共查询到20条相似文献，搜索用时 159 毫秒
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为满足深拖式高分辨多道地震勘探需求,设计并实现了海洋地震拖缆数据的实时传输系统。系统由数传包与地震采集站连接组成,采用推荐标准485(Recommended Standards 485,RS485)串行总线实现了采集站与数传包的物理连接,利用低电压差分信号(Low-Voltage Differential Signaling,LVDS)、预加重/均衡器、8位/10位(8 bit/10 bit)编码等技术实现了数传包之间的通信链路。设计了无等待反馈重传的差错控制方法,提高系统高效性和可靠性;在现场可编程门阵列(Field Programmable Gate Array,FPGA)内部采用先进先出(First Input First Output,FIFO)构建多优先级任务队列的多级流水线设计,解决了大容量数据并发而产生的数据漏帧问题。在实验室用已知正弦信号对系统进行了对比测试,结果表明系统能够满足海洋多道地震勘探的数据传输需求,对于海洋多道高分辨率地震资料的可靠获取具有重要的意义。 相似文献
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对运用小排列高分辨多道地震系统获取的岱山岛大桥附近海域高精度的地震数据进行了综合分析和处理,查明了调查区域的工程地质条件,并对两个桥址方案进行了地质条件的对比。采用的地震系统参数:拖缆为24道,道间距为2 m,偏移距为46 m,枪容积为10 in3,频带范围为1~1 000Hz。结果表明:(1)采用了统一方法和流程对岱山岛大桥工程中所获得的地震数据进行分析、处理,保证了两种选址方案调查结果的一致性。(2)舟山本岛-岱西桥位(方案Ⅰ)和舟山本岛-双合山桥位(方案Ⅱ)海底地形平缓,不存在海底滑坡体等不良地质现象,调查区域虽分别有6条和5条断裂,但所有断层的上覆第四系均未发生错断,断裂均为非活动性断裂,两个方案桥位线均具有建桥的良好工程地质条件。(3)与单道地震相比,小排列高分辨多道地震系统能得到更为丰富的地层反射地震数据,而该系统比传统的多道反射地震方法具有作业方便、经济的优势,可见,该调查方法适用于近岸区域浅水工程环境的地质调查工作,是一种方便、实用和经济的地质调查手段。 相似文献
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为了检验光纤水听器阵列在海洋地震勘探中应用的性能, 在南海, 使用1024基元的光纤水听器阵列与进口的360道压电水听器海洋地震勘探仪, 采用相同的作业方式在同一位置进行海洋地震勘探调查, 对两个设备采集的海洋地震勘探资料进行对比。试验结果表明, 光纤水听器阵列采集的数据主频范围达到10~120Hz, 宽于压电水听器海洋地震勘探仪的主频范围10~80Hz; 地震剖面分辨率优于压电水听器海洋地震勘探仪。光纤水听器阵列在经过适应性改进后完全能够满足海洋地震勘探的性能要求。 相似文献
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海洋拖缆主动源多道地震技术是应用于海洋天然气水合物资源调查的主要技术方法。不同于常规油气藏勘探,海底天然气水合物成藏机制复杂多样,海底似反射(Bottom Simulating Reflector,BSR)特征与水合物赋存并非完全对应。为提高海洋天然气水合物矿体识别的可靠性,地震属性技术在水合物资源调查中发挥着越来越重要的作用。本文对我国南海北部海域天然气水合物调查中的关键属性进行了对比、分析及筛选试验研究。试验针对海洋高分辨多道三维地震数据,采用三维地震层速度控制综合处理技术完成了BSR区域的成像,提取了与BSR相关的多种地震属性,并对BSR地震属性体的内部特性进行了分析,实现了BSR特征水合物矿体的识别,并提取了BSR上方和下部结合层带的地震属性。研究结果表明,在水合物赋存地层极其复杂的条件下,地震属性分析技术在海洋复杂浅地层水合物识别方面具有可行性和技术优势。 相似文献
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拖缆式浅地层剖面采集系统改进方法 总被引：1，自引：0，他引：1
传统拖缆式浅地层剖面地震资料采集系统中往往采用检波点组合的方式进行资料采集,当海水深度较深时,可以忽略组内距对地震资料的影响,当海水深度较浅时,这种采集方式容易导致波形畸变和高频信息丢失。利用多道地震的思想,对传统拖缆式浅地层剖面采集系统进行改进。新的浅地层剖面采集系统采用拖缆式施工、多道、无组合单点接收方式进行采集,即可以获得各检波点采集到的数据,同时改进数据记录的方式。新的采集系统中可以同时监控原始单炮记录、直接叠加后单道记录、时差校正后叠加单道记录、时差校正后地震剖面。 相似文献
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拖缆采集的海上多道地震数据受海水间传播的多次波影响,往往在共炮点道集上发育周期性的强振幅干扰波,这些噪音会掩盖海底以下及强反射层以下地层的面貌,严重影响多道地震数据的成像效果。为了消除海上多道地震数据中存在的海水间传播的多次波对地震数据的干扰,首先分析浅水多次波在海水间多次震荡的产生机制,采用了τ-P域静校正延迟技术对其进行压制,处理的核心是在τ-P域对周期性多次波模型进行预测,再通过自适应相减以去除地震数据中的多次波。实际资料处理结果表明,方法对海水间震荡的浅水多次波具有很好的压制效果,经过浅水多次波去除后的叠加剖面信噪比得到有效提高,剖面的品质得以提升。 相似文献
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海洋多道地震数据建模和成像是获取洋壳速度和构造信息的重要手段。海水层的存在使得多道地震拖缆接收到的折射波走时信息仅仅存在于较远的炮检距, 近炮检距被强振幅海底反射波覆盖, 制约了走时数据拾取和反演效果。本文基于波动方程的Kirchhoff积分法, 成功实现了多道地震数据向下延拓, 获取到了更大炮检距区间的初至折射波走时拾取, 并将其应用于洋中脊新生洋壳2A/2B层的合成多道地震数据走时反演。比较向下延拓前后的走时拾取范围及走时反演结果表明, 向下延拓法能够保持地震波场的运动学和动力学特征不变, 在共炮集数据的更大炮检距范围内进行初至折射走时拾取, 从而增加反演的数据选择和浅层射线覆盖, 反演结果能更加准确地分辨出洋壳2A/2B层界面, 并得到更高的分辨率和更准确的速度结构剖面。 相似文献
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E. A. Ryzhov Yu. G. Izrailsky K. V. Koshel 《Izvestiya Atmospheric and Oceanic Physics》2014,50(4):420-425
