低致病性禽流感H9N2病毒感染鸡群引起巴氏杆菌的内源性感染

摘要：目的 研究低致病性禽流感H9N2病毒感染鸡群的变化。方法 用107.4 EID50/0.1ml H9N2病毒,0.5ml/只,接种1月龄SPF鸡。结果 5日后引起鸡群发病,并引起一些个体发生死亡,剖检发现喉头充血、肺淤血,气囊膜增厚,皮下胶样浸润、出血,腺胃乳头出血,十二指肠出血。肝、脾、肾、肺常见有灰黄色坏死灶。无菌取肺组织做细菌培养时发现在血平板上有白色露珠状菌落,挑取菌落做碱性美蓝染色镜检发现两极浓染的杆状菌;经生化和PCR检验确认该菌属于多杀性巴氏杆菌。结论 低致病性禽流感H9N2病毒感染鸡群可引起巴氏杆菌的内源性感染,从而导致鸡群的高发病率与高死亡率现象。     

基于地下水合理埋深的井渠结合灌区水资源联合调控

以泾惠渠灌区为例,针对井渠结合灌区地下水超采及地下水位上升而导致的农田灌溉水环境等问题,从水位调控水量的角度出发,提出了基于地下水位合理埋深的水资源调控模式。在确定不同水文地质单元和不同植被类型条件下地下水位合理埋深上下限的基础上,结合PSO-RBF神经网络对地下水位埋深预测的结果,设计了基本、节水两种水资源联合方案,对不同保证率下的灌区水资源进行了联合调控。结果表明:泾惠渠灌区地下水位合理埋深上限介于1.76~3.50m,下限介于8.7~25.0m,不同水文地质单元、植被类型的水位埋深上下限值差异较大;水资源联合调控时,局部地区出现地下水超采,需加强节水灌溉和多水源的联合调控。     

食源性致病菌单细胞观测与预测的研究进展

微生物在单细胞水平下的生长普遍具有随机性和变异性,同时低菌量污染食品所造成的危害风险亦不可忽视,因此食源性致病菌单细胞的生长观测及预测研究逐渐成为食品预测微生物学及食源性致病菌风险评估的研究热点。在分析现有相关文献的基础上,将目前主要的食源性致病菌单细胞生长观测研究分为间接推断和直接观测两类方法;同时对食源性致病菌单细胞生长预测的模型参数与建模过程进行概述,比较了传统预测微生物的决定模型与微生物单细胞的随机模型二者之间的区别,强调了单细胞生长模型需在随机建模的基础上开展,并通过个体建模方法进一步联系其与所在食品环境之间的关系。最后,分析了食源性致病菌单细胞生长观测与预测的现状,并展望了其未来与食品安全风险评估相结合的发展趋势。     

不同施肥条件下微生物对棕壤团聚体和碳分布的影响

以北京市延庆县绿富隆有机肥蔬菜研究基地长期定位肥料试验地为试验平台,利用湿筛法获得不同粒级的团聚体,通过16SrDNA-PCR-DGGE技术进行测序分析,研究不同施肥条件下微生物群落对棕壤土团聚体和碳分布的影响。结果表明,有机肥(OF)处理的0.25～2 mm水稳性团聚体增加,增加幅度为109.0%;0.053～0.25 mm和小于0.053 mm粒级团聚体的含量均下降,与CK(不施肥)相比分别下降了31.9%和142.1%。OF处理对土壤各粒级团聚体中碳含量均有显著提高,与CK相比,提高15.2%～46.9%,其中大于2 mm团聚体中碳含量提高了46.9%。棕壤碳含量与大于2 mm粒级团聚体含量呈正相关;与0.25～2 mm粒级团聚体呈极显著正相关;与0.053～0.25 mm粒级团聚体含量呈极显著负相关;与小于0.053 mm粒级团聚体呈显著负相关。     

Vermicomposting of coffee pulp using the earthworm Eisenia fetida: Effects on C and N contents and the availability of nutrients

In Colombia, more than 1 million tons of coffee pulp are produced every year. Its transformation into compost by means of turned piles has led to a final product with poor physical and chemical characteristics and vermicomposting has been suggested as an alternative method of transforming these wastes into a useful organic fertilizer. The ability of the earthworm Eisenia fetida to transform coffee pulp into a valuable compost was evaluated. The influence of bed depth and time on different C fractions, N content and availability of nutrients was studied. The results showed that the C and N contents were not affected by the depth of the bed, whereas time affected both. An increase in the fractionation ratio, determined by calculating the C in the fraction smaller than 100 m as a percentage of C in the samples as a whole, and low values of humic-like substances were recorded during vermicomposting. After ingestion of the pulp by the earthworms, an increase in available P, Ca, and Mg but a decrease in K were detected.     

