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1.
Microorganisms (348 fungi, 388 actinomycetes and 319 bacteria) were isolated from a nodulation problem soil, a non-problem virgin soil, a cultivated problem soil and the rhizosphere of clover plants grown in the problem soil. Rhizobium trifolii TA 1 which failed to establish in problem soils was inhibited on laboratory media by a greater number of these soil microorganisms than the better soil colonizing R. trifolii (WU95 and WU290) and R. lupini (WU425). R. lupini was not inhibited or stimulated on agar by many soil or rhizosphere isolates. R. meliloti showed greater stimulation than either R. trifolii or R. lupini and was inhibited by relatively few soil microorganisms so that its poor soil survival was thought to be due to chemical or physical soil conditions rather than to biotic factors. The greatest incidence of rhizobial inhibitors, mainly associated with TA 1, was found among the isolates from the clover rhizosphere. There was a reduction in the relative numbers of rhizobial inhibitors isolated from the cultivated soil compared with the virgin problem soils, a result possibly due to the changed soil environment changing with cultivation, altered vegetation and the addition of superphosphate. Inhibitors of rhizobia were more frequent amongst the bacteria than fungi or actinomycetes. Strong stimulation was more commonly shown by fungi than by actinomycetes or bacteria. The interaction on agar between rhizobia and the soil microflora is related to soil colonization and persistence. 相似文献
2.
Barbara Thuerig 《Soil biology & biochemistry》2009,41(10):2153-2161
The aim of this study was to investigate the potentials and limitations in restoring soil suppressiveness in disturbed soils. Soils from three sites in UK and Switzerland (STC, REC, THE) differing in their level of suppressiveness to soil-borne and air-borne diseases were γ-irradiated and this soil matrix was re-inoculated with 1% (w/w) of either parent native soil or native soil from the other sites (‘soil inoculum’). Suppressiveness to air-borne and soil-borne diseases was quantified by means of the host-pathogen systems Lepidium sativum (cress)-Pythium ultimum, an oomycete causing root rot and seedling damping-off, and Arabidopsis thaliana-Hyaloperonospora parasitica, an oomycete causing downy mildew. Soil microbial biomass, activity and community structure, as determined by phospholipid fatty acid (PLFA) profiles, were measured in native, γ-irradiated, and re-inoculated soils. Both, L. sativum and A. thaliana were highly susceptible to the pathogens if grown on γ-irradiated soils. Re-inoculation completely restored suppressiveness of soils to the foliar pathogen H. parasitica, independently of soil matrix or soil inoculum, whereas suppressiveness to P. ultimum depended on the soil matrix and, to a lesser extent, on the soil inoculum. However, the soil with the highest inherent suppressiveness did not reach the initial level of suppressiveness after re-inoculation. In addition, native microbial populations as defined by microbial biomass, activity and community structure, could not be fully restored in re-inoculated soils. As for suppressiveness to P. ultimum, the soil matrix, rather than the source of soil inoculum was identified as the key factor for re-establishing the microbial community structure. Our data show that soils do not or only slowly fully recover from sterilisation by γ-irradiation, indicating that agricultural soil management practices such as soil fumigation or heat treatments frequently used in vegetable cropping should be avoided. 相似文献
3.
Populations of the mycophagous soil ncmatode Aphelenchus avenae living in sterile sand were reduced by addition of conidia of Nematoctonus concurrens and N. haptocladus. Natural, mixed nematode populations in non-sterile soil were unaffected by comparable treatments. Observations on conidia placed in contact with non-sterile soil showed that their germination was inhibited and that lysis of their germlings occurred. 相似文献
4.
Ecosystems of northern North America existed without earthworm fauna until European settlers arrived and introduced European species. The current extent of invasion by some of these species, Lumbricus terrestris L., Octolasion tyrtaeum Savigny and Dendrobaena octaedra Savigny, into an aspen forest in the Canadian Rocky Mountains and the effects of the invasion on soil chemistry, microflora, soil microarthropods and vegetation were investigated. Densities of earthworm species, soil structure, plant coverage and abundance were determined along three transects starting at the edge of the forest. At locations with L. terrestris, litter was incorporated into the soil, and where O. tyrtaeum was present, organic layers were mixed with mineral soil layers. Organic layers disappeared almost entirely when both species occurred together. Carbon and nitrogen concentrations were reduced in organic layers in the presence of L. terrestris and O. tyrtaeum. Microbial biomass and basal respiration were reduced when L. terrestris and O. tyrtaeum were present, presumably due to resource competition and habitat destruction. Microarthropod densities and the number of microarthropod species were strongly reduced in the presence of O. tyrtaeum (−75% and −22%, respectively), probably through mechanical disturbances, increasing compactness of the soil and resource competition. The coverage of some plant species was correlated with earthworm abundance, but the coverage of others was not. Despite harsh climatic conditions, the invasion of boreal forest ecosystems by mineral soil dwelling earthworm species is proceeding and strongly impacts soil structure, soil chemistry, microorganisms, soil microarthropods and vegetation. 相似文献
5.
