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61.
It is expected that the vortex-induced vibration response of long flexible tubular structures exposed to a shear current will consist of multiple modes of standing and traveling waves simultaneously. The vibration characteristics of traveling wave caused by VIV and its effect on the vibration form for a flexible pipe model are presented in this paper. Two methods are proposed to reveal the characteristics of standing and traveling waves from the perspective of an instantaneous illustration and a time-averaged statistical analysis separately. The first is associated with the adoption of an illustration method depending upon an instantaneous local upper envelope to identify the dominance of the standing or traveling wave. It is found that the in-line and cross-flow wave types show synchronization in that the wave types are mostly changeless or occasionally transform from one type to the other nearly simultaneously. In both the in-line and cross-flow directions, it is evident that the vibration response is not dominated by the standing wave characteristics but can often be characterized by the alternate presence of a traveling wave and a hybrid standing-traveling wave. The second method is associated with the adoption of the significant strain peak concept proposed to estimate the occurrence of the peak strain response and fatigue damage risk. It is found that the strain peak value attributed to in-line static strain accounts for a large proportion of the final equivalent significant strain peak near the pipe end with high reduced velocities, especially when the flow velocity is high. With the occurrence of a hybrid pattern of standing-traveling wave for higher velocities, the distribution of the significant cross-flow strain peak becomes uniform and its corresponding wave shape is apt to be flat. 相似文献
62.
相山火山盆地磁性结构分布特征 总被引：1，自引：0，他引：1
以相山地区大比例尺重磁测量结果为基础,建立正演计算模型,采用模拟退火算法,反演计算了相山盆地不同深度下的物性结构分布特征,对该盆地地下岩层结构及界面变化趋势进行了半定量和定性分析;盆地深部构造岩浆活动发育,局部地段次火山岩体具向下延深和扩大的趋势;西北面磁性界面变化较复杂,磁性岩体的埋深均小于800 m;东南面磁性界面变化相对较平缓,磁性岩体的埋深均大于800 m;盆地中有多个岩浆通道,后期构造岩浆活动主要发生在盆地西南侧、南侧以及东侧,这可能是导致北西侧铀富集成矿好于这些部位的主要原因,受构造影响,盆地中部及西北部,磁性基底呈块状分布.这对指导相山的攻深找盲工作有重要意义. 相似文献
63.
2008年1月末九江雨凇转大雪天气过程成因分析 总被引：1，自引：1，他引：0
对2008年1月25—29日九江市一次雨凇转大到暴雪天气过程的大气垂直结构进行了分析。结果表明,在雨凇和降雪区域中层有暖层,低层有冷层,且存在对称不稳定层结。垂直风切变明显,有利于对称不稳定能量积累和上升气流的形成。高、低空急流辐散、辐合相互垂直,引发的较强上升运动是雨雪天气得以维持的重要条件。东西风向切变使冷、暖气流在雨雪区域上空交汇,形成水平气旋性辐合,产生垂直运动,且与垂直风切变相互作用,促动上、下层动量传递,使高、低空急流维持。雨凇转大到暴雪时,暖层气温降低,垂直风切变向上增强,对称不稳定能量增大,风向切变辐合加大,上升气流和水汽输送加大。 相似文献
64.
This is a brief research report about the recently-discovered and currently being explored Dahutang tungsten deposit (or ore field) in northwestern Jiangxi, south-central China. The deposit is located south of the Middle–Lower Yangtze River valley Cu–Au–Mo–Fe porphyry–skarn belt (YRB). The mineralization is genetically associated with Cretaceous porphyritic biotite granite and fine-grained biotite granite and is mainly hosted within a Neoproterozoic biotite granodiorite batholith. The Dahutang ore field comprises veinlets-disseminated (~ 95% of the total reserve), breccia (~ 4%) and wolframite–scheelite quartz vein (~ 1%) ore styles. The mineralization and alteration are close to the pegmatite shell between the Cretaceous porphyritic biotite granite and Neoproterozoic biotite granodiorite and the three styles of ore bodies mentioned above are related to zoned hydrothermal alteration that includes greisenization, K-feldspar alteration, silicification, carbonatization, chloritization and fluoritization arranged in time (early to late) and space (bottom to top).Five samples of molybdenite from the three types of ores have been collected for Re/Os dating. The results show Re/Os model ages ranging from 138.4 Ma to 143.8 Ma, with an isochron age of 139.18 ± 0.97 Ma (MSWD = 2.9). The quite low Re content in molybdenite falls between 0.5 ppm and 7.8 ppm that is indicative of the upper crustal source. This is quite different from molybdenites in the YRB Cu–Au–Mo–Fe porphyry–skarn deposits that contain between 53 ppm and 1169 ppm Re, indicating a mantle source.The Dahutang tungsten system is sub-parallel with the YRB porphyry–skarn Cu–Au–Mo–Fe system. Both are situated in the north margin of the Yangtze Craton and have a close spatial–temporal relationship. This possibly indicates a comparable tectonic setting but different metal sources. Both systems are related to subduction of the Paleo-Pacific plate beneath the Eurasian continent in Early Cretaceous. The Cu–Au–Mo–Fe porphyry–skarn ores are believed genetically related to granitoids derived from the subducting slab, whereas the porphyry W deposits are associated with S-type granitoids produced by remelting of the upper crust by heat from upwelling asthenoshere. 相似文献
65.
