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51.
文章以南宁市“十二五”期间城市道路网建设规划为例,根据城市道路建设的影响因素类别,剖析并协调道路建设的重大影响因素,并通过指标测算确定了规划期内道路网建设的合理规模. 相似文献
52.
随着高速公路通车里程的不断增加,如何提高高速公路的施工质量成为重要的研究课题。基于某公路沥青路面的施工实践,通过对路面平整度、密实度、离析率的控制,对如何铺就高质量的沥青路面做了详细的分析与探讨。实际施工情况表明,通过改进施工工艺,路面效果明显改善。 相似文献
53.
54.
油船货油装卸操作模拟器的系统设计 总被引:1,自引:1,他引:0
油船货油装卸操作模拟器是我们自行开发研制的用于培训油船船员的大型仿真系统。针对该模拟器的功能、要求及特点,本文主要论述了该模拟系统的硬件拓扑结构、并行智能化的软件内核设计以及模拟器的各项仿真作业功能 相似文献
55.
结构可靠度理论越来越多地被用到桥梁设计、评估与管理领域。其中一个重要的参数———目标可靠指标的取值直接影响分析结果的可靠性。采用近年发展起来的基于风险分析的生活质量准则,结合对既有公路桥梁的时变可靠度分析提出了确定桥梁评估实时的目标可靠指标的方法。通过对一座我国路网常见的简支梁桥的实例分析,阐述了该方法的过程。算例分析表明,基于生活质量分析确定的目标可靠指标考虑了不同发达水平的社会承担桥梁失效风险的能力与期望,较规范校准法的目标可靠指标取值要更合理。本文方法可为基于可靠度和风险的既有桥梁评估和管理提供理论基础。 相似文献
56.
Hydrodynamic processes control many geochemical and ecological processes in the sea. In this paper, the influence of up- and downwelling and entrainment on the ecosystem components are studied. The ecohydrodynamic model was initially used to simulate the whole Baltic Sea to get the boundary conditions for the Gulf of Riga. Then, to study the influence of different hydrodynamic conditions on the algal bloom, three simulations were made for the Gulf of Riga using different boundary and entrainment conditions. It appears that upwelling in the gulf was strongly dependent on open boundary conditions between the Baltic Proper and the gulf. The vertical transport in the Gulf of Riga was many times more intensive in the calculation system Baltic Proper and Gulf of Riga, than in the case where only the Gulf of Riga was simulated. The blue–green algal bloom was influenced by the vertical transport due to different nutrients' limitation mechanism. 相似文献
57.
The biogeochemistry of the sulfur cycle in a ca. 5-m-long sediment core from the eastern slope (221 m water depth) of the Landsort Deep in the west-central Baltic Sea was investigated by analyzing the solid phase records of sulfur isotopes and pyrite textures, besides selected main and minor elements. The sediments were deposited during post-glacial history of the Baltic Sea when the basin experienced alteration of brackish (Yoldia Sea, Littorina Sea) and freshwater (Baltic Ice Lake, Ancylus Lake) conditions. The stable isotopic composition of total sulfur was analyzed as a function of depth. In selected samples pyrite (FeS2), greigite (Fe3S4), and barite (BaSO4) fractions were separated for isotope analyses. Pyrite textures were analyzed by SEM and optical microscopy.Microbial reactions associated with the oxidation of organic matter resulted in assemblages of authigenic sulfide minerals which for the post-Ancylus Lake brackish water environment are dominated by pyrite and for freshwater environments by Fe-monosulfides. The sulfur isotopic composition of the brackish water Littorina Sea sediments (δ34S between −40 and −27‰ vs. V-CDT) is believed to be determined by cellular sulfate reduction rates and reactions involving intermediate sulfur species. The availability of reactive iron and decomposable organic matter as well as sedimentation rate and the chemocline position are important variables upon the δ34S values of sulfides in brackish water environment. The syn-depositional abundance of sulfur and organic matter, and transport of dissolved sulfur species vs. rates of microbial reactions determine δ34S in the freshwater sediments. The upper part of the Ancylus Lake sediments is sulfidized by downward diffusing H2S and/or sulfate from overlying brackish water sediments. Minor concretionary barite formation in the freshwater sediments is most likely due to the reaction of pore water sulfate diffusing downward from brackish water sediments with barium desorbed from freshwater sediments. The size distribution of pyrite framboids in the brackish sediments indicates that the formation mainly occurred from anoxic pore waters, although some pyrite formation in an anoxic water column cannot be excluded. 相似文献
58.