The aerobic and anaerobic degradation of phenol and selected chlorophenols was examined in a clay loam soil containing no added nutrients. A simple, efficient procedure based on the high solubility of these compounds in 95% ethanol was developed for extracting phenol and chlorophenol residues from soil. Analysis of soil extracts with UV spectrophotometry showed that phenol,o-chlorophenol,p-chlorophenol, 2,4-dichlorophenol, 2,6-dichlorophenol and 2,4,6-trichlorophenol were rapidly degraded, whilem-chlorophenol, 3,4-dichlorophenol, 2,4,5-trichlorophenol and pentachlorophenol were degraded very slowly by microorganisms in aerobically-incubated soil at 23°C. Both 3,4,5-trichlorophenol and 2,3,4,5-tetra chlorophenol appeared to be more resistant to degradation by aerobic soil microorganisms at 23°C. None of the compounds examined were degraded by microorganisms in anaerobically-incubated soil at 23°C. Direct microscopic observation revealed that phenol and selected chlorophenols stimulated aerobic and to a lesser extent, anaerobic microbial growth in soil, and aerobic soil bacteria were responsible for the degradation of 2,4-dichlorophenol in aerobically-incubated soil at 23°C. Phenol,o-chlorophenol,m-chlorophenol,p-chlorophenol and 2,4-dichlorophenol underwent rapid non-biological degradation in sterile silica sand. Non-biological decomposition contributed, perhaps substantially, to the removal of some chlorophenols from sterile aerobically-incubated soil and both sterile and non-sterile anaerobically-incubated soil. 相似文献
6.
The distribution of β-glucosidase activity in a tomato-field soil was examined. Of the total activity found, > 50% was in the < 2mm soil fraction, 20% in the organic debris and a significant proportion in roots. In an attempt to determine the origin of β-glucosidase in this soil, the properties of β-glucosidase of various fungal and bacterial isolates from the soil, and of plant materials, were studied.Selective inhibition of bacterial or fungal growth in re-moistened, over-dried, inoculated soil indicated that fungi were a more important source of β-glucosidase in this soil. Monierella, Actinomucor, Coniochaeta and Penicillium were the principal fungi isolated from the soil by the dilution-plate technique, comprising over 60% of the total isolates. Remoistened oven-dried soil, inoculated with Mortierella and Actinomucor spp exhibited higher β-glucosidase activity after incubation than did soil inoculated with other strains.The β-glucosidase activity of extracts from cultured fungal strains had similar pH optima and Q10 values to those of soil extracts. The β-glucosidase of extracts from isolates of bacteria and actinomycetes had similar Q10 values, but higher pH optima, than did that of soil extracts.These results indicate that fungi, mainly some of the mucoraceous fungi, may be the primary source of β-glucosidase in tomato-field soil. 相似文献
7.
Plant invasions alter soil microbial community composition; this study examined whether invasion-induced changes in the soil microbial community were reflected in soil aggregation, an ecosystem property strongly influenced by microorganisms. Soil aggregation is regulated by many biological factors including roots, arbuscular mycorrhizal fungal hyphae, and microbially-derived carbon compounds. We measured root biomass, fungal-derived glomalin-related soil protein (GRSP), and aggregate mean weight diameter in serpentine soils dominated by an invasive plant (Aegilops triuncialis (goatgrass) or Centaurea solstitialis (yellow starthistle)), or by native plants (Lasthenia californica and Plantago erecta, or Hemizonia congesta). Root biomass tended to increase in invaded soils. GRSP concentrations were lower in goatgrass-dominated soils than native soils. In contrast, starthistle dominated soil contained a higher amount of one fraction of GRSP, easily extractable immunoreactive soil protein (EE-IRSP) and a lower amount of another GRSP fraction, easily extractible Bradford reactive soil protein (EE-BRSP). Soil aggregation increased with goatgrass invasion, but did not increase with starthistle invasion. In highly aggregated serpentine soils, small increases in soil aggregation accompanying plant invasion were not related to changes in GRSP and likely have limited ecological significance. 相似文献
8.
Disease suppressiveness against Rhizoctonia solani AG 2-1 in cauliflower was studied in two marine clay soils with a sandy loam texture. The soils had a different cropping history. One soil had a long-term (40 years) cauliflower history and was suppressive, the other soil was conducive and came from a pear orchard not having a cauliflower crop for at least 40 years. These two soils were subjected to five successive cropping cycles with cauliflower or remaining fallow in a greenhouse experiment. Soils were inoculated with R. solani AG 2-1 only once or before every crop. Disease decline occurred in all treatments cropped with cauliflower, either because of a decreased pathogen population or increased suppressiveness of the soil. Disease suppressiveness tests indicated that the conducive soil became suppressive after five subsequent cauliflower crops inoculated each cycle with R. solani AG 2-1. Suppressiveness of all treatments was measured in a seed germination test (pre-emergence damping-off) as well as by measuring the spread of R. solani symptoms in young plants (post-emergence damping-off). Results showed that suppressiveness was significantly stimulated by the successive R. solani inoculations; presence of the cauliflower crop had less effect. Suppressiveness was of biological origin, since it disappeared after sterilization of the soil. Moreover, suppressiveness could be translocated by adding 10% suppressive soil into sterilized soil. The suppressive soil contained higher numbers of culturable filamentous actinomycetes than the conducive soil, but treatments enhancing suppressiveness did not show an increased actinomycetes population. The suppressiveness of the soil samples did also not correlate with the number of pseudomonads. Moreover, no correlation was found with the presence of different mycoparasitic fungi, i.e. Volutella spp., Gliocladium roseum, Verticillium biguttatum and Trichoderma spp. The suppressive soil contained a high percentage of bacteria with a strong in vitro inhibition of R. solani. These bacteria were identified as Lysobacter (56%), Streptomyces (23%) and Pseudomonas (21%) spp. A potential role of Lysobacter in soil suppressiveness was confirmed by quantitative PCR detection (TaqMan), since a larger Lysobacter population was present in suppressive cauliflower soil than in conducive pear orchard soil. Our experiments showed that successive cauliflower plantings can cause a decline of the damage caused by R. solani AG 2-1, and that natural disease suppressiveness was most pronounced after subsequent inoculations with the pathogen. The mode of action of the decline is not yet understood, but antagonistic Lysobacter spp. are potential key organisms. 相似文献
9.
Inês Rocha Edgar Pinto Isabel M. P. L. V. O. Ferreira Manuela V. da Silva Rui S. Oliveira 《Journal of Soils and Sediments》2014,14(4):829-834
Purpose
Polycyclic aromatic hydrocarbons (PAHs) are a class of organic compounds commonly found as soil contaminants. Fungal degradation is considered as an environmentally friendly and cost-effective approach to remove PAHs from soil. Acenaphthylene (Ace) and Benzo[a]anthracene (BaA) are two PAHs that can coexist in soils; however, the influence of the presence of each other on their biodegradation has not been studied. The biodegradation of Ace and BaA, alone and in mixtures, by the white rot fungus Pleurotus ostreatus was studied in a sandy soil.Materials and methods
Experimental microcosms containing soil spiked with different concentrations of Ace and BaA were inoculated with P. ostreatus. Initial (t 0) and final (after 15 days of incubation) soil concentrations of Ace and BaA were determined after extraction of the PAHs.Results and discussion
P. ostreatus was able to degrade 57.7% of the Ace in soil spiked at 30 mg kg?1 dry soil and 65.8% of Ace in soil spiked at 60 mg kg?1 dry soil. The degradation efficiency of BaA by P. ostreatus was 86.7 and 77.4% in soil spiked with Ace at 30 and 60 mg kg?1 dry soil, respectively. After 15 days of incubation, there were no significant differences in Ace concentration between soil spiked with Ace and soil spiked with Ace + BaA, irrespective of the initial soil concentration of both PAHs. There were also no differences in BaA concentration between soil spiked with BaA and soil spiked with BaA + Ace.Conclusions
The results indicate that the fungal degradation of Ace and BaA was not influenced by the presence of each other’s PAH in sandy soil. Bioremediation of soils contaminated with Ace and BaA using P. ostreatus is a promising approach to eliminate these PAHs from the environment. 相似文献10.
