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Long-term partial substitution of chemical fertilizers regulates soil quality and productivity of semi-arid Inceptisols under a pearl millet–wheat system 长期部分替代化肥对半干旱珠粒-小麦体系下黄壤土壤质量和生产力的调节作用
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2026-01-20 DOI: 10.1016/j.geodrs.2026.e01052
Manu Rani , V. Goyal , Pradip Dey , Mamta Phogat , Manoj Kumar , S.R. Singh , I.C. Haokip
<div><div>The long-term effect of partially substituting chemical fertilizers by organic inputs on soil quality and yield of pearl-millet and wheat under semi-arid region of Indo-Gangetic plains of India is unclear. This decadal field experiment (2009–2019) evaluated the impact of partial substitution of chemical fertilizers through organic inputs on soil carbon, microbial dynamics, soil quality and yield of pearl millet-wheat system. The experiment was laid out under randomized block design (RBD) with seven treatments and three replications in ten consecutive cropping cycles from 2009 to 2019. The seven treatments were: Ck- no chemical fertilizer, FYM-farm yard manure @15 Mg ha<sup>−1</sup>, RDF- recommended dose of N and P, STCR-I- chemical fertilizer for achieving 3.0 and 5.5 Mg ha<sup>−1</sup> targeted yield of pearl millet and wheat, respectively, STCR-II- chemical fertilizer for achieving 3.5 and 6.0 Mg ha<sup>−1</sup> targeted yield of pearl millet and wheat, respectively, IPNS-I- FYM + chemical fertilizer for achieving 3.0 and 5.5 Mg ha<sup>−1</sup> targeted yield of pearl millet and wheat, respectively and IPNS-II-FYM + chemical fertilizer for achieving 3.5 and 6.0 Mg ha<sup>−1</sup> targeted yield of pearl millet and wheat, respectively. Treatment IPNS-I and IPNS-II improved nutrient supply system, and yields of pearl millet and wheat by lowering soil pH (7.78 and 7.79), soil bulk density (1.38 Mg m<sup>3</sup>) and enhancing soil organic carbon (0.83 and 0.85%), C-stock (17.1 and 17.6 Mg C ha<sup>−1</sup>) and its buildup rate (1.71 to 1.76 Mg C ha<sup>−1</sup> yr<sup>−1</sup>). Treatments FYM, IPNS-I and IPNS-II significantly (<em>P</em> < 0.05) enhanced microbial biomass carbon, potential activities of soil enzymes, soil nutrients and soil quality over the STCR-II, STCR-I, RDF and Ck, however, microbial (M<sub>q</sub>) and metabolic quotient exhibited reverse trends. The highest SQI (0.795) was recorded with IPNS-I followed by IPNS-II (0.791), T<sub>2</sub> (0.771) and the lowest in Ck (0.341). Available P, acid phosphatase, available N and Mq were the key soil quality indicators in MDS for the pearl millet-wheat production in semi-arid zone, contributing 20.4, 21.0, 19.6 and 7.96% toward soil quality development, respectively. Treatment IPNS-I and IPNS-II not only achieved the targeted yield of pearl millet and wheat within ±10% yield deviation, but also increased pearl millet yields by 7.83 and 25.6%, and wheat yield by 10.4 and 23.9% over RDF, respectively due to improving SQI. As a result, SQI had significant correlation with grain and stover/straw yield of pearl millet and wheat indicated prominent influence of partial substitution of organic manure to inorganic fertilizers. Thus, our results evinced that long-term partial substitution of inorganic fertilizer based on targeted yield approach of soil test crop response (STCR) provides better environment for pearl millet-wheat productivity in semi-arid Inceptisol of India.</div
