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Impact of coupled heat transfer and water flow on soil borehole thermal energy storage (SBTES) systems: Experimental and modeling investigation

机译:传热和水流耦合对土壤钻孔热能存储(SBTES)系统的影响:实验和模型研究

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A promising energy storage option is to inject and store heat generated from renewable energy sources in geothermal borehole arrays to form soil-borehole thermal energy storage (SBTES) systems. Although it is widely recognized that the movement of water in liquid and vapor forms through unsaturated soils is closely coupled to heat transfer, these coupled processes have not been considered in modeling of SBTES systems located in the vadose zone. Instead, previous analyses have assumed that the soil is a purely conductive medium with constant hydraulic and thermal properties. Numerical modeling tools that are available to consider these coupled processes have not been applied to SBTES systems partly due to the scarcity of field or laboratory data needed for validation. The goal of this work is to test different conceptual and mathematical formulations that are used in heat and mass transfer theories and determine their importance in modeling SBTES systems. First, a non-isothermal numerical model that simulates coupled heat, water vapor and liquid water flux through soil and considers non-equilibrium liquid/gas phase change was adopted to simulate SBTES systems. Next, this model was used to investigate different coupled heat transfer and water flow using nonisothermal hydraulic and thermal constitutive models. Data collected from laboratory-scale tank tests involving heating of an unsaturated sand layer were used to validate the numerical simulations. Results demonstrate the need to include thermally induced water flow in modeling efforts as well as convective heat transfer, especially when modeling unsaturated flow systems. For the boundary conditions and soil types considered, convective heat flux arising from thermally induced water flow was greater than heat transfer due to conductive heat flux alone. Although this analysis needs to be applied to the geometry and site conditions for SBTES systems in the vadose zone, this observation indicates that thermally induced water flow can have significant effects on the efficiency of heat injection and extraction. (C) 2015 Elsevier Ltd. All rights reserved.
机译:一个有前途的储能选择是将可再生能源产生的热量注入并储存在地热井眼阵列中,以形成土壤钻孔热能存储(SBTES)系统。尽管人们普遍认为水以液态和蒸气形式通过不饱和土壤的运动与热传递密切相关,但是在位于渗流区的SBTES系统的建模中并未考虑这些耦合过程。取而代之的是,先前的分析假设土壤是具有恒定水力和热力特性的纯导电介质。可用于考虑这些耦合过程的数值建模工具尚未应用于SBTES系统,部分原因是验证所需的现场或实验室数据稀缺。这项工作的目的是测试传热和传质理论中使用的不同概念和数学公式,并确定它们在SBTES系统建模中的重要性。首先,采用非等温数值模型来模拟通过土壤的热,水蒸气和液态水的耦合通量,并考虑了非平衡的液/气相变化来模拟SBTES系统。接下来,该模型用于使用非等温水力和热本构模型研究不同的耦合传热和水流。从涉及不饱和砂层加热的实验室规模罐试验中收集的数据用于验证数值模拟。结果表明,在建模工作以及对流传热过程中,尤其是在对非饱和流系统进行建模时,需要将热诱导的水流包括在内。对于所考虑的边界条件和土壤类型,由热引起的水流产生的对流热通量大于仅由传导性热通量引起的热传递。尽管需要将分析应用于渗流带中SBTES系统的几何形状和现场条件,但该观察结果表明,热诱导的水流可能对热注入和提取的效率产生重大影响。 (C)2015 Elsevier Ltd.保留所有权利。

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