FPSO甲板上浪研究现状

浮式生产储油轮（FPSO）是当今海洋石油开发的主流设施。FPSO通常采用单点系泊系统,船首暴露在波浪作用下,定位于特定海域进行长达数年的长期作业,上浪的风险很大。甲板上浪及其产生的载荷已是当前国际FPSO工程和研究领域的热点之一。介绍了国内外在试验研究和理论研究两方面对FPSO甲板上浪研究的进展情况,并建议我国开展这方面的研究。     

不同浪向下大型回转式起重船回转起吊作业过程的动力学分析

随着海洋开发从浅水走向深水,各种特种船舶在海洋工程建设中发挥的作用日益重要。起重船是海洋工程建设的重要工程船舶,是海洋开发的必备工具。为了更好的开发利用海洋资源,有必要进行相关设备的研究。参考某回转式起重船的具体参数,结合该船工作时的具体过程,利用大型水动力分析软件OrcaFlex建立了该起重船回转起吊作业状态下的动力学分析简化模型。通过调节不同海况下的浪向,实现了对大型回转式起重船回转起吊作业过程的的动力学分析,得到了吊物就位时不同浪向下的与接收船甲板的碰撞力、吊缆张力等,对比并分析了不同浪向时吊缆的张力变化,确定了吊物的最小碰撞力和吊缆的张力大小及波浪方向,结合计算结果,给出了大型回转式起重船回转起吊作业的优化设计方案。     

豪华邮轮耐波性及救生艇砰击载荷特性研究

利用基于三维势流理论的Wasim软件,系统研究了在不同海况下大型豪华邮轮的耐波性能及作用在救生艇上的砰击载荷。首先计算豪华邮轮在规则波和不规则波中的运动响应,分析航速、浪向和海况对豪华邮轮运动响应的影响规律,然后计算救生艇在不同海况下砰击载荷的变化规律,根据变化规律评估救生艇在实际航行中的安全性。结果表明：豪华邮轮运动响应幅值随着航速和海况的增大整体呈增大趋势,规则波中横摇运动响应幅值在浪向90°时最大;当豪华邮轮处于4级和6级海况时救生艇不发生砰击;当豪华邮轮处于8级海况且航速大于10.29 m/s时救生艇发生砰击,为保证救生艇的安全,邮轮应避免在浪向120°和浪向150°下航行,此时建议邮轮以低于12.35 m/s的航速迎浪180°航行。     

恩平油田FPSO船体总体设计研究

以作业于恩平油田15万载重吨的FPSO(浮式生产储卸油装置)为研究对象,介绍了该油田的开发方案,FPSO主要尺度、总布置以及船体性能特点。阐述了满足500年一遇环境条件、30年设计寿命、南海FPSO双层底和双船级等要求的总体设计特点。分析了使用FLUENT进行线型优化的效果;对比了基于迎浪角分析的运动性能数值计算结果和模型试验值,解释了横摇运动差异原因,描述了试验中的甲板上浪现象及采取的防护措施。     

单点系泊FPSO气隙预报的时域和频域分析

以单点系泊的FPSO为研究对象,Matlab软件为计算工具,在百年一遇的极限海况下,采用频域和时域方法对FPSO的气隙进行了数值模拟。针对频域计算结果,预报FPSO在不同浪向下的上浪危险点,并基于时域和频域计算结果,比较FPSO的气隙预报的差异。分析表明:频域方法能够用来快速预测气隙危险点的位置,但是会相对低估各个上浪分析点处的气隙高度值,而且无法考虑风标效应,频域方法无法模拟FPSO在实际环境中真实的气隙变化过程,这会高估在横浪下的FPSO的危险性。     

不同浪向下脐带缆与主平台回接过程中的动力学响应

参考文昌油气田的脐带缆截面设计及具体工作环境参数,利用水动力分析软件OrcaFlex建立了文昌缆与主平台回接过程中的动力学响应模型,计算了在不同浪向下脐带缆在与主平台回接过程中的水动力响应。通过水动力分析结果可知:绞车的牵引速度和浪向的改变对脐带缆的牵拉过程有很大影响;脐带缆发生明显弯曲的部位von mises应力也会发生明显变化,但应力仍小于API 2RD的允许应力,可满足工程安全要求。     

