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701.
Cable-membrane structures have small rigidity and are highly sensitive to wind. Structural health monitoring is necessary to ensure the serviceability and safety of the structure. In this research, the design method of a structural health monitoring system is using the characteristics of a cable-membrane structure. Taking the Yueyang Sanhe Airport Terminal as an example, a finite element model is established to determine the critical structural components. Next, the engineering requirements and the framework of the monitoring system are studied based on the results of numerical analysis. The specific implementation of the structural health monitoring is then carried out, which includes sensor selection, installation and wiring. The proposed framework is successfully applied to the monitoring system for the Yueyang Airport terminal building, and the synchronous acquisition of fiber Bragg grating and acceleration sensor signals is implemented in an innovative way. The successful implementation and operation of structural health monitoring will help to guarantee the safety of the cablemembrane structure during its service life.  相似文献   
702.
According to the actual observation conditions of the Yangtze River valley from Anqing city to Maanshan city, we designed the 3D acquisition geometry, and applied the multi-scale checkerboard semblance analysis to assess the preliminary resolution of the designed observation. The checkerboard semblance tests use the refraction and reflection travel-time simultaneous inversion algorithm to quantitatively provide both resolution assessment of velocity structure and Moho topography. The multi-scale checkerboard semblance recovery results show that while the checkerboard semblance threshold value is 0.5, the preliminary resolution of the designed acquisition geometry is better than 10 km in the upper crust (the depth is less than 10 km), around 15 km in the mid-crust (the depth is 10?25 km), and better than 20 km in the lower crust (the depth is 25?33 km). The preliminary tomographic resolution for the Moho topography is about 20 km in the ray-path coverage area beneath the acquisition geometry. While the checkerboard semblance threshold value is 0.75, the preliminary resolution is 20 km in the upper crust, around 20?25 km in the mid-crust and 25 km in the lower crust. And the preliminary tomographic resolution for the Moho topography is better than 30 km in the ray-path coverage area beneath the acquisition geometry. These non-linear checkerboard tests reveal that the designed acquisition geometry is suitable to image the crustal velocity structure of the Yangtze River valley in the Anhui province.  相似文献   
703.
本文应用三维柱坐标时域有限差分方法模拟了多极子随钻声波测井的波场,提出了在横向各向同性(TI)慢速地层倾斜井中,使用四极源激发、多模式采集进行各向异性参数反演的方法.模拟结果表明:在强各向异性地层大角度倾斜井中使用四极源能够激发出多极模式波,并且井孔内的声场会随着声源方向角β(声源方向和快横波偏振方向的夹角)的改变而发生变化.使用四极子采集方式记录时,可以发现波形会分裂成快慢两种波;并且在声源方向与地层快横波偏振方向成45°时,分裂的两种波形的速度更趋近于地层快慢横波波速,用此可反演地层各向异性值大小.使用单极子采集方式记录时,其波形能量与声源方向角β大致成cos22β的关系,在声源方向角为45°时,其波形幅度最小,用此可判断与快横波偏振方向成45°角的方向.使用AC方向(与声源同方向)偶极子采集方式记录时,当声源方向与快横波偏振方向一致时,采集到的波形幅度最小;而与快横波偏振方向垂直时,波形幅度最大,所以通过偶极子采集方式记录的波形可以判断快横波偏振方向.因此,在强各向异性倾斜井中进行随钻四极子测量时,可以使用多模式采集方式来进行地层各向异性的反演.  相似文献   
704.
Distributed acoustic sensing uses an optical fibre together with an interrogator unit to perform strain measurements. The usage of distributed acoustic sensing in geophysics is attractive due to its dense spatial sampling and low operation cost if the optical fibre is freely accessible. In the borehole environment, optical fibres for distributed acoustic sensing are often readily available as a part of other sensing tools, such as for temperature and pressure. Although the distributed acoustic sensing system promises great potential for reservoir monitoring and surface seismic acquisition, the single axial strain measurement of distributed acoustic sensing along the fibre is inadequate to fully characterise the different wave modes, thus making reservoir characterisation challenging. We propose an acquisition system using five equally spaced helical optical fibres and a straight optical fibre to obtain six different strain projections. This system allows us to reconstruct all components of the 3D strain tensor at any location along the fibre. Analysing the condition number associated with the geometry of the optical fibre, we can systematically search for the optimum design parameters for our configuration. Numerical examples demonstrate the effectiveness of our proposed method to successful reconstruction of the full strain tensor from elastic wavefields of arbitrary complexity.  相似文献   
705.
Since its introduction in the late 1950s, hydraulic vibrators have become the dominant source for land seismic surveys. The hydraulic vibrators typically used for commercial land seismic acquisition, however, are large, costly to operate and expensive to purchase. This inhibits their use for small-scale and short-duration surveys as well as Vibroseis research. In this paper we describe, in detail, the construction of a portable vibrator from commercially available components for a cost of less than $US2,000. Data shows that the vibrator is able to successfully transmit sweeps from 15 to 180 Hz with different spectral contents. The vibrator produces a stronger signal than a sledgehammer and we estimate its output to be around 1 kN. The frequency content of the data was concentrated at lower frequencies (<100 Hz) and the ground-roll was far more energetic than that produced using a sledgehammer.  相似文献   
706.
