Extraction of High Chargeability Distribution using Joint Inversion of Direct Current Resistivity and Time Domain Induced Polarization Data: A Development and Test Results on Uranium Bearing Target Rock

IF 1.9 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Vishnu Kant Verma, Shalini Singh, Anand Singh
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引用次数: 0

Abstract

Induced polarization datasets, which assess the overvoltage characteristics of the subsurface, are becoming increasingly prevalent. These datasets are not limited to mineral resource exploration but are also gaining traction in various engineering applications. We present the result of joint inversion of direct current resistivity and induced polarization data. We have obtained two subsurface properties: electrical resistivity and chargeability, by minimizing the single objective function. For this purpose, we have computed the distorted apparent resistivity using the secondary voltage measure at each time gate. We compared our results with the conventional inversion of induced polarization on synthetic data with both high and low chargeable mineralized ore bodies. We noted that our approach provides a more reasonable model for high chargeable ore bodies. However, both joint inversion and nonlinear approaches give similar results for low-chargeable ore bodies. Nonlinear inversion of induced polarization was accomplished by solving two objective functions: One for resistivity and another one for induced polarization. Thus, error in the resistivity inversion propagates in the chargeability computation due to consequences. Further, the developed joint inversion algorithm is also applied to a field data set measured at the Beldih mine located in the West Bengal, India. We compared our final chargeability models with the local geology and geologic models obtained via other geophysical methods on the same profiles and found an excellent correlation in both models.

利用直流电阻率和时域诱导极化数据的联合反演提取高电荷率分布:含铀靶岩的开发与测试结果
摘要 评估地下过电压特征的感应极化数据集正变得越来越普遍。这些数据集不仅限于矿产资源勘探,在各种工程应用中也越来越受到重视。我们介绍了直流电阻率和感应极化数据联合反演的结果。通过最小化单一目标函数,我们获得了两种地下属性:电阻率和带电率。为此,我们利用每个时间门的二次电压测量值计算了扭曲的视电阻率。我们将我们的结果与传统的感应极化反演结果进行了比较,并对高电荷和低电荷矿体的合成数据进行了比较。我们注意到,我们的方法为高电荷矿体提供了更合理的模型。不过,联合反演和非线性方法对低电荷矿体的结果相似。感应极化的非线性反演是通过求解两个目标函数完成的:一个是电阻率目标函数,另一个是感应极化目标函数。因此,电阻率反演中的误差会在电荷率计算中传播。此外,开发的联合反演算法还应用于在印度西孟加拉邦贝尔迪赫矿区测量的现场数据集。我们将最终的电荷率模型与在相同剖面上通过其他地球物理方法获得的当地地质和地质模型进行了比较,发现两种模型之间具有极好的相关性。
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来源期刊
pure and applied geophysics
pure and applied geophysics 地学-地球化学与地球物理
CiteScore
4.20
自引率
5.00%
发文量
240
审稿时长
9.8 months
期刊介绍: pure and applied geophysics (pageoph), a continuation of the journal "Geofisica pura e applicata", publishes original scientific contributions in the fields of solid Earth, atmospheric and oceanic sciences. Regular and special issues feature thought-provoking reports on active areas of current research and state-of-the-art surveys. Long running journal, founded in 1939 as Geofisica pura e applicata Publishes peer-reviewed original scientific contributions and state-of-the-art surveys in solid earth and atmospheric sciences Features thought-provoking reports on active areas of current research and is a major source for publications on tsunami research Coverage extends to research topics in oceanic sciences See Instructions for Authors on the right hand side.
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