东北羊草草原主要植物群落土壤过氧化氢酶活性的研究

东北羊草草原3种植物群落土壤过氧化氢酶活性的季节变化曲线基本都呈抛物线型,虎尾草群落季节变化幅度比羊草群落和碱茅群落大,造成这种现象的原因可能是“种子效应”,对不同土层度过氧化氢酶活性与环境因子的相关分析表明,土壤过氧化氢酶活性随着土层的加深而递减,并与降雨量和大气温度有较强的相关性,且受土壤温度和土壤含水量的协同作用,此外,土壤过氧化氢酶活性与地上植被明显相关,可以反映出植物群落的生长状态。     

Vertical Profile of Phosphatase Activity in the Sundarban Mangrove Forest,North East Coast of Bay of Bengal,India

Impact of phosphate solubilizing bacteria along with soil phosphatase activity on phosphorous cycle was found to be quiet interesting in the Sundarban mangrove ecosystem. Soil phosphatase activity showed a decreasing pattern with increase in depth [soil phosphatase activity (μg pnp produced g^?1 dry wt of soil) = 906.85 – 5.6316 Depth (cm)] from the deep forest region of the Sundarban forest ecosystem. Soil salinity showed a very little effect on soil phosphatase activity whereas soil temperature and pH was found to show significant impact on the soil phosphatase activity. This ensured that the microbes associated with phosphate mineralization present in the Sundarban forest ecosystem are more tolerant to fluctuation in salinity than that of temperature and pH. A direct correlation was perceptible between the number of phosphate solubilizing bacteria and phosphatase activity in the soil during the study period from 2007 to 2012. Soil phosphate concentration was found to be directly governed by the soil phosphatase activity [The regression equation is: avg PO₄^?3-P (μg g^?1 dry wt of soil) = 0.0311 + 0.000606 soil phosphatase activity (μg pnp produced g^?1 dry wt of soil); R² = 63.2%, p < 0.001, n = 62].     

Effect of the chemical and physical condition of the soil on Verticillium wilt of antirrhinum

Summary In vitro study showed thatVerticillium dahliae Kleb. grew well in a wide range of acid and alkaline media (viz. pH 3.5 to 10.5). The best growth of the fungus was observed in pH 5.5. Soil pH 3.5 was toxic for growing antirrhinum seedlings. Development of Verticillium wilt of antirrhinum was affected by soil pH. The severity of the disease was greater in alkaline soil conditions compared with acid conditions. Soil of pH 3.5 gave very good control of the symptom expression by the infected plants. Rhizosphere analysis results showed that fungal population with the exception ofPenicillium spp., was drastically reduced in the rhizosphere of the plants grown in acid soil. Although the overall population of fungi was reduced in theV. dahliae infected antirrhinum rhizosphere in acid soil, the population ofPenicillium spp. markedly increased. The antagonistic activity of thePenicillium spp. in the rhizosphere might also have reduced the disease severity. Since the seedlings did not grow properly in very dry and very wet soil, rhizosphere analysis of these soils was not possible. Disease severity was much less in wet soil compared with plants grown in medium moisture level and dry soil, but the plant growth was very poor. Dedicated to the memory of the late Prof. H. K. Baruah from whom I had the inspiration for research     

Non-symbictic nitrogen fixation in the rhizosphere of Digitaria smutzii stent

Summary The acetylene reduction technique was used to test for the activity of nitrogenase in the rhizosphere of Digitaria smutzii grown in a solodic soil, and in the same soil in the absence of grass. The tests were made in McCartney bottles and regression analysis was used to compare rates of ethylene production. Roots with rhizosphere soil attached, exposed to acetylene and incubated anaerobically for 34 hours produced ethylene at a mean rate of 29 n moles C₂H₄/g root/h. No significant activity was detected under anaerobic conditions in the unplanted soil. Under aerobic conditions, significant but very low rates of ethylene production were observed in both the presence and absence of grass. Temperature treatments within the range 20°–32°C had no significant effect on rates of ethylene production.     

Inhibition of soil urease activity by amido derivatives of phosphoric and thiophosphoric acids

Summary A laboratory experiment was conducted to study inhibition of soil urease activity by amido derivatives of phosphoric and thiophosphoric acids. Results showed that derivatives with higher amido substitutions have greater inhibitory effect on urea hydrolysis in the soils used in our study. Triamides of phosphoric and thiophosphoric acids were found to be very effective inhibitors of soil urease. These compounds seem to have potential as fertilizer amendments for inhibiting soil urease activity and for improving the efficiency of nitrogen use from urea.     

