施肥对玉米田大型土壤动物群落的影响

采用手捡法对玉米田秸秆回填及施肥处理条件下大型土壤动物群落组成及多样性进行研究。结果表明,玉米田内土壤动物数量与施肥情况有关。不同施肥处理玉米田内土壤动物个体总数从多到少依次为：NPK正常施肥秸杆不回田处理〉不施肥处理;全部秸杆回田处理〉CK对照处理（秸杆不回田、不施肥）。土壤动物类群数依次为：NPK正常施肥秸杆不回田处理=不施肥处理（全部秸杆回田）〉CK对照处理（秸杆不回田,不施肥）。生物多样性指数分析表明,不同处理之间生物多样性无明显差异,但在玉米生长不同时期内,生物多样性有明显差异。     

Effect of N fertilizer rate and soil pH on N efficiency in corn

Nitrogen (N) efficiency components and N accumulation parameters were determined for seven commercially available corn (Zea mays L.) hybrids grown on a Cecil sandy loam soil (Typic Hapludult) in the Southeasten U.S. The hybrids were grown in field plots at three soil pH levels (4.8, 5.5, and 6.6) and four N fertilizer rates (0.4, 1.8, 3.2, and 6.0, g plant⁻¹). Nitrogen uilitzation efficiency (grain yield/total N uptake) was significantly different among hybrids in both 1983 and 1984. Differences in N use efficiency (grain yield/N supply) and N uptake efficiency (total N uptake/N supply) ranged from 100.4 to 114.6 and from 1.62 to 1.90, respectively, in 1984. Nitrogen fertilizer rate significantly affected all measured N accumulation and efficiency parameters except N uptake after silking in 1983. The results indicate that improving N uptake or soil N availability might increase grain yields for hybrids with higher N utilization efficiency.     

我国土壤动物群落生态学研究综述

总结了我国土壤动物群落生态学研究的特点,即区域分布集中于中国东部、研究的生态系统类型广泛、研究角度多种多样与应用研究发展迅速。并从土壤动物群落与环境关系、土壤动物群落的组成和多样性、土壤动物群落结构、土壤动物群落功能、土壤动物群落演替与受干扰生态系统的土壤动物群落6个方面综述其最新研究成果。在此基础上指出我国土壤动物群落生态学中有待开拓的研究领域是基础研究、特色区域和生态系统的研究、土地覆盖/土地利用对土壤动物的影响研究、土壤动物多样性及其保护研究、土壤动物在土壤生态系统和陆地生态系统物质循环和能量流动中的作用研究、全球变化响应研究与土壤动物应用研究。     

Effect of soil aggregate size on methanogenesis and archaeal community structure in anoxic rice field soil

In anoxically incubated slurries of Italian rice field soil, CH(4) production is initiated after a lag phase during which ferric iron and sulfate are reduced. The production of CH(4) was affected by the size of soil aggregates used for the preparation of the soil slurry. Rates of CH(4) production were lowest with small aggregates (<50 and 50-100 μm), were highest with aggregates of 200-2000 μm size and were intermediate with aggregates of 2000-15000 μm size. The different amounts of CH(4) accumulated were positively correlated to the concentrations of acetate, propionate and caproate that transiently accumulated in the slurries prepared from different aggregate sizes and also to the organic carbon content. The addition of organic debris that was collected from large-size aggregates to the aggregate size fractions <200 and <50 μm resulted in an increase of CH(4) production to amounts that were comparable to those measured in unamended aggregates of 200-2000 μm size, indicating that CH(4) production in the different aggregate size fractions was limited by substrate. The distribution of archaeal small-subunit rRNA genes in the different soil aggregate fractions was analyzed by terminal restriction fragment length polymorphism which allowed seven different archaeal ribotypes to be distinguished. Ribotype-182 (consisting of members of the Methanosarcinaceae and rice cluster VI), ribotype-389 (rice cluster I and II) and ribotype-820 (undigested DNA, rice cluster IV and members of the Methanosarcinaceae) accounted for >20, >30 and >10% of the total, respectively. The other ribotypes accounted for <10% of the total. The relative quantity of the individual ribotypes changed only slightly with incubation time and was almost the same among the different soil aggregate fractions. Ribotype-389, for example, slightly decreased with time, whereas ribotype-182 slightly increased. At the end of incubation, the relative quantity of ribotype-182 seemed to be slightly higher in soil fractions with larger than with smaller aggregates, whereas it was the opposite with ribotype-80 (Methanomicrobiaceae) and ribotype-88 (Methanobacteriaceae). Ribotype-280 (Methanosaetaceae and rice cluster V), ribotype-375 (rice cluster III), ribotype-389 and ribotype-820, on the other hand, were not much different among the different soil aggregate size fractions. However, the differences were not significant relative to the errors encountered during the extraction of polymerase chain reaction (PCR)-amplifiable DNA from soil. In conclusion, soil aggregate size and incubation time showed a strong effect on the function but only a small effect on the structure of the methanogenic microbial community.     

