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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Here we found a function K w we can call a propagation constant in line with Futterman.

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. Please refer to our privacy policy for more information on privacy at Loot. Studia Geophysica et Geodaetica 46, 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.

In his outline Wang calls the Kolsky-Futterman model the Kolsky model. Views Read Edit View history. Email address subscribed successfully.

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

The basic Kolsky model is presented in Kolsky’s book “Stress waves in solids” that are available as a Google book. We never store sensitive information about our customers in cookies. The first part, Elastic Waves, covers propagation in both an extended and a bounded plastic medium and experimental investigations with elastic materials.

The text is completely corrected, and the valuable material on waves in modern plastic substances is even more useful to physics students and engineers in the field than in earlier editions.


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Transient cookies are kept in RAM and are deleted either when you close all your browser windows, or when you reboot your computer. Product Description Product Details The theory of the propagation of waves in solids was developed during the 19th century but, in the first quarter of this century, it fell into neglect. Authentication ends after about 15 minutues kolaky inactivity, or when you explicitly choose to end it. Subscribe to our stresss Some error text Name.

In both cases you should know how to switch cookies back on! The appendix contains material on notations for stress; strain and elastic constants; vector form of wave equations; and curvilinear orthogonal coordinates.

The author, who has taught applied physics on the college level for many years, gives a concise account 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 work of recent years.

They used the Kolsky model as a reference model. When the expiry date is reached your computer deletes the cookie. A new bibliography of post literature is appended.

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. 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.

Included in this material are kolky of the components of stress and strain; Hooke’s law; Rayleigh waves; reflection and refraction of elastic waves; vibrations of rods; the Pochhammer equation; wwaves of an elastic pulse along cylindrical, conical, and non-circular bars; ultrasonic measurements; and other sub-topics.


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.

Stress Waves in Solids

Seismic inverse Q filteringContents. Let’s connect Contact Details Facebook Twitter.

Only recently, as the result of new techniques of study and the development of new plastics and other such materials, has it again become the object of intensive investigation. Seismic inverse Q filtering. This functions kolwky be regarded as a Q-model.

Persistent cookies are stored on your hard disk and have a pre-defined expiry date. From Wikipedia, the free encyclopedia. This page was last edited on 18 Julyat But then the Kolsky’s modified model comes to our rescue, producing an accurate representation of the velocity dispersion within the seismic frequency band.

Please click the link in that email to activate kolsly subscription. Reprint of the corrected edition. Cookies come in two flavours – persistent and transient. Journal of Geophysical Research A activation email has been sent to you. Where c r and Q r are the phase velocity and the Q value at a reference frequency w r.

All mainstream modern browsers have cookies solirs by default, so if you’ve been directed to this page it probably means you’re uisng a weird and wonderful browser of your own choosing, or have disabled cookies yourself. The strwss background for mathematical Q models can be found in the Wikipedia article: