Importance of soil-water relations in assessing the endpoint of bioremediated soils

This study was conducted to investigate water movement in hydrocarbon contaminated soils. Three soils were studied, a hydrocarbon contaminated soil, the same soil after 3 years of bioremediation, and a control soil from the same site. There was a critical soil water content around 18% (bioremediated soil) and 20% (contaminated soil), above which the sorptivity of the contaminated soil was near that of the control soil. For soils with water contents below this value, there was a strong divergence in sorptivity between contaminated and control or bioremediated soils. Results suggest that water availability in contaminated soils will be highly dependent on soil water properties as water potential approaches the permanent wilting point (-1.5 MPa matrix potential).Infiltration of water into air dry (2% m.c. w/w) hydrocarbon contaminated soils was up to three orders of magnitude slower than for the control soil. For air dried soils, the infiltration rate of the contaminated and bioremediated soils was constant with time. This was in contrast to the control soil where infiltration rate was a function of the reciprocal of the square root of time.     

蚂蚁筑巢对不同恢复阶段热带森林土壤易氧化有机碳时空动态的影响

为探明热带森林恢复过程中蚂蚁筑巢对土壤易氧化有机碳(readily oxidizable carbon, ROC)时空动态的影响及机制, 本研究以西双版纳白背桐(Mallotus paniculatus)群落、野芭蕉(Musa acuminata)群落和崖豆藤(Mellettia leptobotrya)群落3种恢复阶段热带森林为研究对象, 设置“蚂蚁筑巢地”与“非巢地”2种处理进行野外控制实验, 对比分析蚁巢和非蚁巢土壤ROC含量的时空变化特征, 并揭示这些变化与土壤微生物生物量碳及理化性质之间的相互关系。结果表明: (1)蚂蚁筑巢显著影响热带森林土壤ROC含量(P < 0.05), 蚁巢土壤ROC含量较非蚁巢提高了14.2%。不同恢复阶段蚁巢与非蚁巢土壤ROC含量大小顺序为: 野芭蕉群落 > 崖豆藤群落 > 白背桐群落。(2)不同恢复阶段热带森林蚁巢与非蚁巢土壤ROC含量均呈单峰型的时间变化趋势(P < 0.05), 最大值出现在6月, 且各月份蚁巢土壤ROC含量均高于非蚁巢。(3)不同恢复阶段热带森林蚁巢和非蚁巢土壤ROC含量均随土层深度增加呈显著递减的垂直变化趋势(P < 0.05), 且蚁巢土壤ROC含量均大于非蚁巢(P < 0.05)。(4)蚂蚁筑巢引起的土壤理化性质变化对土壤ROC含量产生了一定的影响。土壤ROC含量与土壤pH和容重呈显著负相关(P < 0.05), 与土壤有机碳、微生物生物量碳、全氮、铵态氮及硝态氮呈显著正相关(P < 0.05)。土壤微生物生物量碳与总有机碳是蚁巢土壤ROC时空变化的主要贡献者, 而铵态氮、全氮和总有机碳是非蚁巢ROC时空变化的主控因子。因此, 蚂蚁筑巢改变热带森林土壤微生物量(如微生物生物量碳)及土壤理化性质(如总有机碳、铵态氮与全氮等), 进而显著影响土壤ROC的时空动态。     

Biological consequences of ancient gene acquisition and duplication in the large genome of Candidatus Solibacter usitatus Ellin6076

Members of the bacterial phylum Acidobacteria are widespread in soils and sediments worldwide, and are abundant in many soils. Acidobacteria are challenging to culture in vitro, and many basic features of their biology and functional roles in the soil have not been determined. Candidatus Solibacter usitatus strain Ellin6076 has a 9.9 Mb genome that is approximately 2-5 times as large as the other sequenced Acidobacteria genomes. Bacterial genome sizes typically range from 0.5 to 10 Mb and are influenced by gene duplication, horizontal gene transfer, gene loss and other evolutionary processes. Our comparative genome analyses indicate that the Ellin6076 large genome has arisen by horizontal gene transfer via ancient bacteriophage and/or plasmid-mediated transduction, and widespread small-scale gene duplications, resulting in an increased number of paralogs. Low amino acid sequence identities among functional group members, and lack of conserved gene order and orientation in regions containing similar groups of paralogs, suggest that most of the paralogs are not the result of recent duplication events. The genome sizes of additional cultured Acidobacteria strains were estimated using pulsed-field gel electrophoresis to determine the prevalence of the large genome trait within the phylum. Members of subdivision 3 had larger genomes than those of subdivision 1, but none were as large as the Ellin6076 genome. The large genome of Ellin6076 may not be typical of the phylum, and encodes traits that could provide a selective metabolic, defensive and regulatory advantage in the soil environment.     