《Geoderma》2005,124(1-2):193-202
In semiarid climate soils, the establishment of a plant cover is fundamental to avoid degradation and desertification processes. A better understanding of the ability of plants to promote soil microbial processes in these conditions is necessary for successful soil reclamation. Six different plant species were planted in a semiarid soil, in order to know which species are the most effective for the reclamation of semiarid areas. Six years after planting, the rhizosphere soils were studied by measuring chemical (pH, electrical conductivity, total organic carbon and other carbon fractions), physical (% of saggregates), microbiological (microbial biomass carbon and soil respiration), and biochemical (dehydrogenase, phosphatase, β-glucosidase and urease activities) parameters. In general, in all the soil–plant systems plant nutrients, organic matter and microbial activity increased compared to the control soil. For some species, such as Rhamnus lycioides, the increase in the total organic carbon content (TOC) in the rhizosphere zone was almost 200%. A positive correlation was found between TOC and water-soluble carbon (p<0.001); both parameters were negatively correlated with electrical conductivity. Microbial biomass carbon and soil respiration were highest in the rhizosphere of Stipa tenacissima (98% and 60%, respectively, of increase on soil control values) and Rosmarinus officinalis (94% and 51%, respectively, of increase on soil control values). These microbiological parameters were correlated with the percentage of stable aggregates (p<0.01). Enzyme activities were affected by the rhizosphere, their values depending on the shrub species. 相似文献
11.
Jenny S.K. Bäckman Anna HermanssonChristoph C. Tebbe Per-Eric Lindgren 《Soil biology & biochemistry》2003,35(10):1337-1347
The autotrophic ammonia-oxidising bacterial (AOB) community composition was studied in acid coniferous forest soil profiles at a site in southwestern Sweden 6 years after liming. Liming caused a significant increase in pH in the organic horizons, while the mineral soil was unaffected. The AOB communities were studied by single-strand conformation polymorphism (SSCP) in parallel with denaturing gradient gel electrophoresis (DGGE) analysis of partial 16S rRNA genes amplified by PCR using primers reported to be specific for β-Proteobacteria AOB, followed by nucleotide sequencing. High genetic diversity of Nitrosospira-like sequences was found in the limed soil profiles, whereas no AOB-like sequences were detected in the control soil at any depth, according to both the SSCP and DGGE analyses. This clearly showed that liming induced growth of a diverse flora of AOB at this forest site. Both Nitrosospira cluster 2 and cluster 4 sequences were present in the limed soil profiles, regardless of soil pH, but we found a higher number of sequences affiliated with cluster 4. The high lime dose seemed to affect the AOB community more than the low dose, and its effects reached deeper into the soil profile. Seven different Nitrosospira-like sequences were found 10 cm under the litter layer in the soil limed with the high dose, but only two in the soil amended with the low lime dose. 相似文献
12.
Paula Lorenzo Susana Rodríguez-Echeverría Luís González Helena Freitas 《Applied soil ecology》2010,44(3):245-251
Acacia dealbata Link is an Australian woody legume that has become a serious environmental problem in Northwest Spain where it forms dense monospecific patches modifying the structure of different native ecosystems and threatening native aboveground biodiversity. In spite of the dramatic changes observed in the vegetation of invaded sites little is known about the consequences of invasion for soil microorganisms. To investigate the effect of A. dealbata invasion on the structure of soil fungi and bacteria communities, samples were taken from invaded and non-invaded areas from three different ecosystems in Northwest Spain: pine forest, shrubland and grassland. In each ecosystem type, soil samples were taken in areas of native vegetation, areas invaded by A. dealbata and in the transition zone between native and invaded vegetation. Soil microorganisms were analyzed in the different samples by PCR-DGGE using general primers for eubacteria and fungi. Soil analyses were also performed to evaluate the effect of A. dealbata invasion on soil fertility.The invasion by A. dealbata consistently increased soil N, C, organic matter and exchangeable P content in the three studied ecosystems. A clear effect of the invasion on the overall structure of microorganism communities was only observed in the shrubland where soil fungal communities in the invaded and transition areas clustered together and apart from the native soil. Significant differences in soil microorganisms richness and diversity between invaded and not invaded soils were only found in the grassland. Grassland invasion by A. dealbata lead to a significant increase of bacterial richness and to a significant reduction in fungal richness and diversity. Our results show that although the changes on soil chemistry due to A. dealbata invasion are consistent among the studied ecosystems, the effect on soil microorganisms depends on the ecosystem type affected by the invasion. 相似文献
13.
