纳米Fe3O4对生菜生长及土壤细菌群落结构的影响

纳米Fe₃O₄的广泛应用增加了其暴露到农田环境的可能性,因此亟待研究纳米Fe₃O₄对农业生态环境的影响.本研究采用盆栽试验方式,研究不同浓度纳米Fe₃O₄颗粒(1、10、100 mg·kg^-1)对生菜生长及土壤细菌群落的影响,并与相应浓度的普通Fe₃O₄处理进行对比.通过测定植物光合速率常数、植株Fe含量来评价植物生长;采用高通量测序技术研究土壤细菌群落结构及组成.结果表明: 不同浓度纳米Fe₃O₄的影响不同.低浓度纳米Fe₃O₄能提高植物生物量,增强植物叶片光合速率,增加土壤中黄单胞菌目的相对丰度,降低蓝细菌、鞘脂杆菌纲的相对丰度,但对群落多样性指数影响不显著.高浓度纳米Fe₃O₄抑制作物生长,提高植株中Fe积累及土壤电导率,降低细菌群落系统发育多样性,降低黄单胞菌目、鞘脂杆菌纲相对丰度,增加蓝细菌相对丰度.此外,一些土壤功能微生物对纳米Fe₃O₄及普通Fe₃O₄处理的响应也存在差异,说明不同粒径及浓度的Fe₃O₄均会对土壤微生物群落产生影响,并可能影响地上部分植物性状.因此,在评估纳米颗粒的生物学效应时需较多关注土壤微生物.     

磁性纳米金属对盐单胞菌生长特性及胞内Ectoine的积聚影响

为了提高野生型坎帕尼亚盐单胞菌株(Halomonas campaniensis sp. XH26)胞内Ectoine的积聚量,选用磁性纳米金属颗粒(Fe₃O₄ NPs),采用单因素实验、Plackett-Burman设计和响应面法分析菌株胞内的Ectoine积聚量和菌株生长量,并探讨Fe₃O₄ NPs应用于盐单胞菌发酵的可行性。单因素分析表明Fe₃O₄ NPs能促进菌株生长和促进菌株Ectoine的积聚,菌株生长对数期是最佳的Fe₃O₄ NPs添加时期。Plackett-Burman及响应面分析表明：优化条件下(0.05 g/L Fe₃O₄ NPs、1.53 mol/LNaCl和0.03 mol/LL-谷氨酸钠),摇瓶发酵Ectoine的积聚量可达640.28 mg/L,与野生菌株(391.35 mg/L)相比提高了63.61%。透射电镜显示Fe₃...     

蒙古栎叶片及其土壤碳、氮同位素自然丰度对大气CO2浓度升高的响应

大气CO₂浓度升高对土壤氮素转化过程产生重要影响,研究其变化有助于更好地预测陆地生态系统的固碳潜力.氮同位素自然丰度作为生态系统氮素循环过程的综合指标能够有效地指示CO₂浓度升高对土壤氮素转化过程的影响.本研究采用开顶箱CO₂ 熏蒸法研究连续10年的大气CO₂ 浓度升高对我国东北地区蒙古栎及其土壤和微生物生物量碳、氮同位素自然丰度的影响.结果表明: 大气CO₂浓度升高改变了土壤氮循环过程,增加了土壤微生物和植物叶片δ¹⁵N;促进了富¹³C土壤有机碳分解,中和了贫¹³C植物光合碳输入的效果,导致土壤可溶性有机碳和微生物碳δ¹³C在CO₂升高条件下没有发生显著变化.这些结果表明,CO₂浓度升高很可能促进了土壤有机质矿化过程,并加剧了系统氮限制的状态.     