在印度恒河平原半干旱区,有机投入部分替代化肥对土壤质量和珍珠粟、小麦产量的长期影响尚不清楚。本年代际田间试验(2009-2019)评估了有机投入部分替代化肥对珍珠粟-小麦系统土壤碳、微生物动态、土壤质量和产量的影响。试验于2009 - 2019年采用随机区组设计(RBD), 7个处理,3个重复,连续10个种植周期。这七种治疗方法是:Ck-无化肥,FYM-农场厩肥@15 Mg ha - 1, RDF- N和P推荐用量,STCR-I-珍珠谷子和小麦目标产量分别达到3.0和5.5 Mg ha - 1的化肥,STCR-II-珍珠谷子和小麦目标产量分别达到3.5和6.0 Mg ha - 1的化肥,IPNS-I- FYM +珍珠谷子和小麦目标产量分别达到3.0和5.5 Mg ha - 1的化肥,IPNS-II-FYM +化肥分别可实现珍珠粟和小麦3.5和6.0 Mg ha−1的目标产量。IPNS-I和IPNS-II处理通过降低土壤pH值(7.78和7.79)、土壤容重(1.38 Mg m3)、提高土壤有机碳(0.83和0.85%)、碳储量(17.1和17.6 Mg C ha−1)及其积累速率(1.71 ~ 1.76 Mg C ha−1年−1),改善了珍珠粟和小麦的养分供应系统和产量。与STCR-II、STCR-I、RDF和Ck处理相比,FYM、IPNS-I和IPNS-II处理显著(P < 0.05)提高了土壤微生物生物量碳、土壤酶活性、土壤养分和土壤质量,但微生物(Mq)和代谢商呈相反趋势。IPNS-I组SQI最高(0.795),其次为IPNS-II组(0.791),T2组(0.771),Ck组最低(0.341)。有效磷、酸性磷酸酶、有效氮和Mq是半干旱区珍珠小麦生产MDS中土壤质量的关键指标,对土壤质量发展的贡献率分别为20.4%、21.0、19.6%和7.96%。IPNS-I和IPNS-II处理不仅实现了珍珠粟和小麦在±10%产量偏差内的目标产量,而且由于SQI的改善,珍珠粟产量和小麦产量分别比RDF提高了7.83%和25.6%,小麦产量分别提高了10.4%和23.9%。结果表明,SQI与珍珠粟和小麦的籽粒及秸秆产量呈极显著相关,表明有机肥部分替代无机肥对SQI的影响显著。因此,本研究结果表明,在印度半干旱地区,基于土壤试验作物响应目标产量法(STCR)的长期部分替代无机肥料为珍珠粟-小麦生产提供了更好的环境。
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引用次数: 0
Spatial variability and environmental drivers of the soil erodibility factor (K) at a regional scale in the Italian Alps 意大利阿尔卑斯地区土壤可蚀性因子(K)的空间变异及其环境驱动因素
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2026-02-11 DOI: 10.1016/j.geodrs.2026.e01061
Valeria Cesarini , Sara Agaba , Michele Eugenio D'Amico , Emanuele Pintaldi , Michele Freppaz , Silvia Stanchi
Understanding and predicting soil erodibility in mountain environments is challenging due to complex interactions among environmental, pedological, and biological processes, which contribute to high spatial variability. This is particularly evident in the Aosta Valley Region (NW Italian Alps), where previous studies reported pronounced soil heterogeneity. Building on these findings, we estimated the topsoil erodibility factor (K factor of the USLE), assuming that, given the uniform texture, soil organic matter (SOM) would be the main driver of K variation. K was calculated using two equations—USLE and EPIC. We also tested, in a demonstrative way, SOM values beyond the conventional threshold of the USLE nomograph to explore its influence on K in highly organic alpine soils. A digital soil mapping (DSM) approach with machine learning was used to model the spatial distribution of K. Pedological field data were analyzed to evaluate their relationship with K, and USLE-based erosion values were calculated for observed profiles to assess K estimate reliability. Results show that: (i) the USLE K equation better captures mountain complexity; (ii) SOM significantly reduces K, with stone cover exerting additional influence; (iii) the model identified key regional drivers of K (carbon stock, elevation, pH), producing consistent spatial maps at 40 m resolution; and (iv) K values vary across soil horizons, humus systems, land uses, and soil types. Complementary analysis of erosional denudation supports the central role of SOM in enhancing alpine soil resistance. These findings provide insights for future soil monitoring, conservation, and restoration strategies in mountain ecosystems.
由于环境、土壤学和生物过程之间复杂的相互作用导致了高空间变异性,理解和预测山区土壤可蚀性具有挑战性。这在奥斯塔山谷地区(意大利阿尔卑斯山脉西北部)尤其明显,此前的研究报告了那里明显的土壤异质性。基于这些发现,我们估计了表层土壤可蚀性因子(USLE的K因子),假设在质地均匀的情况下,土壤有机质(SOM)将是K变化的主要驱动因素。K使用usle和EPIC两个方程计算。我们还以示范性的方式测试了SOM值超出USLE nomograph的常规阈值,以探索其对高有机高山土壤中K的影响。采用基于机器学习的数字土壤制图(DSM)方法对K的空间分布进行建模,分析土壤田数据以评估其与K的关系,并计算基于usle的观测剖面的侵蚀值以评估K估计的可靠性。结果表明:(1)USLE K方程较好地反映了山地复杂性;(ii) SOM显著降低K值,其中石覆盖对K值有额外影响;(iii)该模型识别了K(碳储量、海拔、pH)的关键区域驱动因素,生成了40 m分辨率的一致性空间图;K值因土层、腐殖质系统、土地利用和土壤类型而异。对侵蚀剥蚀的补充分析支持SOM在增强高山土壤抵抗力方面的核心作用。这些发现为未来山区生态系统的土壤监测、保护和恢复策略提供了见解。
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引用次数: 0
Rapid prediction of soil hydraulic and physicochemical properties using the Nix Pro color sensor 使用Nix Pro颜色传感器快速预测土壤的水力和物理化学性质
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2026-02-26 DOI: 10.1016/j.geodrs.2026.e01064
Fatemeh Cheshmberah , Ali.A. Zolfaghari , Ruhollah Taghizadeh-Mehrjardi , Ronny Berndtsson
Color is the most obvious and easily determined soil property that can provide crucial information about soil composition. The NIX™ Pro color sensor (Nix) presents a user-friendly alternative to the traditional Munsell manual method, with reduced sensitivity to environmental and human factors. Therefore, a new method was developed to use Nix in combination with machine learning to quickly and affordably estimate improved physical, hydraulic, and chemical soil properties. This study extends the application of the Nix sensor from chemical properties to include soil hydraulic properties, providing a rapid, reproducible, and practical prediction tool. The Nix and the Random Forest (RF) algorithm were employed to analyze the spectra of 150 soil samples collected from 0 to 30 cm depth in semi-arid regions of Iran. The results indicated that using the RF algorithm with CIE L*a*b* Color System data from the Nix, the best predictive performance was observed for CaCO₃ (R2 = 0.62, RMSE = 2.25) and field capacity (FC) (R2 = 0.50, RMSE = 4.99). Predictions for clay (R2 = 0.59, RMSE = 7.26), permanent wilting point (PWP) (R2 = 0.62, RMSE = 2.04), and sand (R2 = 0.49, RMSE = 10.08) also showed good agreement with measured values. Bulk density (BD) (R2 = 0.45, RMSE = 0.11) and soil available water (SAW) (R2 = 0.51, RMSE = 4.97) predictions exhibited higher errors relative to the observed ranges. The findings indicate that the Nix sensor's portability and cost-effectiveness, along with the RF algorithm, make it a practical tool for field applications. It provides quick, reliable, and improved estimates of CaCO₃ and FC, with good performance also observed for clay, PWP, and sand. The results reflect the method's efficacy, its possible adaptation to other areas with proper adjustment, and its integration into precision agriculture and environmental applications.
颜色是最明显和最容易确定的土壤属性,可以提供有关土壤组成的关键信息。NIX™Pro颜色传感器(NIX)提供了传统Munsell手动方法的用户友好替代方案,降低了对环境和人为因素的敏感性。因此,开发了一种新方法,将Nix与机器学习相结合,快速、经济地评估改善的物理、水力和化学土壤特性。本研究将Nix传感器的应用从化学性质扩展到土壤水力性质,提供了一种快速、可重复、实用的预测工具。采用Nix和随机森林(Random Forest, RF)算法对伊朗半干旱区0 ~ 30 cm深度的150份土壤样品进行光谱分析。结果表明,使用来自Nix的CIE L*a*b* Color System数据的RF算法,对CaCO₃(R2 = 0.62, RMSE = 2.25)和场地容量(FC) (R2 = 0.50, RMSE = 4.99)的预测性能最好。粘土(R2 = 0.59, RMSE = 7.26)、永久凋零点(PWP) (R2 = 0.62, RMSE = 2.04)和沙子(R2 = 0.49, RMSE = 10.08)的预测值也与实测值吻合良好。容重(BD) (R2 = 0.45, RMSE = 0.11)和土壤有效水分(SAW) (R2 = 0.51, RMSE = 4.97)的预测误差相对于观测范围较大。研究结果表明,Nix传感器的便携性和成本效益,以及RF算法,使其成为现场应用的实用工具。它提供了快速、可靠和改进的CaCO₃和FC的估计,对粘土、PWP和沙子也有良好的性能。结果反映了该方法的有效性,以及在适当调整后对其他领域的适应性,并与精准农业和环境应用相结合。
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引用次数: 0
Do South African restoration projects overpromise on carbon sequestration potential? 南非的恢复项目对碳封存潜力的承诺过高了吗?
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2026-02-13 DOI: 10.1016/j.geodrs.2026.e01060
Jessica Prevôst , Heidi-J Hawkins , Michael Denis Cramer
Modelled effects of human land use indicate that South Africa has the highest predicted loss of soil organic carbon (SOC) globally. This requires an urgent need to better understand actual losses across different land uses, drivers of loss, and the potential that restoration holds for SOC storage. We extend previous mapping of SOC in South Africa by addressing these knowledge gaps and hypothesise that SOC losses and potential gains depend on prior land use and on the local climatic, edaphic, and vegetation context. We modelled SOC stocks (SOCs) as a function of environmental predictors using both linear mixed models and boosted regression trees, based on 6063 SOC samples collected over four decades across South Africa. We found that South Africa has lost between 9.3% and 14.9% of its total 0–30 cm surface SOCs due to land-use change, which is greater than the global average loss of 3.6% across the same soil depth. SOCs differed markedly among land uses: croplands, abandoned land, and barren land had 11%, 10%, and 43% lower SOCs than untransformed native vegetation (grasslands, savannas, and shrublands). Exotic tree plantations had approximately 8% higher SOCs than untransformed vegetation, but this may reflect pre-existing environmental conditions rather than causal effects. The dominant climatic, edaphic, and vegetation predictors of SOCs varied by land-use type, and this knowledge could assist in management decisions, e.g., active restoration via planting and irrigation in abandoned and barren lands. The greatest potential for SOC recovery through restoration was identified in mesic north-eastern regions, while arid zones had little recovery potential. Even complete restoration of all transformed land would yield a total SOC sequestration potential that is small in the global context, indicating limited mitigation potential at the national scale despite substantial co-benefits for biodiversity and soil health. Thus, protecting existing untransformed land through conservation and sustainable management remains essential, as regaining lost SOC is slow, costly, and uncertain.
人类土地利用的模拟效应表明,南非是全球土壤有机碳(SOC)预测损失最高的国家。这就迫切需要更好地了解不同土地利用方式的实际损失、损失的驱动因素以及恢复土壤有机碳存储的潜力。通过解决这些知识空白,我们扩展了南非以前的有机碳制图,并假设有机碳损失和潜在收益取决于以前的土地利用以及当地的气候、地理和植被环境。基于南非40多年来收集的6063份土壤有机碳样本,我们使用线性混合模型和增强回归树将土壤有机碳储量作为环境预测因子的函数进行建模。我们发现,由于土地利用变化,南非的0-30厘米表层有机碳总量损失了9.3%至14.9%,高于相同土壤深度的全球平均损失3.6%。不同土地利用方式的soc差异显著:农田、废弃土地和荒地的soc比未转化的原生植被(草原、稀树草原和灌丛地)低11%、10%和43%。外来人工林的soc比未转化植被高约8%,但这可能反映了预先存在的环境条件,而不是因果关系。土壤有机碳的主要气候、土壤和植被预测因子因土地利用类型而异,这些知识有助于管理决策,例如,通过在废弃和贫瘠土地上种植和灌溉来积极恢复。土壤有机碳恢复潜力最大的是东北中部地区,而干旱区恢复潜力较小。即使完全恢复所有改造过的土地,在全球范围内产生的总有机碳封存潜力也很小,表明在国家范围内的缓解潜力有限,尽管对生物多样性和土壤健康有巨大的共同利益。因此,通过保护和可持续管理来保护现有的未改造土地仍然是必不可少的,因为恢复失去的有机碳是缓慢、昂贵和不确定的。
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引用次数: 0
Surface soil physical property fingerprint of piping influenced gully erosion 地表土壤物性特征对沟沟侵蚀有影响
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2026-02-14 DOI: 10.1016/j.geodrs.2026.e01062
Nikola Živanović , Vukašin Rončević , Seyed Hamidreza Sadeghi , Vladimir Čebašek , Veljko Rupar , Siniša Polovina , Stevan Ćorluka
Understanding how soil physical properties differ between eroded and adjacent non-eroded microsites is essential for diagnosing early-stage rill–gully development and shallow piping in forested landscapes, yet paired microsite evidence remains limited. We quantified soil physical contrasts between gully/rill beds microsites (eroded) and adjacent banks (visually stable) across 13 cross-sections in a forested watershed in Serbia, while minimizing background variability in site conditions. We hypothesized that gully-bed soils differ from banks and that these contrasts are depth-dependent. Samples from two depth intervals (5–10 and 20–25 cm) were analyzed for soil moisture, density-based indices (bulk and dry bulk density, porosity, void ratio), particle-size distribution, Atterberg limits, and the clay activity index (AI). Microsite differences were strongest in the surface layer: gully-bed soils were wetter and showed lower clay, higher sand, higher AI, and higher liquid limit (wL) than banks. At 20–25 cm, microsite contrasts were weaker overall, but clay and sand contents remained significantly different, whereas silt content and particle density showed no meaningful variation across microsites or depths. Two-way ANOVA indicated that depth dominated density-derived indices and significantly affected moisture, clay, and plastic limit (wP), while sampling position significantly affected moisture, clay, AI, and wP; the depth × position interaction was significant only for moisture. An exploratory PCA-based composite score (E-PCS) summarized coordinated texture–consistency/activity shifts and separated gully-bed from bank samples across both depths. Overall, even incipient piping-related incision produced measurable, depth-dependent microsite contrasts, supporting shallow-horizon prioritization and depth stratification in monitoring designs for similar forested watersheds.