Effects of organic matter on sulphur oxidation in soil and influence of sulphur oxidation on soil nitrification

Summary The effects of wheat straw and pressed sugar beet pulp on sulphur oxidation were determined in a loam soil amended with 1% (w/w) elemental sulphur. Wheat straw stimulated the oxidation of elemental sulphur over the first 2 to 3 weeks of the incubation period, resulting in an increase in LiCl-extractable sulphate. After 4 to 7 weeks incubation however, the only significant increase in soil sulphate followed the 1% straw addition, while at week 7 sulphate concentrations in the 0.25% and 5.0% straw amended soils were lower than the control. Pressed sugar beet pulp (1% w/w) initially stimulated the oxidation of elemental sulphur in the soil, but by weeks 3 to 7 of the incubation period rates of oxidation in pulp-amended soils were lower than the control. Towards the end of the incubation period however, sulphate concentrations in the amended soils exceeded the control values, significantly so by week 11. The concentration of thiosulphate and tetrathionate also increased in soils receiving sugar beet pulp. Nitrification was inhibited in soils in which sulphur oxidation was actively occurring. Although possible alternatives are mentioned, such inhibition appears to result from a decrease in soil pH brought about by the oxidation of elemental sulphur to sulphuric acid.     

4种绿化树种盆栽土壤微生物对柴油污染响应及对PAHs的修复

采用室内盆栽实验,利用柴油按不同比例混合土壤0 g/kg(CK),2 g/kg(L1),10 g/kg(L2)和50 g/kg(L3)制备了含不同浓度PAHs的污染土样,选择1年生樟树(Cinnamomum camphora)、广玉兰(Magnolia grandiflora)、栾树(Koelreuteria bipinnata)、马褂木(Liriodendron chinense)幼苗为供试植物,进行了土壤微生物对柴油的响应及对PAHs的修复研究。结果表明:(1)4个树种土壤微生物区系组成以细菌占优势,放线菌次之,真菌最少。(2)在各测定时间树种间土壤微生物总数对污染处理响应差异较大。栾树各污染处理组土壤微生物总数均高于对照组;樟树各污染处理土壤微生物在实验前期低于对照;广玉兰为污染处理组在4月份显著低于对照,而在其他月份多高于对照;马褂木在4月份均低于对照,其他月份为L1处理低于对照,L2、L3处理高于对照(1月L2除外)。(3)4个树种对照土壤中微生物总数随时间的变化都是从10月逐渐增加至翌年4月,然后不断减少至10月;污染处理土壤微生物总数呈现峰值提前或滞后现象,主要出现在1月或7月。真菌是控制PAHs降解的重要因素。(4)经过1a实验,各树种L1、L2处理土壤中的PAHs浓度已与对照土壤相当;L3处理各树种土壤中PAHs含量为马褂木>栾树>广玉兰>樟树。     

Influence of plant polymers on the distribution and cultivation of bacteria in the phylum Acidobacteria

Members of the phylum Acidobacteria are among the most abundant bacteria in soil. Although they have been characterized as versatile heterotrophs, it is unclear if the types and availability of organic resources influence their distribution in soil. The potential for organic resources to select for different acidobacteria was assessed using molecular and cultivation-based approaches with agricultural and managed grassland soils in Michigan. The distribution of acidobacteria varied with the carbon content of soil: the proportion of subdivision 4 sequences was highest in agricultural soils (ca. 41%) that contained less carbon than grassland soils, where the proportions of subdivision 1, 3, 4, and 6 sequences were similar. Either readily oxidizable carbon or plant polymers were used as the sole carbon and energy source to isolate heterotrophic bacteria from these soils. Plant polymers increased the diversity of acidobacteria cultivated but decreased the total number of heterotrophs recovered compared to readily oxidizable carbon. Two phylogenetically novel Acidobacteria strains isolated on the plant polymer medium were characterized. Strains KBS 83 (subdivision 1) and KBS 96 (subdivision 3) are moderate acidophiles with pH optima of 5.0 and 6.0, respectively. Both strains grew slowly (μ = 0.01 h(-1)) and harbored either 1 (strain KBS 83) or 2 (strain KBS 96) copies of the 16S rRNA encoding gene-a genomic characteristic typical of oligotrophs. Strain KBS 83 is a microaerophile, growing optimally at 8% oxygen. These metabolic characteristics help delineate the niches that acidobacteria occupy in soil and are consistent with their widespread distribution and abundance.     