天宝岩长苞铁杉林倒木接触处土壤酶活性变化及其环境效应

倒木是森林生态系统中重要的结构性和功能性成分,但分解过程十分缓慢,目前有关土壤生物学特性对其分解影响机制的研究甚少。通过分析环境因子对选择天宝岩国家级自然保护区长苞铁杉林内倒木接触处土壤酶活性的影响,探讨酶活性对倒木分解机制、土壤进程的影响及特定酶活性的时空分布格局。研究结果表明:天宝岩长苞铁杉林内倒木接触处土壤酶活性的变异系数属中高等变异程度,纤维素分解酶活性受环境影响最大,蛋白酶受影响最小;倒木的覆盖有利于提高土壤酶活性,尤其是显著地提高了纤维素酶活性,蛋白酶及脲酶活性随腐烂等级升高而降低,纤维酶活性呈升高趋势;在所有环境因子中,土壤基质环境对土壤酶活性的解释量最大,表明化学基质环境对土壤酶活性的影响不容忽视,土壤酶活性随土壤SOC、TN含量的增加而升高,随海拔升高而降低,越往南坡,土壤酶活性越高。研究揭示倒木分解与土壤酶活性之间相互促进、相互制约,倒木的存在对驱动森林生态系统的碳循环有重要意义。     

Huge increase in bacterivores on freshly killed barley roots

Abstract Adding fresh roots to intact soil cores resulted in marked increases in microbial and microfaunal activity at the resource islands. Microbial activity increased in two phases following root addition. Respiratory activity and concentration of respiratory enzyme (dehydrogenase) in soil adhering to the roots was very high during the first three weeks resulting in anaerobic conditions in the soil. After a period of low respiratory activity and enzyme content, these quantities increased from 6 to 20 weeks, but not enough to maintain anaerobic conditions. Numbers of protozoa peaked earlier than the nematodes. Based on yield coefficients of microbes and bacterivores, the increase in bacterivores was in accordance with root-induced respiration activity. In soil adhering to roots, numbers of bacterial grazers (protozoa and nematodes) were up to 80 and 30 times higher, respectively, than in the surrounding soil. This effect is up to 20 times higher than observed around live root systems, which may suggest that the rhizosphere effect on microbivores could for the major part result from the decomposition of dead segments of the root system.     

The role of root exudates and allelochemicals in the rhizosphere

Plant roots serve a multitude of functions in the plant including anchorage, provision of nutrients and water, and production of exudates with growth regulatory properties. The root–soil interface, or rhizosphere, is the site of greatest activity within the soil matrix. Within this matrix, roots affect soil structure, aeration and biological activity as they are the major source of organic inputs into the rhizosphere, and are also responsible for depletion of large supplies of inorganic compounds. Roots are very complicated morphologically and physiologically, and their metabolites are often released in large quantities into the soil rhizosphere from living root hairs or fibrous root systems. Root exudates containing root-specific metabolites have critical ecological impacts on soil macro and microbiota as well as on the whole plant itself. Through the exudation of a wide variety of compounds, roots impact the soil microbial community in their immediate vicinity, influence resistance to pests, support beneficial symbioses, alter the chemical and physical properties of the soil, and inhibit the growth of competing plant species. In this review, we outline recent research on root exudation and the role of allelochemicals in the rhizosphere by studying the case of three plants that have been shown to produce allelopathic root exudates: black walnut, wheat and sorghum     

Microbiological aspects of determination of trichloroacetic acid in soil

Soils have been shown to possess a strong microbial trichloroacetic acid (TCA)-degrading activity. High TCA-degradation rate was also observed during soil extraction with water. For correct measurements of TCA levels in soil all TCA-degrading activities have to be inhibited immediately after sampling before analysis. We used rapid freezing of soil samples (optimally in liquid nitrogen) with subsequent storage and slow thawing before analysis as an efficient technique for suppressing the degradation. Frozen soil samples stored overnight at -20 degrees C and then thawed slowly exhibited very low residual TCA-degrading activity for several hours. Omitting the above procedure could lead to the confusing differences between the TCA levels previously reported in the literature.     

