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SPECTRAL INDUCED POLARIZATION: A NEW WAY FOR HYDROCARBON PROSPECT PREDICTION

机译:谱诱发的极化:预测烃的新方法

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The Induced Polarization (IP) method extends the resistivity method by making an additional measurement of the ability of the ground to store electrical charge. IP instruments measure both the conductive and capacitive properties of the subsurface using either time domain or frequency domain techniques. Spectral Induced Polarization (SIP) is generalization method of IP. Principle of SIP measurement is finding the sequence of time series is used to produce the resistivity spectrum. It can be used to measures the complex resistivity in dependence of frequency, remove EM coupling effects from IP data, and to identify the source of the IP response. Through these advantages, it is more reliable to detect hydrocarbon prospect. Since IP is sensitive to surface area with enhanced oxidation due to contaminant conversion, hydrocarbon prospect area indicates high resistivity very clearly.Data acquisition has improved using high-power transmitter, receiver with GPS-synchronization, CPU controls each auxiliary acquisition unit, and receives data via two-way wireless communication. Data processing approach to spectral parameters (phase-staggered fitting) that is designed for dipole-dipole SIP uses Cole-Cole and Brown Models. The combined model can be used to calculate electromagnetic spectral, resistivity and phase contrast, and then extract four spectral IP parameters by inverting and fitting the amplitude and phase spectra obtained by normalizing observed apparent resistivity.The SIP system provides more efficient field work, better signal-to-noise ratio, and increased exploration depth rather than the conventional method. However, equipment is heavy and field operations are relatively slow, particularly in complicated areas. Many tests and predictions have shown the usefulness of the method checkingknown traps for hydrocarbon, exploring for new hydrocarbon trap, and for optimizing drilling location.
机译:感应极化(IP)方法通过对地面存储电荷的能力进行额外的测量,从而扩展了电阻率方法。 IP仪器使用时域或频域技术来测量地下的导电性和电容性。光谱诱导极化(SIP)是IP的推广方法。 SIP测量的原理是找到用于产生电阻率谱的时间序列。它可用于测量依赖于频率的复电阻率,消除IP数据中的EM耦合效应,并确定IP响应的来源。通过这些优点,检测碳氢化合物前景更加可靠。由于IP对污染物敏感的表面积具有增强的氧化作用,因此很敏感,因此烃类勘探区非常清楚地显示出高电阻率。 使用大功率发射器,具有GPS同步的接收器,CPU控制每个辅助采集单元并通过双向无线通信接收数据,从而改善了数据采集。专为偶极-偶极SIP设计的光谱参数数据处理方法(相位交错拟合)使用Cole-Cole和Brown模型。组合模型可用于计算电磁频谱,电阻率和相位对比,然后通过对通过归一化观察到的视电阻率而获得的幅度和相位频谱进行求逆和拟合来提取四个频谱IP参数。 与传统方法相比,SIP系统提供了更有效的现场工作,更好的信噪比和更大的探测深度。但是,设备笨重,现场操作相对较慢,尤其是在复杂区域。许多测试和预测表明方法检查的有用性 已知的碳氢化合物捕集阱,探索新的碳氢化合物捕集阱,以及优化钻井位置。

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