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1.
一株红壤溶磷菌的分离、鉴定及溶磷特性   总被引:9,自引:0,他引:9  
【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。  相似文献   

2.
一株节杆菌溶解磷矿粉的动态   总被引:2,自引:0,他引:2  
磷矿粉用量明显地影响节杆菌1TCRi7菌株对其溶解,随着磷矿粉用量的增加,溶磷率急剧下降,超过5 g/L,溶磷率不到0.1%,培养液的pH也随磷矿粉用量增加而升高,但菌体生长繁殖几乎不受磷矿粉用量的影响。振荡培养时,第1 d菌体繁殖量就达到高峰,pH也降至最低,同时表现出强烈的溶磷活力,但菌株的溶磷量并不与其生长量吻合,溶磷量第9 d才达到高峰,以后逐渐下降。培养过程中有机酸分泌发生交替变化,主要分泌乙酸和丙二酸。第1 d、第9 d和第15 d出现3个峰值,说明微生物利用了所分泌出来的有机酸,并发生了有机酸代谢的变化。  相似文献   

3.
不同碳源对三种溶磷真菌溶解磷矿粉能力的影响   总被引:18,自引:0,他引:18  
通过液体培养法 ,对 3种溶磷真菌利用葡萄糖、果糖、蔗糖、麦芽糖、淀粉和纤维素等碳源溶解宜昌产磷矿粉的试验 ,结果表明 ,菌株P2 3在供给葡萄糖时的溶磷能力最高 ,并在一定程度上能够利用长链碳源淀粉和纤维素为营养而溶磷 ;而高效溶磷菌株P6 6和P39溶磷的最佳碳源是果糖和麦芽糖 ,该两菌株利用淀粉和纤维素的溶磷效果很小 ,甚至不溶磷。 3种溶磷真菌培养滤液 pH值、可滴定酸含量与其溶磷量之间的相关性因菌株而异 ,差别很大。菌株P2 3培养滤液pH值、可滴定酸含量与其溶磷量之间相关性很低 ,但菌株P6 6和P39培养滤液pH值、可滴定酸含量与其溶磷量之间相关性却达到极显著水平 (P <0 0 1)。结果表明 ,不同碳源对溶磷菌溶解磷矿粉能力影响很大 ,分析推断 3种菌株产生的有机酸活化磷矿粉能力为P6 6>P39>P2 3。  相似文献   

4.
石灰性土壤拉恩式溶磷细菌的筛选鉴定及溶磷特性   总被引:3,自引:0,他引:3  
从山西石灰性土壤作物根际分离筛选出多株溶磷细菌,经过多次分离纯化得到一株溶磷能力较强的菌株W25,通过菌落形态、生理生化特性和16S rRNA序列分析,确定溶磷菌W25为拉恩式菌属.对W25溶解磷特性进一步研究表明:其对磷酸三钙、磷酸铝和磷酸铁最高溶磷能力分别为385.5、110.4、216.6 mg·L-1;在磷酸铝和磷酸铁培养液中,W25溶磷量与培养液pH的相关系数分别为0.56和0.81,呈极显著负相关;在不同碳氮源条件下,W25以葡萄糖为碳源和NH4NO3为氮源时对磷酸三钙的溶磷量最高,对碳源的利用顺序依次为葡萄糖>乳糖>蔗糖>甘露醇>淀粉,对氮源的利用顺序依次为NH4NO3 >NH4Cl>(NH4)2SO4>NaNO3>KNO3.不同氮源对W25产生有机酸的种类影响较大,以铵态氮为氮源产生甲酸和乙酸,以硝态氮为氮源产生草酸和琥珀酸,以硝酸铵为氮源还产生柠檬酸.  相似文献   

