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Divergent accumulation of particulate and mineral-associated organic carbon driven by intercropping duration in apple orchards 间作期驱动苹果园颗粒和矿物相关有机碳的发散性积累
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-14 DOI: 10.1016/j.still.2026.107128
Rongqin Zhang , Xiaomeng Wei , Ming Li , Huike Li , Xining Zhao , Zhilong Duan , Hua Gao , Xiaolin Song
Particulate organic carbon (POC) and mineral-associated organic carbon (MAOC) are critical to soil organic carbon (SOC) accumulation and stabilization, yet their responses to intercropping duration and underlying microbial drivers remain poorly understood. Using a long-term apple orchard experiment on the Loess Plateau, this study evaluated white clover intercropping of 8 years (8-yr) and 16 years (16-yr) on POC and MAOC contents across the 0–60 cm soil profile, and examined accumulation mechanisms through microbial life-history strategies, enzyme activities, and microbial carbon pump efficiency. The results demonstrate that MAOC (66–90 %) accounted for a larger proportion of SOC than POC (10–34 %). In the 0–20 cm soil layer, MAOC primarily drove SOC increases induced by intercropping. In deeper soil layers, 8-yr increased POC in the 20–40 and 40–60 cm but did not alter MAOC, whereas 16 yr increased MAOC by 62 % and 34 %, respectively. Intercropping increased microbial necromass carbon (MNC), but the extent varied with intercropping duration and soil depth. Specifically, 8-yr increased both bacterial and fungal necromass (BNC and FNC) in the 0–40 cm soil layer. In contrast, 16-yr enhanced MNC across the entire 0–60 cm profile and notably promoted the accumulation of BNC in 40–60 cm soil layers. Random forest and path modeling indicated stronger links of microbial necromass and resource-acquisitive traits to MAOC than POC. These findings reveal duration-dependent shifts in SOC fraction dynamics regulated by microbial life-history strategies and MCP efficiency. Our work provides a mechanistic basis for optimizing intercropping duration to enhance SOC sequestration in intercropping systems.
颗粒有机碳(POC)和矿物相关有机碳(MAOC)对土壤有机碳(SOC)的积累和稳定至关重要,但它们对间作时间和潜在微生物驱动因素的响应尚不清楚。本研究利用黄土高原苹果园长期试验,评价了白三叶草间作8年(8年)和16年(16年)对0 ~ 60 cm土壤剖面POC和MAOC含量的影响,并通过微生物生活史策略、酶活性和微生物碳泵效率研究了土壤POC和MAOC的积累机制。结果表明,有机碳中mac(66-90 %)的比例大于POC(10-34 %)。在0 ~ 20 cm土层,MAOC主要驱动间作土壤有机碳的增加。在较深的土层中,8年处理增加了20-40和40-60 cm的POC,但未改变MAOC,而16 年处理使MAOC分别增加了62 %和34 %。间作增加了微生物坏死体碳(MNC),但其增加程度随间作年限和土壤深度的不同而不同。具体来说,8年在0-40 cm土层中细菌和真菌坏死块(BNC和FNC)均增加。相反,16年在0-60 cm剖面上增加了MNC,并显著促进了40-60 cm土层的BNC积累。随机森林和路径模型表明,微生物坏死块和资源获取性状与MAOC的关系强于POC。这些发现揭示了微生物生活史策略和MCP效率对有机碳分数动态变化的持续依赖。本研究为优化间作年限以提高间作系统有机碳固存提供了机制依据。
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引用次数: 0
Unraveling mechanistic insights into soil nitrogen transformation processes for improving NUE in paddy rice systems 揭示提高水稻系统氮素利用效率的土壤氮素转化过程的机理
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-09 DOI: 10.1016/j.still.2026.107104
Shending Chen , Ahmed S. Elrys , Qiaodong Chi , Wenyan Yang , Lei Meng , Zucong Cai , Jinbo Zhang , Baojing Gu , Christoph Müller
Rice generally exhibits lower nitrogen use efficiency (NUE) than other crops, yet the nitrogen (N) process-level mechanisms underlying regional variation remain unclear. Here, we conducted a multi-scale investigation combining laboratory soil incubations, pot experiments with 15N tracings, and field trials across 50 soil samples from China’s rice fields. We quantified soil N transformation rates, evaluated pot-based NUE, and tested N management strategies in two paddy sites with contrasting soils. Results revealed substantial regional differences in gross N transformations, including mineralization, nitrification, and ammonium immobilization, with northern soils exhibiting longer mean retention times of ammonium (average 19.5 days) than southern soils (average 5.4 days). Ammonium retention time was more closely associated with NUE than temperature, precipitation, or nitrification rates. Field trials confirmed that ammonium-stabilizing treatments, particularly combined nitrification and urease inhibitors, improved both yield and NUE in alkaline soils. These findings provide a mechanistic basis for region-specific N management to enhance rice productivity while reducing environmental losses.
