土生空团菌对白云母的风化作用及解钾特性

摘要:【目的】为了提高森林土壤含钾硅酸盐矿物利用率和改善树木钾素营养,探讨外生菌根真菌对白云母矿物的解钾及风化效应。【方法】通过5种外生菌根真菌在贫钾条件下与白云母的相互作用,考察了3种常用培养基对菌株解钾能力的影响;采用解钾效果最高的土生空团菌在Modified Melin-Norkrans(MMN)培养基条件下,进一步研究了21d浸出过程中主要矿质元素的释放量、生物量、剩余葡萄糖量、产生的小分子有机酸种类及含量、菌丝-矿物微环境的改变,利用扫描电子显微镜观测白云母被风化的痕迹。【结果】培养基对不同外生菌根真菌解钾能力的影响各异,其中土生空团菌在MMN培养基条件下解钾能力最强,其解钾量与生物量、剩余葡萄糖量、pH值显著相关。土生空团菌能够分泌有助于菌丝-矿物粘附的胞外多糖以形成菌丝-矿物微环境,并富集有机酸,促进微环境内钾的释放;菌丝不仅能够粘附在白云母表面产生刻蚀作用,还能破坏矿物深入其内部。【结论】外生菌根真菌具有促进白云母风化并释放钾素的能力,这种能力可能与菌丝、有机酸、多糖的协同作用有关。     

低分子量有机酸对含钾矿物钾素释放及其动力学模型的影响

采用连续流动浸提的方法,研究了酒石酸和草酸对不同含钾矿物(黑云母、白云母和微斜长石)钾释放及动力学模型的影响。结果表明:酒石酸连续流动浸提条件下,黑云母、白云母和微斜长石的释钾量分别是对照处理(去离子水)各矿物释钾量的2.2、3.3和2.6倍;草酸浸提条件下,黑云母、白云母和微斜长石的释钾量分别是对照处理的2.7、4.5和10.1倍;不同溶液连续流动浸提条件下,各矿物的释钾量均表现为黑云母﹥白云母﹥微斜长石;分别采用抛物线扩散模型、双常数模型、Elovich模型和一级动力学模型对不同矿物中钾的释放量进行方程拟合,结果表明,4种模型模拟条件下黑云母、白云母的钾释放动力学方程均达到了极显著的水平,决定系数R2介于0.591~0.999;一级动力学模型模拟下微斜长石钾释放的动力学方程达到了极显著水平。连续流动条件下,低分子量有机酸可显著提高不同含钾矿物的钾素释放量。     

矿物分解细菌Bacillus sp.L11对钾长石的风化作用北大核心CSCD

【目的】明确从南京钾矿区土壤中分离到的一株矿物分解细菌的分类地位,阐明其对钾长石矿物的风化效应及机制,为深入研究微生物-矿物相互作用提供参考依据。【方法】通过16S rRNA基因序列分析及其系统发育分析对菌株L11进行鉴定。采用摇瓶试验评估菌株L11对钾长石的风化能力,利用SEM/EDS观察钾长石矿物的形貌变化,使用X-射线衍射技术对小于2μm矿物进行了鉴定。【结果】菌株L11的16S rRNA基因序列与Bacillusaltitudinis的相似性最高,为99.9%,初步鉴定其为Bacillus sp.L11。摇瓶试验表明,菌株L11能够通过产生有机酸风化钾长石矿物,释放出Si、Al和Fe等元素。通过SEM发现第30 d的钾长石表明形貌发生了较大变化,表面有许多细菌存在,并形成了一些球形物质,EDS分析表明其Fe的含量较高。XRD结果表明,钾长石经菌株L11作用后可能形成了新矿物——菱铁矿。【结论】菌株Bacillus sp.L11能够加速钾长石的风化,改变其形貌,并能诱导新矿物的形成。     