基于HA修饰的CoFe2O4-TiO2纳米颗粒体外PDT灭活HL60细胞的试验研究

通过水热法和表面修饰法制备了以Co Fe₂O₄为内核、Ti O₂为外壳、用透明质酸修饰的HA@Co Fe₂O₄-Ti O₂。利用场发射扫描电子显微镜(SEM)成像、能谱分析(EDS)、X射线衍射(XRD)、X射线光电子谱(XPS)、紫外-可见吸收光谱(UV-Vis)以及傅里叶变换红外光谱(FTIR)对复合纳米颗粒的理化性质进行表征。用细胞计数试剂(CCK-8)法研究HA@Co Fe₂O₄-Ti O₂复合纳米颗粒在暗室条件下对白血病HL60细胞的毒性，以及在光照条件下的光动力疗法(PDT)灭活效果。结合复合纳米颗粒的荧光光谱(FS)、细胞内活性氧(ROS)产量和摄取纳米颗粒水平分析，初步探究Co Fe₂O₄和透明质酸与Ti O₂结合影响PDT灭活HL60细胞的作用机制。试验结果表明，HA@Co Fe₂O     

模拟增温对青海湖鸟岛土壤微生物的影响

【背景】土壤微生物对其生存的微环境变化极为敏感,鸟岛作为湖滨湿地,对气候变化具有敏感性,但目前关于青海湖鸟岛的土壤微生物鲜有研究。【目的】探究气候变暖后青海湖鸟岛土壤微生物群落特征的变化。【方法】利用开顶箱模拟增温,通过高通量测序方法了解温度升高后土壤细菌及真菌的群落结构以及多样性的变化情况。【结果】温度的升高并未改变青海湖鸟岛土壤微生物的优势菌群,细菌优势菌群为变形菌门和酸杆菌门;真菌优势菌门为子囊菌门,优势菌纲为座囊菌纲。但增温改变了土壤微生物的群落结构,显著升高了拟杆菌门、蓝细菌门、Patescibacteria及球囊菌纲的相对丰度,显著降低了锤舌菌纲的相对丰度。土壤微生物群落的多样性指数也发生了变化,温度上升后微生物的ACE指数及Chao1指数均降低,细菌的Simpson指数及真菌的Shannon指数降低。【结论】青海湖鸟岛土壤微生物对温度升高的响应明显,增温改变了土壤细菌拟杆菌门、蓝细菌门、Patescibacteria的相对丰度及真菌的球囊菌纲、锤舌菌纲的相对丰度,降低了土壤微生物的多样性。     

基于稳定碳同位素技术研究大气CO2浓度升高对植物-土壤系统碳循环的影响

大气CO₂浓度升高影响植物光合作用过程和生物量积累,改变植物地上和地下生物量的动态分配.土壤有机质的形成和周转依赖于植物组分的输入,因此,CO₂浓度升高所造成的植物生理和代谢的变化对土壤碳库收支平衡具有重要影响.采用稳定碳同位素(¹³C)技术研究土壤-植物系统的碳循环可阐明大气CO₂浓度升高条件下光合碳在植物各器官的分配特征和时间动态,明确光合碳在土壤中的积累、分解与迁移转化过程以及对土壤有机碳库周转的影响.本文综述了基于¹³C自然丰度法或¹³C示踪技术研究大气CO₂浓度升高对土壤-植物系统碳循环的影响,主要包括:1)对植物光合作用的同位素分馏的影响;2)对植物光合碳(新碳)分配动态的影响;3)对土壤有机碳新老碳库动态以及微生物转化过程的影响.明确上述过程及其调控机制可为预测CO₂浓度升高对陆地生态系统碳循环及源汇效应的长期影响奠定基础.     