了解侵蚀和邻近非侵蚀微站点之间土壤物理性质的差异对于诊断森林景观中早期沟沟发育和浅管道至关重要,但相关的微站点证据仍然有限。在塞尔维亚森林流域的13个断面上,我们量化了沟/沟床微点(侵蚀)和相邻河岸(视觉稳定)之间的土壤物理对比,同时最大限度地减少了场地条件下的背景变异性。我们假设沟床土壤与河岸不同,这些差异与深度有关。对2个深度区间(5-10 cm和20-25 cm)的土壤水分、基于密度的指标(体积和干体积密度、孔隙率、空隙率)、粒径分布、Atterberg极限和粘土活性指数(AI)进行了分析。表层土壤微场差异最大:沟底土壤较湿润,粘土含量较低,砂粒含量较高,人工智能(AI)和液限(wL)较高。在20 ~ 25 cm处,微站点的差异总体上较弱,但粘土和砂粒含量仍有显著差异,而粉砂含量和颗粒密度在微站点和深度之间没有显著差异。双向方差分析表明,深度主导密度衍生指数,显著影响水分、粘土和塑性极限(wP),而采样位置显著影响水分、粘土、AI和wP;深度-位置交互作用仅对湿度有显著影响。探索性基于pca的复合评分(E-PCS)总结了协调的纹理一致性/活动变化,并将两个深度的沟床与河岸样本分开。总的来说,即使是早期的管道相关切口也产生了可测量的、与深度相关的微点对比,支持了类似森林流域监测设计中的浅层优先级和深度分层。
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引用次数: 0
Combining proximal and remote sensors for regional soil characterization in rural Haiti 结合近端和远程传感器在海地农村进行区域土壤表征
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2025-11-21 DOI: 10.1016/j.geodrs.2025.e01030
Anshuman Nayak , Reginald Cean , Somsubhra Chakraborty , Noura Bakr , Asim Biswas , Bin Li , D.K. Swain , David C. Weindorf
Agronomic optimization is critical in developing countries, especially where soil resources are constrained. This research, the first of its kind in Haiti, used predictive modeling to relate laboratory-derived physical and chemical soil data to proximal and remotely sensed data collected on 32,949 georeferenced surface soil (0–20 cm) samples in the Arcahaie region. A representative subset of collected samples (n = 300) was then tested using a litany of predictive models (e.g., random forest, gradient boosting, stacking ensemble, XGBoost) relating the lab-derived to proximally sensed data for the prediction of soil pH, sand, silt, clay, soil organic matter, cation exchange capacity, soil organic carbon, and plant available P, K, Si, Fe, and Cu. Results showed that sand, silt, clay, soil organic carbon, soil organic matter and cation exchange capacity all have predictive R2 of ≥0.80; predictions of soil texture components and soil organic carbon/organic matter were particularly strong. Other parameters, while still significant, were less robust. The models were used to predict the physical and chemical properties of the full dataset, then spatially interpolated to provide parameter variability maps across the region in support of agronomic optimization. Future research should work to extend the methodology successfully demonstrated herein to other regions of agronomic importance in Haiti and other developing countries. Furthermore, the approaches could be extended to three-dimensional modeling of subsoil properties elucidating optimal soil fertility in the rooting zone.
