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    • 2. 发明授权
    • Using electrical resistance tomography to map subsurface temperatures
    • 使用电阻断层扫描来映射地下温度
    • US5346307A
    • 1994-09-13
    • US072601
    • 1993-06-03
    • Abelardo L. RamirezDwayne A. ChesnutWilliam D. Daily
    • Abelardo L. RamirezDwayne A. ChesnutWilliam D. Daily
    • G01K13/00G01N27/04G01N33/24G01K3/00G01K7/16
    • G01N27/043G01K13/00G01N33/24
    • A method is provided for measuring subsurface soil or rock temperatures remotely using electrical resistivity tomography (ERT). Electrical resistivity measurements are made using electrodes implanted in boreholes driven into the soil and/or at the ground surface. The measurements are repeated as some process changes the temperatures of the soil mass/rock mass. Tomographs of electrical resistivity are calculated based on the measurements using Poisson's equation. Changes in the soil/rock resistivity can be related to changes in soil/rock temperatures when: (1) the electrical conductivity of the fluid trapped in the soil's pore space is low, (2) the soil/rock has a high cation exchange capacity and (3) the temperature changes are sufficiently high. When these three conditions exist the resistivity changes observed in the ERT tomographs can be directly attributed to changes in soil/rock temperatures. This method provides a way of mapping temperature changes in subsurface soils remotely. Distances over which the ERT method can be used to monitor changes in soil temperature range from tens to hundreds of meters from the electrode locations.
    • 提供了一种使用电阻率层析成像(ERT)远程测量地下土壤或岩石温度的方法。 使用植入到土壤和/或地面的钻孔中的电极进行电阻率测量。 重复测量,因为一些过程会改变土壤质量/岩体的温度。 基于使用泊松方程的测量计算电阻率的断层图。 土壤/岩石电阻率的变化可能与土壤/岩石温度的变化有关:(1)被困在土壤孔隙中的流体的导电性低,(2)土壤/岩石具有较高的阳离子交换能力 和(3)温度变化足够高。 当这三个条件存在时,ERT断层扫描仪观察到的电阻率变化可以直接归因于土壤/岩石温度的变化。 这种方法提供了一种远程映射地下土壤温度变化的方法。 使用ERT方法监测土壤温度范围从距离电极位置几十米到几百米的距离。