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The Use of Infrared Thermography for Porosity Assessment of Intact Rock

机译:红外热成像技术在完整岩石孔隙率评估中的应用

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摘要

Preliminary results on a new test for the indirect assessment of porosity through infrared thermography are presented. The study of the cooling behavior of rock samples in laboratory, through the analysis of thermograms, proved an innovative tool for the estimation of such an important property, which is one of the main features affecting the mechanical behavior of rocks. A detailed experimentation was performed on artificially heated volcanic rock samples characterized by different porosity values. The cooling trend was described both graphically and numerically, with the help of cooling curves and Cooling Rate Index. The latter, which proved strictly linked to porosity, was employed to find reliable equations for its indirect estimation. Simple and multiple regression analyses returned satisfactory outcomes, highlighting the great match between predicted and measured porosity values, thus confirming the goodness of the proposed model. This study brings a novelty in rock mechanics, laying the foundation for future researches aimed at refining achieved results for the validation of the model in a larger scale.
机译:介绍了通过红外热成像法间接评估孔隙度的新测试的初步结果。通过对热分析图的分析,对实验室岩石样品的冷却行为进行了研究,证明了评估这种重要性能的创新工具,这是影响岩石力学性能的主要特征之一。对以不同孔隙率值为特征的人工加热的火山岩样品进行了详细的实验。借助冷却曲线和冷却速率指数,以图形和数字方式描述了冷却趋势。后者被证明与孔隙率严格相关,被用于寻找可靠的方程式进行间接估算。简单和多元回归分析得出令人满意的结果,突出显示了预测的孔隙率值和测量的孔隙率值之间的巨大匹配,从而证实了所提出模型的优越性。这项研究带来了岩石力学方面的新颖性,为将来的研究奠定了基础,这些研究旨在细化所取得的成果,以进行更大范围的模型验证。

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