Abstract
An original experimental apparatus developed at the Geothermometry Laboratory of the Faculty of Physics of the MSU was used to measure the thermal diffusivity of several mantle minerals over a wide temperature range, extending up to the melting point. Application of the temperature wave method made it possible to account for the radiative heat transfer from the sample surface into ambient space and, thus, to achieve high accuracy in measuring this important thermal characteristic for each substance.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Disclaimer: 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.