重金属污染土壤植物修复中的微生物功能研究进展

综述了国内外在重金属污染土壤植物-微生物联合修复领域的研究报道,总结了近5年的研究实例。植物-微生物联合修复体系具有生物固定与生物去除土壤重金属的两种功能,根际微生物可以菌根、内生菌等方式与根系形成联合体,通过增强植物抗性和优化根际环境,促进根系发展,增强植物吸收和向上转运重金属的能力。建立植物-微生物联合修复体系,可充分发挥植物与微生物作用功能的优势,提高污染土壤的修复效率。增强植物修复体系中微生物功能的重点是深入研究根际微生物、根系和介质载体三者之间复合功能,结合污染土壤类型与植物群落配置的特点筛选扩繁高效菌种与菌群。     

微生物在镉污染土壤修复中的应用及其作用机理

土壤中镉（Cd）含量的超标导致了土壤生态系统的恶性发展,微生物作为土壤中的常见组分之一在缓解土壤镉污染中展现出巨大潜力。本文总结了微生物、微生物-植物和微生物-生物炭在镉污染土壤修复中的应用并阐述了相关的作用机理。芽孢杆菌（Bacillus）、不动杆菌（Acinetobacter）、荧光假单胞菌（Pseudomonas fluorescence）、丛枝菌根真菌（arbuscular mycorrhizal fungi,AMF）等微生物可以通过吸附、矿化、沉淀、溶解等方式改变镉的生物有效性,从而达到缓解镉污染的目的。pH值、温度、微生物生物量、镉初始浓度以及时间等对微生物降低镉的生物有效性方面有着显著的影响。假单胞菌、伯克霍尔德菌（Burkholderia）、黄杆菌（flavobacterium）等微生物可以通过促生、活化等作用促进超富集植物对Cd²⁺的吸收。生物炭作为一种土壤改良剂,其独有的理化性质可以作为微生物的庇护所。微生物-生物炭联合使用与单用生物炭相比可以进一步促进镉的残渣态的增加,降低土壤中有效态的比例。     

生物炭对土壤有机碳矿化的激发效应及其机理研究进展

近年来由于生物炭具有碳素稳定性强和孔隙结构发达等特性,其在土壤固碳减排方面的作用研究受到广泛关注.然而当生物炭进入土壤环境后最终是增加土壤碳的储存还是促进土壤碳的排放?目前学术界对该问题仍存在争议.生物炭对土壤有机碳的激发效应及其机理研究有待进一步深入开展.本文在分析生物炭自身碳素组分和稳定性、孔隙结构及表面形态特征的基础上,综述了添加生物炭对土壤本底有机碳矿化产生激发效应的研究进展,分别阐述了产生正激发和负激发效应(即促进和抑制矿化)的机制机理,认为正激发效应主要是基于生物炭促进土壤微生物活性增强、生物炭中易分解组分的优先矿化以及由此引发的土壤微生物的共代谢作用,而负激发效应主要是基于生物炭内部孔隙结构和外表面对土壤有机质的包封作用和吸附保护作用、生物炭促进土壤有机-无机复合体形成的稳定化作用、生物炭对土壤微生物及其酶活性的抑制作用.最后对今后相关研究方向进行了展望,以期为生物炭在土壤固碳减排方面的应用提供理论依据.     

间套作控制作物病害的机理研究进展

合理间套作是抑制植物病害流行的天然屏障,利用间套作持续控制作物病害是国内外近年来的研究热点。目前,有关间套作的研究主要集中在田间作物搭配模式、光热和养分资源高效利用、病害控制效果及产量优势等方面。然而,有关间套作控病机理尚缺乏系统总结。本文首先综述了间套作对气传病害和土传病害的控制效果;其次,从寄主作物抗性、病原菌和环境(土壤及田间小气候)三方面阐述间套作控制病害的机理,主要为:(1)合理间套作促进养分吸收利用,改善寄主作物的生理生化特性,进而提高寄主作物的抗病性;(2)间套作一方面增加地上部作物多样性,形成物理屏障阻挡病原菌的传播,另一方面增加地下部根系分泌物的多样性,对病原菌进行化感抑制,降低病原菌的存活与侵染;(3)间套作改变田间小气候(田间湿度、温度和通风等)及土壤微生态环境(微生物区系、群落结构和土壤酶活性)而增强间套作的控病效果。最后,讨论了当前间套作与病害控制研究方法的局限性,并展望了间套作控制病害的未来研究方向。     

