Shale Characterization Using T1-T2* Magnetic Resonance Relaxation Correlation Measurement at Low and High Magnetic Fields

Mohammad Sadegh Zamiri, Jiangfeng Guo, F. Marica, L. Romero-Zerón, B. Balcom
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Abstract

Shale characterization is complicated by low porosity and low permeability. Nano-porosity and a high degree of heterogeneity present further difficulties. 1H magnetic resonance (MR) methods have great potential to provide quantitative and spatially resolved information on fluids present in porous rocks. The shale MR response, however, is challenging to interpret due to short-lived signals that complicate quantitative signal detection and imaging. Multicomponent signals require high-resolution methods for adequate signal differentiation. MR methods must cope with low measurement sensitivity at low field. In this paper, T1-T2* and Look-Locker T1*-T2* methods were employed to resolve the shale signal for water, oil, and kerogen at high and low field. This permits fluid quantification and kerogen assessment. The T1-T2* measurement was employed to understand and control contrast in the single-point ramped imaging with T1 enhancement (SPRITE) imaging method. This permitted imaging that gave separate images of water and oil. Water absorption/desorption, evaporation, step pyrolysis, and water uptake experiments were monitored using T1-T2* measurement and MR imaging. The results showed (i) the capability of the T1-T2* measurement to differentiate and quantify kerogen, oil, and water in shales, (ii) the characterization of shale heterogeneity on the core plug scale, and (iii) demonstrated the key role of wettability in determining the spatial distribution of water in shales.
利用T1-T2*磁共振弛豫相关测量在低磁场和高磁场下表征页岩
页岩的低孔低渗特征使其表征变得复杂。纳米孔隙度和高度非均质性是进一步的困难。1H磁共振(MR)方法在提供多孔岩石中流体的定量和空间分辨信息方面具有很大的潜力。然而,页岩的MR响应很难解释,因为短时间信号使定量信号检测和成像变得复杂。多分量信号需要高分辨率的方法来充分区分信号。磁流变法必须解决低场测量灵敏度低的问题。本文采用T1-T2*和Look-Locker T1*-T2*两种方法对高、低场页岩水、油、干酪根信号进行了解析。这允许流体定量和干酪根评估。采用T1- t2 *测量来了解和控制单点斜坡成像与T1增强(SPRITE)成像方法的对比度。这使得成像可以得到水和油的独立图像。通过T1-T2*测量和MR成像监测吸水/解吸、蒸发、阶跃热解和吸水实验。结果表明:(1)T1-T2*测量能够区分和量化页岩中的干酪根、油和水,(2)在岩心塞尺度上表征页岩非均质性,(3)证明了润湿性在确定页岩中水的空间分布方面的关键作用。
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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