海洋导管架平台优化中灵敏度分析的解析方法     

王立成  宋玉普等 《海洋工程》2001,19(3):20-24

基于杆件有限单元法和海洋导管架平台的结构特点，提出了一种导管架平台灵敏度分析的简化解析方法，给出了灵敏度分析的解析公式，指出可以在结构有限元分析的同时采用此解析方法进行灵敏度分析，相对有限差分法和半解析方法能够在很大程度上提高计算精度，减少结构重分析的次数，利用编制的灵敏度分析计算程序，对渤海BZ28－1油田储油平台进行了灵敏度验算，证明了该方法的有效性和可行性。  相似文献   

Multi-Objective Fuzzy Optimum Design Based on Reliability for Offshore Jacket Platforms     

KANG  Haigui 《中国海洋工程》2001,(4):467-478

In consideration of the fuzzy constraint boundary and through analysis of structural reliability, a model of structural fuzzy optimum design is established based on reliability for offshore jacket platforms. According to the characteristics of offshore jacket platforms, the tolerance coefficient of the constraint boundary is determined with the fuzzy optimization method. The optimum level cut set which is the intersection of the fuzzy constraint set and fuzzy objective set, is determined with the bound search method, and then the fuzzy optimum solution to the fuzzy optimization problem is obtained. The central offshore platform SZ36-1 is designed with the fuzzy optimum model based on reliability; the results are compared with those from deterministic optimum design and fuzzy optimum design. The tendency of design variables in the above three methods and its reasons are analyzed. The results of an example show that the fuzzy optimum design based on reliability is stable and reliable.  相似文献   

南海北缘一统暗沙附近深水等深流沉积体系特征          下载免费PDF全文

陈慧  解习农  毛凯楠 《地球科学》2015,40(4):733-743

利用高分辨率2D地震资料揭示南海北缘一统暗沙附近(水深700~1 000 m)发育海山相关的深水等深流沉积体系, 为南海北部陆缘深水洋流循环和深海动力学研究, 以及深水油气矿产资源勘探提供了新的资料.一统暗沙南、北两侧发育边缘侵蚀槽沟, 其中北缘的边缘槽沟可称为"环槽", 反映底流(可能属于南海中层水循环体系)自西向东流经海山.一套等深流沉积的伸长状-丘状漂积体沿环槽北岸发育.一统暗沙南侧和背侧还发育黏附型漂积体、南侧沉积区和补丁型漂积体.地震沉积记录显示该区稳定底流侵蚀-沉积活动可追溯至晚中新世早期.   相似文献   

珠江口盆地白云凹陷珠江组深水牵引流沉积特征及其地质意义   总被引：2，自引：0，他引：2  

李云  郑荣才  朱国金  胡晓庆 《海洋学报》2012,34(1):127-135

研究深水牵引流对古大洋环流重建、陆坡位置判断及沉积矿产和能源资源勘探具有重要意义。珠江口盆地白云凹陷中新统珠江组取心段发育丰富的、与远洋低密度浊流和半远洋-远洋悬移沉积有明显区别的深水牵引流沉积,产物包括平行层理细砂岩、双泥岩纹层、双向交错层粉-细粒砂岩、波状层理和脉状层理灰质粉-细粒砂岩、波状层理和脉状层理抱球虫灰岩、透镜状沙纹层理粉砂岩等岩石相类型。珠江组深水牵引流沉积的发现具有重要地质意义,由其可以推测自渐新世末(23.8 Ma)白云凹陷陆架坡折带形成之后就开始存在沿着陆架坡折带活动的深水牵引流,并可能影响和改变沉积物的物质组成和区域分布,这将为南海北部古大洋洋流循环重建起到重要启示作用。  相似文献   

