Water bottom multiple











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Three successive rebounds within the water layer, if not more, are visible and can be readily accounted for. The two interfaces, at either side of the water level, are excellent reflector.. In some areas, there occur anomalous up-hole times which are difficult to explain http. The marine section illustrated on Plate 56, from offshore Labrador, shows this kind of multiple.

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Seismic Methods And Applications

Plate The reverberation in water illustrated on this sketch corresponds to persistence of a wave sound after its source has stopped, caused by multiple reflection of the wave within a closed space in this case the water layer. Reflected refractions contain information only about the refractor. The two interfaces, at either side of the water level, are excellent reflector.. This is particularly true, on hard water-bottom areas where sediments are compacted and well consolidated. A reflection event arriving a short time after the primary from the surface or the base of weathered layer buried explosion on land. A strong reflection, culminating at approximately 2 seconds, is visible in the middle of the section. Admittedly, this line is affected by numerous multiples.

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Assuming a constant avo water

However, this is not always the case. Plate Multiply reflected seismic energy or any event in seismic data that has incurred more than one reflection in its travel path is considered a multiple. In addition to rays that return to the surface after reflection at single interface, known as primary reflection , there are many paths in a layered subsurface by which rays may return to the surface after reflection at more than one interface Plate As illustrated a peg leg multiple is a type of short-path multiple, or multiply-reflected seismic energy, which has an asymmetric path. Reflected refractions contain information only about the refractor. Diffraction refers to various phenomena which occur when a wave encounters an obstacle. Plate The reverberation in water illustrated on this sketch corresponds to persistence of a wave sound after its source has stopped, caused by multiple reflection of the wave within a closed space in this case the water layer.

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Description: The sketch illustrated on Plate 57 attempts to schematize the most probable paths, between shot point and receiver that an acoustic wave traveling through the sedimentary intervals may chose. As illustrated a peg leg multiple is a type of short-path multiple, or multiply-reflected seismic energy, which has an asymmetric path. The more frequent multiples, that is to say, reflection events having suffered more than one reflection, as illustrated on Plate 57, are.. In practice, the measured travel time is influenced by charge size, by filter setting, by instrument sensitivity, and by previous history of the shot hole. Their presence on a recorded section is due to the fact that an acoustic impedance contrast between two adjacent layers, reflects down-going waves up as well as down. In some cases, the period of the peg-leg multiple is so brief that it interferes with primary reflections, and its interference causes a loss of high frequencies in the wavelet http. In addition to rays that return to the surface after reflection at single interface, known as primary reflection , there are many paths in a layered subsurface by which rays may return to the surface after reflection at more than one interface Plate
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