《Applied soil ecology》2007,35(1):237-246
Effectiveness of Trichoderma strains for biocontrol of soilborne pathogens requires an improved understanding of soil and root ecology of this fungus. We compared the population dynamics of Trichoderma hamatum strain T382 (T382) and indigenous Trichoderma spp. in soil and on roots in different strawberry production systems. Strawberry transplants, either amended or not-amended with Trichoderma biocontrol strains, were planted in field soil left untreated or treated with soil fumigant, compost, and compost-amended with T382. Soil and root samples were taken between October and June of two production seasons (2002-03 and 2003-04), and Trichoderma populations were assessed by plating soil dilutions and root pieces onto selective medium. Identity of T382 was confirmed using strain-specific primers. T382 became established and maintained a stable population of 103 cfu/g soil throughout the growing season when added to field soil in amended compost, but T382 was rarely isolated from strawberry roots. Populations of indigenous Trichoderma spp. were up to 60-fold greater in fumigated soil than in any other soil treatment. Indigenous Trichoderma spp. were isolated from a greater proportion (20–50%) of roots in fumigated soil than from roots in the other treatments (0–20%). Transplant treatments did not significantly affect Trichoderma populations on roots or in soil during field production. This study showed that compost may be used as a substrate to establish and promote survival of Trichoderma in field soil, and illustrates how soil manipulation can affect population dynamics of indigenous Trichoderma spp. on roots and in soil. 相似文献
14.
H.Pauline McColl 《Soil biology & biochemistry》1984,16(2):139-143
Enchytraeid and earthworm populations of a Typic Haplaquoll soil after application of the nematicides oxamyl and phenamiphos were examined for 1 yr. The nematicides had no effect on enchytraeid numbers, which were positively correlated with soil moisture and the previous month's rainfall. Earthworm populations were dominated by Allolobophora caliginosa (Savigny) with A. trapezoides (Duges) and Eiseniella tetraedra (Savigny) also present. Both nematicides initially depressed earthworm numbers and the effects of phenamiphos appeared to persist until the soil became wet in Autumn. Earthworm numbers were positively correlated with soil moisture and previous month's rainfall. Enchytraeid numbers at 2.5–5 cm depth were negatively correlated with soil temperature. Numbers of enchytraeids at 0–2.5 cm depth and earthworms were not significantly related to soil temperature. 相似文献
15.
The effect of bacteria represented by indigenous soil microflora or a mixture of soil bacteria Pseudomonas aeruginosa and Rhodococcus erythropolis on fungal growth, extracellular enzyme production and polycyclic aromatic hydrocarbons (PAHs) biodegradation efficiency in soil of white-rot fungi Trametes versicolor and Irpex lacteus was investigated. Both fungi were able to colonize soil. The growth yields measured by ergosterol were about two-fold in I. lacteus after 10 weeks. Laccase was produced in T. versicolor cultures in the presence or absence of bacteria but live bacteria reduced the laccase levels in soil about 5 times. Manganese-dependent peroxidase (MnP) was not detected in T. versicolor cultures. The amounts of MnP and laccase in I. lacteus cultures were not affected by the presence of bacteria. T. versicolor was more efficient in PAH removal for all PAHs tested although its capacity to colonize soil was lower. The removal rates of PAHs by T. versicolor in sterile soil were 1.5-fold, 5.8-fold and 1.8-fold for 2-3-ring, 4-ring and 5-6-ring PAHs, compared to I. lacteus, respectively. I. lacteus showed a low efficiency of removal of pyrene, benzo[a]anthracene and benzo[k]fluoranthene, compared to T. versicolor, whereas chrysene and benzo[b]fluoranthene were degraded by neither fungus. The main effect of the presence of the indigenous microflora or R. erythropolis and P. aeruginosa was a significant decrease of degradation of total PAHs by both T. versicolor and I. lacteus. Weak fungal/bacterial synergistic effects were observed in the case of removal of acenapthylene, benzo[a]pyrene, dibenzo[a,h]anthracene and benzo[g,h,i]perylene by I. lacteus and acenapthylene by T. versicolor. However, the bacterial effects were different in the two fungi. PAH abiotic losses represented 15 and 21% of the total PAHs after 5 and 10 weeks, respectively; naphthalene and acenaphthene were removed from the soil due to volatilization. 相似文献
16.
