锰结壳厚度双框架声探头实时控制研究

T. Sato, B. Thornton, A. Bodenmann, A. Asada, T. Ura
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引用次数: 4

摘要

锰结壳作为一种潜在的矿产资源受到广泛关注。地壳形成了一层薄薄的沉积物,分布在海底山表面的大片区域上。迄今为止,了解锰结壳厚度的唯一方法是通过取样和钻探,但这些方法既昂贵又耗时。我们开发了一种声学装置,可以在使用水下机器人进行调查时确定锰结壳的厚度。该系统在西北太平洋Takuyo-Daigo海山的平顶海试中取得了成功。然而,众所周知,锰壳不仅分布在平坦的表面上,而且分布在海山的斜坡上,虽然在海底相对平坦的地区可以进行精确的测量,但在陡峭的斜坡上进行的测量质量却因声学探头必然窄波束的大入射角而下降。本研究的目的是探讨提高陡坡上锰壳厚度测量数据返回率的潜在方法。实验确定了入射角对锰壳样品声反射的影响,发现入射角大于3°对测量的反射信号有不利影响。利用“seaxerrocks”三维可视化测绘设备获取的高分辨率三维测深数据进行分析,以确定地壳覆盖海底的实际局部倾角。在此基础上,建议引入双框架系统,主动控制声探头的角度,使声波束垂直进入海底。为了实现实时控制,需要一种基于海底稀疏测量的相对角度确定方法。所开发的控制算法利用安装在水下机器人前后的两个距离传感器,即直线投影激光和单点声波距离传感器,实时确定海底的相对倾斜度。所开发的双万向节系统的性能已在已知几何形状的简单倾斜模型的水箱试验中进行了评估。实验结果表明,由于主动控制,斜坡的声反射强度得到了改善。该装置在锰包覆海山进行了海试,测量了陡峭的斜坡表面,并给出了海试的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Towards real-time control of a double gimbaled acoustic probe for measurement of manganese crusts thickness
Manganese crusts are the focus of much attention as a potential mineral resource. The crusts form a thin layer of deposit that is distributed over wide areas on the surface of seamounts. To date, the only way to know the thickness of manganese crusts has been through sampling and drilling, but these methods are expensive and time consuming. We have developed an acoustic device that can determine the thickness of manganese crusts during surveys using an underwater robot. This system has worked successfully during sea trials on the flat top of Takuyo-Daigo seamount, located in the northwest Pacific. However, manganese crusts are known to be distributed not only on flat surfaces but also on the slopes of seamounts, and while accurate measurements are possible on relatively flat areas of the seafloor, the quality of measurements made on steep slopes are degraded by the large angle of incidence of the necessarily narrow beam of the acoustic probe. The aim of this research is to investigate potential methods to improve data return rates of manganese crust thickness measurements on steep slopes. The effects of the angle of incidence on the acoustic reflections measured from a manganese crust sample are determined experimentally and it is found that an angle of incidence larger than 3° has a detrimental effect on the measured reflected signal. High resolution 3D bathymetry data acquired using the 3D visual mapping device `SeaXerocks' was analyzed, so as to determine the actual local inclination of crust covered seafloor. Based on the analysis, it is suggested that a double gimbal system should be introduced to actively control the angle of the acoustic probe so that the acoustic beam enters the seafloor orthogonally. In order to achieve real-time control, a method to determine the relative angle based on sparse measurements of the seafloor is necessary. The control algorithm developed uses two range sensors, consisting of a line projected laser and a single point acoustic range sensor, mounted on front and back of underwater robot so that the relative inclination of seafloor can be determined in real-time. The performance of the developed double gimbal system has been assessed in water tank experiments working on simple sloped models of known geometry. The experiments demonstrate an improvement in the intensity of the acoustic reflections from the slopes as a result of the active control. The setup was used during sea trials at a manganese encrusted seamount to survey steeply sloped surfaces, and the results of the sea trials are presented.
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