Lime and compost promote plant re-colonization of metal-polluted, acidic soils

The revegetation of soils affected by historic depositions of an industrial complex in Central Chile was studied. The plant re-colonization from the existing soil seed bank and changes in the physico-chemical properties of the soil were evaluated in field plots amended with lime and/or compost. We found that the application of lime and/or compost decreased the Cu2+ ion activity in the soil solution and the exchangeable Cu in the soil, showing an effective Cu immobilization in the topsoil. Whereas lime application had no effect on plant productivity in comparison with the unamended control, the application of compost and lime+compost increased the plant cover and aboveground biomass due to the higher nutrient availability and water-holding capacity of the compost-amended soils. Although the Cu2+ activity and the exchangeable Cu were markedly lower in the amended soils than in the unamended control, the shoot Cu concentrations of Lolium spp. and Eschscholzia californica did not differ between the treatments.     

Molecular characterization of methanotrophic communities in forest soils that consume atmospheric methane

Methanotroph abundance was analyzed in control and long-term nitrogen-amended pine and hardwood soils using rRNA-targeted quantitative hybridization. Family-specific 16S rRNA and pmoA/amoA genes were analyzed via PCR-directed assays to elucidate methanotrophic bacteria inhabiting soils undergoing atmospheric methane consumption. Quantitative hybridizations suggested methanotrophs related to the family Methylocystaceae were one order of magnitude more abundant than Methyloccocaceae and more sensitive to nitrogen-addition in pine soils. 16S rRNA gene phylotypes related to known Methylocystaceae and acidophilic methanotrophs and pmoA/amoA gene sequences, including three related to the upland soil cluster Alphaproteobacteria (USCalpha) group, were detected across different treatments and soil depths. Our results suggest that methanotrophic members of the Methylocystaceae and Beijerinckiaceae may be the candidates for soil atmospheric methane consumption.     

接种泡囊假单胞菌对土壤生物性质及A. corsicum吸收Ni的影响

采用室内模拟试验方法,研究了在水稻土、元江土和墨江土中添加泡囊假单胞菌（Pseulormanas vesicularis）后土壤中微生物种群数量、土壤酶活性和镍超积累植物Alyssum corsicum对土壤镍的富集效果.土壤接种泡囊假单胞菌70d后,水稻土中DTPA提取态镍较对照土中的明显减少、元江土和墨江土中的有所减少;土壤中细菌、真菌和放线菌数量增加,5种土壤酶活性提高.试验结果表明,水稻土、元江土、墨江土添加泡囊假单菌后植物地上部生物量较对照分别增加了29%、309%和43%,进而提高了A.corsicum自土壤中富集镍的效率：水稻土中增加54%,元江土中增加306%,墨江土中增加32%.泡囊假单胞菌这一新用途的发现,可为植物修复微生物制剂和基因工程菌的开发提供本土的微生物的菌种资源.     

Effect of pH on isolation and distribution of members of subdivision 1 of the phylum Acidobacteria occurring in soil

The pH strongly influenced the development of colonies by members of subdivision 1 of the phylum Acidobacteria on solid laboratory media. Significantly more colonies of this group formed at pH 5.5 than at pH 7.0. At pH 5.5, 7 to 8% of colonies that formed on plates that were incubated for 4 months were formed by subdivision 1 acidobacteria. These colonies were formed by bacteria that spanned almost the entire phylogenetic breadth of the subdivision, and there was considerable congruence between the diversity of this group as determined by the cultivation-based method and by surveying 16S rRNA genes in the same soil. Members of subdivision 1 acidobacteria therefore appear to be readily culturable. An analysis of published libraries of 16S rRNAs or 16S rRNA genes showed a very strong correlation between the abundance of subdivision 1 acidobacteria in soil bacterial communities and the soil pH. Subdivision 1 acidobacteria were most abundant in libraries from soils with pHs of <6, but rare or absent in libraries from soils with pHs of >6.5. This, together with the selective cultivation of members of the group on lower-pH media, indicates that growth of many members of subdivision 1 acidobacteria is favored by slightly to moderately acidic growth conditions.     

