All Days 2009
DOI: 10.2118/119321-ms
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Identification and Qualification of Shale Annular Barriers Using Wireline Logs During Plug and Abandonment Operations

Abstract: It has long been recognised that during and after drilling through certain formations, the rock moves inward and begins to close off the well. Normally this phenomenon is considered undesirable since it can cause problems for drilling and casing running. It can however be put to good use as the mechanism to create an annular barrier behind casing. In order to extend the life of a number of North Sea brown fields many well slots on production platforms and sub-sea templates are being re-used. This process invol… Show more

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Cited by 35 publications
(16 citation statements)
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“…Creeping formations, for example, tend to experience more or less fast viscoelastic or viscoplastic deformation that can bridge the annular gap or increase radial stresses on the cement sheath, thereby preventing the occurrence of microannuli or resealing them; some shales, halites, and possibly ice belong to this category and at least one such rock, the Hordaland Green Clay, has been qualified as a well barrier in Norway (Williams et al 2009). …”
Section: Methodsmentioning
confidence: 99%
“…Creeping formations, for example, tend to experience more or less fast viscoelastic or viscoplastic deformation that can bridge the annular gap or increase radial stresses on the cement sheath, thereby preventing the occurrence of microannuli or resealing them; some shales, halites, and possibly ice belong to this category and at least one such rock, the Hordaland Green Clay, has been qualified as a well barrier in Norway (Williams et al 2009). …”
Section: Methodsmentioning
confidence: 99%
“…In addition, performed extended leak off (XLOT) tests show qualified seals [26]. The question is how this could be happened?…”
Section: In Situ Formation (Formation As Barrier)mentioning
confidence: 99%
“…The existence of such fracture systems can be excluded for plastic materials. For these types of materials selfhealing effects are known and described in the literature [66][67][68]. Plastic behavior can be assumed for unconsolidated clay layers (in Northern Germany observed for clay layers of tertiary age, e.g., Rupelian) and for salt layers (in Northern Germany observed, e.g., in Muschelkalk, Buntsandstein, and in particular Zechstein) [14].…”
Section: Cap Rockmentioning
confidence: 99%