生物质炭生物与非生物氧化特性研究进展

生物质炭是由植物生物质热解炭化产生的一类高度芳香化难熔性固态物质。生物质热解炭化还田能否成为人类应对全球气候变化的重要途径直接取决于其在土壤生态系统中的稳定性。生物质炭稳定性的研究对科学计算和评估土壤生态系统生物质炭输入的碳固持与减排作用具有重要现实意义。重点概述了土壤生态系统生物质炭生物与非生物氧化特性、影响因素及其机理研究进展,并对生物质炭在土壤环境中的稳定性预测模型研究进行了分析。在此基础上,今后需针对不同类型旱地土壤生态系统和不同类型稻田土壤生态系统生物质炭稳定性及其机理开展研究,并进一步开展土壤生态系统生物质炭稳定性预测模型研究。     

根系分泌物介导的植物对土传病害的抗性机制

根系分泌物作为地下防御物质越来越受到关注。近年来,研究逐渐揭示了植物在病原胁迫下根系分泌物的表达特征及其在植物抗病性中的作用,一些由根分泌物介导的抗性调节机制也已被模拟。鉴于土传病害造成的损失日益增加,了解根系分泌物如何抵抗各种病原菌已成为研究热点。本文全面综述了土壤病原胁迫下根系分泌物介导的植物抗性机制,研究病原胁迫下根系分泌物的表达特征,根系分泌物在植物抗病过程中的作用,以及抗性根介导的分泌物和植物抗性的功能。讨论了当前植物病害条件下根系分泌物对植物抗性的影响,旨在为今后土传病害抗性机制的研究提供思路。     

溶磷微生物在钝化和植物修复重金属污染土壤中的作用

钝化和植物修复是重金属污染土壤修复的重要技术手段,而溶磷微生物可进一步增强钝化和植物修复重金属污染土壤的作用。介绍了钝化和植物修复重金属污染土壤的基本原理,总结了溶磷微生物对土壤中难溶性磷酸盐的溶解、利用磷酸盐钝化修复重金属污染土壤、溶磷微生物对磷酸盐钝化修复的强化以及溶磷微生物强化植物修复重金属污染土壤的研究进展,探讨了溶磷微生物对重金属的抗性及其溶磷机理、溶磷微生物对磷酸盐钝化修复重金属污染土壤的强化作用机理以及溶磷微生物强化植物修复重金属污染土壤的作用机理。旨在为生物修复重金属污染土壤研究提供一定的理论依据和技术支撑。     

硼抑制植物病害作用及机制的研究进展

硼不仅是植物生长必需的营养元素,也可减少和降低植物病害的发生。本文总结了硼抑制植物病害发生的作用机制：参与植物细胞壁和膜形成,增强植物细胞稳定性;诱导植物产生系统获得性抗性;诱导植物细胞产生适量的酚类和过氧化物;抑制病原菌菌丝生长,扭曲病原菌菌丝结构形态;破坏病原茵活性氧代谢系统,加快膜脂过氧化作用;与生防菌协同控制植物病害发生等。另外,还探讨了矿质元素防治植物病害可能存在的问题以及应用前景,以期为进一步的研究提供参考。     

