FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1969802241> ?p ?o ?g. }

• W1969802241 endingPage "2172" @default.
• W1969802241 startingPage "2156" @default.
• W1969802241 abstract "Ketzin, in the Northeast German Basin (NEGB), is the site for pilot injection of CO2 (CO2SINK project) into a saline aquifer (the Upper Triassic Stuttgart Formation) situated at a depth of about 630–700 m. This paper reports the baseline characterization of the reservoir formation based on new core material and well-logs obtained from one injection well and two observations wells, drilled at a distance from 50 m to 100 m from each other. The reservoir is lithologically heterogeneous and made up by fluvial sandstones and siltstones interbedded with mudstones showing remarkable differences in porosity. The thickest sandstone units are associated with channel sandstone, whose thickness varies over short lateral distances. In-depth petrographic, mineralogical, mineral-chemical, and whole-rock geochemical analysis were performed focusing on the sandstone intervals, which display the best reservoir properties for CO2 injection. The dominantly fine-grained and well to moderately-well sorted, immature sandstones classify as feldspathic litharenites and lithic arkoses. Quartz (22–43 wt.%), plagioclase (19–32 wt.%), and K-feldspar (5–13 wt.%) predominate mineralogically. Muscovite plus illite and mixed-layer minerals are omnipresent (4–13 wt.%). Quartz, feldspar, as well as meta-sedimentary and volcanic rock fragments comprise the most abundant detrital components, which often are rimmed by thin, early diagenetic coatings of ferric oxides, and locally of clay minerals. Feldspar grains may be unaltered and optically clear, partially to completely dissolved, partially altered to sheet silicates (mainly illite), or albitized. Analcime and anhydrite constitute the most widespread, often spatially associated pore-filling cement minerals. Authigenic dolomite, barite, and coelestine is minor. The percentage of cements ranges in total from about 5 vol.% to 32 vol.%. Except of samples intensely cemented by anhydrite and analcime, total porosities of the sandstones range from 13% to 26%. The fraction of intergranular porosity varies between 12% and 21%. About 1–5% porosity has been generated by dissolution of detrital plagioclase, K-feldspar, and volcanic rock fragments. The comparatively large modal abundance of feldspars, micas, chlorite, clay minerals, Fe–Ti-oxides, and analcime account for the richness in Ti, Al, Fe, Mg, Na, and K, and the paucity in Si, of the Stuttgart sandstones relative to mature sandstones. Altogether, these sandstones are comparatively rich in minerals that may potentially react with the injected CO2." @default.
• W1969802241 created "2016-06-24" @default.
• W1969802241 creator A5014268501 @default.
• W1969802241 creator A5016869328 @default.
• W1969802241 creator A5025459069 @default.
• W1969802241 creator A5031286344 @default.
• W1969802241 creator A5054942272 @default.
• W1969802241 creator A5061413851 @default.
• W1969802241 creator A5063394414 @default.
• W1969802241 creator A5074423143 @default.
• W1969802241 creator A5091354403 @default.
• W1969802241 date "2010-12-01" @default.
• W1969802241 modified "2023-10-10" @default.
• W1969802241 title "Reservoir characterization of a CO2 storage aquifer: The Upper Triassic Stuttgart Formation in the Northeast German Basin" @default.
• W1969802241 cites W1966189692 @default.
• W1969802241 cites W1975042776 @default.
• W1969802241 cites W2017259665 @default.
• W1969802241 cites W2022412805 @default.
• W1969802241 cites W2024202801 @default.
• W1969802241 cites W2032906522 @default.
• W1969802241 cites W2051940629 @default.
• W1969802241 cites W2080786667 @default.
• W1969802241 cites W2084733538 @default.
• W1969802241 cites W2121860965 @default.
• W1969802241 cites W2126820166 @default.
• W1969802241 cites W2140841495 @default.
• W1969802241 cites W2149505200 @default.
• W1969802241 cites W2224103689 @default.
• W1969802241 cites W2332230385 @default.
• W1969802241 cites W2781872186 @default.
• W1969802241 cites W2994679179 @default.
• W1969802241 cites W4253937712 @default.
