Rotliegend sandstones from the UK Southern North Sea, well 48/11b-A5. The parallel-laminated sands represent aeolian deposits, and it is not difficult to imagine that these are low in clay content. Photo: North Sea Core.
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Carbon Capture & Storage

The benefits of being an oil veteran when assessing depleted fields for carbon storage

Making sense of old core analysis data certainly helps when you have worked with it at an earlier stage of your career

“ In some ways, knowing the reser­voir storage capacity of a CCS project is even more critical than knowing the size of the same reservoir prior to gas production,” said Alan Johnson at the start of his presentation at the Aber­deen Formation Evaluation Society.

This is mainly because storage con­tracts will often need to be signed be­fore FID for a CO2 capture project is considered. Of course, this is all still a bit theoretical, as there are not that many examples of CO2 storage pro­jects that have experienced FID, but the reasoning makes sense. At the end of the day, a chain of investments on the capture side is heavily dependent on the ability to store the CO2 at the downstream end of the line.

For that reason, Harbour UK asked Alan to carefully assess the sub­surface data of the Viking A depleted Rotliegend reservoir in the UK South­ern North Sea, with the main under­lying question of how reliable the core and wireline data are as input to cal­culating its ultimate storage capacity. The Viking A field is one of the earli­est discoveries made in the UK North Sea, 1969 to be precise.

Having started his career in petro­physics in 1974, just a few years after the first major gas discoveries were announced, it is easy to see why Har­bour asked Alan to carry out this job. He worked with the data types used back then and knew about the uncer­tainties, which is surely an advantage when revisiting it 50 years later.

One of the main questions cen­tred around the reliability of porosity data from core measurements carried out in those early years. Often, core reports from back then do not accu­rately describe the ways the cores were dried, which might have had implica­tions for the amount of water still in the core at the moment a porosity cal­culation is made. For instance, state­ments such as “Thoroughly dried” are a common occurrence, which clearly leaves room for speculation at which temperature the cores were actually dried.

However, despite these uncertain­ties, a careful analysis of various ways in which cores were prepared for anal­ysis indicated that the drying method­ology was not of detrimental effect on the reliability of the data. Why is that?

“The Rotliegend reservoir sands are quite forgiving,” concluded Alan at the end of his presentation. As the sands are often quite well sorted and without significant clay content, he concluded that the drying method has ultimately had little effect on the relia­bility of the porosity data. This is good news when it comes to using old data to calculate storage space in this area. However, if it would have been anoth­er reservoir with more of a mix of lith­ologies, this certainly would have been a little harder to conclude.

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