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International Journal of Fluid Mechanics Research

Published 6 issues per year

ISSN Print: 2152-5102

ISSN Online: 2152-5110

The Impact Factor measures the average number of citations received in a particular year by papers published in the journal during the two preceding years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) IF: 1.1 To calculate the five year Impact Factor, citations are counted in 2017 to the previous five years and divided by the source items published in the previous five years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) 5-Year IF: 1.3 The Eigenfactor score, developed by Jevin West and Carl Bergstrom at the University of Washington, is a rating of the total importance of a scientific journal. Journals are rated according to the number of incoming citations, with citations from highly ranked journals weighted to make a larger contribution to the eigenfactor than those from poorly ranked journals. Eigenfactor: 0.0002 The Journal Citation Indicator (JCI) is a single measurement of the field-normalized citation impact of journals in the Web of Science Core Collection across disciplines. The key words here are that the metric is normalized and cross-disciplinary. JCI: 0.33 SJR: 0.256 SNIP: 0.49 CiteScore™:: 2.4 H-Index: 23

Indexed in

Wave Reflection from the Free Boundary of Porous-Elastic Liquid-Saturated Half-Space

Volume 32, Issue 3, 2005, pp. 327-339
DOI: 10.1615/InterJFluidMechRes.v32.i3.60
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ABSTRACT

On the basis of Biot’s theory, predicting the existence of three types of bulk waves in a porous-elastic fluid-saturated medium, the analysis of bulk wave reflection from the free boundary is conducted. The energy distribution of the incident wave between the reflected waves is found. The qualitative distinctions between energy reflection coefficients of slow longitudinal wave from the free boundaries with open and closed pores are discovered. For vertical components of period-average power flow vector the energy superposition principle occurs valid. This principle states that energy of the incident wave is equal to that of the reflected waves. There is no energy transfer by inhomogeneous waves deep into medium. However, the energy superposition principle is not correct along the boundary of the half-space.

CITED BY
  1. Arora Ashish, Tomar S.K., The effect of inertial coupling on seismic reflection amplitudes, Geophysical Prospecting, 56, 5, 2008. Crossref

  2. Yeh Chao-Lung, Lo Wei-Cheng, Jan Chyan-Deng, Yang Chi-Chin, Reflection and refraction of obliquely incident elastic waves upon the interface between two porous elastic half-spaces saturated by different fluid mixtures, Journal of Hydrology, 395, 1-2, 2010. Crossref

  3. Singh Dilbag, Tomar S.K., Wave propagation in micropolar mixture of porous media, International Journal of Engineering Science, 44, 18-19, 2006. Crossref

  4. Bala Neeru, Arora Ashish, Effect of pore connectivity on reflection amplitudes of an inhomogeneous wave in a composite porous solid saturated by two immiscible fluids, Journal of Earth System Science, 127, 4, 2018. Crossref

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