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Cover cropping and minimum tillage improved microbial functional resilience to compaction stress in an acidic soil 覆盖和少耕提高了酸性土壤微生物功能对压实胁迫的恢复能力
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-19 DOI: 10.1016/j.still.2025.107031
Apsara Amarasinghe , Chengrong Chen , Lukas Van Zwieten , Michael T. Rose , Mehran Rezaei Rashti
Sustainable agriculture requires maintaining soil health, yet conventional management (CM) practices may not protect soils from stresses such as compaction. This study compared microbial resilience to compaction in two soils collected from sugarcane farms under improved management (IM: minimum tillage, cover cropping and stubble retention) and CM (conventional tillage, no cover crop and stubble retention) practices. Samples were placed in 96-well deep-well plates and compacted using a bespoke device to achieve bulk densities of 0.9 (control), 1.1 (low), and 1.2 g cm⁻³ (moderate). Microbial resistance was assessed 14 days after compaction, and resilience 14 days after stress relief. Under low and moderate compaction, IM soils showed 49.5 % and 45.7 % higher CO₂ emission resistance indices (i.e., the ability of soil to maintain microbial respiration under compaction stress) than CM, indicating greater stability. Microbial biomass carbon and nitrogen were 56.2 % and 47.9 % higher in IM soils under low compaction, compared to CM. Soil microbial metabolic quotient (qCO₂) was similar across compaction levels within each system, but was 19.5 %–36.3 % lower in IM soils than CM at equivalent compaction, indicating lower microbial stress under IM. Fourteen days after stress relief, qCO₂ in moderately compacted CM soil increased by 41.1 % and 25.0 % compared to control and low compaction. In contrast, IM soil under moderate compaction had 40.6 % lower qCO₂ than CM. The CM showed no effects of compaction on hot water extractable organic carbon content, while compaction of IM showed a 13 % decline compared to its control. Hot water extractable total nitrogen did not vary with compaction within the management systems but was 12 %–15 % higher in IM than CM under the same compaction during the resistance phase. Total mineral nitrogen was unaffected by compaction treatments under each system but was 11 %–13 % higher in IM than CM during resistance phase. These findings highlight the potential of improved management practices to sustain soil health and resilience under compaction stress.
可持续农业需要保持土壤健康,但传统的管理方法可能无法保护土壤免受压实等压力的影响。本研究比较了从改良管理(IM:最少耕作、覆盖种植和留茬)和CM(传统耕作、不覆盖种植和留茬)的甘蔗农场收集的两种土壤的微生物对压实的恢复力。样品被放置在96孔深孔板中,并使用定制的设备进行压实,以达到0.9(对照),1.1(低)和1.2 g cm⁻³ (中等)的体积密度。压实后14 d评估微生物耐药性,缓解胁迫后14 d评估恢复力。在低压实和中等压实条件下,IM土壤的CO₂排放阻力指数(即土壤在压实胁迫下维持微生物呼吸的能力)比CM土壤高49.5 %和45.7 %,表现出更强的稳定性。低压实条件下IM土壤微生物量碳和氮分别比CM土壤高56.2% %和47.9 %。土壤微生物代谢商(qCO₂)在不同压实水平下相似,但在相同压实度下,IM土壤比CM土壤低19.5 % -36.3 %,表明IM土壤的微生物胁迫较低。应力解除14 d后,中等压实CM土的qCO₂比对照和低压实分别增加了41.1% %和25.0% %。中等压实条件下IM土壤的qCO₂含量比CM土壤低40.6 %。压实处理对有机碳含量无显著影响,而压实处理的有机碳含量比对照降低13 %。在不同的管理体系中,热水可提取的总氮不随压实度的变化而变化,但在相同压实度下,在抵抗阶段,IM比CM高12 % -15 %。各体系下的总矿物氮不受压实处理的影响,但在抗性阶段,IM比CM高11 % ~ 13 %。这些发现强调了改善管理措施在压实压力下维持土壤健康和恢复力的潜力。
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引用次数: 0
Iron fractionation-directed mechanisms of soil organic carbon: A geochemically-grounded hypothesis and validation 土壤有机碳的铁分馏导向机制:基于地球化学的假设与验证
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-19 DOI: 10.1016/j.still.2025.107029
Fei Xie , Yuanqing Tang , Jin-E. Wei , Yangzheng Liu , Weifang Chen , Chengmei Liao , Changwei Lü
