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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。
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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。
{"title":"Soil strength after 21 years of conventional and organic cropping practices in the Mid-Atlantic region, USA","authors":"Harry H. Schomberg ,&nbsp;Kipling S. Balkcom ,&nbsp;Michel A. Cavigelli ,&nbsp;Kathryn E. White","doi":"10.1016/j.still.2025.107020","DOIUrl":"10.1016/j.still.2025.107020","url":null,"abstract":"<div><div>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.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107020"},"PeriodicalIF":6.8,"publicationDate":"2025-12-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145732409","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
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
Phosphorus adsorption-desorption dynamics across a soil texture gradient in floodplain agricultural soilscape of the middle Yellow River, China 黄河中游河漫滩农业土壤中磷在土壤结构梯度上的吸附-解吸动态
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-11 DOI: 10.1016/j.still.2025.107007
Xiaojun Nie , Xingyu Du , Tongqian Zhao , Jinchan Zheng , Xinyi Li , Wenjing Zhang
Little attention has been paid to Phosphorus (P) adsorption-desorption in agricultural soilscape with varying soil textures under field-relevant P application practices. This study examined these processes in the Middle Yellow River floodplain landscapes, focusing on field-relevant P application rates and soil disturbance. At a field-relevant 10 mg P L−1 rate, finer-textured ground soils (silty clay, loam, silty loam) exhibited an initial fast adsorption and gradual equilibrium and best obeyed the Elovich model, indicating chemisorption on heterogeneous surfaces. Coarse-textured loamy sand exhibited desorption–adsorption at ≤ 100 mg P L⁻¹ , transitioning to Elovich-type adsorption only at ≥ 200 mg L⁻¹ . Silty clay had the most available adsorption sites, loamy sand the fewest. As soil texture coarsened, P adsorption-desorption maximum potentials, binding strength and buffering capacity decreased, while its reversibility increased (26 % in silty clay to 54 % in loamy sand). At the field rate, P adsorption/desorption correlated with clay, sand, CaCO₃, and soil organic matter (SOM), with clay explaining 81 % of adsorption variance and sand 65 % of desorption variance (p < 0.05). Undisturbed soil experiments showed higher adsorption at 5 mg P L⁻¹ addition but lower adsorption at 100 mg L⁻¹ for loamy sand and silty clay. Across textures undisturbed soils had very low P adsorption (1.3 %–10.1 % of ground soils) at field rates (5–30 mg P L⁻¹), underscoring soil disturbance’s impact and real-ideal disparity. These findings demonstrate that soil clay and sand contents dominate field-relevant P adsorption-desorption in agricultural soilscape with varying textures. Undisturbed soil’s P adsorption is minimal, which complements ground soil experiment-derived understanding. Texture-specific P management is vital for floodplain sustainable agriculture and aquatic protection.
不同土壤结构的农田土壤中磷的吸附-解吸特性在不同施用条件下一直受到较少关注。本研究在黄河中游漫滩景观中考察了这些过程,重点研究了与农田相关的施磷量和土壤扰动。在与现场相关的10 mg P L−1速率下,细质土壤(粉质粘土、壤土、粉质壤土)表现出最初的快速吸附和逐渐平衡,并最符合Elovich模型,表明化学吸附在非均质表面上。粗质壤土砂在≤ 100 mg P L⁻¹ 时表现出解吸-吸附,仅在≥ 200 mg L⁻¹ 时向elovic型吸附过渡。粉质粘土的有效吸附位点最多,壤土砂最少。随着土壤质地变粗,磷的最大吸附解吸势、结合强度和缓冲能力降低,而其可逆性增加(粉质粘土为26 %,壤土砂为54 %)。在现场速率下,P的吸附/解吸与粘土、沙子、CaCO₃和土壤有机质(SOM)相关,粘土解释81 %的吸附方差,沙子解释65 %的解吸方差(P <; 0.05)。未受干扰的土壤实验表明,添加5 mg P L⁻¹ 时吸附性较高,而添加100 mg L⁻¹ 时吸附性较低。在不同的结构中,未受干扰的土壤在田间速率(5-30 mg P L⁻¹)下的P吸附量非常低(地表土壤的1.3 % -10.1 %),强调了土壤干扰的影响和实际理想的差异。这些结果表明,在不同质地的农业土壤中,土壤粘粒和沙粒含量主导着田间相关磷的吸附-解吸。未受干扰的土壤对磷的吸附最小,这补充了地面土壤实验得出的认识。土壤磷管理对河漫滩可持续农业和水生生物保护至关重要。
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引用次数: 0
While legume-based rotation influences the chemical composition of mineral-associated organic matter, tillage has little effect on its persistence 以豆科植物为基础的轮作影响矿物相关有机质的化学组成,而耕作对其持久性影响不大
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-11 DOI: 10.1016/j.still.2025.107014
