實驗室尺度異質性含水層之地下水熱傳輸試驗與模式分析

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秦淑娟(Shu-Chaun Chin) 查詢紙本館藏

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論文名稱

實驗室尺度異質性含水層之地下水熱傳輸試驗與模式分析
(Experimental and numerical analysis of groundwater heat transport in a lab-scale heterogeneous aquifer)

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摘要(中)

與化學示踪劑相比，溫度作為示踪劑除了可反映地下水流及熱傳輸的動態過程，還可以減少對環境的負面影響。為增進以溫度示踪劑推估含水層內水流及溫度傳遞行為之精確度，本研究通過建立異質性環境的砂箱來進行注水試驗，並以HYDRUS-2D數值模式進行模擬，其中模擬項目包含水溫、水流及熱傳輸的過程。數值模擬需材料的土壤特徵參數及熱性質參數，透過室內實驗取得，相關參數包含飽和水力傳導係數、非飽和土壤van Genuchten特徵曲線、熱導率及容積熱容等。砂箱試驗於室內恆溫環境下進行，砂箱長155公分、寬2公分、高55公分，砂箱左右各有一水槽調節水位，使左右邊界皆為定水頭，用蠕動馬達以定流量持續以單點注水方式注熱水5小時，觀察並量測相對高溫水注入相對低溫水中的熱傳輸動態歷程。試驗顯示在砂箱下半部的飽和區溫度受到熱水影響較為顯著，越接近注水點溫度上升越快，溫度達峰值時間越短，停止注水後溫度下降越快，並且最快降為室溫。數值模擬結果案例一能大致模擬砂箱注水情況，案例二模擬與試驗結果誤差較大。應用模型進行注水溫度與注入流量對熱傳輸距離影響測試時，在注入水溫與環境溫度溫較接近時，增加溫度的熱傳輸距離增幅較大，隨著注水溫度越大，距離增幅程度降低，表示一定程度升溫是有助於增加傳輸距離，但增溫的效果有限，效益會逐漸減小。

摘要(英)

Heat is one of tracers that can reflect groundwater flow and heat transport. Using temperature as a natural tracer, compared with chemical tracer, reduces negative impacts on the environment. In order to improve the accuracy of estimating the water flow and temperature transfer behavior in aquifers, this study employs experimental approaches and HYDRUS-2D numerical model to analyze the water temperature, water flow and heat transport. Laboratory experiments are also considered in this study to get sandbox material parameters that include hydraulic conductivity, van Genuchten parameter, thermal conductivity and volumetric heat capacity. The sandbox was placed at a constant temperature environment, which is 155 cm in length, 2 cm in width, and 55 cm in height. There are tanks on both left and right sides of the sandbox to control the water level. The hot water was injected into the sandbox by a single point with constant injection rate for 5 hours, and the dynamic process of heat transport was measured during the experiment. Experiments show that the temperature of the lower half of the sandbox is more significantly affected by hot water. The closer to the water injection point, the faster the temperature rise and the shorter the time to reach the temperature peak. After the water injection is stopped, the temperature drops quickly, and it drops to room temperature the fastest. The numerical simulation result of Case 1 can roughly simulate the water injection situation of the sand box, and the simulation and test results of Case 2 have large errors. When the model is used to test the influence of injection temperature and injection flow rate on the heat transfer distance, when the injected water temperature is close to the ambient temperature, the heat transfer distance increases as the temperature increases. As the water injection temperature increases, the increase in distance decreases. It means that a certain degree of temperature rise will help increase the transmission distance, but the effect of temperature rise is limited, and the benefits will
gradually decrease.

關鍵字(中)

★ 異質性含水層
★ 溫度示蹤劑
★ 熱傳輸
★ 砂箱試驗
★ HYDRUS-2D

關鍵字(英)

★ Heterogeneous aquifer
★ Heat tracer
★ Heat transport
★ Sandbox experiment
★ HYDRUS-2D

論文目次

摘要 i
Abstract ii
目錄 v
圖目錄 viii
表目錄 xiii
符號說明 xv
第一章緒論 1
1-1 背景與動機 1
1-2 研究目的 2
1-3 文獻回顧 2
1-3-1 示蹤劑 2
1-3-2 地下水偵溫方法 5
1-3-3 數值模式分析地下水溫度 7
1-4 研究流程 7
第二章研究方法 9
2-1 落水頭試驗(Falling-head test) 9
2-2 壓力鍋試驗(Pressure plate test) 10
2-3 熱性質試驗(Thermal property test) 12
2-4 砂箱注水試驗 14
2-4-1 分佈式光纖偵溫系統原理 14
2-4-2 砂箱介紹 15
2-4-3 砂箱材料 18
2-4-4 試驗設置 19
2-5 數值模式 HYDRUS-2D 23
2-5-1 控制方程式 23
2-5-2 初始條件 26
2-5-3 邊界條件 26
2-5-4 模型建置流程 27
2-5-5 敏感度分析 29
2-6 統計誤差 30
第三章結果與討論 31
3-1 室內試驗結果 31
3-1-1 落水頭試驗 31
3-1-2 壓力鍋試驗 33
3-1-3 熱性質試驗 35
3-1-4 砂箱注水試驗 40
3-3 數值模式 HYDRUS-2D 57
3-3-1 敏感度分析 57
3-3-2 建模設定 70
3-3-3 穩態模型條件設定 72
3-3-4 注水模型條件設定 74
3-3-5 水力特徵參數率定 75
3-3-6 熱參數率定 79
3-3-7 溫度模擬結果 80
3-4 模擬與試驗結果分析 87
3-5 熱傳輸距離測試 99
第四章結論與建議 102
4.1 結論 102
4.2 建議 103
參考資料 104
附錄一 111
附錄二 116
附錄三 117
附錄四 118
附錄五 121

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指導教授

倪春發(Chuen-Fa Ni)

審核日期

2021-9-22

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