水稻氮素利用效率(NUE)普遍低于其他作物,但区域差异背后的氮素过程水平机制尚不清楚。在这里,我们进行了多尺度的调查,结合实验室土壤培养、盆栽15N示踪和田间试验,从中国稻田的50个土壤样品。我们量化了土壤氮素转化率,评估了基于盆栽的氮素利用效率,并在两个不同土壤的水稻基地测试了氮素管理策略。结果显示,总氮转化(包括矿化、硝化和铵固定化)存在显著的区域差异,北方土壤铵的平均滞留时间(平均19.5天)比南方土壤(平均5.4天)更长。与温度、降水或硝化速率相比,铵态氮滞留时间与氮肥利用率的关系更为密切。田间试验证实,氨稳定处理,特别是联合硝化和脲酶抑制剂,提高了碱性土壤的产量和氮肥利用效率。这些发现为区域氮管理提供了机制基础,以提高水稻生产力,同时减少环境损失。
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引用次数: 0
Tracing the source of organic carbon in particulate and mineral-associated soil fractions in response to tillage and nitrogen fertilization intensities 追踪土壤颗粒和矿物相关组分中有机碳的来源对耕作和氮肥强度的响应
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-09 DOI: 10.1016/j.still.2026.107113
Hem C. Sharma , Wei Ren , Laura E. Lindsey , Hanna Poffenbarger , Pierre-Andre Jacinthe
While tillage management and nitrogen (N) fertilization can affect soil organic carbon (SOC) status, information is limited regarding the combined effect of these practices on SOC distribution between the labile particulate organic matter (POM) and the stable mineral-associated organic matter (MAOM) soil fractions. Given that low tillage intensity favors SOC protection and N fertilization increases crop residue input into soil systems, it was hypothesized that long-term no-till (NT) (compared to moldboard plow, MB) and high rate of N fertilization would enhance SOC stability by promoting the conversion of POM into stable MAOM. To test that hypothesis, surface (0–5 cm) and subsurface (15–30 cm) soil samples were collected from research plots (Kentucky, USA) under continuous corn (Zea mays L.) for 52 years, managed with either NT or MB, and receiving N fertilizer at 0, 84 or 168 kg N ha−1 y−1. Soil samples were fractionated using sonication and sieving (POM: >20 μm; MAOM <20 μm), and the amount of corn-derived C in each fraction was quantified using ¹ ³C natural abundance. Results showed that, in the surface soil layer, NT (compared to MB) enhanced total C and corn-derived C in both the POM and MAOM fractions whereas N application only impacted the MAOM fraction. Further, in the NT surface soil layer, the soil microbial biomass carbon (MBC), and the fungal-to-bacterial ratios were all higher than under MB. These, along with a strong relationship between MBC and MAOM, indicated greater retention of corn residue C as microbial by-products in MAOM under NT than MB. In the subsurface layer, the MAOM was also higher under NT than under MB (despite similar POM level), suggesting that leaching of dissolved organic C and subsequent formation of organo-mineral complexes at depth could be the underlying mechanism. Overall, NT positively impacted both the labile POM and the stable MAOM soil fractions, underscoring its contribution to soil health and SOC sequestration in agroecosystems.
虽然耕作管理和氮肥施用可以影响土壤有机碳(SOC)状态,但这些措施对土壤中稳定颗粒有机质(POM)和稳定矿物伴生有机质(MAOM)土壤组分之间有机碳分布的综合影响信息有限。考虑到低耕作强度有利于有机碳保护,而施氮增加了作物残茬对土壤系统的输入,我们假设长期免耕(NT)(相对于犁耕,MB)和高施氮量可以通过促进POM向稳定的MAOM转化来增强有机碳稳定性。为了验证这一假设,在美国肯塔基州的研究地块上,连续种植玉米(Zea mays L.) 52年,采用NT或MB管理,施氮量分别为0、84或168 kg N ha - 1 y - 1,收集表层(0 - 5 cm)和地下(15-30 cm)土壤样品。土壤样品采用超声波和筛分(POM: >20 μm; MAOM <20 μm)进行分选,每个分选组分中玉米衍生的碳含量采用¹ ³C自然丰度进行定量。结果表明,在表层土壤中,施用氮肥(与施用MB相比)提高了POM和MAOM组分的总C和玉米源C,而施用氮肥仅影响MAOM组分。此外,在NT表层,土壤微生物生物量碳(MBC)和真菌细菌比均高于MB,且MBC与MAOM之间存在较强的关系,表明NT下MAOM中玉米残碳作为微生物副产物的保留率高于MB。在亚表层,尽管POM水平相似,但NT下MAOM也高于MB。这表明溶解有机碳的浸出和随后在深部形成的有机矿物复合体可能是潜在的机制。总体而言,NT对土壤中稳定POM和稳定MAOM组分均有正向影响,表明NT对土壤健康和有机碳固存的贡献。
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引用次数: 0
Functional differentiation of cover crops in the long-term no-tillage vegetable system 长期免耕蔬菜体系覆盖作物的功能分化
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-05 DOI: 10.1016/j.still.2026.107102
Lucas Raimundo Rauber , Leonardo Khaoê Giovanetti , Carolina Oliveira De Alcântara , Pedro de Mello Holme , Cledimar Rogério Lourenzi , Claudinei Kurtz , Jucinei José Comin , Arcângelo Loss