增施CO2对植物修复土壤DEHP污染的影响

修复效率低一直是植物修复技术需要解决的关键问题之一.基于我国的CO₂减排压力和CO₂对植物生长的必要性,选择C3植物绿豆和C4植物玉米作为修复植物,以DEHP为目标污染物,探索增施CO₂对植物修复土壤DEHP污染的影响.结果表明: DEHP对两种植物生长和根际微环境都产生了抑制性影响.增施CO₂后,两种植物地上干质量显著增加,叶片SOD酶活性明显下降,根际土壤碱性磷酸酶活性增加,根际微生物群落结构改变,根际耐DEHP胁迫微生物数量增加,表明增施CO₂对促进植物生长、增强植物抗DEHP胁迫能力、改善根际微环境有积极作用.增施CO₂还促进了两种植物对DEHP的吸收,特别是植物地下部分.这些共同作用导致增施CO₂后的两种植物根际DEHP残留浓度明显下降,土壤污染植物修复效率提高.整体上看,增施CO₂对C3植物绿豆的影响明显大于C4植物玉米.可以将增施CO₂ 作为强化植物修复过程的措施之一.     

超小粒径的纳米Ag协同Cu基铁氧体复合材料的制备及其对金黄色葡萄球菌抑菌机制研究

超小粒径的纳米银(Ag)可通过细菌细胞壁,进入细菌内环境后对细菌造成不可逆损伤,因而具备较强的抑菌活性.但是超小粒径的纳米Ag易团聚,且单独使用时毒性较强,这些缺点限制了其应用.本研究利用生物相容性较高的Fe和Cu化合物制备了Fe₃O₄/Cu/CuO载体(F),将介孔(mesoporous, m)ZrO₂包覆在F上合成纳米Fe₃O₄/Cu/Cu O@mZrO2(FZ),然后将～3 nm的Ag负载在其表面,制备出核壳型纳米Fe₃O₄/Cu/CuO@mZrO₂@Ag(FZA)复合材料. FZA不仅可解决纳米Ag团聚的问题,而且通过Fenton反应缓释的ROS(·OH)和Cu²⁺可协同纳米Ag具备较强的抑菌性能.研究结果表明, FZA在40 min,150μg/mL时对金黄色葡萄球菌(S. aureus)和耐甲氧西林金黄色葡萄球菌(T-S. aureus)的抑菌率为99.99%,可有效破坏细菌细胞...     

开放式空气CO2浓度升高与作物/杂草的竞争关系

CO₂浓度升高对植物的光合作用、呼吸作用和水分利用等生理过程产生直接影响,进而影响植物的生长和繁殖.CO₂浓度升高对于具有C₃光合途径的植物较具C₄光合途径的植物更为有益.由于许多重要的杂草是C₄植物,而许多重要的作物是C₃植物,CO₂浓度升高对杂草/作物的相互关系将有重要影响.本文就全球CO₂浓度升高和气候变化对杂草/作物之间竞争关系影响进行综述,同时针对目前研究现状和可持续农业的需要,提出CO₂浓度升高条件下杂草/作物之间竞争关系及未来农田杂草治理方面理论与实践中有待解决的问题.     

不同生境中桂花和夹竹桃叶际细菌的群落结构

植物叶际微生物多样性是目前植物-微生物关系研究的热点之一,但影响叶际微生物群落结构的主要因素目前还存在很大争议.本研究以生长在3处生境的桂花和夹竹桃为对象,基于高通量测序技术,分析2种植物叶际细菌的群落结构,探讨影响植物叶际细菌群落结构的主要因素.结果表明:来自3处生境的2种植物叶际细菌多样性无显著差异,构成叶际细菌群落的优势门主要包括放线菌门、拟杆菌门、衣原体门、蓝细菌门、厚壁菌门和变形菌门,优势属主要包括甲基杆菌属、鞘氨醇单胞菌属、薄层杆属、Polaromonas和无毛螺旋体属.植物种类、生境及二者的交互作用均能显著影响叶际细菌群落结构,其中生境的影响最大.     

