RESPONSE OF SOFT SEDIMENTS AT SEA BOTTOM TO SOUND WAVES

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DC Field	Value	Language
dc.contributor.author	Yadav, Mohit	-
dc.date.accessioned	2025-06-25T12:53:18Z	-
dc.date.available	2025-06-25T12:53:18Z	-
dc.date.issued	2014-06	-
dc.identifier.uri	http://localhost:8081/jspui/handle/123456789/17136	-
dc.description.abstract	Different kinds of sediments occur on the sea floor. Sound waves provide the best means of exploring the nature of these sediments. When sound waves are incident at the surface of these sediments they are reflected as well as scattered. The reflection coefficients as a function of angle of incidence have been computed for different kind of sediments vatying from clay to coarse sand. It has been found that in general reflection coefficients are higher when the wave velocities in the sediments are greater. Scattering of sound waves is a function of frequency. The scattered energy decrease as frequency increases	en_US
dc.description.sponsorship	INDIAN INSTITUTE OF TECHNOLOGY ROORKEE	en_US
dc.language.iso	en	en_US
dc.publisher	I I T ROORKEE	en_US
dc.subject	Different Kinds	en_US
dc.subject	Different Kinds	en_US
dc.subject	Reflection Coefficients	en_US
dc.subject	General Reflection	en_US
dc.title	RESPONSE OF SOFT SEDIMENTS AT SEA BOTTOM TO SOUND WAVES	en_US
dc.type	Other	en_US
Appears in Collections:	MASTERS' THESES (Earth Sci.)

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