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1.
原位测量技术在黄海沉积声学调查中的应用   总被引:8,自引:3,他引:8  
介绍了最新研制的基于液压驱动贯入的自容式海底沉积声学原位测量系统及其在南黄海中部海底沉积声学调查中的应用。该系统可以实现对海底沉积物声速和声衰减系数进行原位测量,通过液压驱动装置将四根声学探杆匀速贯入到海底沉积物中,减少了对沉积物的扰动,可按照预设的工作参数在海底全自动工作,无需甲板上人员实时控制,采集的声波信号自容式存储于存储单元。系统工作水深为500 m,测量深度为1 m,测量频率为30 kHz,采样频率为10 MHz。使用该系统在南黄海中部获得了40个站位不同类型沉积物的声学特性原位测量数据,并使用CTD剖面仪对该系统声速测量进行了标定,相对误差均小于0.5%,表明该系统测量数据准确、可靠。  相似文献   

2.
便携式海底沉积声学原位测量系统研制及应用   总被引:1,自引:0,他引:1  
详细介绍了最新研制的便携式海底沉积声学原位测量系统的工作原理和结构组成.与基于液压驱动的海底沉积声学原位测量系统相比,该系统操作简单,轻便灵活,易于吊放.2010年中国科学院南海海洋研究所“实验3”号科考船南海开放航次应用该系统在南海北部开展了海底沉积声学原位测量,首次获得该海区海底沉积物声速和声衰减系数原位测量数据.将原位测量声速与实验室测量声速进行了对比分析,结果表明二者存在明显差异,从而表明温度和压力等环境参数对沉积物声速具有重要影响.  相似文献   

3.
海底浅表层沉积物原位声学测量方法探讨   总被引:3,自引:1,他引:2  
邹大鹏  阚光明  龙建军 《海洋学报》2014,36(11):111-119
研究透射式和折射式两类海底沉积声学原位测量方法,通过分析10种海底浅表层沉积物声学原位测量仪器的特征,指出不同声学原位测量技术对沉积物声学特性测量结果的影响。比较黄海海底浅表层沉积声学原位测量数据与实验室测量结果的差异,分析原位声学测量数据普遍小于实验室测量数据的原因,指出原位测量的作用和重要性。探讨指出海底浅表层沉积物原位声学测量所需要配合发展的其他物理性质原位测量技术。  相似文献   

4.
文中设计基于可编程逻辑控制器(PLC)的测控平台、伺服加压控制、步进推动控制、多传感器测量、触摸屏交互等功能的温压可控声学测量系统,实现海底沉积物样品的孔隙水自动可控加压,通过声学测量功能单元测量海底沉积物在各个压力下的声速,模拟海底沉积物处于大陆坡2 000 m以浅海底表层任何深度变化时的声学特性测量,得到海底沉积物声速-压力特性,为校正实验室测量数据还原到海底原位测量数据提供一种方法。  相似文献   

5.
浅海沉积声学原位探测系统研制及深海功能拓展   总被引:1,自引:0,他引:1  
海底沉积物的声速和声衰减系数等声学特性参数是影响水下声场空间结构、水声通讯、水声设备使用性能、海底目标探测的重要因素。介绍了最新研制的浅海海底沉积声学原位测量系统的工作原理、结构组成和性能特点,并对系统在黄海和南海海底沉积物声学特性调查中的应用情况进行了总结。最后,对系统在满足深海应用方面的功能拓展进行了讨论和展望。  相似文献   

6.
为了能够快速准确的测量海底表层沉积物的声学参数,避免取样测量产生测量误差,研制出一种海底底质声学原位测量系统。为了检验原位测量系统的工作性能,在胶州湾海域进行了初步的测量实验分析。通过对测量结果的分析研究,验证了原位测量系统的一些工作性能,同时发现了一些需要改进的问题。  相似文献   

7.
海底底质声学性质原位测量技术研究   总被引:4,自引:0,他引:4  
系统介绍了海底底质声学性质原位测量技术,提出了新的原位测量方法,并根据这一测量方法,初步设计制作了相应的海底原位测量仪器。利用初步制作的测量仪器在实验室内对砂质沉积物进行了模拟测量试验,仪器测量得到的沉积物声速与直接透射法测量获得的声速基本一致。在宁波近海海域进行了海上实际测量试验,获得了该测量区域海底底质的声速,验证了此测量技术的可行性,为进一步研发先进的海底原位测量仪器奠定了基础。  相似文献   

8.
研究原位测量技术中表层沉积物声学原位测量技术、声波测井技术和OBS测量技术的特点和差异,得出3种技术的分辨率虽然依次降低,但测量尺度依次增大,可以应用不同深度和结构层序的海底沉积物声学物理性质研究.3种原位测量技术基于海底原位状态,可以测得海底沉积物的纵波和横波特性,通过比较纵波特性、纵横波速比和计算泊松比可以提高沉积...  相似文献   

