Creep properties and constitutive model of diabase in deep water conveyance tunnels

IF 5
Deep Underground Science and Engineering Pub Date : 2026-06-26 Epub Date: 2025-04-29 DOI:10.1002/dug2.70022
Zhigang Tao, Pengxiao Guan, Xiaojie Yang, Keyuan Liu, Mingjiu Cai, Hong Yang
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Abstract

Aiming at the creep characteristics of the surrounding rock of the Haidong water conveyance tunnel of the Central Yunnan water diversion project and taking the diabase at the tunnel fault zone as the research object, compression creep tests were conducted under a range of confining pressures, revealing the axial and lateral creep characteristics of diabase. Based on the theory of fractional derivative, a nonconstant coefficient Abel dashpot considering damage was established, and the simplified equation form was used to facilitate parameter identification and calculation. By combining a nonlinear Kelvin model, a classical element model, and a simplified Abel dashpot that accounts for damage effects, a constitutive model was established to describe the diabase creep process. The constitutive relations for one-dimensional and three-dimensional creep were provided. The results show that the sample exhibits both a decay creep stage and a steady-state creep stage when the stress level is below the diabase's stress threshold; when the stress level surpasses the threshold, the sample goes through an accelerated creep stage with a quickly growing creep rate and ultimately fails. Diabase mostly experiences axial creep deformation at low-stress conditions, followed by more significant lateral creep deformation under high-stress conditions. Comparing the triaxial compression creep test curve with the theoretical curve revealed that the model more accurately characterized the nonlinear creep properties of diabase.

Abstract Image

深水输水隧道中辉绿岩蠕变特性及本构模型
针对滇中引水工程海东输水隧洞围岩蠕变特征,以隧洞断裂带辉绿岩为研究对象,在一定围压条件下进行了压缩蠕变试验,揭示了辉绿岩轴向和侧向蠕变特征。基于分数阶导数理论,建立了考虑损伤的非常系数阿贝尔阻尼器,并采用简化方程形式进行参数辨识和计算。将非线性Kelvin模型、经典单元模型和考虑损伤效应的简化Abel阻尼模型相结合,建立了辉绿岩蠕变过程的本构模型。给出了一维和三维蠕变的本构关系。结果表明:当应力水平低于辉绿岩的应力阈值时,试样表现为衰减蠕变阶段和稳态蠕变阶段;当应力水平超过阈值后,试样进入加速蠕变阶段,蠕变速率快速增长,最终破坏。辉绿岩在低应力条件下以轴向蠕变为主,在高应力条件下以横向蠕变为主。将三轴压缩蠕变试验曲线与理论曲线进行比较,表明该模型更准确地表征了辉绿岩的非线性蠕变特性。
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