• W1969802241 doi "https://doi.org/10.1016/j.marpetgeo.2010.07.010" @default.
• W1969802241 hasPublicationYear "2010" @default.
• W1969802241 type Work @default.
• W1969802241 sameAs 1969802241 @default.
• W1969802241 citedByCount "98" @default.
• W1969802241 countsByYear W19698022412012 @default.
• W1969802241 countsByYear W19698022412013 @default.
• W1969802241 countsByYear W19698022412014 @default.
• W1969802241 countsByYear W19698022412015 @default.
• W1969802241 countsByYear W19698022412016 @default.
• W1969802241 countsByYear W19698022412017 @default.
• W1969802241 countsByYear W19698022412018 @default.
• W1969802241 countsByYear W19698022412019 @default.
• W1969802241 countsByYear W19698022412020 @default.
• W1969802241 countsByYear W19698022412021 @default.
• W1969802241 countsByYear W19698022412022 @default.
• W1969802241 countsByYear W19698022412023 @default.
• W1969802241 crossrefType "journal-article" @default.
• W1969802241 hasAuthorship W1969802241A5014268501 @default.
• W1969802241 hasAuthorship W1969802241A5016869328 @default.
• W1969802241 hasAuthorship W1969802241A5025459069 @default.
• W1969802241 hasAuthorship W1969802241A5031286344 @default.
• W1969802241 hasAuthorship W1969802241A5054942272 @default.
• W1969802241 hasAuthorship W1969802241A5061413851 @default.
• W1969802241 hasAuthorship W1969802241A5063394414 @default.
• W1969802241 hasAuthorship W1969802241A5074423143 @default.
• W1969802241 hasAuthorship W1969802241A5091354403 @default.
• W1969802241 hasConcept C115393850 @default.
• W1969802241 hasConcept C120806208 @default.
• W1969802241 hasConcept C127313418 @default.
• W1969802241 hasConcept C130452526 @default.
• W1969802241 hasConcept C138170599 @default.
• W1969802241 hasConcept C151730666 @default.
• W1969802241 hasConcept C17409809 @default.
• W1969802241 hasConcept C192241223 @default.
• W1969802241 hasConcept C199289684 @default.
• W1969802241 hasConcept C2776044767 @default.
• W1969802241 hasConcept C2776543301 @default.
• W1969802241 hasConcept C2778520076 @default.
• W1969802241 hasConcept C2779181077 @default.
• W1969802241 hasConcept C2779229104 @default.
• W1969802241 hasConcept C2779429093 @default.
• W1969802241 hasConcept C2779870107 @default.
• W1969802241 hasConcept C40212044 @default.
• W1969802241 hasConcept C59235061 @default.
• W1969802241 hasConcept C6494504 @default.
• W1969802241 hasConceptScore W1969802241C115393850 @default.
• W1969802241 hasConceptScore W1969802241C120806208 @default.
• W1969802241 hasConceptScore W1969802241C127313418 @default.
• W1969802241 hasConceptScore W1969802241C130452526 @default.
• W1969802241 hasConceptScore W1969802241C138170599 @default.
• W1969802241 hasConceptScore W1969802241C151730666 @default.
• W1969802241 hasConceptScore W1969802241C17409809 @default.
• W1969802241 hasConceptScore W1969802241C192241223 @default.
• W1969802241 hasConceptScore W1969802241C199289684 @default.
• W1969802241 hasConceptScore W1969802241C2776044767 @default.
• W1969802241 hasConceptScore W1969802241C2776543301 @default.
• W1969802241 hasConceptScore W1969802241C2778520076 @default.
• W1969802241 hasConceptScore W1969802241C2779181077 @default.
• W1969802241 hasConceptScore W1969802241C2779229104 @default.
• W1969802241 hasConceptScore W1969802241C2779429093 @default.
• W1969802241 hasConceptScore W1969802241C2779870107 @default.
• W1969802241 hasConceptScore W1969802241C40212044 @default.
• W1969802241 hasConceptScore W1969802241C59235061 @default.
• W1969802241 hasConceptScore W1969802241C6494504 @default.
• W1969802241 hasFunder F4320320300 @default.

• next