页岩中次生Fe(OH)3相表征与建模

IF 5.3 3区 工程技术 Q2 ENERGY & FUELS
Qingyun Li*, , , Cynthia M. Ross*, , , Zuhao Kou, , , Vladimir Alvarado, , and , Saman A. Aryana, 
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引用次数: 0

摘要

水力压裂涉及将大量水基流体注入页岩地层,形成复杂的裂缝网络,从而导致页岩和注入物之间发生化学相互作用。本研究通过实验和建模方法研究了酸性压裂液与页岩岩心相互作用所导致的矿物学变化,重点研究了铁(氢)氧化物Fe(OH)3的二次沉淀。实验采用了两种条件:一种是纯盐水,即页岩全程与地层盐水反应;另一种是B + S,即中途注入增产液与反应中的盐水混合。聚焦离子束扫描电镜(FIB-SEM)和扫描电镜(SEM)显示了页岩中次要次生Fe(OH)3相的形态和空间分布。发现次生Fe(OH)3的两相结构:(1)一相取代黄铁矿而保留其草莓状结构(微晶黄铁矿球形团簇);(2)另一相在铁白云石溶解形成的次生孔隙中形成松散的团簇聚集体。Fe(OH)3的两种次级相均在纳米尺度的空间内析出。在固相表征的基础上,建立了基于实验装置的反应输运模型,以探索控制页岩基质中次生Fe(OH)3分布的关键因素。根据实验结果进行校准表明:(1)两个次级Fe(OH)3相具有相似的溶解度;(ii)黄铁矿取代Fe(OH)3的反应速率较低;(3)二次Fe(OH)3的分布受实验设计的影响。本研究的发现为在实验设计的背景下解释实验结果提供了一个框架。此外,它们有助于更好地理解页岩中次生Fe(OH)3的形成及其对页岩基质内输运过程的潜在影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Characterization and Modeling of Secondary Fe(OH)3 Phases in Stimulated Shale

Characterization and Modeling of Secondary Fe(OH)3 Phases in Stimulated Shale

Hydraulic fracturing involves the injection of large volumes of water-based fluids into shale formations to create complex fracture networks, leading to opportunities for chemical interactions between shale and injectates. This study examines the mineralogical alterations resulting from the interaction between acidic stimulation fluids and a shale core using experimental and modeling approaches, focusing on secondary precipitation of ferric (hydr)oxides, Fe(OH)3. Two experimental conditions were used: a brine-only case, where the shale was reacted with formation brine throughout, and a B + S case, where stimulation fluid was introduced midway to mix with the reacting brine. Focused ion beam-equipped scanning electron microscopy (FIB-SEM) and SEM provided the morphology and spatial distribution of minor secondary Fe(OH)3 phases in shale. Two phases of secondary Fe(OH)3 were revealed: (1) one phase replaced pyrite while preserving its framboidal structure (spherical clusters of microcrystalline pyrite), and (2) the other formed loosely clustered aggregates in secondary pores generated by ankerite dissolution. Both secondary phases of Fe(OH)3 precipitated within nanoscale spaces. Following solid-phase characterization, a reactive transport model was developed based on the experimental setup to explore the key factors controlling secondary Fe(OH)3 distribution within the shale matrix. Calibration against experimental observations suggested that (i) both secondary Fe(OH)3 phases exhibited similar solubilities; (ii) pyrite-replacing Fe(OH)3 had a lower reaction rate; and (iii) the distribution of secondary Fe(OH)3 was influenced by the experimental design. Findings from this study provide a framework for interpreting experimental results within the context of the experimental design. Additionally, they contribute to a better understanding of secondary Fe(OH)3 formation in shale and its potential impact on transport processes within shale matrices.

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来源期刊
Energy & Fuels
Energy & Fuels 工程技术-工程:化工
CiteScore
9.20
自引率
13.20%
发文量
1101
审稿时长
2.1 months
期刊介绍: Energy & Fuels publishes reports of research in the technical area defined by the intersection of the disciplines of chemistry and chemical engineering and the application domain of non-nuclear energy and fuels. This includes research directed at the formation of, exploration for, and production of fossil fuels and biomass; the properties and structure or molecular composition of both raw fuels and refined products; the chemistry involved in the processing and utilization of fuels; fuel cells and their applications; and the analytical and instrumental techniques used in investigations of the foregoing areas.
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