Paulina B. Ramírez , Surendra Singh , Stephen Machado , Roser Matamala , Shikha Singh , Francisco Calderón
Legume-based rotations are key to enhancing soil carbon (C) storage in stable forms such as mineral-associated organic matter (MAOM), improving soil health, and helping maintain long-term C stock. This study investigates how plant inputs and tillage practices influence the distribution, composition, and persistence of MAOM in wheat cropping systems when legumes are incorporated into the rotation. Soil samples were collected from Walla Walla silty loam of northeast Oregon, including conventional tillage (CT) and no-till (NT) treatments in a long-term dryland winter wheat (Triticum aestivum L.) and spring pea (Pisum sativum L.) rotation experiment, with an adjacent grass pasture (GP) plot serving as the baseline. Bulk soil, particulate organic matter (POM), and MAOM fractions were scanned using mid-infrared (Mid-IR) spectroscopy and analyzed for total C and nitrogen (N) as well as radiocarbon age, aggregate stability, and mineralizable C. In WP systems, NT promoted greater C accumulation and stabilization in MAOM than CT, reaching levels similar to those under native GP conditions. Furthermore, our findings indicate that decades of continuous legume-based rotation were insufficient to restore total bulk C content to levels observed in the undisturbed reference site (GP) in the 0–30 cm layer, with increases limited to the surface layer. The Mid-IR data provided insights into how cultivation may alter the chemical composition of MAOM. An increase in amide bands was observed in GP, while legume-based rotation systems favored an abundance of aliphatic (C-H) components in the MAOM fraction. In cultivated soils, C in MAOM exhibited longer residence times under arable conditions than in grassland, while POM remained an actively cycled pool across all treatments. Despite variations in the chemical composition of MAOM across treatments, mineralizable C emissions from MAOM fractions remained statistically unchanged during the 96-hour incubation period. Our findings suggest that soil physical protection, enhanced by reduced tillage, is the primary factor influencing MAOM cycling.
豆类轮作是提高土壤碳(C)以矿物相关有机质(MAOM)等稳定形式储存、改善土壤健康和帮助维持长期碳储量的关键。本研究调查了当豆类轮作时,植物投入和耕作方式如何影响小麦种植系统中MAOM的分布、组成和持久性。在美国俄勒冈州东北部的Walla Walla粉质壤土上采集土壤样品,采用常规耕作(CT)和免耕(NT)处理,以相邻草地(GP)小区为基准,进行旱地冬小麦(Triticum aestivum L.)和春豌豆(Pisum sativum L.)长期轮作试验。利用中红外(Mid-IR)光谱扫描土壤、颗粒有机质(POM)和MAOM组分,并分析总C和氮(N)、放射性碳年龄、团聚体稳定性和可矿化C。在WP系统中,NT比CT促进MAOM中更多的C积累和稳定,达到与原生GP条件相似的水平。此外,我们的研究结果表明,连续数十年的豆科植物轮作不足以将0-30 cm层未受干扰的参考点(GP)的总体积C含量恢复到观测到的水平,增加仅限于表层。中红外数据提供了培养如何改变MAOM化学成分的见解。在GP中观察到酰胺带的增加,而豆科植物为基础的旋转系统有利于MAOM部分中脂肪族(C-H)成分的丰富。在耕地土壤中,土壤中碳在耕地条件下的停留时间比在草地条件下更长,而POM在所有处理下都是一个活跃的循环池。尽管不同处理的MAOM的化学成分有所不同,但在96小时的孵育期间,MAOM馏分的可矿化C排放量在统计上保持不变。研究结果表明,减少耕作所增强的土壤物理保护是影响MAOM循环的主要因素。
{"title":"While legume-based rotation influences the chemical composition of mineral-associated organic matter, tillage has little effect on its persistence","authors":"Paulina B. Ramírez ,&nbsp;Surendra Singh ,&nbsp;Stephen Machado ,&nbsp;Roser Matamala ,&nbsp;Shikha Singh ,&nbsp;Francisco Calderón","doi":"10.1016/j.still.2025.107014","DOIUrl":"10.1016/j.still.2025.107014","url":null,"abstract":"<div><div>Legume-based rotations are key to enhancing soil carbon (C) storage in stable forms such as mineral-associated organic matter (MAOM), improving soil health, and helping maintain long-term C stock. This study investigates how plant inputs and tillage practices influence the distribution, composition, and persistence of MAOM in wheat cropping systems when legumes are incorporated into the rotation. Soil samples were collected from Walla Walla silty loam of northeast Oregon, including conventional tillage (CT) and no-till (NT) treatments in a long-term dryland winter wheat (<em>Triticum aestivum L</em>.) and spring pea (<em>Pisum sativum L</em>.) rotation experiment, with an adjacent grass pasture (GP) plot serving as the baseline. Bulk soil, particulate organic matter (POM), and MAOM fractions were scanned using mid-infrared (Mid-IR) spectroscopy and analyzed for total C and nitrogen (N) as well as radiocarbon age, aggregate stability, and mineralizable C. In WP systems, NT promoted greater C accumulation and stabilization in MAOM than CT, reaching levels similar to those under native GP conditions. Furthermore, our findings indicate that decades of continuous legume-based rotation were insufficient to restore total bulk C content to levels observed in the undisturbed reference site (GP) in the 0–30 cm layer, with increases limited to the surface layer. The Mid-IR data provided insights into how cultivation may alter the chemical composition of MAOM. An increase in amide bands was observed in GP, while legume-based rotation systems favored an abundance of aliphatic (C-H) components in the MAOM fraction. In cultivated soils, C in MAOM exhibited longer residence times under arable conditions than in grassland, while POM remained an actively cycled pool across all treatments. Despite variations in the chemical composition of MAOM across treatments, mineralizable C emissions from MAOM fractions remained statistically unchanged during the 96-hour incubation period. Our findings suggest that soil physical protection, enhanced by reduced tillage, is the primary factor influencing MAOM cycling.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107014"},"PeriodicalIF":6.8,"publicationDate":"2025-12-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145732410","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
Divergent responses of soil carbon dynamics to terracing under natural aridity in semi-arid regions 半干旱区自然干旱条件下土壤碳动态对梯田的差异性响应
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-10 DOI: 10.1016/j.still.2025.107006
Shuaihao Mo , Ying Wang , Ziji Lv , Xinhao Li , Yanxing He , Peidan Xu , Shiwei Zhao , Jinghua Huang , Xuan Du , Jinshi Jian
Drylands play a crucial role in global soil carbon (C) sequestration, with soil C dynamics jointly determined by soil organic C (SOC) and inorganic C (SIC). In addition to aridity’s control, soil C dynamics in drylands are also influenced by human activities, such as terrace construction, thereby augmenting the uncertainty in assessing and predicting soil C sequestration functions. Terraces converted from sloping farmland are an important agricultural land use type, but there has been limited research on the effects of terracing on SOC, SIC, and soil total C (STC) under varying aridity. Here, we selected four representative terracing sites on the Chinese Loess Plateau, two in regions with lower aridity and the other two in regions with higher aridity. SOC, SIC, and STC contents along with influencing variables were analyzed to investigate how terracing affects soil C dynamics under different aridity conditions. Results showed that both SOC and SIC contents synergistically increased following sloping farmland conversion to terraces under lower aridity conditions, thus contributing to an elevation in STC content. However, terracing increased SOC content yet reduced SIC content under higher aridity conditions, and SOC-SIC trade-offs caused fluctuation or even loss in STC content. Consequently, soil C dynamics in terraces exhibited divergent responses to shifts in aridity, and this effect intensified with the terraced age (p < 0.05). Moreover, soil pH emerged as the primary driver of C dynamics in terraced soils under different aridity conditions, with SOC and STC declining and SIC increasing significantly as pH increased (p < 0.05). In addition, mineral protection enhanced SOC accrual under lower aridity conditions, as evidenced by a significant positive correlation between SOC and clay contents (p < 0.001). SOC and SIC contents responded positively (p = 0.001) and negatively (p < 0.001) to soil moisture variations under higher aridity conditions, respectively. In conclusion, these findings highlight the importance of simultaneously considering changes in both SOC and SIC when predicting and enhancing the C sequestration capacity of terraced soils in drylands, thus contributing to mitigating global climate change.
