A 1-g shaking table investigation on response of a micropile system to earthquake excitation

Acta Geotechnica - Considering the increasing applications of micropile systems in seismically active areas, a better understanding of their seismic performance and the key controlling factors is...     

Mineralization age and sources of ore‐forming material of the Nanmushu Zn‐Pb deposit in the Micangshan Tectonic Belt at the northern margin of the Yangtze Craton,China: Constraints from Rb‐Sr dating and Sr‐Pb isotopes

The Nanmushu Zn‐Pb deposit, hosted by the Neoproterozoic Dengying Formation dolostone, is located in the eastern part of the Micangshan tectonic belt at the northern margin of the Yangtze Craton, China. This study involves a systematic field investigation, detailed mineralogical study, and Rb‐Sr and Pb isotopic analyses of the deposit. The results of Rb‐Sr isotopic dating of coexisting sphalerite and galena yield an isochron age of 486.7 ± 3.1 Ma, indicating the deposit was formed during the Late Cambrian to Early Ordovician. This mineralization age is interpreted to be related to the timing of destruction of the paleo‐oil reservoir in the Micangshan tectonic belt. All initial ⁸⁷Sr/⁸⁶Sr ratios of sphalerite and galena (0.70955–0.71212) fall into the range of the Mesoproterozoic Huodiya Group basement rocks (0.70877–0.71997) and Dengying Formation sandstone (0.70927–0.71282), which are significantly higher than those of Cambrian Guojiaba Formation limestone (0.70750–0.70980), Cambrian Guojiaba Formation carbonaceous slate (0.70766–0.71012), and Neoproterozoic Dengying Formation dolostone (0.70835–0.70876). Such Sr isotope signatures suggest that the ore strontium was mainly derived from a mixed source, and both of the Huodiya Group basement rocks and Dengying Formation sandstone were involved in ore formation. Both sphalerite and galena are characterized by an upper‐crustal source of lead (²⁰⁶Pb/²⁰⁴Pb = 17.849–18.022, ²⁰⁷Pb/²⁰⁴Pb = 15.604–15.809, and ²⁰⁸Pb/²⁰⁴Pb = 37.735–38.402), and their Pb isotopes are higher than, but partly overlap with, those of the Huodiya Group basement rocks, but differ from those of the Guojiaba and Dengying Formations. This suggests that the lead also originated from a mixed source, and the Huodiya Group basement rocks played a significant role. The Sr and Pb isotopic results suggest that the Huodiya Group basement rocks were one of the most important sources of metallogenic material. The geological and geochemical characteristics show that the Nanmushu Zn‐Pb deposit is similar to typical Mississippi Valley type, and the fluid mixing may be a reasonable metallogenic mechanism for Nanmushu Zn‐Pb deposit.     

“地理国情监测”服务县域生态环境监测及动态分析

走生态优先、绿色发展之路,是推动经济发展的基本要求。生态环境保护是我国当前及今后长期坚持的一项基本任务,已居于压倒性的战略地位。本文以多期地理国情监测数据为主要数据源,开展县域生态环境监测及动态评价,推进地理国情普查与监测成果的社会化应用。     

强干扰背景下水中微弱信号的垂直阵波束形成研究

针对垂直阵在强干扰背景下采用常规波束形成方法难以估计目标俯仰角的问题,研究了超波束与逆波束形成等方法在垂直阵中的应用。讨论了超波束与逆波束形成原理,仿真分析了其波束图,表明分辨率比常规波束形成有明显提高。实测数据分析表明：超波束方法可以分辨目标与干扰的俯仰角轨迹,对角加载逆波束 MVDR 方法可以获得目标的俯仰角轨迹。研究结果解决了强干扰背景下微弱目标信号俯仰角难以估计的问题,为微弱目标定位提供了新的途径。     

基于拉格朗日分析法的中尺度涡精细三维结构研究及其误差估计

在前人的工作中,拉格朗日分析法被用来演示大尺度环流,同时拉格朗日拟序结构可以较好的演示中尺度涡两维结构的发展过程。然而,很少研究关注怎么利用拉格朗日分析法针对中尺度涡三维结构进行演示。与以往利用欧拉方法研究中尺度涡三维结构的工作不同,我们利用拉格朗日分析法,从另一个视角来研究涡旋结构。我们在海山上方模拟出一个理想的气旋涡,涡旋内的下沉流和涡旋旁的上升流形成一个闭合的环流。这种结构很难从欧拉角度来演示。然而,粒子的运动轨迹很好地展示了整个循环:流体在涡旋中旋转下沉,汇聚到底层的上升流区,并通过上升流返回到海表面。我们也将拉格朗日分析法应用于真实的模拟结果中。作为中国南海的一个重要现象,靠近越南中部的海域中的偶极子（反气旋涡/气旋涡）,关于其结构的研究已经比较成熟了,但这些研究主要关注的是海面过程。通过拉格朗日分析,我们很好的演示了偶极子的三维结构:流体在反气旋涡(气旋涡)内部旋转上升(下沉)。更重要的是,粒子的轨迹表明,这两个涡旋之间不存在水团交换,因为强边界急流将它们彼此分开。以上结论均得到了计算误差估计的可信度支持。尽管在强辐散流和强垂直扩散流中,计算误差逐渐增大,但是在一定的时间步长和积分周期内,计算误差始终保持在一个较小的值。     