不同风化程度钾长石表面矿物分解细菌的筛选及遗传多样性

【目的】不同风化程度钾长石表面矿物分解细菌生物多样性研究将有助于了解矿物生物风化、生物成矿和土壤形成的演化规律和机理。【方法】采用纯培养法自南平钾矿区高、中、低风化度钾长石以及矿区土壤样品中分离矿物分解细菌,通过摇瓶释硅实验比较不同菌株分解矿物能力,采用16SrDNA限制性酶切多态性分析(Amplified rDNA Restriction Analysis,ARDRA)研究了供试菌株的遗传多样性。【结果】分离筛选到35株生长良好的矿物分解细菌,与对照相比,接菌处理发酵液中有效硅增加了101～206%;所有供试菌株可分为11个OTU,分别属于5个门,6个科,7个属。多数菌株(74%)属于γ-变形杆菌纲(γ-Proteobacteria)。泛菌属(Pantoea),沙雷氏菌属(Serratia),假单胞菌属(Pseudomonas)为优势种群。【结论】南平钾矿区矿物分解细菌具有丰富的微生物种群多样性,且γ-变形杆菌纲(γ-Proteobacteria)细菌在钾长石风化过程中可能起了重要的作用。     

硫酸铵对两株钾矿物分解细菌生长代谢和风化钾长石的影响

【目的】为了明确钾矿物分解细菌Bacillus globisporus Q12和Rhizobium sp.Q32最合适的产酸和胞外多糖条件,并进一步阐明供试菌株对钾长石的溶解效应及其机制。【方法】分别向培养基中加入0-1.2 g/L(NH4)2SO4,选择菌株最适的产酸及合成胞外多糖条件,研究菌株对钾长石的溶解效果,并采用扫描电镜(SEM)观察钾长石表面形态及菌体分布特征。【结果】0.6、0和0.3 g/L(NH4)2SO4分别能使菌株Q12、Q32和混合菌株(Q12+Q32)产生较多的有机酸、胞外多糖以及有机酸和胞外多糖的复合物。菌株Q12、Q32及其混合菌株均能够显著地溶解钾长石,并释放出矿质元素,其中混合菌株的溶解效果要优于单一菌株;SEM分析表明,混合菌株对钾长石的溶蚀作用最强。【结论】(NH4)2SO4的含量能够影响供试菌株Q12和Q32的生长代谢及其对钾长石的风化作用,混合菌株可以通过产生的有机酸和胞外多糖的联合作用加速对钾长石的风化。     

外生菌根真菌对土壤钾的活化作用

【目的】外生菌根真菌是森林生态系统中的重要组成成分,与木本植物的根系形成菌根,参与树木养分吸收。【方法】试验在液培条件下,以土壤为钾源,利用我国西南地区分离的牛肝菌(Boletnus sp.,Bo 07)、松乳菇(Lactarius delicious,Ld 03)、彩色豆马勃(Pisolithus tinctorius,Pt 715)和内蒙古大青山分离的土生空团菌(Cenococcum geophilum,Cg 04)为材料,研究了它们的生长、钾吸收、氢离子和有机酸分泌,以及土壤钾的变化。【结果】结果表明,Bo 07、Ld 03和Pt 715的生物量、含钾量和吸收量显著高于Cg 04,说明在长期缺钾的环境中,外生菌根真菌经过"物竞天择"可能进化出适应低钾和较强的吸钾能力。以土壤为钾源培养菌根真菌,培养液中的钾浓度显著提高,故外生菌根真菌可促进土壤钾的溶解。在外生菌根真菌的培养液中,分别检测到苹果酸、丁二酸和柠檬酸,均检测到草酸和乙酸。Bo 07、Ld 03和Pt 715显著提高土壤交换性钾含量,Bo 07和Ld 03还显著降低矿物结构钾含量,说明外生菌根真菌不同程度地活化了土壤无效钾,分离自南方的菌株Bo 07、Ld 03和Pt 715总体上大于分离自北方的菌株Cg 04。此外,土壤矿物结构钾分别与总有机酸和草酸分泌量呈极显著负相关(r有机酸=-0.989**,r草酸=-0.950*,n=5),与培养液pH值呈显著正相关(r=0.916*,n=5),故外生菌根真菌分泌的氢离子和有机酸尤其是草酸可能活化土壤无效钾。【结论】供试外生菌根真菌能不同程度的活化土壤无效钾,其活化能力可能与分泌氢离子和有机酸尤其是草酸密切相关。     

