FAST HANKEL TRANSFORMS*

IF 1.8 3区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
H. K. JOHANSEN, K. SØRENSEN
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引用次数: 174

Abstract

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 (K0)/r) · exp (−ρω0/Δ), Δ being the logarthmic sampling distance.

Due to the explicit expansions of H* the tails of the infinite summation

((mn)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).

Abstract Image

快速汉克尔变换*
受1970年d.p. Ghosh引入的线性滤波方法的启发,我们发展了一种用于数值计算Hankel型积分的一般理论:用sinsh (x) =a·sin (ρx)/sinh (ρx)代替通常的正弦插值函数,其中平滑参数a选择为“小”,我们得到sinsh响应或滤波函数H*的显式级数展开。如果已知输入函数f(λ exp (iω))在o <区域内是解析函数;λ& lt;∞,|ω|≤ω0时,我们可以证明输出函数上的绝对误差小于(K(ω0)/r)·exp(−ρω0/Δ), Δ为对数采样距离。由于H*的显式展开,无限求和((m−n)Δ)的尾部可以解析处理。因为对顺序的唯一限制是ν >−1,傅里叶变换是理论的一个特例,ν=±1/2分别给出正弦和余弦变换。在理论模型计算中,该方法比快速傅里叶变换(FFT)有效得多。
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来源期刊
Geophysical Prospecting
Geophysical Prospecting 地学-地球化学与地球物理
CiteScore
4.90
自引率
11.50%
发文量
118
审稿时长
4.5 months
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.
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