The Effect of Pyroclasts in Geothermal Borehole Heat Exchangers Performance on the Volcanic Island of Lanzarote (Canary Islands, Spain)

Samanta Gasco Cavero, Giovanni Lemes Pacheco, A. García-Gil, J. Rodríguez-Martín, Cristo Expósito, N. Cruz-Pérez, J. C. Santamarta
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Abstract

The design of a geothermal heat pump system and geothermal heat exchangers to replace conventional cold and heat production systems in a winery on the island of Lanzarote (Canary Islands, Spain), taking into account its active volcanic geological peculiarities, is presented in this work. Firstly, a study was carried out to estimate the cold and heat needs of the winery during its operation. A calculation program was implemented in Matlab software framework to estimate the influences of the winemaker’s decisions on the cold and heat consumption of the winery. Once the needs were determined, a commercial geothermal heat pump (GHP) was selected, using exhaust heat to produce hot and cold water at the same time. After assessing hot and cold-water consumption along with heat pump requirements, a field of closed-loop borehole heat exchangers (BHE) was designed using a finite element heat transport numerical model. The existing geological profile, characterized by alternating basalt lava flows and pyroclasts, was carefully considered. The high porosity of the pyroclastic layers resulted in a 20.1% reduction in BHE performance compared to the initial expectations. Consequently, the depth of the 12 BHE was increased 21.9 additional meters from the original design. Thus, it was concluded that the alternation of basaltic lava flows and pyroclasts is prevalent in volcanic islands, emphasizing the need to attentively account for these pyroclastic layers in such environments.
兰萨罗特火山岛(西班牙加那利群岛)地热井热交换器性能中火成岩的影响
考虑到兰萨罗特岛(西班牙加那利群岛)的活火山地质特征,本作品介绍了地源热泵系统和地源热泵热交换器的设计,以取代兰萨罗特岛(西班牙加那利群岛)一家葡萄酒厂的传统冷热生产系统。首先,对酒厂运行期间的冷热需求进行了估算。在 Matlab 软件框架内实施了一个计算程序,以估算酿酒师的决策对酒厂冷热消耗的影响。确定需求后,选择了商用地源热泵 (GHP),利用废热同时生产热水和冷水。在对冷热水消耗量和热泵需求进行评估后,使用有限元热传输数值模型设计了一个闭环钻孔热交换器(BHE)区域。设计中仔细考虑了以玄武岩熔岩流和火成岩交替为特征的现有地质剖面。与最初的预期相比,火成碎屑层的高孔隙率导致 BHE 性能降低了 20.1%。因此,12 个 BHE 的深度比原设计增加了 21.9 米。因此,得出的结论是,玄武岩熔岩流和火成碎屑的交替在火山岛中很普遍,强调了在这种环境中需要仔细考虑这些火成碎屑层。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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