共 50 条
Numerical modeling of ground thermal response with borehole heat exchangers connected in parallel
被引:24
|作者:
Monzo, Patricia
[1
]
Puttige, Anjan Rao
[1
]
Acuna, Jose
[1
]
Mogensen, Palne
[1
]
Cazorla, Antonio
[2
]
Rodriguez, Juan
[3
]
Montagud, Carla
[2
]
Cerdeira, Fernando
[4
]
机构:
[1] KTH Royal Inst Technol, Brinellvagen 68, S-10044 Stockholm, Sweden
[2] Univ Politecn Valencia, IUIIE, Camino Vera S-N, E-46022 Valencia, Spain
[3] EnergyLab, Fonte Abelleiras S-N,Campus Univ Vigo, Vigo 36310, Spain
[4] Univ Vigo, Maxwell 16, Vigo 36310, Spain
关键词:
Borehole heat exchanger;
Numerical modeling;
Monitoring;
Fluid temperature prediction;
Boundary condition;
GEOTHERMAL BOREHOLES;
FIELDS;
FLUID;
PUMP;
PERFORMANCE;
OPERATION;
SYSTEMS;
FLOW;
WALL;
D O I:
10.1016/j.enbuild.2018.04.057
中图分类号:
TU [建筑科学];
学科分类号:
0813 ;
摘要:
With bore fields for energy extraction and injection, it is often necessary to predict the temperature response to heat loads for many years ahead. Mathematical methods, both analytical and numerical, with different degrees of sophistication, are employed. Often the g-function concept is used, in which the borehole wall is assumed to have a uniform temperature and the heat injected is constant over time. Due to the unavoidable thermal resistance between the borehole wall and the circulating fluid and with varying heat flux along the boreholes, the concept of uniform borehole wall temperature is violated, which distorts heat flow distribution between boreholes. This aspect has often been disregarded. This paper describes improvements applied to a previous numerical model approach. Improvements aim at taking into account the effect of thermal resistance between the fluid and the borehole wall. The model employs a highly conductive material (HCM) embedded in the boreholes and connected to an HCM bar above the ground surface. The small temperature difference occurring within the HCM allows the ground to naturally control the conditions at the wall of all boreholes and the heat flow distribution to the boreholes. The thermal resistance between the fluid and the borehole wall is taken into account in the model by inserting a thermally resistive layer at the borehole wall. Also, the borehole ends are given a hemispherical shape to reduce the fluctuations in the temperature gradients there. The improvements to the HCM model are reflected in a changed distribution of the heat flow to the different boreholes. Changes increase with the number of boreholes. The improvements to the HCM model are further illustrated by predicting fluid temperatures for measured variable daily loads of two monitored GCHP installations. Predictions deviate from measured values with a mean absolute error within 1.1 and 1.6 K. (C) 2018 Elsevier B.V. All rights reserved.
引用
收藏
页码:371 / 384
页数:14
相关论文