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111.
Study on Effects of Building Morphology on Urban Boundary Layer
Using an Urban Canopy Model 下载免费PDF全文
An urban canopy model is incorporated into the Nanjing University Regional Boundary Layer Model.
Temperature simulated by the urban canopy model is in better agreement with the observation, especially in the night time, than that simulated by the traditional slab model. The coupled model is used to study the effects of building morphology on urban boundary layer and meteorological environment by changing urban area, building height, and building density.
It is found that when the urban area is expanded, the urban boundary layer heat flux, thermal turbu-
lence, and the turbulent momentum flux and kinetic energy all increase or enhance, causing the surface air temperature to rise up. The stability of urban atmospheric stratiˉcation is a?ected to diffierent extent at diffierent times of the day.
When the building height goes up, the aerodynamic roughness height, zero plane displacement height
of urban area, and ratio of building height to street width all increase. Therefore, the increase in building height results in the decrease of the surface heat flux, urban surface temperature, mean wind speed, and turbulent kinetic energy in daytime. While at night, as more heat storage is released by higher buildings,thermal turbulence is more active and surface heat flux increases, leading to a higher urban temperature.
As the building density increases, the aerodynamic roughness height of urban area decreases, and the
effect of urban canopy on radiation strengthens. The increase of building density results in the decrease in urban surface heat flux, momentum flux, and air temperature, the increase in mean wind speed, and the weakening of turbulence in the daytime. While at night, the urban temperature increases due to the release of more heat storage. 相似文献
112.
红纤维虾海藻作为海洋沉水高等植物具有重要的生态与渔业价值。该物种目前已经处于濒 危状态, 且研究资料十分匮乏。本研究通过实地生境调查, 对其进行了形态学与解剖学研究, 并在此 基础上对其海洋环境的结构适应性进行了较为深入的探讨。研究结果表明: 红纤维虾海藻须根末端 膨大并密生根毛, 有利于增强植株的抓附能力和吸收能力; 表皮细胞细胞壁具有类似栓化细胞初生 壁性质的六面加厚现象, 与外部多层皮层厚角组织形成机械组织区, 叶鞘内侧含有丰富的机械组织, 使结构的抗性加强, 能承受较强的海流冲击; 雄花序中无退化雌蕊, 雌花序兼具雌蕊和退化的雄蕊, 花序轴两侧着生数枚桨状小苞片, 花粉丝状, 利于授粉, 传粉方式为水媒和半水媒传粉; 小坚果密 生倒向长鬃毛, 便于果实在海流中固着锚定。该研究弥补了目前对海洋沉水高等植物适应性进化特 征理解的不足, 也为该物种在生态修复中的应用提供了科学依据。 相似文献
113.
Four Haynesville Shale and four Bossier Shale samples were investigated using a combination of Scanning Electron Microscopy (SEM) and Broad Ion Beam (BIB) polishing. This approach enables the microstructure and porosity to be studied down to the mesopore size (<50 nm) in representative areas at the scale of the BIB cross-sections. The samples vary in mineralogy, grain size and TOC and the maturity ranges from 2.42 to 2.58 VRr in the Haynesville Shale to 1.79–2.26 VRr in the Bossier Shale. This variety within the samples enabled us to study controls on the porosity distribution in these shales. Visible pores exist as intraparticle pores mainly in carbonate grains and pyrite framboids and as interparticle pores, mainly in the clay-rich matrix. Pores in organic matter show a characteristic porosity with respect to the type of organic matter, which mainly consists of mixtures of amorphous organic matter and minerals, organic laminae and discrete macerals. A clear positive trend of organic-matter porosity with maturity was found. Pore sizes are power law distributed in the range of 4.4 μm to at least 36 nm in equivalent diameter. The differences in power law exponents suggest that a more grain supported, coarse-grained matrix may prevent pores from mechanical compaction. Porosities measured in the BIB cross-sections were significantly lower in comparison to porosities obtained by Mercury Intrusion Porosimetry (MIP). This difference is mainly attributed to the different resolution achieved with BIB-SEM and MIP and type of pore network. Extrapolation of pore size distributions (PSDs) enables the BIB-SEM porosity to be estimated down to the resolution of the MIP and thus to upscale microstructural observation at the confined space of the BIB-SEM method to bulk porosity measurement. These inferred porosities are in good agreement with the MIP determined porosities, which underpins the assumption that pores segmented in BIB-SEM mosaics are representative of the MIP methodology. 相似文献
114.
