酚类物质对土壤和植物的作用机制研究进展

酚类物质是重要的植物次生代谢物质之一,它对植物的生长、养分吸收、生理特性、酶活性以及生长环境中的土壤、微生物等都存在影响。本研究对酚类物质对土壤和植物的作用机制、植物生态系统中酚类物质的含量分布、酚类物质对植物生理生化特性的影响以及对土壤理化特性的影响进行探讨,展望农林生产实践中酚类物质的研究趋势,为解决农业和林业生产中因酚类物质的影响引起生产力下降问题提供依据。     

假单胞菌的微生态调节作用

假单胞菌能够抑制植物病原微生物的生长 ,对改善植物营养、促进植物生长具有很好的作用 ,同时假单胞菌还能够对土壤中的有毒物质进行降解 ,可以作为一种理想的植物微生态制剂生产菌种进行开发     

施用茶树菇栽培废料对青菜土壤中微生物学特征的影响

通过温室盆栽实验研究了施用茶树菇栽培废料对青菜生物量及株高、土壤微生物数量、酶活性及碳源利用能力的影响。结果表明,施用茶树菇栽培废料显著增加了青菜生物量及土壤中放线菌、有机解磷菌、无机解磷菌、纤维素降解菌的数量,改善了土壤微生物区系,提高了土壤磷酸酶活性。单碳源利用图谱显示,施用茶树菇栽培废料增加了土壤微生物功能多样性指数（Shannon指数）,降低了均一性指数（McIntosh指数）。主成分分析结果表明,施用茶树菇栽培废料导致土壤微生物主要对糖类物质的利用能力产生分异。研究表明茶树菇栽培废料可作为一种良好的有机肥料,通过增加非优势土壤微生物的功能多样性而改善土壤微生物特性,从而加速土壤碳、磷等元素循环以促进作物生长和增加产量。     

铝胁迫对大豆根际土壤微生物区系的影响

通过盆栽试验研究了不同浓度外源铝对大豆根际土壤微生物区系的影响。结果表明:在低浓度下,铝对土壤细菌、放线菌具有刺激作用,在高浓度下,表现为抑制作用。铝对真菌的生长具有明显的刺激作用。在高浓度下,铝对土壤硝化细菌、反硝化细菌、自生固氮菌均产生强烈的抑制作用,最大抑制率分别为96%、98%和89%。土壤硝化细菌、反硝化细菌可以作为铝污染土壤生态环境的指示菌。铝对两个大豆品种根际土壤微生物区系组成的影响不一致,揭示铝胁迫的生物效应还与植物生长、植物根际效应有关。     

蚯蚓粪益生菌肥对铁棍山药不同生长时期 共生微生物群落及其品质的影响

蚯蚓粪富含有机质、腐殖酸及微生物菌群,可作为植物养分供应和土壤理化性质改善的常用有机肥基质,然而,其对山药的生长和品质的影响尚不清楚。以木质纤维素饲喂的赤子爱胜蚓得到的蚯蚓粪为基质配施益生菌剂开展山药施用效果的研究,统计分析蚯蚓粪益生菌肥添加对山药生长和品质的变化,探究其对于山药共生微生物群落的影响。结果表明:蚯蚓粪益生菌肥的使用促进了铁棍山药的株高及单株重,提高了山药的产量,收获期铁棍山药中黄酮含量升高了2.48 mg/g,增长约37.48%,可溶性糖、蛋白质及皂苷等营养成分分别提高0.26、0.14、0.31 倍;通过对铁棍山药不同生长时期根际微生物和内生微生物群落结构的分析表明,施肥后根际土壤中链霉菌、鞘氨醇单胞菌、芽孢杆菌明显增多,绿僵菌等明显减少,并且这些丰度明显改变的微生物也与土壤理化性质之间有着明显的相关性。内生微生物中泛菌、枝孢菌明显增多,青枯菌、Cyphellophora 等病原微生物丰度明显减少。蚯蚓粪益生菌肥的施用改善了山药根际微生态健康状况,减少了发病率,提高了山药品质。     

连作土壤微生物区系分析、调控及高通量研究方法

土壤连作后导致土壤微生物生态失衡、病原微生物富集、有益微生物减少,土壤微生物从细菌主导型向真菌主导型转化,使病原菌更容易侵染植物而引发植物的各种土传病害。施用微生物有机肥可以将失衡的微生物区系恢复到健康的状态,从而可以起到防治土传病害的作用。本文围绕连作引起的土壤中各大类微生物数量和种类的变化以及连作土壤施用微生物有机肥修复后其微生物数量和种类的变化进行了综述,并通过与传统技术比较,介绍了454高通量测序研究方法的优越性,指出了其在土壤微生物区系研究中的重要性。     