Effect of temperature on composition of the methanotrophic community in rice field and forest soil

Temperature change affects methane consumption in soil. However, there is no information on possible temperature control of methanotrophic bacterial populations. Therefore, we studied CH(4) consumption and populations of methanotrophs in an upland forest soil and a rice field soil incubated at different temperatures between 5 and 45 degrees C for up to 40 days. Potential methane consumption was measured at 4% CH(4). The temporal progress of CH(4) consumption indicated growth of methanotrophs. Both soils showed maximum CH(4) consumption at 25-35 degrees C, but no activity at >40 degrees C. In forest soil CH(4) was also consumed at 5 degrees C, but in rice soil only at 15 degrees C. Methanotroph populations were assessed by terminal restriction fragment length polymorphism (T-RFLP) targeting particulate methane monooxygenase (pmoA) genes. Eight T-RFs with relative abundance >1% were retrieved from both forest and rice soil. The individual T-RFs were tentatively assigned to different methanotrophic populations (e.g. Methylococcus/Methylocaldum, Methylomicrobium, Methylobacter, Methylocystis/Methylosinus) according to published sequence data. Two T-RFs were assigned to ammonium monooxygenase (amoA) gene sequences. Statistical tests showed that temperature affected the relative abundance of most T-RFs. Furthermore, the relative abundance of individual T-RFs differed between the two soils, and also exhibited different temperature dependence. We conclude that temperature can be an important factor regulating the community composition of methanotrophs in soil.     

玉米秸秆还田培肥土壤的效果

辽北地区玉米根茬还田、秸秆直接还田或间接还田的3年微区培肥试验研究结果表明,无机肥的增产效果特别明显,而施有机物料,更主要的作用是改善土壤的物理、化学性质、培肥地力,与无肥对照相比,有机无机肥料配合施用可使土壤有机质提高3．06％－27．78％,各有机物料对土壤有机质提高的顺序依次为100％秸秆＞50％秸秆＞土粪＞牛粪＞33％秸秆＞根茬。在含C量相等的条件下,秸秆对土壤有机质的保持和提高好于土粪,土粪好于牛粪。同时,与单施化肥比,有机无机肥料配合施用可使土壤易氧化有机质增加10．91％－20．67％,使浸提腐殖酸提高1．43％－14．28％,使结合态腐殖酸的松／紧比值提高0．07－0．19,HA／FA比值提高0．07－0．24,并且能改善土壤的N、P、K营养状况、土壤水分和土壤孔隙状况,这标志着土壤有机质活性的提高和土壤肥力状况的改善。因此,应该大力提倡玉米秸秆秋季直接还田,其最佳施入量应为当年生产量的30％－50％。     

Influence of fertilizer on southwestern corn borer, Diatraea grandiosella, infestation and damage to field corn

Nitrogen (N) and phosphorus (P) fertilizers have differing effects on southwestern corn borer (SWCB). Diatraea grandiosella Dyar, densities and damage to field corn, Zea mays L. Nitrogen fertilization of corn is associated with an increase in number of stalks infested and girdled by corn borers, while addition of P has the opposite effect. When combinations of N and P were applied, there were no significant differences in SWCB infestation or damage from plots receiving no fertilizer. The effect of combinations of N and P on SWCB were intermediate to either element alone.

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Résumé Nous avons étudié les corrélations entre l'utilisation d'engrais azotés et phosphatés d'une part, l'infestation et l'alimentation de D. grandiosella sur maïs en champs d'autre part. Les formules d'engrais comparées étaient: pas d'engrais, 90 et 179 kg N/ha sans P, 45 et 90 kg P/ha sans N, et les combinaisons de ces deux teneurs en N et P.La contamination était plus élevée dans les lots ayant reçu de l'azote que dans ceux traités sans N, mais la présence d'azote n'a pas réduit le décapage des tiges et la verse dus à l'alimentatin larvaire. A l'inverse, les lots n'ayant reçu que du phosphore avaient des pourcentages plus faibles de tiges contaminées par D. grandiosella et ainsi décapées et versées, que ceux qui n'avaient pas reçu P. Il n'a pas eu de différences significatives dans les contaminations ou les dégats entre les lots ayant reçu différentes combinaisons de N et P, et les effets de ces combinaisons sur l'insecte étaient intermédiaires à ceux de N et P seuls.