9.
为满足在底水温度波动较大的海域进行海底热流原位长期观测的需求,研制了一种低功耗温度长期采集电路,并与钛合金耐压外壳集成为微型自容式测温单元,在室内和海上进行了一系列测试。室内测试结果表明:当测温电路进行连续采集时,其平均动态电流为2.1 m A;当电路不进行采集工作保持低功耗状态时,整个测温电路的电流消耗达到最低值,实测为4μA,达到预期设计指标。通过将微型测温单元捆绑在海底地震仪上,在南海西沙和东沙海域成功进行了6个站位的海底原位底水温度长期观测测试,获取了最长约17 d的底水温度波动数据,验证了测量电路的稳定性和实用性。  相似文献   

10.
海底表层沉积物具有多相、多颗粒、多形态的组成结构,导致其声学特性复杂多样。通过分析压缩波速度和切变波速度特性的研究现状,指出有待于解决的科学问题和关键技术问题。在分析国内外有关海底沉积层声速特性研究基础上,提出采取系统、可控的实验测量手段解决当前测量存在的4点问题。综合分析了压缩波速度和切变波速度存在的统计回归关系和理论分析关系,探讨了当前地声反演、采样样品声学测量、原位声学测量3种方法存在的测量尺度、测量频率、测量状态等的差异,探讨建立不同测量方法和测量技术对测量结果进行统一性解释的方法,从而获得不同类型、不同区域的海底表层沉积物真实的声速特性。最后,从实验室声学测量、物理力学参数测量、流固耦合特性分析、原位测量及海底监测、采样测量与原位测量的误差分析及校正、海底大纵深声学测量6个方面提出技术需求,为提高声学探测海洋和海底的精度服务,推动海洋声学探测和海洋工程发展。  相似文献   

11.
Seabed sediment microstructure has an influence on its acousto-physical properties, and the properties in a length of the sediment column reflect an aspect of the macroscopic behavior of the microstructure. An original measurement method of the sound attenuation within small distance cross sections in a sediment column, and the corresponding approach in data processing to attain an attenuation factor are detailed in the paper. This method was used to measure the compressional wave in series of points with a small distance in the sediment column, and it is shown that exponential attenuation is a type of compressional wave attenuation model for a sediment column in its full length. It indicates that there are various models of compressional wave attenuation in seabed sediments in the South China Sea after comparison of data from other literature. The method of measuring sound attenuation satisfies the sampling space interval in the acoustical forward and inverse problems in seabed sediments, and the original method provides a new approach for finding out sound attenuation mechanism in seabed sediments on small length scale.  相似文献   

12.
为研究小尺度海底沉积物样品的声衰减特性,作者提出了用声学探针测量海底沉积物声波幅值的新方法,对沉积物样品扰动小,两个测量点的距离可小于波长,为海底沉积物微观声衰减测量提供了新手段。作者用小于波长的间隔逐点测量了沉积物的压缩波幅值,数据分析表明沿沉积物柱状样全长的声衰减满足指数衰减模型。目前主要用同轴差距衰减测量法获得海底沉积物声衰减数据,但该方法不能辨识声衰减模型,因此不同海区的测量结果难以建立联系。对此作者又提出用声吸收系数反演的幅值比与声衰减系数反演的R值(两种幅值比的比值)作评价依据,分析了垂直轴差距衰减测量法获得的南海海底沉积物声衰减测量数据,发现部分沉积物样品声衰减的R值远大于1,其声衰减不满足指数衰减模型。在声衰减满足指数衰减模型的条件下,用Hamilton的声衰减和频率经验公式预报的南海沉积物声衰减比与作者用声学探针测量海底沉积物所得的声衰减比对比,通过对R值分析得出Hamilton的声衰减和频率经验公式可以预报南海沉积物声衰减比的范围。作者提出的声学探针测量海底沉积物声衰减的方法的优点是既能获得声衰减数据又能辨识声衰减模型,不同海区测量的沉积物声衰减比可用R值建立联系。  相似文献   

13.
南海浅海海底沉积物的声衰减   总被引:3,自引:0,他引:3       下载免费PDF全文
刘强  卢博 《海洋学报》2008,30(4):48-55
报道了南海浅海海底沉积物的声衰减性质。给出了测量和计算海底沉积物声衰减的方法。分析讨论了不同频率下的声衰减以及与若干个海底沉积物物理参数的关系,结果表明,同一类型沉积物在高频段时的声衰减要比低频段的声衰减大;同一频段下粗颗粒沉积物的声衰减要比细颗粒的声衰减大;北部湾海底浅层沉积物声衰减在低频100kHz下为80~150dB/m,在高频1MHz下为150~360dB/m;海南岛南部外海海底浅层沉积物声衰减在低频下为66~160dB/m,在高频1MHz下为190~350dB/m;高频段的数据与台湾海峡北部海底表层沉积物声衰减测量分析数据比较接近,而低频段的数据与台湾海峡北部海底表层沉积物声衰减测量分析数据有较大的差别。  相似文献   

