用于岩土工程实验室试验应变场测量的光纤传感

G. Della Ragione, C. N. Abadie, X. Xu, T. S. da Silva Burke, T. Möller, E. Bilotta
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引用次数: 0

摘要

三维试验中土体内部的应变测量是岩土工程物理建模人员面临的一个真正的挑战。光纤传感的使用提供了在小规模实验室实验中以高空间和时间分辨率连续测量深度应变的可能性。尽管这项技术还没有完全准备好进行离心实验,但这是岩土工程的一个重要发展。本文探讨了分布式光纤传感(DFOS)作为直接深度测量土壤应变剖面的解决方案的能力。通过一系列的小尺度平面应变试验,模拟了沉降形成的简单情况。在土样中敷设DFOS电缆,直接将应变与土的运动进行对比,通过粒子图像测速仪用摄像机记录。结果表明,DFOS在检测土壤运动方面的能力,并强调了这类实验中预期的典型特征应变曲线。进行了有限元分析,以进一步支持在1g下进行这些测试的结果,并将研究结果扩展到3D和岩土离心机的潜在应用。这为三维检测土体内部的土壤应变曲线显示了有希望的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Fibre optic sensing for strain-field measurement in geotechnical laboratory experiments
Strain measurement inside the soil body in three-dimensional (3D) experiments is a real challenge for physical modellers in geotechnics. The use of fibre optic sensing offers the possibility of continuous measurement of the strain at depth with high spatial and temporal resolution in small-scale laboratory experiments. Despite the technology not being fully ready yet for centrifuge experiments, this is an important development in geotechnics. This paper explores the capacities of distributed fibre optic sensing (DFOS) as a solution for direct soil strain profile measurement at depth. A series of small-scale plane-strain experiments is used to simulate the simple case of the formation of a downwards subsidence. DFOS cables are laid in the soil specimen, and strains are directly compared with the soil movement, recorded with cameras through particle image velocimetry. Results indicate the ability of DFOS in detecting soil movements and underline the typical signature strain profile expected during this type of experiments. Finite-element analyses are carried out to further underpin the consequences of performing these tests at 1g and extend the findings to potential applications in 3D and on the geotechnical centrifuge. This shows promising results for detection of soil strain profiles inside the soil body in 3D.
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