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Microbial effect on soil organic carbon accumulation and stabilization is lithology-depend in subtropical coniferous forest 微生物对亚热带针叶林土壤有机碳积累和稳定的影响是由岩性决定的
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-14 DOI: 10.1016/j.apsoil.2025.106103
Tao Yang , Liang Dong , Haoran Zhang , Chenghao Zheng , Jinxing Zhou , Xiawei Peng
Lithology plays a crucial role in controlling the soil carbon (C) pool in forest ecosystems. The dynamics of soil organic C (SOC) are significantly influenced by the composition and function of the soil microbial community. However, the mechanisms by which lithology influences SOC and the involvement of microbes in this process remain unclear. To assess both the accrual and stability of SOC, we analyzed its content and physical composition by fractionating it into labile particulate organic C (POC) and stable mineral-associated organic C (MAOC). The study was conducted in two representative plantation coniferous forests developed on karst (limestone) and non-karst (shale) soils, with the aim of elucidating potential microbial regulatory mechanisms underlying lithology-mediated differences in SOC dynamics. Our findings revealed that SOC concentration was significantly higher in karst soils compared to non-karst soils at both depths, primarily due to the greater accumulation of MAOC, while lithology had a different effect on POC between topsoil and subsoil. Interestingly, the ratio of MAOC to POC was higher in karst soils compared to non-karst forests only in subsoils. These results imply the crucial role of lithology on SOC accrual and stability in coniferous forests. Soil nutrients stoichiometry, pH and exchangeable calcium ions (Ca2+) have exerted influence over microbial community composition, whereas microbial biodiversity and life history strategies only affected by soil nutrients. Additionally, structural equation modeling analyses revealed that lithology exerts a stronger influence on SOC than tree species, as lithology affects soil nutrient availability, thereby indirectly regulating the microbial impact on SOC accumulation. Nonetheless, both tree species and lithology significantly influence Ca2+, which indirectly promote SOC accumulation by enhancing the stability of SOC pool. Collectively, our study highlights the key role of lithology in SOC stability and accrual, providing a lithology-dependent linkage between microbial communities and the soil C pool.
在森林生态系统中,岩性对土壤碳库的控制起着至关重要的作用。土壤有机碳(SOC)动态受土壤微生物群落组成和功能的显著影响。然而,岩性影响有机碳的机制以及微生物在这一过程中的参与尚不清楚。为了评估土壤有机碳的积累和稳定性,我们将土壤有机碳分为易失稳颗粒有机碳(POC)和稳定矿物伴生有机碳(MAOC),分析了土壤有机碳的含量和物理组成。本研究以喀斯特(石灰岩)和非喀斯特(页岩)土壤上发育的两种具有代表性的人工针叶林为研究对象,旨在阐明岩性介导的有机碳动态差异背后的潜在微生物调控机制。研究结果表明,在两个深度,喀斯特土壤的有机碳浓度明显高于非喀斯特土壤,这主要是由于MAOC的积累较多,而岩性对表土和底土POC的影响不同。有趣的是,与非喀斯特森林相比,喀斯特土壤中MAOC与POC的比值仅在底土中较高。这些结果表明,岩性对针叶林有机碳的积累和稳定起着至关重要的作用。土壤养分化学计量、pH和交换性钙离子(Ca2+)对微生物群落组成有影响,而微生物多样性和生活史策略仅受土壤养分的影响。此外,结构方程模型分析表明,岩性对土壤有机碳的影响强于树种,因为岩性影响土壤养分有效性,从而间接调节微生物对有机碳积累的影响。然而,树种和岩性对Ca2+均有显著影响,Ca2+通过增强有机碳库的稳定性间接促进了有机碳的积累。总的来说,我们的研究强调了岩性在有机碳稳定性和积累中的关键作用,提供了微生物群落和土壤碳库之间的岩性依赖联系。
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引用次数: 0
Urbanization enhances soil nitrogen mineralization mainly by increasing particulate organic nitrogen fractions in urban park greenspaces: A case study in Hangzhou, China 城市化主要通过增加城市公园绿地中的颗粒有机氮组分来提高土壤氮矿化度:中国杭州案例研究
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-14 DOI: 10.1016/j.apsoil.2025.106098
Bo Fan , Yuye Shen , Yan Wang , Liming Yin , Kumuduni Niroshika Palansooriya , Yongfu Li , Bing Yu , Scott X. Chang , Yanjiang Cai
