A permanent seismic station beneath the Ocean Bottom

The Hawaii Institute of Geophysics began development of the Ocean Subbottom Seisometer (OSS) system in 1978, and OSS systems were installed in four locations between 1979 and 1982. The OSS system is a permanent, deep ocean borehole seismic recording system composed of a borehole sensor package (tool), an electromechanical cable, recorder package, and recovery system. Installed near the bottom of a borehole (drilled by the D/V Glomar Challenger), the tool contains three orthogonal, 4.5-Hz geophones, two orthogonal tilt meters; and a temperature sensor. Signals from these sensors are multiplexed, digitized (with a floating point technique), and telemetered through approximately 10 km of electromechanical cable to a recorder package located near the ocean bottom. Electrical power for the tool is supplied from the recorder package. The digital seismic signals are demultiplexed, converted back to analog form, processed through an automatic gain control (AGC) circuit, and recorded along with a time code on magnetic tape cassettes in the recorder package. Data may be recorded continuously for up to two months in the self-contained recorder package. Data may also be recorded in real time (digital formal) during the installation and subsequent recorder package servicing. The recorder package is connected to a submerged recovery buoy by a length of bouyant polypropylene rope. The anchor on the recovery buoy is released by activating either of the acoustical command releases. The polypropylene rope may also be seized with a grappling hook to effect recovery. The recorder package may be repeatedly serviced as long as the tool remains functionalA wide range of data has been recovered from the OSS system. Recovered analog records include signals from natural seismic sources such as earthquakes (teleseismic and local), man-made seismic sources such as refraction seismic shooting (explosives and air cannons), and nuclear tests. Lengthy continuous recording has permitted analysis of wideband noise levels, and the slowly varying parameters, temperature and tilt.Hawaii Institute of Geophysics Contribution 1909.     

Display of acoustic reflection profiles using a dot matrix plotter

Acoustic reflection profiling data display is traditionally done with the aid of a facsimile type of recorder. It is not uncommon to record the unprocessed acoustic data on a tape recorder for subsequent playback through a laboratory computer. This still involves the use of some sort of facsimile recorder for the ultimate display of profiles. This paper presents the results of a study to adapt a high-speed digital dot matrix plotter for the ultimate display in place of the conventional facsimile recorder. Because a minicomputer drives the display directly, a host of signal conditioning procedures are permitted, with the final display being generated in real time. Algorithms are developed to control the marking density, allow adaptive threshold control, bottom tracking, automatic gain control, and de-emphasis of water column boundary reverberation. These techniques are just a few of the many that can be employed since the computer can readily be carried on a large ship in deep water, or a small vessel in a harbour. Shallow water is the difficult case for high energy acoustic sources because the water column boundaries behave much like an excited acoustic cavity. For this reason, a section of seismic profile is shown which was obtained with a 7·5 kHz pinger in only 8 m of water in Narragansett Bay. This research was partiallysupported by the Division of Computer Research of the National Science Foundation.     

A digital event-recording ocean bottom seismometer capsule

The ocean bottom seismometer capsule contains a 1 Hz. vertical seismometer and triggerable or programmable digital recording system. The output of the seismometer is continuously digitized at a preselected rate of 64, 128, or 256 samples/sec. The digital data words are mixed with a time code and synchronization characters, serialized and passed through a 1536 sample shift register which acts as a delay line. The serial output bits are then encoded and recorded on a SONY TC800B tape recorder which is turned on when a seismic event occurs. The event trigger occurs when the seismic signal jumps to 8 times the time averaged input signal. A memory may be programmed to run the recorder on a schedule so that small amplitude signals from refraction shots are sure to be recorded. Data are recovered using the same recorder for playback and a decoder which provides an analog output for field data interpretation or a digital output for computer analysis. An acoustic transponder allows precise ranges between the capsule and ship to be determined. In addition, commands for the capsule to release or to transmit diagnostic data may be given from the surface ship. The capsule falls freely to the ocean bottom. After a predetermined time or when a release command is received, it is released from a 68 kg steel tripod and floats to the surface. A dual timer and explosive bolt system is used to increase recovery reliability.The first capsules were designed and constructed between October 1972 and October 1973. Good results were obtained from 38 out of 43 launchings made on six expeditions in 1974, 1975, and 1976. Four capsules have been lost.     

