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CO2 storage monitoring: leakage detection and measurement in subsurface volumes from 3D seismic data at Sleipner

机译:二氧化碳封存监测:sleipner三维地震数据的地下体积泄漏检测和测量

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摘要

Demonstrating secure containment is a key plank of CO2 storage monitoring. Here we use the time-lapse 3D seismic surveys at the Sleipner CO2 storage site to assess their ability to provide robust and uniform three-dimensional spatial surveillance of the Storage Complex and provide a quantitative leakage detection tool. We develop a spatial-spectral methodology to determine the actual detection limits of the datasets which takes into account both the reflectivity of a thin CO2 layer and also its lateral extent. Using a tuning relationship to convert reflectivity to layer thickness, preliminary analysis indicates that, at the top of the Utsira reservoir, CO2 accumulations with pore volumes greater than about 3000 m3 should be robustly detectable for layer thicknesses greater than one metre, which will generally be the case. Making the conservative assumption of full CO2 saturation, this pore volume corresponds to a CO2 mass detection threshold of around 2100 tonnes. Within the overburden, at shallower depths, CO2 becomes progressively more reflective, less dense, and correspondingly more detectable, as it passes from the dense phase into a gaseous state. Our preliminary analysis indicates that the detection threshold falls to around 950 tonnes of CO2 at 590 m depth, and to around 315 tonnes at 490 m depth, where repeatability noise levels are particularly low. Detection capability can be equated to the maximum allowable leakage rate consistent with a storage site meeting its greenhouse gas emissions mitigation objective. A number of studies have suggested that leakage rates around 0.01% per year or less would ensure effective mitigation performance. So for a hypothetical large-scale storage project, the detection capability of the Sleipner seismics would far exceed that required to demonstrate the effective mitigation leakage limit. More generally it is likely that well-designed 3D seismic monitoring systems will have robust 3D detection capability significantly superior to what is required to prove greenhouse gas mitigation efficacy.
机译:证明安全遏制是二氧化碳封存监控的关键。在这里,我们使用Sleipner CO2储存站点上的延时3D地震勘测来评估其提供强大而统一的3D立体空间监视存储库并提供定量泄漏检测工具的能力。我们开发了一种空间光谱方法来确定数据集的实际检测极限,同时考虑到薄的CO2层的反射率及其横向范围。通过使用调谐关系将反射率转换为层厚,初步分析表明,在Utsira油藏顶部,孔厚大于约3000 m3的CO2积聚对于层厚大于1米的层应该可以被可靠地检测到,通常这将是案子。保守地假设完全CO2饱和,该孔体积对应于大约2100吨的CO2质量检测阈值。在覆盖层内,在较浅的深度,随着CO2从密相进入气态,它逐渐变得更具反射性,密度较小,并且相应地更易于检测。我们的初步分析表明,检测阈值在590 m深度下降到大约950吨CO2,在490 m深度下降到315吨,其中可重复性噪声水平特别低。检测能力可以等于符合其温室气体减排目标的存储地点的最大允许泄漏率。许多研究表明,每年约0.01%或更低的泄漏率将确保有效的缓解性能。因此,对于一个假设的大型存储项目,Sleipner地震的探测能力将远远超过证明有效缓解泄漏极限所需的探测能力。更一般而言,精心设计的3D地震监测系统可能具有强大的3D检测能力,大大优于证明温室气体缓解功效所需的能力。

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