In addition to the direct input of inorganic nitrogen (N), the supply of plant-available N driven by soil organic N mineralization is crucial for the development of urban greenspaces, which are essential components of urban ecosystems. Soil N mineralization may vary with urbanization, but the responses of soil N mineralization to different urbanization intensities remain controversial. In this study, we investigated the responses of urban park soil (planted with trees, shrubs or grasses) N mineralization to different urbanization intensities (low, medium and high) in Hangzhou, China. To further evaluate the relative importance of soil organic N fractions in explaining variations in N mineralization, we analyzed the responses of soil particulate organic N (PON) and mineral-associated organic N (MAON) to different urbanization intensities, as well as their relationships with N mineralization. Our results indicated that soil N mineralization increased with increasing urbanization intensity, likely due to increases in soil organic carbon concentration, clay content, microbial biomass and activity under high urbanization intensity. Notably, compared to soil MAON, the increase in soil PON induced by urbanization was more pronounced, and its relationship with soil N mineralization was stronger. Furthermore, soil N mineralization and its relationships with soil organic N fractions varied substantially among different vegetation types. These findings suggest that researchers and urban planners should evaluate the N supply mineralized from soil organic N fractions, particularly PON fractions, to optimize N and vegetation management strategies in urban greenspaces under different urbanization intensities.
除了无机氮的直接输入外,由土壤有机氮矿化驱动的植物速效氮供应对城市绿地的发展至关重要,而城市绿地是城市生态系统的重要组成部分。土壤N矿化随城市化进程而变化,但不同城市化强度下土壤N矿化的响应仍存在争议。研究了杭州市城市公园土壤(乔灌木草)N矿化对不同城市化强度(低、中、高)的响应。为了进一步评价土壤有机氮组分在解释氮矿化变化中的相对重要性,我们分析了土壤颗粒有机氮(PON)和矿物相关有机氮(MAON)对不同城市化强度的响应,以及它们与氮矿化的关系。结果表明,随着城市化强度的增加,土壤N矿化程度增加,这可能与高城市化强度下土壤有机碳浓度、粘土含量、微生物量和活性的增加有关。值得注意的是,与土壤MAON相比,城市化导致的土壤PON增加更为明显,且与土壤N矿化的关系更强。此外,不同植被类型的土壤氮矿化及其与土壤有机氮组分的关系存在较大差异。这些研究结果表明,研究人员和城市规划者应该评估土壤有机氮组分,特别是PON组分矿化的氮供应,以优化不同城市化强度下城市绿地的氮和植被管理策略。
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引用次数: 0
Lupin-barley intercropping: Root to root interactions drive nitrogen transfer from legume to cereal 羽扇豆与大麦间作:根与根之间的相互作用驱动氮素从豆科植物向谷类作物的转移
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-11 DOI: 10.1016/j.apsoil.2025.106069
Anna Massa , Marta Gil-Martinez , Anders Michelsen , Dorte Bodin Dresbøll , Rasmus Kjøller
Intercropping cereals and legumes is a means to reduce fertilizer input in agriculture. Transfer of biologically fixed N often occurs in cereal-legume intercropping and this study aims to understand the mechanism behind. Lupins are legumes of agronomical interest due to their high protein content and effective soil P extraction. However, as lupins are commonly described as non-mycorrhizal the transfer route of N from lupin to barley remains to be elucidated. We investigated the growth and nutrient content of barley intercropped with lupins, to test whether transfer of symbiotically fixed N from lupins to barley occurs, with focus on any role of arbuscular mycorrhizal (AM) fungi in this transfer.
Lupin species and barley were grown in pots (as sole crop or intercropped) ± mesh enclosures restricting mycelial and/or root growth between compartments. Plant growth and AM fungal root colonization were recorded, and plant 15N natural abundance was measured to determine potential transfer routes of fixed N from lupin to barley.
Intercropped treatments showed increased barley growth and N contents, most pronounced if root-root intermingling of the two species was allowed. Also, 15N natural abundance in plants corroborated N transfer from lupins to barley. As lupin roots remained non-mycorrhizal, even in presence of a mycorrhizal donor plant, hyphal translocation of N was unlikely.