The stabilization of soil organic carbon (SOC) by reactive iron (Fe) minerals is a critical yet poorly quantified process in the global carbon cycle. To elucidate the specific mechanisms of Fe-mediated OC (organic carbon) fractionation, we employed a sequential chemical extraction protocol on < 53 μm soil fractions to isolate distinct Fe phases. This method was rigorously validated using X-ray diffraction (XRD) to correlate the extracted Fe species with specific mineral phases. A key methodological advancement was the developmen of a novel approach to quantify OC co-extracted with each Fe phase, enabling the first direct assessment of MAOC (mineral-associated organic carbon) partitioning to specific mineral hosts. Operationally, citrate-bicarbonate-dithionite (CBD) extraction targeted reactive Fe (FeHR) minerals (e.g., lepidocrocite, goethite, maghemite), while 12 M HCl dissolved poorly reactive Fe (FePR) phases (e.g., ankerite, magnetite, illite, montmorillonite). The residual silicate-bound Fe (FeU), such as grossular, riebeckite, mica, and orthoclase remained in the final residue. Our results revealed a quantitative partitioning of MAOC: FeU-OC dominated (47.9 %), indicative of long-term geological inheritance via physical occlusion within silicate matrices. FePR-OC (36.3 %) was stabilized predominantly by micropore confinement in low-activity minerals and cation bridging, effectively shielding OC from redox-driven dissolution. In contrast, FeHR-OC constituted the smallest fraction (15.8 %) but was the most dynamic, with its concentration strongly correlated with precipitation-induced Fe (oxyhydr)oxide transformation and vegetation diversity, leading to the formation of mineral-organic complexes. Mechanistically, we identified three distinct stabilization pathways: (1) reactive Fe/Al-(hydr)oxides bound OC mainly through chemical complexation or co-precipitation at high-surface-area mineral surfaces; (2) low-activity Fe/Al-(hydr)oxides associated with OC via physical adsorption; and (3) FeU-OC through physical encapsulation within silicate mineral frameworks and lattice-defects. These findings provide a mechanistic and quantitative framework for predicting the persistence of Fe-OC associations under changing environmental conditions.
在全球碳循环中,活性铁(Fe)矿物对土壤有机碳(SOC)的稳定作用是一个关键的但缺乏量化的过程。为了阐明铁介导OC(有机碳)分馏的具体机制,我们采用顺序化学萃取方案在<; 53 μm土壤组分上分离不同的铁相。用x射线衍射(XRD)对该方法进行了严格的验证,以确定提取的铁与特定矿物相的相关性。一个关键的方法进步是开发了一种新的方法来量化与每个Fe相共萃取的OC,从而首次直接评估MAOC(矿物相关有机碳)与特定矿物宿主的分配。在操作上,柠檬酸盐-碳酸氢盐-二硫代矿(CBD)萃取的目标是活性铁(FeHR)矿物(如绢云母、针铁矿、磁铁矿),而12 M HCl溶解的是活性较差的铁(FePR)相(如铁云母、磁铁矿、伊利石、蒙脱石)。残余的硅酸结合铁(FeU),如粗晶铁、辉贝克石、云母和正长石在最终残渣中残留。我们的研究结果揭示了MAOC的定量划分:FeU-OC占主导地位(47.9 %),表明在硅酸盐基质中通过物理遮挡进行了长期的地质继承。FePR-OC(36.3% %)主要通过低活性矿物的微孔限制和阳离子桥接来稳定,有效地屏蔽了氧化还原驱动的OC溶解。FeHR-OC占比最小(15.8 %),但其浓度与降水诱导的铁(氧)氧化物转化和植被多样性密切相关,导致矿物-有机复合物的形成。在机理上,我们确定了三种不同的稳定途径:(1)活性Fe/Al-(水合)氧化物结合OC主要通过化学络合或在高表面积矿物表面共沉淀;(2)低活性Fe/Al-(水合)氧化物通过物理吸附与OC结合;(3) FeU-OC通过硅酸盐矿物框架和晶格缺陷的物理封装。这些发现为预测在变化的环境条件下Fe-OC关联的持久性提供了一个机制和定量框架。
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引用次数: 0
Benchmarking soil potassium extraction methods and establishing critical thresholds for wheat production in Inceptisols 对土壤钾提取方法和建立小麦生产的临界阈值进行基准分析
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-16 DOI: 10.1016/j.still.2025.107017
Shubhadip Dasgupta , Rajat Pandit , Sudip Sengupta , Arup Dey , Kallol Bhattacharyya , Sanjay Srivastava , Owais Bashir , Kiran Lata , Somsubhra Chakraborty , Nicola Senesi , Abdessalam Ouallali , Mohamed Beroho , Shuraik Kader
Accurate assessment of plant-available potassium (K) in soils is crucial for optimizing crop nutrition and enhancing the efficiency of fertilizer use. This study systematically benchmarked ten widely used soil K extractants, Calcium Chloride (CaCl2), Ammonium Acetate (NH4OAc), Ammonium Bicarbonate-Diethylenetriaminepentaacetic Acid (AB-DTPA), Morgan's extractant (Morgan), Calcium acetate lactate extractant (Ca-AL), Kelowna extractant (Kelowna), Olsen extractant (Olsen), Modified Kelowna extractant (Kelowna-2), Nitric Acid (HNO₃), and Sodium Tetraphenylborate (NaTPB) to identify the most effective method for quantifying available K and defining critical thresholds for wheat production in Inceptisols. Pot trials were conducted on soils from twenty Inceptisol series in the Gangetic alluvial plains of Eastern India using five K fertilizer rates that simulates the wide K variability in real field situations. Among the tested methods, NaTPB emerged as the most reliable extractant, showing the strongest correlation (R2 = 0.83, P < 0.05) with Bray’s percent yield (BPY) and a critical K threshold of 1110.3 kg ha−1. CaCl2 also demonstrated high accuracy (R² = 0.82). Multivariate analysis revealed that NaTPB-extractable K was significantly influenced by soil clay content and electrical conductivity, which together explained 76.9 % of its variability. Furthermore, NaTPB effectively captured K from multiple pools, including water-soluble, exchangeable, and non-exchangeable pools, providing a more comprehensive index of plant-available K. A critical K concentration of 0.35 % in wheat grain was identified as the threshold for optimal yield, offering a practical benchmark for site-specific K management. By integrating chemical extraction, crop response modeling, and soil property analysis, this research presents a novel and scientifically robust framework for assessing K fertility. With the successful implementation in Eastern India, the findings have benchmarked broader applicability to Inceptisols in other agroecological regions, providing a scalable diagnostic approach for sustainable nutrient management. This study makes a significant contribution to precision agriculture and global efforts to optimize fertilizer recommendations through the development of improved soil testing methodologies.
准确评估土壤植物速效钾对优化作物营养和提高肥料利用效率至关重要。本研究系统地对十种广泛使用的土壤K萃取剂:氯化钙(CaCl2)、乙酸铵(NH4OAc)、碳酸氢铵-二乙烯三胺五乙酸(AB-DTPA)、摩根萃取剂(Morgan)、醋酸钙乳酸萃取剂(Ca-AL)、基洛纳萃取剂(Kelowna)、奥尔森萃取剂(Olsen)、改性基洛纳萃取剂(Kelowna-2)、硝酸(HNO₃)、和四苯基硼酸钠(NaTPB),以确定最有效的方法来量化有效钾和确定Inceptisols小麦生产的临界阈值。在印度东部恒河冲积平原的20个Inceptisol系列土壤上进行了盆栽试验,使用了5种钾肥率,模拟了实际现场情况下钾的广泛变化。在试验方法中,NaTPB是最可靠的萃取剂,与Bray产率(BPY)的相关性最强(R2 = 0.83, P <; 0.05),临界K阈值为1110.3 kg ha−1。CaCl2也显示出较高的准确性(R²= 0.82)。多变量分析表明,土壤粘土含量和电导率对natpb可提取钾的影响显著,两者共同解释了其变异率的76.9% %。此外,NaTPB有效地捕获了包括水溶性、交换性和非交换性在内的多个钾库,提供了更全面的植物速效钾指数。小麦籽粒中钾的临界浓度为0.35 %,是最佳产量的阈值,为特定地点的钾管理提供了实用基准。通过综合化学提取、作物响应模型和土壤性质分析,本研究提出了一个新的、科学可靠的评估钾肥力的框架。随着在印度东部的成功实施,研究结果为Inceptisols在其他农业生态区域的广泛适用性提供了基准,为可持续营养管理提供了可扩展的诊断方法。本研究通过改进土壤测试方法的发展,为精准农业和优化肥料建议的全球努力做出了重大贡献。
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引用次数: 0
The improved integral suspension pressure method for particle size analysis agrees well with the standard hydrometer method 改进的积分悬浮压力法与标准比重计法具有较好的一致性
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-16 DOI: 10.1016/j.still.2025.107021
Sára Poláchová, Martin Kovář, Lukáš Jačka
Particle size distribution (PSD) is a fundamental property of soil, influencing its physical and chemical properties. Consequently, PSD is commonly used to estimate other critical but harder-to-measure soil properties, such as hydraulic conductivity and soil water retention characteristics. Traditionally, PSD is determined using standard sedimentation methods, such as the pipette or hydrometer method. These conventional methods are, however, currently being replaced by innovative automated techniques, including approaches that measure pressure changes in suspensions. This study compares the standard hydrometer method (HM) with the improved integral suspension pressure method (ISP+), both of which operate on the same physical principle. Measurements were performed on fourteen soil types of varying texture, with identical sample pretreatment. For each type, four PSD analyses were carried out by the HM and four by the ISP+, yielding 112 analyses in total. The two methods showed strong agreement for clay fraction (R2 = 0.987; RMSE = 1.62 %) as well as the sand (R2 = 0.996; RMSE = 1.65 %) and silt fraction (R2 = 0.987; RMSE = 2.11 %). The strong correspondence in clay is particularly important, as it is corrected by oven-drying in ISP+ and represents a direct rather than an indirect estimate as in the case of silt. According to paired t-tests, there is no statistically significant difference between the methods. Although pretreatment and handling are similar to HM, ISP+ provides more detailed PSD data and can support more efficient laboratory workflows than standardized methods, representing a reliable alternative for routine soil texture determination.
