{"title":"CO2 Storage Potential Of The Neogene Stratigraphy In The North Viking Graben","authors":"C. Lloyd, M. Huuse","doi":"10.3997/2214-4609.201802987","DOIUrl":null,"url":null,"abstract":"The main Neogene reservoirs for CO2 storage in the North Viking Graben are the Utsira and Skade Formations, collectively known as the Utsira- Skade Aquifer. This is one of ten aquifers in the North Sea that is deemed suitable for CO2 storage (Halland et al., 2011). Most studies have been either a large scale assessment of the entire aquifer or finer detailed studies in the southern area, as this is currently where injection of CO2 is currently taking place at the Sleipner storage facility. This study assesses the suitability of the aquifer and its surrounding stratigraphy in the North Viking Graben. Analysis showed that a lack of a thick depocentre at a suitable depth results in poorer potential in this region compared to its southern counterpart. Injection into the Utsira Formation would need to occur in the north-east section to be at a suitable depth, utilising mostly 20-100m thick sands with a maximum migration distance of 90 km. The Skade Formation benefits from 85m thick closed traps but a max migrati","PeriodicalId":254996,"journal":{"name":"Fifth CO2 Geological Storage Workshop","volume":"1 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2018-11-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Fifth CO2 Geological Storage Workshop","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3997/2214-4609.201802987","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
摘要
北维京地堑新近系主要的二氧化碳储层是Utsira和Skade地层,统称为Utsira- Skade含水层。这是北海十个被认为适合储存二氧化碳的含水层之一(Halland et al., 2011)。大多数研究要么是对整个含水层进行大规模评估,要么是对南部地区进行更细致的研究,因为目前正在Sleipner储存设施注入二氧化碳。本研究评估了北维京地堑含水层及其周围地层的适宜性。分析表明,与南部地区相比,该地区缺乏合适深度的厚沉积,其潜力较差。Utsira地层的注入需要在东北段合适的深度进行,主要利用20-100米厚的砂岩,最大运移距离为90公里。Skade组受益于85米厚的封闭圈闭,但运移最大
CO2 Storage Potential Of The Neogene Stratigraphy In The North Viking Graben
The main Neogene reservoirs for CO2 storage in the North Viking Graben are the Utsira and Skade Formations, collectively known as the Utsira- Skade Aquifer. This is one of ten aquifers in the North Sea that is deemed suitable for CO2 storage (Halland et al., 2011). Most studies have been either a large scale assessment of the entire aquifer or finer detailed studies in the southern area, as this is currently where injection of CO2 is currently taking place at the Sleipner storage facility. This study assesses the suitability of the aquifer and its surrounding stratigraphy in the North Viking Graben. Analysis showed that a lack of a thick depocentre at a suitable depth results in poorer potential in this region compared to its southern counterpart. Injection into the Utsira Formation would need to occur in the north-east section to be at a suitable depth, utilising mostly 20-100m thick sands with a maximum migration distance of 90 km. The Skade Formation benefits from 85m thick closed traps but a max migrati