We conclude that N transfer from non-mycorrhizal lupins to mycorrhizal barley primarily occurred through bulk flow, stimulated by interspecific root-to-root contact. This may contribute to the success of lupin and barley intercropping.
谷物和豆类间作是减少农业肥料投入的一种手段。谷物-豆科作物间作中经常发生生物固定氮的转移,本研究旨在了解其背后的机制。羽扇豆因其高蛋白含量和有效的土壤磷提取而成为农艺学上的重要豆类。然而,由于羽扇豆素通常被描述为非菌根,氮从羽扇豆到大麦的转移途径仍有待阐明。我们研究了间作羽扇豆素的大麦的生长和营养含量,以测试共生固定氮是否会从羽扇豆素转移到大麦,并重点研究了丛枝菌根真菌(AM)在这种转移中的作用。卢平和大麦种植在盆栽中(作为单一作物或间作)±网眼围栏,限制隔间之间菌丝和/或根的生长。记录植物生长和AM真菌根定植情况,测定植株15N自然丰度,确定固定N从卢平向大麦转移的潜在途径。间作处理显著提高了大麦的生长和氮含量,在两种作物根际杂交的情况下效果最为显著。此外,植物中15N的天然丰度证实了N从羽扇豆向大麦的转移。由于露平根仍然是非菌根,即使存在菌根供体植物,菌丝N的易位也不太可能。我们得出结论,从非菌根羽扇豆到菌根大麦的氮转移主要是通过大流量进行的,这是由种间根与根接触刺激的。这可能有助于黑豆与大麦间作的成功。
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引用次数: 0
Angelica cultivation and mycorrhizal inoculation improve microbial diversity, functions and network complexity of trace elements-polluted soil: A three-year field study 当归栽培和菌根接种对微量元素污染土壤微生物多样性、功能和网络复杂性的影响
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-11 DOI: 10.1016/j.apsoil.2025.106082
Julien Langrand , Anissa Lounès-Hadj Sahraoui , Papa Mamadou Sitor Ndour , Frédéric Laruelle , Natacha Facon , Jérôme Duclercq , Joël Fontaine
Growing aromatic and medicinal plants for producing essential oils has been presented as an innovative and economically viable alternative for phytomanaging soils polluted by trace elements (TE). However, the influence of aromatic plants, particularly angelica cultivation, on the soil microbial communities has received little attention. Thus, this work is aimed at studying changes in the biomass, composition, functional diversity, and network complexity of soil bacterial and fungal communities during three years of cultivation. Although growing angelica had little effect on fungal richness and diversity, the biomass and diversity of bacterial communities increased, as did the complexity of interactions between various microorganisms in the polluted soil compared to the initial state. Saprotrophic fungi became significantly more abundant after angelica cultivation, contributing to increased soil organic carbon and organic matter content. Arbuscular mycorrhizal fungi inoculation enhanced microbial network complexity from the year 2. Finally, an improvement in the abundance of functional genes linked to the carbon cycle was demonstrated. The findings evidenced the ecological requalification of TE-polluted soil thanks to the angelica cultivation.
种植用于生产精油的芳香和药用植物已被认为是一种创新和经济可行的植物管理受微量元素(TE)污染的土壤的替代方法。然而,芳香植物,特别是当归栽培对土壤微生物群落的影响却很少受到关注。因此,本研究旨在研究三年内土壤细菌和真菌群落的生物量、组成、功能多样性和网络复杂性的变化。尽管种植当归对真菌丰富度和多样性的影响不大,但与初始状态相比,污染土壤中细菌群落的生物量和多样性增加了,各种微生物之间相互作用的复杂性也增加了。当归栽培后腐养真菌数量显著增加,土壤有机碳和有机质含量增加。丛枝菌根真菌接种从2年起增强了微生物网络的复杂性。最后,与碳循环相关的功能基因的丰度得到了改善。结果表明,当归种植对te污染土壤具有生态再认证作用。
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引用次数: 0
Nematode communities respond more to N enrichment than to plant community changes over decades in tallgrass prairie 高草草原线虫群落对N富集的响应大于对植物群落变化的响应
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-10 DOI: 10.1016/j.apsoil.2025.106096
T.C. Todd , J.M. Blair , M.A. Callaham Jr.
