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溫度對不同尺寸砂巖巴西劈裂特性影響

孫浩 蘇楠 金愛兵 陳帥軍 韋立昌 徐浩淳

孫浩, 蘇楠, 金愛兵, 陳帥軍, 韋立昌, 徐浩淳. 溫度對不同尺寸砂巖巴西劈裂特性影響[J]. 工程科學學報, 2022, 44(1): 26-38. doi: 10.13374/j.issn2095-9389.2021.07.26.001
引用本文: 孫浩, 蘇楠, 金愛兵, 陳帥軍, 韋立昌, 徐浩淳. 溫度對不同尺寸砂巖巴西劈裂特性影響[J]. 工程科學學報, 2022, 44(1): 26-38. doi: 10.13374/j.issn2095-9389.2021.07.26.001
SUN Hao, SU Nan, JIN Ai-bing, CHEN Shuai-jun, WEI Li-chang, XU Hao-chun. Effects of temperature on Brazilian splitting characteristics of sandstone with different sizes[J]. Chinese Journal of Engineering, 2022, 44(1): 26-38. doi: 10.13374/j.issn2095-9389.2021.07.26.001
Citation: SUN Hao, SU Nan, JIN Ai-bing, CHEN Shuai-jun, WEI Li-chang, XU Hao-chun. Effects of temperature on Brazilian splitting characteristics of sandstone with different sizes[J]. Chinese Journal of Engineering, 2022, 44(1): 26-38. doi: 10.13374/j.issn2095-9389.2021.07.26.001

溫度對不同尺寸砂巖巴西劈裂特性影響

doi: 10.13374/j.issn2095-9389.2021.07.26.001
基金項目: 國家自然科學基金資助項目(52174106,52004017);中國博士后科學基金資助項目(2020M670138);中央高校基本科研業務費專項資金資助項目(FRF-TP-19-026A1,FRF-IDRY-20-021)
詳細信息
    通訊作者:

    E-mail: jinaibing@ustb.edu.cn

  • 中圖分類號: TU458

Effects of temperature on Brazilian splitting characteristics of sandstone with different sizes

More Information
  • 摘要: 為研究高溫與尺寸效應耦合作用下的砂巖巴西劈裂特性,分別對經過25、200、400、600、800和1000 ℃高溫處理后的標準砂巖試件進行巴西劈裂室內試驗,并基于顆粒流軟件開展不同尺寸高溫砂巖巴西劈裂數值模擬,研究砂巖巴西劈裂強度及其劣化規律、孔隙率增加相對于裂紋擴展貫通的滯后性規律。研究結果表明:(1)在25~1000 ℃的溫度范圍和50~100 mm的直徑范圍內,溫度與尺寸效應對砂巖巴西劈裂強度均有顯著影響,且尺寸效應影響程度更大。在加熱過程中,由于巖石內部首先發生熱膨脹,然后在熱應力作用下產生損傷,因此砂巖劈裂強度先有所增大,在400 ℃之后持續降低,劈裂強度下降約34.66%~35.10%;隨著尺寸增大,巖石內部積聚的能量釋放產生大量微裂隙,導致砂巖試樣劈裂強度降低,下降約55.61%~56.99%。(2)砂巖巴西劈裂強度劣化幅值與其直徑之間滿足負指數函數關系,可用于預測不同尺寸高溫砂巖的巴西劈裂強度。(3)砂巖在巴西劈裂過程中的孔隙率增加相對于裂隙擴展貫通滯后的荷載差值隨溫度升高以及尺寸增大而增大;考慮兩因素的耦合作用,尺寸效應對荷載差值的影響程度隨溫度的升高而降低,溫度對荷載差值的影響程度隨砂巖尺寸的增大而降低。研究成果對火災后頂板維護,初步預測頂板強度具有一定參考意義,也可為核廢料處理、地熱資源開發和深井工程等涉及高溫和尺寸變化的巖體工程設計提供有益參考。

     

  • 圖  1  巴西劈裂室內試驗。(a)YAW?600電液壓伺服巖石壓力試驗機;(b)巴西圓盤試件

    Figure  1.  Laboratory test of Brazilian splitting: (a) YAW?600 electro hydraulic servo rock pressure testing machine; (b) Brazilian disk specimen

    圖  2  不同溫度下砂巖平均縱波波速。(a)康科瑞NM?4B非金屬超聲檢測分析儀;(b)縱波波速曲線

    Figure  2.  P-wave velocity of sandstone at different temperatures: (a) concrete NM?4B metalloid ultrasonic testing analyzer; (b) P-wave velocity curve

    圖  3  砂巖礦物成分衍射強度隨溫度變化曲線

    Figure  3.  Variation curves of the mineral composition diffraction intensity of sandstone with temperature