喀斯特石漠化山地不同类型人工林土壤的基本性质和综合评价

以贵州喀斯特石漠化山地退耕还林工程区的刺槐(Robinia pseudoacacia)人工林(RP)、千香柏(Cupressus duclouxiana)人工林(CD)、刺槐千香柏混交林(RD)及未造林地(CK)为研究对象, 探讨了土壤物理、化学性质和土壤酶活性的动态变化, 并对不同恢复类型的土壤质量进行了综合评价。结果显示: 1)各类型人工林的土壤物理特性明显优于未造林地。2)在RP、CD、RD及CK下, 土壤养分和pH值存在显著差异, 且速效养分在不同月份差异明显(p < 0.01)。3) RP、CD、RD及CK下的土壤脲酶的最大活性出现在9月, 最小活性出现于1月; 不同类型的人工林及CK下土壤蔗糖酶的活性存在显著差异(p < 0.01); 土壤过氧化氢酶的活性在一年的测定期内的变化趋势一致, 呈单峰型分布, 而碱性磷酸酶的活性却出现了两次峰值和一次谷值; 土壤多酚氧化酶的最小活性均出现在1月, RP在整个研究期间多酚氧化酶的活性最小。RP、CD、RD及CK下, 土壤脲酶、蔗糖酶、过氧化氢酶、碱性磷酸酶和多酚氧化酶5种酶的活性在整个研究期间的平均值排序不同。4)土壤质量综合评价的结果表明, 土壤质量综合评价指数值(SQI)的大小排序为: RP (0.748) > RD (0.590) > CD (0.406) > CK (0.315)。结果表明, 退耕还林后土壤质量得到较明显的改善, 其中刺槐纯林和混交林的效果较好。     

Impact of an Herbicide Combination of Bromoxynil and Prosulfuron on Soil Microorganisms

Soil microcosm experiments were used to investigate the effects on growth and activity of soil microorganisms of an herbicide combination (60% bromoxynil + 3% prosulfuron) frequently used to provide a broad spectrum control of weed species. Culturable aerobic bacteria, fungi, and actinomycetes, the fundamental groups of heterotrophic microorganisms, and nitrifiers, considered a very sensitive group to these compounds, were evaluated. Since herbicides have been found to inhibit decomposition of cellulose in soil, the effects on cellulolytic bacteria and fungi were determined. Dehydrogenase activity as a measure of microbial activity was another parameter considered. The results emphasized a tendency of reversible stimulatory/inhibitory effects of the tested compounds on soil microorganisms, with fungi as an exception. A long-lasting negative action on the activity of the dehydrogenase (DHA), commonly used as an index of the overall microbial activity in soil, was found. The magnitude of these effects were dependent on the assayed concentrations of the herbicides mixture. We concluded that the presence of bromoxynil + prosulfuron could induce significant changes in the microbial populations of the soil, concerning the activity and balance of microbial community. Possible environmental risks must be considered. Dehydrogenase activity was shown to be an important indicator of side-effects attributed to these herbicides.     

植被不同退化状态下尕海湿地土壤氮含量及酶活性特征

土壤中氮素的吸收、转化及含量的变化是影响植被生长的关键因素。为探讨湿地植被不同退化状态对土壤氮组分含量和相关酶活性的影响,以及土壤氮组分含量与相关酶活性之间的关系,以甘南尕海湿地不同植被退化状态样地（未退化CK、轻度退化SD、中度退化MD和重度退化HD）为研究对象,采用野外采样与室内实验相结合的方法,分析了植被不同退化状态下不同形态氮组分（全氮、铵态氮、硝态氮和微生物量氮）含量的变化特征,以及土壤氮转化酶（蛋白酶、脲酶、硝酸还原酶和亚硝酸还原酶）活性之间的相关关系。结果表明：（1）在植被退化状态下,土壤含水量逐渐减小,土壤温度呈先减小后增大的趋势;（2）随着植被退化程度的加剧,硝态氮含量呈增加趋势,而全氮、铵态氮和微生物量氮含量均随退化程度加剧呈减小趋势;土壤蛋白酶活性随退化程度的加剧而减小,脲酶活性呈先减小后增大的趋势,重度退化活性最高,轻度退化最低;硝酸还原酶活性随退化程度的加剧而增加,亚硝酸还原酶活性表现为"升-降-升"的变化趋势,即轻度退化活性最高,未退化和中度退化较低;（3）土壤蛋白酶活性与全氮、铵态氮和微生物量氮呈极显著正相关关系（P < 0.01）,与硝态氮含量呈显著负相关关系（P < 0.05）;硝酸还原酶活性与蛋白酶活性恰好相反;脲酶活性与微生物量氮含量呈极显著正相关关系（P < 0.01）,与全氮含量呈显著正相关关系（P < 0.05）;亚硝酸还原酶活性与全氮和铵态氮含量呈极显著正相关关系（P < 0.01）,与硝态氮含量呈显著负相关关系（P < 0.05）。综上,在尕海湿地植被退化条件下,土壤氮组分含量增加可以有效提高相关酶活性。     

