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师文豪, 吴伊锋. 基于土石混合体随机重构的路基空洞地质雷达响应特征[J]. 岩土工程学报. DOI: 10.11779/CJGE20240750
引用本文: 师文豪, 吴伊锋. 基于土石混合体随机重构的路基空洞地质雷达响应特征[J]. 岩土工程学报. DOI: 10.11779/CJGE20240750
Response characteristics of ground-penetrating radar for subgrade void based on random reconstruction of soil-rock mixture[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20240750
Citation: Response characteristics of ground-penetrating radar for subgrade void based on random reconstruction of soil-rock mixture[J]. Chinese Journal of Geotechnical Engineering. DOI: 10.11779/CJGE20240750

基于土石混合体随机重构的路基空洞地质雷达响应特征

Response characteristics of ground-penetrating radar for subgrade void based on random reconstruction of soil-rock mixture

  • 摘要: 为研究非均质土石混合体对路基空洞地质雷达反射波的影响规律,利用伸缩因子函数对椭圆进行伸缩变形得到符合自然块石颗粒形状,采用随机投放和随机生长算法重构带有孔隙的土石混合体细观模型,并提出土石混合体非均匀性的评价方法,基于时域有限差分算法模拟电磁波在土石混填路基空洞的传播过程,定量计算了电磁波传播特征,揭示路基土层块石含量、孔隙度和含水率对空洞反射信号的影响规律。研究结果表明:电磁波信号在土石混填路基中的波场快照和剖面图呈现随机扰动特征,且非均匀度越大随机扰动的程度越大;块石颗粒和孔隙形成电磁波反射界面,增强空洞信号振幅;一定的块石含量可以增强空洞信号振幅,超过一定含量会对空洞信号产生衰减;孔隙度和含水率通过影响路基介质的介电常数来影响空洞反射波信号的振幅和双程走时;该研究可为非均质土石混填路基空洞识别与解释提供理论与方法支撑。

     

    Abstract: To study the influence of heterogeneous soil-rock mixtures on the ground penetrating radar reflection waves of subgrade voids, an elliptical dilation deformation using a scaling factor function was employed to create shapes resembling natural block stone particles. A random placement and growth algorithm was used to reconstruct a mesoscopic model of soil-rock mixtures with voids. A method to evaluate the heterogeneity of soil-rock mixtures was proposed. Using the Finite-Difference Time-Domain algorithm, the propagation process of electromagnetic waves in soil-rock-filled subgrade voids was simulated. The electromagnetic wave propagation characteristics were quantitatively calculated, and the influence of block stone content, porosity, and moisture content on void reflection signals was revealed. The results showed that the wave field snapshots and profiles of electromagnetic wave signals in soil-rock-filled subgrade exhibited random disturbance characteristics, with the degree of disturbance increasing with greater heterogeneity. Block stone particles and voids formed electromagnetic wave reflection interfaces, enhancing the amplitude of void signals. A certain amount of block stone content could enhance the void signal amplitude, but exceeding a certain content would attenuate the void signal. Porosity and moisture content affected the amplitude and two-way travel time of void reflection signals by influencing the dielectric constant of the subgrade medium. This study provides theoretical and methodological support for the identification and interpretation of voids in heterogeneous soil-rock-filled subgrades.

     

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