1994
DOI: 10.1016/0920-4105(94)90083-3
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Dynamic behavior of radio-labelled water tracer candidates for chalk reservoirs

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Cited by 15 publications
(6 citation statements)
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“…the ideal water tracer, HTO. This is often observed with negatively charged compounds and rock material with negatively charge surface (BjSrnstad et al [11]). Also shown in Tab.…”
Section: Resultsmentioning
confidence: 96%
“…the ideal water tracer, HTO. This is often observed with negatively charged compounds and rock material with negatively charge surface (BjSrnstad et al [11]). Also shown in Tab.…”
Section: Resultsmentioning
confidence: 96%
“…To better explain abnormalities in similar experiments (Bjørnstad et al, 1994) presented a method to visualise if the rates of production of the tracer candidates differ significantly from the ones of the reference tracer at different moments of the production. This allows to identify patterns that could be missed by the results presented so far.…”
Section: Flooding Experiments In Water Saturated Coresmentioning
confidence: 99%
“…Reversible adsorption can also cause a delay of the partitioning tracers relatively to the passive ones and would translate in the same type of response as partitioning to the oil phase on the production curves. While this has not been reported specifically for oil/water partitioning tracer candidates, (Bjørnstad et al, 1994) reported reversible adsorption of Iand SO4 2when investigating new passive water tracers for chalk reservoirs and (Strand et al, 2006) developed a method for measuring wettability of chalk cores based on the reversible adsorption of SO4 2-. Most of the molecules used in the early days of inter-well tracer tests in oil reservoirs were selected after their successful use in hydrogeology applications (Ahmad et al, 2003).…”
Section: Introductionmentioning
confidence: 99%
See 1 more Smart Citation
“…Seven substances were tested: tritiated water (HTO) and the ions S 14 CN − , 36 Cl − , 131 I − , 35 SO 4 2− , H 14 CO 3− , and 22 Na + . However, 131 I − and 35 SO 4 2− show a more complicated behavior because of ion exclusion, adsorption, desorption, and chemical reactions [270]. However, 131 I − and 35 SO 4 2− show a more complicated behavior because of ion exclusion, adsorption, desorption, and chemical reactions [270].…”
Section: Radioactive Tracersmentioning
confidence: 99%