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61.
The study is concerned with the influence of various factors on vibro compaction in calcareous soils, This include effect of carbonate content, and influence of pore water pressures in sand, settlements during vibrocompaction, vibroaccelerations during sand column installation compared to earthquake accelerations and finally the liquefaction design based on average CPT parameters. Previous experiences with calcareous sands and literature review confirm the necessity to apply a correlation factor for calcareous material to the raw cone penetration resistance CPT values obtained in the field. Because of the very fragile grains of the Dubai calcareous sands the penetration resistance will be influenced by crushing and grinding. To accommodate for effect of calcareous sands on measured CPT values, a best fit correlations formula called here “correlation factor” is developed. A parametric dynamic triaxial liquefaction testing programme has been executed on representative samples with loose and dense zones. Representative testing parameters for field conditions and earthquake design accelerations have been applied indicating that ground improvement is necessary. It was observed during the dynamic triaxial tests that the whole soil mass consisting of dense columns and looser zones in between behaves jointly, and therefore compaction control using an average-CPT approach is possible.  相似文献   
62.
The non-marine bivalve species Trigonioides (Kumamotoa) quadratus Gu and Ma is described from the Fourth Member of the Hekou Formation in western Fujian, southeastern China. This species previously was regarded to belong to the subgenus Trigonioides (s.s.), which is restricted to the Early Cretaceous. Herein, it is included into the subgenus Kumamotoa. It is compared to Cenomanian (early Late Cretaceous) species from Japan and Korea such as Trigonioides (Kumamotoa) mifunensis Tamura, Trigonioides (Kumamotoa) matsumotoi Kobayashi and Suzuki and Trigonioides (Kumamotoa) paucisulcatus Suzuki. The age of the Fourth Member of the Hekou Formation is discussed.  相似文献   
63.
张刚生  严俊 《矿产与地质》2006,20(3):323-324,F0003
应用光学显微镜及扫描电镜对双壳纲贝壳韧带结构色的研究表明,韧带具有非常美丽的结构色,可以做为宝石材料或收藏品.韧带结构色可能是由定向排列的纳米级文石及蛋白质纤维构成的光珊衍射引起的.韧带结构色的发现为宝石的颜色成因及光子带隙材料等研究提供了新的思路.  相似文献   
64.
凯威特型索承网壳结构的自振特性及参数分析   总被引:4,自引:0,他引:4  
索承网壳结构是由单层球面网壳和去掉上层索的张拉整体结构组成的一种跨越能力大、经济合理的新型杂交空间结构。选用梁元、杆元和索元的混合有限元模型,采用分块Lanczos法,对凯威特型索承网壳结构的自振特性及其影响因素进行了系统分析研究,并与单层网壳结构进行比较,得出了可用于工程实践的结论,对其抗震、抗风性能分析研究以及工程应用有参考价值。  相似文献   
65.
The paper is focused on the evolution of the Earth starting with the planetary accretion and differentiation of the primordial material (similar in composition to CI chondrites) into the core and mantle and the formation of the Moon as a result of the impact of the Earth with a smaller cosmic body. The features of the Hadean eon (ca. 4500–4000 Ma) are described in detail. Frequent meteorite-asteroid bombardments which the Earth experienced in the Hadean could have caused the generation of mafic/ultramafic primary magmas. These magmas also differentiated to produce some granitic magmas, from which zircons crystallized. The repeated meteorite bombardments destroyed the protocrust, which submerged into the mantle to remelt, leaving refractory zircons, indicators of the Early Earth’s geologic conditions, behind.The mantle convection that started in the Archean could possibly be responsible for the Earth’s subsequent endogenous evolution. Long-living deep-seated mantle plumes could have promoted the generation of basalt-komatiitic crust, which, thickening, could have submerged into the mantle as a result of sagduction, where it remelted. Partial melting of the thick crust, leaving eclogite as a residue, could have yielded tonalite-trondhjemite-granodiorite (TTG) melts. TTG rocks are believed to compose the Earth’s protocrust. Banded iron bodies, the only mineral deposits of that time, were produced in the oceans that covered the Earth.This environment, recognized as LID tectonics combined with plume tectonics, probably existed on the Earth prior to the transitional period, which was marked by a series of new geologic processes and led to a modern-style tectonics, involving plate tectonics and plume tectonics mechanisms, by 2 Ga. The transitional period was likely to be initiated at about 3.4 Ga, with the segregation of outer and inner cores, which terminated by 3.1 Ga. Other rocks series (calc-alkaline volcanic and intrusive) rather than TTGs were produced at that time. Beginning from 3.4-3.3 Ga, mineral deposits became more diverse; noble and siderophile metal occurrences were predominant among ore deposits. Carbonatites, hosting rare-metal mineralization, could have formed only by 2.0 Ga. From 3.1 to 2.7 Ga, there was a period of “small-plate” tectonics and first subduction and spreading processes, which resulted in the first supercontinent by 2.7 Ga. Its amalgamation indicates the start of superplume-supercontinent cycles.Between 2.7 and 2.0 Ga, the D″ layer formed at the core-mantle interface. It became a kind of thermal regulator for the ascending already tholeiitic mantle plume magmas. All deep-seated layers of the Earth and large low-velocity shear provinces, called mantle hot fields, partially melted enriched EM-I and EM-II mantles, and the depleted recent asthenosphere mantle, which is parental for midocean-ridge basalts, were finally generated by 2 Ga. Therefore, an interaction of all Earth’s layers began from that time.  相似文献   
66.
