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Hankel transformations

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Book Chapter

Series: Society of Exploration Geophysicists Geophysical References Series
Published: 01 January 1999
DOI: 10.1190/1.9781560801825.ch7
EISBN: 9781560801825
... complicate things substantially. This chapter demonstrates that problems involving point sources are almost always more easily analyzed in terms of a different sort of basic function, called Bessel functions. Hankel transforms (which use Bessel functions) are introduced, using a modernized version...
Journal Article
Journal: Geophysics
Published: 05 April 2012
Geophysics (2012) 77 (3): F21–F30.
...Kerry Key ABSTRACT The fast Hankel transform (FHT) implemented with digital filters has been the algorithm of choice in EM geophysics for a few decades. However, other disciplines have predominantly relied on methods that break up the Hankel transform integral into a sum of partial integrals...
FIGURES | View All (10)
Journal Article
Journal: Geophysics
Published: 01 February 1989
Geophysics (1989) 54 (2): 263–266.
...Walter L. Anderson Abstract A hybrid fast Hankel transform algorithm has been developed that uses several complementary features of two existing algorithms: Anderson's digital filtering or fast Hankel transform (FHT) algorithm and Chave's quadrature and continued fraction algorithm. A hybrid FHT...
Journal Article
Journal: Geophysics
Published: 01 December 1983
Geophysics (1983) 48 (12): 1671–1686.
...Alan D. Chave Abstract An algorithm for the accurate evaluation of Hankel (or Bessel) transforms of algebraically related kernel functions. The algorithm performs the automatic integration of the product of the kernel and Bessel functions between the asymptotic zero crossings of the latter and sums...
Journal Article
Journal: Geophysics
Published: 01 October 1984
Geophysics (1984) 49 (10): 1811–1813.
...Walter L. Anderson; Alan D. Chave Abstract Chave presents an excellent algorithm and computer subprogram that evaluate Hankel transforms by quadrature and continued fraction summation. This subprogram would be a valuable addition to any mathematical computer library. Chave refers to digital filter...
Journal Article
Journal: Geophysics
Published: 01 October 1984
Geophysics (1984) 49 (10): 1754–1759.
...Walter L. Anderson Abstract A new method is presented that rapidly evaluates the many Green's tensor integrals encountered in three-dimensional electromagnetic modeling using an integral equation. Application of a fast Hankel transform (FHT) algorithm (Anderson, 1982) is the basis for the new...
Journal Article
Journal: Geophysics
Published: 01 July 1979
Geophysics (1979) 44 (7): 1287–1305.
...W. L. Anderson Abstract A linear digital filtering algorithm is presented for rapid and accurate numerical evaluation of Hankel transform integrals of orders 0 and 1 containing related complex kernel functions. The kernel for Hankel transforms is defined as the non-Bessel function factor...
Journal Article
Journal: Geophysics
Published: 31 March 2025
Geophysics (2025) 90 (3): KS47–KS59.
... on the ocean-bottom interface. We attempt to extract useful Scholte wave dispersion energy spectra from independent hydrophone or geophone signals of OBC systems by an extended frequency-Hankel transform method. Results show that this transform method can extract high-quality multimodal Scholte wave dispersion...
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Journal Article
Journal: Geophysics
Published: 14 February 2024
Geophysics (2024) 89 (2): KS69–KS81.
...Zhentao Yang; Yao-Chong Sun; Dazhou Zhang; Pen Han; Xiaofei Chen ABSTRACT Rayleigh wave dispersion energy spectra have been widely used to extract dispersion curves and invert underground S-wave velocity structures for engineering geophysics and seismology. We develop a frequency-Hankel (F-H...
FIGURES | View All (10)
Journal Article
Journal: Geophysics
Published: 01 October 1979
Geophysics (1979) 44 (10): 1769.
... Abstract The author of the recent computer program, “Numerical integration of related Hankel transforms of orders 0 and 1 by adaptive digital filtering” (Walter L. Anderson, Geophysics, July 1979 p. 1287–1305) wishes to correct the following errors. On p. 1290, under FUN =, the use of brackets...
Journal Article
Journal: Geophysics
Published: 01 June 1994
Geophysics (1994) 59 (6): 864–880.
... electric and magnetic sources are composed of lengths of straight wire, which may be grounded. If the source-receiver separation is large enough, the composite electrical dipoles may be considered to be infinitely small, and in a 1-D earth model the fields are expressed as Hankel transforms of an input...
Image