Temperate grasslands such as the North American tallgrass prairie are among the most endangered terrestrial ecosystems due to changes in climate and land-use practices. While belowground responses of terrestrial ecosystems to perturbations have received greater attention in recent years, there is a dearth of long-term studies documenting changes over decadal scales. The current study addresses the long-term effects of fire (annual burning or fire exclusion), mowing, and nitrogen (N) and phosphorus (P) fertilization on the structure and composition of a tallgrass prairie nematode community after 32 years of experimental treatments. Fire exclusion resulted in conversion of grassland to woodland, and a general decrease in nematode population densities, while annual prescribed fire maintained a grassland state. Although the change in vegetative state affected overall nematode abundance, vegetative structure was not the major driver of nematode community composition. Rather, changes in nitrogen availability appeared to be the dominant driver of nematode community dynamics. Responses of herbivorous taxa were dominated by interactions among burning, mowing, and N fertilization treatments and varied across taxonomic groups, but a general pattern of increasing relative abundances with N fertilization was observed, particularly in the presence of annual burning or mowing. In contrast, the relative abundance of the fungivorous Tylenchidae, the dominant nematode family in terms of abundance, declined from 44 % to 26 % after 32 years of N enrichment, while fire exclusion favored the opportunistic bacterivorous Rhabditidae. Although higher trophic level responses were generally uninformative, our results confirmed the value of nematode community analysis in soil food web diagnostics, with fungivore to bacterivore ratios and the maturity index (MI) identified as useful community indices.
由于气候和土地利用方式的变化,北美高草草原等温带草原是最濒危的陆地生态系统之一。虽然近年来陆地生态系统对扰动的地下响应受到了更多的关注,但缺乏记录十年尺度变化的长期研究。本研究通过32年的试验处理,探讨了火(每年燃烧或禁火)、割草和氮磷施肥对高草草原线虫群落结构和组成的长期影响。禁火导致草地向林地转化,线虫种群密度普遍下降,而年度规定火维持草原状态。虽然营养状态的变化影响线虫的总体丰度,但营养结构不是线虫群落组成的主要驱动因素。相反,氮有效性的变化似乎是线虫群落动态的主要驱动因素。草食性类群的响应主要由焚烧、刈割和氮肥处理之间的相互作用所主导,并且在不同分类类群之间存在差异,但总体上观察到氮肥处理的相对丰度增加,特别是在每年焚烧或刈割的情况下。相比之下,富氮32年后,以真菌为主的线状线虫科(Tylenchidae)的相对丰度从44%下降到26%,而不加火则有利于机会性细菌线状线虫科(Rhabditidae)。虽然更高营养水平的响应通常不具有信息性,但我们的研究结果证实了线虫群落分析在土壤食物网诊断中的价值,其中真菌与细菌的比值和成熟度指数(MI)被确定为有用的群落指标。
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引用次数: 0
Compost, digestate, and vermicompost from the recycling of urban biowaste have different impacts on earthworm behavior: A mesocosm study 来自城市生物垃圾回收的堆肥、消化物和蚯蚓堆肥对蚯蚓行为有不同的影响:一项中观研究
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-10 DOI: 10.1016/j.apsoil.2025.106095
Vincent Ducasse , Line Capowiez , Joséphine Peigne , Yvan Capowiez
The valorization of Organic Fraction of Municipal Solid Waste (OFMSW) is mandatory in Europe since 2024. Composting, anaerobic digestion (AD), and vermicomposting are the techniques most commonly used for recycling OFMSW. When applied to soil, these products can have different effects on earthworms with either positive (food effect) or negative effects (toxic or repellent effect). We thus carried out a laboratory experiment to assess their influence on different facets of the earthworm behavior (bioturbation and cast production) for two earthworm species (Lumbricus terrestris and Aporrectodea caliginosa) currently found in arable lands. Mesocosms (30 cm depth and 16 cm diameter) were filled with soil from a field crop each product was mixed with soil at two doses: equivalent to 80 kg of N per hectare (normal practice for wheat crop) and 160 kg. N.ha−1. Barium sulfate was also spread at 2.5 cm depth (i.e. between the two soil layers containing the products) as a contrast agent visible in X-ray tomography. After 2 months, the burrowing activity of earthworms within mesocosms was analyzed using X-ray tomography, surface casts were collected, and earthworms weighed. With compost, L. terrestris burrowed closer to the surface (in the 0–5 cm layer) compared to when in the presence of vermicompost and digestate (with 0.85, 0.55, and 0.29 cm3 of burrows, respectively). Moreover, signs of avoidance were detected for this species when digestate was present with deeper burrows (in a 15–25 cm layer). With compost, A. caliginosa burrowed more compared to when in the presence of vermicompost and digestate (with 3.22, 2.64, and 0.97 cm3, in the totality of mesocosm respectively). Digestate has no negative impact on the behavior of A. caliginosa. Barium enables the characterization of the ingestion and displacement of the soil layer containing the products. The displaced volumes were in the following order Compost > Vermicompost > Digestate with larger effects for the 160 than for the 80 kg.N.ha−1 dose. Globally, compost had higher and positive effects for both species activities whereas digestate showed some negative impact on L. terrestris only. Vermicompost had positive effects but less marked than those of compost. These effects should however still be validated under field conditions.