    圖  4  砂巖電鏡掃描圖像。(a)800 ℃時掃描電鏡圖像;(b)1000 ℃時掃描電鏡圖像

    Figure  4.  SEM images of sandstone at: (a) 800 ℃; (b) 1000 ℃

    圖  5  砂巖試樣X射線衍射結果。(a)D8 DISCOVER X射線衍射儀;(b)衍射強度圖譜;(c)礦物成分含量

    Figure  5.  X-ray diffraction results of sandstone samples: (a) photograph of D8 DISCOVER X-ray diffractometer; (b) diffraction intensity pattern; (c) mineral composition content

    圖  6  PFC中熱力學計算時熱存儲器和熱管示意圖

    Figure  6.  Schematic of the heat storage and heat pipe for the thermodynamic calculation of PFC

    圖  7  砂巖數值模型

    Figure  7.  Sandstone numerical model

    圖  8  砂巖數值模擬結果與室內試驗結果對比。(a)砂巖試樣;(b)顆粒流模型

    Figure  8.  Comparison of numerical simulation and laboratory test results of sandstone with a diameter of 50 mm: (a) sandstone sample; (b) particle flow model

    圖  9  高溫與尺寸效應耦合作用下的砂巖巴西劈裂強度。(a)砂巖劈裂強度與溫度及尺寸的關系;(b)垂直方向投影圖

    Figure  9.  Brazilian splitting strength of sandstone under the coupling effects of high temperature and size: (a) relationship between the splitting strength of sandstone and temperature and size; (b) vertical projection

    圖  10  不同溫度下各尺寸砂巖巴西劈裂強度的劣化幅值。(a)200 ℃;(b)400 ℃;(c)1000 ℃

    Figure  10.  Degradation amplitude of the Brazilian splitting strength of sandstone of different sizes at (a) 200 ℃; (b) 400 ℃; (c) 1000 ℃

    圖  11  砂巖孔隙率增加相對裂隙擴展貫通滯后的荷載差值與溫度和尺寸的關系。(a)荷載差值;(b)垂直方向投影圖

    Figure  11.  Relationship between the load difference of the sandstone porosity relative to the fracture propagation and penetration and temperature and size: (a) load difference; (b) vertical projection

    圖  12  常溫下直徑50 mm和100 mm砂巖裂隙演化過程

    Figure  12.  Evolution of sandstone fractures with diameters of 50 mm and 100 mm at room temperature

    圖  13  不同溫度下砂巖試樣孔隙率測試值。(a)25 ℃;(b)400 ℃;(c)800 ℃;(d)1000 ℃

    Figure  13.  Test results of the porosity of sandstone samples at (a) 25 ℃; (b) 400 ℃; (c) 800 ℃; (d) 1000 ℃

    表  1  不同溫度下砂巖試樣的劈裂強度

    Table  1.   Splitting strengths of sandstone samples at different temperatures

    Temperature/℃Splitting strength/MPaAverage value/MPa
    ABC
    252.2382.2372.2542.243
    2002.3412.5882.2262.385
    4002.4253.8322.4392.432
    6002.2211.9552.4042.193
    8001.9642.2602.2492.158
    10001.4451.6823.7981.564
    Note:A, B, C is the test values of three groups of Brazilian splitting tests; Average value is the average of three test values.
    下載: 導出CSV

    表  2  砂巖數值模型細觀參數組合

    Table  2.   Combination of meso-parameters of the sandstone numerical model

    ParametersValueParametersValue
    Minimum radius of particles/mm0.10Elastic modulus/GPa5
    Particle size ratio1.50Parallel bond modulus/GPa5
    Particle density/(kg·m?3)2300Local damping coefficient0.70
    Splitting strength/MPa2.24Thermal conductivity[35]/(W·m?1·K?1)5.91
    Friction coefficient0.50Coefficient of linear thermal expansion/(10?4 K?1)Quartz1.37
    Porosity0.18Kaolinite0.53
    Stiffness ratio1.30Mica2.80
    下載: 導出CSV

    表  3  不同砂巖在巴西劈裂模擬下的劈裂強度

    Table  3.   Splitting strengths of different sandstone samples under Brazilian splitting simulations

    Sample numberTemperature/℃Diameter/mmSplitting strength/MPaSample numberTemperature/℃Diameter/mmSplitting strength/MPa
    125502.23913600502.190
    225602.01514600602.013
    325801.27615600801.223
    4251000.963166001001.004
    5200502.36417800502.145
    6200602.15118800601.798
    7200801.37119800801.174
    82001001.040208001000.862
    9400502.320211000501.516
    10400602.123221000601.275
    11400801.361231000800.807
    124001001.0372410001000.673
    下載: 導出CSV
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  • 收稿日期:  2021-07-26
  • 網絡出版日期:  2021-09-08
  • 刊出日期:  2022-01-01

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