徐云山, 曾召田, 吕海波, 范理云, 覃汉莲. 2017: 高温下红黏土热导率的变化规律试验研究. 工程地质学报, 25(6): 1465-1473. DOI: 10.13544/j.cnki.jeg.2017.06.009
    引用本文: 徐云山, 曾召田, 吕海波, 范理云, 覃汉莲. 2017: 高温下红黏土热导率的变化规律试验研究. 工程地质学报, 25(6): 1465-1473. DOI: 10.13544/j.cnki.jeg.2017.06.009
    XU Yunshan, ZENG Zhaotian, LÜ Haibo, FAN Liyun, QIN Hanlian. 2017: EXPERIMENTAL STUDY ON VARIATION OF THERMAL CONDUCTIVITY OF RED CLAY AT HIGH TEMPERATURE. JOURNAL OF ENGINEERING GEOLOGY, 25(6): 1465-1473. DOI: 10.13544/j.cnki.jeg.2017.06.009
    Citation: XU Yunshan, ZENG Zhaotian, LÜ Haibo, FAN Liyun, QIN Hanlian. 2017: EXPERIMENTAL STUDY ON VARIATION OF THERMAL CONDUCTIVITY OF RED CLAY AT HIGH TEMPERATURE. JOURNAL OF ENGINEERING GEOLOGY, 25(6): 1465-1473. DOI: 10.13544/j.cnki.jeg.2017.06.009

    高温下红黏土热导率的变化规律试验研究

    EXPERIMENTAL STUDY ON VARIATION OF THERMAL CONDUCTIVITY OF RED CLAY AT HIGH TEMPERATURE

    • 摘要: 目前国际上对高温下土壤热导率的试验和模型预测研究比较缺乏,通过KD2 Pro测试两种红黏土在较广温度范围(5~90℃)和含水率范围内的热导率,并选择IPCHT模型预测高温下体积含水率-热导率的变化规律。测试结果表明,两种红黏土的热导率对体积含水率的敏感程度与温度有关,且热导率均随温度的升高而增大,在90℃时热导率最高可达5℃的3~4倍。60~90℃范围内热导率随体积含水率的变化存在明显的临界含水率(对应土壤的塑性指数),但相同温度、体积含水率下,柳州红黏土中水汽潜热传输效应较桂林红黏土要明显。模型预测研究表明,除粉砂质黏壤土外,高温下IPCHT模型预测效果均不理想,经传质增强因子ξ修正后,柳州红黏土以及细砂的热导率预测值和实测值均相符得较好(RMSE < 30%),但桂林红黏土的整体预测效果仍较差。

       

      Abstract: Currently, there is a lack of experimental study and model prediction of thermal conductivity of soil under high temperature around the world. Tests are conducted through KD2 Pro on two kinds of lateritic clay within a wide range of temperatures(5~90℃) and water contents. Meanwhile, the IPCHT model is chosen to predict the variation of the volumetric water content and thermal conductivity under high temperature. The results of test indicate that the sensitivity of the thermal conductivity on the two kinds of lateritic clay to the volumetric water content is related to the temperature. The thermal conductivity increases with the increase of temperature. The thermal conductivity under 90℃ is 3 or 4 times as high as that under 5℃. The change of thermal conductivity with volumetric water content has obvious critical water content under 60~90℃(correspond to the plasticity index of soil). However, the latent heat transfer effect of water vapor in the lateritic clay of Liuzhou is more obvious than that in the lateritic clay of Guilin under the same temperature and volumetric water content. The results of model fit show that the prediction results of IPCHT model are not ideal except for the silty clay loam, after modification of the mass transfer enhancement factor ξ. The simulated values of the thermal conductivity of lateritic clay in Liuzhou and fine sand are in good agreement with the measured values(RMSE < 30%). However, the overall prediction effect of the lateritic clay in Guilin is still not ideal.

       

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