地下核试验近场水热运移数值模拟

Water and Heat Flow Simulation After Underground Nuclear Test

  • 摘要: 根据内华达核试验场的一次地下核试验CHESHIRE的核爆破坏区情况和围岩水文地质信息,采用FEFLOW程序对试验的近场空间区域进行水热运移数值模拟,计算了空腔内熔岩玻璃体的温度下降曲线,计算结果与CHESHIRE现场温度测量结果相符。模拟结果表明,熔岩玻璃体的降温近似服从指数衰减规律,地下水对流散热是影响熔岩玻璃体降温的主要因素。

     

    Abstract: Based on the information about the damaged zone and local hydraulic data of CHESHIRE which is an underground nuclear test at the Nevada Test Site, a model was developed to simulate water and heat transport process using FEFLOW software. The temperature descending curve of the melt glass was acquired. The simulated temperature was consistent with the measured data. According to the simulation result, the temperature descending process obeys an exponent decay function, and the groundwater convection mainly affects the melt glass temperature descending process.

     

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