Numerical analysis of heat gain to geothermal heat exchangers with moisture evaporation in the structure

被引:0
|
作者
Polovnikov, V. Yu. [1 ]
Shelemekhova, S. D. [1 ]
Lyubivy, E. V. [1 ]
机构
[1] Natl Res Tomsk Polytech Univ, Tomsk, Russia
来源
BULLETIN OF THE TOMSK POLYTECHNIC UNIVERSITY-GEO ASSETS ENGINEERING | 2024年 / 335卷 / 06期
基金
俄罗斯科学基金会;
关键词
geothermal energy; geothermal heat exchanger; mathematical modeling; heat gain; evaporation; BOREHOLE; STORAGE;
D O I
10.18799/24131830/2024/6/4579
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Relevance.Provisions on the need to transition to alternative energy sources and energy security, reduc-tion ofenvironmental emissions and energy conservation in various industries can largely rely on the use of geo-thermal energy. A separate area in the field of modeling geothermal technologies is the study of thermal regimes of geothermal heat exchangers. The need to ensure reliable thermal contact between the geothermal heat ex-changer and its environment leads to the use of a variety of backfills, including pre-moistened ones.Aim. Study of the intensification of heat supply to geothermal heat exchangers, taking into account the effectof moisture evap-oration in its backfill, its characteristics and operating conditions of the systems under consideration.Methods.The solution to the problem was obtained by the finite difference method. An implicit difference scheme and sweep algorithm were used. The coordinate step ranged from 1 to 10 mm. Results and conclusions. Study was carried out for six months of continuous operation of a geothermal heat exchanger. When analyzing the thermal conditions of the system under consideration, the main attention was paid to the study of the intensification of heat supply to the geothermal heat exchanger, taking into account the effect of moisture evaporation in its back-fill, its characteristics and operating conditions of the systems under consideration. It was established that an increase in the sand backfill humidity of a geothermal heat exchanger leads to a growth in heat inflows by 3.2-7.8%. A significant effect of the unsteadiness of transfer processes on heat transfer intensification in the system under consideration was revealed. It was shown that the increase in heat flow to the geothermal heat ex-changer due to the presence of evaporation is about 22%. The conclusion is substantiated that when choosing an option for regulating the thermal conditions of geothermal heat exchangers, the volumetric humidity of the sand backfill should be primarily changed.
引用
收藏
页码:89 / 97
页数:9
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