低丘红壤有机碳库的密度及变异

在中国科学院红壤生态实验站,采样分析了不同利用方式下土壤有机C 库的密度及其变异。结果表明,低丘红壤有机C 的密度0 ~ 20cm为(2.09 0.69) kg/m2,0 ~ 100 cm为(5.01 1.46) kg/m2; 全N密度0 ~ 20 cm为(0.20 0.07) kg/m2, 0 ~ 100 cm为(0.59 0.14) kg/m2。从裸地到稀疏荒草地,0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度可以提高1.0 kg/m2和1.7 kg/m2;而从稀疏荒草地到人工林地或园地,0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度可以提高0.7 kg/m2和0.9 kg/m2;稀疏荒草地如果开垦利用为水田,经长期培肥达到高度熟化,则0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度可以提高2.3 kg/m2和4.4 kg/m2。即使不同类型的人工林地和园地之间,0 ~ 20 cm和0 ~ 100 cm土壤有机C 的密度差异也可达到1.0 kg/m2和3.5 kg/m2。不同地形部位之间0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度差异达到1.3 kg/m2和2.9 kg/m2,全N密度差异达0.1 kg/m2和0.3 kg/m2;不同肥力水平之间0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度差异达到1.5 ~ 2.2 kg/m2和2.8 ~ 4.1 kg/m2,全N密度差异达0.07 ~ 0.11 kg/m2和0.20 ~ 0.23 kg/m2; 强烈侵蚀可以降低0 ~ 20 cm和0 ~ 100 cm土壤有机C 密度1.4 kg/m2和2.2 kg/m2。因此,通过调整土地利用方式,可以提高土壤有机C 库密度,增     

Carbon sequestration and saving potential associated with changes to the management of agricultural soils in England

Abstract. The potential for soil organic carbon sequestration, energy savings and the reduction of the emission of greenhouse gases were investigated for a range of changes in the management of tilled land and managed grassland. These parameters were modelled on a regional basis, according to local soils and crop rotations in England, and avoided the use of soil related indices. The largest carbon sequestration and saving contribution possible comes from an increase in the proportion of permanent woodland, such that a 10% change in land use could amount to 9 Mt C yr⁻¹ in the initial years (arable and grassland). Changes in arable management could make a significant contribution to an abatement strategy if carried out in concert with greater use of permanent conservation field margins, increased returns of crop residues and reduced tillage systems, contributing 1.3 Mt C yr⁻¹ in the initial years. It should be noted, however, that true soil carbon sequestration would be only a minor component of this (125 kt C yr⁻¹), the main part being savings on CO₂ emissions from reduced energy use, and lower N₂O emissions from reduced use of inorganic nitrogen fertilizer.     

Grazing intensity alters soil respiration in an alpine meadow on the Tibetan plateau

Grazing intensity may alter the soil respiration rate in grassland ecosystems. The objectives of our study were to (1) determine the influence of grazing intensity on temporal variations in soil respiration of an alpine meadow on the northeastern Tibetan Plateau; and (2) characterise the temperature response of soil respiration under different grazing intensities. Diurnal and seasonal soil respiration rates were measured for two alpine meadow sites with different grazing intensities. The light grazing (LG) meadow site had a grazing intensity of 2.55 sheep ha⁻¹, while the grazing intensity of the heavy grazing (HG) meadow site, 5.35 sheep ha⁻¹, was approximately twice that of the LG site. Soil respiration measurements showed that CO₂ efflux was almost twice as great at the LG site as at the HG site during the growing season, but the diurnal and seasonal patterns of soil respiration rate were similar for the two sites. Both exhibited the highest annual soil respiration rate in mid-August and the lowest in January. Soil respiration rate was highly dependent on soil temperature. The Q₁₀ value for annual soil respiration was lower for the HG site (2.75) than for the LG site (3.22). Estimates of net ecosystem CO₂ exchange from monthly measurements of biomass and soil respiration revealed that during the period from May 1998 to April 1999, the LG site released 2040 g CO₂ m⁻² y⁻¹ to the atmosphere, which was about one third more than the 1530 g CO₂ m⁻² y⁻¹ released at the HG site. The results suggest that (1) grazing intensity alters not only soil respiration rate, but also the temperature dependence of soil CO₂ efflux; and (2) soil temperature is the major environmental factor controlling the temporal variation of soil respiration rate in the alpine meadow ecosystem.     

青藏高原农田生态系统碳平衡

为探讨青藏高原农田生态系统碳平衡规律及其影响因子 ,并揭示其对全球含碳温室气体源、汇变化的贡献与响应 ,1 998～ 1 999连续 2年在拉萨农业生态站农田用静态箱法和生物量取样法开展土壤—植被界面CO2 吸收与排放的试验研究。农作物生长季 ,以冬小麦为例 ,生长前期 (从播种到拔节 )土壤碳排放量高于植被碳固定 ,生长后期 (灌浆到成熟 )则是植被碳固定高于土壤碳排放量 ,从全年来看 ,土壤碳排放量略高于植被碳固定     

碳平衡法测量汽油车燃油消耗量的研究

针对当前车辆燃油消耗量测量操作不便的问题,根据碳平衡法油耗量原理,建立了采用流量计的碳平衡法油车油耗测量模型及测量系统,并在实车上进行了试验验证,结果表明：该方法具有较高的精度及稳定性,为车辆耗油量的不解体测量提供了理论依据及应用可能性。