LRS-16A地震记录系统记录技术的革新

ＬＲＳ－１６Ａ地震系统原以Ｔｅｌｅｘ６２５３盘式带了系统进行记录,随着技术的发展,用３４８０盒 式带子系统取代Ｔｅｌｅｘ６２５３盘式带子系统成为可能,为此,针对ＬＲＳ－１６Ａ地震系统,购买了ＩＢＭ９４８０盒式带子系统,进行相应的替换,但在实际应用过程中,出现了系统兼容性问题,导致文件记录不完整,针对这些问题,进行了技术革新。     

Multipath channel identification with wavelet packets

This paper deals with the basic modeling problem in underwater acoustics that is the characterization of the channel between a transmitter and a receiver. The problem is analyzed here using an array of sensors that receive PSK signals emitted by several sources. Data come from an experiment realized by a physical system situated in the Mediterranean Sea. In order to identify the multipath channel, we need to access the propagation time delay and the angle of arrival of each propagation ray. However, many of these acoustic ray paths are too close to be separated by classic processing methods (matched filter, beamforming, etc.); new methods with better resolution must be applied in order to analyze the experimental signals and to determine their arrival time on the array of sensors. After a presentation of this problem, we will first discuss high-resolution methods that are usually applied in the localization problem; we will then focus on wavelet packet analysis which provides good results by improving the temporal resolution of acoustic signals     

A fast algorithm for high-accuracy frequency measurement:application to ultrasonic Doppler sonar

In an attempt to investigate the technical feasibility of a CW Doppler sonar, we have examined a method of measuring low velocities with a high-velocity resolution, or frequency resolution, by use of a simple circuit configuration employing digital signal processing technique. The following discussion presents the results of the investigation. In the measuring method described, the fast Fourier transform (FFT) of undersampled data is calculated and the Doppler shift is obtained by searching for a peak frequency of the power spectrum. To achieve the intended frequency resolution of 1 Hz by FFT operation, measurement of data for a minimum measuring period of 1 s is essential. If the sampling frequency is set to 50 kHz, the number of samples obtained during the minimum measuring period of I s would amount to 50000. This is not practical in light of the time required for the FFT operation. To overcome this problem, our new measuring method employs a decimation technique for reducing the number of samples down to 1024 while maintaining a frequency resolution of about 1 Hz. This paper describes how the processing time can be drastically reduced to about 1/300th compared to the conventional technique by a combination of complex exponential functions, filtering and decimation, and thereby indicates the possibility of real-time CW Doppler data processing     

Ocean-bottom-seismograph of the Institut für Geophysik,Hamburg

The ocean bottom seismograph (OBS) of the Institut für Geophysik, Hamburg (IfG) is designed for refraction seismic experiments and for recording microseismic noise. Hydrophone signals are recorded directly on a casette tape recorder with a band width of 3–60 Hz. Signals from three component 1 Hz seismometers are recorded on a 2nd casette tape recorder in FM for a frequency range of 0.1–1 Hz. A telemetering buoy at the surface is connected with the OBS by a polypropylene rope.     

Calculation of the added mass of circular cylinders in shallow water

The added mass of hull section shapes must be known, in order to carry out any studies of ship motions, which may be associated with either seakeeping or manoeuvring. Determination of the added mass in deep water can involve conformal mapping or surface singularity distributions. However, in shallow water the problem of determining the added mass is made more difficult by the proximity of the seabed. In this paper, three approaches to the problem of finding the added mass of semi-circular sections are explored. Although there is no known exact solution to this problem, the relationships given by the three methods are compared and the approximate nature of the solutions is examined. The first method is a series solution, which is taken here to include more terms than are normally given in the existing literature. The other two solutions are considered to be new, and so are given in some mathematical detail.     

Frequency management support for remote sea-state sensing using the JINDALEE skywave radar

Successful operation of a skywave (over-the-horizon, OTH) radar in a remote sea-state sensing mode is critically dependent upon the application of comprehensive frequency management techniques. In addition to the problem of selecting a frequency yielding an adequate signal-to-noise ratio in the geographical area under investigation, attention must be paid to minimization of ionospheric multimode and other phenomena capable of distorting or convoluting the sea backscatter spectrum. This paper describes the manner in which these problems have been addressed in the JINDALEE skywave radar, and relates the practical difficulties inherent in the task of frequency management in support of an OTH radar involved in sea-state sensing. Measurement techniques include backscatter and oblique-incidence sounding, HF spectral surveillance, and a low-powered frequency-agile "miniradar" capable of operating in either a conventional backscatter or alternate oblique-incidence mode. In addition to providing the main radar with real-time frequency management advice, a principal emphasis has been the acquisition of a synoptic data base suitable for off-line statistical analysis.     

Ocean bottom seismograph development at Hawaii Institute of Geophysics

Three distinct ocean bottom seismograph (OBS) systems have been developed at the Hawaii Institute of Geophysics to satisfy the different requirements for short-range refraction and anisotropy experiments, long-range refraction experiments, and short-term and semi-permanent monitoring for earthquakes. One system, originally designed for semi-permanent use in conjunction with a monster buoy of the IDOE North Pacific Experiment has been modified for emplacement off Oahu. It contains 3-component 1 Hz seismometers and a hydrophone and obtains power and transmits data via tow conductor cable. Two additional systems were designed for short-term use: a 2 Hz telemetering system (TOBS); and 4.5 Hz free-fall pop-up system (POBS). The TOBS contains 3-component seismometers and a hydrophone and transmits data to the ship via light-weight single-conductor electromechanical cable and an HF-VHF radio link from a surface buoy. The bottom package also includes a backup tape recorder. This system exhibits the advantages of real-time data acquisition (e.g. precise timing, rapid appraisal of data quality, optimum use of explosives, and common recording with other data) and the complexities and difficulties associated with a deep-sea mooring. However, use of cable with near neutral bouyancy permits the design of a deep-water system with low weights and stress levels. The POBS is a self-contained package containing a vertical and single horizontal seismometer, hydrophone, cassette tape recorder, and pre-set timed release. This system is relatively simple and inexpensive. Total weight of 150 kg in air (before launch) permits emplacement and retrieval from a ship with no special equipment by two (strong) persons. Experience to data suggests that the optimum deployment scheme for many studies is a combination of TOBS's and POBS's.Hawaii Institute of Geophysics Contribution 835.     

Uncertainty analysis on extreme value analysis of significant wave height at eastern coast of Korea

In this study, we considered the problem of estimating long-term predictions of design wave height based on the observation data collected over 10–15 years along the eastern-coast of the Korean peninsula. We adopted a method that combines Bayesian method and extreme value theory. The conventional frequency analysis methods must be reconsidered in two ways. First, the conventional probability distributions used in the frequency analysis should be evaluated to determine whether they can accurately model the variation in extreme values. Second, the uncertainty in the frequency analysis should also be quantified. Therefore, we performed a comparative study of the Gumbel distribution and GEV distribution to show the higher efficiency of the latter. Further, we compared the Bayesian MCMC (Markov Chain Monte Carlo) scheme and the MLE (Maximum Likelihood Estimation) with asymptotic normal approximation for parameter estimation to confirm the advantage of the Bayesian MCMC with respect to uncertainty analysis.     

一种神经网络计算器VLSI实现可行性研究

本文以一种新型激光扫描３－Ｄ视觉传播系统中快速求解３－Ｄ坐标值等为例子,展示ＢＰ神经网络的并行分布处理在本质上具有高速度优势及硬件容错能力;以及如何实现基于模拟神经网络的二进制数字量映射的无误差操作：进而阐明用模拟ＶＬＳＩ技术实现训练后神经网络芯片的可行性和推广意义。     

Acoustic transmission of images using a microprocessor-based video bandwidth reduction technique

The problems associated with the acoustic transmission of real-time television pictures are considered in this paper. A solution to the high data rate video source is found in the application of a spatial data redundancy reduction algorithm, Micro Adaptive Picture Sequencing (MAPS). This algorithm has been implemented on two commercially available microprocessors (M68000), which operate on a digitized image to produce a coded image which is transmitted and reconstructed. Using the spatial data reduction algorithm it is possible to transmit 1 to 2 frames per second of a96 times 96 pixel times 4bits gray level image over a 9600 baud link. Although these images do not possess the full dynamic range and resolution of home quality video, this work suggests that the acoustic channel could be utilized for control of an unmanned untethered submersible. Also, the transmission of high resolution information is made practical when some data reductions are performed prior to acoustic transmission.     

Planning for quality data

Advance planning is essential for the production of quality data. Before any planning is attempted, a well-defined model of the problem under investigation must be established. The measurements may be made to test the model or they may be used with the model to clarify or solve the problem under investigation.In the planning process, chemical measurement must be considered as a system consisting of sampling, calibration, analysis, and data processing. Appropriate quality assurance procedures must be applied to ensure statistical control and evaluation of the data. Because of the interdependence of the various aspects of measurement, they must be planned in a coordinated mode, involving subject matter, measurement, and statistical expertise.Details of all of the above are discussed in the paper.     

