Ground natural potential data acquisition processing method based on minor cycle plane multipolar synchronous base point
A self-potential and small-cycle technology, applied in the field of geophysical exploration, can solve problems such as unguaranteed data quality, difficult drift control, and difficulty in distinguishing true and false natural potentials.
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Embodiment 1
[0109] Embodiment 1: The following is the data acquisition method of multi-pole synchronous base point data on the ground natural potential small cycle plane. The implementation steps are as follows:
[0110] (1) Choose to lay out a base point in a place where the terrain in the work area is flat and far away from industrial power grids, substations and other equipment. The base point electrode layout method adopts two electrodes, the deep layer electrode b2 and the shallow layer electrode b1, which are arranged longitudinally. The buried depth of the deep layer electrode is 130cm, and the buried depth of the shallow layer electrode is 30cm. During the daily construction period, an instrument automatically records the natural potential time series of the deep and shallow electrodes at the base point (synchronized with ordinary measuring points) U b2 (t i ), (i=1, n); U b1 (t i ), (i=1, n). Calculate the difference ΔU b (t i ) = U b1 (t i )-U b2 (t i ), (i=1, n).
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Embodiment 2
[0148] Embodiment 2: The following is the data acquisition method of multi-pole synchronous base point data on the ground natural potential small cycle plane. The implementation steps are as follows:
[0149] (1) Choose to lay out a base point near the work area where the terrain is flat and away from industrial power grids, substations and other equipment. The base point electrode layout method adopts two electrodes, the deep layer electrode b2 and the shallow layer electrode b1, which are arranged longitudinally. The buried depth of the deep layer electrode is 130cm, and the buried depth of the shallow layer electrode is 30cm. During the daily construction period, an instrument automatically records the natural potential time series of the deep and shallow electrodes at the base point (synchronized with ordinary measuring points) U b2 (t i ), (i=1, n); U b1 (t i ), (i=1, n). Calculate the difference ΔU b (t i ) = U b1 (t i )-U b2 (t i ), (i=1, n).
[0150] (2) Di...
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