Modeling of embankment beneath marine deposited soft sensitive clays considering straightforward creep degradation

Abstract

One method straightforwardly describing the creep degradation behavior of soft marine clay is proposed and applied to the embankment modeling. Based on the experimental phenomena, the evolution of creep coefficient of soft structured clay is identified comparing with reconstituted clay, and formulated using the creep coefficient of reconstituted clay and a creep-based structure parameter relating to the inter-particle bonding. The contributions of inter-particle bonding and debonding to creep coefficient are thus considered and the creep degradation behavior is then captured straightforwardly. The creep coefficient is extended to 3D and incorporated into a newly developed elasto-viscoplastic model to describe the creep degradation in a direct way. Based on the correlations, the liquid limit is adopted as the viscosity related input parameter. The model is derived using Newton–Raphson algorithm and implemented into a Finite Element code for coupled consolidation analysis. The general applicability on creep degradation of the model is validated by simulating 1D creep, 1D CRS (constant strain rate) and 3D undrained creep tests. Finally, the enhanced model considering creep degradation is applied and validated by simulating one test embankment and one test fill on marine deposited soft sensitive clays.     

Method for calculating the encounter probability in network space

Probabilistic time geography (PTG) can be used to measure the probability of random encounters between two moving objects. Available PTG methods are based on homogeneous space, while the network space is typically heterogeneous, which constrains individuals to the network. Therefore, the PTG of the network must consider the geographic network. Based on this, we put forward a method for calculating the encounter probability of objects that are moving in a network by considering network constraints on movement. These constraints not only restrict the space‐time accessibility of the moving objects, but also affect the probability of them visiting locations or encountering other objects in space and time. Therefore, in network space, our method improves measures of the likelihood of encounters between moving objects, thereby enabling more accurate predictions of encounter events and their probabilities. Finally, the performance of the method is experimentally evaluated. In the experiment, campus road network data and simulated trip data are used to calculate the encounter probabilities of two moving objects and to determine when and where two moving objects meet with the highest probability.     

中国城市流动人口房租收入比时空格局及驱动因素

针对2012~2016年中国城市不同职业流动人口房租收入比时空变动特征及驱动力的研究表明：①流动人口房租收入比整体上呈“东高西低,南高北低”分异态势,较高及以上等级房租收入比地市集中于东部沿海发达地区及中西部省会城市。②各职业房租收入比逐渐形成金字塔形结构,但职业间房租收入比差距较大。③东部地区流动人口房租收入比多呈向下和平稳混杂分布,中部地区呈向下、平稳和向上镶嵌分布,西部地区以平稳为主,向上转移为辅。④经济、人口、社会及预期因素对房租收入比的解释力依次降低,消费水平、租赁户比例、地产投资密度、人口吸引力及收入水平是影响房租收入比的关键因素。     

Talc-beating serpentinized peridotites from the southern Mariana forearc： implications for aseismic character within subduction zones

The serpentinized peridotites overlying the subducted zones in the Izu-Bonin-Mariana (IBM) arc system have been interpret as the cause of the low-velocity layer identified beneath the IBM froearc, in turn few earthquakes occurred along the plate boundary. Chrysotile, which is a low temperature and highly hydrated phase of serpentine with low frictional strength, has been suggested as the low velocity material in the serpentinized peridotites, besides, brucite is inferred to be likely conducive to stable sliding. However, such idea encounters challenging in our serpentinized peridotites from the southern Mariana forearc, which absent both the above minerals. The presence of talc, which characterized by its weak, low-friction and inherently stable sliding behavior, provides new clue. Here we report the occurrence of talc in serpentinized peridotites collected from the landward trench slope of the southern Mariana forearc. We infer that talc is mainly forming as a result of the reaction of serpentine minerals with silica-saturated fluids released from the subducting slab, and talc also occurs as talc veins sometimes. Due to its unique physical properties, talc may therefore play a significant role in aseismic slip in the IBM subduction zone.

     

基于GPS/全站仪的村镇土地外业执法系统的研究与实现

针对我国村镇土地外业执法测量的高精度需求以及现有手段的不足,设计了基于GPS/全站仪的执法测量的业务流程;在PDA环境下建立了该系统,实现了GPS RTK高精度定位以及全站仪信号的读取和解析;并且针对GPS信号遮挡和全站仪控制网布设困难等问题,研究并实现了一种基于公共点自由设站的全站仪坐标转换方法,从而提高村镇土地执法工作的效率和精度。