FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2015263708> ?p ?o ?g. }

• W2015263708 endingPage "573" @default.
• W2015263708 startingPage "555" @default.
• W2015263708 abstract "The chemical and isotopic characterization of formation water from 18 oil production wells, extracted from 5200 to 6100 m b.s.l. at the Jujo–Tecominoacán carbonate reservoir in SE-Mexico, and interpretations of historical production records, were undertaken to determine the origin and hydraulic behavior of deep groundwater systems. The infiltration of surface water during Late Pleistocene to Early Holocene time is suggested by 14C-concentrations from 2.15 to 31.86 pmC, and by 87Sr/86Sr-ratios for high-salinity formation water (0.70923–0.70927) that are close to the composition of Holocene to modern seawater. Prior to infiltration, the super-evaporation of seawater reached maximum TDS concentrations of 385 g/L, with lowest δ18O values characterizing the most hypersaline samples. Minor deviations of formation water and dolomite host rocks from modern and Jurassic 87Sr/86Sr-seawater composition, respectively, suggest ongoing water–rock interaction, and partial isotopic equilibration between both phases. The abundance of 14C in all sampled formation water, 87Sr/86Sr-ratios for high-salinity water close to Holocene – present seawater composition, a water salinity distribution that is independent of historic water-cut, and a total water extraction volume of 2.037 MMm3 (1/83–4/07) excludes a connate, oil-leg origin for the produced water of the Jurassic–Cretaceous mudstone-dolomite sequence. Temporal fluctuations of water chemistry in production intervals, the accelerated migration of water fronts from the reservoir flanks, and isotopic mixing trends between sampled wells confirms the existence of free aquifer water below oil horizons. Vertical and lateral hydraulic mobility has probably been accelerated by petroleum extraction. The combination of interpreting historical fluctuations of salinity and water percentage in production wells with chemical-isotopic analysis of formation water resulted in a successful method to distinguish four groundwater bodies, stratified vertically within the Jujo–Tecominoacán reservoir. Two with low TDS from 10 to 23 g/L are preserved in the upper reservoir section, mainly in Lower Cretaceous and Kimmeridgian strata. For the deeper part of the reservoir, 87Sr/86Sr trends indicate an affiliation of most samples to two independent mixing trends between “intermediate saline” (TDS ∼200 g/L) and hypersaline (>350 g/L) groundwater end-members." @default.
• W2015263708 created "2016-06-24" @default.
• W2015263708 creator A5013980648 @default.
• W2015263708 creator A5025251080 @default.
• W2015263708 creator A5071973712 @default.
• W2015263708 creator A5072080804 @default.
• W2015263708 date "2009-04-01" @default.
• W2015263708 modified "2023-10-02" @default.
• W2015263708 title "Origin and evolution of formation water at the Jujo–Tecominoacán oil reservoir, Gulf of Mexico. Part 2: Isotopic and field-production evidence for fluid connectivity" @default.
• W2015263708 cites W1965781903 @default.
• W2015263708 cites W1972789764 @default.
• W2015263708 cites W1993041545 @default.
• W2015263708 cites W1997749699 @default.
• W2015263708 cites W1998933135 @default.
• W2015263708 cites W2009187061 @default.
• W2015263708 cites W2022600615 @default.
• W2015263708 cites W2024035779 @default.
• W2015263708 cites W2032597545 @default.
• W2015263708 cites W2032753546 @default.
• W2015263708 cites W2035559075 @default.
• W2015263708 cites W2042976058 @default.
• W2015263708 cites W2045606424 @default.
• W2015263708 cites W2052597986 @default.
• W2015263708 cites W2053047171 @default.
• W2015263708 cites W2068828703 @default.
• W2015263708 cites W2090365149 @default.
• W2015263708 cites W2094679907 @default.
• W2015263708 cites W2147966596 @default.
• W2015263708 cites W39381521 @default.
• W2015263708 cites W4294555410 @default.
• W2015263708 doi "https://doi.org/10.1016/j.apgeochem.2008.12.010" @default.
• W2015263708 hasPublicationYear "2009" @default.