5.
溶磷菌和固氮菌溶解磷矿粉时的互作效应   总被引:13,自引:0,他引:13       下载免费PDF全文
采用4株溶磷菌(Lx81、Dm84、Jm92、Lx191)、和3株固氮菌(ChW5、ChW6、ChO6)单独和混合接种后测定培养液有效磷含量、pH值及总有机酸含量的方法,研究溶磷菌和固氮菌溶解磷矿粉时的互作效应。结果表明,相对于单独接种溶磷菌:Lx81与3株固氮菌分别混合培养能提高磷矿粉的溶解能力,4株溶磷菌与ChW6,Lx81、Dm84、Lx191与Ch06分别混合培养及Jm92+ChW5组合溶磷量极显著增加(P〈0.01);Dm84+ChW5、Lxl91+ChW5、Jm92+Ch06组合的溶磷量下降(P〈0.01)。除Lx81+ChW6、Lx81+Ch06培养液pH值降低外,混合培养的其它组合培养液pH值均较单独接种溶磷菌时升高。有机酸测定结果表明,Lx81、Jm92与ChW5、Ch06分别混合培养、ChW6+Lx81组合有机酸含量升高(P〈0.01),其它7种组合的有机酸含量均较单独接种溶磷菌的值下降(P〈0.01)。溶磷菌和固氮菌单菌培养时溶磷量与pH值、溶磷量与总有机酸含量及pH值与总有机酸含量之间呈现线性相关;Dm84、Lx191与3株固氮菌分别混合培养溶磷量与pH值之间、Lx81与3株固氮菌分别混合培养溶磷量与总有机酸含量之间呈现线性相关,其它组合的溶磷量与pH值、总有机酸含量间没有相关性。溶磷菌和固氮菌混合培养对溶解磷矿粉既有协同作用也有拮抗作用。  相似文献   

6.
从湖南、湖北、云南等地磷矿开采场的土壤样品中筛选到一株溶磷能力较强的菌株P21,结合生理生化指标和16S rDNA序列分析鉴定其属于草生欧文氏菌菠萝变种(Erwinia herbicola var.ananas).该菌能溶解磷酸三钙、羟基磷灰石、磷酸铁、磷酸锌,其中对磷酸三钙和羟基磷灰石的每升液体培养基溶磷量(P2O5)分别高达1206.20mg、529.67mg.溶磷菌草生欧文氏菌菠萝变种P21对产地不同的8种磷矿石溶解能力不同,对云南晋宁和昆阳、四川雅安、江苏锦屏等地磷矿石有较强的溶解能力,每升液体培养基溶磷量分别为96.64mg、78.46mg、67.07mg、65.24mg,对其它产地的磷矿石溶解能力较差.实验表明,培养液的pH下降与溶磷菌P21的溶磷量无直接关系.  相似文献   

7.
两株对花生促生的芽孢杆菌的鉴定及溶磷特性研究   总被引:1,自引:0,他引:1  
土壤中绝大多数的磷以难溶态存在而不能被利用,溶磷微生物可以溶解难溶性磷,提高土壤的速效磷水平,从而促进植物生长。本研究利用盆栽实验测定从茶树根际分离的2株溶磷细菌对花生生长的影响,发现均具有显著促生效应,尤以HP9菌株表现更为明显。通过形态、生理生化试验及分子生物学方法进行鉴定,将HP9、HP10菌株分别鉴定为贝莱斯芽孢杆菌(Bacillus velezensis)和坚强芽孢杆菌(Bacillus firmus)。研究2个菌株在不同碳氮源条件下的溶磷性,结果显示HP9菌株具有更强的溶磷能力,2个菌株溶磷的最优碳源均为葡萄糖,最优氮源则有明显差异,HP9菌株优先利用硝酸钾,而HP10菌株则以硫酸铵为氮源时溶磷量更高;进一步研究菌株的溶磷机制,相关性分析显示2个菌株培养液中的可溶磷含量与pH值呈显著负相关,GC-TOF-MS测定表明2个菌株代谢产物中产生的有机酸是其溶磷的重要原因,而产生的有机酸类型和含量的明显不同与菌株溶磷水平的差异有关,研究结果解析了芽孢杆菌属不同种菌株在溶磷机制上存在的多样性。  相似文献   

