On the Kramers-Kronig relations

被引:38
作者
Carcione, Jose M. [1 ,2 ]
Cavallini, Fabio [1 ]
Ba, Jing [2 ]
Cheng, Wei [2 ]
Qadrouh, Ayman N. [3 ]
机构
[1] Ist Nazl Oceanog & Geofis Sperimentale OGS, Borgo Grotta Gigante 42c, I-34010 Trieste, Italy
[2] Hohai Univ, Sch Earth Sci & Engn, Nanjing 211100, Jiangsu, Peoples R China
[3] SAC KACST, POB 6086, Riyadh 11442, Saudi Arabia
关键词
Kramers-Kronig relations; Sokhotski-Plemelj equation; Causality; Viscoelasticity; Waves; Zener model; DISPERSION;
D O I
10.1007/s00397-018-1119-3
中图分类号
O3 [力学];
学科分类号
08 ; 0801 ;
摘要
We provide a new derivation of the Kramers-Kronig relations on the basis of the Sokhotski-Plemelj equation with detailed mathematical justifications. The relations hold for a causal function, whose Fourier transform is regular (holomorphic) and square-integrable. This implies analyticity in the lower complex plane and a Fourier transform that vanishes at the high-frequency limit. In viscoelasticity, we show that the complex and frequency-dependent modulus describing the stiffness does not satisfy the relation but the modulus minus its high-frequency value does it. This is due to the fact that despite its causality, the modulus is not square-integrable due to a non-null instantaneous response. The relations are obtained in addition for the wave velocity and attenuation factor. The Zener, Maxwell, and Kelvin-Voigt viscoelastic models illustrate these properties. We verify the Kramers-Kronig relations on experimental data of sound attenuation in seabottoms sediments.
引用
收藏
页码:21 / 28
页数:8
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