微生物次级代谢产物抗辣椒疫霉的研究进展CSCD

辣椒疫霉(Phytophthora capsici)是一种破坏性极强的蔬菜作物病原菌,会使植物患疫病,已对农业生产造成巨大的经济损失。微生物次级代谢产物可通过破坏细胞膜通透性、干扰蛋白质合成以及诱导植物产生抗性等机制来抑制辣椒疫霉,在防治辣椒疫霉和其他植物病原菌中发挥着重要作用。微生物源次级代谢产物如吩嗪-1-羧酸是我国自主创制的绿色杀菌剂申嗪霉素(shenqinmycin)的主要成分,对包括辣椒疫病在内的多种植物病害有良好的防治效果。因此,微生物次级代谢产物的应用是生物防治中控制植物病害的有效手段,也是实现农业绿色发展的有效策略。本文以微生物类型(细菌、放线菌和真菌)为主线,简要综述了近二十年来94种具有抗辣椒疫霉活性的微生物次级代谢产物的来源、抗菌效果和部分次级代谢产物的抗菌机理,以期为微生物源次级代谢产物抗辣椒疫霉的研究与开发提供参考。     

禾草内生真菌对其它微生物的影响研究进展

禾草内生真菌在宿主植物的茎叶等地上组织中普遍存在,不仅能够提高禾草对生物与非生物逆境的抗性,而且能够对周围环境中的不同微生物类群产生影响。主要总结了禾草Neotyphodium/Epichlo内生真菌对病原真菌、丛枝菌根真菌和土壤微生物的影响及其作用机理。发现禾草内生真菌普遍存在对病原真菌的抑制作用,而对丛枝菌根真菌存在不对称的竞争作用,且因种类而异。禾草内生真菌对土壤微生物群落的作用则会随着土壤类型和时间等外界因素发生变化。禾草内生真菌对不同类群微生物的影响机制主要包括:通过生态位竞争、抑菌物质分泌、诱导抗病性等对病原真菌造成影响;通过根系化学物质释放、营养元素调节、侵染条件差异等对丛枝菌根真菌造成影响;通过根际沉积物和凋落物等对土壤微生物群落造成影响。禾草内生真菌产生的生物碱能提高宿主植物对包括昆虫在内草食动物采食的抗性,影响病原菌的侵入、定殖和扩展;根组织分泌物中包含次生代谢产物能够抑制菌根真菌、土传病原真菌及其它土壤微生物的侵染与群落组成;也可能通过次生代谢物影响禾草的其它抗性。因此,禾草内生真菌在植物-微生物系统中的作用应该给予更多的关注和深入研究。     

Comparative efficiency of wheat straw and sugarcane bagasse biochar reduces the cadmium bioavailability to spinach and enhances the microbial activity in contaminated soil

Abstract

Biochar is considered a novel soil amendment for cadmium (Cd) stabilization in contaminated soils. A pot experiment was conducted to examine the efficiency of wheat straw and sugarcane bagasse induced biochar on Cd mobility in soil and its bioavailability to spinach in contaminated soil. Soil pH, Cd contents in plant tissues and microbial biomass were examined. Results showed that Cd was significantly decreased by 30.95% and 20.83% with wheat straw and sugarcane bagasse biochar at 2% application rate respectively, relative to the control. Similarly, Cd contents were decreased in plants shoots by 15.41 and 14.33%, while in roots by 48.3 and 35.54%, when wheat straw and sugarcane biochar were added at 2% application rate respectively. Moreover, soil microbial biomass was significantly increased with the application of all biochar types and their applications rates. Finally, wheat straw biochar at 2% application rate can be considered as an effective approach for Cd stabilization in contaminated soils.     

生物炭对温室黄瓜不同连作年限土壤养分和微生物群落多样性的影响

以温室黄瓜连作6年和10年土壤添加质量比为5%生物炭为处理,以不添加生物炭为对照,采用桶栽的方法,研究了生物炭对不同年限连作土壤养分和微生物群落多样性的影响.结果表明: 与连作土壤相比,生物炭处理的连作6年土壤的黄瓜单株产量提高11.4%,连作10年土壤产量提高62.8%.施入生物炭显著降低了2种连作土壤容重,显著提高了有机质、速效磷含量、阳离子交换量(CEC)和pH;显著提高了土壤细菌数量和细菌/真菌,降低了真菌和尖孢镰刀菌数量,使土壤类型由真菌型向细菌型转变,尤其对连作10年土壤作用最为明显,土壤细菌和细菌/真菌分别是未处理的2.00和3.64倍,真菌和尖孢镰刀菌数量分别是未处理的54.8%和55.9%.土壤微生物群落碳源利用分析表明,10年连作土壤施入生物炭可显著提高土壤微生物活性、Shannon指数和均匀度指数,分别是未处理的1.50、2.14和1.31倍,同时显著提高了土壤微生物对糖类、氨基酸类、酚酸类和胺类碳源的利用强度,分别是未处理的1.62、1.81、1.74和1.93倍.相关性分析表明,土壤容重、速效磷含量、CEC和pH 4个指标对微生物群落变化的影响较显著.综上,生物炭通过对连作土壤理化性质及土壤微生物生态系统的改善,优化了黄瓜根区环境,促进了黄瓜产量的提高,缓解了温室黄瓜连作障碍.     