Elevated atmospheric CO2 affects soil microbial diversity associated with trembling aspen

The effects of elevated atmospheric CO₂ (560 p.p.m.) and subsequent plant responses on the soil microbial community composition associated with trembling aspen was assessed through the classification of 6996 complete ribosomal DNA sequences amplified from the Rhinelander WI free-air CO₂ and O₃ enrichment (FACE) experiments microbial community metagenome. This in-depth comparative analysis provides an unprecedented, detailed and deep branching profile of population changes incurred as a response to this environmental perturbation. Total bacterial and eukaryotic abundance does not change; however, an increase in heterotrophic decomposers and ectomycorrhizal fungi is observed. Nitrate reducers of the domain bacteria and archaea, of the phylum Crenarchaea , potentially implicated in ammonium oxidation, significantly decreased with elevated CO₂. These changes in soil biota are evidence for altered interactions between trembling aspen and the microorganisms in its surrounding soil, and support the theory that greater plant detritus production under elevated CO₂ significantly alters soil microbial community composition.     

Synthesis and structures of the cuboidal iron-sulfur-nitrosyl-phosphine clusters [Fe4S3(NO)4(PR3)3] (R = Et, Pr, C6H11)

A series of cuboidal iron-sulfur clusters [Fe₄S₃(NO)₄(PR₃)₃]^0,1+ (R = Et, Prⁱ, Cy) were synthesized by two routes: reductive desulfurization of [Fe₄S₄(NO)₄] by tertiary phosphines, and substitution of triphenylphosphine in [Fe₄4S₃(NO)₄(PPh₃)₃] by a more basic phosphine. The structures of 3[Fe₄S₃(NO)₄(PEt₃)₃] · 0.5Et₂O, [Fe₄S₃(NO)₄(PEt₃)₃] [Fe₄S₃(NO)₇] and partially substituted [Fe₄S₃(NO)₄(PPh₃)_2⁻ (PPrⁱ₃)] have been determined by X-ray diffraction in order to define the cuboidal Fe₄S₃ core, previously known only in Roussin's black anion and its reduced form, [Fe₄S₃(NO)₇7]^1−,2−, and as a part of the iron-molybdenum cofactor of nitrogenase.     

The coordination chemistry of cationic main group clusters: syntheses and structures of [Fe3(Se2)2(CO)10] and [Fe4(Se2)3(CO)12]

The reactions of the polysulfur and selenium cationic clusters S₈²⁺ and Se₈²⁺ with various iron carbonyls were investigated. Several new chalcogen containing iron carbonyl cluster cations were isolated, depending on the nature of the counteranion. In the presence of SbF₆⁻ as a counterion, the cluster [Fe₃(E₂)₂(CO)₁₀] [SbF₆]₂·SO₂ (E = S, Se) could be isolated from the reaction of E₈²⁺ and excess iron carbonyl. The cluster is a picnic-basket shaped molecule of two iron centers linked by two Se₂ groups, with the whole fragment capped by an Fe(CO)₄ group. Crystallographic data for C₁₀O₁₂Fe₃Se₄Sb₂F₁₂S (I): space group monoclinic P2₁/c, A = 11.810(9), b = 24.023(6), c = 10.853(7) Å, β = 107.15(5)°, V = 2942(3) ų, Z = 4, R = 0.0426, R_w = 0.0503. When Sb₂F₁₁⁻ is present as the counterion, or Se₄[Sb₂F₁₁]₂ is used as the cluster cation source, a different cluster can be isolated, which has the formula [Fe₄(Se₂)₃(CO)₁₂] [SbF₆]₂·3SO₂. The dication contains two Fe₂Se₂ fragments bridged by an Se₂ group. Crystallographic data for C₁₂O₁₈Fe₄Se₆Sb₂F₁₂S₃ (III): space group triclinic , b = 18.400(9), C = 10.253(4) Å, = 93.10(4), β = 103.74(3), γ = 93.98(3)°, V = 1995(1) ų, Z = 2, R = 0.0328, R_w = 0.0325. The CO stretches in the IR spectrum all show a large shift to higher wavenumbers, suggesting almost no τ backbonding from the metals. This also correlates with the observed bond distances. All the compounds are extremely sensitive to air and water, and readily lose SO₂ when removed from the solvent. Thus all the crystals were handled at −100°C. The clusters seem to be either insoluble or unstable in all solvents investigated.     