Based on support vector machines, three modeling methods, i.e., white-box modeling, grey-box modeling and black-box modeling of ship manoeuvring motion in 4 degrees of freedom are investigated. With the whole-ship mathematical model for ship manoeuvring motion, in which the hydrodynamic coefficients are obtained from roll planar motion mechanism test, some zigzag tests and turning circle manoeuvres are simulated. In the white-box modeling and grey-box modeling, the training data taken every 5 s from the simulated 20°/20° zigzag test are used, while in the black-box modeling, the training data taken every 5 s from the simulated 15°/15°, 20°/20° zigzag tests and 15°, 25° turning manoeuvres are used; and the trained support vector machines are used to predict the whole 20°/20° zigzag test. Comparisons between the simulated and predicted 20?/20° zigzag tests show good predictive ability of the proposed methods. Besides, all mathematical models obtained by the proposed modeling methods are used to predict the 10°/10° zigzag test and 35° turning circle manoeuvre, and the predicted results are compared with those of simulation tests to demonstrate the good generalization performance of the mathematical models. Finally, the proposed modeling methods are analyzed and compared with each other in aspects of application conditions, prediction accuracy and computation speed. The appropriate modeling method can be chosen according to the intended use of the mathematical models and the available data needed for system identification. 相似文献
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67.
首次运用Re-Os同位素定年法对武山铜矿南矿带的辉钼矿进行年龄测试,测得5件样品的模式年龄变化于144.0～145.7Ma,等时线年龄为146.4±2.6Ma,与花岗闪长斑岩145±3.9Ma的SISM法年龄值相吻合,表明武山铜矿南矿带成矿与晚侏罗世中酸性岩浆活动关系密切。该矿床北矿带层状、似层状硫化物型矿体曾经历海西期海底喷流-沉积成矿,而燕山期岩浆期后热液叠加改造对其形成具有重要作用,即武山铜矿最终形成于晚侏罗世。以矽卡岩型-(似)层状硫化物型矿化为主的武山铜矿稍早于同属九-瑞矿集区、以斑岩型-(似)层状硫化物型矿化为主的城门山铜矿形成,由于其成矿伴随着下扬子地区岩石圈的大规模减薄事件,成矿时间差很可能是导致两者矿化特征差异的重要原因。武山铜矿及九-瑞矿集区与铜陵、安庆和鄂东南矿集区的成岩成矿时代高度一致,它们是在统一的构造-岩浆作用过程中、与燕山期花岗质岩浆活动有关的产物。 相似文献
68.
位于青藏高原中部班公错-怒江一线的中特提斯洋盆从早侏罗世至晚白垩世,经历了从板内裂谷-洋盆扩张-双向俯冲-碰撞闭合-整体造山的全部过程,构成一个完整的威尔逊旋回.作为"活动陆缘"的羌南盆地记载着中特提斯洋盆从形成-消亡的全部沉积历史:包括裂离阶段的陆相碎屑岩、洋盆扩张阶段的稳定型碳酸盐岩、板块俯冲阶段的活动型碎屑岩、火山岩、碰撞闭合阶段的前陆盆地和弧前盆地碎屑岩、碳酸盐岩及整体造山阶段的山间盆地陆相磨拉石建造. 相似文献
69.
