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Assessing the effect of velocity model accuracy on microseismic interpretation at the In Salah carbon capture and storage site

机译:评估速度模型精度对SALAH碳捕获和储存网站的微震解释对微震解释的影响

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Injection of carbon dioxide (CO2) to be stored at depth at the In Salah Carbon Capture and Storage (CCS) site began in 2004 with the subsequent installation of a pilot microseismic monitoring well in 2009. The project is one of only two industrial-scale storage projects to have been monitored for microseismicity. Such projects are vital to demonstrate the validity of CCS technology and the role of microseismic monitoring, a technology that could be used in real-time to regulate the geomechanical response of a site to CO2 injection. Substantial microseismicity (over 9000 events) was recorded by a single three-component geophone situated at 80m deep almost directly above one of the In Salah injection wells. The events occur in two main clusters with estimated locations of well-recorded events within one of these clusters to be within Ikm horizontal distance from the geophone and between 2.1km and 2.7km deep, at least 200m below the injection depth and CO2 storage interval. Errors in the depth range of event locations are investigated using modified velocity models, revealing that 10% slower velocities create uncertainties up to 450m in depth. Alternatively, 20% slower velocities in the shallow sub-surface or an anisotropic model have a similar effect. Independent of the absolute depth, there is no migration of event locations to shallower depths with time. Evidence from the analysis of shear-wave splitting delay times implies that, between 2009 and 2011, CO2 injection is opening pre-existing fractures that then close as pressure decreases, rather that creating new fractures. The estimated dominant fracture orientation is approximately NW-SE, in agreement with fracture orientations inferred from logging data, and the observed maximum moment magnitude, Mw = 1.7, is also consistent with estimated pre-existing fracture dimensions at the injection depth. This work demonstrates the value of microseismic monitoring of CCS projects, even with a limited array, but an accurate velocity model is critical to allow reliable interpretation of the data. We recommend that microseismic monitoring is conducted prior to CO2 injection at future CCS sites to enable baseline and comparative studies. Real-time microseismic monitoring would help inform injection decision and contribute to the safe operation of a project.
机译:在沙拉碳捕获和储存(CCS)现场储存的二氧化碳(CO2)注射储存在2004年的储存(CCS)现场储存,随后于2009年的试验微震监测井安装。该项目仅为两个工业规模之一要监控微震性的存储项目。这些项目对于展示CCS技术的有效性和微震监测的作用至关重要,这是一种可以实时使用的技术来规范部位的地质力学响应至CO2注射。在萨拉注射孔中的80米处,单个三组成的地震仪记录了大量的微震性(超过9000个事件)。该事件发生在两个主群中,其中一个主要群集,其中一个集群内的一个常录事件的位置,以在距地理孔的Ikm水平距离内,并且在2.1km和2.7km之间深度,在注射深度和CO2存储间隔以下至少200米。使用改进的速度模型研究了事件位置的深度范围内的误差,揭示了10%的速度较慢的速度产生高达450米的不确定性。或者,浅亚表面或各向异性模型中的20%较慢的速度具有类似的效果。独立于绝对深度,事件位置没有迁移到较浅的时间。来自分析剪切波分裂延迟时间的证据意味着,2009年至2011年,CO2注射正在打开预先存在的骨折,然后随后截止为压力,而是产生新的骨折。估计的主要断裂取向是大约NW-SE,与从测井数据推断的断裂取向一致,并且观察到的最大矩大小MW = 1.7也与注射深度的估计预先存在的断裂尺寸一致。这项工作展示了CCS项目的微震监测的价值,即使有一个有限的阵列,但准确的速度模型对于允许可靠地解释数据至关重要。我们建议在未来CCS站点的CO2注射之前进行微震监测,以实现基线和比较研究。实时微震监测将有助于提供注入决定并有助于项目的安全操作。

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