油田外排水对干旱戈壁区人工湿地土壤微生物生物量的影响

为研究油田外排水对干旱戈壁区人工湿地土壤微生物生物量的影响,选择干旱戈壁区某油田外排水形成的湿地内坝内、内外坝间、外坝边缘土壤,及不受排水影响的对照土壤,采用磷脂脂肪酸(PLFA)方法,分析外排水对土壤细菌、真菌、放线菌生物量的影响。结果表明:湿地内坝内、内外坝间、外坝边缘土壤与对照土壤的pH和容重均无显著差异,内外坝间的土壤含水量、电导率、溶解性全盐和全碳含量最高,显著高于内坝内土壤;除含水量外,对照土壤的主要物理性质和养分特征与湿地内坝内、内外坝间、外坝边缘的土壤无显著差异。土壤总微生物量、细菌和真菌生物量从湿地内坝内至外坝边缘逐渐增加。土壤总微生物量、细菌、真菌、放线菌与全氮含量均呈显著正相关,丛枝菌根真菌与全碳呈显著正相关,真菌、丛枝菌根真菌与总石油烃呈显著正相关。研究结果表明,油田外排水增加了湿地外坝边缘的土壤微生物量。     

Harvester ant nests, soil biota and soil chemistry

Many ant species accumulate organic debris in the vicinity of their nests. These organic materials should provide a rich resource base for the soil biota. We examined the effect of harvester ant nests (Pogonomyrmex barbatus) on the soil community and soil chemistry. Ant nest soils supported 30-fold higher densities of microarthropods and 5-fold higher densities of protozoa than surrounding, control soils. The relative abundances of the major groups of protozoa differed as well: amoebae and ciliates were relatively overrepresented, and flagellates underrepresented, in ant nest versus control soils. Densities of bacteria and fungi were similar in the two soil types. Concentrations of nitrate, ammonium, phosphorus, and potassium were significantly higher in ant nest soils, while concentrations of magnesium, calcium, and water were similar in nest and control soils. Ant nest soils were marginally more acidic than controls. The results demonstrate that P. barbatus nests constitute a significant source of spatial heterogeneity in soil biota and soil chemistry in arid grasslands. Received: 17 March 1997 / Accepted: 10 June 1997     

Long-term orchard groundcover management systems affect soil microbial communities and apple replant disease severity