土壤粒度分布是土壤的基本性质,影响土壤的理化性质。因此,PSD通常用于估计其他关键但难以测量的土壤特性,如水力导电性和土壤保水特性。传统上,PSD是用标准沉淀方法测定的,如移液器或比重计法。然而,这些传统的方法目前正在被创新的自动化技术所取代,包括测量悬架压力变化的方法。本研究比较了标准比重计法(HM)和改进的积分悬浮压力法(ISP+),两者在相同的物理原理下工作。在相同的样品预处理条件下,对14种不同质地的土壤进行了测量。对于每种类型,HM进行了4次PSD分析,ISP+进行了4次分析,总共进行了112次分析。两种方法对粘土组分(R2 = 0.987, RMSE = 1.62 %)、砂土组分(R2 = 0.996, RMSE = 1.65 %)和粉砂组分(R2 = 0.987, RMSE = 2.11 %)的测定结果吻合较好。粘土中的强对应关系尤其重要,因为它是通过ISP+ 的烘箱干燥来纠正的,并且代表了直接而不是像淤泥那样的间接估计。根据配对t检验,两种方法之间没有统计学上的显著差异。虽然预处理和处理类似于HM, ISP+ 提供更详细的PSD数据,可以支持比标准化方法更有效的实验室工作流程,代表常规土壤质地测定的可靠替代方案。
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引用次数: 0
Rainfall simulations on granite-derived red soils: How jute geotextile mulching regulates erosion dynamics and sediment sorting 花岗岩红壤的降雨模拟:黄麻土工织物覆盖物如何调节侵蚀动力学和沉积物分选
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-16 DOI: 10.1016/j.still.2025.107023
Shimin Ni , Yang Zhou , Chongfa Cai , Junguang Wang , Ziqiang Zou
Water-induced soil erosion severely endangers the sustainability of granite-derived red soil regions in southern China, where jute geotextiles hold promise for erosion control—yet their mechanisms in regulating erosion dynamics and sediment sorting remain poorly understood. This study investigated the erosion mitigation performance and underlying mechanisms of jute geotextile mulching through rainfall simulations, employing a 2 m × 1.2 m soil plot with four soil horizons (eluvium-A, illuvium-B, transitional-BC, parent material-C), two rainfall intensities (60 and 90 mm h−1), two slope gradients (5.56 % and 16.67 %), and three mulching treatments (bare control-CK, low-coverage-6.54 % and high-coverage-13.08 % jute geotextiles). Runoff, soil loss, flow hydrodynamics, and sediment sorting characteristics were analyzed to quantify treatment effects. High-coverage geotextiles could significantly reduce runoff coefficients by an average of 22.75 % and sediment loss by 50.01 % relative to CK. Hydrodynamically, jute geotextile could reduce mean flow velocity by 36.30 % and stream power by 22.75 %, facilitating a laminar-dominated flow regime (Re < 800) and suppressing transitions to supercritical flow. Sediment particle-size distribution (PSD) analysis revealed that clay-silt fractions (< 0.05 mm) were preferentially transported (enrichment ratio > 1), while sand-gravel fractions (> 0.05 mm) were retained in place (enrichment ratio < 1). This selectivity was amplified by high-coverage geotextiles, enabling an increase of clay enrichment ratio by 0.27–0.51 and a reduction of sediment mean weight diameter (MWD) by 0.09–0.17 mm, thereby promoting fine-particle enrichment and delaying sediment coarsening. Additionally, as rainfall progressed, a potential sediment transport mechanism was observed, namely the shift of sediment transport mode from initial suspension-saltation (fine-particle-domination) to later saltation-rolling (coarse-particle-domination). Importantly, this transition was delayed by jute geotextiles via intercepting coarse particles and sustaining fine-particle production. In conclusion, jute geotextiles can effectively mitigate sheet erosion in granite-derived red soils by regulating runoff energy and enhancing sediment sorting. Further research should prioritize optimization of geotextile grid density and synergies between geotextile mulching and local quartz gravels to balance erosion control efficacy, ecological benefits, and economic feasibility.
