Substructure hybrid testing of reinforced concrete shear wall structure using a domain overlapping technique

An online hybrid test was carried out on a 40-story 120-m high concrete shear wall structure. The structure was divided into two substructures whereby a physical model of the bottom three stories was tested in the laboratory and the upper 37 stories were simulated numerically using ABAQUS. An overlapping domain method was employed for the bottom three stories to ensure the validity of the boundary conditions of the superstructure. Mixed control was adopted in the test. Displacement control was used to apply the horizontal displacement, while two controlled force actuators were applied to simulate the overturning moment, which is very large and cannot be ignored in the substructure hybrid test of high-rise buildings. A series of tests with earthquake sources of sequentially increasing intensities were carried out. The test results indicate that the proposed hybrid test method is a solution to reproduce the seismic response of high-rise concrete shear wall buildings. The seismic performance of the tested precast high-rise building satisfies the requirements of the Chinese seismic design code.     

美国建筑抗震设计的法规体系与设计地震动的确定

本文论述了美国建筑抗震设计法规体系发展演变过程及其代表性的规范、标准与技术文档;分析了美国当前建筑法规中设计地震动参数的重要技术见解,设计地震动的不同层次与作用,基于目标风险的最大考虑地震概念等技术的进展,同时,也总结了美国抗震设计相关法规中设计地震动确定的基本规定。本文旨在从美国庞大复杂的建筑设计法规体系中,梳理出清晰的建筑抗震设计的法规体系脉络与设计地震动的要求,为我国建筑抗震设计中设计地震动的相关研究提供参照。     

Interaction of multiple courses of wave‐induced fluid flow in layered porous media

Different theoretical and laboratory studies on the propagation of elastic waves in layered hydrocarbon reservoir have shown characteristic velocity dispersion and attenuation of seismic waves. The wave‐induced fluid flow between mesoscopic‐scale heterogeneities (larger than the pore size but smaller than the predominant wavelengths) is the most important cause of attenuation for frequencies below 1 kHz. Most studies on mesoscopic wave‐induced fluid flow in the seismic frequency band are based on the representative elementary volume, which does not consider interaction of fluid flow due to the symmetrical structure of representative elementary volume. However, in strongly heterogeneous media with unsymmetrical structures, different courses of wave‐induced fluid flow may lead to the interaction of the fluid flux in the seismic band; this has not yet been explored. This paper analyses the interaction of different courses of wave‐induced fluid flow in layered porous media. We apply a one‐dimensional finite‐element numerical creep test based on Biot's theory of consolidation to obtain the fluid flux in the frequency domain. The characteristic frequency of the fluid flux and the strain rate tensor are introduced to characterise the interaction of different courses of fluid flux. We also compare the behaviours of characteristic frequencies and the strain rate tensor on two scales: the local scale and the global scale. It is shown that, at the local scale, the interaction between different courses of fluid flux is a dynamic process, and the weak fluid flux and corresponding characteristic frequencies contain detailed information about the interaction of the fluid flux. At the global scale, the averaged strain rate tensor can facilitate the identification of the interaction degree of the fluid flux for the porous medium with a random distribution of mesoscopic heterogeneities, and the characteristic frequency of the fluid flux is potentially related to that of the peak attenuation. The results are helpful for the prediction of the distribution of oil–gas patches based on the statistical properties of phase velocities and attenuation in layered porous media with random disorder.     

基于磁力资料的南海及邻区磁性基底和居里面深度特征研究

磁性基底和居里面是研究地壳和岩石圈的地质构造和热演化过程的两个重要磁性界面.为了研究南海及邻区磁性基底和居里面所反映的深部构造及其热活动的地质效应,本文在对磁异常进行化极处理的基础上,采用最小曲率位场分离方法,获得了磁性基底和居里面引起的化极磁异常,利用双界面模型快速反演方法,反演了南海及邻区的磁性基底和居里面深度,研究了磁性基底、居里面深度及其分布特征,讨论了磁性基底、居里面与新生界深度之间相关性特征及其地质意义.研究表明,磁性基底深度5~20 km,洋盆南北两侧磁性基底走向分别以NE、NEE向为主,中南半岛周缘磁性基底呈NW、NNW走向.居里面深度15~32 km,宏观表现为"洋壳浅、周缘深"及周缘"北浅南深"的特征,洋盆地区居里面深度呈现"西南浅、东部深",洋壳与陆壳接触带在居里面深度上表现为梯级带特征.新生界深度与磁性基底深度相关性（Correlation between the depth of magnetic basement and Cenozoic,CDMBC）多以不规则形状分布,在盆地的沉积中心呈现正相关;新生界深度与居里面深度相关性（Correlation between the depth of Curie surface and Cenozoic,CDCSC）多呈NE、NEE向带状正相关分布,走向与盆地走向一致;莺歌海盆地、琼东南盆地、万安盆地南部和曾母盆地CDMBC呈正相关、CDCSC呈负相关,莺歌海相关性特征推测为：居里面随岩石圈变形隆起而抬升,磁性基底张裂下沉,发生大规模沉降引起;琼东南盆地相关性特征推测为：居里面随岩石圈变形下坳而下降,沉积中心与磁性基底下沉方向一致;万安盆地和曾母盆地相关性特征推测为：深部流体沿南海西缘断裂直接进入地壳,引起该处居里面深度变浅.     

