森林、光梯度增强机(LightGBM)和极端梯度增强4种机器学习算法与14个高分辨率环境因子相结合,预测土壤质量指数(SQI)。结果表明,土壤含水量、土壤有机碳和田间持水量是构建SQI的核心指标。LightGBM预测精度最高(平均绝对误差= 0.10,均方根误差= 0.12,决定系数= 0.72,一致性相关系数= 0.81),对去除冗余环境因素效果最佳。纬度(19.5 % ~ 40.6 %)、年平均气温(12.8 % ~ 19.1 %)和近地面风速(10.1 % ~ 12.5 %)是SQI空间变异的主要驱动因子。土壤质量呈现由东北向西南递减的趋势,低纬度、高温、强风速地区SQI值较低(<0.4, 27.2 %);网络分析、高分辨率环境因素和机器学习的集成为评估土壤质量提供了一个有效的框架。值得注意的是,在未来全球变暖的背景下,低纬度、高温和强风速地区的土壤质量应该得到重视。
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引用次数: 0
Enhancing aboveground biomass estimation for winter wheat using UAV-based color space transformation and spectral feature reconstruction 基于无人机的色彩空间变换和光谱特征重构增强冬小麦地上生物量估算
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-10 DOI: 10.1016/j.still.2026.107120
Yang Xu, Xiaobo Gu, Penglin Li, Bowen Sun, Zhikai Cheng, Tongtong Zhao, Zhengtao Zhang, Chunyu Wei, Yadan Du
Timely and precise quantification of aboveground biomass (AGB) is essential for evaluating crop development, optimizing agronomic practices, and ensuring food security. However, traditional AGB estimation approaches are destructive, time-consuming, and impractical for extensive-scale applications. Remote sensing methods, although non-destructive, often encounter obstacles including spectral saturation and interference from soil or plastic mulch, especially under dense canopy cover or within ridge-furrow mulching systems. To overcome these limitations, this study focused on winter wheat cultivated under a ridge-furrow film mulching system, utilizing high-resolution UAV imagery combined with machine learning techniques to reconstruct spectral information by integrating vegetation indices, textural metrics, and color space-converted variables. Feature selection was performed using Recursive Feature Elimination (RFE), and three modeling strategies—vegetation indices and texture features (VT), VT with color space transformation (VTSC), and VTSC with spectral reconstruction (REVTSC)—were developed and evaluated using Ridge Regression (RR), Support Vector Machine (SVM), and Random Forest (RF) algorithms across the turning green, jointing, heading, and filling growth stages. The results showed that integrating color space-transformed features significantly enhanced AGB prediction accuracy, especially during early growth stages (turning green and jointing stages). Spectral feature reconstruction further improved model performance by mitigating background interference from soil and plastic mulch. The highest estimation accuracy was achieved during the filling stage, with R2 of 0.81 and 0.76, and RMSE of 1581.16 kg ha–1 and 1737.47 kg ha–1 for the training and test sets, respectively. An improvement in R2 of up to 33.10 % was observed when using the REVTSC model over the VT model, underscoring the benefit of spectral reconstruction. RR performed better in early growth stages (turning green and jointing stages), while SVM showed the weakest performance throughout the whole growth stages of winter wheat. The results of present study would provide a novel approach to AGB estimation under mixed background conditions by integrating color space transformation and spectral reconstruction, offering a scalable, accurate solution for AGB monitoring in plastic-mulched cropping systems.
及时、准确地量化地上生物量(AGB)对于评估作物发展、优化农艺做法和确保粮食安全至关重要。然而,传统的AGB估计方法是破坏性的,耗时的,并且不适合大规模的应用。遥感方法虽然是非破坏性的,但经常遇到障碍,包括光谱饱和和土壤或塑料覆盖的干扰,特别是在茂密的树冠覆盖下或垄沟覆盖系统内。为了克服这些局限性,本研究以垄沟膜覆盖系统下栽培的冬小麦为研究对象,利用高分辨率无人机图像结合机器学习技术,通过整合植被指数、纹理指标和色彩空间转换变量,重构光谱信息。利用递归特征消除(RFE)进行特征选择,并利用岭回归(RR)、支持向量机(SVM)和随机森林(RF)算法开发了植被指数和纹理特征(VT)、VT结合色彩空间变换(VTSC)和VTSC结合光谱重建(REVTSC)三种建模策略,并对其在绿化、拔节、抽头和填充生长阶段进行了评估。结果表明,整合颜色空间变换特征显著提高了AGB预测精度,特别是在生长早期(变绿期和拔节期)。光谱特征重建通过减轻土壤和地膜的背景干扰进一步提高了模型的性能。在填充阶段估计精度最高,R2分别为0.81和0.76,训练集和测试集的RMSE分别为1581.16 kg ha-1和1737.47 kg ha-1。与VT模型相比,REVTSC模型的R2提高高达33.10 %,这表明了光谱重建的优势。在冬小麦生育早期(转绿期和拔节期),RR表现较好,而SVM在整个生育期表现最弱。本文的研究结果将为混合背景下的AGB估计提供一种新的方法,该方法将结合色彩空间变换和光谱重建,为地膜作物系统AGB监测提供一种可扩展、精确的解决方案。
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引用次数: 0
Trade-offs between root exudation and root traits induced by coexisting species under a grazing gradient can mobilize available nitrogen to promote grassland productivity 在放牧梯度下,共存物种诱导的根系分泌与根系性状之间的权衡可以调动有效氮,促进草地生产力的提高
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-07 DOI: 10.1016/j.still.2026.107108
Guisen Yang, Jirui Gong, Shangpeng Zhang, Ruijing Wang, Tong Wang, Yaohong Yu, Qin Xie
Root exudates mobilize soil nutrients and create an important pathway for plants to obtain resources. Understanding nutrient-acquisition strategies based on root exudation by coexisting grassland species is crucial for vegetation regrowth and productivity after grazing. We analyzed the nutrient-acquisition strategies and productivity maintenance mechanisms of Leymus chinensis, Stipa grandis and Cleistogenes squarrosa over two consecutive years in a long-term grazing experimental plot in a typical grassland in Inner Mongolia. Grazing significantly promoted the root exudation rates of carbon (C), nitrogen (N), and organic acids. Grazing increased the maximum quantum efficiency of photosystem II, root salicylic acid, and total soluble sugars (TSS), which increased root exudation by improving competitive traits such as root nitrogen (RN) and specific root area (SRA), while reducing tissue-construction traits such as root tissue density (RTD). This shift led L. chinensis to adopt a competitive strategy. Stipa grandis exhibited a higher net photosynthetic rate and non-photochemical quenching, which promoted C and organic acid exudation, thereby increasing specific root length (SRL). Nitrogen exudation further increased RTD, resulting in a conservative strategy. Cleistogenes squarrosa demonstrated a higher carboxylation efficiency, electron transport rate, and TSS, which promoted N and organic acid exudation, and increased SRA and RTD, whereas C exudation increased RN, forming a facultative nutrient-acquisition strategy. These processes mobilized rhizosphere soil nutrients, especially ammonium nitrogen (NH4+-N), and thereby improved aboveground productivity. Our results highlight the importance of plant metabolite in regulating changes in root exudation rates. Furthermore, the trade-offs between plant root exudation and root morphology determined the strategy of belowground resource acquisition, and the mobilization of soil nitrogen and other nutrients. Our results have important theoretical and practical implications for understanding the coexistence of grassland species under grazing pressure and for developing restoration strategies for degraded grasslands.
根系分泌物调动土壤养分,是植物获取资源的重要途径。了解基于根系分泌物的共生草地物种的养分获取策略对放牧后植被的再生和生产力至关重要。在内蒙古某典型草地长期放牧试验地,连续2年对羊草、大针茅和粗锁蒜草的养分获取策略和生产力维持机制进行了研究。放牧显著提高了根系碳(C)、氮(N)和有机酸的分泌速率。放牧提高了光系统II、根水杨酸和总可溶性糖(TSS)的最大量子效率,通过提高根氮(RN)和比根面积(SRA)等竞争性状增加了根系分泌量,同时降低了根组织密度(RTD)等组织构建性状。这种转变导致羊草采取竞争策略。大针茅表现出较高的净光合速率和非光化学猝灭,促进了C和有机酸的分泌,从而增加了比根长。氮渗出进一步增加RTD,导致保守策略。锁丝草羧基化效率、电子传递速率和TSS较高,促进了氮和有机酸的分泌,增加了SRA和RTD,而C的分泌增加了RN,形成兼性营养获取策略。这些过程调动了根际土壤养分,特别是铵态氮(NH4+-N),从而提高了地上生产力。我们的研究结果强调了植物代谢物在调节根渗出速率变化中的重要性。此外,植物根系分泌物和根系形态之间的权衡决定了地下资源获取策略,以及土壤氮和其他养分的动员。研究结果对了解放牧压力下草原物种的共存,制定退化草原的恢复策略具有重要的理论和实践意义。
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