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The paper contains results of a in situ research main task of which was to detect objects buried, partially or completely, in the sea bottom. Object detecting technologies employing acoustic wave sources based on nonlinear interaction of elastic waves require application of parametric sound sources. Detection of objects buried in the sea bottom with the use of classic hydroacoustic devices such as the sidescan sonar or multibeam echosounder proves ineffective. Wave frequencies used in such devices are generally larger than tens of kHz. This results in the fact that almost the whole acoustic energy is reflected from the bottom. On the other hand, parametric echosounders radiate waves with low frequency and narrow beam patterns which ensure high spatial resolution and allows to penetrate the sea bottom to depths of the order of tens of meters. This allows to detect objects that can be interesting, among other things, from archaeological or military point of view.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
99--104
Opis fizyczny
Bibliogr. 10 poz., rys.
Twórcy
autor
- Polish Naval Academy Smidowicza 69, 81-103 Gdynia, Poland
- Gdansk University of Technology Narutowicza 11/12, 80-233 Gdansk, Poland
autor
- Polish Naval Academy Smidowicza 69, 81-103 Gdynia, Poland
autor
- Polish Naval Academy Smidowicza 69, 81-103 Gdynia, Poland
autor
- Polish Naval Academy Smidowicza 69, 81-103 Gdynia, Poland
Bibliografia
- 1.Galloway J., Collins W. (1998), Dual frequency acoustic classification of seafloor habitat using the QTCview, Oceans’98, Nice, France.
- 2. Grelowska G., Kozaczka E., Szymczak W. (2010), Methods of data extraction from sub-bottom profiler’s signal, Hydroacoustics, 13, 109-118.
- 3. Hamilton L., Mulhearn P., Poeckert R. (1999), Comparison of RoxAnn and QTC-view acoustic bottom classification system performance for the Cairns area, Great Barier Reef, Australia, Continental Shelf Research 19, 1577-1597.
- 4. Kozaczka E., Grelowska G., Kozaczka S. (2012a), Searching of the buried objects in the sea bottom by means of noninvasive methods, Proceedings of the 11th European Conference on Underwater Acoustics.
- 5. Kozaczka E., Grelowska G., Kozaczka S., Szymczak W. (2012b), Processing data on sea bottom structure obtained by means of the parametric sounding, Polish Maritime Research, 19, 4(76), 3-10.
- 6. Sternlicht D. D., Moustier Ch. P. (2003), Time dependent seafloor acoustic backscatter (10-100) kHz, J. Acoust. Soc. Am., 114, 2709-2723.
- 7. Turgut A. (1998), Method and apparatus of classifying marine sediment, Technical Report U.S.
- 8. Uscinowicz S., Zachowicz J. (1994), Geological map of the bottom of the Baltic Sea, 8 sheets and pamphlet, scale 1:200,000, Polish Geological Institute, Warsaw.
- 9. Walter D., Lambert D., Young D., Stephens K. (1997), Mapping sediment acoustic impedance using remote sensing acoustic techniques in a shallow-water carbonate environment, Geo-Marine Letters, 17, 260-267.
- 10. Wunderlich J., Müller S. (2003), High-resolution sub-bottom profiling using parametric acoustics, International Ocean Systems, 7, 4, 6-11.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-7bc252a4-402e-4772-83c5-6538a2b17587
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