自2024年以来,欧洲城市固体废物有机组分(OFMSW)的定价是强制性的。堆肥、厌氧消化(AD)和蚯蚓堆肥是回收城市固体垃圾最常用的技术。当应用于土壤时,这些产品可以对蚯蚓产生不同的效果,要么是积极的(食物效果),要么是消极的(有毒或驱避效果)。因此,我们进行了一项实验室实验,以评估它们对目前在耕地中发现的两种蚯蚓(Lumbricus terrestris和Aporrectodea caliginosa)的蚯蚓行为(生物扰动和cast production)的不同方面的影响。中囊(30厘米深,16厘米直径)填入田间作物的土壤,每种产品以两种剂量与土壤混合:相当于每公顷80公斤氮(小麦作物的常规做法)和160公斤氮。N.ha−1。硫酸钡也作为x射线断层扫描可见的造影剂散布在2.5厘米深度(即在含有产品的两层土壤之间)。2个月后,利用x射线断层扫描分析蚯蚓在中囊内的挖洞活动,收集表面铸型,并对蚯蚓称重。与蚯蚓堆肥和消化液相比,有堆肥的土栖L. terrestris挖洞更靠近地表(0-5 cm层)(分别为0.85、0.55和0.29 cm3)。此外,当消化物存在于更深的洞穴(在15-25厘米的层中)时,发现了这种物种回避的迹象。有堆肥时,与有蚯蚓堆肥和消化液时相比,A. caliginosa挖洞更多(分别为3.22 cm3、2.64 cm3和0.97 cm3)。消化液对假单胞菌的行为无负面影响。钡能够表征含有产品的土层的摄入和位移。位移体积按以下顺序排列:Vermicompost祝辞消化对160公斤体重的影响大于对80公斤体重的影响。ha−1剂量。在全球范围内,堆肥对这两种植物的活动均有较高的正向影响,而消化液仅对陆生l.s terrestris的活动有一定的负面影响。蚯蚓堆肥有积极作用,但效果不如堆肥显著。然而,这些影响仍应在现场条件下进行验证。
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引用次数: 0
Potential effect of biogas slurry application to mitigate of peak N2O emission without compromising crop yield in North China Plain cropping systems 施用沼液在不影响作物产量的情况下缓解华北平原种植系统N2O峰值排放的潜在效应
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-09 DOI: 10.1016/j.apsoil.2025.106083
Zhichao Zou , Yue Li , Xueqin Ren , Zichao Zhao , Zhangliu Du , Di Wu
Biogas slurry (BS) produced from anaerobic digestion of livestock manure can be benefit for crop yields and soil fertility in cropping systems as compared to sole synthetic fertilization, but its impact on nitrous oxide (N2O) emissions is inconsistent in the literatures. The North China Plain (NCP) serves as a vital agricultural region in China, contributing approximately 40 % of the nation's total wheat and maize production. However, owing to the lack of relevant field studies, the understanding of how BS affects crop yield and N2O emissions in NCP remains unclear. Here, we assessed the effects of BS substitution (0 % substitution, CF; 50 % substitution, 50%BS; 100 % substitution, 100%BS) on the amount and sources of N2O emissions by monitoring N2O fluxes combined with the isotopomer ratios of soil-derived N2O in the NCP. The results showed that, compared with the control, CF, 50 % BS, and 100 % BS significantly increased wheat grain yield by 66.1 %–67.9 % and silage maize yield by 46.3 %–53.3 %, respectively. Compared with CF, 50%BS reduced N2O emissions by 40.1 % in the wheat season and by 35.5 % maize season, while 100%BS reduced N2O emissions by 31.9 % in the wheat season and by 49.2 % in the maize season. Further site preference analysis revealed that nitrification and fungal denitrification together contributed to 40.3–44.9 % of the peak N2O emissions in CF, 50%BS, and 100%BS, with no significant differences in SP values among them. Compared with CF, 100%BS significantly reduced the copy numbers of AOB-amoA, nirK, and nirS by 65 %, 41 %, and 35 %, respectively, which may be key factors in reducing N2O emissions. Our results showed that the partial substitution of chemical fertilizers with BS is an efficacious practice for maintaining crop yields while simultaneously reducing N2O emissions in the NCP.