Persistence of Invertebrate iridescent virus 6 in soil

Soil represents an important reservoir for mostentomopathogenic viruses. Invertebrateiridescent viruses (IIVs) (Iridoviridae) arenon-occluded DNA viruses that infectagriculturally and medically important insectspecies, especially in damp or aquatichabitats. We used virus extraction and insectbioassay techniques to determine the effect ofsoil moisture and soil sterility on thepersistence of Invertebrate iridescentvirus 6 (IIV-6) in a soil over a 90 day periodin the laboratory. Loss of activity of IIV-6in dry soil (6.4% moisture, –1000 kPa matricpotential) was very rapid and was not studiedbeyond 24 h. Soil moisture did not affect therate of inactivation of virus in damp (17%moisture, –114 kPa matric potential) or wetsoil (37% moisture, –9.0 kPa matricpotential). In contrast, soil sterilizationsignificantly improved the persistence of IIV-6activity, both in damp and wet soil. Controlvirus suspensions retained 0.72–0.87% oforiginal activity after 90 days, which wassignificantly more than the activity retainedin soil. These figures represent half lives of4.9 days for IIV-6 in non-sterile soil, 6.3days in sterilized soil (data pooled formoisture treatments), and 12.9 days for thecontrol virus suspension. We conclude thatextra-host persistence in soil habitats may bean important aspect of the ecology of IIVs.     

Effect of Soil Texture and Moisture on the Activity of Entomopathogenic Nematodes Against Female Boophilus annulatus Ticks

Soil texture, chemistry and moisture have a profound effect upon the activity and persistence of entomopathogenic nematodes (EPNs). Whereas nematodes’ natural habitat is within the soil, ticks and other arthropod pests prefer to stay on the soil surface and under stones or leaf litter; they spend much of their life cycle in the humid environment of the soil upper layer, therefore consideration of the effect of the soil environment on nematode activity is a pre-requisite for the sucessful use of EPNs against arthropod pests. In the present study we investigated the effects of soil type, and humidity on various nematode strains and on their effectiveness against ticks. Many infective juveniles (IJs) of Steinernema carpocapsae and S. riobrave were found in the uppermost soil layer whereas the heterorhabditid strains were almost absent from the upper 6 cm of the soil profile. The IJs of S. feltiae, and the S. carpocapsae strain S-20, exhibited an intermediate behavior. It was found that the activity of IJs of S. carpocapsae in the soil upper layer (1 cm depth) was strongly affected by soil type: the greatest number of IJs were recorded from sandy loam soil; less were found in the lighter soils – ‘Marine sand’ and ‘Calcareous sandstone’ – and only very few were recovered from heavy soils. Strikingly, even when the soil moisture was low and the number of nematodes found in the upper layer correspondingly low, tick mortality remained high. The results demonstrate: (a) the possible use of the nematodes as an anti-tick agent; (b) the importance of knowing the exact interaction of nematodes with the immediate environment of the pest, in order to optimize the pest-control activity of the nematode.     

Acetylene Reduction by Soil Cores of Maize and Sorghum in Brazil

Nitrogenase activity was measured by the C₂H₂ reduction method in large soil cores (29 cm in diameter by 20 cm in depth) of maize (Zea mays) and sorghum (Sorghum vulgare). The activity was compared to that obtained by a method in which the roots were removed from the soil and assayed for nitrogenase activity after an overnight preincubation in 1% O₂. In a total of six experiments and 28 soil cores, the nitrogenase activity of the cores was an average of 14 times less than the activity of roots removed from the same cores and preincubated. Nitrogenase activity in the cores was very low and extrapolated to an average nitrogen fixation rate of 2.8 g of N/hectare per day. It was shown that inadequate gas exchange was not a reason for the lower activity in the soil cores, and the core method gave satisfactory results for nitrogenase activity of soybeans (Glycine max) and Paspalum notatum.     

硫对铅污染水稻土微生物活性及群落结构的影响

对含有不同浓度铅的水稻土添加硫代硫酸钠进行土培试验,研究硫作用下铅污染水稻土微生物活性及群落结构的变化.结果表明:添加硫底物后,土壤的氧化还原电位(Eh)升高,呼吸强度增强,硫氧化菌的数量显著增加.硫促进了土壤中硫氧化菌等微生物的生长并引起群落结构的变化,克隆测序表明,加硫处理下土壤微生物的特异性条带与拟杆菌、硫杆菌、β-变形菌和嗜酸菌具有很高的相似性.硫处理下土壤碳酸盐结合态及铁锰结合态铅含量发生了显著变化.     