Fe2+对水稻生长及土壤微生物活性的影响

通过盆栽试验,模拟冷浸田土壤亚铁毒害,研究了土壤-水稻-亚铁-微生物相互作用的体系中,外加Fe2+ 不同处理水平 (0、 100、 200、 400、 800和1600 mg/kg) 对水稻苗期和分蘖期相关生理指标、 土壤微生物活性及其生态特征的影响。结果表明, 在含一定亚铁本底（207.77 mg/kg）的正常稻田土壤中,外源性Fe2+的加入将逐步抑制水稻生长、 降低土壤微生物活性。外源Fe2+浓度达100 mg/kg后,水稻的株高、 干物质积累量显著降低; 水稻叶片生理指标叶绿素含量（SPAD值）、 脯氨酸含量、 抗氧化酶系统活性则显著增加,表明外源Fe2+浓度100 mg/kg 是本研究条件下外源Fe2+ 对水稻生长产生显著毒害影响的临界点; 同时随外源Fe2+浓度的增加, 土壤微生物活性指标土壤微生物量碳、 微生物三大基础菌系总量（细菌、 真菌、 放线菌）、 功能菌系总量（氨化细菌、 固氮菌、 纤维分解菌）、 铁还原菌总量总体是先快速下降,后逐渐平稳降低。 半效应浓度EC50分析表明,外源Fe2+浓度100 mg/kg 为多数土壤微生物活性指标（微生物基础菌系总量、 功能菌系总量、 铁还原菌）EC50变化的临界值; 体系中土壤微生物活性指标和水稻生长指标的变化存在显著的相关性, 表明供试土壤亚铁对水稻生长的影响是亚铁对土壤-植物-土壤微生物系统同步影响的结果。综上结果可知,外源Fe2+浓度100 mg/kg为导致供试土壤中水稻生长及土壤微生物活性受到显著负效应的临界值,进而推知,本研究所用土壤对水稻生长和微生物活性的亚铁毒胁迫临界浓度约为300 mg/kg（含本底）, Fe2+含量超出该浓度时,需采取合理的农艺措施控制其负效应。     

添加葡萄糖和胞外多糖条件下土壤细菌多样性与青枯病病原菌入侵关系研究

微生物多样性、病原菌入侵及微生物群落物质利用的关系尚未系统阐明。本研究通过土壤悬液梯度稀释并外源添加方法构建不同多样性的微生物群落,借以研究土壤微生物多样性与青枯病病原菌(青枯菌)入侵的关系,并通过添加低分子量葡萄糖和高分子量胞外多糖探索物质添加对土壤微生物多样性与病原菌入侵关系的影响。结果表明土壤悬液梯度稀释并外源添加方法能有效构建不同多样性的微生物群落。随着森林和菜地土壤微生物多样性的上升,青枯菌入侵成功率均逐渐降低。此外,添加葡萄糖至不同微生物多样性土壤中均能显著促进青枯菌的生长,而胞外多糖仅在土壤微生物多样性较高时(即竞争较为激烈时)可体现对青枯菌生长的促进作用。综上,土壤微生物多样性与病原菌入侵成功率呈负相关关系,这一关系受土壤微生物群落来源影响较小,物质添加能降低微生物多样性对病原菌入侵的抑制能力,但是该效应与碳源的性质有关。     

内生菌-植物联合修复污染土壤研究进展

环境污染对生态系统及人类健康造成严重威胁。近年来,许多学者研究发现内生菌联合植物修复体系对修复自然环境中的重金属和有机物具有巨大的潜力。本文主要从内生菌联合植物进行污染修复的机理和应用两方面入手,介绍了内生菌接种宿主植物根、茎、叶部的几种方法及定殖的检测方法,总结了污染土壤中内生菌在植物组织内的定殖动态,以及内生菌-植物联合体系强化有机物污染和重金属污染修复效果的应用,并从内生菌调节生长因子、生物固氮和溶磷、在宿主植物体内的共代谢有机物、产生特异性酶降解有机物、提升植物对重金属抗性和降低重金属毒性几个方面解释了内生菌和植物的联合修复机理。最后指出,虽然已经有许多对于内生菌联合植物修复体系的研究,但是目前两者相互作用机理尚未完全清楚,对于多种内生菌组合体系以及处理水体和大气污染的研究并不完善,这些都将成为今后的研究重点。     

