Autonomous Underwater Vehicles (AUVs): Their past, present and future contributions to the advancement of marine geoscience

海底扩张 地质学 潜艇 水下 海洋学 海床 深海热液喷口 遥控车辆 地球科学 深海 古生物学 热液循环
作者
Russell B. Wynn,Veerle A.I. Huvenne,T. P. Le Bas,Bramley J. Murton,Douglas P. Connelly,Brian J. Bett,Henry A. Ruhl,Kirsty J. Morris,Jeff Peakall,Daniel R. Parsons,E. J. Sumner,Stephen E. Darby,R. M. Dorrell,James E. Hunt
出处
期刊:Marine Geology [Elsevier BV]
卷期号:352: 451-468 被引量:840
标识
DOI:10.1016/j.margeo.2014.03.012
摘要

Autonomous Underwater Vehicles (AUVs) have a wide range of applications in marine geoscience, and are increasingly being used in the scientific, military, commercial, and policy sectors. Their ability to operate autonomously of a host vessel makes them well suited to exploration of extreme environments, from the world's deepest hydrothermal vents to beneath polar ice sheets. They have revolutionised our ability to image the seafloor, providing higher resolution seafloor mapping data than can be achieved from surface vessels, particularly in deep water. This contribution focuses on the major advances in marine geoscience that have resulted from AUV data. The primary applications are i) submarine volcanism and hydrothermal vent studies, ii) mapping and monitoring of low-temperature fluid escape features and chemosynthetic ecosystems, iii) benthic habitat mapping in shallow- and deep-water environments, and iv) mapping of seafloor morphological features (e.g. bedforms generated beneath ice or sediment-gravity flows). A series of new datasets is presented that highlight the growing versatility of AUVs for marine geoscience studies, including i) multi-frequency acoustic imaging of trawling impacts on deep-water coral mounds, iii) collection of high-resolution seafloor photomosaics at abyssal depths, and iii) velocity measurements of active submarine density flows. Future developments in AUV technology of potential relevance to marine geoscience include new vehicles with enhanced hovering, long endurance, extreme depth, or rapid response capabilities, while development of new sensors will further expand the range of geochemical parameters that can be measured.
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