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Heat pulse line-source method to determine thermal conductivity of consolidated rocks

机译:热脉冲线源法确定固结岩的导热系数

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摘要

An instrument designed to measure thermal conductivity of consolidated rocks, dry or saturated, using a transient method is presented. The instrument measures relative values of the thermal conductivity, and it needs calibration to obtain absolute values. The device can be used as heat pulse line source and as continuous heat line source. Two parameters to determine thermal conductivity are proposed: TMAX, in heat pulse line source, and SLOPE, in continuous heat line source. Its performance is better, and the operation simpler, in heat pulse line-source mode with a measuring time of 170 s and a reproducibility better than 2.5%. The sample preparation is very simple on both modes. The performance has been tested with a set of ten rocks with thermal conductivity values between 1.4 and 5.2 W m¿1 K¿1 which covers the usual range for consolidated rocks.
机译:提出了一种使用瞬态方法测量干燥或饱和固结岩石导热系数的仪器。该仪器测量热导率的相对值,并且需要进行校准以获得绝对值。该设备可用作热脉冲线源和连续热线源。提出了两个确定导热系数的参数:热脉冲线源中的TMAX和连续热线源中的SLOPE。在热脉冲线源模式下,其性能更好,操作更简单,测量时间为170 s,重现性优于2.5%。两种模式下的样品制备都很简单。该性能已经用一组十个岩石的热导率值在1.4和5.2 W m-1 K-1之间的岩石进行了测试,涵盖了固结岩石的通常范围。

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