4.5 Article

Repeated ETRTs in a Complex Stratified Geological Setting: High-Resolution Thermal Conductivity Identification by Multiple Linear Regression

出版社

ASCE-AMER SOC CIVIL ENGINEERS
DOI: 10.1061/(ASCE)GT.1943-5606.0002724

关键词

Enhanced thermal response test (ETRT); Hybrid fiber optic cable; First-order approximation; Ground thermal conductivity; Distributed optical fiber sensing; Stratified geological setting

资金

  1. project GEO4CIVHIC: Most Easy, Efficient and Low Cost Geothermal Systems for Retrofitting Civil and Historical Buildings from the European Union's Horizon 2020 research and innovation program [792355]

向作者/读者索取更多资源

This article introduces an innovative method using hybrid optic fiber cables to detect vertical profile of ground thermal conductivity. The method has high spatial and temporal resolution and can accurately evaluate the local heat exchange capability. By conducting experiments on a well in the Po Plain, a new multiple linear regression analysis method is proposed to distinguish the thermal conductivity of different granulometric units.
For the design of ground-source heat-pump systems, the local subsoil is an invariant factor. To improve the evaluation of the local heat exchange capability, significant efforts recently have been devoted to identifying the ground thermal conductivity vertical profile. In recent years, an innovative method using hybrid optic fiber cables inserted into the ground has been developed. The technique relies on copper wires that thermally stimulate the ground. Optical fibers measure the temperature variation over time all along the cable at a high spatial and temporal resolution. In this work, the hybrid cable was grouted into a 125-m well located in the Po Plain in Northern Italy. The provided core defined the geological environment as a continuous succession of unconsolidated alluvial deposits of very limited thickness, grouped in 15 different granulometric units. Three enhanced thermal response test (ETRT) data sets were acquired in different seasons; for 5 days of heating followed by 5 days of recovery, the soil temperature was recorded continuously along the well, with a spatial resolution of 1 m. A new approach using a multiple linear regression is proposed to analyze the data sets to distinguish the thermal conductivity of each individual granulometric unit. The obtained thermal conductivity values were compared and discussed considering the standard thermal response test outputs and the thermal conductivity data obtained from direct measurements performed on the cores. The analytical method's reliability stands due to the high repeatability of the obtained results, despite the increased complexity of the treated geological setting.

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