深水半潜式生产平台耦合动力特性对比研究

应用数值模拟与模型试验相结合的方法研究半潜式生产平台系泊状态下的耦合动力特性。建立耦合分析模型,时域内计算求解平台的动力响应,选取缩尺比为1∶60,采用等效截断模型方法对数值模拟结果进行验证。通过对比模型试验与数值模拟结果发现:等效截断系泊系统可以较好地模拟平台的位移响应,但在系泊张力方面却差异较大,此外极端海况下平台的甲板上浪问题也必须得到充分重视。     

三向载荷联合作用下的大型集装箱船结构可靠性研究

大型集装箱船（LCS）具有较大的甲板开口，抗扭刚度非常低。在恶劣海况下航行时，大型集装箱船可能会遭遇斜浪的作用，此时船体将受到三向载荷的联合作用，水平波浪弯矩和扭转波浪弯矩可能会接近甚至超过垂向波浪弯矩，船体可能因发生组合变形而破坏。因此有必要研究大型集装箱船在三向载荷联合作用下的结构可靠性。在研究三向载荷联合作用下各维度极限强度的相互关系的基础上，提出了大型集装箱船的极限承载能力的可靠性评估方法，并对目标船在各浪向角下的结构可靠性进行评估。结果表明：目标船在0°浪向角下的失效概率最高；考虑水平波浪弯矩影响后目标船的结构可靠性有所降低；扭转波浪弯矩对目标船船中剖面的结构可靠性影响较小。     

Truss Spar平台桁架管节点疲劳分析

Truss Spar平台在风、浪、流的作用下,结构受力十分复杂,准确分析其疲劳强度相当困难。通过建立Truss Spar平台三维有限元模型,利用HydroD软件进行载荷预报、波浪搜索,得到产生最大应力幅响应的最不利浪向和相位角。运用Sestra软件进行整体有限元分析,得到的结果作为桁架管节点细化模型的边界条件,再用Nastran软件进行局部分析求得节点的热点应力,修正壁厚影响。最后根据DNV规范的S-N曲线计算了管节点的疲劳寿命。     

波浪在三维圆形岛地形上的绕射研究

波浪在传播过程中遇到岛屿就会发生绕射。本文使用混合元方法对修正型缓坡方程进行了数值求解,并与KUO et al的解析解进行了比较验证。在此基础上研究了工程尺度背景下,波浪在三维圆形岛地形上的绕射,计算了不同入射波浪周期、浅滩形状参数和岛屿尺寸情况下,沿波浪传播方向断面上和岛屿岸线上的相对波高大小。计算结果表明：随着入射波周期的减小、浅滩形状参数的增大和岛屿尺寸的减小,圆形岛迎浪侧的相对波高振荡幅度、圆形岛背浪侧的相对波高大小以及岛屿岸线上的相对波高振幅和大小均随之增大。不同情况下,岛屿岸线上的相对波高最大值大多数发生在迎浪点,个别发生在迎浪点两侧20°~25°处;最小值发生在背浪点两侧30°附近。     

Ring-waves generated by water drops impacting on water surfaces atrest

Radar observations of the ocean surface can be affected by impacting raindrops. Ring-wave measurements are presented for drops of 2.2 and 2.8 mm in diameter impacting on fresh and salt water surfaces initially at rest. They are based on the observation of the mirror image of a sharp edge on the perturbed surface. The retrieved wave profiles show a rather stable characteristic wavenumber (0.2 mm^-1) and very small wave amplitudes: the fraction of the incident kinetic energy converted into ring-waves is of the order of 1%     

南海表面浮力通量、水型变性及南海"暖水"的消长分析

利用英国南安普敦海洋中心(SOC)海-气界面的热量和淡水通量资料以及世界大洋图集(WOA01)的海面温度和盐度资料计算了南海表面各月的有效浮力通量及水型变性矢量场,分析了南海表层暖水形成和发展的季节性特征。研究结果表明,南海表层暖水的发展、维持以及消亡在很大程度上受到海洋表层浮力通量的影响;此外,南海上层水体密度的垂直结构和变化也深受表面浮力通量和表层水型变性的影响。在中、北部,南海的垂向结构季节性变化较为明显,其中冬季表层水体的下沉强度最大,深度最深,而夏季表层水体却无下沉趋势。     