水致土壤侵蚀严重危及中国南方花岗岩红壤地区的可持续性,黄麻土工布有望控制侵蚀,但其调节侵蚀动力学和沉积物分选的机制尚不清楚。这项研究调查了减缓侵蚀性能和潜在机制的黄麻土工布覆盖通过降雨模拟,采用2 m×1.2  m土壤图有四个视野(eluvium-A、illuvium-B transitional-BC,父material-C),两个降雨强度(60和90年 mm h−1),两个坡渐变(5.56 % 16.67 %),和三个覆盖治疗(裸control-CK、低覆盖13.08 - 6.54 %和高覆盖率 %黄麻土工布)。径流、土壤流失、水流动力学和泥沙分选特性进行了分析,以量化处理效果。与对照相比,高盖度土工布可显著降低径流系数22.75% %,显著降低泥沙损失量50.01 %。在流体动力学上,黄麻土工布可以使平均流速降低36.30 %,水流功率降低22.75 %,促进层流主导的流动状态(Re < 800),并抑制向超临界流动的过渡。沉积物粒径分布(PSD)分析显示,粘土粉砂组分(< 0.05 mm)被优先搬运(富集比>; 1),砂砾组分(> 0.05 mm)被保留(富集比<; 1)。高覆盖度土工布放大了这种选择性,使粘土富集比提高了0.27-0.51,沉积物平均重径(MWD)降低了0.09-0.17 mm,从而促进了细颗粒富集,延缓了沉积物粗化。此外,随着降雨的增加,还发现了一种潜在的输沙机制,即输沙模式从最初的悬浮-跳跃(细颗粒为主)向后期的跳跃-滚动(粗颗粒为主)转变。重要的是,黄麻土工布通过拦截粗颗粒和维持细颗粒的生产,延缓了这种过渡。综上所述,黄麻土工布可以通过调节径流能量和加强沉积物分选来有效缓解花岗岩红壤的片层侵蚀。进一步的研究应优先考虑优化土工布网格密度以及土工布覆盖与当地石英石之间的协同作用,以平衡侵蚀控制效果、生态效益和经济可行性。
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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 : 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
Side soil covering and high-frequency low-volume irrigation improve cotton seedling emergence by altering soil physical properties and salinity 侧覆和高频小水量灌溉通过改变土壤物理性质和盐分来提高棉花出苗率
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-15 DOI: 10.1016/j.still.2025.107025
Fukui Gao , Qisheng Han , Jingsheng Sun , Qingyao Zhao , Guang Yang , Xianbo Zhang , Djifa Fidele Kpalari , Huifeng Ning , Hao Liu
The southern Xinjiang region is currently facing a situation of high per capita water resources but low per land water resources. With the expansion of agricultural irrigation areas and extensive water use, the actual water consumption has far exceeded the red line of total water use, and the existing water resources can no longer meet the needs of normal winter and spring irrigation. The aim of this study is to learn from the water-saving planting technology of dry sowing and wet emergence (DSWE) to promote the sustainable development of agriculture and optimize soil covering methods and irrigation management measures in Northern Xinjiang. A field experiment was conducted from 2021 to 2024. The local non-growing season drip spring irrigation mode (CK1, spring irrigation quota 90 mm) and conventional spring irrigation mode (CK2, spring irrigation quota 180 mm) were used as controls. For the DSWE planting technology, two soil covering forms of top sealing soil (TSS) and side sealing soil (SSS) were set up, and four irrigation quotas (G1: 30 mm, G2: 37.5 mm, G3: 45 mm, G4: 52.5 mm) were applied under each soil covering form. The results indicated that the TSS form was more effective in providing stable soil moisture and temperature conditions, whereas the SSS form significantly increased the cotton emergence rate and shortened emergence time by minimizing sowing depth and physical barriers. Crucially, the SSS form effectively mitigated the negative impacts caused by the increased sowing depth inherent in DSWE technology. By optimizing the SSS approach with precise, low-volume irrigation, we achieved cotton emergence performance comparable to conventional irrigation methods, while realizing water savings of over 40 % and up to 70 % compared with standard practices. This research provides a practical and highly efficient strategy for applying DSWE technology in water-scarce, saline environments, offering significant potential for mitigating agricultural water-use conflicts and promoting sustainable development in arid regions.