不同磷水平配施生物炭对土壤磷有效性

生物炭在提高土壤磷素有效性及促进作物生长方面具有显著作用,但其效果因土壤类型不同存在较大差异。试验以赤红壤(pH 4.91)和褐土(pH 7.24)为供试土壤,设置3种磷肥水平(0、30、90 kg P·hm^-2,分别以不施磷、低磷、高磷表示)配施稻秆生物炭(0、4%)的大豆盆栽试验,研究了不同磷水平下配施生物炭对土壤磷有效性、磷酸单酯酶活性和植株磷吸收的影响。结果表明: 不同磷水平配施生物炭显著提高了两种土壤的速效磷和全磷含量,且低磷水平添加生物炭处理速效磷增幅最大,在赤红壤和褐土的增幅分别为192.6%和237.1%。与低磷相比,赤红壤中低磷配施生物炭处理的碱性磷酸单酯酶活性显著增加78.9%,活性有机磷含量降低39.3%,同时显著促进了植株生长与磷吸收;生物炭添加显著降低了褐土活性有机磷含量,但不同处理对土壤磷酸单酯酶活性和植株生长无显著影响。土壤活性有机磷含量与速效磷含量均呈显著负相关。综上,生物炭对土壤磷有效性的作用因土壤类型和磷肥水平差异而不同,其在赤红壤上对植株生长和磷吸收的促进效应强于褐土,且在低磷条件下效果更佳。本研究为生物炭在减施磷肥和促进大豆磷吸收,特别是在赤红壤上的应用提供了科学依据。     

Biostimulation potential of biochar for remediating the crude oil contaminated soil and plant growth

Crude oil contamination is a serious environmental threat to soil and plants growing in it. Biochar has the potential of biostimulation for remediation of crude oil-contaminated soil. Therefore, the current research was designed to analyze the bio-stimulatory impact of biochar for remediating the crude oil contaminated soil (10%, and 15%), and growth of maize under glasshouse conditions. Biochar was produced by pyrolysis of Australian pines at 350 °C. Soil incubations were done for 20 days. The results of soil analysis showed that the crude oil degradation efficiency of biochar was 34%. The soil enzymatic activities had shown 38.5% increase in fluorescein diacetate (FDA) hydrolysis and 55.6% increase in dehydrogenase activity in soil incubated with biochar in comparison to control. The soil microbial diversity was improved to 41% in biochar treated soil with respect to untreated one, while microbial respiration rate had shown a 33.67% increase in soil incubated with biochar with respect to control under oil stress. Gas Chromatography Mass spectrometry (GC-MS) analysis had shown the high content of low molecular weight hydrocarbons (C₉-C₁₃) in the soil incubated with biochar in comparison to untreated soil. Biochar showed a significant increase in fresh and dry biomass (25%, 14.61%), leaf area (10%), total chlorophyll (11%), water potential (21.6%), osmotic potential (21%), and membrane stability index (12.7%). Moreover, biochar treatment showed a higher increase in the contents of proline (29%), total amino acids (18%), soluble sugars (30.4%), and antioxidant enzymes like superoxide dismutase (16.5%), catalase (11%), and peroxidase (12%). Overall, the results of the present study suggest the bio-stimulating potential of biochar for degradation of hydrocarbons in crude oil contaminated soil and their growth-stimulating effects on maize.     

