含水煤系沉积岩压实阶段非线性变形损伤本构模型研究

Weinan Wang , Qiangling Yao , Aiwen Wang , Karen A. Hudson-Edwards , Chuangkai Zheng , Lun Yan , Lianpeng Dai , Yihong Liu
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引用次数: 0

摘要

工程煤系沉积岩(包括煤岩矿柱、水库岸坡、煤矿地下水库边界富水隧道)的反复浸没疲劳损伤问题对其稳定性、安全性和运行具有深远的影响,甚至可能导致地质灾害。为了解决这一问题,本文旨在建立一个准确捕捉含水煤系沉积岩变形破坏综合过程的本构模型。探讨了这些地层的变形特征,为水岩相互作用诱发地质灾害的数值模拟提供了理论基础。在考虑浸没循环影响的情况下,综合考虑了煤系沉积岩中孔隙和基质的变形机制。随后,建立了分段本构模型,描述了单轴压缩下循环浸没含水煤系沉积岩的变形破坏全过程。通过与实验研究结果和已有相似模型的理论曲线的比较,验证了所提模型的准确性和合理性。结果表明,该模型在描述非致密含水煤系沉积岩在单轴压缩或低围压下达到峰值应力之前的变形行为方面是有效的,尽管可能需要进一步改进以精确捕捉峰后变形特征。随着浸泡次数的增加,孔隙的弹性模量(Ev)和与微量元素的平均强度相关的参数(F0)呈指数下降,而孔隙之间的变形量(γ0)则呈指数增长。均匀度(m)没有明显的规律。这些研究成果为水-岩相互作用下工程煤系沉积岩的稳定性控制及相关地质灾害的防治提供了有价值的见解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Study of a damage constitutive model for water-bearing coal measures sedimentary rock with nonlinear deformation during compaction stage

The problem of repeated immersion-induced fatigue damage in engineering coal measures sedimentary rock, including coal-rock pillars, reservoir bank slopes, and water-rich tunnels at the boundary of coal mine underground reservoirs, has profound implications for their stability, safety, and operation, and can even lead to geological disasters. To address this issue, this paper aims to construct a constitutive model that accurately captures the comprehensive process of deformation and failure in water-bearing coal measures sedimentary rock. It explores the deformation characteristics of these formations and provides a theoretical foundation for numerical simulations of geological disasters induced by water-rock interaction. This study integrates the deformation mechanisms of void and matrix deformation in coal seam sedimentary rocks, while considering the influence of immersion cycles. Subsequently, it formulates a segmented constitutive model to depict the entire process of deformation and failure in cyclically immersed water-bearing coal measures sedimentary rock under uniaxial compression. The proposed model's accuracy and rationality are validated through comparisons with experimental research findings and existing theoretical curves from similar models. The results demonstrate the model's effectiveness in describing the deformation behavior of non-dense water-bearing coal measures sedimentary rock under uniaxial compression or low confining pressure before reaching peak stress, although further refinements may be necessary to precisely capture post-peak deformation characteristics. Model parameters, including the deformation caused by voids (γ0) between voids, increase exponentially with immersion times, while the elastic modulus (Ev) of voids and the parameter (F0) related to the average strength of microelements decrease exponentially. The homogeneity degree (m) exhibits no discernible pattern. These research outcomes provide valuable insights for the stability control of engineering coal measures sedimentary rock under water-rock interaction and the mitigation of related geological disasters.

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