农艺优化在发展中国家至关重要,特别是在土壤资源有限的国家。这项研究是海地同类研究中的第一个,它使用预测模型将实验室获得的物理和化学土壤数据与Arcahaie地区32949个地理参考表层土壤(0-20厘米)样本的近端和遥感数据联系起来。然后使用一系列预测模型(例如,随机森林、梯度增强、堆叠集合、XGBoost)对收集的样本的代表性部分进行测试,这些预测模型将实验室导出的数据与近端感知数据相关联,用于预测土壤pH值、沙子、淤泥、粘土、土壤有机质、阳离子交换容量、土壤有机碳和植物有效磷、钾、硅、铁和铜。结果表明:沙土、粉土、粘土、土壤有机碳、土壤有机质、阳离子交换量的预测R2均≥0.80;对土壤质地成分和土壤有机碳/有机质的预测效果特别强。其他参数虽然仍然很重要,但鲁棒性较差。这些模型用于预测整个数据集的物理和化学性质,然后进行空间插值,以提供跨区域的参数变异图,以支持农艺优化。今后的研究应努力将本文成功示范的方法推广到海地和其他发展中国家的其他重要农业地区。此外,该方法还可扩展到阐明生根区最佳土壤肥力的底土特性的三维建模。
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引用次数: 0
Soil security assessment based on ethnopedological studies 基于人种学研究的土壤安全评价
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2025-12-05 DOI: 10.1016/j.geodrs.2025.e01035
Georgina Pérez-Rodríguez , Carlos Alberto Ortiz-Solorio , Ma. del Carmen Gutiérrez-Castorena , Atenógenes Leobardo Licona-Vargas , Javier Leonardo Toxqui-Roldan , Víctor Manuel Ordaz-Chaparro
Soil security assessment has been carried out on a regional or global scale using five dimensions that are difficult to assess due to lack of data, especially for connectivity. In contrast, ethnopedological studies are based on local knowledge of the soil and the value they place on their land, but their application is at the local level. The integration of these methodologies can overcome current limitations in data collection and in bridging scales and promote a more holistic approach to soil security assessment.
The objective of this research is to evaluate the soil security using an ethnopedological approach in a region of state-level agricultural significance in Mexico. The study employs an ethnopedological approach, encompassing five primary dimensions and proposing 17 sub-dimensions. The findings suggest that farmers contributed 60 % of the data, with the remaining 40 % comprising a blend of technical information and local soil knowledge, signifying a process of knowledge integration. The utilization of local soil knowledge facilitates not only the assessment of connectivity but also the determination of parameters for evaluating capacity, condition, capital, and codification. Furthermore, this approach yielded detailed maps for each of the dimensions, sub-dimensions, and levels of soil security for the five soil classes. The information can be beneficial for assessing soil security at the local level within the framework of small-scale farming, especially in countries with traditional knowledge and land management practices. In addition, it has the potential to play a key role in the formulation of public policy, particularly at the municipal level. This is due to its ability to enhance comprehension of the socio-cultural, and environmental dynamics of local areas.
土壤安全评估在区域或全球范围内进行,使用五个维度,由于缺乏数据,特别是连通性难以评估。相比之下,人种学研究是基于当地对土壤的了解和他们对土地的价值,但它们的应用是在地方一级。这些方法的综合可以克服目前在数据收集和衔接尺度方面的限制,促进对土壤安全评估采取更全面的办法。本研究的目的是利用民族志方法评估墨西哥国家级农业重要地区的土壤安全。该研究采用人种学方法,包括5个主要维度,并提出17个子维度。研究结果表明,农民贡献了60%的数据,剩下的40%混合了技术信息和当地土壤知识,表明了知识整合的过程。利用当地土壤知识不仅有助于评估连通性,还有助于确定评估能力、条件、资本和编纂的参数。此外,该方法还生成了五个土壤类别的每个维度、子维度和土壤安全级别的详细地图。这些信息有助于在小规模农业框架内评估地方一级的土壤安全,特别是在拥有传统知识和土地管理做法的国家。此外,它有潜力在制订公共政策方面发挥关键作用,特别是在市政一级。这是由于它能够增强对当地社会文化和环境动态的理解。
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引用次数: 0
Historical manure application affects accumulation pattern of residue-derived carbon via promoting macro-aggregation in Andosols, Japan 历史施用粪肥通过促进宏观聚集影响日本安多索的残馀碳积累模式
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2025-12-05 DOI: 10.1016/j.geodrs.2025.e01037
Hideaki Yasuno, Han Lyu, Haruo Tanaka, Soh Sugihara
Managing post-harvest crop residues is key to maintaining soil organic carbon (SOC) for achieving sustainable agriculture and mitigating climate change. However, how historical land management and residue quality affect residue-derived carbon (C) accumulation and pattern through aggregate formation and stabilization remains unclear, especially in Andosols. We conducted a 450-day in-situ incubation experiment using 13C-labeled maize residues (leaf: C/N = 15; root: C/N = 30) at historical managed cropland (Andosols) in Tokyo, Japan, under three land managements—manure (M), chemical fertilizer (Cf), and no fertilizer (Nf). Soil samples collected at 20, 60, 120, and 450 days were fractionated into macroaggregates (>250 μm), microaggregates (53–250 μm), and the silt+clay fraction (<53 μm) and analyzed. After 450 days, the remaining proportions of residue-derived C were 23 % (leaf) and 29 % (root), with no significant differences among land managements. However, decomposition rates at 450 days estimated by two-pool first-order model were significantly lower in M (0.37 mg C kg−1 day−1) than in Cf (0.60), indicating that manure application affected the accumulation pattern of residue-derived C. Because the macroaggregate mass proportion was higher in M (82 %) than in Cf (70 %), historical manure application should promote the macroaggregate formation and enhance the physical protection of residue-derived C, resulting in higher residue-derived C in macroaggregates at 450 days in M (0.38 g C kg−1) than in Cf (0.29). Overall, historical manure application caused the different accumulation pattern of residue-derived C especially at later period via macro-aggregation in Andosols, Japan.
