The unsteady heat transfer test of the surrounding rock

Wu Lei, Z. Qing
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引用次数: 1

Abstract

The heat transfer between airway and airflow is an unsteady problem. Three experimental schemes (1, Variable wind temperature, the temperature of air flow are 15°C, 20°C, 25°C, 30°C; 2, Variable speed, wind speed are 1m/s, 2m/s, 3m/s; 3, Periodic wind temperature, 15°C∼25°C and 20°C∼30°C) are used to simulate the actual heat transfer process between airway and airflow. Test results show that it exists obvious unstable heat transfer characteristics; the temperature of airway is stable in the last. And the temperature increased with the decreasing difference in temperature between air flow and surrounding rock; and the time required to reach a steady was reduced; with the increase of airflow speed, the stable temperature of the soil was lower and the time required to reach a steady was reduced; when airflow temperature periodic changes, the heat transfer in the soil has obvious "lag" effect. The entire heat transfer process can be divided into severe heat section, excessive heat segment and stable heat section.
围岩非定常换热试验
气道与气流之间的换热是一个非定常问题。三种实验方案(1、变风温,气流温度分别为15℃、20℃、25℃、30℃;2、变频调速,风速有1m/s、2m/s、3m/s;3、周期性风温(15°C ~ 25°C和20°C ~ 30°C)用于模拟气道与气流之间的实际传热过程。试验结果表明,它存在明显的不稳定传热特性;最后气道温度稳定。温度随气流与围岩温差的减小而升高;达到稳定所需的时间减少了;随着风速的增大,土壤的稳定温度降低,达到稳定所需的时间缩短;当气流温度周期性变化时,土壤中的换热具有明显的“滞后”效应。整个传热过程可分为剧烈热段、过热段和稳定热段。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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