基于MATLAB对船用辅助鼓风机性能曲线可视化研究

船用辅助鼓风机(以下简称风机)是在柴油机启动及低速工况为满足扫气系统的要求而附设的一种装置,这种风机与一般离心式通风机有明显不同,在外形尺寸上不仅要满足柴油机的安装要求,在性能上也必须达到给定的A点及B点空气流量和压力以满足柴油机起动及低负荷时对空气量的需求[1]。如何运用一种合理、高效的方法对试验数据的分析,是对风机的设计制造有着十分重要工程应用价值。因此通过运MATLAB可视化编程功能对辅助鼓风机测试数据进行最小二乘法曲线拟合,并对其拟合结果进行了分析, 拟合误差在3% 之内,得到了精准的风机的性能曲线。     

小水线面双体船减摇鳍的疲劳强度分析

针对某大型小水线面双体船两种连接方式的减摇鳍,即轴连接式和插入式减摇鳍,分别建立有限元模型,计算应力响应传递函数,确定减摇鳍疲劳累积损伤度,并对比两种类型减摇鳍的损伤结果特性。结果表明:减摇鳍与小水线面双体船下潜体相交各个部位热点应力较大,容易产生疲劳问题,且轴连接式减摇鳍的疲劳损伤比插入式的略为严重大,在设计和建造时应对这些部位重点关注。     

FPSO池火灾分析

结合现役FPSO海洋平台,基于FDS软件,编写海洋平台上部结构池火灾模拟程序。对海洋平台上部结构在不同风速下池火灾的火焰形态进行对比,对温度场进行分析,并探究不同火场的热辐射通量分布规律。分析结果对海洋平台进行火灾风险评估具有一定的工程指导意义。     

船型标准化率对三峡船闸实际通过能力的影响

推进船型标准化是提高三峡船闸实际通过能力的有效途径之一。为定量研究船型标准化程度对船闸实际通过能力的提升效果,在研究三峡库区船舶过闸流程的基础上采用系统仿真方法构建三峡库区船舶过闸仿真模型,模拟不同船型标准化率下三峡船闸的实际通过能力。仿真试验结果表明:仿真模型可以真实地反映三峡库区船舶过闸情况;船型标准化率达到90%以上时,标准船型对提升船闸运行效率的优势凸显。相比于对船闸实际通过能力的提升,船型标准化率的提高对船舶过闸服务质量的改善更为显著。     

三峡库区大型散货出口码头结构型式和装卸工艺

三峡库区具有特殊的水文地质条件,散货出口码头结构型式和装卸工艺相对落后。文章结合重庆某专用矿石出口码头的建设,提出3种适用于大型散货出口码头的结构型式和相应的装卸工艺。研究认为架空直立墩式结构及相配套的装卸工艺具有占用岸线短、使用方便、装卸效率高和造价低等优点,适宜在三峡库区大型散货出口码头建设中推广应用。     

三峡库区特殊地质3.0m直径深水桩基冲孔技术

石忠高速公路忠县长江大桥南主塔墩基础为φ3.0 m直径的19根群桩,采用冲击钻成孔施工工艺,受三峡三期蓄水影响,要求该墩桩基在4个月内完成.文章针对三峡库区特殊地质和施工环境,重点介绍了冲击钻成孔工艺的钻机设备选型、泥浆指标及除渣清孔方法、冲孔工艺工法、特殊问题处理措施等,并结合施工工效和施工实际总结分析,证明设计工艺和预案能满足本项目施工需要.     

一种新型防腐技术在舰船电子设备上的应用探讨与展望

本文简要介绍了达克罗防腐技术的发展、特点、防腐机理及工艺流程,对达克罗涂层和电镀锌镀层的性能进行了对比分析和探讨,展望了达克罗防腐技术在舰船电子设备上应用趋势。     

三峡水库变动回水区河床演变及航道整治

在系统总结前人对三峡水库变动回水区泥沙和航运问题研究主要成果的基础上,从三峡水库建库前的天然水文泥沙条件、河道边界形态及组成、河床演变规律、滩险及航道现状,建库后的水力因子变化、泥沙淤积分布及规律、河床变形及发展趋势、航道条件变化、上游来水来沙条件变化等方面,对建库后三峡变动回水区河段的演变规律及其影响因素进行了分析。在此基础上,对三峡水库变动回水区泥沙淤积对航道与港口的影响及其治理措施等进行了分析研究。     

Weathering sources in the Gaoping (Kaoping) river catchments, southwestern Taiwan: Insights from major elements, Sr isotopes, and rare earth elements

This study aims at quantifying the distribution of REEs associated with chemical weathering processes, as well as investigating weathering mechanisms and source regions of the Gaoping (formerly spelled Kaoping) River (KPR) catchment basin located at southwestern Taiwan. Spatial distributions of dissolved rare earth elements, as well as major ions, trace elements and Sr isotopes in river waters were analyzed using SF-ICPMS and TIMS. Our results indicate that REE concentrations and patterns predominantly reflect sources and intensity of chemical weathering along the river's catchment. Most specimens have high Na/Cl (4.2–30.1 mol/mol) ratios due to strong weathering intensity in the upper stream. The Na/Ca and Mg/Ca ratios suggest the main contribution is from weathering of silicates and carbonates. Total concentrations of REEs are rather low in the Gaoping (Kaoping) River (6.7–15.4 ng/L), possibly influenced by adsorption onto suspended particles. The REE patterns also reflect source heterogeneity in weathering minerals with large LREE depletion and MREE enrichment. Europium is strongly enriched in the Gaoping (Kaoping) River water, as a result of its preferential dissolution from suspended particles. Unique Gadolinium anomaly is present in all specimens, likely related to contamination due to clinic waste disposal. Small fractionations of LREE/HREE have occurred along the KPR and can be used as a distinct signature for source identification. The main stream samples exhibit a relatively wide range of ⁸⁷Sr/⁸⁶Sr, 0.71265–0.71360, with a systematical increase downstream due to source mixing of dissolved basalt (less radiogenic) and sedimentary rocks. Each tributary shows distinct Sr isotope signatures due to different rock types and ages. These isotopic and elemental compositions provide important information on weathering source and erosion budget.     

Late summer stratification, internal waves, and turbulence in the Yellow Sea

Microstructure profiling measurements at two locations in the Yellow Sea (a deeper central basin and a local shelf break) were analyzed focusing on tidal and internal-wave induced turbulence near the bottom and in the pycnocline. A classical three-layer density structure consisting of weakly stratified surface and bottom boundary layers and a narrow sharp pycnocline is developed by the end of warm season. Turbulence in the surface layer was not influenced by the tidal forcing but by the diurnal cycle of buoyancy flux and wind forcing at the sea surface. The enhanced dissipation and diffusivity generated by the shear stress at the seafloor was found in the water interior at heights 10–15 m above the bottom with a phase shift of ~ 5–6 m/h. No internal waves, turbulence, or mixing were detected in the pycnocline in the central basin, in contrast to the pycnocline near the local shelf break wherein internal waves of various frequencies were observed all the time. The thickness of the surface layer near the local shelf break slightly exceeded that of the bottom layer (20 vs. 18 m). A 5–6 m high vertical displacement of the pycnocline, which emerged during the low tide, was arguably caused by the passage of an internal soliton of elevation. During this episode, the gradient Richardson number decreased below 0.25 due to enhanced vertical shear, leading to local generation of turbulence with dissipation rates exceeding the background level by an order of magnitude.