Precise acoustic ranging and positioning: a progress report

Y. Osada, H. Fujimoto, K. Koizumi, T. Kanazawa, H. Murakami
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引用次数: 2

Abstract

The authors carried out an experiment in April 1999 by using a 2 m-square surface buoy and the RV Tansei-maru, Ocean Research Institute, University of Tokyo. Three GPS antennae were fixed on the top of the buoy and an acoustic transducer on the bottom. GPS reference station for kinematic GPS positioning from the study area was set at Aburatsubo, about 35 km away. Both the reference station and the GPS receivers installed on the buoy were recorded at 1 Hz sampling. An acoustic ranging system was developed under the Ocean Hemisphere Project, but the resolution of the acoustic ranging was 10 cm. Three acoustic transponders were deployed on the seafloor at about 1400 m water depth. The authors carried out acoustic positioning every 20 s for 30-60 minutes. The effect of motion of the buoy was only removed using the data of the GPS receivers; the problem was that timing of acoustic measurements was not so precise. The repeatability of the buoy's positioning is estimated to be 20-30 cm. The objective was to establish sea-floor reference points for the measurement of tectonic plate movements and crustal deformations.
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精确的声学测距和定位:进度报告
作者于1999年4月利用一个2平方米的水面浮标和东京大学海洋研究所的RV Tansei-maru进行了一次实验。三个GPS天线固定在浮标的顶部,一个声学换能器固定在底部。研究区运动学GPS定位参考站设置在35 km外的Aburatsubo。参考站和安装在浮标上的GPS接收器均以1 Hz采样记录。在海洋半球项目下研制了声测距系统,但声测距分辨率为10厘米。三个声波应答器部署在1400米水深的海底。每隔20秒进行一次声波定位,持续30-60分钟。仅利用GPS接收机的数据去除浮标运动的影响;问题是声学测量的时间不是那么精确。浮标定位的可重复性估计为20-30厘米。目的是为测量构造板块运动和地壳变形建立海底参考点。
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