Analysis of quaternary thermal properties and influencing factors on shallow geothermal energy exploitation in Beijing plain

LI Juan; ZHENG Jia; LEI Xiaodong; DU Jingran; LI Fu; JIA Zilong; LIU Aihua

doi:10.12029/gc20220512

GEOLOGY IN CHINA > 2022 > 49(5): 1543-1554. > DOI: 10.12029/gc20220512

LI Juan, ZHENG Jia, LEI Xiaodong, DU Jingran, LI Fu, JIA Zilong, LIU Aihua. Analysis of quaternary thermal properties and influencing factors on shallow geothermal energy exploitation in Beijing plain[J]. GEOLOGY IN CHINA, 2022, 49(5): 1543-1554. DOI: 10.12029/gc20220512

Citation:

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Analysis of quaternary thermal properties and influencing factors on shallow geothermal energy exploitation in Beijing plain

LI Juan^{1, 2,},
ZHENG Jia^{1, 2},
LEI Xiaodong³,
DU Jingran^{1, 2},
LI Fu^{2, 4},
JIA Zilong^{1, 2},
LIU Aihua^{1, 2}

1.
Beijing Geothermal research institute, Beijing 102218, China
2.
Key Laboratory of Shallow Geothermal Energy, MNR, Beijing 102218, China
3.
Beijing Institute of Ecological Geology, Beijing 100120, China
4.
Beijing Huaqing Geothermal Development Group Co. LTD, Beijing 102218, China

Funds:

sustainable utilization of shallow geothermal energy and construction of demonstration projects in Beijing PXM2018-158309-000002

More Information

Author Bio:
LI Juan, female, born in 1983, senior engineer, mainly engaged in the research of shallow geothermal energy utilization; E-mail: lj1983205@163.com
Received Date: February 05, 2021
Revised Date: May 31, 2021
Available Online: September 25, 2023

Graphical Abstract

Abstract

Abstract

This paper is the result of the geothermal geological survey engineering.
Objective
Thermal properties are important parameters for the evaluation and utilization of shallow geothermal energy resources.
Methods
In this work, we collected 695 quaternary samples from alluvial and diluvial fans in Beijing plain. Then thermal properties and geotechnical parameters were tested, and the characteristics of thermal properties and their influence on shallow geothermal energy extraction were analyzed.
Results
The results show that the average range of quaternary samples in Beijing plain is 1.465-2.022 W/(m·K) for thermal conductivity, 0.450×10^-6-0.841×10^-6 m²/s for thermal diffusion, and 2.323-3.080 MJ/(m³ · K) for specific heat, respectively. There is a linear relationship between the thermal conductivity (λ) and the thermal diffusivity (κ) with correlation equations λ =1.6973κ + 0.6127. The finer the particles size of quaternary loose sediments, the lower the thermal conductivity. The thermal conductivity increases rapidly with the moisture content within the range of 0-5% and tends to stabilize within the range of 5%-20%. The thermal conductivity decreases with the increase of water content within the range of 20%-40%. Under natural state, the thermal conductivity increases with the increase of the density and decreases with the increase of the pore ratio. When the sample temperature is in the range of 0-40 ℃, the thermal conductivity first decreases and then increases and keeps lowest at 20 ℃.
Conclusions
Thermal properties of the quaternary vary with geological conditions. They are related to the storage, collection and diffusion capacity of shallow geothermal energy. The larger the thermal conductivity, thermal diffusivity and specific heat capacity, the greater the soil heat storage and thermal conductivity.
- thermal conductivity,
- thermal diffusion,
- specific heat,
- quaternary,
- shallow geothermal energy,
- geothernal survey engineering,
- Beijing plain

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References (65)

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Analysis of quaternary thermal properties and influencing factors on shallow geothermal energy exploitation in Beijing plain