黑曲霉-矿物聚集体的形成及其分泌的多糖特性

【目的】为深入理解黑曲霉(Aspergillus niger)对含钾矿粉的风化作用,研究在旋转发酵方式下形成的黑曲霉-矿物聚集体及其多糖,并分析它们在含钾矿粉风化过程中的作用。【方法】采用不同组合培养基,研究黑曲霉-矿物聚集体的形成和形貌;联合紫外-可见分光光谱(UV-Vis)、傅立叶变换红外光谱(FT-IR)、气相色谱(GC)、电子扫描显微镜(SEM)、X射线能谱仪(EDS)等分析手段研究黑曲霉-矿物聚集体形成前后微环境中多糖的变化以及这种改变对风化产生的意义。【结果】黑曲霉菌丝与矿粉在多糖等代谢产物帮助下,通过相互缠绕、吸附、粘合等作用形成黑曲霉-矿物聚集体,聚集体形成前后多糖浓度和多糖结构均发生显著改变。【结论】含钾矿粉诱导黑曲霉多糖结构发生明显变化并且浓度增大,这种改变可促进多糖对矿物颗粒的吸附,有助于螯合金属离子和吸附水分子,从而为真菌有效利用矿物营养提供有利的微环境。     

Pseudomonas azotoformans F77和Pseudomonas paracarnis P1风化黑云母的效应及机制比较

【目的】比较高效矿物风化固氮假单胞菌(Pseudomonas azotoformans) F77及其亲缘关系较近的假单胞菌(Pseudomonas paracarnis) P1风化黑云母的效应和机制。【方法】通过检测两株菌在不同时间点的发酵液中细胞数量、pH值、葡萄糖剩余量、葡萄糖酸浓度和可溶性Fe、Al释放量,比较它们对黑云母的风化效果与生理机制。采用RNA-seq技术研究这两株菌风化黑云母过程中出现差异的分子机制。【结果】在持续5 d的风化试验中,菌株F77发酵液中的细胞数量和pH值低于菌株P1,葡萄糖酸浓度是菌株P1的27.3-53.9倍,Fe和Al元素的释放量是菌株P1的3.3-23.3倍。比较转录组数据表明,菌株F77特有的基因数量(2 872)和差异基因数量(1 832)均多于菌株P1 (分别为1 903和1 258)。菌株F77在胞内物质跨膜转运与碳代谢、细胞运动、趋化与信号诱导等途径中基因数量也高于菌株P1。此外,菌株F77的超氧化物歧化酶和过氧化氢酶基因差异表达倍数、葡萄糖酸合成基因数量和差异表达倍数也明显高于菌株P1。【结论】菌株F77风化黑云母以及合成葡萄糖酸的能力显著高于菌株P1。菌株F77通过产生葡萄糖酸来促进黑云母的风化。添加黑云母显著促进了菌株F77胞内与矿物风化相关基因的表达,如物质跨膜转运、细胞运动与趋化、信号诱导、碳代谢及能量代谢等途径基因。此外,葡萄糖酸合成途径基因、超氧化物歧化酶基因以及过氧化氢酶基因在矿物风化中可能发挥重要作用。     

