FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2549898405> ?p ?o ?g. }

• W2549898405 endingPage "1049" @default.
• W2549898405 startingPage "1031" @default.
• W2549898405 abstract "While hydraulic fracturing is the key to unlocking the potential of unconventional low-permeability hydrocarbon resources, challenges remain in the monitoring of subsurface propagation of fractures and the determination of which geologic intervals have been contacted. This is particularly challenging for wells that are completed in multiple hydraulic fracture stages (multi-fractured horizontal wells or MFHWs) where fracture spacing may be very close and fracture geometry complex. Understanding the fracture extent is important not only for assisting with hydraulic fracture design, but also for mitigating unwanted fracture growth into non-target geologic intervals that do not contain hydrocarbons (e.g. zones with high water saturation). Popular current technologies used for hydraulic fracture surveillance include microseismic (surface and subsurface monitoring) and tiltmeter surveys. While these methods have proven useful for characterizing the extent of created hydraulic fractures, they do not necessarily lead to an understanding of what portions of the geologic section (bounding and target intervals for MFHWs, for example) are in direct hydraulic communication with the well. A solution for establishing the extent of hydraulic fracture growth from target to bounding zones is to first obtain a fluid composition fingerprint of those intervals while drilling through them, and then compare these data with fluid compositions obtained from flowback after hydraulic fracturing. In the current work, a MFHW completed in a liquid-rich tight reservoir is used to test this novel concept. Gas samples extracted from the headspace of isojars® containing cuttings samples, obtained during drilling of the MFHW well, were used to geochemically fingerprint geologic intervals through which the well was drilled. The cuttings samples were collected at high frequency in the vertical, bend and lateral sections of the well over a measured depth range of 4725 ft (1440 m). A compositional marker was identified in the bend of the horizontal well above which the average methane to ethane (C1/C2) ratio was 15.7, versus 2.6 below it. The flowback gas compositions were observed to be intermediate (average C1/C2 = 7.4) between the reservoir above and below the marker, suggesting fracture height grew above the compositional marker. In order to estimate fracture height growth from the geologic interval and flowback compositions, a compositional numerical simulation study was performed. An innovative approach was used to estimate recombined in-situ fluid compositions, on a layer-by-layer basis, by combining the cuttings gas compositional data with separator oil compositions. The resulting numerical simulation model, initialized through use of the layered fluid model and a detailed geological model developed for the subject well and offset drilling locations, was used to history match flowback rates, pressures and gas compositions. The gas compositions of the fingerprinted geologic intervals were therefore employed as a constraint on fracture height growth, estimated in the model to be 175 ft (53 m, propped height). However, because of the uncertainty in model input parameters, a stochastic approach was required to derive a range in hydraulic fracture properties. The current study demonstrates for the first time that it is possible to constrain fracture height growth estimates from flowback data, combined with gas compositional data obtained from cuttings data, provided that the geochemical fingerprints are distinct." @default.
• W2549898405 created "2016-11-30" @default.
• W2549898405 creator A5003345953 @default.
• W2549898405 creator A5011286576 @default.
• W2549898405 creator A5038810220 @default.
• W2549898405 creator A5044001680 @default.
• W2549898405 creator A5056848342 @default.
• W2549898405 creator A5057654527 @default.
• W2549898405 creator A5075371671 @default.
• W2549898405 creator A5089185999 @default.
• W2549898405 date "2016-11-01" @default.
• W2549898405 modified "2023-10-05" @default.
• W2549898405 title "Estimation of fracture height growth in layered tight/shale gas reservoirs using flowback gas rates and compositions–Part II: Field application in a liquid-rich tight reservoir" @default.
• W2549898405 cites W1976883852 @default.
• W2549898405 cites W1977959969 @default.
• W2549898405 cites W1985967631 @default.
• W2549898405 cites W1992637041 @default.
• W2549898405 cites W2010384661 @default.
• W2549898405 cites W2030308632 @default.
• W2549898405 cites W2069006571 @default.
• W2549898405 cites W2126800276 @default.
• W2549898405 cites W2152785811 @default.
• W2549898405 cites W2209504942 @default.
• W2549898405 cites W2342676110 @default.
• W2549898405 cites W2398772388 @default.
• W2549898405 cites W3023799655 @default.
• W2549898405 doi "https://doi.org/10.1016/j.jngse.2016.11.014" @default.
