安康水电站表孔预应力闸墩优化设计

笔者以安康水电站表孔预应力闸墩为实例 ,对锚索锚固部位进行了研究 ,提出“深槽 +锚孔”结构 ,较原设计方案节省约 5 0 %锚索 ,同时方便了施工 ,为提前发电创造了条件 .     

考虑平台作用的顶张式立管动力分析

上层浮式平台的运动幅度比固定式平台大,对立管的影响更明显.为了解平台对顶张式立管动力的影响,提出一种动力分析方法.在一定的条件下建立立管的数学模型,采用软件Tube2D对平台和立管进行动力响应和弯曲应力分析,得到考虑平台作用的立管扶正器布置间距参数的敏感性和立管弯曲应力的变化.结果表明:对于考虑平台作用的立管模型而言,...     

钢套箱封底混凝土与钢管桩间的握裹力分析

承台施工时,钢套箱浇筑封底混凝土,与钢管桩粘结在一起,二者之间的握裹效果决定了承台施工的成败。采用AN SY S中的子模型技术建立了握裹力模型,验算了各种工况下的握裹力,结果表明:封底混凝土1.0 m厚时,可以满足承台一次性浇筑要求;仅有粘结应力作用时,可以保证二者间的有效结合;在桩周增设环形钢筋网片和剪力键后,握裹效果会要好。     

不同位置裂纹间的互相作用及其影响规律的有限元分析

基于有限元软件France-2D,利用J积分对含有多个裂纹的板进行应力强度因子计算。通过定义基础裂纹、干扰裂纹以及干扰参数,给出了随干扰参数改变,干扰裂纹对基础裂纹应力强度因子的影响曲线,并分析了它们的规律,其结果可为工程应用参考。     

海工混凝土结构荷载水平分析

为了获得典型构件在实际服役环境中的荷载水平范围,选取在役的3个码头梁构件设计实例,以横梁、纵梁、轨道梁为研究对象,理论分析出构件在"永久荷载"或"永久荷载+可变荷载"作用下的荷载水平;另在华南地区选取某高桩码头,进行现场应力测试与分析,得到实际服役环境下的构件荷载水平。通过现场应力测试及典型实例理论分析,确定了码头正常使用条件下钢筋混凝土结构荷载水平范围为0.1~0.47,为开展在役海工结构实际服役状态的荷载模拟试验提供依据,为码头结构设计提供参考。     

温度-围压作用下盾构隧道衬砌应力变化规律研究

为分析围岩压力和温度变化对盾构隧道衬砌应力变化的影响。文中推导了衬砌应力计算公式,并利用所得公式采用MATLAB绘制了衬砌应力变化图,对衬砌应力变化规律进行了理论分析。结果表明,①衬砌各方向应力随围岩压力的增大而线性增加;②径向与环向应力随内外壁温差增加,压应力逐渐减小到0 kPa后转变为拉应力并逐渐增大,纵向应力基本不随温差而发生改变;③当温差为正时,径向拉应力和纵向压应力逐渐减小,环向压应力减小到0 kPa后转变为拉应力逐渐增大,当温差为负时,径向压应力减小,环向和纵向压应力随半径增加而变大。分析得到的衬砌应力变化规律可为隧道支护结构设计提供参考。     

导管架平台拆除安全性分析

随着海洋石油工业的迅猛发展,废弃海洋平台的拆除问题已成为海洋工程界的研究热点,并得到世界各国该领域的广泛关注．在废弃导管架平台拆除过程中,保证其安全性是非常重要的．本文提出了用于分析导管架平台拆除安全性的危险指标Do和Ds,通过对Do和Ds的各列数据进行比较或对Do和Ds的各行数据做出折线图,可以很容易的得出最安全的桩基切割顺序。     

海洋环境温度下固体火箭发动机的温度和应力分析

为了预估海洋环境温度对舰载导弹固体火箭发动机的累积损伤作用,保证发动机的正常工作,以2个海区为环境对象,通过环境温度模型、传热模型和粘弹性本构关系,用有限元法求解了舰载导弹固体火箭发动机对海洋环境的温度和应力响应,得到了发动机中的温度分布和应力分布.结果表明,同样粘结强度时,发动机第一粘结界面比第二粘结界面更容易脱粘;药柱中星尖处应力最大,是产生裂纹的危险部位;冬季是发动机药柱容易产生裂纹的危险季节.     

表面裂纹Ⅰ型应力强度因子间的互相作用及影响规律

基于有限元软件France-3D对含有多个裂纹的平板进行应力强度因子计算．通过定义基础裂纹、干扰裂纹以及干扰参数r,α,β和2b等,给出了随干扰参数r,α,β改变,干扰裂纹对基础裂纹应力强度因子影响的λ-4,λ-α理曲线,并分析其规律,其结果可为工程应用参考．     

Circulation features in the Japan/East Sea related to statistically obtained wind patterns in the warm season

A response of the circulation in the Japan/East Sea (JES) to different kinds of wind forcing is studied, with the emphasis on the warm season, using a primitive equation oceanic model. Wind forcing is based on typical patterns obtained from complex empirical orthogonal functions of 1°-gridded NCEP/NCAR 6 h winds for 1998–2005. These patterns are distinguished by a prevailing wind direction. Northwestern wind and strong cyclonic (C) curl prevail in winter, while a variety of patterns occur in the warm season, differing in the wind direction and curl. Three model runs are performed to examine the circulation in response to a prevailing C wind stress curl or an alternating C and anticyclonic (AC) curl or a strong C curl in the warm season. The simulated features are consistent with the observational evidence, in particular with thermal fronts and frequent eddy locations derived from multi-year infrared satellite imagery. The simulated C circulation intensifies and the subarctic region extends southward with the strengthening of a summer C wind stress curl over the JES. Variability of Subarctic Front (SF) in the western JES (between 130°E and 133°E) is strongly affected by summer wind stress curl. Forcing by an AC curl tends to shift SF northward, while SF shifts to the south under the forcing by a C curl, reaching the southern Ulleung Basin in the case of the strong C curl. In the northwestern JES (off Peter the Great Bay, Russia, and North Korea), the SF northwestern branch (NWSF) is simulated. It is a known feature in autumn and early winter and can also occur in the warm season. The simulation results suggest an AC wind stress curl as the forcing of the formation of the NWSF in the warm season. The Siberia Seamount and sharply bending coastline near Peter the Great Bay facilitate partial separation of the Primorye (Liman) Current from the coast. The wind stress curl can be an additional forcing of the Tsushima Warm Current (TWC) branching off the Korea Strait to the East Korea Warm Current (EKWC) and the offshore branch (OB). In the warm season, the simulated TWC bifurcation occurs farther north, the EKWC is strong, and the OB is weak under the forcing of the AC wind stress curl. The EKWC is weak and the OB is strong under the forcing of the strong C wind stress curl.