8.
王丹  詹婧  孙庆业 《生态学杂志》2014,25(7):2079-2084
从安徽省铜陵市铜官山尾矿库木贼根际分离筛选出的出芽短梗霉F4,以磷酸钙、磷酸铝、磷酸铁和磷矿粉4种不同磷源进行液体培养,测定培养液的pH、水溶性磷、菌体磷及有机酸含量.结果表明: 菌株F4对不同磷源的溶磷能力为:磷酸铝>磷酸铁、磷酸钙>磷矿粉,溶磷量均高于200 mg·L-1;培养液pH在48 h内迅速下降,以磷酸铝、磷酸铁为磷源的培养液pH下降幅度明显大于磷酸钙与磷矿粉.出芽短梗霉F4产生的有机酸主要为草酸、柠檬酸和酒石酸,其中,以草酸为主.菌株的溶磷能力与有机酸无显著相关性,而与pH呈显著相关.接种出芽短梗霉F4时加入葡萄糖,尾矿中速效磷含量显著增加,说明出芽短梗霉F4在尾矿生态修复中具有潜在的应用价值.
  相似文献   

9.
一株溶磷真菌筛选鉴定及其溶磷促生效果   总被引:4,自引:0,他引:4  
【目的】从高产农田筛选高效溶磷微生物菌株,为溶磷微生物肥料开发提供高效菌种资源。【方法】利用菌株的形态学特性、培养特征和ITS rDNA序列分析方法进行菌株鉴定,结合液体培养和土壤培养方法研究菌株的溶磷能力,进而采用温室盆栽和田间小区试验,明确溶磷菌P83促进作物生长和提高作物产量的作用效果。【结果】溶磷菌株P83鉴定为斜卧青霉菌(Penicillium decumbens)。液体条件下培养10 d,菌株P83表现显著高效的溶磷能力,对Ca3(PO4)2(5g/L)的溶解效果,有效磷达956 mg/L,溶解率为42.68%,对湖南永和磷矿粉的溶液效果,有效磷达到152.8 mg/L;将P83菌株分别接种于施用Ca3(PO4)2、Zn3(PO4)2和磷矿粉(RP)3种磷源的盆栽试验土壤中,结果显示,菌株P83对玉米植株促生效果比对照显著提高,玉米植株鲜重提高9.5%-89.2%、干重增加35%-231%,土壤有效磷提高2.1-40.5 mg/kg。田间小区玉米产量结果显示,溶磷菌P83增产效果最好(P=0.05),玉米子粒产量达9.2t/hm2,比不接种菌剂的对照增加2.4 t/hm2,增产率为35.3%。【结论】获得了一株溶解难溶磷的斜卧青霉菌P83,它能够活化多种难溶磷、显著增加土壤有效磷水平,对玉米生长和增加作物产量具有显著作用,是一株展现良好应用前景的高效溶磷菌种。  相似文献   

10.
一株耐盐日本曲霉的筛选及其溶磷促生作用   总被引:2,自引:0,他引:2  
【目的】从内蒙古种植葵花的盐碱地中筛选高效溶磷真菌,为盐碱地增产节肥开发生物肥料提供溶磷菌种资源。【方法】利用ITS r DNA序列鉴定菌株、固体培养基测定耐盐性,液体摇床培养与盆栽试验结合分析菌株溶磷能力,盆栽和田间试验明确菌株M1促进作物生长和增产作用;LC-MS技术测定菌株M1在液体培养基中分泌有机酸和植物激素含量,明确菌株M1的溶磷和促生机理。【结果】溶磷菌株M1鉴定为日本曲霉(Aspergillus japonicus)。液体培养基接种菌株M1培养6 d,以Ca_3(PO_4)_2为磷源时上清液有效磷达1020.89 mg/L,溶解率为63.30%;以AlPO_4为磷源时有效磷达995.69 mg/L,溶解率为48.59%;以贵州开阳磷矿粉、江苏锦屏磷矿粉、云南晋宁磷矿粉、河北钒山磷矿粉和云南昆阳磷矿粉为磷源接种菌株M1,从晋宁磷矿粉释放的有效磷浓度最高,达到363.64 mg/L。菌株M1可耐受10%NaCl。将M1制备的菌剂分别接种于施用Ca_3(PO_4)_2、AlPO_4和开阳磷矿粉3种磷源的4种盆栽试验土壤包括北京石灰性潮土、安徽黏性潮土、安徽水稻土和山东沿海盐潮土。结果显示,菌株M1对玉米植株促生效果显著,玉米植株鲜重比对照提高2.14%–90.91%、干重增加22.15%–268.28%;土壤有效磷提高21.81–24.27 mg/kg。菌株M1与4种土壤的适配性均高于对照菌株DSM 821。田间小区花生产量结果显示,接种溶磷菌剂M1增产效果最好,花生果实产量达4.46 t/hm~2,比不接种菌剂的对照处理增加0.81 t/hm~2,增产22.19%。菌株M1在含有磷酸三钙、磷酸铝和开阳磷矿粉3种难溶磷培养液中经过6 d培养,均产生7种有机酸,其中草酸和柠檬酸含量最高,分别为616.16 mg/L和413.69 mg/L;培养液均能检测到吲哚乙酸(IAA)和玉米素,IAA含量为15.45–77.58 mg/L,玉米素浓度为0.06–0.11 mg/L。【结论】获得了一株高效溶解多种难溶磷的日本曲霉菌M1,它能显著增加土壤有效磷、促进玉米生长和花生增产,与4种典型土壤适配性好,具有良好的农业应用前景。  相似文献   

11.
Summary Surface samples of six Ontario soils were selected to provide a range in pH, texture and carbonate content. Phosphorus was added to the soil samples at the rate of 200, and 2000 pounds. P2O5 per acre and the inorganic phosphates associated with aluminum (Al-P), iron (Fe-P) and calcium (Ca-P) were analysed 15, 30, and 335 days after treatment. Samples of the check soils were leached with the equivalent of 7 litres of soil-percolated water and then analysed for phosphate fractions. In 5 soils with added phosphorus the Al-P fraction increased at both rates of added phosphorus, Fe-P increased only at the higher rate of added phosphorus and Ca-P did not increase at either rate. In the sixth soil (69.9% CaCO3 equivalent) Ca-P increased at both rates of added phosphorus, but proportionately less than the water-soluble phosphorus. These changes in phosphorus values existed relatively unchanged for 335 days after the addition of phosphorus. Leaching generally removed phosphorus from all phosphorus fraction. At or below pH 7.1 (soil paste) the Al-P decreased proportionately more than the Fe-P and Ca-P. Above pH 7.1 the Ca-P decreased proportionately more than the other two fractions upon leaching.Contribution from Dept. of Soil Science, O.A.C., Guelph, Canada. Part of thesis submitted by junior author to the Graduate School, University of Toronto, in partial fulfilment of the requirements for the M.S.A. degree.  相似文献   

12.
定位施肥对紫色菜园土磷素状况的影响   总被引:10,自引:0,他引:10  
基于紫色菜园土壤莴笋-白菜轮作3a的12季连续定位施肥试验,研究施肥对土壤磷素状况的影响。结果表明,在紫色土上以化肥为基础增施有机肥(泥炭或菜籽粕)既提高土壤磷含量,又增加无机磷组分中有效磷源和缓效磷源的比例,且不会增加磷素淋失的风险,是所有处理中最优者;增磷、增钾处理虽然提高了土壤磷含量,但未能提高速效磷源与缓效磷源的比例;增氮、增硼及常规施肥降低土壤磷含量和提高无效磷源的比例;无肥处理磷含量最低,无效磷源比例最高。紫色菜园土无机磷约为有机磷的4—6倍,无机磷各组分以钙磷为主,占I-P总量的60.89%—67.92%,显示紫色土风化程度较低。各形态磷素呈Ca10-P>Ca8-P>Fe-P≈Al-P≈OC-P>Ca2-P序列变化,其中Ca2-P和Al-P总共仅占无机磷总量的11.47%—19.43%,表明紫色土中对植物最有效的磷源不足;而Ca10-P和OC-P共占无机磷总量的42.48%—59.55%,意味着紫色土无机磷有一半左右是以作物不可利用的形态存在的。紫色土全磷与无机磷、有机磷、Ca2-P、Ca8-P、Al-P、Fe-P、OC-P及Ca10-P呈显著正相关;无机磷与多种形态磷呈显著正相关(除有机磷、Ca2-P、有效磷外);有机磷与全磷、Ca2-P显著正相关;有效磷与全磷、Ca2-P、Al-P、Fe-P显著正相关;无机磷组分间也都存在显著正相关关系(OC-P与Ca10-P间有极显著正相关,但它们与其它无机磷组分无相关性)。表明在土壤磷的整个循环系统中,不同组分无机磷与有机磷之间处于一个动态平衡中,它们之间存在着相互影响和制约。土壤pH与各形态磷关系密切。对土壤有效磷与无机磷组分间的关系进行系统分析,简单相关分析结果土壤有效磷与Ca2-P、Fe-P呈极显著正相关,与Al-P呈显著正相关,与Ca8-P、OC-P、Ca10-P正相关但不显著;通径分析结果对土壤有效磷直接影响较大的无机磷组分是Al-P、Ca8-P与Ca2-P,其中Ca8-P的直接影响为负效应;逐步回归分析结果与通径分析一致。综合分析得出,Ca2-P、Al-P是最有效的磷源,Fe-P、Ca8-P次之,Ca10-P与OC-P是非有效磷源。莴笋和白菜产量与紫色土壤Ca2-P、Ca8-P、Al-P、Fe-P呈显著正相关,与OC-P、Ca10-P无相关性。紫色土各形态无机磷与两种蔬菜产量的相关系数r大小依次为Ca2-P>Fe-P>AL-P>Ca8-P>Ca10-P>OC-P,这与各形态无机磷与有效磷简单相关分析的结果一致。  相似文献   