土壤呼吸对秸秆与秸秆生物炭还田的响应及其微生物机制

土壤呼吸释放CO_2是温室气体排放的重要途径之一,减少土地利用中温室气体排放、增强土壤碳汇聚能力对于减缓全球温室效应具有重要意义。生物炭具有改善土壤理化性质、增加作物产量、调节土壤微生物性质等特性。本研究采用室外盆栽的方式,以地肤草为目标植物,研究了芦苇、水稻、互花米草三种农林秸秆及其秸秆生物炭还田对土壤的改良效应,以及对土壤呼吸的影响及其微生物机制。结果表明:秸秆及其秸秆生物炭均可改善土壤肥力,促进植物生长,且生物炭改良效果略好于秸秆直接还田。但秸秆生物炭还田的土壤呼吸显著低于秸秆直接还田,其中芦苇生物炭最低。秸秆直接还田可促进土壤β-糖苷酶、脱氢酶和活性微生物量等微生物活性指标,从而促进土壤呼吸,增加土壤CO_2的释放,而生物炭还田对土壤微生物活性无显著的促进作用,反而有一定的抑制作用,这可能是由于生物炭中易降解有机物含量很低,可降解性较低的缘故。     

生物炭对农田土壤微生物生态的影响研究进展

生物炭作为新型土壤改良剂在国内外环境科学等领域受到广泛的关注.关于生物炭对土壤理化性质的改良研究较早,目前虽然已深入到土壤微生物生态的领域,但是大多数将土壤理化性质与土壤微生物生态分开考虑,缺乏对二者相互作用的系统评述.本文总结了施用生物炭后土壤理化性质的改变与土壤微生物群落变化之间的相互关系:生物炭不仅能够提高土壤pH值、增强土壤的持水能力、增加土壤有机质等,而且会影响土壤微生物的群落结构、改变细菌和真菌的丰度;施用生物炭后,土壤环境和土壤微生物之间互相影响互相制约,共同促进了土壤微生物生态系统的改良.本文旨在为生物炭改良农田土壤微生态的深入研究提供新的思路,从生态系统的角度促进生物炭环境效应影响的研究,使生物炭的应用更具有科学性和有效性,并对生物炭在相关领域的应用进行了展望.     

Biochar as Electron Acceptor for Microbial Extracellular Respiration

Biochar is a charred carbonaceous material that has recently been identified to provide many potential environmental and agricultural applications. Biochar amendments are shown to effectively improve the quality of soil and increase soil microbial biomass. However, the interactions between biochar and microorganisms and the mechanisms through which biochar influences soil microbial growth and activities remain unclear. In this study, we investigated the potential for biochar to function as an electron acceptor for microbial extracellular respiration and growth. Anaerobic incubation of Geobacter sulfurreducens revealed that biochar was used as a sole terminal electron acceptor, as evidenced by a 31-fold increase of biomass and gradual increase in reducing equivalents of biochar and the consumption of acetate after 15 d. An electron stoichiometry analysis showed that 58.7% of the electrons released from acetate oxidation could be recovered in biochar, which was comparable to that of humic substances (44.8%). The finding that biochar participates in microbial extracellular respiration may have important environmental implications considering the widespread existence of both extracellular-respiring microorganisms and black carbon in the environment.     

Soil and greenhouse gas responses to biochar additions in a temperate hardwood forest