The motion of a point vortex along a rectilinear boundary with a circle cavity, which models the coastline of a bay, and associated fluid particle advection are studied within a model of barotropic inviscid fluid. Using an analytical expression for the complex potential through which the velocity field is determined, we show that fluid particles start moving irregularly when the vortex is passing the cavity due to the nonstationarity of the velocity field generated by the vortex. Some of the fluid particles which were initially inside the vortex atmosphere leave it due to the irregularity and remain within the cavity vicinity. Depending on the initial position of the vortex and a parameter that determines the cavity size, the fraction of these fluid particles can differ significantly from fluid particles initially uniformly distributed within the vortex atmosphere. The escape of fluid particles from the vortex atmosphere is shown to be most efficient in the case of a relatively closed cavity under the condition that the initial vortex atmosphere area should be significantly smaller than the cavity area. 相似文献
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Shigehisa Nakamura 《Journal of Oceanography》1977,33(1):47-53
By a model bay with a mouth and a narrow, an experiment on long period waves is carried out to discuss the behavior of the tsunamis and storm surges. Emphasis is placed on the analysis of the characteristics of the current velocities associated with the long period waves incoming through the mouth in terms of Ursell's parameter. 相似文献
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This paper is concerned with the vibrations of a thin plate resting on a fluid-layer subjected to a moving point force. The frequency is assumed to be low and the fluid is deep. Both the fluid and the point force are always in contact with the plate. Hankel Transform and complex integration techniques are used to calculate the lateral displacements withrespect to a moving coordinate system and a coordinate transformation is used to achieve the results with respect to a fixed point. Numerical results are discussed with respect to the velocity of the moving force, its direction of movement and the fluid depth. 相似文献
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With an additional vertical duct at the wave-beaten side, an OWC is expected to give some much better performances. This is, essentially, due to two reasons. First, an OWC with the additional vertical duct (U-OWC) has an eigenperiod greater than the eigenperiod of a conventional OWC. Second, the amplitude of the pressure fluctuations on the opening of a U-OWC is greater than the amplitude of the pressure fluctuations on the opening of a conventional OWC (the greater the smaller the wave period is). For the first reason, a U-OWC can give performances better than those of a conventional OWC both with swells and large wind waves. For the second reason, a U-OWC can give performances better than those of a conventional OWC also with small wind waves. 相似文献
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A two-dimensional analytical solution is presented to study the reflection and transmission of linear water waves propagating past a submerged horizontal plate and through a vertical porous wall. The velocity potential in each fluid domain is formulated using three sets of orthogonal eigenfunctions and the unknown coefficients are determined from the matching conditions. Wave elevations and hydrodynamic forces acting on the porous wall are computed. Reflection and transmission coefficients are presented to examine the performance of the breakwater system. The present analytical solutions are found in fairly good agreement with the available laboratory data. The results indicate that the plate length, the porous-effect, the gap between plate and porous wall, and the submerged depth of the plate all show a significant influence on the reflected and transmitted wave fields. It is also interesting to note that the submerged plate plays an important role in reducing the transmitted wave height, especially for long incident waves. 相似文献