14.
The Drag-type In-Situ Acoustic Measurement System (DISAMS) is a new instrument designed for rapid measurement of seabed sediment acoustic parameters, including the sediment sound velocity and acoustic attenuation coefficient. The DISAMS consists of six independent acoustic probes arranged symmetrically such that each side has one transmitting probe and two receiving probes. The entire operation is controlled and monitored in real time by a deck control unit on board, and the center frequency of the DISAMS is 30?kHz. The DISAMS can record full waveforms to determine the sound velocity and attenuation coefficient in the seabed sediment. In addition to site measurements, the DISAMS can also carry out towing measurements, resulting in improved efficiency compared with existing in-situ acoustic measurement systems. This article presents the configuration, electronics, and tests of the DISAMS in detail. Laboratory tests were conducted in a sediment pool, sea trials were carried out in the Zhoushan Islands, and sound velocity and attenuation coefficient data were obtained. The test results demonstrated that the DISAMS performed well and was able to measure the sound velocity and attenuation coefficient rapidly and accurately in both site measurements and towing measurements.  相似文献   

15.
The mechanical structure, the function modules, the working principles, and a sea trial of the newly developed ballast in situ sediment acoustic measurement system are reported in this study. The system relies on its own weight to insert transducers into seafloor sediments and can accurately measure the penetration depth using a specially designed mechanism. The system comprises of an underwater position monitoring and working status judgment module and has two operation modes: self-contained measurement and real-time visualization. The designed maximum working water depth of the system is 3,000?m, and the maximum measured depth of seafloor sediment is 0.8?m. The system has one transmitting transducer with the transmitting frequency band of 20–35?kHz and three receiving transducers. The in situ acoustic measurement system was tested at 15 stations in the northern South China Sea, and repeated measurements in seawater demonstrated good working performance. Comparison with predictions from empirical equations indicated that the measured speed of sound and attenuation fell within the predicted range and that the in situ measured data were reliable.  相似文献   

16.
Abstract

A new kind of visual acoustic measurement system was developed to obtain the acoustic characteristics of seabed sediment and the working state of in situ measuring equipment in real time. The control unit of the system structure is mainly made up of the underwater control unit and the deck control unit. In comparison with similar traditional systems, the system can transmit the working video image, the measured acoustic data and the waveform synchronous from the underwater control equipment to the deck control unit through the connecting cable. Apart from self-contained in situ measurement, the working modes of it include visual online real-time control. In order to guarantee the stability and measurement precision of the video control system, the process control of in situ measurement was strictly tested in the experimental tank. In 2017, sea trials of the in situ measurement system was carried out in the South China Sea. In the process, data related to measurement, including the acoustic velocity and attenuation coefficient of the seabed sediment, were obtained as well. The results from sea trials show that the control process of the visual system is intuitive, reliable and accurate, and therefore it can be popularized and applied.  相似文献   

17.
南海北部大陆架海底沉积物物理性质研究   总被引:6,自引:0,他引:6  
用物理(声学的、工程地质的、扫描电子显微镜)等技术方法,综合分析了沉积物结构特征和工程力学性质,研究了颗粒接触、堆垒、孔隙等现象与物理性质之间的关系,得出了沉积物声学物理参数和应力一应变性质之间的关系。结果表明,南海北部大陆架海底沉积物有6种结构类型,其中混合接触结构类型的沉积物具有较高的抗压强度和声速,浅层海底存在着高、低声速分层的中尺度结构。  相似文献   

18.
Using physical (acoustical engineering mechanics and scanning electron microscope) and other technical methods, is study makes a comprehensive analysis of the structural characteristics and engineering mechanics properties of sediments, the sediment structure, microstructure and their classification characteristics and in the light of the physical-mechanical characteristic parameters, the relations between the grain contact, grain accumulation, and porosity with the physical-mechanical characteristics of sediment, and reports the relationship between the acoustic physical parameters and the stress-strain properties of sediment. Results show that there are six structural types in the shelf seabed sediment of the northern South China Sea, among which, the mixed contact structural type sediment has a higher compressive strength and a higher sound velocity than others, and that in the shallow seabed there exists a mesoscale structure with high and low velocity layers.  相似文献   

19.
ABSTRACT

Using physical (acoustical engineering mechanics and scanning electron microscope) and other technical methods, is study makes a comprehensive analysis of the structural characteristics and engineering mechanics properties of sediments, the sediment structure, microstructure and their classification characteristics and in the light of the physical-mechanical characteristic parameters, the relations between the grain contact, grain accumulation, and porosity with the physical-mechanical characteristics of sediment, and reports the relationship between the acoustic physical parameters and the stress-strain properties of sediment. Results show that there are six structural types in the shelf seabed sediment of the northern South China Sea, among which, the mixed contact structural type sediment has a higher compressive strength and a higher sound velocity than others, and that in the shallow seabed there exists a mesoscale structure with high and low velocity layers.  相似文献   

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