定向钻探新型双滑块连续造斜器研究与应用

机械式连续造斜器是定向钻探技术手段之一,目前常用的LZ型连续造斜器采用单滑块与孔壁支撑,径向制动扭矩小,造斜过程中容易发生角位移,影响造斜效果,并且造斜强度不易调节。为解决造斜稳定性问题,特别设计研制了一种新型双滑块连续造斜器,该造斜器卡固稳定,造斜强度可调,器具经过野外试验验证工作可靠。新型连续造斜器的创新点在于：（1）采用双滑块结构形式,在国内还没有先例,已经取得实用新型专利;（2）增加了造斜强度调节机构,可根据施工需要调节;（3）通过工作弹簧与上滑块组件之间的螺纹连接方式来实现上滑块回位;（4）采用分压接头控制上滑块侧向力,在满足卡固要求情况下,降低造斜钻进阻力。新型双滑块连续造斜器为国内外首创,具有自主知识产权,使用效果良好,具备较好的开发推广前景。     

随时间变化的海洋平台结构系统可靠性分析

海洋平台在服役期间由于受到各种损伤,其系统可靠性将随时间而变化。本文分析了几种典型损伤——疲劳损伤、腐蚀损伤对海洋平台结构系统可靠性的影响,在考虑其对结构构件强度和承受载荷的影响情况下分析随时间而变化的海洋平台结构的系统可靠性。首先得到考虑时间因素的结构构件的强度和载荷函数,采用分枝界限法寻找结构的主要失效路径,最后以Ｄｉｔｌｅｖｓｅｎ界限法求取结构的系统失效概率。算例说明,在考虑时间因素的条件下,结构的系统可靠性将会迅速下降。按以上思路编制了空间刚架在构件强度随时间变化条件下的通用可靠性分析程序,算例表明程序是合理有效的。     

Rotation, planets, and the 'second parameter' of the horizontal branch

We analyse the angular momentum evolution from the red giant branch (RGB) to the horizontal branch (HB) and along the HB. Using rotation velocities for stars in the globular cluster M13, we find that the required angular momentum for the fast rotators is up to 1–3 orders of magnitude (depending on some assumptions) larger than that of the Sun. Planets of masses up to 5 times Jupiter's mass and up to an initial orbital separation of ~2 au are sufficient to spin-up the RGB progenitors of most of these fast rotators. Other stars have been spun-up by brown dwarfs or low-mass main-sequence stars. Our results show that the fast rotating HB stars have been probably spun-up by planets, brown dwarfs or low-mass main-sequence stars while they evolved on the RGB. We argue that the angular momentum considerations presented in this paper further support the 'planet second parameter' model. In this model, the 'second parameter' process, which determines the distribution of stars on the HB, is interaction with low-mass companions, in most cases with gas-giant planets, and in a minority of cases with brown dwarfs or low-mass main-sequence stars. The masses and initial orbital separations of the planets (or brown dwarfs or low-mass main-sequence stars) form a rich spectrum of different physical parameters, which manifests itself in the rich varieties of HB morphologies observed in the different globular clusters.     

Flow and sediment processes in a cutoff meander of the Danube Delta during episodic flooding

This article analyzes the water and suspended solid fluxes through a straightened meander of the southern branch of the Danube Delta (the St. George branch) during episodic flooding. The Mahmudia study site corresponds to a vast natural meander which was cut off in 1984–1988 by an artificial canal opened to shipping. The meander correction accelerated fluxes through the artificial canal and dramatically enhanced deposition in the former meander. After his formation, the cutoff meander acted as sediment storage locations, essentially removing channel and point bar sediments from the active sediment budget of the main channel. Increases in slope and stream power in reaches upstream and downstream have also occurred, but to a lesser degree. During the one-hundred-year recurrent flood in April 2006, bathymetry, flow velocity and discharge data were acquired across several sections of both natural and artificial channels with an acoustic Doppler current profiler (aDcp Workhorse Sentinel 600 kHz, Teledyne RDI) in order to investigate the distribution of the flow and sediment and his impact on sedimentation in a channelized reach and its adjacent cutoff. The contrasting hydro-sedimentary processes at work in both channels and bifurcation/confluence nodal points are analyzed from the measured flux distribution, morphological profiles and velocity and concentration patterns. In the cutoff, a diminishing of the intensity of the flow velocity (c. 50%) and of the SSC was observed correlated with the aggradation of the river bed. In the bifurcation/confluence nodal points and in the artificial canal were observed the most intensive hydrodynamic activity (high flow velocity, SSC concentration, degradation of the river bad). Both the event-scale and long-term morphological trends of the alluvial system are discussed analyzing the boundary shear stress and SSC variability. Excess boundary shear stress in the sub-reaches directly affected by cutoffs resulted in scour that increased downstream bed material load. These high sediment loads play a key role in driving morphological adjustments towards equilibrium in the cutoff channel.The approach followed in this paper combines detailed episodic in-situ aDcp measurements and robust numerical 1D modeling in order to provide a practical comprehension of the relevant morphodynamical processes. The 1D model reproduces robustly the continuity of hydrodynamical variables along the streamwise axes of the two-channel network. The simulated are used in the paper for highlighting reach-scale morphological processes, at both event and long-term scales.     