水温变动对2009年西北太平洋柔鱼产量下降的影响   总被引：1，自引：0，他引：1  

陈峰  陈新军  钱卫国  刘必林  田思泉 《广东海洋大学学报》2010,30(1):65-71

分布在西北太平洋的柔鱼是我国远洋鱿钓渔业的重要捕捞对象,近些年来其产量一直处在稳定的水平。然而,2009年8～10月旺汛期间在传统作业渔场(150°E～165°E、38°E～46°E)柔鱼产量出现大幅度下降,其日产量仅为正常年份的一半。为此,根据2007～2009年8～10月我国在西北太平洋鱿钓生产数据,以及产卵场表层水温,探讨2009年柔鱼产量下降及渔场变动的原因。研究表明,其产量出现下降的原因可能有2个:(1)柔鱼产卵场(20°N～30°N,130°E～170°E)黑潮大弯曲的发生,使得21℃等温线向南偏移,使得柔鱼资源补充量受到影响,从而使得渔汛期间柔鱼产量的下降;(2)旺汛期间(8～9月)传统作业渔场(42°N～46°N,150°E～165°E)的100m水层有一个明显冷水南下,分布位置为154°E～156°E,将传统作业渔场(150E～165°E)一分为二,向南的前锋(水温低于5℃)到达42°N,明显不同于正常年份,使得作业渔场的范围明显缩小,不适合柔鱼的集群,导致产量出现大幅下降。  相似文献   

Age estimation, growth, maturity, and distribution of the bluemouth rockfish Helicolenus d. dactylopterus (Delaroche 1809) from the Rockall Trough     

Kelly  C. J.; Connolly  P. L.; Bracken  J. J. 《ICES Journal of Marine Science》1999,56(1):61-74

  相似文献   

Numerical simulation of tidal current and erosion and sedimentation in the Yangshan deep-water harbor of Shanghai   总被引：2，自引：1，他引：1  

ZUO Shu-Hua  ZHANG Ning-Chuan  LI Bei  ZHANG Zheng  ZHU Zhi-Xia Ph.D c  idate  State Key Laboratory of Coastal  Offshore Engineering  Dalian University of Technology  Dalian  China  Key Laboratory of Engineering Sediment of Ministry of Communications  Tianjin Research Institute of Water Transport Engineering  Tianjin  China. Dr.  Prof.  China Research Scientist  Key Labor... 《国际泥沙研究》2009,24(3):287-298

Yangshan near-shore sea area is the multi-island and multi-channel area with strong flow velocity and high suspended sediment concentration. Based on the characteristics of tidal currents, waves, and sediment in the Yangshan area, a two-dimensional numerical model of tidal currents, sediment transport, and sea bed deformation is developed. In the model, the effects of tidal currents and wind waves on sediment transport are considered. According to characteristics of the study area, unstructured grids are applied to fit the boundaries of the near-shore sea area. The results show that the calculated values are in good agreement with the measured data. The field of tidal currents, suspended sediment concentrations, and the deformation of the seabed can be successfully simulated.  相似文献   

Diversity history of Ordovician graptolites and its relationship with environmental change     

Zhang YuanDong  Chen Xu 《中国科学D辑(英文版)》2008,51(2):161-171

Statistical analysis based on global data indicated that the planktonic graptolites presented a distinguished pattern from that of benthic communities during the great Ordovician biodiversification. The graptolites started to diversify from the beginning of Ordovician and reached an acme in the early Middle Ordovician, but subsequently underwent a steady decline to the end of Ordovician. During the Ordovician, many clades of the graptolites made their originations, flourishing and replacements. However, in different regions and distinct environments across the world, graptolites may presumably display distinct patterns of radiation and evolution, a hypothesis to be tested. Herein a study of the graptolite diversity in the Early to Middle Ordovician in the Upper Yangtze Region (Platform) and Jiangnan Region (Slope), South China, is conducted. The results indicate that graptolites underwent a remarkable increase in both regions, but with distinct magnitude, scope, process and patterns. The diversification of graptolites in the Upper Yangtze Region, though less prominent, is divided into four stages and includes two peaks. In the Jiangnan Region, the graptolite diversification is far more prominent and includes three stages and one peak. Based on the distinct diversity histories and composition of graptolites in the two representative regions, a 'deep-water origin and shallow-water dispersal' model is proposed for the Ordovician graptolite faunas. According to the model, the major graptolite faunas of Ordovician originated in the deep-water region on the continental slope, the source of the graptolite novelties, and subsequently spread into shallow-water region on the shelf. Besides, we also conduct a comparison study of the Ordovician graptolite diversity in South China and other major regions. The results display that the graptolites diversified globally in the Early and Middle Ordovician. At the beginning of Ordovician, graptolites underwent a significant ecological innovation of graptolites: planktonic forms were derived from their benthic ancestors. This derivation resulted in the great guild expansion of graptolites. In late Early Ordovician (Floian), the global expansion of graptolites commenced. From the Floian to the end of Middle Ordovician, the graptolites diversity increased remarkably and displayed three peaks for all the regions. However, the peaks are somewhat distinct in magnitude and timing among regions. The Darriwilian peak is prominent in both South China and Baltic region, but inconspicuous in Australasia. No close relationship between the graptolite diversification and the palaeolatitudes are supported herein. Instead, the graptolite diversification seems to coincide with the global sea-level rises, suggesting a possible intrinsic relationship between them.  相似文献   