土壤中解钾菌K02的筛选、鉴定及培养条件优化

解钾微生物是能够在土壤或纯培养条件下,将含钾矿物如长石、云母等不能被作物吸收利用的矿物态钾分解,并产生水溶性钾的微生物。利用以钾长石粉为唯一钾源的硅酸盐细菌选择性培养基,采用梯度稀释分离法平板划线对番茄土壤中的钾细菌进行筛选。利用原子吸收火焰分光光度法测定钾细菌培养液中可溶性钾的含量,筛选高效解钾菌株。通过形态观察和16S rDNA序列GenBank比对,同时利用clustalx和MEGA 4.0等相关软件构建系统进化树对解钾能力最强的菌株K02进行鉴定,初步鉴定该解钾菌为胶质类芽胞杆菌(Paenibacillus mucilaginosus);利用单因素试验法对K02菌株培养基组分及发酵条件进行优化,初步确定菌株K02最佳培养基组分以解钾复筛培养基为基础,其碳源、氮源及无机盐以可溶性淀粉1%、酵母膏0.2%、K_2HPO_40.05%为最佳;菌株K02最佳发酵条件:培养温度为30℃,培养时间为48 h,培养基装量为50 mL/250 mL,培养基初始pH值为7.5,接菌量为5%,这一结果为解钾菌肥的研制和生产提供参考。     

一株红壤溶磷菌的分离、鉴定及溶磷特性

【目的】为了提高红壤磷素利用率,探讨溶磷菌溶磷机理。【方法】利用难溶性无机盐培养基从花生根际土壤样品中分离到一株溶磷菌C5-A,结合菌落形态特征、生理生化和16S rRNA序列确定该菌株的系统发育地位;通过菌株C5-A在NBRIP液体培养基培养过程中培养液pH变化确定其溶磷能力;利用液体发酵实验测定不同的碳源、氮源对菌株C5-A溶磷的影响;通过高效液相色谱检测C5-A在不同氮源培养液中有机酸的种类和浓度。【结果】菌株C5-A鉴定为洋葱伯克霍尔德氏菌(Burkholderia cepacia),遗传稳定性较好。在FePO4和AlPO4培养液中,菌株C5-A的溶磷量和pH变化呈显著负相关;菌株C5-A对磷酸三钙、磷酸铝、磷酸铁、磷矿粉均有较强的溶解能力,最高溶磷量分别为125.79、227.34、60.02和321.15 mg/L;菌株C5-A对不同浓度的两种磷矿粉有较强的溶解能力;分别以麦芽糖和草酸铵为碳源和氮源时溶磷量最高。高效液相色谱检测出10种有机酸,分别为草酸(葡萄糖酸)、乙酸、苹果酸、琥珀酸和5种未知有机酸,然而,乙酸而非草酸似乎是影响C5-A溶磷的重要有机酸。【结论】从红壤花生根际土壤中筛选到一株对难溶性无机盐具有较强溶解能力溶的菌株C5-A,有望为开发高效红壤微生物磷肥提供种质资源。     

Effects of Mineral Structure and Microenvironment on K Release from Potassium Aluminosilicate Minerals by Cenococcum geophilum fr

K-bearing minerals with enormous reserve in the world, were not easy to provide the available K nutrient element for plant direct uptake because of the slow K release rate. With the potential potassium-solubilizing microorganisms, the slow K release rate from minerals would be improved significantly. In this work, Cenococcum geophilum Fr, one of the most common ectomycorrhizal fungi in boreal to temperate regions, was adopted to dissolve K-bearing minerals for K release. Five kinds of potassium aluminosilicate minerals were tested by bioleaching experiments in pure culture, including feldspar, nepheline, biotite, muscovite and illite. The available and unavailable potassium amounts in minerals before and after bioleaching were measured and compared with each other. The effect of mineral structure on the potassium solubilization efficiency by Cenococcum geophilum Fr. was discussed. Furthermore, the microenvironment formation between fungi and mineral surface to enhance the K release rate was investigated through detecting K, Al, Si concentrations and metabolites amounts (polysaccharide and organic acids) in microenvironment and external environment, respectively. Experimental results demonstrated that Cenococcum geophilum Fr. was a potential candidate of potassium solubilizing microorganisms, and both mineral structure and microenvironment have significant effects on the K release rate.     