Biochar additions can improve soil fertility and sequester carbon, but biochar effects have been investigated primarily in agricultural systems. Biochar from spruce and maple sawdust feedstocks (with and without inorganic phosphorus in a factorial design) were added to plots in a commercially managed temperate hardwood forest stand in central Ontario, Canada; treatments were applied as a top‐dressing immediately prior to fall leaf abscission in September 2011. Forests in this region have acidic, sandy soils, and due to nitrogen deposition may exhibit phosphorus, calcium, and magnesium limitation. To investigate short‐term impacts of biochar application on soil nutrient supply and greenhouse gas fluxes as compared to phosphorus fertilization, data were collected over the first year after treatment application; linear mixed models were used to analyze data. Two to six weeks after treatment application, there were higher concentrations of potassium in spruce and maple biochar plots, and phosphorus in spruce biochar plots, as compared to the control treatment. There were higher concentrations of calcium, magnesium, and phosphorus in the phosphorus plots. In the following spring and summer (9–12 months after treatment application), there were higher soil calcium concentrations in maple biochar plots, and phosphorus plots still had higher soil phosphorus concentrations than control plots. No treatment effects on fluxes of carbon dioxide, methane, or nitrous oxide were detected in the field; however, laboratory incubations after 12 months showed higher microbial respiration in soils from maple biochar plots as compared to spruce biochar, despite no effect on microbial biomass. The results suggest that the most important short‐term impact of biochar additions in this system is the increased supply of the limiting plant nutrients phosphorus and calcium. We expect that larger changes in mineral soil physical and chemical properties will occur when the surface‐applied biochar becomes incorporated into the soil after a few years.     

Functional response of the soil microbial community to biochar applications

Biochar has the potential to mitigate the impacts of climate change and soil degradation by simultaneously sequestering C in soil and improving soil quality. However, the mechanism of biochar's effect on soil microbial communities remains unclear. Therefore, we conducted a global meta‐analysis, where we collected 2,110 paired observations from 107 published papers and used structural equation modeling (SEM) to analyze the effects of biochar on microbial community structure and function. Our result indicated that arbuscular mycorrhizal fungal abundance, microbial biomass C, and functional richness increased with biochar addition regardless of loads, time since application, and experiment types. Results from mixed linear model analysis suggested that soil respiration and actinomycetes (ACT) abundance decreased with biochar application. With the increase of soil pH, the effect of biochar on fungal abundance and C metabolic ability was lessened. Higher biochar pH associated with higher pyrolysis temperatures reduced the abundance of bacteria, fungi, ACT, and soil microbes feeding on miscellaneous C from Biolog Eco‐plate experiments. SEM that examined the effect of biochar properties, load, and soil properties on microbial community indicated that fungal abundance was the dominant factor affecting the response of the bacterial abundance to biochar. The response of bacterial abundance to biochar addition was soil dependent, whereas fungi abundance was mostly related to biochar load and pyrolysis temperature. Based on soil conditions, controlling biochar load and production conditions would be a direct way to regulate the effect of biochar application on soil microbial function and increase the capacity to sequester C.     

Biochar stimulates the decomposition of simple organic matter and suppresses the decomposition of complex organic matter in a sandy loam soil

Incorporating crop residues and biochar has received increasing attention as tools to mitigate atmospheric carbon dioxide (CO₂) emissions and promote soil carbon (C) sequestration. However, direct comparisons between biochar, torrefied biomass, and straw on both labile and recalcitrant soil organic matter (SOM) remain poorly understood. In this study, we explored the impact of biochars produced at different temperatures and torrefied biomass on the simple C substrates (glucose, amino acids), plant residues (Lolium perenne L.), and native SOM breakdown in soil using a ¹⁴C labeling approach. Torrefied biomass and biochars produced from wheat straw at four contrasting pyrolysis temperatures (250, 350, 450, and 550 °C) were incorporated into a sandy loam soil and their impact on C turnover compared to an unamended soil or one amended with unprocessed straw. Biochar, torrefied biomass, and straw application induced a shift in the soil microbial community size, activity, and structure with the greatest effects in the straw‐amended soil. In addition, they also resulted in changes in microbial carbon use efficiency (CUE) leading to more substrate C being partitioned into catabolic processes. While overall the biochar, torrefied biomass, and straw addition increased soil respiration, it reduced the turnover rate of the simple C substrates, plant residues, and native SOM and had no appreciable effect on the turnover rate of the microbial biomass. The negative SOM priming was positively correlated with biochar production temperature. We therefore ascribe the increase in soil CO₂ efflux to biochar‐derived C rather than that originating from SOM. In conclusion, the SOM priming magnitude is strongly influenced by both the soil organic C quality and the biochar properties. In comparison with straw, biochar has the greatest potential to promote soil C storage. However, straw and torrefied biomass may have other cobenefits which may make them more suitable as a CO₂ abatement strategy.