• W2549898405 hasPublicationYear "2016" @default.
• W2549898405 type Work @default.
• W2549898405 sameAs 2549898405 @default.
• W2549898405 citedByCount "27" @default.
• W2549898405 countsByYear W25498984052017 @default.
• W2549898405 countsByYear W25498984052018 @default.
• W2549898405 countsByYear W25498984052019 @default.
• W2549898405 countsByYear W25498984052020 @default.
• W2549898405 countsByYear W25498984052021 @default.
• W2549898405 countsByYear W25498984052022 @default.
• W2549898405 countsByYear W25498984052023 @default.
• W2549898405 crossrefType "journal-article" @default.
• W2549898405 hasAuthorship W2549898405A5003345953 @default.
• W2549898405 hasAuthorship W2549898405A5011286576 @default.
• W2549898405 hasAuthorship W2549898405A5038810220 @default.
• W2549898405 hasAuthorship W2549898405A5044001680 @default.
• W2549898405 hasAuthorship W2549898405A5056848342 @default.
• W2549898405 hasAuthorship W2549898405A5057654527 @default.
• W2549898405 hasAuthorship W2549898405A5075371671 @default.
• W2549898405 hasAuthorship W2549898405A5089185999 @default.
• W2549898405 hasBestOaLocation W25498984052 @default.
• W2549898405 hasConcept C120882062 @default.
• W2549898405 hasConcept C127313418 @default.
• W2549898405 hasConcept C127413603 @default.
• W2549898405 hasConcept C151730666 @default.
• W2549898405 hasConcept C153127940 @default.
• W2549898405 hasConcept C165205528 @default.
• W2549898405 hasConcept C168630323 @default.
• W2549898405 hasConcept C183250156 @default.
• W2549898405 hasConcept C187320778 @default.
• W2549898405 hasConcept C25197100 @default.
• W2549898405 hasConcept C2777447996 @default.
• W2549898405 hasConcept C2779096232 @default.
• W2549898405 hasConcept C41625074 @default.
• W2549898405 hasConcept C43369102 @default.
• W2549898405 hasConcept C54355233 @default.
• W2549898405 hasConcept C548895740 @default.
• W2549898405 hasConcept C7266685 @default.
• W2549898405 hasConcept C78519656 @default.
• W2549898405 hasConcept C78641617 @default.
• W2549898405 hasConcept C78762247 @default.
• W2549898405 hasConcept C81803558 @default.
• W2549898405 hasConcept C86803240 @default.
• W2549898405 hasConceptScore W2549898405C120882062 @default.
• W2549898405 hasConceptScore W2549898405C127313418 @default.
• W2549898405 hasConceptScore W2549898405C127413603 @default.
• W2549898405 hasConceptScore W2549898405C151730666 @default.
• W2549898405 hasConceptScore W2549898405C153127940 @default.
• W2549898405 hasConceptScore W2549898405C165205528 @default.
• W2549898405 hasConceptScore W2549898405C168630323 @default.
• W2549898405 hasConceptScore W2549898405C183250156 @default.
• W2549898405 hasConceptScore W2549898405C187320778 @default.
• W2549898405 hasConceptScore W2549898405C25197100 @default.
• W2549898405 hasConceptScore W2549898405C2777447996 @default.
• W2549898405 hasConceptScore W2549898405C2779096232 @default.
• W2549898405 hasConceptScore W2549898405C41625074 @default.
• W2549898405 hasConceptScore W2549898405C43369102 @default.
• W2549898405 hasConceptScore W2549898405C54355233 @default.
• W2549898405 hasConceptScore W2549898405C548895740 @default.
• W2549898405 hasConceptScore W2549898405C7266685 @default.
• W2549898405 hasConceptScore W2549898405C78519656 @default.
• W2549898405 hasConceptScore W2549898405C78641617 @default.
• W2549898405 hasConceptScore W2549898405C78762247 @default.
• W2549898405 hasConceptScore W2549898405C81803558 @default.
• W2549898405 hasConceptScore W2549898405C86803240 @default.
• W2549898405 hasLocation W25498984051 @default.
• W2549898405 hasLocation W25498984052 @default.
• W2549898405 hasOpenAccess W2549898405 @default.
• W2549898405 hasPrimaryLocation W25498984051 @default.
• W2549898405 hasRelatedWork W1967103021 @default.
• W2549898405 hasRelatedWork W2027614683 @default.

• next