Experimental Study of Spectral Induced Polarization Response Based on Laboratory Measurement

D. A. Zaky, Suparwoto Suparwoto
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引用次数: 0

Abstract

The spectral induced polarization (SIP) method can provide apparent complex resistivity based on measurements of multi frequency. SIP method also can provide more detail information about physical properties of rocks and minerals because SIP can give spectral parameters or Cole-Cole parameters such as, changeability (m), time constant (τ) and frequency dependence (c). An Experimental study in laboratory has been conducted to knowing the SIP response of some test sample. The measurement system is built with digital oscilloscope Pico ADC-100 as device for sampling the input and output voltage. Amplifier is used to doubled up the signal and input differential. The range frequency of measurement is 10−2 Hz - 103 Hz. Porouspot Cu − CuSO4 is used to minimize the polarization at potential electrode. A Matlab listings is used to calculate the response of impedance and phase. The result from calibration that used the parallel circuit RC indicate that the measurement system was good. SIP response of porous model indicate that the response form an asymptotic resistivity, and the peak of phase is in the range frequency where the dispersion happen. The result also indicate that resistivity of small grain size model is larger than the big grain size model. Result from sample of mineralized rocks did not indicate a perfect SIP response, it is influenced by the contact between mineral and water was minimum.
基于实验室测量的光谱诱导极化响应实验研究
光谱诱导极化(SIP)方法可以根据多频测量结果提供视复电阻率。SIP方法还可以提供更多关于岩石和矿物物理性质的详细信息,因为SIP可以给出光谱参数或Cole-Cole参数,如可变性(m)、时间常数(τ)和频率依赖性(c)。为了了解某些测试样品的SIP响应,我们在实验室进行了实验研究。该测量系统采用Pico数字示波器ADC-100作为输入输出电压采样装置。放大器用于将信号和输入差分加倍。测量频率范围为10−2hz ~ 103hz。孔点Cu−CuSO4用于最小化电位电极的极化。利用Matlab列表计算了阻抗和相位的响应。采用并联电路RC进行标定,结果表明测量系统性能良好。多孔模型的SIP响应表明,响应形成了一个渐近电阻率,相位峰值位于色散发生的范围频率内。结果还表明,小晶粒尺寸模型的电阻率大于大晶粒尺寸模型。矿化岩石样品的SIP响应并不完美,受矿物与水接触的影响最小。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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