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Oceanology - Abstract—The nonlinear problem of run-up of a long wave on a plane beach in presence of a tide is solved within nonlinear shallow water theory using the Carrier–Greenspan... 相似文献
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Using a vertically two-dimensional, two-layer model, we have analytically examined the generation mechanism of a nonzero Eulerian
residual flow by strong tide-topography interaction in a narrow channel where the frictional effect is not included. In this
case, tidally generated baroclinic disturbances are forced non-uniformly in space and time while being advected by a strong tidal flow over the non-uniform slope of the bottom topography. Consequently, nonzero Eulerian residual flow results when averaged over one tidal period.
Although the time average of the velocity field is thus nonzero, the associated Eulerian residual transport in each layer
is compensated by a Stokes transport so that no Lagrangian residual transport results in both layers. This warns us that simple
time averaging of the velocity data obtained at a fixed mooring station might lead to a spurious material transport.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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曹天德 《海洋学报(英文版)》2010,29(11)
This paper deduces that the particular electronic structure of cuprate superconductors confines Cooper pairs to be first formed in the antinodal region which is far from the Fermi surface, and these pairs are incoherent and result in the pseudogap state. With the change of doping or temperature, some pairs are formed in the nodal region which locates the Fermi surface, and these pairs are coherent and lead to superconductivity. Thus the coexistence of the pseudogap and the superconducting gap is explained when the two kinds of gaps are not all on the Fermi surface. It also shows that the symmetry of the pseudogap and the superconducting gap are determined by the electronic structure, and non-s wave symmetry gap favours the high-temperature superconductivity. Why the high-temperature superconductivity occurs in the metal region near the Mott metal-insulator transition is also explained. 相似文献
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数据稀缺生态系统中多种类质量谱模型的构建 总被引：1，自引：0，他引：1
多种类生态模型已经被广泛应用于渔业活动影响应预测和管理措施效果评估。质量谱模型是一种基于生理过程构建的生态模型,该模型为描述鱼类群落在个体摄食变异和随个体发生的生态位迁移提供了一个可行的方法。尽管生态模型在增进生态系统认识上具有重要意义,其应用在数据稀缺的渔业中受到很大限制。作为实践基于生态系统渔业管理(EBFM)的第一步,本研究构建了海州湾鱼类群落的质量谱模型。本研究详述了数据收集和模型参数化的过程,以促进该模型在数据稀缺的生态系统中未来的应用。作为一个范例,研究展示了不同捕捞努力量对生态系统的影响,并采用一套生态指标监测其动态。群落生物量、多样性指数、W指数,大鱼指数(LFI),平均体重和群落质量谱斜率对捕捞压力的响应呈非线性,最大的捕捞强度并非总是对鱼类群落产生最强的影响。本文强调了构建谱模型在生态研究中的的价值和可行性,并讨论了模型的局限性和改进的可能。本研究旨在促进质量谱模型的广泛应用以更好地支持基于生态系统的渔业管理。 相似文献
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Experimental results of hydrofoil singing on a full-scale passenger ship are reported. It is proposed that hydrodynamic generation of a tone is caused by self-excited oscillation of a foil trailing edge. The natural frequency of the vibrating structure as well as the frequency of the external force are estimated. A lift-oscillator model is applied for modeling purposes. One effective method of eliminating the hydrofoil singing is discussed. 相似文献