13.
The occurrence and distribution of an actinobacteria group of bacteria capable of dissolving insoluble phosphates were investigated in this study in marine environments, especially in sediments of Chorao Island, Goa Province, India. A total of 200 bacterial isolates of actinobacteria was isolated. All isolates were screened for phosphate-solubilizing activity on Pikovskaya’s agar. Thirteen different isolates exhibiting maximum formation of halos (zone of solubilization) around the bacterial colonies were selected for quantitative estimations of P-solubilization. Quantitative estimations for P-solubilization were analyzed for up to 10 days at intervals of 24 h. Maximum solubilization from 89.3 ± 3.1 to 164.1 ± 4.1 μg ml?1 was observed after 6 days of incubation in six of all isolates, while the isolate NII-1020 showed maximum P-solubilization. The increase in solubilization coincided with the drop in pH. Many of these species showed wide range of tolerance to temperature, pH, and salt concentrations. Further, 16S rRNA gene sequence analyses were carried to identify the bacterial groups which are actively solubilized phosphate in vitro. Gene sequencing results reveal that all isolates were clustered into six different actinobacterial genera: Streptomyces, Microbacterium, Angustibacter, Kocuria, Isoptericola, and Agromyces. The presence of phosphate-solubilizing microorganisms and their ability to solubilize phosphate were indicative of the important role played by bacteria in the biogeochemical cycle of phosphorus and the plant growth in coastal ecosystems.  相似文献   

14.
A total of 30 bacteria were isolated from the rhizoplane of rice cv. BR29 cultivated in Mymensingh, Bangladesh and from the seedlings obtained from surface-sterilized seeds of BR29. Upon screening, 6 isolates showed varying levels of phosphate solubilizing activity in both agar plate and broth assays using National Botanical Research Institute's phosphate medium. The bacterial isolates were identified based on their phenotypic and 16S rRNA genes sequencing data as Acinetobacter sp. BR-12, Klebsiella sp. BR-15, Acinetobacter sp. BR-25, Enterobacter sp. BR-26, Microbacterium sp. BRS-1 and Pseudomonas sp. BRS-2. The BR-25 exhibited highest phosphate solubilizing activity followed by BR-15. They grew rapidly in the liquid medium at pH 5 and 7 but almost no growth occurred at pH 3. The pH value of the culture medium was decreased with bacterial growth suggesting that they might secrete organic acids to solubilize insoluble phosphorus. Scanning electron microscope analysis of two-week-old rice seedlings germinated from seeds previously inoculated with BR-25 and BR-15 revealed dense colonization at the root surfaces presumably using fimbriae on the bacterial cells.  相似文献   