Geophysical surveying of the Arctic will become increasingly important in future prospecting and monitoring of the terrestrial and adjacent areas in this hemisphere. Seismic data acquired on floating ice are hampered with extensive noise due to ice vibrations related to highly dispersive ice flexural waves generated by the seismic source. Several experiments have been conducted on floating ice in van Mijenfjorden in Svalbard in the Norwegian Arctic to specifically analyse the extent of flexural waves recorded with various seismic receivers and sources deployed both on top of ice and in the water below. The data show that flexural waves are severely damped at 5 m or deeper below the ice and hydrophone data suffer less from these vibrations compared with data recorded on the ice. Aliasing of single receiver hydrophone data can to some extent be suppressed using an in-line line source of detonating cord. Experiments on ice on shallow water show prominent guided wave modes often referred to as Scholte waves propagating along the seabed. In this case, both flexural and Scholte waves interfere and make a complicated pattern of coherent noise. On shallow water, the positioning and type of the seismic source must be evaluated with respect to the coherent noise generated by these waves. Geophone strings of 25 m effectively suppress both flexural and Scholte waves due to their relative short wavelengths. An airgun generates relative more low-frequency energy than a surface source of detonating cord. Accordingly, seismic mapping of deep seismic horizons seem to be best achieved using geophone strings of such length and an airgun source. For shallow targets, the use of hydrophones in combination with detonating cord is an appropriate solution. Seismic surveying in the Arctic always have to follow environmental restrictions of not disturbing or harming wildlife and not causing permanent footprints into the vulnerable tundra, which implies that the choice of seismic acquisition strategy might occur as a trade-off between optimum data quality and environmental constraints.  相似文献   
707.
刘勇  庹先国  李怀良  沈统  陆景 《地球物理学报》2017,60(11):4302-4312
随着多波多分量技术的发展,宽频数据采集逐渐成为地震勘探的发展趋势.通过高保真获取全波场信息,并尽可能保留高频有效成分,进而利用多种波场信息相互验证和补充,是提高地震勘探精度的有效方法.受仪器带宽限制,常规设备在高频段很难同时保持高分辨率和大动态范围特征,在多波地震采集时,极容易出现分辨率不足和限幅失真等现象,极大影响多波多分量方法的实际应用效果.鉴于此,本文给出一种利用积分器、高频ADC、DAC和抽取滤波器构成的低成本宽频数据采集方法.通过构造环路滤波器(调制器),对高频ADC输出数据中的量化噪声二次整形,并配合抽取滤波,对带外噪声进行有效压制.实际测试表明,通过精细电路结构设计,采集站有效分辨率可达24位(采样率为2 kHz),动态范围超过140 dB,SNR达142 dB.相比传统设备,其采集数据在5~25 Hz的低频段和100 Hz以上的高频段都具有更加丰富的有效信息,非常适合多波多分量数据采集.  相似文献   
708.
基于WSN的分布式节点地震仪分层通信网络   总被引:1,自引:1,他引:0       下载免费PDF全文
针对深部探测对节点地震仪器提出的质量监控和数据现场回收要求,本文设计了基于WSN的三维地震勘探分层通信网络.分层网络由骨干网和多跳网两个网络层构成:骨干网使用LTE技术与监控中心进行数据交换,并实现了链路带宽的合理分配与大范围的信号覆盖;多跳网结合地震勘探的特点,使用私有路由协议和数据传输协议完成了仪器的组网与数据的接力式传输.测试结果验证了组网协议的设计正确性与数据传输的稳定性,且网络总体性能满足实际应用的需求.数据多跳传输实现了无线局域网技术的远程访问,从而提高了勘探作业效率.  相似文献   
709.
针对可控震源高频拓展,一些使用者只是简单提高高频截止频率,出现了较多问题,如在沙漠、草场等疏松地表区域会出现高频畸变,严重影响了资料品质.为此,从高频段畸变现象入手,建立可控震源与地表振动模型,深入研究了震源振动输出力信号.分析表明高频段重锤与平板加速度之间产生较大相位差,造成可控震源系统过载是产生高频畸变的原因,并进一步提出了高频优化能量补偿扫描技术的方法改善高频畸变,通过试验对比说明了该方法能够提高高频输出信号的稳定性,降低高频畸变,也为以后解决类似问题提供帮助.  相似文献   
710.
范文龙  黄小仙  傅雨田 《遥感学报》2022,26(8):1589-1601
对海温分布与变化的探测是海洋一号卫星主载荷水色水温扫描仪(简称水色仪,COCTS)的主要任务之一。考虑到对海冰和海洋上空台风等气象要素的同时探测,实际水温探测通道的动态范围要求涵盖200—320 K的温度区间。由于某些洋面区域微弱温度的变化将会导致严重天气灾害的发生,因此海温探测通道还需满足探测灵敏度与定量化的精度要求。本文旨在依据技术指标要求,设计水色仪红外通道的信息获取电路,包括对探测器微弱信号进行放大的前置放大电路,消除基础电平以提高动态范围的交流放大器,以及实现信号的直流恢复与动态范围调整的通道放大电路。基于对所使用的光导型红外探测器工作机理的研究,结合水色仪的系统组成与特性,为确保同时满足高动态范围与高灵敏度这一对相互矛盾的指标要求,通过理论分析计算、电路仿真等方法,确定各级放大电路的形式及参数。在真空环境模拟实验室对水色仪的系统性能进行测定,以验证信息获取电路设计的合理性。在实验室进行的红外辐射定标结果表明和在轨测试结果均表明,水色仪两个红外通道的动态范围和噪声等效温差(NETD)均能较好的满足技术指标要求。红外通道能够实时跟踪星上黑体信号随时间与周围环境的变化,可据此来对红外通道的定标系数进行即时修正,从而达到预期的在轨实时辐射定标的目的,为定量化反演海温奠定了基础,并能获取且制作出高质量的全球海温产品。  相似文献   
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