{"title":"快速汉克尔变换*","authors":"H. K. JOHANSEN, K. SØRENSEN","doi":"10.1111/j.1365-2478.1979.tb01005.x","DOIUrl":null,"url":null,"abstract":"<div>\n \n <p>Inspired by the linear filter method introduced by D. P. Ghosh in 1970 we have developed a general theory for numerical evaluation of integrals of the Hankel type:</p>\n <p>\n </p><div><span></span><span></span></div>\n \n <p>Replacing the usual sine interpolating function by sinsh (<i>x</i>) =<i>a</i>· sin (ρ<i>x</i>)/sinh (<i>a</i>ρ<i>x</i>), where the smoothness parameter <i>a</i> is chosen to be “small”, we obtain explicit series expansions for the sinsh-response or filter function <i>H</i>*.</p>\n <p>If the input function <i>f</i>(λ exp (iω)) is known to be analytic in the region o < λ < ∞, |ω|≤ω<sub>0</sub> of the complex plane, we can show that the absolute error on the output function is less than (<i>K</i>(ω<sub>0</sub>)/<i>r</i>) · exp (−ρω<sub>0</sub>/Δ), Δ being the logarthmic sampling distance.</p>\n <p>Due to the explicit expansions of <i>H</i>* the tails of the infinite summation \n </p><div><span></span><span></span></div>\n ((<i>m</i>−<i>n</i>)Δ) can be handled analytically.\n <p>Since the only restriction on the order is ν > − 1, the Fourier transform is a special case of the theory, ν=± 1/2 giving the sine- and cosine transform, respectively. In theoretical model calculations the present method is considerably more efficient than the Fast Fourier Transform (FFT).</p>\n </div>","PeriodicalId":12793,"journal":{"name":"Geophysical Prospecting","volume":"27 4","pages":"876-901"},"PeriodicalIF":1.8000,"publicationDate":"1979-12-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1111/j.1365-2478.1979.tb01005.x","citationCount":"174","resultStr":"{\"title\":\"FAST HANKEL TRANSFORMS*\",\"authors\":\"H. K. JOHANSEN, K. SØRENSEN\",\"doi\":\"10.1111/j.1365-2478.1979.tb01005.x\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div>\\n \\n <p>Inspired by the linear filter method introduced by D. P. Ghosh in 1970 we have developed a general theory for numerical evaluation of integrals of the Hankel type:</p>\\n <p>\\n </p><div><span></span><span></span></div>\\n \\n <p>Replacing the usual sine interpolating function by sinsh (<i>x</i>) =<i>a</i>· sin (ρ<i>x</i>)/sinh (<i>a</i>ρ<i>x</i>), where the smoothness parameter <i>a</i> is chosen to be “small”, we obtain explicit series expansions for the sinsh-response or filter function <i>H</i>*.</p>\\n <p>If the input function <i>f</i>(λ exp (iω)) is known to be analytic in the region o < λ < ∞, |ω|≤ω<sub>0</sub> of the complex plane, we can show that the absolute error on the output function is less than (<i>K</i>(ω<sub>0</sub>)/<i>r</i>) · exp (−ρω<sub>0</sub>/Δ), Δ being the logarthmic sampling distance.</p>\\n <p>Due to the explicit expansions of <i>H</i>* the tails of the infinite summation \\n </p><div><span></span><span></span></div>\\n ((<i>m</i>−<i>n</i>)Δ) can be handled analytically.\\n <p>Since the only restriction on the order is ν > − 1, the Fourier transform is a special case of the theory, ν=± 1/2 giving the sine- and cosine transform, respectively. In theoretical model calculations the present method is considerably more efficient than the Fast Fourier Transform (FFT).</p>\\n </div>\",\"PeriodicalId\":12793,\"journal\":{\"name\":\"Geophysical Prospecting\",\"volume\":\"27 4\",\"pages\":\"876-901\"},\"PeriodicalIF\":1.8000,\"publicationDate\":\"1979-12-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://sci-hub-pdf.com/10.1111/j.1365-2478.1979.tb01005.x\",\"citationCount\":\"174\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geophysical Prospecting\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1111/j.1365-2478.1979.tb01005.x\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geophysical Prospecting","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1111/j.1365-2478.1979.tb01005.x","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Inspired by the linear filter method introduced by D. P. Ghosh in 1970 we have developed a general theory for numerical evaluation of integrals of the Hankel type:
Replacing the usual sine interpolating function by sinsh (x) =a· sin (ρx)/sinh (aρx), where the smoothness parameter a is chosen to be “small”, we obtain explicit series expansions for the sinsh-response or filter function H*.
If the input function f(λ exp (iω)) is known to be analytic in the region o < λ < ∞, |ω|≤ω0 of the complex plane, we can show that the absolute error on the output function is less than (K(ω0)/r) · exp (−ρω0/Δ), Δ being the logarthmic sampling distance.
Due to the explicit expansions of H* the tails of the infinite summation
((m−n)Δ) can be handled analytically.
Since the only restriction on the order is ν > − 1, the Fourier transform is a special case of the theory, ν=± 1/2 giving the sine- and cosine transform, respectively. In theoretical model calculations the present method is considerably more efficient than the Fast Fourier Transform (FFT).
期刊介绍:
Geophysical Prospecting publishes the best in primary research on the science of geophysics as it applies to the exploration, evaluation and extraction of earth resources. Drawing heavily on contributions from researchers in the oil and mineral exploration industries, the journal has a very practical slant. Although the journal provides a valuable forum for communication among workers in these fields, it is also ideally suited to researchers in academic geophysics.