Bioweathering of Kupferschiefer black shale (Fore-Sudetic Monocline, SW Poland) by indigenous bacteria: implication for dissolution and precipitation of minerals in deep underground mine

The Upper Permian polymetallic, organic-rich Kupferschiefer black shale in the Fore-Sudetic Monocline is acknowledged to be one of the largest Cu-Ag deposits in the world. Here we report the results of the first study of bioweathering of this sedimentary rock by indigenous heterotrophic bacteria. Experiments were performed under laboratory conditions, employing both petrological and microbiological methods, which permitted the monitoring and visualization of geomicrobiological processes. The results demonstrate that bacteria play a prominent role in the weathering of black shale and in the biogeochemical cycles of elements occurring in this rock. It was shown that bacteria directly interact with black shale organic matter to produce a widespread biofilm on the Kupferschiefer shale surface. As a result of bacterial activity, the formation of pits, bioweathering of ore and rock-forming minerals, the mobilization of elements and secondary mineral precipitation were observed. The chemistry of the secondary minerals unequivocally demonstrates the mobilization of elements from minerals comprising Kupferschiefer. The redistribution of P, Al, Si, Ca, Mg, K, Fe, S, Cu and Pb was confirmed. The presence of bacterial outer membrane vesicles on the surface of black shale was observed for the first time. Biomineralization reactions occurred in both the membrane vesicles and the bacterial cells.     

Effect of Neotyphodium endophyte-tall fescue symbiosis on mineralogical changes in clay-sized phlogopite and muscovite

Numerous studies have been conducted to determine the positive effects of Neotyphodium endophye-tall fescue symbiosis on plant resistance to different stresses. However, its effects on the uptake of potassium (K) and transformation of K-bearing minerals are not yet known. The objective of this research was to investigate the possible effects of such symbiosis on the transformation of clay-sized micaceous minerals. Tall fescue genotype 75B, both infected and non-infected with natural Neotyphodium endophyte, was cultivated in a mixture of quartz sand and phlogopite or muscovite. Pots were irrigated with distilled water and complete or K-free nutrient solutions for a period of 140 days. K concentrations in shoot and root were determined using a flame photometer and the clay-sized particles in each pot were analyzed using an X-ray diffractometer. Results revealed vermiculitization of phlogopite under both nutrient solutions. In addition to vermiculite, smectite was detected as a newly formed mineral in phlogopite-amended pots. In contrast, a very weak rate of vermiculitization was observed in muscovite-treated media. The rate of phlogopite transformation was significantly higher under the endophyte-infected plants, particularly when the K-free nutrient solution had been applied. Also, the significant decrease in pH value in the rhizosphere of infected plants confirmed the positive effect of endophyte-tall fescue symbiosis on mineral transformation.     

Fungal biotransformation of zinc silicate and sulfide mineral ores

In this work, several fungi with geoactive properties, including Aspergillus niger, Beauveria caledonica and Serpula himantioides, were used to investigate their potential bioweathering effects on zinc silicate and zinc sulfide ores used in zinc extraction and smelting, to gain understanding of the roles that fungi may play in transformations of such minerals in the soil, and effects on metal mobility. Despite the recalcitrance of these minerals, new biominerals resulted from fungal interactions with both the silicate and the sulfide, largely resulting from organic acid excretion. Zinc oxalate dihydrate was formed through oxalate excretion by the test fungi and the mineral surfaces showed varying patterns of bioweathering and biomineral formation. In addition, calcium oxalate was formed from the calcium present in the mineral ore fractions, as well as calcite. Such metal immobilization may indicate that the significance of fungi in effecting metal mobilization from mineral ores such as zinc silicate and zinc sulfide is rather limited, especially if compared with bacterial sulfide leaching. Nevertheless, important bioweathering activities of fungi are confirmed which could be of local significance in soils polluted by such materials, as well as in the mycorrhizosphere.     