管理收获后作物残茬是维持土壤有机碳(SOC)以实现可持续农业和减缓气候变化的关键。然而,历史上的土地管理和残留物质量如何通过聚集体的形成和稳定影响残留物衍生的碳(C)积累和模式尚不清楚,特别是在安多索尔。我们在日本东京的历史管理农田(Andosols)进行了为期450天的原位培养实验,使用13c标记的玉米残留物(叶片:C/N = 15;根部:C/N = 30),采用三种土地管理方式——粪肥(M)、化肥(Cf)和不施肥(Nf)。在20、60、120和450天采集的土壤样品被分成大团聚体(>250 μm)、微团聚体(53 - 250 μm)和粉土+粘土组分(<53 μm)并进行分析。450 d后,残馀碳的剩余比例分别为23%(叶片)和29%(根),不同土地管理方式间差异不显著。然而,两池一级模型估算的450 d分解率在M (0.37 mg C kg - 1 day - 1)显著低于Cf(0.60),表明施用粪肥影响了残源碳的积累模式。由于M的大团聚体质量比例(82%)高于Cf(70%),历史施用粪肥应促进大团聚体的形成,增强残源碳的物理保护。结果表明,在M中,450天大团聚体中残留衍生的碳含量(0.38 g C kg - 1)高于Cf(0.29)。总体而言,历史施肥导致日本安多索尔地区残馀源碳的累积模式不同,尤其是后期的宏观聚集。
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引用次数: 0
An alternative to mitigate soil compaction and improve crop yield under no-till systems 一种在免耕制度下减轻土壤压实和提高作物产量的替代方法
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2026-01-22 DOI: 10.1016/j.geodrs.2026.e01051
Camila Jorge Bernabé Ferreira , Vívian Ribeiro de Oliveira Preto , Cassio Antonio Tormena , Marcio Renato Nunes , Guilherme Braga Pereira Braz , Eduardo da Costa Severiano , Alvaro Sanz Saez de Jauregui
Soil compaction has caused significant crop yield losses owing to deleterious changes in the soil physical quality in the root zone. Our objective was to evaluate the use of seed drills equipped with fixed shanks operating at two depths under different levels of soil compaction as an alternative to mitigate soil compaction and improve crop yield in no-till (NT) conditions. The study was conducted in Paraná, southern Brazil, on a Rhodic Ferralsol under 20 years of NT management. The treatments included (i) four levels of induced soil compaction (0, 3, 6, and 9 tractor passes) and (ii) two operating depths of the seed drill shank (shallow = 10 cm and deep = 15 cm) as a strategy to mitigate soil compaction. The treatment effects on soil physical quality were quantified through soil air permeability, bulk density, water and air storage capacity, and penetration resistance, measured within 0–10 cm and 10–20 cm soil depths. Plant responses to the treatments were quantified by measuring the stem diameter, shoot dry mass, leaf area, plant height, and light interception. We measured the number of pods per plant at harvest, root diameter and length, and the grain yield. Soil compaction caused by tractor traffic increases water retention and decreases air storage capacity in the soil. The deep-acting shank significantly improved soil physical conditions for root growth and development compared with the shallow shank (10 cm), reducing soil bulk density by approximately 20% and penetration resistance by nearly 50%. Improved soil physical conditions within deeper soil layers promoted greater root length in the first 20 cm of soil profile, ensuring greater crop resistance to extreme weather. Overall, using seed drills equipped with deep-acting shanks is an efficient alternative for mitigating topsoil compaction (up to 15 cm) and promoting plant development in NT systems.