基于壳板和齿舌形态对中国沿岸几种常见多板纲软体动物的分类研究 总被引:1,自引:1,他引:0
多板纲软体动物统称石鳖,是软体动物门较为低等的一个类群,在软体动物的系统进化中占有重要的地位。但有关我国沿海多板纲软体动物的调查研究十分欠缺,而且对中国沿海多板纲的分布状况和区系特点尚不明确,并存在着一些鉴定错误和分类混乱现象。本研究利用10%Na OH溶液处理齿舌部获取齿舌带和壳板的方法,通过扫描电镜和显微镜观察拍照,对我国沿岸常见多板纲软体动物中5科7属13种的齿舌和壳板形态结构进行了描述,并进行了比较研究。 相似文献
115.
《International Journal of Digital Earth》2013,6(3):217-228
Chinese tamarisk (saltcedar) is a deciduous shrub that occurs widely across the Yellow River Delta in China. The spatial structure of Chinese tamarisk is believed to have an influence on the landscape and habitats of rare birds. In this study, first, Chinese tamarisk is detected using Canny edge detector and mathematical morphological operators based on SPOT 5 fusion-ready imagery. Then the numbers, areas, locations, and patch spacing of Chinese tamarisk patches are calculated. The experiments show that the detection accuracy of Chinese tamarisk patches is about 93.4% after the disconnection of connected patches. The distribution orientation of about 70% of the patches is approximately south–north. About 91% of the minimum distances among the patches are between 12.5 and 57.5 m. The rose graph indicates that the main azimuth between patches is north–northwest, and the second is northeast and southeast. The present study indicates that the integrating Canny edge detector with the algorithms for extracting circular and elliptical objects based on mathematical morphology is simple and effective for detecting Chinese tamarisk patches and is easy to identify the spatial structure of Chinese tamarisk patches, which reduces the time and labor for the visual interpretation of Chinese tamarisk patches. 相似文献
116.
Michael J Kingsford 《新西兰海洋与淡水研究杂志》2013,47(3):294-312
Abstract Plankton includes the primary producers and consumers that are critical for healthy ecosystem function in the marine realm. My objective was to identify the major contributions of the Leigh Marine Laboratory to our broader understanding of planktonic assemblages. Significant contributions were made prior to 1990 on the ecology of larval fishes. From the 1990s the focus changed to the sensory biology of larval invertebrates and fishes, with a strong emphasis given to the role of reef sound in attracting potential settlers. Both early and post 1980s research has been highly influential in a paradigm shift away from passively drifting larvae that have little control over their fate. Important contributions have also been made on the dynamics of nutrient–phytoplankton interactions, larval development and aquaculture. Opportunities abound for future research on the dynamics of planktonic assemblages in shelf waters and in changing seas. 相似文献
117.
Pauline A. Nye 《新西兰海洋与淡水研究杂志》2013,47(2):243-254
Macrophthalmus hirtipes (Jacquinot, 1853) excavates burrows under water in soft, muddy sand that remains waterlogged at low tide. The crabs are immersed for at least 4 h in every tide. The burrows are usually single, blind‐ending, slightly curved passages; their openings do not appear to be deliberately closed by the crabs. Excavation is effected by using one set of walking legs as a scoop while the other set provides sideways traction. Burrow openings are readily obscured by water movement, so that apparent burrow density does not give a true indication of the number of crabs in an area, but only indicates how many have been active recently; the true density may be found by sieving. The burrowing activity of M. hirtipes is compared with that of other ocypodid crabs, and the functions of burrows are discussed. A distinction is made between excavating a burrow and rapid burying, because the two behaviours are very different, and must involve different adaptations and selection pressures. 相似文献
118.
<正>Epaxial tendons play an important role in the study of the musculoskeletal system and locomotory style of dinosaurs.Although the ossified epaxial tendon lattice is fairly well known in Iguanodontoidea,only recently has knowledge of this complex been extended to ceratopsians.This study concerns the gross morphology and microstructure of the tendon lattice in Psittacosaurus,a basal ceratopsian.As in the neoceratopsian Chasmosaurus,the ossified tendons of Psittacosaurus form a three-layered, lattice-like structure.The microstructure of the tendons in large psittacosaur individuals retains an early stage of ossification,as in juvenile birds and nestling hadrosaurs,suggesting a slow developmental rate of ossification of the tendons in psittacosaur ontogeny.Comparative study indicates that a lattice-like arrangement of three-layered epaxial tendons is widely distributed in Cerapoda.This pattern also extends to Ankylosauria,implying a similar pattern of the epaxial muscles through the ornithischian clade.In addition,comparison with crocodiles implies that the different morphology of ossified tendons in dinosaurs may be associated with adaptive aspects of their paleobiology,not simply a side effect of skeletal ossification.In contrast to the short tendons in quadrupedal Chasmosaurus and Protoceratops,the elongated tendons in Psittacosaurus may be related to the bipedal locomotion characteristic of this taxon. 相似文献
119.
本研究对中国南海3种小型砗磲(Tridacnaspp.)[番红砗磲(Tridacnacrocea,包括2种外壳形态)、长砗磲(Tridacna maxima)和诺亚砗磲(Tridacna noae)]的外壳形态性状进行生物统计学差异分析。研究表明,4组砗磲外壳存在显著形态学差异。单因素方差分析发现9个外壳比例性状能够较好区分3种砗磲,且2种不同外壳形态的番红砗磲在壳宽/壳长、足丝孔宽/壳长、壳质量/壳长和左右壳厚比壳长存在显著性差异(P<0.05);在基于欧氏距离Ward法且指定聚类数k=4的条件下,4组砗磲层次聚类效果较好;主成分分析提取3个主成分建立散点图,累计主成分贡献率73.85%,各主成分贡献率依次为50.47%,13.78%和9.60%;线性判别分析得出3个判别函数,方差解释率依次为70.13%、20.97%和8.90%。3种多元统计方法从不同角度解释各组砗磲的外壳形态差异,结果均显示两组番红砗磲的外壳形态更为接近,同时长砗磲与诺亚砗磲的外壳形态较为接近。 相似文献
120.
沙丘的形态变化与移动蕴含区域风沙环境和地貌演化的关键信息,是风沙地貌研究的重要内容。以腾格里沙漠南缘的长格状和方格状沙丘为研究对象,利用风况资料和Google Earth卫星影像,监测2009—2020年两种格状沙丘的形态变化并分析其移动特征。结果表明:(1)腾格里沙漠西南缘和东南缘的主风向均为西北风,长格状沙丘分布区的次风向为东南风,方格状沙丘分布区次风向为东风和东南风,都属于低风能环境、中变率风况。西南部风能环境大于东南部,研究区近10年风动力呈衰减趋势。(2)格状沙丘的主副梁长度和间距在增加,其中,长格状沙丘高度增加,方格状沙丘高度在降低。沙丘主梁向东偏移,副梁向南偏移,形态整体保持稳定。(3)长格状沙丘平均移动速率为1.57~1.71 m·a-1,方格状沙丘平均移动速率为1.63~2.01 m·a-1,沙丘平均移动方向与合成输沙方向基本一致,沙丘的体积是造成移动速率差异的主因。 相似文献