王祖华  刘东  刘均 《海洋工程》2019,37(4):80-86
为了全面掌握纵横加筋圆锥壳结构参数与其振动特性之间的关系,采用有限元软件ANSYS对纵横加筋圆锥壳进行参数化建模,并基于设计变量全组合数据,采用相关性分析、主效应分析和主成分分析方法,对纵横加筋圆锥壳结构参数与结构第一阶总体弯曲模态频率、激励力处的加速度响应总级以及结构质量之间的关系进行研究,得到了各结构参数与目标量之间关系的定量描述。为正确理解纵横加筋圆锥壳结构参数与振动特征量之间的关系提供了数据支撑,同时为此类结构的工程设计提供了参考依据。  相似文献   
67.
Es werden zwei Modelle der bikonischen Staubnebel mit einem undurchsichtigen Staubtorus in der Symmetrieebene vorgestellt: ein Modell mit Staub im ganzen Doppelkegelraum (A) und ein “leeres” Modell mit einer Staubschicht an der Oberfläche dieses leeren Raumes (B). Die Helligkeits-verteilung an der Oberfläche und die Polarisation des emittierten Lichts werden mit Hilfe einer Monte-Carlo-Simulation des Strahlungstransports im Nebel berechnet. Die Ergebnisse der Berechnungen zeigen charakteristische Merkmale, wie sie auch bei einigen kompakten Reflexionsnebeln zu beobachten sind.  相似文献   
68.
本研究以CaO、煅烧后的牡蛎壳、蛤蜊壳、扇贝壳和脉红螺壳为原料, 分别采用反相微乳液法和聚乙二醇(PEG)辅助微波加热法制备了纳米羟基磷灰石(HA), 并从产物的物理化学特性以及形态学参数方面进行比较。利用傅里叶变换红外光谱、X射线衍射对各组产物进行了化学表征, 扫描电子显微镜观察样品的表面形貌, Zeta电位仪测定样品表面的电势差。结果表明, 反相微乳液法制备的HA尺寸在(104.10±1.95) nm至(207.90±3.75) nm范围内, 为近球形颗粒; 而PEG辅助微波加热法制备得到的HA尺寸在(61.17±3.11) nm与(182.70±1.05) nm范围内, 倾向于形成椭圆及棒状的颗粒, 稳定性更高, 且各组样品均表现出完全的亲水性。此外, 对比于CaO制备的HA, 以贝壳为原料制备的HA具有更好的纳米结构, 其中利用脉红螺壳制备的HA在粒径大小、稳定性以及亲水性等方面均具有优势, 并且具有更接近天然骨的钙磷比。因此脉红螺壳可以作为PEG辅助微波加热法制备羟基磷灰石的主要原料。  相似文献   
69.
渤海湾西北岸全新世牡蛎礁研究概述   总被引:10,自引:0,他引:10  
环太平洋西岸,特别是渤海湾西北岸沿海平原全新世地层中广泛分布着由Crassostrea gigas牡蛎形成的礁体.总结了渤海湾西北岸30余年来众多研究者的主要成果.论述了C.gigas的定名沿革、生态习性、礁体特征、礁体与海面的关系.测定了C.gigas壳体的18O和13C同位素组成,发现了壳体生物碳酸钙的年际变化规律,结合可靠的14C数据,建立了正常建礁与个体分泌壳体之间的线性函数关系(约1 cm/a)、水平夹层的平均历时(约200a/层)等定量参数,进而提出"礁体历时假说",并将该地区时间跨度约7750~950 calBP的化石牡蛎礁划分为8道礁群,论证了礁体内部水平夹层和礁体之上泥质"转换层"可能记录的百年尺度的"缓变型"环境变化.  相似文献   
70.
山东地区人工防雹用弹量的估算   总被引:1,自引:1,他引:0  
陈文选 《气象》2000,26(9):36-38
利用常规探空资料计算各地特征高度,采用711雷达雹云观测资料估算雹云中雹源含水量,从而得出每个作业点一次防雹作业用弹量的近似计算公式,并将计算结果与实际作业情况进行了对比。该方法可适用于山东地区人工防雹作业中用弹量的估算。  相似文献   
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