与单一的合成施肥相比,畜禽粪便厌氧消化产生的沼液(BS)有利于作物产量和土壤肥力,但其对氧化亚氮(N2O)排放的影响在文献中并不一致。华北平原(NCP)是中国重要的农业区,约占全国小麦和玉米总产量的40%。然而,由于缺乏相关的实地研究,对BS如何影响NCP作物产量和N2O排放的理解仍然不清楚。在这里,我们评估了BS替代的效果(0%替代,CF;50%替代,50%BS;100%替代,100%BS)通过监测N2O通量结合NCP中土壤来源N2O的同位素比来确定N2O排放量和来源。结果表明,与对照相比,CF、50% BS和100% BS分别显著提高小麦产量66.1% ~ 67.9%和青贮玉米产量46.3% ~ 53.3%。与CF相比,50%BS在小麦季和玉米季分别减少了40.1%和35.5%的N2O排放量,而100%BS在小麦季和玉米季分别减少了31.9%和49.2%的N2O排放量。进一步的场地偏好分析表明,硝化作用和真菌反硝化作用共同贡献了CF、50%BS和100%BS中N2O峰值排放的40.3 - 44.9%,三者之间的SP值无显著差异。与CF相比,100%BS显著降低了AOB-amoA、nirK和nirS的拷贝数,分别降低了65%、41%和35%,这可能是减少N2O排放的关键因素。我们的研究结果表明,用BS部分替代化肥是保持作物产量同时减少NCP中N2O排放的有效做法。
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引用次数: 0
Community structure and selected genes abundance shift of rhizosphere and endophyte bacteria from roots associated with the sludge application under reclaimed water irrigation 再生水灌溉条件下污泥施用对根际和根内生细菌群落结构及部分基因丰度的影响
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-09 DOI: 10.1016/j.apsoil.2025.106070
Bingjian Cui , Haishu Sun , Erping Cui , Chao Hu , Xiangyang Fan , Zhongyang Li , Chuncheng Liu
Reclaimed water and sewage sludge as renewable resources are urged to be used in agriculture, but their reuse poses potential chemical and microbiological risks. As a waste biomass resource, sludge combined with reclaimed water irrigation is a major way to develop and utilize renewable resources and control environmental pollution. However, whether reclaimed water irrigation and sludge application have adverse effects on the agricultural environment and human health remains a controversial point of discussion. A greenhouse pot experiment was conducted to investigate the effects of reclaimed water and sewage sludge on rhizosphere soil and root endophytic bacterial communities, the abundance of selected genes, and to evaluate the soil quality of sludge application. The results of this study demonstrated that the application of sewage sludge could result in the accumulation of nutrients in soil. The rhizosphere soil and root endophytic bacteria possessed common dominant groups at phylum level, including Proteobacteria, Bacteroidota, Actinobacteriota and Chloroflexi. Reclaimed water irrigation had less effect on rhizosphere soil and root endophytic bacterial communities than sludge application. Pseudomonas showed a decrease in relative abundance in both rhizosphere soil and root endophytes following sludge application, whereas beneficial bacteria like Bacillus, Stenotrophobacter, Cellvibrio and Altererythrobacter experienced an increase. Redundancy analysis (RDA) showed that the diversity and composition of bacterial communities in rhizosphere soil among treatment groups were closely related to soil organic matter, total nitrogen and total phosphate contents. The functional prediction highlighted the participation of functional groups in nitrogen and carbon cycling as well as degradation processes at varying sludge application rates. The abundance of selected genes was more affected by sludge application. A considerable amount of sludge application to the soil resulted in a significant increase in the abundance of pathogens and antibiotic resistance genes, as well as functional genes, compared to unamended soil with sludge treatment. Direct or excessive application of sludge might aggravate the dissemination and accumulation of deleterious genes in soil-crop systems irrigated with reclaimed water. Overall, our study results may provide valuable information on how sludge influences the microbial community characteristics and abundance of specific genes, guiding the assessment of biological quality and the appropriate use of sludge in agriculture irrigated with reclaimed water.