Conservation Agriculture for vegetable production, which is designated as No-Tillage Vegetable System (NTVS) in southern Brazil, sustainably improves food production through the strategic arrangement of cover crops (CCs) in crop rotation. However, the functional differentiation of CCs arrangements needs further understanding in NTVS. This study investigated the functional differentiation of CCs combinations in an NTVS in southern Brazil. The experiment was conducted on a Humic Dystrudept soil in southern Brazil. Treatments included: T1 — fallow in fall/winter (weeds, mainly Galinsoga parviflora) followed by onion (Allium cepa L.) and then corn (Zea mays) (F/Oni/C); T2 — turnip forage (Raphanus sativus L.) in fall/winter followed by onion and then millet (Pennisetum glaucum) (T/Oni/M); T3 — mix of oats (Avena strigosa) and turnip forage in fall/winter, followed by onion and then beans (Phaseolus vulgaris) (O+T/Oni/B); and T4 — oats in fall/winter followed by onion and then soybean (Glycine max) (O/Oni/S). From 2024–2025, after 16 years of long-term experiment that has been carrying out, the following traits were evaluated: soil penetration resistance (PR) (0–50 cm); aggregate stability (0–10 cm); water infiltration into the soil (using concentric double ring); carbon (C) and nitrogen (N) contents (0–10 cm); β-glucosidase enzyme activity and glomalin fractions (0–10 cm); qualitative indices of soil structure and health; and biomass production by CCs. The onion yield data from 2019 to 2024 was also added to the database. The system with the greatest diversity of CCs (O+T/Oni/B) showed the highest water infiltration. The T/Oni/M treatment promoted greater enzymatic activity and lower PR (0–15 cm). Treatments with summer grasses (T/Oni/M; F/Oni/C) resulted in higher biomass production and improved qualitative indexes of soil health, while those with summer legumes (O+T/Oni/B; O/Oni/S) increased onion yield. Aggregate stability, C and N content, and glomalin levels in the soil were high across treatments but had no significant differences. In conclusion, each CC system provides specific benefits to the soil. These findings demonstrate the high degree of functional differentiation of CCs in organic NTVS, allowing management to be tailored to goals (e.g., biomass production, biological activity, water infiltration, or crop yield). The diversity of species, the quantity and type of biomass, and seasonality influence the physical and biological properties of the soil and the functional differentiation between CCs in a long-term organic NTVS. Qualitative indicators of soil health complement quantitative indicators and broaden the functional differentiation of CC arrangements, guiding the regenerative management of soil health.
蔬菜生产的保护性农业,在巴西南部被指定为免耕蔬菜系统(NTVS),通过在作物轮作中战略性地安排覆盖作物(CCs),可持续地提高粮食生产。然而,在ntv中,CCs安排的功能分化需要进一步了解。本研究调查了巴西南部NTVS中CCs组合的功能分化。该试验是在巴西南部腐殖质破坏土壤上进行的。处理包括:T1 -秋冬休耕(杂草,主要是小花椒),其次是洋葱(Allium cepa L.)和玉米(Zea mays) (F/Oni/C);T2 -秋/冬季萝卜饲料(Raphanus sativus L.),其次是洋葱,最后是谷子(Pennisetum glaucum) (T/Oni/M);T3 -秋/冬季燕麦(Avena strigosa)和萝卜混合,然后是洋葱,然后是豆类(Phaseolus vulgaris) (O+T/Oni/B);秋冬季节T4 -燕麦次之,洋葱次之,大豆次之(甘氨酸max) (O/Oni/S)。从2024年到2025年,经过16年的长期试验,评估了以下性状:土壤抗渗透能力(PR)(0-50 cm);总体稳定性(0-10 cm);水渗入土壤(采用同心圆双环);碳(C)和氮(N)含量(0-10 cm);β-葡萄糖苷酶活性和球球蛋白含量(0-10 cm);土壤结构与健康定性指标;和通过CCs生产生物质。2019年至2024年的洋葱产量数据也被添加到数据库中。CCs (O+T/Oni/B)多样性最大的系统,水分入渗最高。T/Oni/M处理提高了酶活性,降低了PR(0-15 cm)。夏草(T/Oni/M; F/Oni/C)处理提高了生物量产量,改善了土壤健康定性指标,而夏豆科(O+T/Oni/B; O/Oni/S)处理提高了洋葱产量。土壤团聚体稳定性、C、N含量和球囊素水平在不同处理间均较高,但差异不显著。总之,每个CC系统对土壤都有特定的好处。这些发现表明,有机ntv中的CCs具有高度的功能分化,可以根据目标(如生物量生产、生物活性、水分渗透或作物产量)进行管理。物种多样性、生物量的数量和类型以及季节性影响着长期有机NTVS土壤的物理和生物特性以及cc之间的功能分化。土壤健康的定性指标是对定量指标的补充,拓宽了CC安排的功能分化,指导土壤健康的再生管理。
{"title":"Functional differentiation of cover crops in the long-term no-tillage vegetable system","authors":"Lucas Raimundo Rauber ,&nbsp;Leonardo Khaoê Giovanetti ,&nbsp;Carolina Oliveira De Alcântara ,&nbsp;Pedro de Mello Holme ,&nbsp;Cledimar Rogério Lourenzi ,&nbsp;Claudinei Kurtz ,&nbsp;Jucinei José Comin ,&nbsp;Arcângelo Loss","doi":"10.1016/j.still.2026.107102","DOIUrl":"10.1016/j.still.2026.107102","url":null,"abstract":"<div><div>Conservation Agriculture for vegetable production, which is designated as No-Tillage Vegetable System (NTVS) in southern Brazil, sustainably improves food production through the strategic arrangement of cover crops (CCs) in crop rotation. However, the functional differentiation of CCs arrangements needs further understanding in NTVS. This study investigated the functional differentiation