南疆地区目前面临着人均水资源高、土地水资源低的局面。随着农业灌溉面积的扩大和用水的粗放,实际用水量已远远超过总用水量红线,现有水资源已不能满足正常冬春灌溉的需要。本研究旨在借鉴干播湿出节水种植技术,促进北疆农业可持续发展,优化土壤覆盖方式和灌溉管理措施。2021 - 2024年进行了野外试验。以当地非生长期滴灌春灌方式(CK1,春灌定额90 mm)和常规春灌方式(CK2,春灌定额180 mm)为对照。DSWE种植技术设置顶封土(TSS)和侧封土(SSS)两种覆土形式,每种覆土形式下分别施用4个灌溉定额(G1: 30 mm, G2: 37.5 mm, G3: 45 mm, G4: 52.5 mm)。结果表明,TSS方式更能提供稳定的土壤湿度和温度条件,而SSS方式通过减少播深和物理屏障,显著提高了棉花出苗率,缩短了出苗期。至关重要的是,SSS形式有效地减轻了DSWE技术固有的播种深度增加所带来的负面影响。通过优化SSS方法,采用精确、小容量灌溉,我们实现了与传统灌溉方法相当的棉花出苗率,同时实现了超过40% %的节水,与标准做法相比节水高达70% %。本研究为在缺水、盐碱化环境中应用DSWE技术提供了一种实用、高效的策略,为缓解干旱地区农业用水冲突和促进可持续发展提供了巨大潜力。
{"title":"Side soil covering and high-frequency low-volume irrigation improve cotton seedling emergence by altering soil physical properties and salinity","authors":"Fukui Gao ,&nbsp;Qisheng Han ,&nbsp;Jingsheng Sun ,&nbsp;Qingyao Zhao ,&nbsp;Guang Yang ,&nbsp;Xianbo Zhang ,&nbsp;Djifa Fidele Kpalari ,&nbsp;Huifeng Ning ,&nbsp;Hao Liu","doi":"10.1016/j.still.2025.107025","DOIUrl":"10.1016/j.still.2025.107025","url":null,"abstract":"<div><div>The southern Xinjiang region is currently facing a situation of high per capita water resources but low per land water resources. With the expansion of agricultural irrigation areas and extensive water use, the actual water consumption has far exceeded the red line of total water use, and the existing water resources can no longer meet the needs of normal winter and spring irrigation. The aim of this study is to learn from the water-saving planting technology of dry sowing and wet emergence (DSWE) to promote the sustainable development of agriculture and optimize soil covering methods and irrigation management measures in Northern Xinjiang. A field experiment was conducted from 2021 to 2024. The local non-growing season drip spring irrigation mode (CK1, spring irrigation quota 90 mm) and conventional spring irrigation mode (CK2, spring irrigation quota 180 mm) were used as controls. For the DSWE planting technology, two soil covering forms of top sealing soil (TSS) and side sealing soil (SSS) were set up, and four irrigation quotas (G1: 30 mm, G2: 37.5 mm, G3: 45 mm, G4: 52.5 mm) were applied under each soil covering form. The results indicated that the TSS form was more effective in providing stable soil moisture and temperature conditions, whereas the SSS form significantly increased the cotton emergence rate and shortened emergence time by minimizing sowing depth and physical barriers. Crucially, the SSS form effectively mitigated the negative impacts caused by the increased sowing depth inherent in DSWE technology. By optimizing the SSS approach with precise, low-volume irrigation, we achieved cotton emergence performance comparable to conventional irrigation methods, while realizing water savings of over 40 % and up to 70 % compared with standard practices. This research provides a practical and highly efficient strategy for applying DSWE technology in water-scarce, saline environments, offering significant potential for mitigating agricultural water-use conflicts and promoting sustainable development in arid regions.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107025"},"PeriodicalIF":6.8,"publicationDate":"2025-12-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145784849","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
Influence of management practices on soil organic matter composition evaluated by complementary analytical techniques: XANES and mass spectrometry 利用互补分析技术:XANES和质谱法评估管理措施对土壤有机质组成的影响
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-12 DOI: 10.1016/j.still.2025.107009
Peter K. Leinweber , Riffat Rahim , Edyta Hewelke , Tom Regier , Jerzy Weber
The impact of soil management practices on carbon (C) sequestration in soil organic matter (SOM) is insufficiently known. We studied relevant treatments, including manure application, legumes incorporation, their combination, conventional and no-tillage systems, as well as tillage with and without catch crops, at three long-term experimental sites in Poland. Bulk soil and humin fractions were analyzed by X-ray absorption near edge structure (XANES) spectroscopy and thermochemolysis-gas chromategraphy/mass spectrometry (TC-GC/MS). XANES and TC-GC/MS revealed treatment-specific molecular enrichments. Legume cropping enhanced total organic carbon (TOC) and enriched aromatic and aliphatic C structures, particularly at Skierniewice, contributing significantly to SOM stabilization. At Chylice, no-tillage preserved a higher aromatic C content, indicating a contribution of relatively stable compounds to SOM enrichment. At Swojec, the application of catch crops resulted in a balanced C profile with aliphatic C enrichments. Humin consistently exhibited greater aromatic and carboxylic C intensities compared to bulk soil, emphasizing its role as a relatively stable C reservoir. The findings demonstrate that for comparable climatic and soil conditions, no-till management is more efficient in enriching relatively recalcitrant aromatic SOM than the addition of organic matter through manure and legumes. No-till is therefore recommended as a first, immediately effective measure for SOM enrichment under Central European conditions.