塔里木盆地东北部中上奥陶统却尔却克群深水碳酸盐岩及白云岩化^*   总被引：1，自引：0，他引：1       下载免费PDF全文

钱一雄  张克银  陈跃  陈强路  田蜜  尤东华  罗宇 《古地理学报》2016,18(1):21-38

塔里木盆地东北部库鲁克塔格中上奥陶统却尔却克群中的深水碳酸盐岩及其白云岩化是较为特殊的沉积与成岩作用类型之一。通过对南雅尔当山剖面详细观察与采样分析,阐明了其沉积学、岩石学及地球化学特征:深水碳酸盐岩的顶、底均与浊积岩伴生,呈重力滑覆-带状分布,主要由黄灰色-灰色、大多呈薄层瘤状的白云岩夹泥页岩构成;可见到海绵骨针、三叶虫等浮游生物化石以及分选差的花岗岩、火山岩及硅质岩等碎屑;基本保留了原始沉积中的溶解、水平层理等较深水沉积的特征。该套白云岩包括泥粉晶白云岩、细晶白云岩或残余陆屑白云岩、巨型藻鲕白云岩和生屑泥粉晶白云岩等9类白云岩;白云石有序度为0.47~0.56和0.70~0.76,中强阴极发光,经历了2期较强的白云岩化作用;富含SiO₂、Al₂O₃、Mg、Mn、Fe、MnO和TiO₂;δ³⁴S_V-CDT为-0.2~6.6,ΣREE含量为46.7×10^-6~67.4×10^-6,呈正铕负铈的“帽式”稀土配分模式,反映相对还原沉积环境;反映沉积水体盐度的Na₂O+K₂O、Sr、Ba含量偏低, ⁸⁷Sr/⁸⁶Sr 值相对偏高,δ¹⁸O_PDB 、δ¹³C_PDB稍低,不能指示原始海水或原始环境。综合上述分析结果认为:这套深水碳酸盐岩形成于向上变浅的缓坡带,其发生了浅埋藏、中-深埋藏条件下的2期白云岩化,且受构造推覆或重力滑覆至外陆棚,并发生裂隙-溶蚀作用和白云石、方解石及烃类的充填作用。  相似文献   

南海北部白云凹陷深水区SQ13.8深水扇砂体识别与分布研究：以SF-5为例     

徐少华  徐国强  杨俊华  李小刚  胡琏  蔡长娥  郭伟 《现代地质》2013,27(2):366-372

珠江口盆地白云凹陷在继“白云运动”之后,在13.8 Ma发生了一次大规模的海退事件,海平面下降至陆架坡折带附近,三角洲向盆地方向推进最远,十分有利于深水扇的发育。通过深水陆坡区B6井及陆架边缘多口井的井震标定,结合钻井、测井分析,系统总结出具有厚度较大（20~40 m）、以泥质粉砂岩为主的斜坡扇储层,对应低频、短轴、强振幅的地震反射特征,在负极性显示的地震剖面上,表现为强波谷地震响应。层序地层格架分析认为工区处于SQ13.8“陆架边缘三角洲—沉积过路区—斜坡扇”的沉积环境,并在层序格架的约束下,通过合成地震记录建立井-震关系,对斜坡扇区第5套砂层组（SF-5）进行储层识别与追踪解释,确定SF-5砂层为主体分布在陆架坡折带外侧陆坡区的丘状体,平面形态似帚状或朵叶状,具有斜坡扇的特征,其优质储层主要分布在工区的中部-西部地区,呈NW-SE方向条带状展布。  相似文献