Dependence of resolvable limit on frequency
A wavelet has a flat frequency spectrum from 0 to above which no frequencies are present. Show that the Rayleigh criterion gives a resolvable limit , where .
A reflecting layer is said to be resolvable if we can distinguish between the reflections from the top and bottom of the layer, usually on the basis of a phase break in the superimposed reflections (see Figure 6.18a). The Rayleigh criterion for vertical resolution states that at least a small depression must appear between successive events in order to recognize that more than one event is present. For this to occur the two reflections must be separated by at least a half-cycle; this corresponds to a minimum thickness of , the two-way thickness then being . This thickness of is called the tuning thickness or resolvable limit.
A boxcar (see Figure 6.18b) is a function whose value is unity within a certain range and zero outside this range (see problem 9.3).
The frequency spectrum is a boxcar extending from , shown in Figure 6.18b, which we write as . The inverse transform of the spectrum is given by equation (9.3d), namely
The Rayleigh criterion gives a resolvable limit corresponding to the first trough (minimum) of the time-domain representation of the boxcar. Hence, we equate the derivative of the sinc function to zero, obtaining
This gives , that is, we must solve the equation where . A graphical solution gives , hence .
Show that the value of for a wavelet with a flat spectrum extending from to (that is, octaves where ) is given by the solution of the equation,
The time-domain function corresponding to the spectrum in Figure 6.18c is
To get the first trough, we write , then equate to zero the derivative of with respect to . This gives
Solve the equation in part (b) for and 1, that is, for bandwidths of 3, 2, 1.5, and 1 octaves, and compare the relation between and .
For , and we have from equation (6.18c)
For , we get , but for slightly greater than zero, is negative and continues to be negative until it changes sign for between 0.5 and 0.6; The corresponding root is , giving .
When , , the root of equation (6.18c) is , giving . For , and the root is , so . For , and the root is , so .
Noting that part (a) involves an infinite number of octaves, what bandwidth is required to give nearly the same result?
The resolution in part (a) is expressed in terms of while those in (c) are in terms of . To compare the results we equate to , so that we have four frequency bands, each with top frequency and extending downward 1, 1.5, 2, 3, and an infinite number of octaves. This means that the values of in (c) must be adjusted to get in the denominator, e.g.,for , . The results are shown in Table 6.18a.
Thus, three octaves bandwidth () gives almost as good resolution as an infinite number of octaves but the resolution deteriorates for band-widths octaves.
|Destructive and constructive interference for a wedge
|Geometry of seismic waves
|Characteristics of seismic events
Also in this chapter
- Characteristics of different types of events and noise
- Horizontal resolution
- Reflection and refraction laws and Fermat’s principle
- Effect of reflector curvature on a plane wave
- Diffraction traveltime curves
- Amplitude variation with offset for seafloor multiples
- Ghost amplitude and energy
- Directivity of a source plus its ghost
- Directivity of a harmonic source plus ghost
- Differential moveout between primary and multiple
- Suppressing multiples by NMO differences
- Distinguishing horizontal/vertical discontinuities
- Identification of events
- Traveltime curves for various events
- Reflections/diffractions from refractor terminations
- Refractions and refraction multiples
- Destructive and constructive interference for a wedge
- Dependence of resolvable limit on frequency
- Vertical resolution
- Causes of high-frequency losses
- Ricker wavelet relations
- Improvement of signal/noise ratio by stacking