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Study of negative polarizability phenomenon due to using induced polarization method in saline-alkali area

机译:盐碱区域中诱导偏振法的负极化现象研究

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When we work in the use of induced polarization method, the strength of secondary field signal of the underground body plays a decisive role in the observations. In different geological background, the impact factors are also different. Using the induced polarization method under the conditions of large power-supply polar distance and saline-alkali area will product negative polarizability phenomenon.we analyze the mechanism of negative polarizability phenomenon. With the power pole distance increasing (power supply limited) resulting in a diminished primary field (Artificial current primary field) conditions, we reaserch relative changes in the law of the effective polarization of secondary field (induced polarization field) strength and interference signal strength. we also explore the reason of stabilizing negative polarizability abnormalities under conditions of the particular small-signal and low resistance of subsurface. Besides,we give a method to Suppression of interfering factors, improving the effective signal components when the negative polarizability phenomenon happens.
机译:当我们在使用诱导的极化方法时,地下体的次级场信号的强度在观察中起着决定性作用。在不同的地质背景中,影响因素也不同。利用诱导的偏振方法在大电源极距离和盐碱面积的条件下将产品负极极化性现象。我们分析了负极化现象的机理。利用电力极距离增加(电源限制)导致主要场(人工电流域)条件减弱,我们将相对变化进行相对变化的次级场(诱导偏振场)强度和干扰信号强度的有效极化定律。我们还探讨了在特定小信号的条件下稳定负极化异常的原因,以及地下的低电阻。此外,我们给出了抑制干扰因素的方法,当发生负极化现象时改善有效信号分量。

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