Dynamics and navigation of autonomous underwater vehicles for submarine gravity surveying

被引:14
作者
Kinsey, James C. [1 ]
Tivey, Maurice A. [2 ]
Yoerger, Dana R. [1 ]
机构
[1] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA
[2] Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA
关键词
SEA-FLOOR GRAVITY; UPPER OCEANIC-CRUST; MID-ATLANTIC RIDGE; PACIFIC RISE CREST; MARINE GRAVITY; POROSITY; DENSITY; EXPLORATION; SHIPBOARD; PROFILE;
D O I
10.1190/GEO2012-0181.1
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We investigated the effect of autonomous underwater vehicle (AUV) dynamics and navigation on underway submarine gravimetry. Our research was motivated by the need to obtain spatially dense marine gravity measurements close to the source of subkilometer-scale geologic features in the shallow oceanic crust. Such measurements have been previously obtained, for instance, with piloted submarines and towed sleds; however, the high cost and, in the case of on-bottom measurements, poor spatial sampling preclude routine acquisition of these measurements. Continuous underway gravity surveys with AUVs is a compelling cost-effective option, but this method requires separating the AUV accelerations from the measured gravity. We show that AUVs with a large distance between the center of buoyancy and the center of gravity have lower vertical accelerations than torpedo-shaped AUVs and consequentially are better suited for underway gravity surveys. Furthermore state estimators, which combine sensor measurements and models of the vehicle's motion, provide superior estimates of the vehicle's vertical accelerations than methods used in previous underway submarine gravity surveys. We simulated the use of these navigation methods in detecting dike swarms at the East Pacific Rise. Analysis showed that we can shorten filters used in reducing gravity data and consequentially provide improved measurements of the free-water anomaly with a minimal detectable spatial wavelength approximately 65% lower than previously reported results.
引用
收藏
页码:G55 / G68
页数:14
相关论文
共 58 条
  • [1] Ageev M. D., 1994, P IEEE MTS OC C, P126
  • [2] Allen B, 1997, OCEANS '97 MTS/IEEE CONFERENCE PROCEEDINGS, VOLS 1 AND 2, P994, DOI 10.1109/OCEANS.1997.624126
  • [3] [Anonymous], 2011, OCEANS
  • [4] Crystal structure of the Mid-Atlantic Ridge south of the Kane Fracture Zone from seafloor and sea surface gravity data
    Ballu, V
    Dubois, J
    Deplus, C
    Diament, M
    Bonvalot, S
    [J]. JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 1998, 103 (B2) : 2615 - 2631
  • [5] The density structure associated with oceanic crustal rifting at the Hess Deep: a seafloor and sea-surface gravity study
    Ballu, V
    Hildebrand, JA
    Canuteson, EL
    [J]. EARTH AND PLANETARY SCIENCE LETTERS, 1999, 171 (01) : 21 - 34
  • [6] Seafloor gravity evidence for hydrothermal alteration of the sediments in Middle Valley, Juan de Fuca Ridge
    Ballu, VS
    Hildebrand, JA
    Webb, SC
    [J]. MARINE GEOLOGY, 1998, 150 (1-4) : 99 - 111
  • [7] Bar-Shalom Y., 2004, Estimation with applications to tracking and navigation: Theory algorithms and software
  • [8] EVALUATION OF THE BGM-3 SEA GRAVITY METER SYSTEM ONBOARD R/V CONRAD
    BELL, RE
    WATTS, AB
    [J]. GEOPHYSICS, 1986, 51 (07) : 1480 - 1493
  • [9] Bell-Aerospace, 1978, TECHNICAL REPORT
  • [10] Caress D., 2008, AUV D. Allan B, P47, DOI [10.4027/mhmta.2008.04, DOI 10.4027/MHMTA.2008.04]