海湾水交换对取排水工程的响应

建立三门湾附近海域的水动力和水质模型,研究核电站取排水工程对海湾水交换的影响。计算得到取排水工程建立后三门湾海域40 d的海水交换率由51.60%变为51.06%,降低了0.54%。将三门湾海域分区分析,结果发现靠近排水工程的汊道水交换率降低最多,降低了5.36%,其余区域水交换率也都有所降低,但是降低幅度不大。结果表明:取排水工程的建立使得湾内水流状况发生变化,不同区域的水交换率变化相差较大;排水工程切断了附近汊道水流与外海的交换,导致排水口附近海域水交换率降低最多。     

Thermodynamic characteristics of water in natural water bodies with a high mineralization

To adequately describe the hydrophysical processes in water bodies with a high mineralization, it is necessary to take into account the dependence that the thermodynamic characteristics of water have on the amount of salts contained in it. This work investigates some widely known formulas for calculating a number of thermodynamic parameters of mineralized water. The density, freezing temperature, specific heat of evaporation, and relative pressure of saturated vapor over the surface are considered. The possibilities of using these formulas when modeling hydrophysical processes in water bodies with salinity in the range of 0–250 pro mille are analyzed. It is shown that the formulas under consideration should be used when the salinity does not exceed 100 pro mille. If the mineralization is higher, it is necessary to elaborate more suitable formulas on the basis of an approximation of in situ data or data from handbooks.     

Study on interaction between the coastal water, shelf water and Kuroshio water in the Huanghai Sea and East China Sea

The main processes of interaction between the coastal water, shelf water and Kuroshiowater in the Huanghai Sea (HS) and East China Sea (ECS) are analyzed based on the observation and study results in recent years. These processes include the intrusion of the Kuroshio water into the shelf area of the ECS, the entrainment of the shelf water into the Kuroshio, the seasonal process in the southern shelf area of the ECS controlled alternatively by the Taiwan Strait water and the Kuroshio water intruding into the shelf area, the interaction between the Kuroshio branch water, shelf mixed water and modified coastal water in the northeastern ECS, the water-exchange between the HS and ECS and the spread of the Changjiang diluted water.     

Refined seaward boundary conditions for modelling shallow water waves in semi-enclosed water bodies

Based on the theory of characteristics, this research elaborates on the numerical treatment of two types of seaward boundary conditions for modelling long-wave dynamics in truncated estuarine and coastal domains. These seaward boundary conditions are devised for the solution of the fully non-linear shallow water equations in the time domain. The first type is the clamped boundary, at which the water level variation is given and the velocity is computed along the characteristic line going out of the domain. The second type is the non-reflecting boundary, where the incident wave information is introduced and the reflected waves from inside the computational domain are allowed to escape at the same time. The essence of its numerical implementation is to distinguish the inward and outward characteristics and to disconnect the incoming characteristic relation from the actual flow inside the domain. Compared with previous techniques, the present method includes extra terms in the derivation to account for the effects of the uneven bed, bottom friction and shape of the characteristic lines. A shock-capturing finite difference method is used to solve the shallow water equations in the deviatoric format, but the seaward boundary algorithms constructed herein are generic and applicable to other solvers. The necessity of these refinements is highlighted by simulating the tidal oscillation in the Persian/Arabian Gulf, periodic wave runup on the coastline and the wave resonance in a narrow harbour. It is found that neglecting the bed slope at the boundary may result in biased mean water levels in the prediction.     

台湾浅滩初夏的暖水块和周围的冷水圈

本文根据1986年6月4日的卫星图像,分析了台湾浅滩及附近海域初夏表面水温分布状况,指出初夏在台湾浅滩上存在着暖水块,而其周围为冷水圈。文中计算了研究海区的潮混合状态,认为潮混合对形成这种特殊水文现象起主导作用。     

夏季楚科奇海河水与海冰融化水组分的空间变化特征

通过对2008年夏季楚科奇海水氧同位素组成的分析,运用S、δ18 O的质量平衡关系计算出河水组分和海冰融化水组分的份额,揭示出楚科奇海河水和海冰融化水组分的空间变化规律,并探讨其影响因素。楚科奇海河水组分的份额介于1.9%~18.4%之间,呈现随深度增加而降低的趋势;河水组分积分高度的变化范围为1.3~16.6m,平均为(4.8±4.0)m。河水组分份额与积分高度均呈现东高西低、北强南弱的特征,与太平洋入流东侧为富含河水组分的阿拉斯加沿岸流、西侧为低河水组分的白令海陆架水,以及北部海域受波弗特流涡埃克曼辐聚作用的影响有关。海冰融化水份额呈现随深度增加而降低的趋势,20~30m以深受到冬季海冰形成时所释放盐卤水的明显影响。海冰融化水积分高度的变化范围为-3.2~1.7m,平均值为(-0.3±1.2)m,其空间分布呈现东低西高、南强北弱的特征,与太平洋入流输入通量的时间变化以及输入路径的西偏有关。     

反渗透海水淡化给水工程的设计与应用

淡水资源短缺和水源污染已成为一个严峻的问题。“开源、节流、回用”是解决我国水问题的一个指导方针。反渗透海水淡化工程的建设,正在缓解淡水供需矛盾。文章在概述海水淡化产量与水价后,用国内外3个不同规模的实例描述反渗透海水淡化给水工程中的膜工艺设计与应用,给出海水淡化反渗透给水工程设计方案与淡化水厂的运行结果。     

Sequentially sampled gas hydrate water,coupled with pore water and bottom water isotopic and ionic signatures at the Kukuy mud volcano,Lake Baikal: ambiguous deep-rooted source of hydrate-forming water

The isotopic and ionic composition of pure gas hydrate (GH) water was examined for GHs recovered in three gravity cores (165–193 cm length) from the Kukuy K-9 mud volcano (MV) in Lake Baikal. A massive GH sample from core St6GC4 (143–165 cm core depth interval) was dissociated progressively over 6 h in a closed glass chamber, and 11 sequentially collected fractions of dissociated GH water analyzed. Their hydrogen and oxygen isotopic compositions, and the concentrations of Cl^– and HCO₃ ^– remained essentially constant over time, except that the fraction collected during the first 50 minutes deviated partly from this pattern. Fraction #1 had a substantially higher Cl^– concentration, similar to that of pore water sampled immediately above (135–142 cm core depth) the main GH-bearing interval in that core. Like the subsequent fractions, however, the HCO₃ ^– concentration was markedly lower than that of pore water. For the GH water fractions #2 to #11, an essentially constant HCO₃ ^–/Cl^– ratio of 305 differed markedly from downcore pore water HCO₃ ^–/Cl^– ratios of 63–99. Evidently, contamination of the extracted GH water by ambient pore water probably adhered to the massive GH sample was satisfactorily restricted to the initial phase of GH dissociation. The hydrogen and oxygen isotopic composition of hydrate-forming water was estimated using the measured isotopic composition of extracted GH water combined with known isotopic fractionation factors between GH and GH-forming water. Estimated δD of ?126 to ?133‰ and δ¹⁸O of ?15.7 to ?16.7‰ differed partly from the corresponding signatures of ambient pore water (δD of ?123‰, δ¹⁸O of ?15.6‰) and of lake bottom water (δD of ?121‰, δ¹⁸O of ?15.8‰) at the St6GC4 coring site, suggesting that the GH was not formed from those waters. Observations of breccias in that core point to a possible deep-rooted water source, consistent with published thermal measurements for the neighboring Kukuy K-2 MV. By contrast, the pore waters of core St6GC4 and also of the neighboring cores GC2 and GC3 from the Kukuy K-9 MV show neither isotopic nor ionic evidence of such a source (e.g., elevated sulfate concentration). These findings constrain GH formation to earlier times, but a deep-rooted source of hydrate-forming water remains ambiguous. A possible long-term dampening of key deep-water source signatures deserves further attention, notably in terms of diffusion and/or advection, as well as anaerobic oxidation of methane.