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511.
512.
研究目的:研究花岗岩残积土的岩性特性,探讨花岗岩残积土及全风化土实测标贯击数N的概率分布,并计算其服从概率分布的概率密度函数.研究结论:目前国内外对标贯实测击数进行杆长修正没有一致意见,建议使用实测击数,可使野外编录、判别的操作性更强.通过实测结果来看,锤击数在15≤N<30范围内可定名为残积土,锤击数在30<N≤50范围内可定名为全风化土.经统计分析认为,深圳地区花岗岩残积土及全风化土实测标贯击数N的概型分布为正态分布. 相似文献
513.
组合熔断丝是将单独分立的熔断丝组合成一个零部件来使用,不仅可以降低成本,而且可以改善电路保护系统的熔断时间,这种设计将是未来汽车电路熔断丝设计的一种趋势。介绍组合熔断丝的型号、特点、优势及在电源分配中的应用。 相似文献
514.
汽车工业已经成为上海工业的龙头产业。整个汽车产业面临的发展机遇,同样为汽车物流和汽车滚装码头装卸及其延伸业务开展的企业带来了良好的发展机遇。本文对上海口岸汽车物流的现状进行调研和分析,并提出物流发展对策。 相似文献
515.
我国物流企业普遍存在条块分割、零散、重复等现象,物流企业的并购很有必要。本文对折现现金流量法在物流企业的并购中的应用作了分析。 相似文献
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517.
以尼群地平为内标,用反相高效液相色谱法(RP-HPLC)测定兔口服地尔硫后血浆和组织器官的药物浓度。药动学符合二房室模型。主要参数∶T1/2(α)=0.51h,T1/2(β)=6.11h,T1/2(ka)=0.25h,T(p)=0.52h,口服2h后在胆汁、血、脾、心、肾、肝、大脑和小脑药物浓度分别为∶0.559mg/L、0.375mg/L、4.562μg/g、0.771μg/g、1.093μg/g、1.439μg/g、0.359μg/g和0.741μg/g。 相似文献
518.
The purpose of this paper is to detect and describe general trends in the spatial distribution of epibenthic and demersal communities of Le Danois Bank (El Cachucho) in relation to the environmental variables that characterize their habitat by means of multivariate ordination. Data were derived from two multidisciplinary surveys carried out in October 2003 and April 2004 included in the ECOMARG project. The surveys were focused on the study of the physical scenario, including both geological (seabed characterization from bathymetry and backscatter data) and hydrographic features, and the different compartments of the benthic fauna (endobenthic, epibenthic, suprabenthic and demersal communities). For the present study, epibenthos and demersal species were sampled using two different gears, a 3.5 m beam trawl and a Porcupine 39/52 type baca otter trawl respectively. The total species richness combining both samplers ascended to 221, including 71 species of fishes, 65 crustaceans, 35 molluscs, 29 echinoderms, 10 cnidarians and 5 sponges.Multivariate methods were used for the study of the characteristics of communities and habitats. Hierarchical cluster analysis was applied to calculate and visualize similarities between samples in terms of species composition. To assess the amount of variation of faunal densities related to a set of eight environmental variables, a redundancy analysis (RDA) was used. The set of environmental variables used were: depth, near-bottom temperature and salinity, sedimentary typology (dry weight percentages of coarse sands, medium and fine sands, silt and organic matter) and seafloor reflectivity. Using the spatial distribution of the ranges of depth and seafloor reflectivity that characterize the habitats of the faunal assemblages we defined the spatial distribution of the different communities.The multivariate analysis of 18 beam-trawl samples and 15 otter trawl samples showed the existence of 4 main assemblages associated with the more characteristic habitats of the area. The Callogorgia–Chimaera community live mainly in the areas at the top of the Bank (425–550 m depth), where the sediment coverage is lower and there exists a high presence of rocky outcrops. The Gryphus–Galeus community were found in the areas at the top of the Bank covered by medium and fine sand sediments with low organic matter content. The Phormosoma–Trachyrincus community live on the sedimentary terraces that characterize the Bank break (550–800 m) and the Pheronema–Deania community occupy all the deeper (800–1050 m) sedimentary grounds of the inner basin. 相似文献
519.
巴黎市域轨道交通线路及车站布置特点分析 总被引:2,自引:0,他引:2
分析了巴黎市域轨道交通(RER)线的发展建设过程和线路特点,并重点研究了市域轨道交通线的几种主要车站布置形式。折返站布置能适应一端折返,且能满足列车越行的需要;终点站的折返能力和存车能力加强;换乘站合理设置侧线、渡线和相应的连络线;分岔站的布置应尽量避免主线和支线间的行车干扰,方便乘客换乘。这些市域轨道交通线线路、车站设置的特点对我国市域轨道交通线的规划、建设具有借鉴作用。 相似文献
520.
Recent sedimentary study of the shelf of the Basque country 总被引:2,自引:1,他引:1
J.-M. Jouanneau O. Weber N. Champilou P. Cirac I. Muxika A. Borja A. Pascual J. Rodríguez-Lzaro O. Donard 《Journal of Marine Systems》2008,72(1-4):397
The Northern Iberian margin of the Spanish Basque country (provinces of Gipuzkoa and Viscaia) is characterized by a narrow continental platform, which receives inputs of riverine particulate matter from the numerous riverine systems located within the Basque country. This particulate matter is subsequently deposited within the Bay of Biscay, and Gouf de Capbreton [Frouin, R., Fiuza, A.F.G., Ambar, I., Boyd, T.J., 1990. Observations of a poleward surface current off the coasts of Portugal and Spain during winter. Journal of Geophysical Research 95 (C1), 679–691]. The main goal of this study is to establish a map of the surface sediment distribution of the Basque continental shelf and more specifically to map the muddy patch located at the eastern side of that continental shelf.Three oceanographic cruises were conducted in 2003 and 2004. From these campaigns 340 surface samples, 12 short cores and 3 gravity cores have been collected over the mid and outer shelf from depths ranging between 50 m and 150 m deep. 3 seismic profiles were obtained across the shelf mud patch using a Sparker device.Sediment grain-size analyses were performed by the classical physical method of sieving and use of settling columns. The POC (Particular Organic Carbon) amounts in sediment and water samples were determined using the Strickland and Parsons' method [Strickland, J.D.H., Parsons, T.R., 1972. Determination of particulate carbon. In : A practical handbook of seawater analysis. Fisheries ResearchBoard of Canada, Ottawa, pp. 207−211] as adapted by Etcheber [Etcheber, H., 1981. Comparaison des diverses méthodes d'évaluation des teneurs en matières en suspension et en carbone organique particulaire des eaux marines du plateau continental aquitain. Journal de Recherche Océanographique VI (2), 37−42]. Radioisotopic measurements (210Pbexc) were made using a semi-planar germanium detector coupled to a multichannel analyser. Radiographical analysis was performed with an X-ray equipment (SCOPIX®) coupled with a radioscopy instrumentation and processing unit.Firstly, a detailed sedimentological map of this shelf has been produced and secondly, geophysical surveys have precisely mapped the geometry of the main mud patch on the continental shelf. In the mud patch itself the rates of sedimentation are between 0.13 and 0.50 cm yr− 1. The maximum rate of sedimentation is located in the central mud patch, whereas the minimum rate of deposition occurs close to the rocky outcrops. These results seem to be in agreement with the estimation of the total thickness of the mud patch revealed by seismic profiles. The central part corresponds to the maximum thickness of 7 m.Interpretations of the associated oceanic current forcing factors (current direction, wave fetch and wind directional modes) relating to the identified sediment depositional zones are also undertaken. 相似文献