利用溫泉井水溫觀測資料推估地層導熱係數之研究

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標題:	利用溫泉井水溫觀測資料推估地層導熱係數之研究 Using a 1D numerical temperature recovery model to estimate in-situ thermal diffusivity by an up-welling heat source in an artesian well
作者:	陳文福
貢獻者:	嘉藥學校財團法人嘉南藥理大學觀光事業管理系
關鍵字:	熱擴散係數溫泉垂直井溫 thermal conductivity hot spring temperature-depth profile
日期:	2019
上傳時間:	2021-11-08 15:53:40 (UTC+8)
摘要:	地層導熱係數是地下傳熱的基本重要控制因素，溫泉觀測井常有自湧現象，因而產生溫度的變化，利用此溫度差，可推求地層導熱係數。本計畫擬先在礁溪溫泉進行現地地層導熱係數研究，此方法確立後也可應用於其他溫泉區，各溫泉區或地熱區之開發，其溫度變化乃受到地層導熱係數之控制，了解地層導熱係數之空間分布，為溫泉地熱開發管理的基礎。 The determination of thermal diffusivity is a pre-requisite for geothermal site characterization and utilization. The temperature recovery (TR) method is a popular method for determining in-situ thermal conductivity together with the thermal response test and thermal conductivity probe methods. To determine in-situ thermal properties of the subsurface following a thermal disturbance produced by drilling processes or a heating cable within a borehole, the TR method is used to record decaying temperatures during the recovery period. However, to date, no studies exist to determine thermal diffusivity using up-welling water within a well. In this study, we introduce a 1D numerical method for estimating in-situ thermal diffusivity of the subsurface using up-welling thermal water as a heat source within an artesian well. Our numerical model includes parameters for the position of a sensor within a borehole, as well as for the thermal properties of a well casing and an annulus.
關聯:	計畫編號：MOEAWRA1080323 計畫年度：108 執行起迄：2019-03~2019-12
顯示於類別:	[觀光事業管理系(含溫泉所)] 科技部計畫

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