Abstract
It is experimentally established that acoustic waves in rocks attenuate abnormally depending on varying amplitude. The amplitude growth results in the increase in elastic wave velocities and decrease in the attenuation decrement. The attenuation rather than wave velocity is more sensitive to the amplitude variations. The obtained data are applicable to diagnose the states of fractured and porous rocks.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
