Abstract
The results of the numerical simulation of geological processes that differ by ten orders of magnitude in flow rate are presented. In one case, it is the gold placer dynamics in a river valley. In another case, it is the rapid movement of the ice-debris mudflow. In both cases, the moving material was considered as an independent flow of solid particles free from host rocks. In order to mathematically describe such a solid flow, a system of viscous compressible fluid flow equations is used. The comparison of the results of the numerical experiments with field data for the real placer and mudflow has shown their sufficient similarity.
Sign-in/Register to access full text options 
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.