Soil microbial responses to increased concentrations of atmospheric CO2

Terrestrial ecosystems respond to an increased concentration of atmospheric CO₂. While elevated atmospheric CO₂ has been shown to alter plant growth and productivity, it also affects ecosystem structure and function by changing below-ground processes. Knowledge of how soil microbiota respond to elevated atmospheric CO₂ is of paramount importance for understanding global carbon and nutrient cycling and for predicting changes at the ecosystem-level. An increase in the atmospheric CO₂ concentration not only alters the weight, length, and architecture of plant roots, but also affects the biotic and abiotic environment of the root system. Since the concentration of CO₂ in soil is already 10–50 times higher than that in the atmosphere, it is unlikely that increasing atmospheric CO₂ will directly influence the rhizosphere. Rather, it is more likely that elevated atmospheric CO₂ will affect the microbe–soil–plant root system indirectly by increasing root growth and rhizodeposition rates, and decreasing soil water deficit. Consequently, the increased amounts and altered composition of rhizosphere-released materials will have the potential to alter both population and community structure, and activity of soil- and rhizosphere-associated microorganisms. This occurrence could in turn affect plant health and productivity and plant community structure. This review covers current knowledge about the response of soil microbes to elevated concentrations of atmospheric CO₂.     

The synthesis and properties of binuclear pentacyanoiron(III)-μ-cyano- amminetetracyanoiron(III) [(C6H5)4P]4[(NC)5Fe---NC---Fe(CN)4NH3]·6H2O

The binuclear cyanoferrate, tetraphenylphosphonium pentacyanoiron(III)-μ-cyano-amminetetracyanoiron(III), [(C₆H₅)₄P]₄[Fe₂(CN)₁₀NH₃]⁴⁻, was synthesized by air oxidation of aqueous solutions of Na₃[Fe(CN)₅NH₃] · 3H₂O. Single crystal X-ray diffraction studies show the compound to contain the binuclear, cyano-bridged anion, [(NC)₅Fe---NC---Fe(CN)₄NH₃]⁴⁻. This compound is structurally identical to the one prepared by A. Ludi et al., [Inorg. Chim. Acta, 34, 113 (1979)], with the exception that [Fe(CN)₆]³⁻ is not required for the synthesis of this compound. The Fe(III) atoms are antiferromagnetically coupled through the CN⁻ bridge, as shown by a maximum in the magnetic susceptibility at 50 K. The electronic and IR spectra of the complex in the solid state and in solution are discussed.     

添加高粱根茬根际土对连作黄瓜生长和根际微生物的影响

为了分析添加高粱根茬根际土对连作黄瓜生长和根际微生物群落特征的影响,本研究通过盆栽试验,采用荧光定量PCR和高通量测序技术分析土壤细菌和真菌群落组成的差异。试验共设4个处理: CK(不施肥),T₁(单施化肥),T₂(优化施肥),T₃(优化施肥+高粱根茬根际土)。结果表明: 与其他处理相比,T₃处理促进了黄瓜生长发育,提高了土壤中16S rRNA和ITS rRNA基因数量。与T₁处理相比,T₂和T₃处理明显提高了细菌群落的丰富度和多样性,不同处理间真菌群落的丰富度和多样性差异不明显。添加高粱根茬根际土在一定程度上改变了基于门、属水平上的细菌和真菌群落结构。其中,细菌中提高了酸杆菌门和拟杆菌门的丰度,降低了变形菌门、厚壁菌门、硝化螺旋菌门和芽孢杆菌属的丰度;真菌中提高了担子菌门、木霉菌属和假散囊菌属的丰度,降低了镰刀菌属和绿僵菌属的丰度。冗余分析表明,土壤硝态氮和有机质含量分别是影响细菌和真菌群落结构差异的关键因子。添加高粱根茬根际土不仅提高了连作黄瓜土壤微生物数量和细菌多样性,而且增加了有益菌木霉菌属的丰度,降低了致病镰刀菌的丰度和数量,保障了黄瓜存活率,为缓解黄瓜连作障碍提供了一条切实可行的解决途径。     