• W2015263708 type Work @default.
• W2015263708 sameAs 2015263708 @default.
• W2015263708 citedByCount "27" @default.
• W2015263708 countsByYear W20152637082012 @default.
• W2015263708 countsByYear W20152637082013 @default.
• W2015263708 countsByYear W20152637082014 @default.
• W2015263708 countsByYear W20152637082015 @default.
• W2015263708 countsByYear W20152637082016 @default.
• W2015263708 countsByYear W20152637082017 @default.
• W2015263708 countsByYear W20152637082019 @default.
• W2015263708 countsByYear W20152637082021 @default.
• W2015263708 countsByYear W20152637082022 @default.
• W2015263708 countsByYear W20152637082023 @default.
• W2015263708 crossrefType "journal-article" @default.
• W2015263708 hasAuthorship W2015263708A5013980648 @default.
• W2015263708 hasAuthorship W2015263708A5025251080 @default.
• W2015263708 hasAuthorship W2015263708A5071973712 @default.
• W2015263708 hasAuthorship W2015263708A5072080804 @default.
• W2015263708 hasConcept C111368507 @default.
• W2015263708 hasConcept C121332964 @default.
• W2015263708 hasConcept C127313418 @default.
• W2015263708 hasConcept C129513315 @default.
• W2015263708 hasConcept C140345934 @default.
• W2015263708 hasConcept C17409809 @default.
• W2015263708 hasConcept C178790620 @default.
• W2015263708 hasConcept C185592680 @default.
• W2015263708 hasConcept C187320778 @default.
• W2015263708 hasConcept C197248824 @default.
• W2015263708 hasConcept C22117777 @default.
• W2015263708 hasConcept C2775865663 @default.
• W2015263708 hasConcept C2780181037 @default.
• W2015263708 hasConcept C2780659211 @default.
• W2015263708 hasConcept C62520636 @default.
• W2015263708 hasConcept C6494504 @default.
• W2015263708 hasConcept C69384203 @default.
• W2015263708 hasConcept C75622301 @default.
• W2015263708 hasConcept C76177295 @default.
• W2015263708 hasConcept C76886044 @default.
• W2015263708 hasConcept C78762247 @default.
• W2015263708 hasConcept C92720285 @default.
• W2015263708 hasConceptScore W2015263708C111368507 @default.
• W2015263708 hasConceptScore W2015263708C121332964 @default.
• W2015263708 hasConceptScore W2015263708C127313418 @default.
• W2015263708 hasConceptScore W2015263708C129513315 @default.
• W2015263708 hasConceptScore W2015263708C140345934 @default.
• W2015263708 hasConceptScore W2015263708C17409809 @default.
• W2015263708 hasConceptScore W2015263708C178790620 @default.
• W2015263708 hasConceptScore W2015263708C185592680 @default.
• W2015263708 hasConceptScore W2015263708C187320778 @default.
• W2015263708 hasConceptScore W2015263708C197248824 @default.
• W2015263708 hasConceptScore W2015263708C22117777 @default.
• W2015263708 hasConceptScore W2015263708C2775865663 @default.
• W2015263708 hasConceptScore W2015263708C2780181037 @default.
• W2015263708 hasConceptScore W2015263708C2780659211 @default.
• W2015263708 hasConceptScore W2015263708C62520636 @default.
• W2015263708 hasConceptScore W2015263708C6494504 @default.
• W2015263708 hasConceptScore W2015263708C69384203 @default.
• W2015263708 hasConceptScore W2015263708C75622301 @default.
• W2015263708 hasConceptScore W2015263708C76177295 @default.
• W2015263708 hasConceptScore W2015263708C76886044 @default.
• W2015263708 hasConceptScore W2015263708C78762247 @default.
• W2015263708 hasConceptScore W2015263708C92720285 @default.
• W2015263708 hasIssue "4" @default.
• W2015263708 hasLocation W20152637081 @default.
• W2015263708 hasOpenAccess W2015263708 @default.
• W2015263708 hasPrimaryLocation W20152637081 @default.

• next