岩面和原始土壤微生物区系的研究

本文研究了原始成土过程中岩石表面和原始土壤的微生物区系。原始成土过程,是和微生物分布、活动紧密相联系的。岩面,主要是染有岩漆、生长地衣的岩面,以及原始土壤中,通常定居着大量的微生物。异养微生物中,细菌占优势,主要是产生黄色、橙色和玫瑰色色素的无孢子杆菌和球菌,霉菌和放线菌较少。微嗜氮菌和硝化菌广泛分布在供试样品中,而自生固氮菌和纤维分解菌只出现在南方石灰岩地区生长地衣的岩面及原始土壤中。微生物通过产酸,溶解岩体中的矿物,利用这些矿物作为养料。     

Responses of extracellular enzymes to simple and complex nutrient inputs

Soil microbes produce extracellular enzymes that mineralize organic matter and release carbon and nutrients in forms that can be assimilated. Economic theories of microbial metabolism predict that enzyme production should increase when simple nutrients are scarce and complex nutrients are abundant; however, resource limitation could also constrain enzyme production. We tested these hypotheses by monitoring enzyme activities and nutrient pools in soil incubations with added simple and complex nutrient compounds. Over 28 days of incubation, we found that an enzyme's activity increased when its target nutrient was present in complex but not simple form, and carbon and nitrogen were available. β-Glucosidase and acid phosphatase activities also increased in treatments where only carbon and nitrogen were added. Glycine aminopeptidase and acid phosphatase activities declined in response to ammonium and phosphate additions, respectively. In some cases, mineralization responses paralleled changes in enzyme activity—for example, β-glucosidase activity increased and respiration was 5-fold greater in soil incubations with added cellulose, ammonium, and phosphate. However, a doubling of acid phosphatase activity in response to collagen addition was not associated with any changes in phosphorus mineralization. Our results indicate that microbes produce enzymes according to ‘economic rules’, but a substantial pool of mineral stabilized or constitutive enzymes mediates this response. Enzyme allocation patterns reflect microbial nutrient demands and may allow microbes to acquire limiting nutrients from complex substrates available in the soil.     

单施和配施有机物料对沙化土壤微生物群落功能多样性的短期影响

为探讨施用有机物料对宁夏沙化土壤的改良效果,以当地易得的杨树枝条、玉米秸秆、牛粪为原料在2015年4~10月期间进行桶栽试验,采用Biolog技术研究了有机物料单施和配施对宁夏沙化土壤微生物群落功能多样性的短期影响。结果显示:(1)施用有机物料使土壤微生物利用碳源总量增加,微生物代谢活性增强。其利用比例较高的碳源类型为氨基酸类、胺类和碳水化合物类。(2)单施有机物料比配施有机物料对微生物代谢的促进作用强;单施杨树枝条粉碎物的土壤微生物平均颜色变化率在所有处理中最大,而且微生物各种多样性指数也有明显提高。(3)对各类碳源的利用强度与土壤易氧化有机碳、全氮含量和碳氮比之间表现出了密切的关系,微生物多样性指数则与土壤易氧化有机碳和无机氮存在紧密联系。本研究表明,土壤施入杨树枝条粉碎物后微生物代谢活性增强、土壤质量提高,对土壤改良有积极作用。     

Ecosystem partitioning of N-glycine after long-term climate and nutrient manipulations, plant clipping and addition of labile carbon in a subarctic heath tundra

Low temperatures and high soil moisture restrict cycling of organic matter in arctic soils, but also substrate quality, i.e. labile carbon (C) availability, exerts control on microbial activity. Plant exudation of labile C may facilitate microbial growth and enhance microbial immobilization of nitrogen (N). Here, we studied ¹⁵N label incorporation into microbes, plants and soil N pools after both long-term (12 years) climate manipulation and nutrient addition, plant clipping and a pulse-addition of labile C to the soil, in order to gain information on interactions among soil N and C pools, microorganisms and plants. There were few effects of long-term warming and fertilization on soil and plant pools. However, fertilization increased soil and plant N pools and increased pool dilution of the added ¹⁵N label. In all treatments, microbes immobilized a major part of the added ¹⁵N shortly after label addition. However, plants exerted control on the soil inorganic N concentrations and recovery of total dissolved ¹⁵N (TD¹⁵N), and likewise the microbes reduced these soil pools, but only when fed with labile C. Soil microbes in clipped plots were primarily C limited, and the findings of reduced N availability, both in the presence of plants and with the combined treatment of plant clipping and addition of sugar, suggest that the plant control of soil N pools was not solely due to plant uptake of soil N, but also partially caused by plants feeding labile C to the soil microbes, which enhanced their immobilization power. Hence, the cycling of N in subarctic heath tundra is strongly influenced by alternating release and immobilization by microorganisms, which on the other hand seems to be less affected by long-term warming than by addition or removal of sources of labile C.     