旱地在全球土壤碳固存中起着至关重要的作用,土壤碳动态是由土壤有机碳(SOC)和无机碳(SIC)共同决定的。除了干旱控制外,旱地土壤C动态也受到阶地建设等人类活动的影响,从而增加了评估和预测土壤C固存功能的不确定性。坡耕地梯田是一种重要的农业用地类型,但不同干旱条件下梯田对土壤有机碳、碳化硅和土壤总碳(STC)的影响研究较少。本文选取了黄土高原4个具有代表性的梯田样地,其中2个位于低干旱区,2个位于高干旱区。分析了不同干旱条件下梯田土壤有机碳(SOC)、碳化硅(SIC)和STC含量及其影响因素。结果表明,低干旱条件下坡耕地退耕还田后,土壤有机碳和碳化硅含量协同增加,导致土壤有机碳含量升高。然而,在高干旱条件下,梯田增加了SOC含量,降低了SIC含量,SOC-SIC权衡导致了STC含量的波动甚至损失。因此,梯田土壤C动态对干旱变化的响应呈差异,且随梯田年龄的增加而增强(p <; 0.05)。土壤pH值是不同干旱条件下梯田土壤碳动态的主要驱动因子,随着pH值的增加,土壤有机碳和碳含量显著下降,碳化硅显著增加(p <; 0.05)。此外,在低干旱条件下,矿物保护增强了有机碳的积累,有机碳与粘土含量之间存在显著的正相关关系(p <; 0.001)。高干旱条件下,土壤有机碳和碳化硅含量对土壤水分变化分别呈正响应(p = 0.001)和负响应(p <; 0.001)。综上所述,这些发现强调了在预测和增强旱地梯田土壤固碳能力时同时考虑有机碳和碳化硅变化的重要性,从而有助于减缓全球气候变化。
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引用次数: 0
Crop planting promotes the stabilization of straw-derived carbon in fertilized soil by regulating soil stoichiometry 作物种植通过调节土壤化学计量来促进施肥土壤中秸秆碳的稳定
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-09 DOI: 10.1016/j.still.2025.107008
Tengxiao Zhu , Xiuwen Mei , Yuping Li , Shuangyi Li , Tingting An , Jingkuan Wang
Straw returning to cropland is a sustainable management practices to enhance soil organic carbon (SOC) sequestration. The dynamics of straw C transformation in soils have been widely studied, however, it is less clear how crop planting regulates the incorporation of added straw C into SOC pools via soil - microbial nutrients status. We designed two sub- treatments, including single application of 13C-labeled straw (S) and its combination with crop planting (SR) in each fertilization treatment, and then conducted a field micro- experiment for 510 days. Regardless of fertilization, the SR treatments increased the content of straw derived mineral associated organic C (13C-MAOC) by 53.19 % and that of straw- derived particulate organic C (13C-POC) by 27.45 % compared with S treatments on the 510th day. And the SR treatments averagely increased the contribution percentage of straw-derived C in total MAOC by 39.44 %, especially under NP soil. Structure equation modeling results indicated crop planting promotes the formation of straw-derived SOC by reducing soil nutrients (r = −0.141, P < 0.05) and soil nutrients stoichiometry (r = −0.232, P < 0.01); fertilization alleviates nutrient limitations by reducing soil nutrients stoichiometry (r = −0.432, P < 0.001), microbial biomass stoichiometry (r = −0.701, P < 0.001), and increasing soil nutrients (r = 0.584, P < 0.001), thereby regulating the formation of straw C. Our results imply that crop planting contributes long-term incorporation of straw C to stable SOC pool via optimizing nutrients within soil-microbial system.