Plants use alternative strategies to utilize nonexchangeable potassium in minerals

Plant species differ in their capacity to use nonexchangeable potassium (NEK) in soils. In this study two typical plants with high K use efficiency, ryegrass and grain amaranth, were compared with regard to their capacity to use K from five K-bearing minerals. Biomass relative yield and K uptake data indicated that ryegrass was much more efficient than grain amaranth at using NEK in minerals. Root exudates of grain amaranth collected under hydroponic culture contained considerable amounts of oxalic and citric acids, while these acids were not detected in ryegrass root exudates. Compared with grain amaranth, the kinetic parameters of K uptake by ryegrass roots were characterized by a significantly higher K uptake rate (V_max) and a significantly lower C_min, the minimum external K concentration at which K is taken up. The dynamic release of NEK from minerals in various solutions showed that the release rate of NEK was largely K-concentration dependent and some thresholds of K concentration prevented further NEK release from minerals. The K thresholds were related to mineral type and increased in the presence of Ca²⁺ or Na⁺ in solutions. The positive effect of H⁺ (20 mmol L^?1) on NEK release was also mainly attributed to elevating the thresholds of K concentration, rather than to the effects of weathering. The results indicated that the main mechanism by which plant species efficiently use NEK in minerals was to the capacity of plants to absorb K at low concentrations. The lower the C_min for the root K uptake, the higher the expected NEK use efficiency of the plant.     

Transformation of vanadinite [Pb5(VO4)3Cl] by fungi

Saprotrophic fungi were investigated for their bioweathering effects on the vanadium‐ and lead‐containing insoluble apatite group mineral, vanadinite [Pb₅(VO₄)₃Cl]. Despite the insolubility of vanadinite, fungi exerted both biochemical and biophysical effects on the mineral including etching, penetration and formation of new biominerals. Lead oxalate was precipitated by Aspergillus niger during bioleaching of natural and synthetic vanadinite. Some calcium oxalate monohydrate (whewellite) was formed with natural vanadinite because of the presence of associated ankerite [Ca(Fe²⁺,Mg)(CO₃)₂]. Aspergillus niger also precipitated lead oxalate during growth in the presence of lead carbonate, vanadium(V) oxide and ammonium metavanadate, while abiotic tests confirmed the efficacy of oxalic acid in solubilizing vanadinite and precipitating lead as oxalate. Geochemical modelling confirmed the complexity of vanadium speciation, and the significant effect of oxalate. Oxalate–vanadium complexes markedly reduced the vanadinite stability field, with cationic lead(II) and lead oxalate also occurring. In all treatments and geochemical simulations, no other lead vanadate, or vanadium minerals were detected. This research highlights the importance of oxalate in vanadinite bioweathering and suggests a general fungal transformation of lead‐containing apatite group minerals (e.g. vanadinite, pyromorphite, mimetite) by this mechanism. The findings are also relevant to remedial treatments for lead/vanadium contamination, and novel approaches for vanadium recovery.     

基于Biolog-FF技术的金霉素降解真菌的碳代谢特征研究

【目的】利用Biolog-FF技术对4种不同金霉素降解真菌代谢95种碳源特征进行测定分析。【方法】测定不同时段4种真菌对95种碳源代谢的吸光值,并将4种真菌分别接种到金霉素药渣固废中,测定不同发酵时间药渣中的总有机碳含量。【结果】4种真菌利用碳源种类和活性差异较大,桔青霉LJ318、哈茨木霉LJ245、小刺青霉LJ236、草酸青霉LJ302能够利用碳源数量依次为41、39、15和14种;菌株LJ245和LJ318利用碳源的平均活性显著高于菌株LJ236和LJ302;4种真菌能够较好利用的碳源类型为糖类、氨基酸类、聚合物类等物质。【结论】菌株LJ245和LJ318代谢药渣中的碳源明显快于菌株LJ236和LJ302,这与Biolog方法测定结果趋势一致。Biolog-FF技术是一种快速测定真菌单菌落碳代谢特征的有效方法。研究为探讨真菌碳代谢特征与生物降解环境残留金霉素提供了科学依据。     