文章提出一种基于BP神经网络确定指标权重的方法,该方法的主要目的在于减少在确定评价指标权重时人为因素的影响,提高权重的准确性和实用性.文章以老铁山水道为例,对老铁山水道的通航现状进行了研究,分析影响其通航安全的相关因素,将灰色致因理论确定老铁山水道的通航安全评价指标体系,最后利用BP神经网络的方法给出评价指标权重,证明... 相似文献
59.
Hydrography, currents and distribution of suspended matter during a dumping experiment in the western Baltic Sea at a site near Warnemünde 总被引:1,自引:1,他引:0
During a dumping experiment on 20/21 June 2001, an extensive data record was collected to understand the dynamical processes in the water column of the investigation area and to validate model results. Weak westerly winds with strongly changing cloud coverage characterized the meteorological situation. During the second day the wind calmed down and moved shortly to easterly directions. The water column was characterized by a strong vertical stratification with discontinuity layers in temperature and salinity in 12 and 16 m. The current regime was dominated by outflow at the water surface and inflow along the German coast, with strong current shearing in the dumping area. The suspended matter clouds could be identified by optical methods and ADCP (Acoustic Doppler Current Profiler) scattering intensity. During the experiment the suspended matter plumes were only visible at the surface up to 1 h after the dumping. The aerial photographs document that the particle clouds at the surface drifted to the west and, after approximately 40 min, they were only weakly visible. The fine material was concentrated in the discontinuity layer leading to substantially higher values of optical parameters and suspended matter concentration than measured in the surface clouds. Due to the vertical current shears the material was transported in the water column in different directions. At the first day the maximum of the suspended matter in the discontinuity layer was in the north-western corner and in the bottom layer in the northeast corner of the dumping area. Strong wind conditions after the dumping led to periodical resuspension processes. 相似文献
60.
On the morphological long-term development of dumped material in a low-energetic environment close to the German Baltic coast 总被引:2,自引:1,他引:1
Karina Stockmann Rolf Riethmüller Martina Heineke Gerhard Gayer 《Journal of Marine Systems》2009,75(3-4):409-420
The development of the bed bathymetry of an experimental dumping area was followed over three-and-a-half years by means of multibeam echosounder techniques. Two types of material were discharged in the bight of Mecklenburg in the Baltic Sea in approximately 20 m of water depth. One set of the discharges was 2900 m3 of glacial till and the other set was a 2400 m3 mixture of glacial till, sand and minor amounts of cohesive matter. Only approximately 2500 m3 (86%) of the glacial till and 1500 m3 (63%) of the mixed soil materials were deposited on the seabed. This means that already during the dumping process a considerable part of the sediment material drifted away. The glacial till formed crater-like rings of 30 m diameter with peaks up to 1.4 m above seabed, whereas the spatial structure of the mixed soil material was somewhat more diffuse, but with similar magnitudes in the peaks and troughs.The morphological changes were small and their quantification required a high measuring precision in the order of few cm in the vertical. The dominant processes of surface deformation was flattening of peaks and filling of troughs. The speed of this process decreased with horizontal scale: structures of less than 4 m horizontal extension had a trend to disappear within less than five years, whereas structures of larger than 8 m extension showed little change and are estimated to remain detectable for many decades. In contrast to the reworking of the matter inside the dumping structures, no net transport of material out of the dumping area could be detected. Extrapolating the observed morphological changes into the future it is estimated that without significant decrease in internal shear strength of the disposed till the structures will persist for at least 70 years. This can be attributed to the high internal stability of the dumped glacial till and the low hydrodynamic forces present at the seabed in this region. 相似文献