of CCs combinations in an NTVS in southern Brazil. The experiment was conducted on a Humic Dystrudept soil in southern Brazil. Treatments included: T1 — fallow in fall/winter (weeds, mainly <em>Galinsoga parviflora</em>) followed by onion (<em>Allium cepa</em> L.) and then corn (<em>Zea mays</em>) (F/Oni/C); T2 — turnip forage (<em>Raphanus sativus</em> L.) in fall/winter followed by onion and then millet (<em>Pennisetum glaucum</em>) (T/Oni/M); T3 — mix of oats (<em>Avena strigosa</em>) and turnip forage in fall/winter, followed by onion and then beans (<em>Phaseolus vulgaris</em>) (O+T/Oni/B); and T4 — oats in fall/winter followed by onion and then soybean (<em>Glycine max</em>) (O/Oni/S). From 2024–2025, after 16 years of long-term experiment that has been carrying out, the following traits were evaluated: soil penetration resistance (PR) (0–50 cm); aggregate stability (0–10 cm); water infiltration into the soil (using concentric double ring); carbon (C) and nitrogen (N) contents (0–10 cm); β-glucosidase enzyme activity and glomalin fractions (0–10 cm); qualitative indices of soil structure and health; and biomass production by CCs. The onion yield data from 2019 to 2024 was also added to the database. The system with the greatest diversity of CCs (O+T/Oni/B) showed the highest water infiltration. The T/Oni/M treatment promoted greater enzymatic activity and lower PR (0–15 cm). Treatments with summer grasses (T/Oni/M; F/Oni/C) resulted in higher biomass production and improved qualitative indexes of soil health, while those with summer legumes (O+T/Oni/B; O/Oni/S) increased onion yield. Aggregate stability, C and N content, and glomalin levels in the soil were high across treatments but had no significant differences. In conclusion, each CC system provides specific benefits to the soil. These findings demonstrate the high degree of functional differentiation of CCs in organic NTVS, allowing management to be tailored to goals (e.g., biomass production, biological activity, water infiltration, or crop yield). The diversity of species, the quantity and type of biomass, and seasonality influence the physical and biological properties of the soil and the functional differentiation between CCs in a long-term organic NTVS. Qualitative indicators of soil health complement quantitative indicators and broaden the functional differentiation of CC arrangements, guiding the regenerative management of soil health.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"260 ","pages":"Article 107102"},"PeriodicalIF":6.8,"publicationDate":"2026-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146134160","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
Electron transfer coupling with biogenic elements conversion in farmland soil: A review 农田土壤中电子传递耦合与生物源元素转化研究进展
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-08-01 Epub Date: 2026-02-09 DOI: 10.1016/j.still.2026.107112
Sihan Zhao , Guang Yang , Yuewei Yang , Xin Yu , Jialu Sun , Xiaolin Zhang , Pinpin Yang , Xiaodong Zhao , Xiaojing Li
Farmland soil is a complex system involving the conversion of multiple biogenic elements, which plays a key role in maintaining soil ecological balance. Extracellular electron transfer (EET) is an essential driving force for material circulation and energy exchange. Thus, it affects the biogeochemical processes and cycles of soil elements, including mineral formation and evolution, nutrient cycling and even the removal of pollutants and the improvement of cultivated land quality. This review summarizes the progress of research on electron transfer in farmland soil. It provides an overview of electroactive microorganisms, electron transfer modes, and their coupled conversion with carbon, nitrogen, sulfur, and iron elements. Afterwards, future research directions are expected, including an in-depth exploration of electron transfer mechanisms, optimization of electron transfer pathways, and improvement of biogenic element conversion. This review puts forward a new way to regulate the biotransformation of elements and provides support for improving the fertility of farmland soil and promoting the sustainable development of agriculture.
