微地震监测技术在Y108水平井的应用

    Application of microseismic monitoring in horizontal well Y108

    • 摘要: 在复杂储层水平井压裂效果评价中,传统微地震监测应用存在两大核心痛点:一是仅依赖单一微地震数据,难以构建与地质条件精准匹配的连续裂缝网络;二是对微地震时空分布主控机制及地应力偏转成因解析不足,导致评价缺乏理论支撑。为此,本文以苏北盆地Y108水平井为研究对象,基于其压裂微地震响应特征,提出多学科参数耦合的微地震—裂缝网络协同建模方法。该方法突破传统单一数据驱动局限,将微地震数据与岩石性质、储层各向异性、岩相差异深度融合,通过最短路径连接准则构建连续裂缝网络,系统揭示微地震时空分布与岩石性质、应力参数的内在关联。研究结果表明:①微地震定位结果与蚂蚁体预测天然裂缝高度相关,构建的裂缝网络与主应力方向契合,符合地质认知;②明确阜四Ⅱ亚段各向异性强、微裂缝发育及岩相差异大是地应力偏转的核心驱动因素,深化了复杂储层压裂响应机制认知;研究成果既为Y108水平井压裂效果精准评估提供了可靠技术支撑,也为同类储层压裂优化设计提供了创新思路,兼具理论与工程价值。

       

      Abstract: In the evaluation of the performance of horizontal well fracturing for complex reservoirs, conventional microseismic monitoring faces two major challenges. First, reliance only on microseismic data renders it difficult to construct a continuous fracture network that precisely matches geological conditions. Second, insufficient analysis of both primary mechanisms governing the spatiotemporal distribution of microseismic events and the causes of in situ stress deflection leads to a lack of theoretical support in the evaluation. This study investigated the Y108 horizontal well in the North Jiangsu Basin. Based on the fracturing-induced microseismic responses of the well, this study proposes a multidisciplinary parameter-coupling method for collaborative microseismic-fracture network modeling. By deeply integrating microseismic data with rock properties, reservoir anisotropy, and lithofacies variations, the proposed method overcomes the limitations of conventional methods driven solely by microseismic data. By constructing a continuous fracture network using the shortest path connection criterion, this study systematically reveals the intrinsic relationship of the spatiotemporal distribution of microseismic events with rock properties and stress parameters. The results indicate that the localization results of microseismic events highly correlate with the distribution of natural fractures predicted based on the ant-tracking volume. The constructed fracture network aligns with the principal stress direction, conforming to geological understandings. The strong anisotropy, extensive microfractures, and significant lithofacies variations in the second submember of the fourth member of the Funing Formation are identified as the core factors driving in situ stress deflection, deepening the understanding of fracturing-induced response mechanisms in complex reservoirs. The results of this study provide reliable technical support for accurately assessing the fracturing performance of horizontal well Y108 and offer an innovative approach for optimizing the fracturing design of similar reservoirs, holding great theoretical and engineering value.

       

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