Feature and mechanism of geoelectric field related to atmospheric pressure
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摘要: 使用宁夏四个地电台站记录的地电场数据,研究其变化特征、频谱特征、与区域气压变化的关系及测量方向与附近断裂走向的关系。研究结果显示:部分地电场具有日变化特征,同时也具有气压非周期性变化特征,这种特征与气压变化呈负相关,当场地裂隙优势方位与附近断裂带方位呈近似垂直或较大夹角时,测向与附近断裂走向近垂直的地电场与气压相关性较高。分析认为地电场具有气压非周期变化特征是因为测量位置基岩孔隙的渗透率与附近断裂裂缝的渗透率不同,流体渗流过程中气压系统变化引起的流体“窜流”所致。Abstract: Using the geoelectric field data recorded by four geoelectric stations in Ningxia, the variation characteristics, spectral characteristics, the relationship with regional pressure variation, and the relationship between the measuring direction and the strike of nearby faults are studied. The research results show that part of the geoelectric field has diurnal variation characteristics, and also has the characteristics of non-periodic variation of atmospheric pressure, which is negatively correlated with the variation of atmospheric pressure, and the correlation is related to the angle between the measuring direction and the strike of nearby faults. It is considered that the geoelectric field has the characteristics of non-periodic change of atmospheric pressure is caused by the fluid “channeling” resulting from the change of air pressure system in the seepage process, which is due to the permeability difference between the bedrock pores and the nearby fault fractures.
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Keywords:
- geoelectric field /
- atmospheric pressure /
- non-periodic /
- variation characteristics
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表 1 海原和固原各测向地电场与气压的月相关系数
Table 1 Monthly correlation coefficient between geoelectric field and atmospheric pressure in Haiyuan and Guyuan
年-月 相关系数 年-月 相关系数 海原 固原 海原 固原 北南 东西 北南 东西 北东 北南 东西 北南 东西 北东 2018-01 −0.66 0.00 −0.36 −0.52 0.67 2019-01 −0.83 −0.11 −0.42 −0.63 0.75 2018-02 −0.77 0.12 −0.29 −0.07 0.64 2019-02 −0.76 −0.04 −0.22 −0.26 0.62 2018-03 −0.75 −0.21 −0.21 −0.62 0.52 2019-03 −0.73 −0.02 −0.27 −0.38 0.26 2018-04 −0.86 −0.16 −0.31 −0.56 0.19 2019-04 −0.71 −0.03 −0.25 −0.06 0.34 2018-05 −0.77 −0.19 −0.32 −0.59 0.57 2019-05 −0.83 0.23 −0.41 −0.54 0.42 2018-06 −0.76 0.10 −0.08 −0.46 −0.01 2019-06 −0.73 −0.07 −0.22 −0.21 0.46 2018-07 −0.58 −0.06 −0.30 −0.19 0.6 2019-07 −0.45 0.02 −0.06 −0.03 0.47 2018-08 −0.89 0.00 −0.35 −0.55 0.82 2019-08 −0.69 0.13 −0.02 −0.39 0.44 2018-09 −0.54 −0.05 −0.18 −0.65 −0.06 2019-09 −0.61 0.26 −0.14 −0.66 0.57 2018-10 −0.75 0.09 −0.24 −0.78 0.3 2019-10 −0.82 0.25 −0.33 −0.43 0.74 2018-11 −0.81 0.17 −0.41 −0.58 0.7 2019-11 −0.83 0.35 −0.61 −0.36 0.81 2018-12 −0.65 0.17 −0.43 −0.72 0.81 2019-12 −0.76 0.63 −0.50 −0.78 0.83 表 2 海原和固原各测向地电场与气温的月相关系数
Table 2 Monthly correlation coefficient between geoelectric field and temperature in Haiyuan and Guyuan
年-月 相关系数 年-月 相关系数 海原 固原 海原 固原 北南 东西 北南 东西 北东 北南 东西 北南 东西 北东 2018-01 0.46 0.15 0.20 0.39 −0.47 2019-01 0.35 0.25 0.30 0.27 −0.42 2018-02 0.48 −0.22 0.08 −0.28 −0.48 2019-02 0.35 −0.01 0.14 0.20 −0.24 2018-03 0.33 −0.21 0.11 −0.15 −0.33 2019-03 0.33 −0.17 −0.06 −0.27 −0.45 2018-04 0.50 −0.07 0.10 0.27 −0.06 2019-04 0.34 −0.06 0.00 −0.13 −0.46 2018-05 0.38 −0.15 −0.02 0.16 −0.42 2019-05 0.28 −0.01 0.03 0.05 −0.47 2018-06 0.09 −0.30 −0.22 0.20 −0.04 2019-06 0.12 −0.17 −0.25 −0.02 −0.48 2018-07 0.00 −0.27 0.09 −0.16 −0.23 2019-07 0.00 −0.23 0.13 0.27 −0.49 2018-08 0.17 −0.08 −0.22 0.25 −0.41 2019-08 0.34 −0.25 0.01 0.25 −0.50 2018-09 0.20 −0.01 −0.18 0.47 0.07 2019-09 0.32 −0.22 0.08 0.28 −0.51 2018-10 0.20 −0.04 0.03 0.01 −0.30 2019-10 0.23 −0.07 0.10 0.14 −0.52 2018-11 0.36 0.01 0.26 0.08 −0.50 2019-11 0.40 −0.07 0.22 0.47 −0.53 2018-12 0.52 −0.11 0.32 0.29 −0.57 2019-12 0.40 −0.10 0.29 0.06 −0.54 表 3 2019年7—12月海原、固原、银川和石嘴山电台各测向地电场与气压相关系数以及各测向与附近断裂走向的夹角
Table 3 Correlation coefficients between geoelectric field and atmospheric pressure in Haiyuan,Guyuan,Shizuishan and Yinchuan geoelectric stations from July to December in 2019 and the angles between each measuring direction and the strike of nearby faults
台站 测向 相关系数 夹角/° 7月 8月 9月 10月 11月 12月 平均值 海原 NS 0.45 0.69 0.61 0.82 0.83 0.76 0.69 70 EW 0.02 0.13 0.26 0.25 0.35 0.63 0.27 20 固原 NS 0.06 0.02 0.14 0.34 0.61 0.50 0.28 40 EW 0.03 0.39 0.66 0.44 0.36 0.78 0.44 50 NE 0.47 0.44 0.57 0.75 0.81 0.83 0.65 85 银川 NS 0.11 0.32 0.01 0.03 0.02 0.50 0.17 0 EW 0.13 0.37 0.67 0.21 0.19 0.47 0.34 90 NE 0.01 0.40 0.31 0.06 0.20 0.04 0.17 45 石嘴山 NS 0.25 0.25 0.51 0.10 0.30 0.43 0.31 15 EW 0.19 0.27 0.70 0.56 0.28 0.56 0.43 75 NW 0.12 0.68 0.66 0.43 0.53 0.61 0.51 60 表 4 各台站主压应力方向、裂隙优势方位角及各测向与附近断裂走向的夹角
Table 4 Principal compressive stress direction and dominant fracture azimuth of each station and the angle between each measuring direction and the strike of nearby faults
主压应力方向/° 裂隙优势方位角/° 附近断裂走向/° 地电场测向与附近断裂走向夹角/° NS EW NE 海原 60 71 290 70 20 固原 60 12 320 40 50 85 银川 42 16 0 0 90 45 石嘴山 26 28 15 15 75 60 (NW) -
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