土壤管理措施对土壤有机质中碳(C)固存的影响尚不清楚。我们在波兰的三个长期试验点研究了相关的处理,包括施肥、豆科植物掺入、它们的组合、常规和免耕系统,以及有和没有捕获作物的耕作。采用x射线吸收近边结构(XANES)光谱和热化学-气相色谱/质谱(TC-GC/MS)分析大块土壤和人体组分。XANES和TC-GC/MS显示了处理特异性的分子富集。豆科作物增加了总有机碳(TOC),并丰富了芳香和脂肪碳结构,特别是在斯基尼维兹,这对SOM的稳定起着重要作用。在Chylice,免耕保留了较高的芳香C含量,表明相对稳定的化合物对SOM的富集有贡献。在Swojec,施用捕捞作物导致碳分布平衡,脂肪族碳富集。与散装土壤相比,胡敏土壤始终表现出更高的芳香碳和羧酸碳强度,强调了其作为相对稳定的碳库的作用。研究结果表明,在可比的气候和土壤条件下,免耕管理比通过粪肥和豆类添加有机质更有效地富集相对顽固的芳香SOM。因此,免耕被推荐为中欧条件下SOM富集的第一个,立即有效的措施。
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引用次数: 0
Soil strength after 21 years of conventional and organic cropping practices in the Mid-Atlantic region, USA 美国中大西洋地区21年传统和有机种植后的土壤强度
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-11 DOI: 10.1016/j.still.2025.107020
Harry H. Schomberg , Kipling S. Balkcom , Michel A. Cavigelli , Kathryn E. White
Soil compaction negatively impacts soil physical properties and crop yields and is influenced by organic matter inputs and tillage management. We evaluated cone index (CI) in five long-term organic and conventional cropping systems at the Farming Systems Project in Beltsville, MD (39.0°N, 76.9°W), to understand how different management systems influence soil strength. Measurements were collected prior to planting corn in 2017 using a tractor-mounted hydraulic five-probe penetrometer for three depths (0–15, 15–30, 30–50 cm) and three positions relative to the crop row (0, 22.5, and 45 cm). The two conventional systems, No-till (NT) and Chisel Till (CT), were both 3-yr corn-rye cover crop/soybean–wheat/soybean rotations. The three organic systems were comprised of: (Org2) 2-yr hairy vetch cover crop/corn-rye cover crop/soybean; (Org3) 3-yr hairy vetch cover crop/corn-rye cover crop/soybean–wheat; and (Org6) 6-yr corn-rye cover crop/soybean–wheat–alfalfa–alfalfa–alfalfa. Org2 and Org3 exhibited the lowest CI in the 0–15 cm depth, due to fall tillage before cover crop planting and weed control in the prior crop. In contrast, surface soil compaction in Org6 was similar to that in the conventional systems, attributed to alfalfa harvest machinery traffic over the past three years and absence of any tillage. At deeper depths (15–30 cm and 30–50 cm), the NT system consistently demonstrated lower CI compared to other systems. For tilled systems, maximum CI values at 15–30 cm were near or exceeded the root-restricting threshold of 2.5 MPa. The NT system potentially provided a larger rooting volume for water and nutrient uptake than tilled systems. Machinery traffic increased compaction, particularly at 22.5 cm from the crop row, likely due to tire sidewall pressure. Overall, the study found moderate effects of contrasting management system practices on soil strength.
土壤压实对土壤物理性质和作物产量产生负面影响,并受有机质投入和耕作管理的影响。我们在马里兰州贝尔茨维尔(39.0°N, 76.9°W)的农业系统项目中评估了五种长期有机和传统种植系统的锥体指数(CI),以了解不同管理系统如何影响土壤强度。在2017年种植玉米之前,使用拖拉机安装的液压五探头贯深仪收集了三个深度(0 - 15、15-30、30-50 cm)和相对于作物行(0、22.5和45 cm)的三个位置的测量数据。免耕(NT)和凿耕(CT)两种常规制度均为3年玉米-黑麦覆盖作物/大豆-小麦/大豆轮作。3个有机体系由:(Org2) 2年叶茅覆盖/玉米-黑麦覆盖/大豆组成;(组织3)3年毛豆覆盖作物/玉米-黑麦覆盖作物/大豆-小麦;6年玉米-黑麦覆盖作物/大豆-小麦-苜蓿-苜蓿。在0 ~ 15 cm深度,Org2和Org3表现出最低的CI,这是由于覆盖作物种植前的秋耕和前茬作物的杂草控制所致。相比之下,Org6的表层土壤压实与常规系统相似,这是由于过去3年的苜蓿收获机械运输和没有任何耕作造成的。在较深的深度(15-30 cm和30-50 cm), NT系统的CI始终低于其他系统。耕制体系在15 ~ 30 cm处的最大CI值接近或超过根系限制阈值2.5 MPa。NT系统可能比耕作系统提供更大的生根体积,以吸收水分和养分。机械交通增加了压实,特别是在距作物行22.5 厘米处,可能是由于轮胎侧壁压力。总体而言,研究发现对比管理制度对土壤强度的影响适中。
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引用次数: 0
