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Civil-Comp Proceedings
ISSN 1759-3433 CCP: 100
PROCEEDINGS OF THE EIGHTH INTERNATIONAL CONFERENCE ON ENGINEERING COMPUTATIONAL TECHNOLOGY Edited by: B.H.V. Topping
Paper 110
Simulation of the Long-Term Behaviour of an Underground Structure in Rock Salt A. Pudewills
Karlsruhe Institute of Technology, Institute for Nuclear Waste Disposal, (KIT-INE), Eggenstein-Leopoldshafen, Germany A. Pudewills, "Simulation of the Long-Term Behaviour of an Underground Structure in Rock Salt", in B.H.V. Topping, (Editor), "Proceedings of the Eighth International Conference on Engineering Computational Technology", Civil-Comp Press, Stirlingshire, UK, Paper 110, 2012. doi:10.4203/ccp.100.110
Keywords: constitutive model, finite element modelling, rock salt, underground structures.
Summary
Within the frame of a national joint research project, five participants performed benchmark like calculations on a three-dimensional underground structure in the rock salt of the Angersdorf mine in northern Germany [1]. The aim of the project was to evaluate the ability of the models to correctly describe the relevant deformation phenomena in rock salt under various influences, (i.e. transient and steady-state creep, the evolution of dilatancy and damage, short-term failure and long-term creep failure, post-failure behaviour and residual strength) and to increase confidence in the results of numerical simulations and enhance the acceptance of the results.
In our institute the finite element code ADINA was used to study the mechanical behaviour of rock salt [2]. A new viscoplastic constitutive model for rock salt that can describe the volumetric strain (dilatancy) and the damage of the rock salt has been proposed and implemented in this code [3]. The model parameters for the numerical simulation have been evaluated on the available laboratory experiments [4,5]. The Angersdorf salt mine consists of a regular pattern of large rooms and pillars at a depth of about 530 m. Therefore, a three-dimensional vertical section was chosen as a representative model. In the first step of the calculations, the initial state of stress taking into account the creep behaviour of the rock salt and the clay layer has been determined. After excavation of the main room and different drifts the calculations have been continued over 100 years. The benchmark results and the comparison of several results with in situ measurements have shown that the numerical model is able to describe the main behaviour of the rock salt such as transient and steady-state creep, dilatancy and material damage around underground openings. A comparison of calculation results from five project partners was performed in a number of papers [1,6]. References
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