Based on the lightning observation data from the Fengyun-4A (FY-4A) Lightning Mapping Imager (FY-4A/LMI) and the Lightning Imaging Sensor (LIS) on the International Space Station (ISS), we extract the “event” type data asthe lightning detection results. These observations are then compared with the cloud-to-ground (CG) lightning observationdata from the China Meteorological Administration. This study focuses on the characteristics of lightning activity inSoutheast China, primarily in Jiangxi Province and its adjacent areas, from April to September, 2017–2022. In addition,with the fifth-generation European Centre for Medium-Range Weather Forecasts reanalysis data, we further delved into thepotential factors influencing the distribution and variations in lightning activity and their primary related factors. Ourfindings indicate that the lightning frequency and density of the FY-4A/LMI, ISS-LIS and CG data are higher in southernand central Jiangxi, central Fujian Province, and western and central Guangdong Province, while they tend to be lower ineastern Hunan Province. In general, the high-value areas of lightning density for the FY-4A/LMI are located in inlandmountainous areas. The lower the latitude is, the higher the CG lightning density is. High-value areas of the CG lightningdensity are more likely to be located in eastern Fujian and southeastern Zhejiang Province. However, the high-value areasof lightning density for the ISS-LIS are more dispersed, with a scattered distribution in inland mountainous areas and alongthe coast of eastern Fujian. Thus, the mountainous terrain is closely related to the high-value areas of the lightning density.The locations of the high-value areas of the lightning density for the FY-4A/LMI correspond well with those for the CGobservations, and the seasonal variations are also consistent. In contrast, the distribution of the high-value areas of thelightning density for the ISS-LIS is more dispersed. The positions of the peak frequency of the FY-4A/LMI lightning andCG lightning contrast with local altitudes, primarily located at lower altitudes or near mountainsides. K-index andconvective available potential energy (CAPE) can better reflect the local boundary layer conditions, where the lightningdensity is higher and lightning seasonal variations are apparent. There are strong correlations in the annual variationsbetween the dew-point temperature (Td) and CG lightning frequency, and the monthly variations of the dew-point tem perature and CAPE are also strongly correlated with monthly variations of CG lightning, while they are weakly correlatedwith the lightning frequency for the FY-4A/LMI and ISS-LIS. This result reflects that the CAPE shows a remarkable effecton the CG lightning frequency during seasonal transitions. 相似文献
70.
We report petrological, cathodoluminescence (CL), major and trace element analyses and fluid inclusion studies on scheelite (W)-mineralized granodiorite porphyries from Dongyuan and Zhuxiling, southern Anhui Province (China). In Dongyuan, the larger part of the granodiorite porphyry body is mineralized with W concentrations up to 1140 g/t (total WO3 reserves >140 000 tonnes), whereas in Zhuxiling mineralization is spatially more limited. All mineralized rocks are strongly altered, containing abundant calcite and no fresh plagioclase. W-mineralized rocks show higher K, Pb and lower Na, Sr, Ti contents compared to the non-mineralized ones. Co-variations between mobile elements (K, Na, Pb, Sr, Rb, etc.) and W, combined with petrological observations, demonstrate that fluid alteration must have controlled the mineralization. In quartz from both deposits 4 types of fluid inclusions have been recognized, i.e., aqueous-carbonic (WC-type), aqueous (W-type, subdivided into Wm-type containing minor detected CO2 and Wn containing no CO2), carbonic (pure CO2, C-type) and late secondary aqueous inclusions (LW-type). WC- and LW-type inclusions represent the original magmatic fluids and meteoric waters, respectively. The other inclusions represent evolved magmatic fluids which are closely related to alteration and mineralization. WC-, Wm- and Wn-type inclusions show higher salinity and lower homogenization temperatures, indicating fluid immiscibility with CO2 effervescence. Additionally, during plagioclase alteration and precipitation of K-feldspar and sericite the K/Na ratio is lowered and Ca released. The precipitation of scheelite must have been promoted by increasing Ca contents in the fluid and also by increasing pH due to CO2 loss. The present study demonstrates that for granitic rocks without calcareous wall rock, plagioclase breakdown must have been the key factor for scheelite mineralization. The presence of CO2-rich fluid indicates that both deposits formed in the same intracontinental extension setting as those in the Nanling region. Thus, the Yanshanian granites from southern Anhui Province may have a great potential for W mineralization, especially the blind ones in deep levels. 相似文献