冷原子荧光法测定近海沉积物中汞含量的不确定度探讨   总被引：1，自引：0，他引：1  

任松 《海洋科学》2004,28(11):6-9

采用直观的因果图,分析冷原子荧光法测定近海沉积物中汞含量的不确定度影响因素。建立有效的数学模型,对测试过程中不确定度的各个分量进行了分步计算及整体合成,并对评定结果进行了讨论。结果表明,校准曲线、测量标准及仪器性能是冷原子荧光法测定近海沉积物中汞含量不确定度的主要影响因素.  相似文献   

2000年8月南海中部与南部海洋温、盐与环流特征   总被引：13，自引：2，他引：11  

王东晓  陈举  陈荣裕  朱伯承  郭小刚  许金电  吴日升 《海洋与湖沼》2004,35(2):97-109

根据2000年8—9月份南海中部与南部航次的温、盐资料,采用P—矢量诊断方法,结合ADCP测流资料和同期伪风应力资料以及TOPEX／Poseidon高度计资料,研究了2000年夏季风持续强迫之后南海大尺度环流与中尺度涡旋的空间结构。结果表明,南海夏季温度和盐度水平分布随深度有显著的变化：中层(250—400m左右)温、盐水平分布与其它各层的温度和盐度分布相比有很大的差异。用诊断方法计算得到的环流场与用TOPEX／Poseidon海面高度计资料计算得到的地转流场比较一致,即流场内部有多个中尺度的涡旋,主要有越南东南外海反气旋涡、中沙群岛东南反气旋涡以及南沙群岛东北角的气旋涡等,这说明南海中部与南部盛夏环流具有较强的地转分量和显著的多涡结构,并且这些中尺度涡在垂向上存在速度场的切变。  相似文献   

集成于海上风电钢管桩基础上的升降式网箱结构波浪场特性研究     

田正林  毛鸿飞  吴光林  赫岩莉  林金波 《海洋工程》2023,41(6):76-86

对安装在海上风电钢管桩基础上的升降式网箱结构的波浪场特性进行研究,掌握升降式网箱结构内部及结构后方水体的运动特征及速度场变化情况。基于OpenFOAM软件包开发了波、流与孔隙介质结构相互作用的数值计算模型,将网箱结构按等效阻力简化为多孔介质结构,开展升降式网箱结构的波浪场特性研究。研究结果表明：网箱结构对流体具有一定的阻流作用,网箱结构内部速度场得到一定程度的减小,网箱结构背浪侧也有一定的速度衰减区域;对比网箱结构顶部不同潜深条件下的网箱结构内部流场特征,网箱结构顶部潜深在1/4D~1/2D（D为水深）范围内网箱结构内部流场速度最小、流场最为稳定、速度分布均匀,网箱结构向浪侧前方和背浪侧后方流场波动较小。所得结论表明在钢管桩基础上安装升降式网箱结构时需要关注的网箱结构对流场特性的影响,充分考虑网箱结构阻力对流速的作用,掌握极端工况下升降式网箱结构保持优良养殖环境需要下潜的高度范围,以保障升降式网箱的安全。  相似文献   

海洋碱性矿物增汇技术发展方向研究          下载免费PDF全文

郭雪飞  张敏吉  周微  任宏伟  郑力文  苏贝  胡玉斌  刘纪化 《海洋开发与管理》2023,40(9):30-36

工业革命以来,近1/3人为排放的二氧化碳被海洋吸收,海洋负排放潜力巨大。海洋碱化技术被认为是最具有固碳潜力的海洋负排放技术之一。硅酸盐碱性矿物橄榄石风化速率高,在自然界中具有广泛的分布。海水增汇效率受到橄榄石的溶解速率、扩散速率等因素的影响。基于近海橄榄石海上反应平台,利用清洁能源将橄榄石破碎、研磨加速其溶解,再由海流将高碱度海水进行扩散促进毗邻海域对大气二氧化碳吸收的方法具有广阔的应用前景。随着我国近海油气资源的开发,基于海上油气平台发展橄榄石碱化增汇技术,降低海上碱化反应平台基建成本的同时,可捕集油气生产过程中的二氧化碳,随碱化后海水入海,进一步提高碱性矿物增汇技术的碳封存效能。  相似文献   