     

Effect of slow-release urea on soil nematode community structure in a Chinese soybean field

The effect of slow-release urea on soil nematode community structure was investigated in a soybean field in northeast China. Three treatments, no urea (CK), conventional urea (U) and slow-release urea (SRU), were arranged in a completely random design. The results show that the abundance of total nematodes was significantly higher in SRU than in CK and U. Significant differences in the abundance of bacterivores with colonizer-persister (cp) values 2–3, fungivores with cp 2 and herbivores with cp 3 were found among different treatments. Forty-one genera were identified, of which Acrobeloides, Aphelenchus and Heterodera were dominant. Soil nematode guilds and genera exhibited different responses to slow-release urea. The most trophic groups and genera had greater abundances in SRU than in CK and U. Slow-release urea had a positive effect on soil nematode community structure.     

生物钾肥的研制及田间应用

原苏联农业学博士в г亚历山大罗夫( 1 95 6 )研究发现硅酸盐细菌能分解土壤最主要组成成分硅铝酸盐 ,释放出钾和其它灰份元素 ,将土壤中磷灰土和磷灰石的磷转变为可给态磷 ,而且能固定空气中的氮素[1] 。 80年代以来 ,我国科技工作者对硅酸盐细菌的特性及其制剂也进行了大量研究、田间示范。本室以我省高寒地区土样中分离到 1株代号为ＨＬ89- 0 4的硅酸盐细菌及保藏的胶质芽孢杆菌硅酸盐亚种为研究对象 ,进行了生物钾肥的研制与田间试验。1　材料和方法1 1　菌种 :ＨＬ89- 0 4分离自土壤 ,经鉴定属胶质芽孢杆菌Ｂａｃｉｌｌｕｓｍｕｃｉ…     

Effect of soil solarization on corn stalk rot

Seven weeks solarization of irrigated soil raised its temperature by 11.5°C over non-solarized soil at 10 cm depth and effectively controlled weeds (98.5%), stalk borer (8.9%) and stalk rot disease (69.1%) in corn. Solarization also reduced symptoms of Fusarium moniliforme and Macrophomina phaseolina significantly by 64.2% and 78.4%, respectively, and completely controlled M. phaseolina in corn cultivars, viz. Pool-10, Shaheen and Gauher. Whereas symptoms of F. moniliforme were observed in these cultivars, Fusarium graminearum was not observed except in two cultivars, Shaheen and Akbar. Growth of crop planted in solarized plots was better and it yielded almost one to three times more grains in cultivars under test. Soil analysis immediately following solarization revealed that essential elements were readily available in simpler forms, which may have increased pest resistance and reduced stalk breakage.     

微生物肥料及其生产应用中的问题

微生物肥料和微生物制剂是新世纪实行绿色农业的重要技术保障,关键是因其中含有大量的有效微生物的生命活动产生特定的肥效或其他生理功能,导致增产,微生物肥料包括根瘤菌肥,解磷菌肥、解钾菌肥、5406菌肥,植物根际促生菌,VA菌根等等,有机肥料堆制剂中含有多种降解农业有机废料的菌种,可缩短堆肥周期,提高养份利用率,由于微生物本身的特殊性,相关市场监督机制不健全,微生物肥料的生产,应用领域存在很多问题,甚至出现明显的伪科学,科研、生产、行政各有关部门应加强基础研究,提高全民科普水平,健全市场监督机制,依靠专家设计严格试验,优选可靠技术,保证良好的经济效益和社会效益。     

长期单施化肥对土壤性状及作物产量的影响

1978－1998年在陕西关中地区农田的长期定位试验研究表明,长期单纯化肥基本上可以维持土壤有机质和NP水平,单施化肥与化肥配合有机肥处理的作物产量基本相当,但是,单施化肥处理使土壤腐殖质能量水平降低,分子缩合程度和芳构化度增大,“老化”作用增强。     

Effect of temperature on carbon and electron flow and on the archaeal community in methanogenic rice field soil