中水和污水污泥作为一种可再生资源,在农业中得到了广泛的应用,但它们的再利用会带来潜在的化学和微生物风险。污泥作为一种废弃生物质资源,结合再生水灌溉是开发利用再生资源和治理环境污染的重要途径。然而,再生水灌溉和污泥应用是否对农业环境和人体健康产生不利影响仍是一个有争议的讨论点。通过温室盆栽试验,研究了再生水和污水污泥对根际土壤和根内生细菌群落、选择基因丰度的影响,评价了污泥施用对土壤质量的影响。本研究结果表明,污水污泥的施用会导致土壤中养分的积累。根际土壤和根内生细菌在门水平上具有共同的优势类群,包括变形菌门、拟杆菌门、放线菌门和绿菌门。再生水灌溉对根际土壤和根内生细菌群落的影响小于污泥灌溉。施用污泥后,根际土壤和根内生菌中假单胞菌的相对丰度均有所下降,而芽孢杆菌、窄滋养杆菌、Cellvibrio和Altererythrobacter等有益菌的相对丰度有所增加。冗余分析(RDA)表明,各处理组根际土壤细菌群落的多样性和组成与土壤有机质、全氮和全磷含量密切相关。功能预测强调了官能团在不同污泥施用量下参与氮和碳循环以及降解过程。所选基因的丰度受污泥施用的影响较大。与未经污泥处理的土壤相比,大量污泥施用于土壤导致病原体和抗生素抗性基因以及功能基因的丰度显著增加。直接或过量施用污泥会加剧再生水灌溉土壤-作物系统中有害基因的传播和积累。总的来说,我们的研究结果可能为污泥如何影响微生物群落特征和特定基因的丰度提供有价值的信息,指导生物质量评估和污泥在再生水灌溉农业中的合理利用。
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引用次数: 0
Changes of microbial turnover and plant uptake of soil amino acids during conversion of a natural forest to a spruce plantation on the eastern Tibetan plateau, China 中国青藏高原东部天然林向云杉人工林转化过程中微生物周转和植物对土壤氨基酸吸收的变化
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-09 DOI: 10.1016/j.apsoil.2025.106085
Ziliang Zhang , Bartosz Adamczyk , Huajun Yin
It is well recognized that amino acids play an important role in soil nitrogen (N) cycling and contribute to plant N supply in forests. Land-use change is likely to alter soil amino- acid cycling and the role of amino acids in plant nutrition by influencing multiple abiotic and biotic factors, which, however, remains poorly understood. Here, by using 15N labeling methods, we quantified effects of land-use change from a natural forest to a spruce plantation on the uptake and turnover of amino acids by soil microbes, as well as trees' ability to take up amino acids on eastern Tibetan, China. Forest conversion from the natural forest to the spruce plantation significantly decreased soil inorganic N availability and N transformation rates, while increased the ratio of amino acids to inorganic N concentration. A soil incubation experiment with 15N-labeled-glycine addition in the laboratory showed that forest conversion inhibited gross consumption of amino acids and facilitated recycling of amino acids within microbial biomass. Furthermore, an in situ 15N-labeling experiment revealed that forest conversion significantly increased the contribution of soil amino acids to the total N uptake by plants, which was attributed to the increased proportion of amino acids in soil available N pools. Collectively, our results demonstrated that forest conversion from natural forests to plantations impacted turnover of amino acids by soil microbes, which consequently influenced plant uptake of amino acids. Our study further highlights the important role of amino acids as a N source for subalpine coniferous plantations and has implications for formulating management practices to maintain long-term productivity and stability of plantations.