Depth-discrepant impact of winter cover crops on particulate and mineral-associated organic carbon in a subtropical paddy field 冬季覆盖作物对亚热带稻田颗粒和矿物相关有机碳的深度差异影响
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-11 DOI: 10.1016/j.still.2025.107015
Zihan Zhang, Dongqiao Yang, Mengya Lu, Bin Zhang, Xueli Ding
Replacing winter fallow with cover crops can improve soil organic carbon (SOC) sequestration in agroecosystems, with cover crop species potentially differing in their contributions to SOC formation and stabilization. However, how different crop species affect the accumulation of distinct SOC fractions (particulate organic C, POC; mineral-associated organic C, MAOC) and their contribution to SOC storage remain unclear, particularly in subsoils of paddy fields. Here, we investigated how POC and MAOC responded to different cover crop species (hairy vetch, Vicia villosa Roth., and winter wheat, Triticum aestivum L.) in both topsoil (0–20 cm) and subsoil (20–40 cm, 40–60 cm) in paddy soils. Our results revealed that different cover crops induced divergent responses in SOC fractions, contingently dependent upon soil depths. Both cover crops significantly stimulated POC accumulation (winter wheat: 41.3 %; hairy vetch: 46.1 %) relative to fallow in topsoil, while cover crop effects on POC gradually diminished in subsoil. Meanwhile, cover crops significantly increased contents of dissolved organic carbon and available phosphorus, particularly in deeper subsoil, which were key factors affecting SOC accumulation. POC and MAOC accumulation along soil depths differed significantly between different cover crops, suggesting a species-specific effect. Winter wheat significantly boosted MAOC in both topsoil and deeper subsoil, while hairy vetch induced a statistically nonsignificant increase in MAOC across three depths compared to fallow. These divergent responses of SOC fractions were closely related to cover crop-induced changes of microbial community composition, necromass accumulation and enzyme activity. Random forest analysis revealed that microbial necromass was the main factor defining MAOC in topsoil, whereas the Fe oxides was the main factor influencing subsoil MAOC accumulation. Overall, winter cover increased total SOC sequestration across 0–60 cm soil depths and more importantly, potential SOC stability (MAOC:POC) was enhanced in subsoil. These findings demonstrate a depth-discrepant impact of cover crops on POC and MAOC in paddy soils. Our work highlights the need to present POC and MAOC fractions into biogeochemical models to better predict responses of SOC to cover crop management practices in rice paddy ecosystems.
以覆盖作物代替冬季休耕可以改善农业生态系统中土壤有机碳(SOC)的固存,但覆盖作物种类对有机碳形成和稳定的贡献可能存在差异。然而,不同作物种类如何影响不同有机碳组分(颗粒有机碳,POC;矿物相关有机碳,MAOC)的积累及其对有机碳储存的贡献尚不清楚,特别是在稻田底土中。本研究研究了不同覆盖作物(毛豆、野豌豆)对POC和MAOC的响应。水稻土表层(0 ~ 20 cm)和底土(20 ~ 40 cm, 40 ~ 60 cm)的冬小麦(Triticum aestivum L.)。研究结果表明,不同覆盖作物对土壤有机碳组分的影响随土壤深度的不同而不同。两种覆盖作物均显著促进表层土壤POC积累(冬小麦:41.3 %;毛杨:46.1 %),而覆盖作物对底土POC的影响逐渐减弱。同时,覆盖作物显著提高了土壤溶解有机碳和速效磷含量,尤其是深层土壤,这是影响土壤有机碳积累的关键因素。不同覆盖作物的POC和MAOC沿土壤深度累积量存在显著差异,表明存在物种特异性效应。与休耕相比,冬小麦显著提高了表层土壤和深层土壤的毛氧含量,而毛豆在三个深度上的毛氧含量都没有显著增加。土壤有机碳组分的差异响应与覆盖作物引起的微生物群落组成、坏死块积累和酶活性的变化密切相关。随机森林分析表明,微生物坏死团块是表层土壤中MAOC的主要决定因素,而铁氧化物是影响底土MAOC积累的主要因素。总体而言,冬季覆盖增加了0-60 cm土壤深度的总有机碳固存,更重要的是,增加了土壤有机碳稳定性(MAOC:POC)。这些结果表明覆盖作物对水稻土POC和MAOC的影响存在深度差异。我们的工作强调需要将POC和MAOC组分纳入生物地球化学模型,以更好地预测水稻生态系统中有机碳对作物管理措施的响应。
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引用次数: 0
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