At the Eastern planes of Venezuela, large to tracts of pastureland are sustained by low fertility acid soils that often lead to overgrazing, decreased pasture production, invasion by weeds, and soil compaction and erosion. The objective of this study was to evaluate the behavior of local forage legume species and its influence on chemical and biochemical properties of soil with the ultimate goal of identifying which one of these species have the potential to be used as cover in the establishment of a “Ley farming” system. The study was conducted on an Oxisol and used five local species from the genus Centrosema (Centrosema brasilianum, Centrosema macrocarpum, Centrosema pascuorum, Centrosema rotundifolium and Centrosema molle) which were established as cover for a period of 3 years. Dry matter (DM) and soil samples were collected twice a year, during the dry season (April) and during the rainy season (October). The soil parameters evaluated were total nitrogen, organic matter, calcium, potassium, magnesium, pH, soil respiration, and enzymatic activities that include β-glucosidase, arylsulphatase, phosphatase, urease, protease, dehydrogenase and catalase. The annual average data were used to identify indicators of soil quality through principal component analysis (PCA) that led to calculate a soil quality index (SQI). The results indicated that DM production varied among the different legume covers, showing C. macrocarpum the greatest productivity (1340 kg h−1). The PCA identified seven of the tested soil variables as quality indicators: total nitrogen, pH, calcium, soil respiration and arylsulfatase and β-glucosidase activities. Total nitrogen, P and β-glucosidase activity were the indicators showing the largest changes over time being able to discriminate between treatments. After the 3 year period of the trial the SQI of the soil tested raised from 0.17 (very low quality) to 0.30 (low quality) where C. brasilianun, C. pascuorum and C. molle were established and to 0.40 (moderate quality) where C. macrocarpum and C. rotundifolium were established. Thus, the legume crop covers influenced positively the soil quality. C. macrocarpum was the legume cover that showed the greatest soil improvement, having the best potential to be used as forage cover to establish a “Ley farming” system at the Eastern planes of Venezuela. 相似文献
17.
G.C. Papavizas 《Soil biology & biochemistry》1977,9(5):343-348
Exposure of sclerotia of Macrophomina phaseolina to 0 and 33% relative humidity (r.h.) for 12 weeks and of Sclerotium cepivorum to 0, 33 and 55% r.h. for 20 weeks did not reduce their germinability on agar. Exposure to 78% r.h. caused high loss of germinability in M. phaseolina and complete loss in S. cepivorum. After 7-day exposures respective moisture contents of sclerotia of M. phaseolina and S. cepivorum were 1 and 2% at 0% r.h.; and 10 and 14% at 78% r.h. M. phaseolina sclerotia held at 0% and 33% r.h. in desiccators for several times up to 12 days did not decrease in subsequent survivability in moist soil, unlike sclerotia held at 78% r.h. for 4 days.More sclerotia of M. phaseolina were colonized by fungi and Streptomyces spp. on alkaline soil than on acid soil. On alkaline soil twice as many sclerotia were colonized after exposure to 0% r.h. as after exposure to 33, 55 and 78% r.h. Colonization of S. cepivorum sclerotia was as high on acid as on alkaline soil and 3 times as high on sclerotia treated at 0% r.h. as on those treated at higher r.h. Attempts to ascertain the effects of colonization on sclerotial viability were unsuccessful. Incubation of sclerotia of M. phaseolina in moist Rumsford sandy loam (50% m.h.c.) for 20 weeks reduced survivability by 43%. At room temperature, alternate drying and wetting of soil containing sclerotia did not appreciably affect survivability of either pathogen. Survivability of S. cepivorum sclerotia was highest when the sclerotia were incubated in air-dried soil (2–3% m.h.c.) for 20 weeks.Incidence of white rot on onion seedlings transplanted to S. cepivorum-infested soil was higher in soil that had been air-dried for 20 weeks than in soil that had been alternately wetted and dried. Sclerotia that were exposed to 0% r.h. for 7 days before soil incubation produced little white rot. 相似文献
18.
