Abstract
This paper presents a stochastic, discrete fracture model to investigate the distance‐dependent dispersion phenomenon in fractured rock. Under imposed boundary conditions, the dispersion behavior of particles is observed. Simulated results demonstrate that the coefficient of anisotropic dispersion tensor increases with an increasing traveled distance. The anisotropic ratio of dispersion tensor is small and almost increased linearly with migration distance at early migration. The anisotropic ratio has the trend to maintain constant or small variation after a specifietl migration distance. It was also noted that the plume of particles is elliptic.
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.