由于根区土壤物理质量的有害变化,土壤压实造成了重大的作物产量损失。我们的目标是评估在不同土壤压实程度下,在两个深度下使用配备固定柄的播种机作为缓解土壤压实和提高免耕(NT)条件下作物产量的替代方法。这项研究是在巴西南部的帕拉纳进行的,在一个Rhodic Ferralsol上进行了20年的NT管理。处理包括(i) 4个级别的诱导土壤压实(0、3、6和9个拖拉机通道)和(ii)两个操作深度的播种机柄(浅= 10 cm和深= 15 cm)作为缓解土壤压实的策略。通过在0 ~ 10 cm和10 ~ 20 cm土壤深度测量土壤透气性、容重、储水储气能力和渗透阻力,量化处理对土壤物理质量的影响。通过测定茎粗、地上部干质量、叶面积、株高和截光量来量化植株对不同处理的响应。我们测量了收获时每株的豆荚数、根的直径和长度以及籽粒产量。拖拉机交通造成的土壤压实增加了土壤的保水能力,降低了土壤的空气储存能力。与浅柄(10 cm)相比,深柄显著改善了根系生长发育的土壤物理条件,土壤容重降低约20%,穿透阻力降低近50%。深层土壤物理条件的改善促进了土壤剖面前20厘米根系长度的增加,确保了作物对极端天气的抵抗力。总的来说,在NT系统中,使用配备深层作用柄的播种机是缓解表土压实(高达15厘米)和促进植物发育的有效替代方法。
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引用次数: 0
Readily available water supply across soil variability in a center-pivot irrigated soybean field using the least limiting water range approach 采用最小限水范围方法的中心-枢纽灌溉大豆田土壤变异性的有效供水量
IF 3.3 2区 农林科学 Q2 SOIL SCIENCE Pub Date : 2026-03-01 Epub Date: 2025-12-09 DOI: 10.1016/j.geodrs.2025.e01040
Igor Alexandre de Souza , Dorotéo de Abreu , Alceu Linares Pádua Junior , Sérgio Henrique Godinho Silva , Bruno Montoani Silva
Intensified agricultural production frequently has a negative impact on soil physical-hydric properties, contributing significantly to soil degradation in the Brazilian Cerrado. The objective of this study was to assess the soil physical-hydric environment within a consolidated no-tillage system with at least 21 years of implementation. Three soil profiles were studied in representative locations of the 110 ha, with disturbed and undisturbed soil samples taken to represent the A, BA, and Bw1 horizons. The morphological description of the soil profiles was first performed, followed by analyses of soil granulometry, bulk density, soil particle density, and least limiting water range (LLWR) models for the entire area and profile of each horizon. The soils of the three profiles were classified as Dystrophic Yellow Latosol and had a sandy clay loam texture. The soil particle density ranged from 2.52 to 2.61 Mg m−3, and the bulk density average was 1.04 Mg m−3. The LLWR for the entire area showed field capacity and wilting point values of 0.26 and 0.22 m3 m−3, respectively, which were indicators of soil degradation in the A horizon. According to LLWR models, soil bulk density levels above 1.24 Mg m−3 impose physical constraints on plant development, with values above 1.31 Mg m−3 indicating more severe limitations. These findings highlight the effectiveness of LLWR in monitoring soil physical and water quality, and the penetration resistance becomes the main factor regardless of water content and aeration porosity.
集约化的农业生产经常对土壤的物理-水文特性产生负面影响,这在很大程度上导致了巴西塞拉多地区的土壤退化。本研究的目的是评估至少实施21年的统一免耕系统内的土壤物理水文环境。在110公顷的代表性地点研究了三种土壤剖面,并采集了受干扰和未受干扰的土壤样本来代表A、BA和Bw1层。首先进行了土壤剖面的形态描述,然后分析了整个区域和每个层位剖面的土壤粒度、体积密度、土壤颗粒密度和最小限水范围(LLWR)模型。3个剖面的土壤均属于营养不良黄壤壤,质地为砂质粘土壤土。土壤颗粒密度为2.52 ~ 2.61 Mg m−3,容重平均值为1.04 Mg m−3。全区LLWR的田间容量和凋萎点值分别为0.26和0.22 m3 m−3,是A层土壤退化的指标。根据LLWR模型,土壤容重高于1.24 Mg m−3会对植物发育产生物理限制,高于1.31 Mg m−3则会对植物发育产生更严重的限制。这些结果突出了LLWR在监测土壤物理和水质方面的有效性,无论含水量和通气性孔隙度如何,渗透阻力都是主要因素。
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引用次数: 0
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Geoderma Regional
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