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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The appendix contains material on notations for stress; strain and elastic constants; vector form of wave equations; and curvilinear orthogonal coordinates. Journal of Geophysical Research 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.

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

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

This is very well documented in Wang They used the Kolsky model as a reference model. Please click the link in that email to activate your subscription. Sometimes, we also use a cookie to keep track of your trolley contents. Views Read Edit View history. 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.

Stress Waves in Solids (Dover Books on Physics) by Kolsky, H

For example, at loot. Cookies come in two flavours – persistent and transient. When the expiry date is reached your computer deletes the cookie. But then the Kolsky’s modified model comes to our rescue, producing an accurate representation of the velocity dispersion within the seismic frequency band.

Studia Geophysica et Geodaetica 46, Oslids doesn’t mean that anyone who uses your computer can access your account information as we separate association what the cookie provides from authentication. 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. Included in this material are discussions of the components of stress and strain; Hooke’s law; Rayleigh waves; reflection and refraction of elastic kolsly vibrations of rods; the Pochhammer equation; propagation of an elastic pulse along cylindrical, conical, and non-circular bars; ultrasonic measurements; and other sub-topics.


Reprint of the corrected edition. Retrieved from ” https: If you have persistent cookies enabled as well, then we will be able to remember you across browser restarts and computer reboots. This functions can be regarded as a Q-model. Where c r and Q r are the phase velocity and the Q value at a reference frequency w r.

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Persistent cookies are stored on your hard disk and have a pre-defined expiry date. 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. By using this site, you agree to the Terms of Use and Privacy Policy. Authentication ends after about 15 minutues of inactivity, or when you explicitly choose to end it.

This book is also available as a Google book: 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.

From Wikipedia, the free encyclopedia. Transient cookies are kept in RAM and are deleted either when you close all your browser windows, or when you reboot your computer. The basic Kolsky model is presented in Kolsky’s book “Stress waves in solids” that are available as a Google book.

For each of the Q models Ursin B. In both cases you should know how to switch cookies back on! Stress Waves in Solids By: We never store sensitive information about our customers in cookies. waevs

The Wavez basic model and modified model for attenuation and dispersion is the mathematical Q models that is most used in seismic applications. 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.


In his outline Wang calls the Kolsky-Futterman model the Kolsky model. The theoretical background for mathematical Q models can be found in the Wikipedia article: The choice of w r as the lowest frequency in the frequency band will introduce phase errors when oslids use the Kolsky model as an inverse Q filter.

This page was last edited stres 18 Julyetress Subscribe to our newsletter Some error text Name. A new bibliography of post literature is appended. Please refer to our privacy policy for more information on privacy at Loot. Wavws Then we can get a correct solution with inverse Q filtering with the Kolsky model. All mainstream modern browsers have cookies enabled 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.

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 correlated with experimental material.


Let’s connect Contact Details Facebook Twitter. 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. The first part, Elastic Waves, covers propagation in both an extended and a bounded plastic medium and experimental investigations with elastic materials.

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.

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. Email address subscribed successfully.