新型多柱桁架式Spar平台水动力性能研究

Spar平台以其较大的水深适应范围,较好的运动性能和稳定性,在深海油气资源开采中得到广泛的使用。随着技术的进步,各种新型的Spar平台形式不断涌现,其各方面的性能也得到大量的研究。结合前几代Spar平台形式的特点,提出了一种新型的多柱桁架式Spar平台概念,希望通过桁架的使用,保持Spar良好的运动和受力总体性能,同时采用多柱式的硬舱结构,降低建造难度和成本。并对该Spar平台的水动力特性,载荷以及运动响应进行了数值建模计算,分析结果表明,其运动响应较小,水动力性能良好。     

FPSO水动力研究与进展

浮式生产储油轮(FPSO)是当今海洋石油天然气开发的主流工程设施。就目前国际上最为关注的FPSO水动力问题,包括深水FPSO与系泊、立管系统的耦合水动力预报、甲板上浪、FPSO与穿梭油轮组成的多浮体系统水动力、横摇运动与减摇措施、单点系泊FPSO的运动稳定性等进行了阐述,介绍了我国在浅水FPSO水动力问题上的研究进展,提出加强相关研究的建议。     

Numerical and Experimental Research on the Global Performances of Cell-Truss Spar Platform

Spar technology has been applied to the deep-sea oil and gas exploitation for several years.From the first generation of classic spar,the spar platform has developed into the second generation of truss spar and the latest cell spar.Owing to its favorable adaptability to wide range of water depth and benign motion performances,spar has aroused quite a lot of interests from oil companies,universities and research institutes.In the present paper,a new cell-truss spar concept,put forward by the State Key Laboratory of Ocean Engineering(SKLOE)at Shanghai Jiao Tong University,is studied both numerically and experimentally.The numerical simulation was conducted by means of nonlinear time-domain fully coupled analysis,and its results were compared to the experimental data.Whereafter,detailed analysis was carried out to obtain the global performances of the new spar concept.Proposals for the improvement of numerical calculation and experimental technique were tabled meanwhile.     

等效水深截断的深海平台混合模型试验方法研究

以工作水深为320 m的转塔式FPSO为例,研究了等效水深截断的混合模型试验方法。选择截断水深为160 m,先后进行了截断水深系统和全水深系统模型试验,并进行了相应截断水深试验的数值重构和全水深系统的数值计算。结果证明混合模型试验技术是切实可行的,可用于深海平台的模型试验。     

颐和园万寿山岩石物理力学试验与岩矿分析

颐和园是世界文化遗产,其万寿山山体既是文物本体,也是建筑、题刻等文物和草木的载体,保护万寿山及其承载的文物,首先需要对万寿山山体的特征和岩体特性进行调查和研究。本文在查阅万寿山地质成因的基础上,测量了岩层的产状和多处裸露岩石的回弹值。对现场散落岩块进行了密度、抗拉强度、抗压强度、抗剪强度等物理力学指标测试。选取典型岩块,开展薄片、光片和电镜扫描等测试分析其矿物成分,获得了万寿山岩石矿物组成与含量比例。以上试验和测试成果是后期万寿山山体工程地质研究和石质文物保护的理论依据,具有重要的理论意义和广泛的应用价值。     

云南大平掌铜多金属矿床成矿作用

云南大平掌矿床位于澜沧江火山岩带的中南段,左侧是澜沧江和酒房深大断裂。矿区内发育一套形成于岛弧环境的上石炭统细碧-石英角斑岩系,矿体产于流纹质火山岩中,产状与火山岩一致。矿体分2类,上部为块状矿体,下部为细脉-浸染状矿体。矿床内热液蚀变发育,特别是浸染状矿体中更强,并从矿体中心向外侧形成分带。具工业意义的Cu、Pb、Zn等元素以硫化物形式产出。S、Pb、Sr、Nd等同位素成分表明,成矿物质来源于地幔-下地壳。尽管矿体受后期构造破坏强烈,但综合研究表明,该矿床仍具有世界上绝大多数火山成因块状硫化物矿床的共同性。它与区内类似矿床的差异性,为在该区寻找火山成因块状硫化物矿床开辟了新方向。     

Hydrodynamic Interactions of Three Barges in Close Proximity in A Floatover Installation

The hydrodynamics of side-by-side barges are much more complex than those of a single barge in waves because of wave shielding, viscous effects and water resonance in the gap. In the present study, hydrodynamic coefficients in the frequency domain were calculated for both the system of multiple bodies and the isolated body using both low-order and higher-order boundary-element methods with different element numbers. In these calculations, the damping-lid method was used to modify the free-surface boundary conditions in the gap and to make the hydrodynamic results more reasonable. Then far-field, mid-field and near-field methods were used to calculate wave-drift forces for both the multi-body system and the isolated body. The results show that the higher-order method has faster convergence speed than the low-order method for the multi-body case. Comparison of different methods of computing drift force showed that mid-field and far-field methods have better convergence than the near-field method. In addition, corresponding model tests were performed in the Deepwater Offshore Basin at Shanghai Jiao Tong University. Comparison between numerical and experimental results showed good agreement.     

渤海油田浅水软刚臂系泊FPSO触底分析

在线性三维势流理论的基础上,采用时域计算方法对BZ25—1油田16万吨级FPSO不同吃水条件下的碰底情况作了分析研究。数值计算结果与模型试验进行了比较,两者吻合较好,说明应用时域计算方法可以从理论上预报FPSO在浅水中的触底情况。这对我国渤海等浅水海域油田应用FPSO系统进行开发具有一定的意义。     

天山-阿尔泰东部地区海西晚期后碰撞铜镍硫化物矿床:主要特点及可能与地幔柱的关系

天山—阿尔泰东部地区是中国重要的铜镍成矿区,近年来针对区内的铜镍矿床和相关岩体的研究不断取得进展,找矿也取得了一系列新突破,已经探明了十几个矿床和矿点。笔者基于以往研究成果,结合目前地质勘查和找矿评价的新进展,比较详细地全面总结了后碰撞铜镍硫化物矿床的基本特点、成矿规律和成矿过程,并建立了描述性成矿模型。这些矿床沿一组平行的走向近东西的深大断裂分布,与成矿有关的镁铁质—超镁铁质杂岩体一般不大于5km2,小的可为一个岩墙。矿化分两种类型:通道型和熔离型。成矿时代为298~270Ma,为中亚成矿带大规模成矿期的组成部分,形成于后碰撞伸展阶段。与这组铜镍硫化物矿床有关的镁铁质—超镁铁质杂岩体可能是早二叠世大面积喷溢岩浆的残留根部或通道部分,可能与地幔柱活动有关。另外,针对区内的地质特征,结合以往找矿的成功经验,对区内进一步的找矿工作提出了一些设想和建议。     

北祁连山西段剪切带型金矿床成矿流体特征

北祁连山西段金矿床以剪切带型为主,控矿的主导因素是剪切构造和成矿流体。对寒山、鹰嘴册和珠龙等代表性矿床的流体包裹体的研究表明,产于剪切带中金矿床的成矿流体具有中低温、低密度和低盐度等特点,包裹体中气候和液体ＣＯ２／Ｈ２Ｏ比值较高。稳定同位素研究结果表明,不同矿床的成矿流体来源不尽相同,鹰嘴山浚矿床和寒山矿床成矿流体来源以深部流体为主,珠龙矿床的成矿流体主要为大气降水。