海上浮式风机气动性能数值模拟   总被引：1，自引：0，他引：1  

吴俊  丁金鸿  何炎平  赵永生  刘亚东 《海洋工程》2016,34(3):38-46

采用计算流体动力学(CFD)方法,基于RANS方程和SST k-ω湍流模型,对OC3-Hywind Spar浮式平台支撑的NREL5 MW风机进行气动性能模拟。对固定式风机的数值模型做网格无关性验证,同时考虑垂直风切变的影响,并将数值结果与NREL设计数据进行对比以验证模型的有效性。在FLUENT软件中,设定嵌入式滑移网格和用户定义程序(UDF)来模拟风机叶轮随平台的周期运动,分别研究浮式平台的纵荡、纵摇和首摇运动对风机气动荷载的影响。数值结果表明平台的纵荡和纵摇运动对输出功率影响较大,且平台运动幅值越大周期越低,其气动荷载变化越剧烈。合理控制平台的运动幅值对提高浮式风机的发电性能和疲劳强度有很大作用。  相似文献   

半主动TLCD对固定式海洋平台的离散神经网络滑模控制   总被引：3，自引：0，他引：3  

金峤  周晶  李昕 《世界地震工程》2005,21(3):28-34

主要研究了半主动调液柱型阻尼器（TLCD）对固定式海洋平台的离散神经网络滑模变结构控制方法。首先建立了平台结构-TLCD控制系统微分方程及其离散化状态空间表达,然后阐述了基于神经网络的滑模变结构控制的基本算法和控制策略,最后应用该神经网络滑模变结构控制策略对一个已建成的实际海洋平台结构的TLCD半主动控制问题进行了数值仿真分析。仿真分析的结果证明了该方法的有效性。  相似文献   

New coring study in Augusta Bay expands understanding of offshore tsunami deposits (Eastern Sicily,Italy)     

Alessandra Smedile  Flavia Molisso  Catherine Chagué  Marina Iorio  Paolo Marco De Martini  Stefania Pinzi  Philip E. F. Collins  Leonardo Sagnotti  Daniela Pantosti 《Sedimentology》2020,67(3):1553-1576

Tsunami deposits present an important archive for understanding tsunami histories and dynamics. Most research in this field has focused on onshore preserved remains, while the offshore deposits have received less attention. In 2009, during a coring campaign with the Italian Navy Magnaghi, four 1 m long gravity cores (MG cores) were sampled from the northern part of Augusta Bay, along a transect in 60 to 110 m water depth. These cores were taken in the same area where a core (MS06) was collected in 2007 about 2·3 km offshore Augusta at a water depth of 72 m below sea level. Core MS06 consisted of a 6·7 m long sequence that included 12 anomalous intervals interpreted as the primary effect of tsunami backwash waves in the last 4500 years. In this study, tsunami deposits were identified, based on sedimentology and displaced benthic foraminifera (as for core MS06) reinforced by X-ray fluorescence data. Two erosional surfaces (L1 and L2) were recognized coupled with grain-size increase, abundant Posidonia oceanica seagrass remains and a significant amount of Nubecularia lucifuga, an epiphytic sessile benthic foraminifera considered to be transported from the inner shelf. The occurrence of Ti/Ca and Ti/Sr increments, coinciding with peaks in organic matter (Mo incoherent/coherent) suggests terrestrial run-off coupled with an input of organic matter. The L1 and L2 horizons were attributed to two distinct historical tsunamis (ad 1542 and ad 1693) by indirect age-estimation methods using ²¹⁰Pb profiles and the comparison of Volume Magnetic Susceptibility data between MG cores and MS06 cores. One most recent bioturbated horizon (Bh), despite not matching the above listed interpretative features, recorded an important palaeoenvironmental change that may correspond to the ad 1908 tsunami. These findings reinforce the value of offshore sediment records as an underutilized resource for the identification of past tsunamis.  相似文献   

