分布式光纤技术在深部煤层二氧化碳地质封存监测中的适配性及关键补位作用

Adaptability and key complementary role of distributed optical fiber technology in the monitoring of deep coal seam carbon dioxide geological storage

  • 摘要: 深部煤层二氧化碳(CO2)地质封存面临高地应力、强非均质性及“流−固−热−化”多场耦合等极端储层挑战。传统地球物理监测方法因时空连续性不足,难以实现井筒及近井区连续、高分辨率、多参量的动态感知,成为制约流体精准成像与风险预警的瓶颈。围绕“渗透率骤降−瞬态应力集中−强非均质信号掩蔽”三大判据,指出当前监测体系的核心缺失在于近井区连续动态感知层。针对上述短板,重构了分布式光纤传感技术(Distributed Fiber-Optic Sensing, DFOS)的工程应用逻辑,提出其核心价值并非新型可选监测手段,而是弥补现有体系关键能力短板的“关键感知层”。立足于深部煤层吸附主导、基质膨胀与微裂隙动态演化的特殊响应特征,系统梳理了分布式温度传感(DTS)、分布式声学传感(DAS)和分布式应变传感(DSS)的适配路径:DTS追踪注入剖面与热−流演化,DAS兼具被动微震监测与主动时移波场成像功能,DSS聚焦基质吸附膨胀与储层原位形变,三者依托同一井下平台实现“温度−声波−应变”原位协同监测,为解析煤层复杂流固耦合机制提供了关键技术手段。在体系协同层面,研究确立了DFOS在“空−天−地−井”立体监测网多尺度联合反演中的核心边界约束地位,将监测体系从“多种孤立方法并存”转化为“以井下连续时间轴为骨架的协同反演系统”,为破解多源信号反演多解性难题提供了可行路径。进一步归纳了微弱信号捕获、封存量精准核算、反演多解性、全周期监测成本及专属标准缺失等5方面技术挑战,总结了完善立体观测体系、建立多模态联合探测、探明煤层专属光纤响应机制及构建标准化体系等关键研究方向。研究为构建深部煤层CO2动态监测与长效安全预警体系提供了系统性方法框架。

     

    Abstract: Geological sequestration of carbon dioxide (CO2) in deep coal seams is confronted by formidable reservoir challenges, encompassing high in-situ stress, pronounced heterogeneity, and complex thermo-hydro-mechanical-chemical (THMC) coupling. Conventional geophysical monitoring methods, constrained by limited spatio-temporal continuity, are inherently incapable of achieving continuous, high-resolution, multi-parameter dynamic perception within the wellbore and near-wellbore zones, thereby constituting a critical bottleneck for precise fluid imaging and early risk warning. Scrutinizing the monitoring demands specific to deep coal seam CO2 storage, three semi-quantitative criteria are delineated, namely, permeability impairment, transient stress concentration, and signal masking under strong heterogeneity, revealing the core capability deficit in current monitoring frameworks: the absence of a continuous dynamic perception layer in the near-wellbore region. Addressing this capability gap, the engineering application logic of Distributed Fiber-Optic Sensing Sensing (DFOS) is reconceptualised. Its core value resides not in its role as an optional supplementary technique, but rather as an indispensable “critical perception layer” that bridges the key capability shortfalls of existing monitoring systems. Grounded in the distinctive physico-mechanical responses of deep coal reservoirs, namely, adsorption-dominated mechanisms, matrix swelling, and the dynamic evolution of micro-fractures, the adaptive pathways for Distributed Temperature Sensing (DTS), Distributed Acoustic Sensing (DAS), and Distributed Strain Sensing (DSS) in deep coal seam scenarios are systematically elucidated. DTS tracks injection profile evolution and thermo-hydraulic dynamics; DAS integrates a dual-modal mechanism encompassing passive microseismic detection and active time-lapse wavefield imaging; DSS targets matrix adsorption-induced swelling and in-situ reservoir deformation. Through a unified downhole platform, the synergistic integration of these three modalities facilitates in-situ “temperature-acoustic-strain” coordinated monitoring, thereby furnishing a pivotal technical means for resolving complex fluid-solid coupling mechanisms in coal seams. At the system level, DFOS is established as the core boundary constraint within the multi-scale joint inversion framework of the comprehensive “space-air-ground-well” three-dimensional monitoring network. The continuous, high-density downhole data acquired by DFOS furnish high-precision in-situ constraints for time-lapse seismic macro-plume imaging, cross-well electromagnetic fluid identification, and microseismic fracture activity monitoring, transforming the monitoring paradigm from the “coexistence of multiple isolated methods” to a “collaborative inversion system anchored by a continuous downhole timeline”. This integration offers a viable pathway to mitigate the non-uniqueness inherent in multi-source signal inversion under conditions of pronounced heterogeneity. Five core technical challenges confronting deep coal seam CO2 storage monitoring are synthesised: reliable capture of weak signals within strongly heterogeneous preferential flow channels, accurate storage capacity quantification under non-negligible adsorbed-phase volume, inversion non-uniqueness driven by multi-field coupling, constraints imposed by full-lifecycle monitoring costs on commercialisation, and the absence of coal-seam-specific monitoring standards and regulatory frameworks. Correspondingly, six prospective research directions are delineated: refining the integrated “space-air-ground-well” observation system, establishing a “one-cable-multi-measurement” multi-modal joint detection methodology, elucidating coal-seam-specific fibre-optic response mechanisms, reinforcing DFOS as the core constraint in joint inversion, developing low-cost modular application schemes, and constructing a long-term standardised application framework. Collectively, these findings furnish a systematic methodological framework for bridging the technical gap in near-wellbore dynamic perception and advancing high-precision, cost-effective dynamic monitoring and long-term safety early-warning systems for deep coal seam CO2 sequestration.

     

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