Use of Subsurface Geology in Assessing the Optimal Co-Location of CO2 Storage and Wind Energy Sites

I. de Jonge-Anderson, J. Underhill
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Abstract

Opportunities exist to re-purpose depleted gas fields in the Southern North Sea as CO2 storage sites if, where and when they meet the right set of geological, engineering, and non-technical criteria. Fields positioned on the western edge of the basin are attractive as they lie close to the major industrial emitters of East England which need to decarbonise if the UK’s Net Zero targets are to be met. Having stopped production in 2018, Pickerill has CO2 storage potential as it is a proven trap from which around 440 Bcf of gas has been produced and it is located near the coastline. We use a public-domain 3D seismic dataset, wireline logs, core reports and production data to assess its CO2 storage potential. The Rotliegend Group reservoir (Leman Sandstone Formation) is a mixed aeolian/fluvial succession with variable thickness (25 m–80 m), high net-to-gross (0.9–1.0), moderate average porosity (9%–17%) and fair-average permeability (>1 mD). The seal is Zechstein Group evaporites and carbonates which thin and swell in response to their post-depositional mobility (halokinesis), further affecting and deforming the overburden. The structure is defined to the south by a WNW-ESE-striking fault system, but the north of the field is characterised mostly by dip closure of the reservoir. NW-SE-striking faults transect the field and segment the structure into several compartments, three of which appear particularly good candidates for CO2 storage and have a combined CO2 storage capacity of 32 MtCO2. If combined with nearby satellite fields, there is potential for the development of a CO2 storage cluster capable of sequestering 60 MtCO2, however, this potential is challenged by the planned development of an offshore wind farm. Turbines fixed to the seabed over the field would restrict where new CO2 injection wells might be drilled and efforts to measure, monitor and verify the CO2 plume using conventional towed-streamer seismic. There is an urgent need to resolve the competition for offshore acreage to ensure that attractive CO2 storage sites like Pickerill are not disadvantaged but can play a full part in complementing alternative renewable energy sources within the energy transition.
利用地下地质评估二氧化碳储存和风能站点的最佳共存位置
如果满足地质、工程和非技术标准,北海南部枯竭的天然气田将有机会成为二氧化碳储存地。位于盆地西部边缘的油田很有吸引力,因为它们靠近英格兰东部的主要工业排放者,如果要实现英国的净零目标,这些排放者需要脱碳。Pickerill于2018年停产,具有二氧化碳储存潜力,因为它是一个经过验证的圈闭,已生产了约4400亿立方英尺的天然气,并且位于海岸线附近。我们使用公共领域的三维地震数据集、电缆测井、岩心报告和生产数据来评估其二氧化碳储存潜力。Rotliegend组储层(Leman砂岩组)为风成/河流混合储层,厚度可变(25 ~ 80 m),净毛比高(0.9 ~ 1.0),平均孔隙度中等(9% ~ 17%),平均渗透率中等(>1 mD)。盖层为Zechstein组蒸发岩和碳酸盐岩,它们在沉积后的运动(卤化运动)中变薄和膨胀,进一步影响和变形了覆盖层。南侧为西北西东向断裂体系,北侧为油气藏倾闭构造。nw - se走向的断层横贯油田,将构造分割成几个隔室,其中三个隔室具有特别好的CO2储存候选者,总CO2储存容量为3200万吨CO2。如果与附近的卫星油田相结合,就有可能开发一个能够隔离6000万吨二氧化碳的二氧化碳储存集群,然而,这种潜力受到海上风力发电场计划开发的挑战。将涡轮机固定在油田上方的海床上,将限制新的二氧化碳注入井的钻探位置,以及使用传统的拖曳式地震来测量、监测和验证二氧化碳羽流的努力。迫切需要解决海上面积的竞争,以确保像Pickerill这样有吸引力的二氧化碳储存地点不会处于劣势,而是可以在能源转型中充分发挥替代可再生能源的补充作用。
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