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УДК 539 This content has been downloaded from IOPscience Please scroll down to see the full text Download details IP Address 95 181 218 166 This content was downloaded on 13/02/2017 at 08 10 Please no[.]

Home Search Collections Journals About Contact us My IOPscience Energy flows in rock mass under tidal deformation This content has been downloaded from IOPscience Please scroll down to see the full text 2017 IOP Conf Ser.: Earth Environ Sci 53 012002 (http://iopscience.iop.org/1755-1315/53/1/012002) View the table of contents for this issue, or go to the journal homepage for more Download details: IP Address: 95.181.218.166 This content was downloaded on 13/02/2017 at 08:10 Please note that terms and conditions apply You may also be interested in: Comparing kinematically detachable rock masses and rockfall scar volumes O Mavrouli and J Corominas Charge and energy flows in ionised thymidine S Maclot, R Delaunay, D G Piekarski et al Permeability estimation of jointed rock mass using fractal network model S-J Li and Y-X Liu Combined identification of constitutive parameters and in-situ stress in layered rock mass formulated by Cosserat theory H T Yang and K Wang Stream function for optical energy flow M V Berry and M R Dennis Effect of Radial Density Configuration on Wave Field and Energy Flow in Axially Uniform Helicon Plasma Chang Lei, Li Qingchong, Zhang Huijie et al Energy flow around a moving dislocation H Koizumi and H O K Kirchner ENVELOPING ALGEBRAS AND DEFORMATIONS V A Ginzburg Concerning the path of light upon total reflection Hans Wolter MSBA IOP Conf Series: Earth and Environmental Science 53 (2017) 012002 IOP Publishing doi:10.1088/1755-1315/53/1/012002 International Conference on Recent Trends in Physics 2016 (ICRTP2016) IOP Publishing Journal of Physics: Conference Series 755 (2016) 011001 doi:10.1088/1742-6596/755/1/011001 Energy flows in rock mass under tidal deformation SV Klishin* and AF Revuzhenko Chinakal Institute of Mining, Siberian Branch, Russian Academy of Sciences, Novosibirsk, Russia E-mail: *sv.klishin@gmail.com Abstract Under analysis is the stress state of an elliptical domain under varying loading conditions The energy flow lines are plotted The paper demonstrates the effect of the boundary conditions on the shape of the flow lines Tidal deformation of the Earth is a global process It exerts influence, in a varying degree, on all geological processes on the planet: evolution of stresses in the interior of the Earth, including mineral mining depths, mass transfer, deformation of blocks on different scales, behavior of interface areas between the blocks, etc [1] Investigation and understanding of the tidal deformation of the Earth is an interesting challenge at this time Tidal deformation is connected with the energy physics On the whole, tidal deformation is induced by kinetic energy of rotation of the Earth Transformation of the energy of rotation into the energy of deformation of the solid and viscous Earth results in deceleration of Earth’s rotation and in elongation of the day length In kinematic models of tides, energy flows through the boundary of a body This energy, in a specified approximation, ensures the same kinematics of mass movement as in deformation under body forces It seems interesting to address energy flows in these situations Let the Cartesian coordinate system Oxy contain an elliptical domain with a center (0, 0) and axes oriented along the axes Ox and Oy x2 y2  1 , (1  m) (1  m) (1) where ≤ m

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