Abstract
Many instruments that operate in the marine environment use microcomputers for control and data-logging. RALPH, designed to study seabed sediment transport processes, is such an instrument. Although the design was started in 1978 and useful data have been collected since 1980 (DeIure, 1983; Boyd et al., 1983), RALPH, like many research tools, has been in a constant state of development. This development has mainly involved the addition of sensors and the provision for more data-logging. These two thrusts have led to RALPHNET.
Keywords
- Suspended Sediment Concentration
- Local Area Network
- External Device
- Punctuation Mark
- Ocean Bottom Seismometer
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.
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References
Boyd, R., Forbes D. L. and Heffler, D. E. 1983. Fairweather sediment dispersal on the shoreface of the Nova Scotia Atlantic Coast (abstract). EOS, Trans. Am. Geophys. Un. 64, 1102.
DeIure, A. 1983. Storm effects in Halifax harbour. M.Sc. Thesis, Dalhousie University, Halifax, Canada.
Heffler, D. E. 1984. RALPH — an instrument to monitor seabed sediments. In Current Research, Part B, Geol. Survey of Canada, Paper 84–1b, pp. 47–52.
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© 1986 Society for Underwater Technology
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Heffler, D. (1986). RALPHNET: An Underwater Local Area Network. In: Oceanology. Advances in Underwater Technology, Ocean Science and Offshore Engineering, vol 6. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-4205-9_21
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DOI: https://doi.org/10.1007/978-94-009-4205-9_21
Publisher Name: Springer, Dordrecht
Print ISBN: 978-94-010-8366-9
Online ISBN: 978-94-009-4205-9
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