氨基酸在森林土壤氮循环和植物氮供应中发挥着重要作用。土地利用变化可能通过影响多种非生物和生物因子来改变土壤氨基酸循环和氨基酸在植物营养中的作用,然而,对这些因素的了解仍然很少。本研究采用15N标记方法,定量分析了西藏东部天然林到云杉人工林的土地利用变化对土壤微生物对氨基酸的吸收和转换以及树木对氨基酸的吸收能力的影响。天然林向云杉人工林的转换显著降低了土壤无机氮有效性和氮素转化率,提高了氨基酸与无机氮的比值。在室内进行的15n标记甘氨酸土壤培养实验表明,森林转化抑制了微生物生物量中氨基酸的总消耗,促进了氨基酸的循环利用。此外,原位15n标记试验表明,森林转换显著增加了土壤氨基酸对植物总氮吸收的贡献,这可能是由于土壤有效氮库中氨基酸的比例增加。总的来说,我们的研究结果表明,从天然林到人工林的森林转化影响了土壤微生物对氨基酸的周转,从而影响了植物对氨基酸的吸收。我们的研究进一步强调了氨基酸作为亚高山针叶人工林氮源的重要作用,并对制定管理措施以保持人工林的长期生产力和稳定性具有重要意义。
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引用次数: 0
Earthworms regulate the response of greenhouse gas emissions in wetland soils to simulated warming and flooding 蚯蚓调节湿地土壤温室气体排放对模拟变暖和洪水的响应
IF 4.8 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2025-04-09 DOI: 10.1016/j.apsoil.2025.106074
Mingzhu Lu , Wenzhi Liu , Lei Fan , Haitao Wu
Wetlands are a significant source of greenhouse gases (GHGs) and provide crucial habitats for soil invertebrates. Climate change, including warming and increased flooding, has considerably altered the exchange of GHGs between wetland soils and the atmosphere. However, whether and how soil fauna regulates the impacts of climate change on GHGs remains obscure. Herein, we conducted a 58-day microcosm incubation of wetland soils at two temperatures (20 and 25 °C) and two soil moisture levels (90 % and 135 % water-filled pore space) to investigate how earthworms (Eisenia fetida) regulate the direction and magnitude of GHG (CO2, CH4, and N2O) responses to simulated warming and flooding scenarios. Results showed that warming increased emissions of all three GHGs, whereas flooding increased CH4 emissions but suppressed CO2 and N2O emissions. Earthworms changed these response patterns by interacting with temperature and soil moisture conditions. Earthworms mitigated the positive effects of warming on CO2 and N2O but strengthened the positive influences of warming on CH4, and they converted the negative response of CO2 to flooding to positive but did not change the response of CH4 and N2O to flooding. In addition, Hierarchical partitioning analysis revealed that soil nitrogen availability (including NH4+-N, NO3-N, and water-soluble nitrogen) and soil aggregates are the dominant factors driving the response of GHG emissions to earthworm activities and climate change. Overall, our findings highlight the crucial role of soil fauna in regulating GHG responses to warming and flooding in wetland soils, with significant implications for climate change mitigation.
湿地是温室气体的重要来源,为土壤无脊椎动物提供了重要的栖息地。气候变化,包括气候变暖和洪水增加,极大地改变了湿地土壤和大气之间的温室气体交换。然而,土壤动物是否以及如何调节气候变化对温室气体的影响仍然不清楚。本研究对湿地土壤在2种温度(20°C和25°C)和2种土壤含水量(孔隙含水量90%和135%)下进行了58天的微观培养,以研究蚯蚓(Eisenia fetida)如何调节温室气体(CO2、CH4和N2O)对模拟变暖和洪水情景的响应方向和强度。结果表明,增温增加了3种温室气体的排放,而洪涝增加了CH4的排放,抑制了CO2和N2O的排放。蚯蚓通过与温度和土壤湿度条件的相互作用改变了这些反应模式。蚯蚓减缓了变暖对CO2和N2O的正向影响,但强化了变暖对CH4的正向影响,将CO2对洪水的负响应转化为正响应,但没有改变CH4和N2O对洪水的响应。土壤氮素有效性(包括NH4+-N、NO3−-N和水溶性氮)和土壤团聚体是驱动温室气体排放对蚯蚓活动和气候变化响应的主导因子。总体而言,我们的研究结果强调了土壤动物在调节湿地土壤对变暖和洪水的温室气体响应中的关键作用,对减缓气候变化具有重要意义。
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引用次数: 0
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Applied Soil Ecology
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