Thermophysical properties of surficial rocks: a tool to characterize geothermal resources of remote northern regions

被引:11
|
作者
Miranda, M. M. [1 ]
Giordano, N. [1 ]
Raymond, J. [1 ]
Pereira, A. J. S. C. [2 ]
Dezayes, C. [3 ]
机构
[1] INRS, 490 Rue Couronne, Quebec City, PQ G1K 9A9, Canada
[2] Univ Coimbra, CIT EUC Ctr Earth & Space Res, Rua Silvio Lima,Polo 2 Univ Coimbra, P-3030790 Coimbra, Portugal
[3] Bur Rech Geol & Minieres, 3 Ave Claude Guillemin,BP 36009, F-45060 Orleans 2, France
关键词
Steady-state temperature distribution; Temperature field; Deep geothermal energy; Nunavik; LOWLANDS SEDIMENTARY BASIN; RADIOGENIC HEAT-PRODUCTION; THERMAL-CONDUCTIVITY; UNGAVA BAY; QUEBEC; CANADA; FLOW; BOREHOLE; ELEMENTS; ENERGY;
D O I
10.1186/s40517-020-0159-y
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
The energetic framework of Canadian remote communities relies on fossil fuels. This has adverse environmental and energy security issues. In order to offset diesel consumption, the search for local, sustainable and carbon-free energy sources is of utmost importance. Unfortunately, in such remote regions, subsurface data to evaluate the geothermal potential is often nonexistent. This raises a key question: how to characterize geothermal resources associated to petrothermal systems based on surface data? Answering this question is the purpose of this work highlighting how outcrops can be used as deep subsurface analogues. The variability induced by laboratory methods to characterize thermophysical properties is further evaluated in the estimation of the present-day temperature at depth. The community of Kuujjuaq, Canada, is used as an example where guidelines are defined to evaluate the steady-state geotherm. Rock samples were collected and analyzed with a guarded heat flow meter and an optical scanner to determine thermal conductivity. Radiogenic elements concentration was evaluated with gamma-ray and mass spectrometry. 2D temperature models were built taking into account the regional geology and the results obtained from the different laboratory methods. A base-case temperature of 57-88 degrees C at 5 km is predicted below Kuujjuaq. This range is based on different methods used to evaluate both thermal conductivity and internal heat generation. The work conducted in Kuujjuaq shows that the combination of gamma-ray spectrometry and optical scanning gives lower base-case temperature predictions when compared to mass spectrometry combined with the guarded heat flow meter. Despite the nonexistence of deep temperature measurements in northern regions, the assessment of thermophysical properties from outcrops is shown to be a useful tool for a preliminary assessment of geothermal resources in remote areas facing critical energy issues.
引用
收藏
页数:27
相关论文
共 4 条
  • [1] Thermophysical properties of surficial rocks: a tool to characterize geothermal resources of remote northern regions
    M. M. Miranda
    N. Giordano
    J. Raymond
    A. J. S. C. Pereira
    C. Dezayes
    Geothermal Energy, 8
  • [2] Combination of Well-Logging Temperature and Thermal Remote Sensing for Characterization of Geothermal Resources in Hokkaido, Northern Japan
    Tian, Bingwei
    Wang, Ling
    Kashiwaya, Koki
    Koike, Katsuaki
    REMOTE SENSING, 2015, 7 (03) : 2647 - 2667
  • [3] Uncertainty and Risk Evaluation of Deep Geothermal Energy Source for Heat Production and Electricity Generation in Remote Northern Regions
    Miranda, Mafalda M.
    Raymond, Jasmin
    Dezayes, Chrystel
    ENERGIES, 2020, 13 (16)
  • [4] Reflecting on siliceous rocks in central Australia: Using advanced remote sensing to map ancient "tool-stone" resources
    Law, Wallace Boone
    Lewis, Megan M.
    Ostendorf, Bertram
    Hiscock, Peter
    GEOARCHAEOLOGY-AN INTERNATIONAL JOURNAL, 2020, 35 (03): : 400 - 415