A transient model for temperature prediction in a salt-gradient solar pond and the ground beneath it

被引:25
|
作者
Amigo, Jose [1 ,2 ,3 ]
Meza, Francisco [4 ,5 ,6 ]
Suarez, Francisco [1 ,2 ,3 ,7 ]
机构
[1] Pontificia Univ Catolica Chile, Dept Ingn Hidraul & Ambiental, Avda Vicuna Mackenna 4860, Santiago, Chile
[2] CONICYT FONDAP 15110020, Ctr Desarrollo Urbano Sustentable CEDEUS, Santiago, RM, Chile
[3] CSET, Santiago, RM, Chile
[4] Pontificia Univ Catolica Chile, Dept Ecosistemas & Medio Ambiente, Fac Agron & Ingn Forestal, Avda Vicuna Mackenna 4860, Santiago, Chile
[5] Pontificia Univ Catolica Chile, Ctr Interdisciplinario Cambio Global, Avda Vicuna Mackenna 4860, Santiago, Chile
[6] Aquasec, IAI Ctr Excellence Water Secur, Santiago, Chile
[7] CEGA, Santiago, RM, Chile
关键词
Solar pond; Transient model; Solar energy; Ground heat storage; HEAT EXTRACTION; SIMULATION-MODEL; ENERGY-STORAGE; EVAPORATION; PERFORMANCE;
D O I
10.1016/j.energy.2017.05.063
中图分类号
O414.1 [热力学];
学科分类号
摘要
Salt-gradient solar ponds are cost-effective long-term solar collectors that can store low-grade heat and deliver it continuously. For design and operation purposes, it is important to develop computational tools that can represent energy fluxes at the interface between the bottom of the pond and the ground beneath it. In this study, a robust one-dimensional transient model is developed to represent the thermal evolution of a salt-gradient solar pond and the ground that surrounds it. The model was evaluated under different contrasting scenarios: buried or unburied ponds, artificially or naturally heated ponds and for deep or shallow groundwater tables. Experimental data from an indoor laboratory-scale solar pond were used for the development, calibration and validation of the model. A good agreement between experimental and modeled results was observed, with a root mean square error (RMSE) of 1.21 degrees C and 1.54 degrees C for the upper and lower convective zones respectively, during a 28-days validation period. Further, the model was validated using experimental data from three outdoor salt-gradient solar ponds obtaining RMSEs that ranged between 1.5 and 6.5 degrees C. Results show that dividing the ground into multiple layers contributes to the robustness of the model, as it allows the representation of the ground heat storage. (C) 2017 Elsevier Ltd. All rights reserved.
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页码:257 / 268
页数:12
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