Error levels for different Hankel transform settings, compared with the analytical solution in Figure 1. (a) The high-precision QWE and (d) the standard FHT have very low error levels, generally in the order of 10−6% or less. The lagged FHT has much higher error levels, and the effects of interpolation can be seen clearly in the ring-like structure. However, almost the entire error is less than 0.1% (10−1%), only the dark black parts have an error of 1% or slightly more. Hankel arguments for QWE: [rel. tol., abs. tol., nr of pts]; for splined FHT: [pts/decade].
Published: 21 August 2017
Figure 2. Error levels for different Hankel transform settings, compared with the analytical solution in Figure  1 . (a) The high-precision QWE and (d) the standard FHT have very low error levels, generally in the order of 10 − 6 % or less. The lagged FHT has much higher error
Image
Inphase and quadrature responses calculated using the fast Hankel transform for 100 frequencies between f=20  kHz and 200 kHz with no shift (dashed lines), best shift (solid lines), and worst shift (dotted lines) of the discrete wavenumbers. The bold solid lines show the quasistatic results. The system parameters are as before.
Published: 09 July 2012
Figure 3. Inphase and quadrature responses calculated using the fast Hankel transform for 100 frequencies between f = 20     kHz and 200 kHz with no shift (dashed lines), best shift (solid lines), and worst shift (dotted lines) of the discrete wavenumbers. The bold solid lines show
Image
Comparison of the best results obtained with fast Hankel transform (FHT, solid lines) and numerical Laplace transform (NLT, dashed lines). The bold solid lines show the quasistatic results. The figure shows that both transforms result in the same response when similar corrections procedures (wavenumber optimization and/or partial integration) are applied to the integration process. The system parameters are the same as before.
Published: 09 July 2012
Figure 10. Comparison of the best results obtained with fast Hankel transform (FHT, solid lines) and numerical Laplace transform (NLT, dashed lines). The bold solid lines show the quasistatic results. The figure shows that both transforms result in the same response when similar corrections
Image
Comparison of the fast Hankel transform and the QWE method for marine CSEM computations. The top panel shows the relative error as a function of offset for 51, 101, and 201-point digital filters and for the QWE approach using five, seven, and nine-point quadrature. The middle panel shows the number of kernel evaluations required by each and the bottom panel shows the corresponding run-times required for each offset.
Published: 05 April 2012
Figure 5. Comparison of the fast Hankel transform and the QWE method for marine CSEM computations. The top panel shows the relative error as a function of offset for 51, 101, and 201-point digital filters and for the QWE approach using five, seven, and nine-point quadrature. The middle panel
Journal Article
Journal: Geophysics
Published: 01 June 1987
Geophysics (1987) 52 (6): 785–793.
... of a vertical magnetic dipole is inverse Laplace transformed into the time domain, for selected values of the Hankel transform variable, using the Gaver-Stehfest method. After interpolation, the result is inverse Hankel transformed (for selected values of distance) using digital filters. Interpolating over...
Journal Article
Journal: Geophysics
Published: 01 October 1990
Geophysics (1990) 55 (10): 1380–1385.
...M. Dietrich Abstract The correct formulation of the plane-wave decomposition of point-source seismograms involves a sequence of Fourier and Hankel transforms which can be evaluated in several ways. The procedure which is proposed here exploits the fact that the plane-wave response is bandlimited...
Book Chapter

Series: Society of Exploration Geophysicists Geophysical References Series
Published: 01 January 1999
DOI: 10.1190/1.9781560801825.ch8
EISBN: 9781560801825
... coordinates. In the following we discuss spatial multiplication and spectral convolution in terms of polar coordinates. Hankel transforms evolved from the Hankel expansion [equations (468) or (478)]. We now coordinate these as the Fourier transform pair which tells us the Hankel expansion coefficients...
Journal Article
Journal: Geophysics
Published: 05 March 2019
Geophysics (2019) 84 (2): F47–F56.
...Dieter Werthmüller; Kerry Key; Evert C. Slob ABSTRACT The open-source code fdesign makes it possible to design digital linear filters for the Hankel and Fourier transforms used in potential, diffusive, and wavefield modeling. Digital filters can be derived for any electromagnetic (EM) method...
FIGURES | View All (11)
Journal Article
Journal: Geophysics
Published: 21 August 2017
Geophysics (2017) 82 (6): WB9–WB19.
...Figure 2. Error levels for different Hankel transform settings, compared with the analytical solution in Figure  1 . (a) The high-precision QWE and (d) the standard FHT have very low error levels, generally in the order of 10 − 6 % or less. The lagged FHT has much higher error...
FIGURES | View All (8)