农田土壤是一个涉及多种生物源元素转化的复杂系统,对维持土壤生态平衡起着关键作用。细胞外电子传递(EET)是物质循环和能量交换的重要驱动力。因此,它影响土壤元素的生物地球化学过程和循环,包括矿物的形成和演化,养分的循环,甚至污染物的去除和耕地质量的提高。本文综述了农田土壤中电子转移的研究进展。它提供了电活性微生物的概述,电子传递模式,以及它们与碳,氮,硫和铁元素的耦合转换。随后,展望了未来的研究方向,包括深入探索电子传递机制,优化电子传递途径,提高生物源元素转化。为调控农田土壤中元素的生物转化提供了新的途径,为提高农田土壤肥力,促进农业可持续发展提供了支持。
{"title":"Electron transfer coupling with biogenic elements conversion in farmland soil: A review","authors":"Sihan Zhao ,&nbsp;Guang Yang ,&nbsp;Yuewei Yang ,&nbsp;Xin Yu ,&nbsp;Jialu Sun ,&nbsp;Xiaolin Zhang ,&nbsp;Pinpin Yang ,&nbsp;Xiaodong Zhao ,&nbsp;Xiaojing Li","doi":"10.1016/j.still.2026.107112","DOIUrl":"10.1016/j.still.2026.107112","url":null,"abstract":"<div><div>Farmland soil is a complex system involving the conversion of multiple biogenic elements, which plays a key role in maintaining soil ecological balance. Extracellular electron transfer (EET) is an essential driving force for material circulation and energy exchange. Thus, it affects the biogeochemical processes and cycles of soil elements, including mineral formation and evolution, nutrient cycling and even the removal of pollutants and the improvement of cultivated land quality. This review summarizes the progress of research on electron transfer in farmland soil. It provides an overview of electroactive microorganisms, electron transfer modes, and their coupled conversion with carbon, nitrogen, sulfur, and iron elements. Afterwards, future research directions are expected, including an in-depth exploration of electron transfer mechanisms, optimization of electron transfer pathways, and improvement of biogenic element conversion. This review puts forward a new way to regulate the biotransformation of elements and provides support for improving the fertility of farmland soil and promoting the sustainable development of agriculture.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"260 ","pages":"Article 107112"},"PeriodicalIF":6.8,"publicationDate":"2026-08-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"146146687","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
Broadcasting cover crops at corn harvest can maximize biomass and reduce nitrogen leaching 玉米收获期撒播覆盖作物可使生物量最大化,减少氮淋失
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-07-01 Epub Date: 2026-01-20 DOI: 10.1016/j.still.2026.107064
Mary Michael Lipford Zahed , Joseph R. Haymaker , Joshua Mott , A. Ozzie Abaye , Mark S. Reiter
Mitigating nitrogen (N) leaching from agricultural fields is critical for improving water quality in the Chesapeake Bay Watershed. Because N mineralization continues after corn (Zea mays L.) uptake ceases, losses may occur between harvest and cover crop (CC) establishment. The objectives of this study were to identify effective establishment methods and CC species for N uptake and biomass production; determine whether planting at harvest enhances N scavenging compared to delayed planting; and assess impacts on corn yield. Four seeding methods were evaluated: (1) broadcasting with incorporation at corn harvest, (2) broadcasting without incorporation at corn harvest, (3) broadcasting with incorporation four weeks post-harvest, and (4) drilling four weeks post-harvest, using cereal rye (Secale cereale L.), hairy vetch (Vicia villosa Roth), rapeseed (Brassica napus L.), and a three-species mix. In Year 2, fall soil nitrate concentrations at 0–15 cm depth in post-harvest treatments (11.4–11.8 mg kg−1) were more than double that of at-harvest treatments (5.2 mg kg−1), with at-harvest incorporated rye showing the lowest winter nitrate (1.7 mg kg−1). At-harvest mix and hairy vetch accumulated the most N in aboveground biomass (181–208 kg ha−1). Year 1 corn yield increased following at-harvest hairy vetch (11,022–11,384 kg ha−1) and incorporated mix (11,587 kg ha−1) compared to the control (8895 kg ha−1), though not in Year 2. Incorporation did not significantly affect outcomes compared to non-incorporated treatments. Planting CCs at corn harvest maximized N accumulation, biomass, and nitrate reduction, offering a practical strategy to mitigate N leaching.
