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An overview of the spectral induced polarization method for near-surface applications (Conference Paper)

机译:光谱感应极化方法在近地表应用中的概述(会议论文)

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Over the last 15 years significant advancements in induced polarization (IP) research have taken place, particularly with respect to spectral IP (SIP), concerning the understanding of the mechanisms of the IP phenomenon, the conduction of accurate and broadband laboratory measurements, the modelling and inversion of IP data for imaging purposes and the increasing application of the method in near-surface investigations. We summarize here the current state of the science of the SIP method for near-surface applications and describe which aspects still represent open issues and should be the focus of future research efforts. Significant progress has been made over the last decade in the understanding of the microscopic mechanisms of IP; however, integrated mechanistic models involving different possible polarization processes at the grain/pore scale are still lacking. A prerequisite for the advances in the mechanistic understanding of IP was the development of improved laboratory instrumentation, which has led to a continuously growing data base of SIP measurements on various soil and rock samples. We summarize the experience of numerous experimental studies by formulating key recommendations for reliable SIP laboratory measurements. To make use of the established theoretical and empirical relationships between SIP characteristics and target petrophysical properties at the field scale, sophisticated forward modelling and inversion algorithms are needed. Considerable progress has also been made in this field, in particular with the development of complex resistivity algorithms allowing the modelling and inversion of IP data in the frequency domain. The ultimate goal for the future are algorithms and codes for the integral inversion of 3D, time-lapse and multi-frequency IP data, which defines a 5D inversion problem involving the dimensions space (for imaging), time (for monitoring) and frequency (for spectroscopy). We also offer guidelines for reliable and accurate measurements of IP spectra, which are essential for improved understanding of IP mechanisms and their links to physical, chemical and biological properties of interest. We believe that the SIP method offers potential for subsurface structure and process characterization, in particular in hydrogeophysical and biogeophysical studies.
机译:在过去的15年中,在感应极化(IP)研究方面取得了重大进展,特别是在频谱IP(SIP)方面,涉及对IP现象机理的理解,准确和宽带实验室测量的进行,建模IP数据的反演和用于成像的目的,以及该方法在近地表调查中的越来越多的应用。我们在这里总结了近地面应用SIP方法的科学现状,并描述了哪些方面仍然代表着未解决的问题,应该成为未来研究工作的重点。在过去的十年中,在对知识产权微观机制的理解上取得了重大进展。但是,仍然缺乏涉及晶粒/孔尺度上不同极化过程的综合力学模型。对IP的机械理解的进步的先决条件是改进实验室仪器的发展,这导致对各种土壤和岩石样品进行SIP测量的数据库不断增长。我们通过制定可靠的SIP实验室测量的关键建议,总结了众多实验研究的经验。为了在田间尺度上利用SIP特性和目标岩石物理特性之间已建立的理论和经验关系,需要复杂的正演模型和反演算法。在这一领域,尤其是随着复杂电阻率算法的发展,允许在频域中对IP数据进行建模和反演,也取得了相当大的进步。未来的最终目标是对3D,延时和多频IP数据进行整体反演的算法和代码,它定义了一个5D反演问题,涉及空间(用于成像),时间(用于监视)和频率(用于光谱)。我们还为IP光谱的可靠和准确测量提供了指南,这对于增进对IP机制及其与感兴趣的物理,化学和生物学特性的联系至关重要。我们认为,SIP方法为地下结构和过程表征提供了潜力,尤其是在水文地球物理和生物地球物理研究中。

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