气候变化对土壤有机碳库分子结构特征与稳定性影响研究进展

气候变化与土壤碳库之间的相互作用及耦合机制一直是学术界研究的热点与难点。虽然目前在群落—生态系统、区域—全球等不同尺度上开展了大量研究,然而在分子尺度上探究气候因子波动对土壤有机碳库化学结构特征影响机制方面却鲜有研究。本文综述了近年来气候因子变化及其导致的环境、生态因子变化与土壤有机碳库分子结构特征的关系。气温升高不仅将改变土壤中源自植物部分的有机碳来源特征,同时也会将加速土壤木质素等碳组分分解,排水或者旱化引起有机质分解加速,土壤中C=O键增加。植被演替、土壤动物及微生物等与气候变化密的切相关的生态因子则会影响输入土壤植被残体性质,加速糖类、脂类及木质素分解、并改变有机碳结构的生物分子标志物;土壤中有机碳稳定性与分子结构特征密切相关,土壤中具有高的苯环结构(芳香族化合物)及O-烷基碳通常表明土壤碳库具有更高的稳定性,而之前认为较为稳定的木质素等结构在气候变暖背景下可能并不稳定。未来研究中应着重关注与土壤有机碳分子标志物的识别与生态意义判读、生物对土壤有机碳分子结构转换过程的调控作用及机制、大尺度环境/生态过程与碳库分子结构转变的耦合机制及新的土壤有机碳分子结构辨识技术及判读等方面的研究。     

Manipulating the soil microbiome to increase soil health and plant fertility

A variety of soil factors are known to increase nutrient availability and plant productivity. The most influential might be the organisms comprising the soil microbial community of the rhizosphere, which is the soil surrounding the roots of plants where complex interactions occur between the roots, soil, and microorganisms. Root exudates act as substrates and signaling molecules for microbes creating a complex and interwoven relationship between plants and the microbiome. While individual microorganisms such as endophytes, symbionts, pathogens, and plant growth promoting rhizobacteria are increasingly featured in the literature, the larger community of soil microorganisms, or soil microbiome, may have more far-reaching effects. Each microorganism functions in coordination with the overall soil microbiome to influence plant health and crop productivity. Increasing evidence indicates that plants can shape the soil microbiome through the secretion of root exudates. The molecular communication fluctuates according to the plant development stage, proximity to neighboring species, management techniques, and many other factors. This review seeks to summarize the current knowledge on this topic.     

植物残体向土壤有机质转化过程及其稳定机制的研究进展

土壤有机质的数量和质量不仅是衡量土壤肥力状况的核心要素,其形成、转化及稳定过程还与全球气候变化密切相关。植物残体是土壤有机质的初始来源,但由于其腐解过程的复杂、多变性以及土壤有机质、微生物的高度异质性,植物残体向土壤有机质的转化和稳定机理尚不十分明确。本文介绍并讨论了近年来关于植物残体向土壤有机质转化相关研究的新发现,探讨了微生物源和植物源有机质对土壤有机质的贡献,概述了土壤有机质形成的微生物驱动机制,并综述了植物残体输入后土壤有机质稳定性的相关研究,最后对该研究领域未来的发展进行展望,以期能够为科学地提高土壤的固碳能力提供参考。     

Importance of rhizodeposition in the coupling of plant and microbial productivity

Plant roots influence the biological, chemical and physical properties of rhizosphere soil. These effects are a consequence of their growth, their activity and the exudation of organic compounds from them. In natural ecosystems, the linkages between inputs of carbon from plants and microbial activity driven by these inputs are central to our understanding of nutrient cycling in soil and the productivity of these systems. This coupling of plant and microbial productivity is also of increasing importance in agriculture, where the shift towards low‐input systems increases the dependence of plant production on nutrient cycling, as opposed to fertilizers. This review considers the processes by which plants can influence the cycling of nutrients in soil, and in particular the importance of organic inputs from roots in driving microbially mediated transformations of N. This coupling of plant inputs to the functioning of the microbial community is beneficial for acquisition of N by plants, particularly in low‐input systems. This occurs through stimulation of microbes that produce exoenzymes that degrade organic matter, and by promoting cycling of N immobilized in the microbial biomass via predation by protozoa. Also, plants increase the cycling of N by changes in exudation in response to nitrogen supply around roots, and in response to browsing by herbivores. Plants can release compounds in exudates that directly affect the expression of genes in microbes, and this may be an important way of controlling their function to the benefit of the plant.     

