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Laboratory Measurements of Gravel Thermal Conductivity: An Update Methodological Approach

机译:砾石导热系数的实验室测量:一种更新方法

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摘要

Direct measurements of gravel thermal properties are quite challenging mainly due to technical issues related with the very coarse sediment size, which impedes an appropriate physical contact between the material and the traditional measuring sensors. In addition, the variability of the mineralogical composition of the polygenic samples in many cases requires a quite large volume of geological material to be involved in the measurement procedure, in order to obtain representative thermal properties values. As a consequence, up to now the reference thermal values provided by literature for gravels are quite limited and dispersed.\udWith the purpose to improve the gravel’s thermal properties knowledge, a new measurement methodology has been proposed and tested on several gravel samples, by means of a single guarded hot plate Taurus Instruments TLP 800 usually used for buildings materials, modified on purpose. The instrument adjustments were needed in order to measure unconsolidated materials and to allow the testing of even with interstitial fluid. The measurements have been performed at the FISTEC laboratory (Environmental Technical Physics Laboratory) of the IUAV University in Venice (Italy). A preliminary calibration has been performed comparing the outcomes obtained with the single guarded hot plate with a needle probe of a portable thermal conductivity meter (ISOMET) by using Standard sand (ISO 67:2009) as reference material. \udThis new measuring procedure has been developed within the Cheap – GSHPs Horizon 2020 project, which focuses on the development of more efficient and safe shallow geothermal systems and on the reduction of their installation costs, in order to improve the evaluation of the ground heat exchange capacity of the site where the Ground Source Heat Pump (GSHP) has to be installed, therefore optimizing the probes total length design phase.
机译:直接测量砾石的热特性非常具有挑战性,主要是由于与非常粗大的沉积物尺寸有关的技术问题,这阻碍了材料与传统测量传感器之间的适当物理接触。另外,在许多情况下,多基因样品的矿物组成的可变性要求相当大量的地质材料参与测量程序,以便获得代表性的热特性值。结果,到目前为止,文献提供的砾石参考热值相当有限且分散。\ ud为了提高砾石的热学性能,人们提出了一种新的测量方法,并通过以下方法对几种砾石样品进行了测试: Taurus Instruments TLP 800的一种带防护的热板,通常用于建筑材料,经有意修改。需要对仪器进行调整,以便测量未固结的材料,并允许甚至对组织液进行测试。测量是在意大利威尼斯的IUAV大学的FISTEC实验室(环境技术物理实验室)进行的。通过使用标准砂(ISO 67:2009)作为参考材料,已进行了初步校准,比较了带有单保护热板和便携式导热率计(ISOMET)的针形探头的结果。 \ ud此廉价的GSHP Horizo​​n 2020项目已开发了这种新的测量程序,该项目专注于开发更高效,更安全的浅层地热系统,并降低其安装成本,以改善对地热交换的评估必须安装地源热泵(GSHP)的站点的容量,因此可以优化探头的总长度设计阶段。

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