2017
DOI: 10.3997/2214-4609.201701295
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Decoding the Water Flooding Processes from Produced Water Composition – A Case Study from the Halfdan Chalk Oil Field, Danish North Sea

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Cited by 2 publications
(8 citation statements)
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“…4) present in the Halfdan field occur in different parts of the field. The FW3 type is present on the southern flank of the field towards the Dan field and is clearly related to the presence of salt dome water (Schovsbo et al 2017) whereas the low salinity type (FW2) appear to be local end-member in the compositional continuum that extends north to the Valdemar/Roar fields. Within the Halfdan field, this suggests that local gradients in compositions exist and that each well location will represent a mix of the formation water produced along the long horizontal well track in contrast to all wells having same discrete compositions.…”
Section: Regional Water Typesmentioning
confidence: 99%
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“…4) present in the Halfdan field occur in different parts of the field. The FW3 type is present on the southern flank of the field towards the Dan field and is clearly related to the presence of salt dome water (Schovsbo et al 2017) whereas the low salinity type (FW2) appear to be local end-member in the compositional continuum that extends north to the Valdemar/Roar fields. Within the Halfdan field, this suggests that local gradients in compositions exist and that each well location will represent a mix of the formation water produced along the long horizontal well track in contrast to all wells having same discrete compositions.…”
Section: Regional Water Typesmentioning
confidence: 99%
“…Average compositions of these local end-members (c.f. Schovsbo et al 2017) are presented in Table 1 and include a Formation Water 2 (FW2) that is characterised by medium to low salinities and medium high Ba 2+ concentrations and a Formation Water 3 (FW3) that is characterised by high Ca 2+ and medium high salinities and medium to low SO4 2concentrations (Fig. 3A).…”
Section: Regional Water Types In Danish Fieldsmentioning
confidence: 99%
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“…Thus, the composition of produced water is known to vary between different fields but also within the same field, which reflects the complex interplay of processes. [2,8,9,10,11,12] Despite this, relatively little work has been done to map these differences. The reported research have mainly focused on the mapping of the Cl − concentration as this ion is considered a relatively inert ion, which is measurably diluted upon seawater injection, as the formation water is typically characterized by significantly higher total salinity.…”
Section: Introductionmentioning
confidence: 99%