The “soil microbial loop” is not always needed to explain protozoan stimulation of plants

Protozoa stimulate plant growth, but we do not completely understand the underlying mechanisms, and different hypotheses seek to explain this phenomenon. To test these hypotheses, we grew the grass Yorkshire fog (Holcus lanatus) in pots with soil, which contained either (1) no organisms but bacteria – or (2) bacteria and protozoa. Half of the pots received a glucose treatment so as to mimic an additional root exudation. We measured plant growth and plant nitrogen uptake, along with various microbial pools and processes that support plant growth. Protozoan presence significantly enhanced soil nitrogen mineralization, plant nitrogen uptake from organic nitrogen sources, plant nitrogen content, and plant growth. By contrast, we found no evidence that glucose addition, mimicking root exudation, increased soil nitrogen availability and plant nitrogen uptake. Moreover, although protozoan presence affected bacterial community structure, it did not affect the proportion of IAA-producing bacteria in the community or plant root morphology. These results refute the “soil microbial loop” hypotheses, which suggest that protozoan stimulation of plant growth results from complex interactions between plant roots, bacteria and protozoa. Our experiment thus favours the simple explanation that increased nitrogen availability is the key factor behind the positive protozoan effect on plant growth. To exploit natural resources in an efficient and environmentally friendly way, we need to understand in detail the functioning of ecosystems. This study stresses that to achieve this, it is still urgent, besides investigating intricate food-web and signal compound interactions, also to focus on the basic stoichiometric and energetic aspects of organisms.     

Effect of temperature on below-ground N-dynamics in a weedy model ecosystem at ambient and elevated atmospheric CO2 levels

Model multispecies terrestrial communities composed of four trophic levels (plants, herbivores, parasitoids, decomposers) were established in the Ecotron controlled environment facility. Two experimental runs enabled us to investigate the effects of enhanced temperature on below-ground microbial processes (N-mineralisation, urease, arginine deaminase, protease activity and potential denitrification) in both ambient and elevated (ambient +200 ppm) CO₂ atmospheres.The enzyme activities involved in nitrogen cycling showed weak responses to elevated temperature in both experimental runs. In the Ambient CO₂ Run, protease and arginine deaminase values tended to be lower in elevated temperature; on the other hand, N-mineralisation, urease and denitrification enzyme activity (DEA) were higher. In the Elevated CO₂ Run, all microbial variables showed higher activities at elevated temperature, although only the results for DEA and arginine deaminase were statistically significant. The interaction between higher temperature and elevated CO₂ weakly affected root growth and tissue C:N ratio, limiting feedbacks into the microbial community.Besides temperature and CO₂, substrate availability, water stress and successional development regulated the response of the soil microbes. The supply of organic carbon and nitrogen in the soil allowed plant growth and maintenance of the microbial population. Nitrogen competition between vegetation and microbes restricted net microbial growth. The increase of dissolved organic carbon (DOC) at higher CO₂ and temperature levels significantly favoured DEA. The high water regime in the soil also favoured DEA and inhibited oxidation of organic compounds, as indicated by low levels of enzyme activity. Additionally, water stress decreased rooting density in the soil; this resulted in negative feedback into microbial processes. We conclude that water stress and soil nitrogen deficiency caused an early levelling-off of both microbial population growth and activity rates during the early part of the model ecosystem's development.     

氮输入对森林土壤有机碳截存与损耗过程的影响

大气氮沉降对受氮限制的陆地生态系统碳截存/损耗的机理尚不清楚,尤其是对土壤有机碳(SOC)的输入、转化和输出过程的认识明显不足。本文论述了外源性氮素(氮沉降、人为增氮)对凋落物分解、土壤有机碳各组分周转的影响,以及土壤呼吸各组分(根系自养呼吸、根际微生物呼吸和SOM分解)对增氮的响应等领域的最新研究进展,指出了在上述研究领域中存在的问题,并提出拟解决的途径以及未来的可能研究方向,以期为该领域的研究提供参考。