Readable survey of the theoretical core of the propagation of waves in solids offers a concise account of the classical theory, considers how this theory has been. The author gives a concise account of the classical theory necessary to an understanding of the subject, considers how this theory has been extended to solids. Download Citation on ResearchGate | Stress waves in solids / by H. Kolsky | Incluye Ă­ndice }.

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This book is also available as a Google book: The theoretical background for mathematical Q models can be found in the Qaves article: Where c r and Q r are the phase velocity and the Q value at a reference frequency w r.

From Wikipedia, the free encyclopedia. To access your account information you need to be authenticated, which means that you need to enter your password to confirm that you are indeed the person that the cookie claims you to be. The Kolsky basic model and modified model for attenuation and dispersion is the mathematical Q models that is most used in seismic applications.

The choice of w r as the lowest frequency in the frequency band will introduce phase errors when we use the Kolsky model as an inverse Q filter. Views Read Edit View history. When the expiry date is reached your computer deletes the cookie.

Retrieved from ” https: The basic Kolsky model is used for its simplicity in seismic data processing, however it does not rigorously satisfy the Minimum phase criterion and cannot satisfy the Kramers—Kronig relations.

Stress Waves in Solids By: The first part, Elastic Waves, covers propagation in both an extended and a bounded plastic medium and experimental investigations with elastic materials. They used the Kolsky model as a reference model. The basic Kolsky model is presented in Kolsky’s book “Stress waves in solids” that are available as a Google book. For example, at loot. Cookies are little nuggets of information that web servers store on your computer to make it easier for them to keep track of your browsing session.


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Seismic inverse Q filtering. This book is the most readable survey of the theoretical core of current knowledge of the subject and, unlike most other studies in the field, it is fully im with experimental material.

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A activation email has been sent to you. In his outline Wang calls the Kolsky-Futterman model the Kolsky model.

The Kolsky basic model and modified model for attenuation and dispersion – Wikipedia

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A new bibliography of post literature is appended. To obtain a solution that can be applied to seismic k w must be connected to a function that represent the way the seismic wave propagates in the seismic media.

The Kolsky basic model and modified model for attenuation and dispersion

Product Description Product Details The theory of the propagation of waves in solids was developed during the 19th century but, in the first quarter kolsjy this century, it fell into neglect.


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A requirement in the theory for materials satisfying the linear attenuation assumption is that the reference frequency w r is a finite arbitrarily small but nonzero cut-off on the absorption. Only recently, as the result of new techniques of soldis and the development of new plastics and other such materials, has it again become the object of intensive investigation.

But then sokids Kolsky’s modified model comes to our rescue, producing an accurate representation of the velocity dispersion within the seismic frequency band.

This functions can be regarded as a Q-model. Email address subscribed successfully. Please refer to our privacy policy for more information on privacy at Loot. According to Kolsky, we are free to choose w r following the phenomenological criterion that it be small compared with the lowest measured frequency w in the frequency band.

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Here we found a function K w we can call a propagation constant in line with Futterman. Seismic inverse Q filteringContents. Studia Geophysica et Geodaetica 46, The author, who has taught applied physics on the college level for many years, gives a concise solixs of the classical theory necessary to an understanding of the subject, considers how this theory has been extended to solids which are not perfectly elastic, and then summarizes the important experimental solis of recent years. Reprint of the corrected edition.