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Hydrocarbon saturation in a Lower-Paleozoic organic-rich shale gas formation based on Markov-chain Monte Carlo stochastic inversion of broadband electromagnetic dispersion logs

机译:基于宽带电磁弥散测井的马尔可夫链蒙特卡洛随机反演的下古生界富有机质页岩气中的烃饱和度

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摘要

An organic-rich shale gas formation generally exhibits high clay content, high total organic carbon (TOC), low porosity, high tortuosity, and the presence of conductive pyrite that adversely affect the well-log-derived hydrocarbon saturation estimations. In the presence of such petrophysical conditions, log-derived hydrocarbon saturation estimates obtained from multi-mineral analysis solver and various subsurface electromagnetic (EM) logs, such as induction resistivity log, dielectric permittivity log, or dielectric dispersion logs, are not consistent and can vary up to 0.5 saturation unit for a single depth. In addition, hydrocarbon saturation estimates derived from EM logs using conventional saturation models tend to break down in organic-rich shale gas formation because of the unaccounted interfacial polarization effects of clays and conductive minerals. Several of the above-mentioned issues can be addressed by processing downhole broadband EM dispersion logs using a mechanistic clay-pyrite interfacial-polarization model to accurately estimate hydrocarbon saturation in organic-rich shale gas formations.EM induction resistivity, logging while drilling (LWD) propagation, and dielectric dispersion logging tools were jointly deployed in a well drilled in an organic-rich shale gas formation to acquire continuous broadband EM dispersion measurements at 7 EM-log-acquisition frequencies for a total depth of 1500 m in the well. This was the first ever acquisition of broadband EM dispersion logs, comprising relative permittivity and conductivity measured at the 7 EM-log-acquisition frequencies. In this paper, a new Markov-chain Monte-Carlo-based (MCMC) stochastic inversion scheme coupled with a clay-pyrite interfacial-polarization (IP) model is used to process the EM broadband dispersion logs, and simultaneously estimate hydrocarbon saturation, connate water conductivity, and surface conductance of clay in the shale gas formation. The proposed Markov-chain Monte Carlo-based stochastic inversion scheme is robust to noise and exhibits fast convergence. The estimated hydrocarbon saturation is also compared against those derived from resistivity log, dielectric dispersion logs, and multi-mineral analysis solver. The estimated hydrocarbon saturation, connate water conductivity, and surface conductance of clay in two specific intervals of the shale gas formation are in the ranges of 0.2-0.9, 0.1 S/m-0.25 S/m, and 1 x 10(-7) S-1 x 10(-6) S, respectively.
机译:富含有机物的页岩气地层通常表现出高粘土含量,高总有机碳(TOC),低孔隙度,高曲折度和导电黄铁矿的存在,这些不利影响对测井得出的烃饱和度估计值。在存在此类岩石物理条件的情况下,从多矿物分析求解器和各种地下电磁(EM)测井(例如感应电阻率测井,介电常数测井或介电弥散测井)获得的对数推导的烃饱和度估算值不一致,并且可以对于单个深度,最大变化为0.5饱和度单位。此外,由于粘土和导电性矿物的界面极化作用无法解释,因此使用常规饱和度模型从EM测井得到的碳氢化合物饱和度估计往往会在富含有机物的页岩气中分解。通过使用机械粘土-黄铁矿界面极化模型处理井下宽带EM分散测井,以准确估算富含有机物的页岩气地层中的烃饱和度,可以解决上述几个问题.EM感应电阻率,随钻测井(LWD)传播和介电色散测井工具被联合部署在富含有机物的页岩气地层中的一口井中,以7个EM测井采集频率连续进行宽带EM色散测量,测井总深度为1500 m。这是宽带EM色散测井的首次采集,包括在7个EM对数采集频率下测得的相对介电常数和电导率。本文采用了一种新的基于马尔可夫链的蒙特卡洛随机(MCMC)随机反演方案并结合了粘土-黄铁矿界面极化(IP)模型来处理EM宽带色散测井,​​同时估算了烃饱和度,页岩气形成过程中水的电导率和粘土的表面电导率。提出的基于马尔可夫链的基于蒙特卡洛的随机反演方案对噪声具有鲁棒性,并且具有快速收敛性。还将估算的烃饱和度与由电阻率测井,介电弥散测井和多矿物分析求解器得出的烃饱和度进行比较。在页岩气形成的两个特定时间段内,估计的烃饱和度,原生水电导率和粘土的表面电导率在0.2-0.9、0.1 S / m-0.25 S / m和1 x 10(-7)的范围内S-1 x 10(-6)S。

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