水分对土壤呼吸的影响及机理

土壤呼吸是陆地碳循环的重要环节,在全球变化的背景下,研究水分对土壤呼吸的影响,能为探索陆地生态系统在碳循环方面的源—汇功能和揭示碳的失汇之迷提供有力的证据。综述了水分对土壤呼吸的影响及其机理。土壤呼吸是一个复杂的生态学过程,大气降水对土壤呼吸的影响结果是因时、因地而异,在湿润的生态系统或者干湿交替的生态系统中比较湿润的季节．降水事件对土壤呼吸可能会产生比较明显的抑制现象;而在干旱的生态系统或有干湿交替季节的生态系统中比较干旱的季节里,降水事件可能会强烈地激发土壤呼吸。其对土壤呼吸的影响机理包括水分对土壤孔隙中CO2替代、对CO2扩散的阻滞、对微生物活动的刺激和对微生物生物量的影响等。由于实验方法和标准的不一致以及影响土壤呼吸的因素的多样性。水分量的变化对土壤呼吸的影响很难以一个统一的方程来描述,总的来说,最优的水分状况通常是接近最大田间持水力,当土壤处于过于或过湿状态时,土壤呼吸会受到抑制。水分量的变化对土壤呼吸的影响机制在于可溶性有机质、土壤的通透性、微生物与植物根系生命活动等都随土壤水分状况不同而发生相应的改变。关于水分与土壤呼吸的关系研究今后应该主要集中在：(1)水分对根系呼吸和土壤微生物呼吸分别产生的影响;(2)全球变化后水分格局的变化对全球陆地生态系统土壤呼吸格局的潜在影响;(3)人类活动通过直接或间接改变水分状况而对土壤释放CO2的贡献率。     

Phosphorus in the soil-plant-animal ecosystem

Summary A compartmental model of phosphorus in soil-plant-animal ecosystem is described. It consists of 17 compartments, five in soil, six in plant, three in above ground fauna and three in soil organisms and microorganisms. Common amounts and rates of turnover in each of these compartments is presented. Though the total amount of P in the ecosystem is large, only a very small part of it is being cycled, and presented data show that removal of P from an agricultural pastoral ecosystem is very slight. Most of the available phosphorus which is absorbed by plant roots is gradually fixed in forms of long-range unavailability, both by plants and by animals. This process of biological fixation is counterbalanced mainly by the activity of soil microorganisms. Quantities of input-output of P in intensive pastoral ecosystems are also presented, and some agronomical and ecological implications are considered. The manipulation of soil microorganisms and change towards more desirable P releasing strains or species may decrease need of fertilization, lower the risk of eutrophication and enhance productivity of such ecosystems. Such manipulations, however, can be achieved only after appropriate research.Contribution from the Agricultural Research Organization, The Volcani Center, Bet Dagan, Israel. 1976 Series No. 160-EThis paper was presented as a lecture at the first N.H. Tadmor Memorial Meeting, December 1974, Jerusalem, Israel     

Soil Microorganisms of the McMurdo Sound Area, Antarctica

A study of soil microorganisms of Ross Island and the adjacent mainland was carried out during the brief austral summer of 1961-1962. In some cases, seasonal changes in microbial numbers were observed, although microorganisms could not be detected in some soils. Bacterial species common to temperate regions were isolated from a number of different samples. Thermophilic bacteria were present in some of the soils, and a significant portion of the bacterial population was capable of growth at 2 C. The soil microflora were capable of carrying out certain reactions of the nitrogen cycle at a very slow rate. In addition to temperature, other environmental factors which might influence growth and metabolic activity were discussed.     

Effect of the insecticide nerametrine EK-15 on the activity of soil microorganisms

The effect of the insecticide Nerametrine EK-15 (containing an active supercypermetrine component) on nitrification, nitrogen fixation, CO₂ production and cellulase activity of soil microorganisms was investigated. Four soil types were sampled from various localities. Supercypermetrine at 31 pmol/kg soil affected remarkably the metabolic activity of all soil samples tested by producing CO₂ after a 1-d exposure. After a 14-d exposure no difference in the metabolic activity related to CO₂ production was noticed in the case of garden soil where the insecticide at 31 pmol/kg soil and the unaffected control were used. As far as other samples are concerned, the supercypermetrine concentration amounting to 31 pmol/kg soil explicitly inhibited the metabolic activity of soil microorganisms. On the other hand, concentrations of 0.61 and 6.1 pmol/kg soil stimulated the metabolic activity of soil in the locality of Senica. The soil samples enriched with nutrients (organic nitrogen in urea) manifested an evident inhibition at 31 pmol/kg soil. The nitrification activity of all soil types was interrupted at 61 pmol/kg soil. Supercypermetrine 0.12 pmol/L stopped completely nitrogen fixation withA. chroococcum and that corresponding to 0.3 pmol/L stopped aerobic cellulase decomposition.