Temperature is an important factor controlling CH(4) production in anoxic rice soils. Soil slurries, prepared from Italian rice field soil, were incubated anaerobically in the dark at six temperatures of between 10 to 37 degrees C or in a temperature gradient block covering the same temperature range at intervals of 1 degrees C. Methane production reached quasi-steady state after 60 to 90 days. Steady-state CH(4) production rates increased with temperature, with an apparent activation energy of 61 kJ mol(-1). Steady-state partial pressures of the methanogenic precursor H(2) also increased with increasing temperature from <0.5 to 3.5 Pa, so that the Gibbs free energy change of H(2) plus CO(2)-dependent methanogenesis was kept at -20 to -25 kJ mol of CH(4)(-1) over the whole temperature range. Steady-state concentrations of the methanogenic precursor acetate, on the other hand, increased with decreasing temperature from <5 to 50 microM. Simultaneously, the relative contribution of H(2) as methanogenic precursor decreased, as determined by the conversion of radioactive bicarbonate to (14)CH(4), so that the carbon and electron flow to CH(4) was increasingly dominated by acetate, indicating that psychrotolerant homoacetogenesis was important. The relative composition of the archaeal community was determined by terminal restriction fragment length polymorphism (T-RFLP) analysis of the 16S rRNA genes (16S rDNA). T-RFLP analysis differentiated the archaeal Methanobacteriaceae, Methanomicrobiaceae, Methanosaetaceae, Methanosarcinaceae, and Rice clusters I, III, IV, V, and VI, which were all present in the rice field soil incubated at different temperatures. The 16S rRNA genes of Rice cluster I and Methanosaetaceae were the most frequent methanogenic groups. The relative abundance of Rice cluster I decreased with temperature. The substrates used by this microbial cluster, and thus its function in the microbial community, are unknown. The relative abundance of acetoclastic methanogens, on the other hand, was consistent with their physiology and the acetate concentrations observed at the different temperatures, i.e., the high-acetate-requiring Methanosarcinaceae decreased and the more modest Methanosaetaceae increased with increasing temperature. Our results demonstrate that temperature not only affected the activity but also changed the structure and the function (carbon and electron flow) of a complex methanogenic system.     

玉米秸秆还田对黑土微生物群落功能多样性的影响

为了解玉米秸秆还田对土壤微生物群落功能多样性的影响,采用ECO-Biolog微平板法,分析了以无玉米秸秆还田为对照(CK),6000 kg·hm^-2(S1)、9000 kg·hm^-2(S2)、12000 kg·hm^-2(S3)和15000 kg·hm^-2(S4)四个秸秆还田量的土壤微生物碳源代谢特征。结果表明:随着玉米秸秆还田量的增加,土壤微生物平均颜色变化率(AWCD)也随之增加,24~96 h的AWCD值变化迅速,96 h后进入平稳期,S4处理AWCD值始终大于其他处理;秸秆还田对Shannon指数与Simpson指数没有显著影响(P>0.05),但与CK相比,S4处理McIntosh指数显著增加了57.5%(P<0.05);主成分分析结果显示,秸秆还田影响着土壤微生物群落碳代谢能力,S1、CK、S2和S3处理在PC1和PC2上出现显著的分异,糖类、多聚物类、羧酸类碳源是研究区域内土壤微生物利用的主要碳源。因此,在东北黑土区增加玉米秸秆还田量能够提高土壤微生物对碳源的利用能力,提升黑土肥力。     

秸秆生物有机肥的施用对土壤供氮能力的影响

通过盆栽试验研究了秸秆生物有机肥的施用对土壤供氮能力的影响。结果表明,与原始秸秆相比,秸秆生物有以与尿素配合施用能明显提高土壤生物量碳,氮的含量,增幅约为3－4倍;土壤微生物量氮与土壤的供氮能力关系非常密切,前期发生强烈的微生物增殖过程,则中后期必会发生无机氮释放过程,这对作物的生长发育极为重要。同时提高了肥料氮利用率,揭示了秸秆生物有机肥配施无机氮肥改善土壤供氮能力的机理。     

Bacterial soil community in a Brazilian sugarcane field

The assessment of bacterial communities in soil gives insight into microbial behavior under prevailing environmental conditions. In this context, we assessed the composition of soil bacterial communities in a Brazilian sugarcane experimental field. The experimental design encompassed plots containing common sugarcane (variety SP80-1842) and its transgenic form (IMI-1 — imazapyr herbicide resistant). Plants were grown in such field plots in a completely randomized design with three treatments, which addressed the factors transgene and imazapyr herbicide application. Soil samples were taken at three developmental stages during plant growth and analyzed using 16S ribosomal RNA (rRNA)-based PCR-denaturing gradient gel electrophoresis (PCR-DGGE) and clone libraries. PCR-DGGE fingerprints obtained for the total bacterial community and specific bacterial groups — Actinobacteria, Alphaproteobacteria and Betaproteobacteria — revealed that the structure of these assemblages did not differ over time and among treatments. Nevertheless, slight differences among 16S rRNA gene clone libraries constructed from each treatment could be observed at particular cut-off levels. Altogether, the libraries encompassed a total of eleven bacterial phyla and the candidate divisions TM7 and OP10. Clone sequences affiliated with the Proteobacteria, Actinobacteria, Firmicutes and Acidobacteria were, in this order, most abundant. Accurate phylogenetic analyses were performed for the phyla Acidobacteria and Verrucomicrobia, revealing the structures of these groups, which are still poorly understood as to their importance for soil functioning and sustainability under agricultural practices.     