Pilar Junier Thomas Junier Karl-Paul Witzel Margarita Carú 《European Journal of Soil Biology》2009,45(2):153-162
The effect of common bean (Phaseolus vulgaris L.) on the composition of nitrogen fixing bacterial assemblages in soil was studied by comparing planted and unplanted soil. The community composition was studied by terminal restriction fragment length polymorphism (T-RFLP) of the nitrogenase reductase gene (nifH). Principal component analysis (PCA) of T-RFLP profiles showed the separation of profiles from planted and unplanted soil. Terminal restriction fragments (T-RFs) corresponding to rhizobial bacteria were identified preferentially in planted soil; however most nifH T-RFs in soil could not be assigned to T-RFs simulated from a database of known diazotrophs. To specifically study rhizobial bacteria in the soil and nodules, PCR products from the alpha subunit of the nitrogenase enzyme (nifD) were analyzed by denaturing gradient gel electrophoresis (DGGE). DGGE results showed the specific stimulation of the rhizobial microsymbionts in planted soil. 相似文献
19.
The interactions between soil type and earthworm species determine the properties of earthworm casts
Earthworms are recognized to increase soil porosity, reorganize soil structure, and stimulate soil microflora and nutrient mineralization. The properties of earthworm casts should depend both on earthworm species or ecological group and on soil properties. Interactions between earthworm species and soil types have been suggested, but only poorly demonstrated. In order to better understand those interactions, two hypotheses led our study: (1) Soil type has a greater influence on cast properties than earthworm; (2) Earthworms from different species influence cast properties differently; (3) The intensity and direction of the impact of each earthworm species on cast properties vary with soil properties. Fifteen physical and chemical variables (N–NH4+, N–NO3−, total organic C and N, C/N ratio, CaCO3, pH, P, K+, Mg2+, Mn2+, Na+, CEC, moisture, wettability) were measured in casts of three earthworm species (Lumbricus terrestris, Allolobophora chlorotica and Aporrectodea rosea) produced in three temperate soils. Univariate and multivariate analyses showed that earthworm species and soil types significantly impacted cast properties. pH, Nt, K and Mg contents were interactively altered by both factors. Multivariate analysis showed that a difference of soil type had a major impact on casts properties (62%) compared to the impact of a difference of earthworm species (10%). Cast properties were most impacted by L. terrestris, then by A. chlorotica and last by A. rosea. The response ratio (ratio of the properties of the casts to the properties of the bulk soil) was used to quantify the effect of earthworm species compared to the control soil. It showed a higher response of variables in casts in nutrient-rich soils, especially in casts of L. terrestris. The interactions between earthworm species and soil types on cast properties were discussed with regards to earthworm ecology, properties of the soil, and earthworm modifications of cast microflora. 相似文献
20.
Yaquelin Nerey Sarah Van Beneden Alexander Jimenez Lidcay Herrera 《Soil biology & biochemistry》2010,42(5):797-803
Calcisol, ferralsol and vertisol soils, representative of different bean production areas of Villa Clara province in Cuba, were selected to determine the impact of soil type on bean hypocotyl rot severity caused by Rhizoctonia solani AG4 HGI (isolate CuVC-Rs7). In inoculated autoclaved soil, hypocotyl rot was most severe in calcisol soil, followed by ferralsol soils and then vertisol soils. In inoculated natural soils, disease severity was lower in vertisol and calcisol soils and higher in ferralsol soil, indicating that biological factors are suppressing or stimulating the pathogenic efficiency of R. solani. Native binucleate Rhizoctonia AGF, Sclerotium rolfsii and R. solani AG 4 HGI were isolated from bean plants grown in natural calcisol, vertisol and ferralsol soils, respectively. Subsequent studies about the interaction between these fungi and R. solani indicated that they were involved in the variability of disease severity caused by R. solani. The addition of R. solani AG4 HGI (isolate CuVC-Rs7) into each autoclaved soil inoculated with binucleate Rhizoctonia or S. rolfsii resulted in a reduction of disease severity caused by this pathogen while in soils inoculated with native R. solani AG4 HGI, disease severity increased. Irrespective of fungal interactions, calcisol was always the most disease conducive soil and vertisol the most disease repressive soil. The mechanisms by which native pathogenic fungi could influence disease severity caused by R. solani are discussed. 相似文献