减少农田氮淋失对改善切萨皮克湾流域水质至关重要。由于氮矿化在玉米(Zea mays L.)吸收停止后仍在继续,因此在收获和覆盖作物(CC)建立之间可能发生损失。本研究的目的是确定氮素吸收和生物量生产的有效建立方法和CC物种;确定收获期播种是否比延迟播种更能提高氮的清除能力;并评估对玉米产量的影响。对四种播种方法进行了评价:(1)玉米收获时撒播混播,(2)玉米收获时不撒播,(3)收获后四周撒播混播,(4)收获后四周打孔,使用谷物黑麦(Secale cereale L.)、毛豌豆(Vicia villosa Roth)、油菜籽(Brassica napus L.)和三种混合物。在第二年,收获后处理0-15 cm深度的秋季土壤硝酸盐浓度(11.4-11.8 mg kg - 1)是收获时处理(5.2 mg kg - 1)的两倍多,收获时掺入黑麦的冬季硝酸盐最低(1.7 mg kg - 1)。收获期混交种和毛缕野豌豆积累的地上生物量氮最多(181 ~ 208 kg ha−1)。与对照(8895 kg ha - 1)相比,收获叶紫薇(11,022-11,384 kg ha - 1)和掺入混合物(11,587 kg ha - 1)后,第一年玉米产量增加,但第二年没有增加。与非合并治疗相比,合并治疗对结果没有显著影响。在玉米收获时种植碳捕集剂可使氮积累、生物量和硝酸盐减少最大化,为缓解氮淋失提供了切实可行的策略。
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引用次数: 0
Combining tillage and nitrogen practices to optimize soil nitrogen dynamics and wheat yield across various soil textures, using RZWQM2 以RZWQM2为研究对象,采用耕作与施氮相结合的方法优化不同质地土壤氮素动态和小麦产量
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-07-01 Epub Date: 2026-01-29 DOI: 10.1016/j.still.2026.107093
Saadi Sattar Shahadha, Mawj R. Al-Hamdany
The optimal combination of tillage and nitrogen practices could be an effective strategy for improving crop yields and mitigating soil nitrogen loss. This study aimed to identify the optimal combination of field management practices for controlling soil nitrogen distribution and enhancing wheat yield across various soil textures in the semi-arid region of Iraq, using agricultural modeling. The Root Zone Water Quality Model (RZWQM2) was calibrated and validated using experimental field data from the 2023 and 2024 wheat-growing seasons. Various modeling scenarios were then created to evaluate and determine the optimal combination of tillage practices (deep tillage and shallow tillage) with nitrogen fertilization rates (100 and 250 kg N/ha) for sandy clay and silty clay soils. The model was successfully calibrated and validated with an accepted range of statistical indicators. Simulation results indicated that both soil textures presented comparable responses to all management practices. Simulation results indicated that, deep tillage practice reduced soil nitrate leaching and N2O emissions by an average of 0.04 μg/cm2 and 0.27 kg/ha, respectively, while increasing nitrate retention in the soil profile and wheat production by an average of 0.05 and 0.03 kg/ha, respectively, compared to shallow tillage. Applying 250 kg N/ha increased soil nitrate flux and N2O emissions, particularly when combined with shallow tillage. Therefore, combining deep tillage with nitrogen application rates is the optimal field management approach and is suggested for both soil textures, as it minimizes soil nitrogen loss and enhances wheat productivity.
耕作与施氮的最佳组合可能是提高作物产量和减轻土壤氮流失的有效策略。本研究旨在利用农业模型,确定控制伊拉克半干旱区不同土壤质地土壤氮素分布和提高小麦产量的最佳田间管理措施组合。利用2023年和2024年小麦生长季的试验田数据对根区水质模型(RZWQM2)进行了标定和验证。然后创建各种模拟情景,以评估和确定砂质粘土和粉质粘土土壤的最佳耕作方式(深耕和浅耕)和施氮量(100和250 kg N/ha)的组合。该模型被成功地校准和验证了一个可接受的统计指标范围。模拟结果表明,两种土壤质地对所有管理措施的响应都具有可比性。模拟结果表明,与浅耕相比,深耕使土壤硝态氮淋溶和N2O排放分别平均减少0.04 μg/cm2和0.27 kg/ha,土壤剖面硝态氮滞留和小麦产量分别平均增加0.05和0.03 kg/ha。施用250 kg N/ha增加了土壤硝酸盐通量和N2O排放,特别是与浅耕结合使用时。因此,深耕与施氮量相结合是最佳的田间管理方法,适用于两种土壤质地,可最大限度地减少土壤氮素流失,提高小麦产量。
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引用次数: 0
Straw return modulates surface energy balance and soil hydrothermal dynamics during freeze-thaw period 秸秆还田调节冻融期地表能量平衡和土壤热液动态
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-07-01 Epub Date: 2026-01-26 DOI: 10.1016/j.still.2026.107083
Wanning Wang , Hexiang Zheng , Xingwang Wang , Delong Tian , Qian Wang , Zailin Huo
Straw return modifies topsoil properties that are crucial for understanding soil-atmosphere interactions and their impact on soil hydrothermal conditions in seasonally frozen areas. However, the effects of uniformly returning crushed straw (3–5 cm in length at 1.6–1.8 kg·m−2) on the surface energy balance (SEB) and soil water-heat dynamics during the freeze-thaw period remain inadequately quantified. We conducted a two-year field experiment in a cold-arid region of Northwest China, employing a Bowen ratio energy balance system (BREBS) to monitor SEB components (Rn, Gs, H, LE), alongside soil temperature and moisture. Results demonstrated that straw return (ST) obviously altered SEB components during freeze-thaw periods. Specifically, over the two-year period, seasonal variations showed that ST reduced Rn by 8.6–9.1 W·m−2 relative to NT, decreased Gs by 0.24 W·m−2, lowered LE by 49 %, while increased the Bowen ratio by 48 % and H. During the thawing period, diurnal variations showed LE decreasing by 36 % and H increasing by 11 % under ST compared to NT. Furthermore, ST delayed topsoil thawing by 3–7 days, increased unfrozen water content (UWC) by 2.9–4.3 %, reduced freezing depth, and stabilized deep-layer soil temperature and moisture. These findings endorse straw return as a viable strategy for conserving soil moisture, mitigating frost damage, and optimizing spring sowing schedules in arid cold regions.’