有机磷农药对土壤动物毒性的影响研究

有机磷农药对土壤动物毒性影响的试验结果表明,土壤动物对农药毒性反应敏感,4种有机磷农药处理组的动物种类和数量明显减少,动物种类的减少主要是常见种和稀有种类,动物数量变化则主要是优势类群的数量消长,毒性毒理试验表明,农药对大型土壤动物蚯蚓有明显致死效应,并对蚯蚓,鞘翅目幼虫和等足类鼠妇虫等大型动物的呼吸强度有显著抑制作用,其呼吸代谢强度随着农药处理浓度增加与染毒历时的延长而迅速减弱。     

Effect of soil temperature on direction of corn root growth

Summary More precise effects of soil temperature on the direction of corn root growth were determined by growing seedlings in soil for short periods in growth cabinets controlled to give a range of soil temperature conditions.The angle of growth (relative to the horizontal) was found to be minimum (10°) at constant 17°C. Above or below this temperature (10–30°C), a more vertical direction occurred. Cyclic temperatures also influenced direction, with the maximum of the cycle apparently determining the angle. The duration of the maximum temperature period in a cycle necessary to initiate a direction effect was not determined, however.The significance of these findings in the field is that modifications of soil temperatures by mulches, etc. probably influence the distribution of roots in the rooting zone of soils. This in turn means that plant behaviour such as moisture and nutrient uptake can be better explained or managed for maximum performance.Former graduate student. Present address, Ministry of the Environment, 135 St. Clair Avenue West, Toronto, Ontario, Canada, M4W IP5. Support received through Canada Department of Agriculture Grant 1045.     

Effect of temperature on structure and function of the methanogenic archaeal community in an anoxic rice field soil.

Soil temperatures in Italian rice fields typically range between about 15 and 30 degrees C. A change in the incubation temperature of anoxic methanogenic soil slurry from 30 degrees C to 15 degrees C typically resulted in a decrease in the CH4 production rate, a decrease in the steady-state H2 partial pressure, and a transient accumulation of acetate. Previous experiments have shown that these changes were due to an alteration of the carbon and electron flow in the methanogenic degradation pathway of organic matter caused by the temperature shift (K. J. Chin and R. Conrad, FEMS Microbiol. Ecol. 18:85-102, 1995). To investigate how temperature affects the structure of the methanogenic archaeal community, total DNA was extracted from soil slurries incubated at 30 and 15 degrees C. The archaeal small-subunit (SSU) rRNA-encoding genes (rDNA) of these environmental DNA samples were amplified by PCR with an archaeal-specific primer system and used for the generation of clone libraries. Representative rDNA clones (n = 90) were characterized by terminal restriction fragment length polymorphism (T-RFLP) and sequence analysis. T-RFLP analysis produced for the clones terminally labeled fragments with a characteristic length of mostly 185, 284, or 392 bp. Sequence analysis allowed determination of the phylogenetic affiliation of the individual clones with their characteristic T-RFLP fragment lengths and showed that the archaeal community of the anoxic rice soil slurry was dominated by members of the families Methanosarcinaceae (185 bp) and Methanosaetaceae (284 bp), the kingdom Crenarchaeota (185 or 284 bp), and a novel, deeply branching lineage of the (probably methanogenic) kingdom Euryarchaeota (392 bp) that has recently been detected on rice roots (R. Grosskopf, S. Stubner, and W. Liesack, Appl. Environ. Microbiol. 64:4983-4989, 1998). The structure of the archaeal community changed when the temperature was shifted from 30 degrees C to 15 degrees C. Before the temperature shift, the clones (n = 30) retrieved from the community were dominated by Crenarchaeota (70%), "novel Euryarchaeota" (23%), and Methanosarcinacaeae (7%). Further incubation at 30 degrees C (n = 30 clones) resulted in a relative increase in members of the Methanosarcinaceae (77%), whereas further incubation at 15 degrees C (n = 30 clones) resulted in a much more diverse community consisting of 33% Methanosarcinaceae, 23% Crenarchaeota, 20% Methanosaetaceae, and 17% novel Euryarchaeota. The appearance of Methanosaetaceae at 15 degrees C was conspicuous. These results demonstrate that the structure of the archaeal community in anoxic rice field soil changed with time and incubation temperature.