荷载作用下挤扩支盘桩支护特性数值模拟分析

采用室内试验和数值分析相互验证方法,对单排挤扩桩和悬臂直桩基坑支护的桩顶位移和受力特征进行了研究,进而对基坑双排挤扩桩支护特性进行了分析。试验结果表明,与悬臂直桩相比,挤扩桩支护桩顶位移小,挤扩桩支盘提供的抗倾覆力矩有效地改善了挤扩桩的工作性状;与单排挤扩桩相比,双排挤扩桩基坑支护结构刚度大,在桩身内力分配以及控制基坑变形等方面有较大优势,是深基坑工程中经济合理的支护形式。     

春季长江口北支邻近海域浮游植物群落及其影响因子

为了解长江口北支邻近海域浮游植物群落结构特征,于2014年5月对该海域进行采样调查,分析了调查区域内的浮游植物群落组成及环境影响因素,并对比了水采和网采两种采样方法所得样品的差异性。结果表明:水采浮游植物种类数(178种)和细胞平均丰度(270.32×103cells/L)均高于网采浮游植物种类数(154种)和细胞平均丰度(6.44×10~3cells/L)。骨条藻Skeletonema spp.、具槽帕拉藻Paralia sulcata和双角缝舟藻Rhaphoneis amphiceros为两种方法的共同优势种。水采样品优势种还包括线形海链藻Thalassiosira lineate、角海链藻Thalassiosira angulate、全沟藻Teleaulax spp.、锥状斯克里普藻Scrippsiella trochoidea、旋链海链藻Thalassiosira curviseriata,而网采样品优势种还有琼氏圆筛藻Coscinodiscus jonesianus。聚类分析结果显示水采浮游植物群落比网采浮游植物群落更聚集,相似性百分比分析进一步揭示两种采样方法群落格局间非相似性高达68.2%,造成两种采样方法差异的主要判别种为旋链海链藻、角海链藻和盾卵形藻Cocconeis scutellum。冗余分析表明,影响浮游植物群落分布的主要环境因子为悬浮物浓度、温度、透明度和盐度。     

长江下游"三沙"航道整治工程表面流速流向观测

简要介绍了长江下游“三沙”航道整治工程中为了掌握双锏沙横流和如皋沙中汊在刘海沙水道的汇流情况,在福姜沙左汊道→双锏沙→浏海沙水道间进行了表面流速流向观测,并对测量成果和航迹线图进行了初步分析,从而为保持双锏沙的稳定、保证如皋沙群水道的长久贯通提出了一些工程措施。     

A Numerical Modeling of the Upper and the Intermediate Layer Circulation in the East Sea

Circulation in the upper and the intermediate layer of the East Sea is investigated by using a fine resolution, ocean general circulation model. Proper separation of the East Korean Warm Current from the coast is achieved by adopting the isopycnal mixing, and using the observed heat flux (Hirose et al., 1996) and the realistic wind stress (Na et al., 1992). The simulated surface circulation exhibits a remarkable seasonal variation in the flow patterns of the Nearshore Branch, the East Korean Warm Current and the Cold Currents. East of the Oki Bank, the Nearshore Branch follows the isobath of shelf topography from late winter to spring, while in summer and autumn it meanders offshore. The Nearshore Branch is accompanied by cyclonic and anticyclonic eddies in a fully developed meandering phase. The meandering and the eddy formation of the Nearshore Branch control the interior circulation in the Tsushima Current area. A recirculation gyre is developed in the region of the East Korean Warm Current in spring and grown up to an Ulleung Basin scale in summer. A subsurface water is mixed with the fresh surface water by winter convection in the northeastern coastal region of Korea. The well-mixed low salinity water is transported to the south by the Cold Currents, forming the salinity minimum layer (Intermediate Water) beneath the East Korean Warm Current water. The recirculation gyre redistributes the core water of the salinity minimum layer in the Ulleung Basin. This revised version was published online in August 2006 with corrections to the Cover Date.     

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