秸秆还田改变了表层土壤的性质,这些性质对于了解季节性冻结地区土壤-大气相互作用及其对土壤热液条件的影响至关重要。然而,在冻融期,秸秆碎料(长度为3-5 cm,长度为1.6-1.8 kg·m−2)均匀回用对地表能量平衡(SEB)和土壤水热动态的影响仍未得到充分量化。在中国西北寒冷干旱区进行了为期两年的田间试验,采用博温比能量平衡系统(BREBS)监测土壤温度和湿度,同时监测土壤SEB组分(Rn、Gs、H、LE)。结果表明,秸秆还田明显改变了冻融期土壤SEB组分。2年的季节变化表明,与NT相比,ST降低了8.6 ~ 9.1 W·m−2,降低了0.24 W·m−2,降低了49 %,增加了48 %和H。在融化期间,日变化表明,与NT相比,ST下LE减少了36 %,H增加了11 %。此外,ST使表土融化延迟了3 ~ 7天,使未冻水含量(UWC)增加了2.9 ~ 4.3 %,降低了冻结深度。稳定了深层土壤的温度和湿度。这些发现支持秸秆还田是在干旱寒冷地区保持土壤水分、减轻霜冻损害和优化春播时间表的可行策略。”
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引用次数: 0
Temporal trajectory and determinants of permanent gully erosion in the grassland: A long-term analysis spanning 1973–2020 草地永久沟蚀的时间轨迹和决定因素:1973-2020年的长期分析
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-07-01 Epub Date: 2026-02-02 DOI: 10.1016/j.still.2026.107098
Zhicai Xiao , Mingming Guo , Xin Liu , Zhuoxin Chen , Xingyi Zhang , Jinzhong Xu , Shaoliang Zhang , Jielin Liu , Xing Han , Ruifeng Xie
Grassland ecosystems, particularly in cold and high-altitude regions, are highly vulnerable to gully erosion owing to their simple structure and environmental sensitivity, making it a severe form of grassland degradation. However, most previous studies have focused on agricultural systems, leaving limited understanding of the long-term evolution and drivers of permanent gullies in grasslands. To address this issue, we analyzed gully erosion dynamics and its determinants in a 103 km² area of the Hulunbuir grassland using remote sensing image from 1973, 1983, 2011, and 2020. Results showed that gully quantity, gully density and ground lacerative degree increased by 54.13 times, 286.66 times, and 591.01 times, respectively from 1973 to 2020, with the annual soil loss thickness of 0.023 mm. From 1973–2020, the average gully erosion rates in length, width, area, and volume were 4.64 m yr⁻¹ , 0.06 m yr⁻¹ , 17.17 m² yr⁻¹ , and 20.44 m³ yr⁻¹ , respectively. The merge of gullies (MG) showed greater linear gully erosion rate and areal gully erosion rate than newly formed gully (NFG) and continuously developing gully (CDG), while NFG showed the highest gully widening rates. Gully erosion rates in length, area and volume peaked at 4–5° slopes, with sunny and semi‑sunny aspects being more conducive to development, and linearly increased with gully drainage area. Cumulative gully growth length (ΔL), area (ΔA), and volume (ΔV) increased as a power relationship of cumulative climate indicators (Pre, R, R10, R95p, RX5day, SDII, Tem) and human activity intensity (grazing intensity, built up area, road density). The coupled effects of human activity with topography and climate exert the greatest influence on gully erosion, with the relative contribution of 37.13 % and 35.75 %, respectively. Overall, during 1973–2020, permanent gullies in the Hulunbuir grassland remained in the early lifecycle stage of development. However, intensifying anthropogenic pressures coupled with amplified climate variability progressively elevated erosion risks. This trajectory necessitates implementation of scientific gully control strategies to curb accelerated soil loss and establish sustainable human-land synergies.
