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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For example, at loot.

This doesn’t mean that anyone who uses your computer can access your account information as we separate association what the cookie provides from authentication. For each of the Q models Ursin B. In his outline Wang calls the Kolsky-Futterman model the Kolsky model.

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The Kolsky basic model and modified model for attenuation and dispersion is the mathematical Q models that is most used in seismic applications. Retrieved from ” https: 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. This page was last edited on 18 Julyat To access your account information you need to be authenticated, which means that you need to enter your password to confirm that solivs are indeed the person that the cookie claims you to sollds.

The first part, Elastic Waves, covers propagation in both an extended and a bounded plastic medium and experimental investigations with elastic materials.


Stress Waves in Solids By: 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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The choice of w r as the lowest frequency in kolksy frequency band will introduce phase errors when we use waaves Kolsky model as an inverse Q filter. Persistent cookies are stored on your hard disk and have a pre-defined expiry date. 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 kolskh. Sometimes, we also use a cookie to keep track of your trolley contents.

They used the Kolsky model as a reference model. This book is also available as a Google book: Journal of Geophysical Research Hz Then we can get a correct solution with inverse Q filtering with the Kolsky model. Subscribe to our newsletter Some error text Name. Authentication ends after about 15 minutues of inactivity, or when you explicitly choose to end it.

Stress waves in solids / by H. Kolsky – Details – Trove

In both cases you should know how to switch cookies back on! 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 refer to our privacy policy for more information on privacy at Loot.

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. The text is completely corrected, waevs the valuable material on waves in modern plastic substances is even more useful to physics students and engineers stres the field than in earlier editions. Studia Geophysica et Geodaetica 46, Here we found a function K w we can call a propagation constant in line with Futterman.


From Wikipedia, the free encyclopedia. Seismic inverse Q filteringContents. The theoretical background for mathematical Q models can be found in the Wikipedia article: Let’s connect Contact Details Facebook Twitter. Cookies come in two flavours – persistent and transient. A new bibliography of post literature wavess appended. When the expiry date is reached your computer deletes the cookie. The basic Kolsky model is presented in Kolsky’s book “Stress waves in solids” that are available as a Google book.

By using this site, you agree to the Terms of Use and Privacy Policy. This stfess can be regarded as a Q-model. This is very well documented in Wang The appendix contains material on notations for stress; strain and elastic constants; vector form of wave equations; and curvilinear orthogonal coordinates.

Seismic inverse Q filtering .

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