15.
Microbial solubilization of rock phosphate is getting more and more attention recently. However, the microorganisms used in previous studies were mostly single or known species, and seldom studies focused on the mixed microorganisms or microbial consortia from natural environments. In this study, a microbial consortium taken from activated sludge was used to solubilize two different mid-low-grade rock phosphates. The results showed that the microbial consortium could effectively solubilize the rock phosphates in National Botanical Research Institute’s phosphate growth medium and released soluble phosphorus in the broth. The biomass increased gradually, whereas the pH decreased sharply during the solubilizing process. The maximum phosphorus solubilization was recorded at particle size of 150?µm. Higher or lower than this optimal particle size, the phosphorus solubilization decreased. The phosphorus solubilization gradually decreased with a larger pulp density from 1 to 5%, and the optimal pulp density was 1%. The solubilization level of microbial consortium varied with different rock phosphates. The results revealed that the soluble phosphorus released from high-silicon ore was higher than which from high-magnesium ore. A strong positive correlation between biomass and phosphorus solubilization in the broth was observed from regression analysis results, and the phosphorus solubilization also had a significant negative correlation with pH in the broth.  相似文献   

16.
温度和施磷对石灰性潮土小麦苗期生长及磷形态的影响   总被引:3,自引:0,他引:3  
以石灰性潮土为对象,通过盆栽试验研究温度和磷肥对小麦苗期生长和土壤无机磷形态转化的影响.结果表明: 温度和磷肥是影响小麦生长的重要因子,但二者交互作用影响不显著.温度对小麦生长的影响大于施用磷肥,15 ℃是小麦苗期的适宜生长温度.与不施磷肥(-P)处理相比,5 ℃下,施磷肥(+P)处理显著促进了小麦生长,小麦地上部、根部生物量分别提高18.2%、33.3%,地上部、根部磷素积累量分别提高30.6%、13.3%,根冠比、株高、分蘖、根系活力分别提高3.5%、10.0%、10.5%、70.3%;15 ℃下,施用磷肥对小麦生物量、分蘖影响不显著,但小麦地上部、根部磷素积累量分别提高32.3%、23.8%,根冠比、株高、根系活力分别提高15.6%、2.5%、32.8%;25 ℃下施用磷肥对小麦生长没有促进作用. 3种温度下,施磷能显著增加各处理土壤有效磷(Olsen-P)、二钙磷(Ca2-P)、八钙磷(Ca8-P)、铝磷(Al-P)和铁磷(Fe-P)含量.-P和+P处理下,温度对Ca2-P含量影响不显著,对Olsen-P、Ca8-P、Fe-P、Al-P含量影响显著.Ca8-P、Fe-P含量表现为5 ℃>15 ℃>25 ℃;Al-P含量表现为25 ℃>15 ℃>5 ℃.小麦苗期可以吸收利用根际土壤Ca2-P、Ca8-P、Al-P、Fe-P,而Al-P、Fe-P对小麦的有效性明显低于Ca2-P、Ca8-P.各处理pH、闭蓄态磷(O-P)和十钙磷(Ca10-P)差异不显著.总之,温度主要通过影响小麦生长来影响磷素吸收,低温下施用磷肥能显著促进小麦生长,高温能加速石灰性土壤有效磷的固定,施磷能缓解这一过程.  相似文献   

17.
A total of 36 fungal species isolated from soil were tested for their ability to solubilize rock phosphate (RP) in agar plates. Most of these fungi were non-rock phosphate solubilizers, but two isolates, Aspergillus niger and Penicillium citrinum, had high activity. Liquid culture experiments revealed that both fungi caused a remarkable drop in pH of culture media and solubilized considerable amounts of phosphate. The effects on wheat of inoculation with vesicular–arbuscular mycorrhizal fungi and rock-phosphate-solubilizing fungi and fertilization with rock phosphate were studied in sterilized pot soils, nonsterilized pot trials and in field plot soils. Rock phosphate fertilization and inoculation with Glomus constrictum and rock-phosphate-solubilizing fungi (A. niger and P. citrinum) significantly increased dry matter yield of wheat plants under all experimental conditions. However, the effect was more evident in non- sterilized pot soils and in the field than in sterilized pots. Rock phosphate had no significant effect on the total phosphorus content of plants grown under pot conditions but it was significantly increased in field plots; the effect of inoculation with fungi (G. constrictum, A. niger and P. citrinum) on plant phosphorus was closely related to this in dry matter production. The greatest positive effect on growth and phosphorus contents of wheat plants was recorded in the treatments that received rock phosphate and were inoculated with a mixed inoculum of the three microorganisms used, followed by dual inoculation treatments of G. constrictum plus either A. niger or P. citrinum.  相似文献   

18.
A total of 36 fungal species isolated from soil were tested for their ability to solubilize rock phosphate (RP) in agar plates. Most of these fungi were non-rock phosphate solubilizers, but two isolates, Aspergillus niger and Penicillium citrinum, had high activity. Liquid culture experiments revealed that both fungi caused a remarkable drop in pH of culture media and solubilized considerable amounts of phosphate. The effects on wheat of inoculation with vesicular–arbuscular mycorrhizal fungi and rock-phosphate-solubilizing fungi and fertilization with rock phosphate were studied in sterilized pot soils, nonsterilized pot trials and in field plot soils. Rock phosphate fertilization and inoculation with Glomus constrictum and rock-phosphate-solubilizing fungi (A. niger and P. citrinum) significantly increased dry matter yield of wheat plants under all experimental conditions. However, the effect was more evident in non- sterilized pot soils and in the field than in sterilized pots. Rock phosphate had no significant effect on the total phosphorus content of plants grown under pot conditions but it was significantly increased in field plots; the effect of inoculation with fungi (G. constrictum, A. niger and P. citrinum) on plant phosphorus was closely related to this in dry matter production. The greatest positive effect on growth and phosphorus contents of wheat plants was recorded in the treatments that received rock phosphate and were inoculated with a mixed inoculum of the three microorganisms used, followed by dual inoculation treatments of G. constrictum plus either A. niger or P. citrinum.  相似文献   

19.
有机酸对土壤无机态磷转化和速效磷的影响   总被引:13,自引:0,他引:13  
土壤有效磷含量低是影响作物生产的重要限制因素之一.作物根分泌活化难溶性磷的有机酸对改善其磷素营养具有重要意义.采用张守敬和Jackson无机磷分级方法,以湖北省3种pH值土壤为材料,加入不同磷源和有机酸,经过室温培养后,测定速效磷含量和无机磷组分的变化.结果表明:施磷显著提高了土壤中速效磷含量,中性土、酸性土Fe-P和Al-P含量大幅上升, Fe-P占增加量的50%以上,而碱性土Ca-P含量显著增加.加施有机酸使中性土速效磷含量增多,除苹果酸处理的变幅较小外,草酸和柠檬酸的加入速效磷显著增加.由于有机酸的作用,中性土Al-P含量下降,Ca-P含量上升,变幅大小依次为草酸>柠檬酸>苹果酸;酸性土中Al-P含量呈下降趋势,碱性土中Ca-P含量有不同程度的减少,3种土壤中O-P含量均有所增加.说明有机酸活化的磷主要来源于中性土和酸性土Al-P、Fe-P及碱性土Ca-P中的磷,同时有机酸能够促进土壤中闭蓄态磷(O-P)的形成与积累.  相似文献   

20.
Five of the 207 isolates from different composts, farm waste compost (FWC), rice straw compost (RSC), Gliricidia vermicompost (GVC), and macrofauna, showed rock phosphate (RP) solubilization in buffered medium in plate culture. When tested in RP broth medium, all five strains, Enterobacter cloacae EB 27, Serratia marcescens EB 67, Serratia sp. EB 75, Pseudomonas sp. CDB 35, and Pseudomonas sp. BWB 21, showed gluconic acid production and solubilized RP. Based on cellulose-degrading and P-solubilizing ability, two strains were selected for further studies. In the presence of different carbon sources, both strains showed a drop in pH and solubilized RP. P released was maximum with glucose (1212 and 522 μmol) and minimum with cellobiose (455 and 306 μmol) by S. marcescens EB 67 and Pseudomonas sp. CDB 35, respectively. Glucose dehydrogenase (GDH) activity was 63 and 77% with galactose and 35 and 46% with cellobiose when compared to glucose (100%) by EB 67 and CDB 35, respectively. Both strains solubilized RP in the presence of different crop residues. EB 67 and CDB 35 showed maximum cellulase activity (0.027 units) in the presence of rice straw and a mixture of rice straw and root. P solubilized from RP in the presence of pigeonpea root was 134 and 140 μmol with EB 67 and CDB 35. Significantly, these bacteria isolated from composts and macrofauna solubilized rock phosphate in the presence of various pure carbon substrates and crop residues and their importance in soil/rhizosphere conditions is discussed.  相似文献   

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