Apple replant disease (ARD) is a soil-disease syndrome of complex etiology that affects apple tree roots in replanted orchards, resulting in stunted tree growth and reduced yields. To investigate whether different groundcover management systems (GMSs) influence subsequent ARD severity, we grew apple seedlings in an outdoor nursery in pots containing orchard soil from field plots where four GMSs had been maintained for 14 years in an orchard near Ithaca, NY, USA. The GMS treatments were: (1) pre-emergence herbicide (Pre-H), bare soil strips maintained by applying tank-mixed glyphosate, norflurazon and diuron herbicides annually; (2) post-emergence herbicide (Post-H), sparse weed cover maintained by applying glyphosate in May and July each year; (3) mowed sod grass (Mowed Sod); and (4) bark mulch (Mulch). Soils were also sampled from the grass drive lane maintained between the trees in the orchard (Grass Lane). Sampled soils (Orchard soil) were either pasteurized or left untreated, placed into 4-L pots, and planted with one apple seedling per pot. After 3 months of growth, soil (Bioassay soil) and apple tree roots (Bioassay roots) were sampled from each pot and microbial populations colonizing samples were characterized. Seedling growth was reduced in soils sampled from all four GMS treatments compared to the Grass Lane soils. Among the GMS treatments, seedling biomass was greater in Pre-H than in the Post-H soil. Soil microbial communities and nutrient availability differed among all four GMS treatments and the Grass Lane. Root-lesion (Pratylenchus sp.) nematode populations were higher in the Mowed Sod than in the other GMS treatments. Soil bacterial and fungal community composition was assessed in Orchard and Bioassay soils and Bioassay roots with a DNA fingerprinting method (T-RFLP). Redundancy analysis indicated that soils sampled from the different GMS treatments differentially influenced seedling biomass. A clone library of 267 soil bacteria was developed from sampled Orchard soils and Bioassay roots. These communities were dominated by Acidobacteria (25% of sequences), Actinobacteria (19%), δ-Proteobacteria (12%), β-Proteobacteria (10%), and these ratios differed among the GMS soils. Members of the family Comamonadaceae were detected only in tree-row soil, not in the Grass Lanes. The dominant sequences among 145 cloned fungi associated with apple seedling roots were Fusarium oxysporum (16% of sequences), an uncultured soil fungus submitted under DQ420986 (12%), and Rhodotorula mucilaginosa (9%). In a redundancy analysis, factors including fungal and oomycete community compositions, soil respiration rates, population sizes of culturable bacteria and fungi, soil organic matter content, and nutrient availability, were not significant predictors of apple seedling biomass in these soils. Different GMS treatments used by apple growers may influence subsequent ARD severity in replanted trees, but edaphic factors commonly associated with soil fertility may not reliably predict tree-root health and successful establishment of replanted orchards.     

Microbial Biomass, Community Structure and Metal Tolerance of a Naturally Pb-Enriched Forest Soil

The effect of long-term elevated soil Pb levels on soil microbiota was studied at a forest site in Norway, where the soil has been severely contaminated with Pb since the last period of glaciation (several thousand years). Up to 10% Pb (total amount, w/w) has been found in the top layer. The microbial community was drastically affected, as judged from changes in the phospholipid fatty acid (PLFA) pattern. Specific PLFAs that were high in Pb-enriched soil were branched (especially br17:0 and br18:0), whereas PLFAs common in eukaryotic organisms such as fungi (18:2ω6,9 and 20:4) were low compared with levels at adjacent, uncontaminated sites. Congruent changes in the PLFA pattern were found upon analyzing the culturable part of the bacterial community. The high Pb concentrations in the soil resulted in increased tolerance to Pb of the bacterial community, measured using both thymidine incorporation and plate counts. Furthermore, changes in tolerance were correlated to changes in the community structure. The bacterial community of the most contaminated soils showed higher specific activity (thymidine and leucine incorporation rates) and higher culturability than that of control soils. Fungal colony forming units (CFUs) were 10 times lower in the most Pb-enriched soils, the species composition was widely different from that in control soils, and the isolated fungi had high Pb tolerance. The most commonly isolated fungus in Pb-enriched soils was Tolypocladium inflatum. Comparison of isolates from Pb-enriched soil and isolates from unpolluted soils showed that T. inflatum was intrinsically Pb-tolerant, and that the prolonged conditions with high Pb had not selected for any increased tolerance.     

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.     

Functional diversity and community structure of micro-organisms in three arctic soils as determined by sole-carbon-source-utilization

Functional diversities of micro-organisms in arctic soils at three incubation temperatures were assessed using sole-carbon-source-utilization (SCSU). Soil samples were collected from an area of anthropogenic fertilization (mixed Dorset/Thule/Historic site), an area of animal enrichment (bird rock perches), and unaltered tundra (raised beach; control soil site). The micro-organisms were extracted from the soil samples and inoculated into Gram-negative (GN) Biolog plates incubated at 30°C, 10°C, and 4°C. Calculations of the Shannon index, substrate utilization richness, Shannon evenness, and the Jaccard coefficient of similarity were based upon substrate utilization on the Biolog plates. Principal component analysis distinguished microbial communities in enriched soils from unenriched soils. At 10°C and 4°C, Shannon indices of enriched soil microbial communities (10°C: soils influenced by wild animals=4.28, soils influenced by human activities=4.20; 4°C: soils influenced by wild animals=4.15, soils influenced by human activities=4.03) were significantly higher than unenriched soil microbial communities (10°C: 3.66; 4°C: 3.38). Substrate utilization richness and evenness displayed similar trends. Although Jaccard coefficients showed uniformity across the different soil samples, cluster analysis supported patterns demonstrated by PCA. Lower temperatures (4°C and 10°C) yielded greater resolution between soil microbial communities than 30°C based on Biolog colour development patterns.     