Preparation and characterization of YADH-bound magnetic nanoparticles

The covalently binding of yeast alcohol dehydrogenase (YADH) to magnetic nanoparticles via carbodiimide activation was studied. The magnetic nanoparticles Fe₃O₄ with a mean diameter of 10.6 nm were prepared by co-precipitating Fe²⁺ and Fe³⁺ ions in an ammonia solution and treating under hydrothermal conditions. Transmission electron microscopy (TEM) micrographs showed that the magnetic nanoparticles remained discrete and had no significant change in size after binding YADH. X-ray diffraction (XRD) patterns indicated both the magnetic nanoparticles before and after binding YADH were pure Fe₃O₄. Magnetic measurement revealed the resultant magnetic nanoparticles were superparamagnetic characteristics, and their saturation magnetization was reduced only slightly after enzyme binding. The analysis of Fourier transform infrared (FTIR) spectroscopy confirmed the binding of YADH to magnetic nanoparticles and suggested a possible binding mechanism. In addition, the measurement of protein content revealed that the maximum weight ratio of YADH bound to magnetic nanoparticles was 0.125, below which the binding efficiency of YADH was almost 100%. The kinetic measurements indicated the bound YADH retained 62% of its original activity and exhibited a 10-fold improved stability than did the free enzyme. The maximum specific activities and Michaelis constants were also determined.     

短期CO2浓度升高和干旱胁迫对白羊草土壤碳氮和微生物根际效应的影响

采用人工气候室和盆栽控水试验研究黄土丘陵区典型草本植物白羊草在倍增CO₂浓度(800 μmol·mol^-1)下和充分供水(75%～80%的田间持水量)、轻度干旱胁迫(55%～60%的田间持水量)和重度干旱胁迫(35%～40%的田间持水量)下根际和非根际土壤碳氮含量和微生物群落结构及其根际效应.结果表明: CO₂浓度升高和干旱胁迫对白羊草根际和非根际土壤有机碳、全氮和水溶性有机碳(DOC)含量及其根际效应均无显著影响.轻度干旱胁迫下CO₂浓度升高显著促进了根际土壤水溶性有机氮(DON)的消耗,导致DOC/DON升高,提高了DON的负根际效应和DOC/DON的正根际效应.干旱胁迫和CO₂浓度升高对土壤总磷脂脂肪酸(总PLFA)和细菌PLFA的根际效应无显著影响.CO₂浓度升高条件下干旱胁迫显著提高了根际土壤G⁺/G^- PLFA,降低了非根际土壤G⁺/G^- PLFA,导致其根际效应显著提高,表明根际微生物群落由自养微生物群落向异养微生物群落的转变.     

Activity of magnetite-immobilized catalase in hydrogen peroxide decomposition

The present work analyzes the activity in decomposition of H₂O₂ using magnetite-immobilized catalase. The support of catalase is a glutaraldehyde-treated magnetite (Fe₃O₄). The data obtained in the H₂O₂ decomposition are analyzed. The fitting of the initial rate of the H₂O₂ decomposition versus hydrogen peroxide concentration data is discussed using a specific program for enzyme kinetics modeling (Leonora). The free catalase from Aspergillus niger (3.5 or 10 U/mL) does not show substrate inactivation up to 0.4 M H₂O₂. The immobilized catalase at low catalyst concentration shows substrate inhibition. Using 1 mg/mL of supported catalase the predicted maximum activity is higher than in the case of the free catalase at similar catalase concentration, although the optimum temperature is lower (40 °C versus 60 °C).