秸秆还田是加强土壤有机碳固存的一种可持续管理措施。秸秆C在土壤中的转化动力学已经得到了广泛的研究,然而,作物种植如何通过土壤微生物养分状态调节添加的秸秆C进入有机碳库的机制尚不清楚。设计了两个亚处理,分别在每个施肥处理中单独施用13c标记秸秆(S)和与作物种植(SR)相结合,并进行了510 d的田间微试验。在不施肥的情况下,与S处理相比,SR处理第510天秸秆源矿物伴生有机C (13C-MAOC)含量提高了53.19 %,秸秆源颗粒有机C (13C-POC)含量提高了27.45 %。SR处理使秸秆源C对总MAOC的贡献率平均提高了39.44 %,特别是NP土壤下。结构方程建模结果表明,作物种植通过降低土壤养分(r = −0.141,P <; 0.05)和土壤养分化学计量(r = −0.232,P <; 0.01)促进秸秆源有机碳的形成;受精减轻营养限制通过减少土壤养分化学计量学(r = −0.432,P & lt; 0.001),微生物生物量化学计量学(r = −0.701,P & lt; 0.001),并增加土壤养分(r = 0.584,P & lt; 0.001),从而调节的形成秸秆C。我们的研究结果表明,作物种植长期秸秆C整合有助于稳定SOC池通过优化养分在土壤微生物系统。
{"title":"Crop planting promotes the stabilization of straw-derived carbon in fertilized soil by regulating soil stoichiometry","authors":"Tengxiao Zhu ,&nbsp;Xiuwen Mei ,&nbsp;Yuping Li ,&nbsp;Shuangyi Li ,&nbsp;Tingting An ,&nbsp;Jingkuan Wang","doi":"10.1016/j.still.2025.107008","DOIUrl":"10.1016/j.still.2025.107008","url":null,"abstract":"<div><div>Straw returning to cropland is a sustainable management practices to enhance soil organic carbon (SOC) sequestration. The dynamics of straw C transformation in soils have been widely studied, however, it is less clear how crop planting regulates the incorporation of added straw C into SOC pools via soil - microbial nutrients status. We designed two sub- treatments, including single application of <sup>13</sup>C-labeled straw (S) and its combination with crop planting (SR) in each fertilization treatment, and then conducted a field micro- experiment for 510 days. Regardless of fertilization, the SR treatments increased the content of straw derived mineral associated organic C (<sup>13</sup>C-MAOC) by 53.19 % and that of straw- derived particulate organic C (<sup>13</sup>C-POC) by 27.45 % compared with S treatments on the 510th day. And the SR treatments averagely increased the contribution percentage of straw-derived C in total MAOC by 39.44 %, especially under NP soil. Structure equation modeling results indicated crop planting promotes the formation of straw-derived SOC by reducing soil nutrients (<em>r</em> = −0.141, <em>P</em> &lt; 0.05) and soil nutrients stoichiometry (<em>r</em> = −0.232, <em>P</em> &lt; 0.01); fertilization alleviates nutrient limitations by reducing soil nutrients stoichiometry (<em>r</em> = −0.432, <em>P</em> &lt; 0.001), microbial biomass stoichiometry (<em>r</em> = −0.701, <em>P</em> &lt; 0.001), and increasing soil nutrients (<em>r</em> = 0.584, <em>P</em> &lt; 0.001), thereby regulating the formation of straw C. Our results imply that crop planting contributes long-term incorporation of straw C to stable SOC pool via optimizing nutrients within soil-microbial system.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"258 ","pages":"Article 107008"},"PeriodicalIF":6.8,"publicationDate":"2025-12-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145731635","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Strategic deep tillage of deep sand soils impacts the sorption and biological availability of trifluralin 深砂土壤策略性深耕对氟乐灵的吸收和生物有效性有影响
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-12-06 DOI: 10.1016/j.still.2025.106997
Tom J. Edwards , Stephen L. Davies , Ron J. Yates , Michael T. Rose , Benedict Arthur , John G. Howieson , Graham O’Hara , Emma J. Steel , David JM Hall
Deep sand soils are inherently fragile with surface layers that are very low in organic matter and clay. Previous studies demonstrate that strategic deep tillage such as soil inversion and deep soil mixing can increase crop production on these soils in Southern Australia. However, the majority of the organic matter and nutrients are concentrated in the top organically stained layer and deep tillage incorporates 50–60 % of the organic layer into the subsoil below 200 mm. The physical composition of the soil (percentage of sand, silt, clay and organic matter) and the chemical properties of the soil (pH, nutrient levels, cation exchange capacity) can strongly influence the soil adsorption of trifluralin. Modest levels of organic matter and clay particles in the topsoil particularly following deep tillage equate to the scant attenuation of herbicides on sandy textured soils. Soil samples (0–100 mm) were collected from three experimental sites; two Arenic Solonetz soils near Esperance and one Arenic Arenosol soil near Geraldton in Western Australia. At all three sites, three experimental treatments were sampled; control (no tillage), deep mixed with a spader to 350 mm and soil inversion with a mouldboard plough to 350 mm. Soil samples were taken on two growing seasons post tillage at Geraldton, three post tillage at Esperance TJM and twelve post tillage at Esperance E1. Tillage reduced the measured soil-liquid partition coefficient (Kd) of trifluralin (p ≤ 0.05) at all three experimental sites. A greenhouse bioassay was developed to determine if soil changes from strategic tillage at one of the Esperance sites and the Geraldton site could be directly related to herbicide bioavailability at two of the experimental sites. Intact cores were used to maintain integrity of the field soils. Cores from both field sites demonstrated that soil inversion reduced the effective dose of trifluralin (p ≤ 0.01) for the bioassay species Lens culinaris. Together these experiments illustrate that strategic deep tillage can increase the bioavailability of trifluralin. These findings offer a valuable insight into the soil behaviour of trifluralin and can help farmers estimate the risk of phytotoxicity based on measurable soil characteristics.
深层沙质土壤本身就很脆弱,表层有机质和粘土含量很低。先前的研究表明,在南澳大利亚州,土壤翻转和深层土壤混合等战略性深度耕作可以增加这些土壤的作物产量。然而,大部分有机质和营养物质集中在表层有机染色层,深耕将50 - 60% %的有机层带入200 mm以下的底土。土壤的物理组成(砂、粉、粘土和有机质的百分比)和土壤的化学性质(pH值、养分水平、阳离子交换能力)会强烈影响土壤对氟乐灵的吸附。表层土壤中有机质和粘土颗粒含量适中,特别是深耕后,相当于沙质土壤中除草剂的衰减不足。土壤样品(0-100 mm)采集于3个试验点;在西澳大利亚的埃斯佩兰斯附近有两个Arenic Solonetz土壤,在杰拉尔顿附近有一个Arenic arennosol土壤。在所有三个地点,采样了三种实验处理;对照(免耕),用锄头深拌至350 毫米,用板犁翻耕至350 毫米。在Geraldton进行2个生长季的耕作后,在Esperance TJM进行3个耕作后,在Esperance E1进行12个耕作后取样。在三个试验点,耕作降低了三氟乐灵的土液分配系数(Kd) (p ≤ 0.05)。开发了一种温室生物测定法,以确定埃斯佩兰斯和杰拉尔顿两个试验点的策略性耕作导致的土壤变化是否与除草剂的生物有效性直接相关。使用完整的岩心来保持现场土壤的完整性。两个试验点的岩心数据表明,土壤反演降低了氟乐灵对生物测定物种蓝蝇(Lens culinaris)的有效剂量(p ≤ 0.01)。综上所述,这些试验说明策略性深耕可以提高氟乐灵的生物利用度。这些发现对氟乐灵的土壤行为提供了有价值的见解,并可以帮助农民根据可测量的土壤特征估计植物毒性的风险。
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Soil & Tillage Research
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