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本文根据福建省龙岩盆地王坑井田的部分测温资料,分析了井田近地表温度在水平方向和垂直方向上的分布规律及灰岩含水层中地下水的运动对温度场的影响。在此基础上,提出了在地下水运动较强烈的地区进行稳态和非稳态测温方法以及孔底温度半对数直线校正法。
Based on the partial temperature data of Wangkeng Minefield in Longyan Basin, Fujian Province, the distribution of near surface temperature in the mine field in horizontal direction and vertical direction and the effect of groundwater movement on the temperature field in limestone aquifer were analyzed. On this basis, the steady-state and unsteady temperature measurement methods and semi-logarithmic linear correction method of the bottom hole temperature are put forward in the areas with strong groundwater movement.