[1]Knott S T. Use of the precision graphic recorder in oceanography[J]. Marine Scientific Instrumentation, 1962, 1: 251-262.
[2]Cacchione D A, Sternberg R W, Ogston A S. Bottom instrumented tripods: History, applications, and impacts[J]. Continental Shelf Research,2006, 26: 2 319-2 334.
[3]Shanghai Center of Marine Science & Technology(Prepartory Office), State Key Laboratory of Marine Geology of Tongji University. China Seafloor Observation—Science and Technology [M]. Shanghai: Tongji University Press, 2011.[上海海洋科技研究中心(筹),海洋地质国家重点实验室(同济大学). 海底观测——科学与技术的结合[M]. 上海:同济大学出版社,2011.]
[4]Sternberg R W. Friction factors in tidal channels with differing bed roughness[J]. Marine Geology,1968, 6: 243-260.
[5]Cacchione D A, Drake D E. A new instrument system to investigate sediment dynamics on continental shelves[J]. Marine Geology,1979, 30: 299-312.
[6]Gross T F, Williams III A J. Characterization of deep-sea storms[J]. Marine Geology,1991, 99: 281-302.
[7]Agrawal Y C, Traykovski P. Particles in the bottom boundary layer: Concentration and size dynamics through events[J]. Journal of Geophysical Research, 2001, 106: 9 533-9 542.
[8]Mikkelsen O A, Pejrup M. The use of a LISST-100 laser particle sizer for in-situ estimates of floc size, density and settling velocity[J]. Geo-Marine Letters, 2001, 20: 187-195.
[9]Sternberg R W, Berhane I, Ogston A S. Measurement of size and settling velocity of suspended aggregates on the northern California shelf[J]. Marine Geology,1999, 154: 43-53.
[10]Rubin D M, Chezar H, Topping D J, et al. Two new approaches for measuring spatial and temporal changes in bed-sediment grain size[C]∥Flemming B W, Hartmann D, Delafontaine M T, eds. International Workshop on Particle Size to Sediment Dynamics. Germany: Hanse Institute, 2004: 126-128.
[11]Tengberg A, De Bovee F, Hall P, et al. Benthic Chamber and Profiling Landers in Oceanography—A Review of Design, Technical Solutions and Functioning[M]. Oxford: Elsevier Science Ltd.1995.
[12]Kuenen Ph H, Migliorini C I. Turbidity currents as a cause of graded bedding[J]. Journal of Geology, 1950, 58(2): 91-127.
[13]Nowell A R M, Hollister C D. The objectives and rationale of HEBBLE[J]. Marine Geology, 1985, 66: 1-11.
[14]Grant W D, Williams A J, Glenn S M. Bottom stress estimates and their prediction on the northern California continental shelf during CODE-1: The importance of wave-current interaction[J]. Journal of Physical Oceanography,1984, 14: 506-527.
[15]McCave I N, Chandler R C, Swift S A, et al. Contourites of the Nova Scotian continental rise and the HEBBLE area[M]∥Stow D A V, Pudsey C J, Howe J A,
et al, eds. Deep-Water Contourite Systems: Modern Drifts and Ancient Series, Seismic and Sedimentary Characteristics. London:Geological Society, 2002.
[16]Boyle E A. Introduction: Chemical oceanography[J]. Chemical Reviews,2007, 107: 305-307.
[17]Black K S, Fones G R, Peppe O C, et al. An autonomous benthic lander: Preliminary observations from the UK BENBO thematic programme[J]. Continental Shelf Research,2001, 21: 859-877.
[18]Priede I G, Bagley P M, Way S, et al. Bioluminescence in the deep sea: Free-fall lander observations in the Atlantic Ocean off Cape Verde[J]. Deep-Sea Research I, 2006, 53: 1 272-1 283.
[19]Jamieson A J, Fujii T, Solan M, et al. HADEEP: Free-falling landers to the deepest places on Earth[J]. Marine Technology Society Journal, 2009, 43(5): 151-160. |