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1.
本文介绍了某型船上建总段组合和吊装方案制定及变形控制措施的应用,并对吊装后变形情况进行了分析。  相似文献   

2.
沪东造船厂在建造47500t级散货船中采用了多项新技术,创造了船台和码头周期各为三个月的新记录。本文据此介绍缩短船台周期的D.C型总段建造技术,其中包括总段设计、精度控制、总装方法、效益等,可供同行借鉴。  相似文献   

3.
本文介绍了公理化设计方法,并基于公理化设计方法提出适合船舶3D打印的设计方法。分析了船舶3D打印需要的设计约束以及3D打印的实现目标,基于NURBS曲线提出了船体的数学型线设计方法。总结了无压载水船体结构,设计了基于3D打印技术的无压载水船体型线设计系统。  相似文献   

4.
C型独立液货舱LNG运输船在其运营期间,要遭受多种复杂载荷的联合作用,这对其整体强度尤其是货舱区结构的可靠性及安全性提出了很高的要求。本文基于CCS相关规范,对C型独立液货舱段的结构直接计算进行研究,得到其载荷计算方法,并针对液货罐与鞍座连接形式的模拟方法进行了不同的尝试与比较。最后通过对一LNG运输船实际算例的分析,得到一套合适、准确的舱段有限元直接计算方法,为LNG运输船货舱结构的设计与校核提出了合理的建议。  相似文献   

5.
中小型LNG船C型独立液货舱载荷分析   总被引:1,自引:0,他引:1  
C型独立液货舱是中小型LNG船的主要液货舱形式,通常为单圆筒或双圆筒。根据《国际散装运输液化气体船舶构造和设备》(IGC)规则,推导了最大液柱高度计算公式,并对某10000m3LNG运输船的C型独立液货舱载荷进行了计算,比较了单圆筒和双圆筒两种液货舱分别采用二维加速度椭圆合成法和三维加速度椭球合成法导致的结果差异。  相似文献   

6.
阐述巴基斯坦集装箱深水港防波堤工程采用Primavera 公司P3E/C 项目管理软件的必要性。介绍该软件的功能和特点,结合该防波堤工程,总结P3E/C 软件应用于工程所需的准备工作,并论述该软件在工程进度控制、费用控制、质量控制和安全文明施工控制方面的具体应用。应用P3E/C 软件有助于企业信息化、专业化和标准化的项目管理体系的建立。  相似文献   

7.
李汉标  张镜端 《港口科技》2010,(1):22-25,40
C型卷钢吊具是一种装卸卷钢的机械属具。用副绳作为平衡方法是一种好的选择。其操作简便,经久耐用。详细介绍了C型钩主、副绳的受力分析和长度的确定。分析了卷钢长度、重量变化对C型钩工作的影响。具有参考价值。  相似文献   

8.
通过对珠江三角洲地区粮食码头及吞吐量现状的分析,结合珠江三角洲地区的粮食需求和生产情况,通过产销平衡法预测未来珠三角粮食需求量及吞吐量,并分析了今后珠三角粮食运输结构的发展趋势。  相似文献   

9.
在具有水下岩基的港区、码头、航道施行拓深、拓宽的钻孔爆破船的快速移位和准确定位,是保证钻孔爆破船工作质量和施工效率至关重要的工序和过程。对传统的锚索定位方法和最时行的桩腿定位方法进行了阐述和比较,并展示了经创新设计的桩腿定位系统的结构和特点。  相似文献   

10.
导航系统的定位精度是影响舰船航行的重要因素。罗兰C系统和北斗定位系统由于受到台链地理位置、定位方式等因素的影响分别存在着定位精度低、安全保密性差等缺点。罗兰C/北斗组合导航系统则较好地解决了上述问题。针对几何精度因子(GDOP)方面对比研究了罗兰C系统和北斗定位系统组合前后的定位误差,并进行仿真分析。结果表明,组合后弥补了北斗定位系统有源定位的不足,一定程度上改善了罗兰C定位精度,提高了有效定位范围。  相似文献   

11.
分析9 艘圆舭型快艇船模浅水阻力系列试验资料,寻找每艘船模阻力变化规律,由108 条内插阻力曲线应用回归分析直接计算及依据深水阻力转换的间接计算分别计算浅水阻力曲线。可用于该类船型浅水功率估算及主尺度优化分析计算。对无浅水影响最小水深及超临界纵倾角也作了一定研究  相似文献   

12.
奚昕 《机电设备》2007,24(5):34-37
介绍了CAD/CAM技术以及如何应用CAD/CAM技术为减摇鳍的设计开发提供更有效的设计平台。  相似文献   

13.
A Pacific basin-wide physical–biogeochemical model has been used to investigate the seasonal and interannual variation of physical and biological fields with analyses focusing on the Sea of Japan/East Sea (JES). The physical model is based on the Regional Ocean Model System (ROMS), and the biogeochemical model is based on the Carbon, Si(OH)4, Nitrogen Ecosystem (CoSiNE) model. The coupled ROMS–CoSiNE model is forced with the daily air–sea fluxes derived from the National Centers for Environmental Prediction (NCEP) and the National Center for Atmospheric Research (NCAR) reanalysis for the period of 1994 to 2001, and the model results are used to evaluate climate impact on nutrient transport in Mixed Layer Depth (MLD) and phytoplankton spring bloom dynamics in the JES.The model reproduces several key features of sea surface temperature (SST) and surface currents, which are consistent with the previous modeling and observational results in the JES. The calculated volume transports through the three major straits show that the Korea Strait (KS) dominates the inflow to the JES with 2.46 Sv annually, and the Tsugaru Strait (TS) and the Soya Strait (SS) are major outflows with 1.85 Sv and 0.64 Sv, respectively. Domain-averaged phytoplankton biomass in the JES reaches its spring peak 1.8 mmol N m− 3 in May and shows a relatively weak autumn increase in November. Strong summer stratification and intense consumption of nitrate by phytoplankton during the spring result in very low nitrate concentration at the upper layer, which limits phytoplankton growth in the JES during the summer. On the other hand, the higher grazer abundance likely contributes to the strong suppression of phytoplankton biomass after the spring bloom in the JES. The model results show strong interannual variability of SST, nutrients, and phytoplankton biomass with sudden changes in 1998, which correspond to large-scale changes of the Pacific Decadal Oscillation (PDO). Regional comparisons of interannual variations in springtime were made for the southern and northern JES. Variations of nutrients and phytoplankton biomass related to the PDO warm/cold phase changes were detected in both the southern and northern JES, and there were regional differences with respect to the mechanisms and timing. During the warm PDO, the nutrients integrated in the MLD increased in the south and decreased in the north in winter. Conversely, during the cold PDO, the nutrients integrated in the MLD decreased in the south and increased in the north. Wind divergence/convergence likely drives the differences in the southern and northern regions when northerly and northwesterly monsoon dominates in winter in the JES. Subjected to the nutrient change, the growth of phytoplankton biomass appears to be limited neither by nutrient nor by light consistently both in the southern and northern regions. Namely, the JES is at the transition zone of the lower trophic-level ecosystem between light-limited and nutrient-limited zones.  相似文献   

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