A comparison of bacterial and fungal biomass in several cultivated soils

Bacterial and fungal biomass was estimated in incubated samples of three cultivated soils, the influence of glucose, ammonium nitrate and cattle slurry on its formation being studied. The microbial biomass was determined in stained microscopic preparations of soil suspension. Bacterial biomass in the control samples was from 0.17 to 0.66 mg dry wt per 1 g dry soil and independently of the applied supplements was on the average two times larger in muck soils than in sand. Fungal biomass in the control soils ranged from 0.013 to 0.161 mg dry wt per 1 g dry soil, no relationship being found between its size and the soil type. As a result, the ratio of the size of fungal to bacterial biomass was dependent on the soil type; in sand the fungal biomass corresponded to 1/3 of the bacterial biomass, and in muck soils--only to 1/7.     

Adsorption and desorption of Hg(II) by three typical soils around the chlor-alkali industry

A series of batch experiments were conducted to assess the adsorption/desorption of Hg(II) within meadow soil, fluvo-aquic soil, and gray desert soil around the chlor-alkali industry in China. Results demonstrated that the descending order of the adsorptive capacity of Hg(II) to the three typical soils around a chlor-alkali plant, i.e., meadow soil (4536.24 mg/kg), fluvo-aquic soil (1598.62 mg/kg), gray desert soil (1272.51 mg/kg), and the soil organic matter, had a significant role in Hg(II) adsorption. Kinetic studies revealed that the Hg adsorption in the three soils was characterized with a fast stage and a slow stage. The Hg(II) adsorption rates are the highest for the fluvo-aquic soil, followed by the meadow soil, and then the gray desert soil. The results will play a guiding role in arid-zone soil pollution control and treatment, which will be a reference for the Northwest Oasis Environmental mercury pollution studies and integrated control in China.     

太子参不同休耕年限土壤理化特征和微生物群落变化

太子参为福建道地中药材,连作效应严重限制其产业发展。休耕可以在一定程度上缓解连作效应,然而休耕对于缓解连作效应的机制尚不清楚。本文通过高通量测序分析不同休耕年限对太子参土壤微生物丰度及群落多样性的影响,并探索土壤理化性质、酚酸类物质与土壤微生物群落之间的关联性。结果表明:与对照太子参土壤相比,休耕土壤真菌多样性降低,细菌多样性增多。在细菌优势菌门中,酸杆菌门相对丰度显著增加,变形菌门与放线菌门相对丰度显著降低;真菌优势菌门相对丰度无显著变化。土壤酸性减弱,有机质含量随休耕年限增加呈现递减模式,酚酸类物质中苯甲酸和水杨酸含量显著降低,而对香豆酸等逐渐积累。综上,太子参土壤休耕改善了土壤微生物的菌群结构、土壤性质,从而缓解了连作效应。     

Effect of pH on Isolation and Distribution of Members of Subdivision 1 of the Phylum Acidobacteria Occurring in Soil

The pH strongly influenced the development of colonies by members of subdivision 1 of the phylum Acidobacteria on solid laboratory media. Significantly more colonies of this group formed at pH 5.5 than at pH 7.0. At pH 5.5, 7 to 8% of colonies that formed on plates that were incubated for 4 months were formed by subdivision 1 acidobacteria. These colonies were formed by bacteria that spanned almost the entire phylogenetic breadth of the subdivision, and there was considerable congruence between the diversity of this group as determined by the cultivation-based method and by surveying 16S rRNA genes in the same soil. Members of subdivision 1 acidobacteria therefore appear to be readily culturable. An analysis of published libraries of 16S rRNAs or 16S rRNA genes showed a very strong correlation between the abundance of subdivision 1 acidobacteria in soil bacterial communities and the soil pH. Subdivision 1 acidobacteria were most abundant in libraries from soils with pHs of <6, but rare or absent in libraries from soils with pHs of >6.5. This, together with the selective cultivation of members of the group on lower-pH media, indicates that growth of many members of subdivision 1 acidobacteria is favored by slightly to moderately acidic growth conditions.