海上风电单桩基础土相互作用特性影响因素分析     

孔德森  刘一  邓美旭  侯迪 《海洋工程》2021,39(1):100-111

采用有限元软件ABAQUS建立了海上风电单桩基础与土相互作用数值计算模型,将波浪、洋流及风荷载等效成双向对称循环荷载,研究了水平循环荷载作用下不同因素对桩身水平位移、剪力和弯矩的影响规律。研究表明,随着循环荷载比的增加,桩身位移零点和桩身剪力反弯点沿埋深逐渐下移,桩身弯矩最大值点位于浅层土体;不同荷载频率时桩身位移在零点以上变化较大,桩身弯矩随着频率的增加逐渐增大;单向循环荷载作用下桩身位移最大,双向对称循环荷载作用下桩身位移最小;壁厚较小时对桩身水平位移影响较大;在位移零点之上范围内可以考虑设计"上厚下薄"的钢管桩,以减小桩身水平位移;不同桩壁厚时桩身剪力曲线在埋深约6D处出现交点,且泥面处桩身弯矩变化不明显。  相似文献   

一种基于状态空间模型的浮式海上升压站平台动力响应计算方法研究     

汤群益  孙震洲  陈杰峰  金磊 《海洋工程》2021,39(2):144-152

浮式海上升压站的动力响应分析是其设计阶段的重要内容,对浮式升压站进行结构优化进而改进其水动力性能意义重大。提出一种基于状态空间模型的浮式海上升压站平台动力响应算法,该方法通过频域拟合的方法计算延迟函数频响函数有理分式的系数,得到延迟函数的极值和留数,进而构建延迟函数的状态空间模型,通过状态空间模型代替Cummins方程中的卷积项,从而计算浮式海上升压站的动力响应。采用日本福岛示范项目的浮式升压站模型对方法进行验证,结果表明计算得到的动力响应与商业软件SESAM计算结果吻合较好,说明方法的有效性。  相似文献   

Existence,morphology and structure of the Yellow Sea Warm Current Branch approaching waters offshore Qingdao,China   总被引：1，自引：0，他引：1  

Xuejun XIONG  Xiaomin HU  Yanliang GUO  Long YU  Liang CHEN  Yuhuan XUE 《中国科学:地球科学(英文版)》2019,(7):1167-1180

In this study, we focused on full-region cruise survey data, near-bottom continuous mooring observations and sea surface wind products from the western South Yellow Sea in winter; after ensuring the data reliability and accuracy, we processed and analyzed the data. Image resolution experiments were carried out to determine the lowest recognition resolutions for all image types, which represent the resolution characteristics of the data. The existence of a warm water tongue originating from the Yellow Sea Warm Current(YSWC) that approached waters offshore Qingdao was confirmed. For the first time, a high salinity water tongue, corresponding to the warm water tongue, was described and found to be more representative of the YSWC branch path. This warm tongue is a sign of the branch originating from the YSWC, which we defined as the Yellow Sea Warm Current Branch approaching waters offshore Qingdao(YSWC-QDB). The pattern of the warm and salty water tongues showed remarkable rear, branching middle, shrinking neck and expanding top regions. These patterns showed a temporal feature of the tongues, and were the result of multi-temporal branches in front of the YSWC main section as well as the YSWC-QDB crossing the southwestward path of the extension of the North Shandong Coastal Current flowing along the southeast coast of the Shandong Peninsula(NSCC-SESE). Analysis using mooring data at a sensitive and representative station also showed the existence of the YSWC-QDB. It is a probabilistic event that manifests as a northwestward flow that decreases gradually from the bottom to the surface in the early cold air transit stage and consistent in the whole water column profile in the later stage. It varies quasi-periodically with weather processes. It also transports some of the YSWC water stored in the entrance area of the Bohai and Yellow seas under winter wind conditions to the western South Yellow Sea as a compensatory current. This current, caused by northerly winds, especially northwest winds and obstruction of the NSCC-SESE, was present, and strong water reduction and compensation caused significant residual sea level oscillations. The compensatory current, if caused by strong northwest wind,began to appear when its direction was opposite to the wind direction. In addition, confirmation of the YSWC-QDB provides an oceanographic basis for the short cooling time and rapid warming in the Qingdao area in winter. This research provides a basis for further studies of the YSWC-QDB at high spatial and temporal resolutions using large sea surface datasets. For monsoon basin dynamics, this study can also be extended to the whole Bohai and Yellow seas and closed or semi-closed basins on the continental margin.  相似文献