响应面法优化细菌EHB01对铜绿微囊藻(Microcystis aeruginosa)的溶藻条件

【背景】水体富营养化导致的蓝藻水华对淡水资源造成了严重污染。利用环境友好型的溶藻菌可有效控制蓝藻的生长,是防治蓝藻水华形成的有效途径之一。【目的】优化溶藻细菌EHB01对铜绿微囊藻(Microcystis aeruginosa)的溶藻条件,以期为治理蓝藻水华污染提供高效的溶藻菌制剂。【方法】采用单因素试验对溶藻的发酵液浓度、温度、光照以及C:N和N:P进行分析,并对溶藻细菌EHB01发酵液的碳源、氮源和p H进行优化。基于单因素试验,选用中心组合试验设计(central composite design,CCD)确定关键因子的最佳数量水平,并以Desig-Expert 8.0.5进行回归分析,通过响应面分析获得溶藻效果最佳的参数。【结果】发酵液浓度对溶藻率的影响表现为持续上升;温度对溶藻率表现为先上升后下降;而光照、C:N和N:P均对细菌EHB01发酵液溶藻率的影响表现为先降低后上升的趋势。溶藻细菌EHB01发酵液所需的最佳碳源为蔗糖,氮源为硝酸钾,pH为7.5,优化条件下溶藻率达86.97%,与优化之前相比提高了21.72%。【结论】采用响应面法优化得出溶藻细菌EHB01发酵液最优的培养条件,且模型拟合效果较好,可为溶藻菌制剂工业化发酵提供有效依据。     

樟绒枝霉(Malbranchea cinnamomea)固体发酵产木聚糖酶的发酵条件优化

[目的] 研究樟绒枝霉(Malbranchea cinnamomea) CAU521利用农业废弃物固体发酵产木聚糖酶的发酵条件.[方法]采用单因素试验法优化影响菌株产酶的各个条件,包括碳源种类、氮源种类、初始pH、初始水分含量、培养温度及发酵时间共6个因素.[结果]获得的最佳产酶条件为:稻草为发酵碳源、2％(W/W)的酵母提取物为氮源、初始pH 7.0、初始水分含量80％和发酵温度45℃.在此条件下发酵6d后木聚糖酶的酶活力达到13 120 U/g干基碳源.[结论]樟绒枝霉固体发酵产木聚糖酶的产酶水平高,生产成本低,具有潜在的工业化应用前景.     

低Mg/Ca条件下丛毛单胞菌HJ-1菌株诱导文石的形成

【目的】为了探讨细菌对碳酸盐矿物种类和形态的影响。【方法】本文利用丛毛单胞菌HJ-1菌株进行了持续50 d的培养实验。在实验过程中,对细菌数量、沉淀物重量、培养液中Ca2+和Mg2+浓度等进行了动态监测。利用扫描电子显微镜对矿物形态进行了观察,并利用X-射线衍射仪对矿物成分进行测定。【结果】丛毛单胞菌HJ-1菌株具有显著的诱导碳酸盐矿物沉淀的能力,碳酸盐矿物的重量随着培养时间的延长而逐渐增加。X-射线衍射结果表明,形成的碳酸盐沉淀主要由文石和高镁方解石组成,其中文石的最高含量达86%。上述矿物在形态上复杂多样,主要有杆状、柱状、哑铃形、球状和板状以及不规则状和鳞片状集合体。【结论】通常,在Mg/Ca≤2并且有微生物参与的条件下极少形成文石。本文在Mg/Ca为2,不含碳酸根离子的培养基中培养HJ-1菌株的过程中发现了文石。作者认为,低Mg/Ca条件下文石的形成主要与HJ-1菌株分泌较多的胞外多糖有关。