基于指标体系的浙江省地震灾害风险评估

在致灾因子危险性分析、脆弱性分析的基础上,通过选取相关指标来体现地震灾害的自然属性和社会属性,以指标权重来表征致灾因子和承灾体之间复杂作用的结果;以模糊理论为基础,采用德尔菲法(Delphi)和层次分析法(AHP)确定各指标权重,通过处理搜集到的各指标数值,得出浙江省各市的风险评估值;讨论浙江省的地震灾害风险特点,为减轻地震灾害风险提供参考。     

Characteristics of particle fluxes in the Prydz Bay polynya,Eastern Antarctica

The settling of particulate carbon in seawater is a key component of the ocean carbon cycle. We deployed a set of sediment trap in the polynya of Prydz Bay from December 2010 to December 2011 to investigate the seasonal variations in particle fluxes. There was a clear seasonal variation in the particle fluxes, with maximum and minimum fluxes recorded during the summer and winter, respectively. The average total flux over the sampling period was 193.58 mg m~(-2)d~(-1), and the average fluxes of organic carbon(C_(org)), inorganic carbon(C_(inorg)), and biogenic silica(Si_(bio)) were 721.78, 28.67, and 2382.80 μmol m~(-2) d~(-1), respectively. Si_(bio)was the main contributor to the total mass flux, and strongly correlated with C_(org). The high Si_(bio)/C_(org)molar ratios(1) suggest that C_(org)was transported to deep sea in association with Si_(bio). By comparing remote sensing data of sea ice and chlorophyll in the upper water column, we found that the dynamics of carbon fluxes were closely related to changes in sea ice. Algae in sea ice may have a key role in biological pump processes in early summer. Apart from the ice algae bloom period, variations in carbon fluxes generally corresponded with phytoplankton blooms in the upper water. The ballast effect controlled the particle settling velocity and the efficiency of the biological pump. Sea ice rafts initiated the first particle export event and enhanced the particle settling efficiency during melting period. As diatoms might become less dominant in the ice-free area, sea ice loss may cause the efficiency of the biological pump efficiency to decrease over the long term.     

基于加权预积分和快速初始化的惯性辅助单目前端模型

针对单目视觉惯性定位系统在复杂环境和相机高动态条件下的实时性和高精度的需求,提出了一种基于加权预积分和快速初始化的惯性辅助单目前端模型Improved_VIO。首先同步视觉和惯性测量数据,建立高精度的IMU加权预积分模型,为联合初始化和视觉跟踪模型提供帧间运动约束;然后构建视觉惯性融合状态向量,建立联合初始化模型,实现视觉惯性松耦合的快速联合初始化;最后在IMU加权预积分和快速初始化方法的基础上,建立一套惯性辅助的视觉跟踪模型,从而有效提高系统定位精度。在EuRoC数据集上的试验结果表明,与传统视觉惯性定位前端模型相比,本文的前端模型提升了单目视觉惯性定位的精度与实时性,初始化时间缩短至10 s内,定位精度提高了约30%。     

GABE: Galaxy Assembly with Binary Evolution

We developed a new semi-analytic galaxy formation model: Galaxy Assembly with Binary Evolution(GABE). For the first time, we introduce binary evolution into semi-analytic models of galaxy formation by using the Yunnan-II stellar population synthesis model, which includes various binary interactions. When implementing our galaxy formation model onto the merger trees extracted from the Millennium simulation, it can reproduce a large body of observational results. We find that in the local universe, the model including binary evolution reduces the luminosity at optical and infrared wavelengths slightly, but it increases the luminosity at ultraviolet wavelengths significantly, especially in FUV band. The resulting luminosity function does not change very much over SDSS optical bands and infrared band, but the predicted colors are bluer, especially when the FUV band is under consideration. The new model allows us to explore the physics of various high energy events related to the remnants of binary stars, such as type Ia supernovae, short gamma-ray bursts and gravitational wave events, and their relation with host galaxies in a cosmological context.     

基于改进的主成分分析法提取GRACE时变重力场信号

针对主成分分析法提取时变重力场模型信号中存在信号泄漏和去条带噪声不明显的问题,提出对球谐位系数主成分分析的改进方法。首先对球谐位系数进行主成分分析,提取主要的模态,再对不同模态根据其自身噪声特点选择合适的滤波方法和参数,最后在此基础上进行信号提取。以CSR发布的2005-01~2013-12(108个月)GRACE时变地球重力场模型进行实验,提取2006-06和2006-12等效水高数据和改进前的主成分分析进行比较,表明此方法在有效地剔除条带误差的同时又使得信号泄漏减小。     

2014年与2015年夏季琼东上升流的年际变化及其成因分析

本文通过2014年与2015年7月琼东海域的现场调查资料,结合卫星遥感数据,对ENSO影响下琼东上升流的变化进行研究分析,结果表明:2015年为强厄尔尼诺年,2015年7月低温高盐水总体上离表层较深,大约为20~30 m（24.5℃等温线和34等盐线）,但在近岸处（离岸20 km以内）却相对较浅,24.5℃等温线和34等盐线在整个断面抬升15~25 m,上升流的爬升现象更为明显;受西南季风影响,表层海水离岸运动,低温高盐水沿地形爬升进行补充,是典型的风生上升流。2014年为正常年份,2014年7月,整个断面低温高盐水更接近表层（近岸例外）,大约为10~20 m,同等深度低温高盐现象比2015年明显,但上升流爬升现象不明显,24.5℃等温线和34等盐线在整个断面抬升不到10 m;盛行风为东南风、向岸风,对上升流的形成起抑制作用,低温高盐水使整个断面的抬升,不符合风生上升流的特征规律,表明该年琼东上升流的形成可能与外海环流变化导致的温跃层抬升有关。