中浅地层剖面质量改进方法及应用

海洋工程勘察中,中浅地层剖面是一种应用广泛的调查设备,其具有便携性、高效率、高主频和高分辨率的特点。实际调查中,随机噪音、多次波等问题严重降低了地层剖面资料的信噪比和分辨率,同时,现场作业对海况的依赖性很强。文中从中浅地层剖面的野外采集设备和室内资料处理方面分析,提出立体震源、多道接收系统、带通滤波、预测反褶积和相关滤波等方法。立体震源拓宽了地层剖面资料的频带,获得了更深的剖面和更高的分辨率;多道接收系统使中浅地层剖面数据由单道变为多道,有利于室内资料处理;对于目前主流的单道中浅地层剖面数据,首先要识别噪音的来源和特征,再通过增益、带通滤波、涌浪校正,预测反褶积等方法来处理,最后获取的高质量地层剖面资料一定是各种方法的综合使用和多次试验的结果。     

中浅地层剖面质量改进方法及应用

海洋工程勘察中,中浅地层剖面是一种应用广泛的调查设备,其具有便携性、高效率、高主频和高分辨率的特点。实际调查中,随机噪音、多次波等问题严重降低了地层剖面资料的信噪比和分辨率,同时,现场作业对海况的依赖性很强。本文从中浅地层剖面的野外采集设备和室内资料处理方面分析,提出立体震源、多道接收系统、带通滤波、预测反褶积和相关滤波等方法。立体震源拓宽了地层剖面资料的频带,获得了更深的剖面和更高的分辨率;多道接收系统使中浅地层剖面数据由单道变为多道,有利于室内资料处理;对于目前主流的单道中浅地层剖面数据,首先要识别噪音的来源和特征,再通过增益、带通滤波、涌浪校正,预测反褶积等方法来处理,最后获取的高质量地层剖面资料一定是各种方法的综合使用和多次试验的结果。     

连云港温盐井水温资料对比分析

随着海洋自动观测系统的推广应用,温盐井也在海洋系统普及开来,对温盐井性能的研究,即所测得的水文数据的有效性进行研究有现实意义。对连云港海洋环境监测站温盐井内外表层海水温度的数据运用传统的统计对比分析,指出该温盐井测得的数据中有96.2%的水温数据符合海滨观测规范规定的三级标准是有效的。从而表明温盐井满足了测量表层海上温度的技术要求。     

An Ocean Bottom Hydrophone instrument for seismic refraction experiments in the deep ocean

Tests of a new Ocean Bottom Hydrophone (obh) instrument have recently been completed at Woods Hole Oceanographic Institution. This instrument is designed to float 3 m above the seafloor at depths of up to 6100 m for periods of up to 10 days and continuously records the output of a single hydrophone on a four-channel 0.064 cm/s (1/40 in./s) analog magnetic tape recorder. This instrument has an acoustic transponder and release system and is designed primarily for multiple deployments as a fixed ocean bottom receiver for seismic refraction work.Contribution No. 4174 of the Woods Hole Oceanographic Institution.     

海上多道地震数据的解编和格式转换

将DFS－V地震仪记录系统的磁带记录方式升级改造为微机文件记录方式，分析比较和实践证明后者具有轻便、经济、易操作等优点。为进行现场数据保存备份和传输交换，作者通过编程在微机上实现了海上多道地震数据的解编，并成功地把非标准的SEGB格式数据转换为通用的标准SEGY格式。文中对该程序的有关技术问题和应用情况作了分析和阐述。     

Practical aspects of frequency-domain identification of dynamic models of marine structures from hydrodynamic data

The motion response of marine structures in waves can be studied using finite-dimensional linear-time-invariant approximating models. These models, obtained using system identification with data computed by hydrodynamic codes, find application in offshore training simulators, hardware-in-the-loop simulators for positioning control testing, and also in initial designs of wave-energy conversion devices. Different proposals have appeared in the literature to address the identification problem in both time and frequency domains, and recent work has highlighted the superiority of the frequency-domain methods. This paper summarises practical frequency-domain estimation algorithms that use constraints on model structure and parameters to refine the search of approximating parametric models. Practical issues associated with the identification are discussed, including the influence of radiation model accuracy in force-to-motion models, which are usually the ultimate modelling objective. The illustration examples in the paper are obtained using a freely available MATLAB toolbox developed by the authors, which implements the estimation algorithms described.