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ORIGINAL RESEARCH article
Front. Earth Sci.
Sec. Petrology
Volume 13 - 2025 | doi: 10.3389/feart.2025.1577262
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In the red-bed region, engineering structures often encounter safety risks due to the swelling and creep properties of mudstone. Presently, there is a deficiency in constitutive equations capable of characterizing mudstone behavior under combined stress and swelling. To tackle this challenge, the deformation characteristics of red-bed mudstone were summarized based on the previous experimental data. A new element combination model (namely swelling-creep model), comprising a Burgers body, swelling body, and nonlinear damper, was established to describe attenuated creep, swelling deformation, and accelerated creep, respectively. Based on this, the threedimensional constitutive equations of the swelling-creep model were derived. Subsequently, based on the UDM program of FLAC 3D , the model was further developed using C++ language. Additionally, the developed swelling-creep model was validated through the numerical simulation experiments. Finally, the swelling-creep deformation process of red-bed mudstone under tensile stress conditions was simulated using the developed swelling-creep model. The research results indicate that the fitting results of the swelling-creep model are in good agreement with the experimental data, demonstrating its accuracy in describing the swelling and creep characteristics of redbed mudstone. Moreover, when red-bed mudstone is subjected to axial tensile stress, the swelling effect significantly increases the axial strain rate and accelerates the transition to the accelerated creep stage.
Keywords: red-bed mudstone, Swelling-creep, Constitutive model, numerical simulation, FLAC 3D
Received: 15 Feb 2025; Accepted: 12 Mar 2025.
Copyright: © 2025 Yan, Yu, Zhu, Yuan, Wang and Wu. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) or licensor are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
* Correspondence:
Feng Yu, Sichuan Third Geological Brigade, Sichan Chengdu, China
Disclaimer: All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article or claim that may be made by its manufacturer is not guaranteed or endorsed by the publisher.
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