草地生态系统结构简单,环境敏感性强,极易受到沟沟侵蚀的影响,是草地退化的一种严重形式,特别是在寒冷和高海拔地区。然而,大多数先前的研究都集中在农业系统上,对草原永久沟壑的长期演变和驱动因素的理解有限。为了解决这一问题,我们利用1973年、1983年、2011年和2020年的遥感图像,分析了呼伦贝尔草原103 km²区域的沟沟侵蚀动力学及其影响因素。结果表明:1973 ~ 2020年沟壑数量、沟壑密度和地面撕裂程度分别增加了54.13倍、286.66倍和591.01倍,年土壤流失厚度为0.023 mm;从1973年到2020年,冲沟侵蚀率平均长度、宽度、面积,和体积是4.64 m 年⁻¹ ,0.06 米 年⁻¹ ,17.17 m²年⁻¹ ,和20.44 m³ 年⁻¹ ,分别。合并沟(MG)比新形成的沟(NFG)和持续发展的沟(CDG)表现出更高的线状沟侵蚀率和面状沟侵蚀率,而NFG则表现出最高的沟壑拓宽率。沟壑侵蚀速率在长度、面积和体积上均在4-5°坡面处达到峰值,阳光和半阳光方向更有利于发育,并随沟壑流域面积线性增加。累积沟谷生长长度(ΔL)、面积(ΔA)和体积(ΔV)与累积气候指标(Pre、R、R10、R95p、RX5day、SDII、Tem)和人类活动强度(放牧强度、建成区面积、道路密度)呈幂函数关系。人类活动与地形和气候的耦合效应对沟蚀的影响最大,相对贡献率分别为37.13% %和35.75% %。总体而言,1973—2020年呼伦贝尔草原永久性沟渠仍处于早期生命周期发育阶段。然而,不断加剧的人为压力加上不断扩大的气候变率,逐渐增加了侵蚀风险。这一趋势要求实施科学的沟壑控制战略,以遏制加速的土壤流失,并建立可持续的人地协同效应。
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引用次数: 0
Threshold effects of resistant-layer thickness on gully development in the black soil region of Northeast China 东北黑土区抗层厚度对沟壑发育的阈值效应
IF 6.8 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2026-07-01 Epub Date: 2026-01-09 DOI: 10.1016/j.still.2026.107059
Lei Ma , Chunmei Wang , Guanghui Zhang , Manuel La Licata , Yanru Wen , Michael Maerker , Qinke Yang , Guowei Pang , Enheng Wang
Gully erosion severely threatens land resources and agricultural sustainability, yet the role of subsurface erosion-resistant soil layers remains poorly understood. This study integrated sub-meter imagery with stratified soil sampling (0–120 cm depth) across 79 gullies with comparable slopes gradient and catchment areas on a farm (570 km2) in the black soil region of northeast China to quantify how erosion-resistant layers control gully sidewall expansion and headcut retreat. Ten soil properties were analyzed to construct a PCA-based comprehensive soil erosion resistance score (CRS), revealing a decline in CRS with profile depth and a hierarchy of soil resistance: Black soil > Black soil-Loess transition layer > Loess > Loess-Sand transition layer > Fluvial sandy. The first two layers were identified as erosion-resistant layers. Through threshold effect analysis, a threshold erosion-resistant layer thickness of 53.88 cm was identified (p < 0.01) for sidewall expansion, revealing a 1.36 cm/yr acceleration in gully sidewall expansion per 1 cm thinning within the threshold thickness. Gullies with erosion-resistant layers below the sensitivity thickness experienced 2.03 times higher expansion rate. Gullies newly formed since 2010 exhibited a lower threshold (34.90 cm) than the pre-existing gullies. Gully headcut retreat rate was 43 % higher if the resistant layer was thinner than 54.28 cm, despite no significant detectable threshold. The threshold erosion-resistant layer thickness is potentially modulated by the depth of soil cracks and needs further investigation. This study highlights the importance of soil-profile features, not just surface properties, in gully erosion research. Integration of this threshold into gully erosion models could revolutionize gully prediction and precision conservation strategies.
沟蚀严重威胁着土地资源和农业的可持续性,但人们对地下抗侵蚀土层的作用知之甚少。该研究将亚米图像与分层土壤采样(0-120 cm深度)整合在中国东北黑土区一个农场(570 km2)的79个具有相似坡度和集水区的沟渠中,以量化抗侵蚀层如何控制沟渠侧壁扩张和头切后退。通过对10种土壤性质的分析,构建了基于pca的土壤抗侵蚀综合评分(CRS),揭示了CRS随剖面深度的递减规律和土壤抗侵蚀能力等级:黑土>; 黑土-黄土过渡层>; 黄土>; 黄土-砂土过渡层>; 河流砂。前两层被确定为抗侵蚀层。通过阈值效应分析,确定了边墙膨胀的阈值抗侵蚀层厚度为53.88 cm (p <; 0.01),表明在阈值厚度范围内,每减薄1 cm,沟道边墙膨胀的加速度为1.36 cm/年。抗蚀层小于敏感厚度的沟槽膨胀率高2.03倍。2010年以来新形成的沟壑的阈值(34.90 cm)低于原有沟壑。当抵抗层厚度小于54.28 cm时,沟顶后退率提高了43 %,尽管没有显著的检测阈值。阈值抗侵蚀层厚度可能受土体裂缝深度的影响,需要进一步研究。这项研究强调了土壤剖面特征在沟蚀研究中的重要性,而不仅仅是表面性质。将这一阈值整合到沟壑侵蚀模型中可以彻底改变沟壑预测和精确保护策略。
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