FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2780138694> ?p ?o ?g. }

• W2780138694 endingPage "315" @default.
• W2780138694 startingPage "307" @default.
• W2780138694 abstract "Stimulation of rocks deteriorates the equilibrium distribution of rare earth elements and yttrium (REY) between solids and brines. By stimulation of the Permian, Lower Rotliegend formations in the well Groß Schönebeck 3/90 the volcanites are less affected by stimulation than the overlying conglomerate and sandstones. Brines from different lithological sections differ in REY patterns and gain anomalies of Eu, Gd, and Y during processes of recrystallization. The initially small anomalies increase during stimulation but decrease with both ongoing pumping and recrystallization. The REY patterns and their Eu, Gd, Y anomalies of brines from the conglomerate and volcanites distinctively differ from those of the sandstones. The Gd and Y anomalies are strongly correlated and both increase in sandstones with distance from the underlying conglomerate and volcanite. The correlation plot of Gd and Y anomalies does not describe a mixing line between brines from the volcanite and conglomerate but it reveals the extent of recrystallization of rapid precipitations and growth of minerals immediately after the stimulation and the slow re-equilibration of REY between solids and brines in each section of rocks. Extreme recrystallization occurred within the conglomerates, the least ones in the volcanite. REY patterns with their characteristic Eu, Gd, and Y anomalies are reliable indicators of the source of brines after stimulation. The time-dependence of changes of Eu, Gd and Y anomalies reflect the process of recrystallization." @default.
• W2780138694 created "2018-01-05" @default.
• W2780138694 creator A5032824960 @default.
• W2780138694 creator A5078648527 @default.
• W2780138694 date "2018-03-01" @default.
• W2780138694 modified "2023-10-17" @default.
• W2780138694 title "Induced rare earth element fractionation in brines by hydraulic fracturing of their aquifer rocks" @default.
• W2780138694 cites W1638709470 @default.
• W2780138694 cites W1974972389 @default.
• W2780138694 cites W1977457396 @default.
• W2780138694 cites W1978190411 @default.
• W2780138694 cites W1981200900 @default.
• W2780138694 cites W1995332806 @default.
• W2780138694 cites W2011449281 @default.
• W2780138694 cites W2016003875 @default.
• W2780138694 cites W2033473502 @default.
• W2780138694 cites W2048667896 @default.
• W2780138694 cites W2054361831 @default.
• W2780138694 cites W2057212379 @default.
• W2780138694 cites W2065096108 @default.
• W2780138694 cites W2068541546 @default.
• W2780138694 cites W2068656752 @default.
• W2780138694 cites W2071103381 @default.
• W2780138694 cites W2077748426 @default.
• W2780138694 cites W2080041512 @default.
• W2780138694 cites W2082330536 @default.
• W2780138694 cites W2105352695 @default.
• W2780138694 cites W2118223953 @default.
• W2780138694 cites W2135307173 @default.
• W2780138694 cites W2605166989 @default.
• W2780138694 doi "https://doi.org/10.1016/j.geothermics.2017.12.008" @default.
• W2780138694 hasPublicationYear "2018" @default.
• W2780138694 type Work @default.
• W2780138694 sameAs 2780138694 @default.
• W2780138694 citedByCount "2" @default.
• W2780138694 countsByYear W27801386942021 @default.
• W2780138694 countsByYear W27801386942022 @default.
• W2780138694 crossrefType "journal-article" @default.
• W2780138694 hasAuthorship W2780138694A5032824960 @default.
• W2780138694 hasAuthorship W2780138694A5078648527 @default.
• W2780138694 hasConcept C106804226 @default.
• W2780138694 hasConcept C109007969 @default.
• W2780138694 hasConcept C114793014 @default.
• W2780138694 hasConcept C127313418 @default.
• W2780138694 hasConcept C151730666 @default.
• W2780138694 hasConcept C17409809 @default.
• W2780138694 hasConcept C178790620 @default.
• W2780138694 hasConcept C183250156 @default.
• W2780138694 hasConcept C185592680 @default.
• W2780138694 hasConcept C195702682 @default.
• W2780138694 hasConcept C199289684 @default.
• W2780138694 hasConcept C2777615417 @default.
• W2780138694 hasConcept C2779096232 @default.
• W2780138694 hasConcept C2779851234 @default.
• W2780138694 hasConcept C2983155866 @default.
• W2780138694 hasConcept C531131001 @default.
• W2780138694 hasConcept C548895740 @default.
• W2780138694 hasConcept C5900021 @default.
• W2780138694 hasConcept C6494504 @default.
• W2780138694 hasConcept C78762247 @default.
• W2780138694 hasConcept C81803558 @default.
• W2780138694 hasConcept C83365034 @default.
• W2780138694 hasConceptScore W2780138694C106804226 @default.
• W2780138694 hasConceptScore W2780138694C109007969 @default.
• W2780138694 hasConceptScore W2780138694C114793014 @default.
• W2780138694 hasConceptScore W2780138694C127313418 @default.
• W2780138694 hasConceptScore W2780138694C151730666 @default.
• W2780138694 hasConceptScore W2780138694C17409809 @default.
• W2780138694 hasConceptScore W2780138694C178790620 @default.
• W2780138694 hasConceptScore W2780138694C183250156 @default.
• W2780138694 hasConceptScore W2780138694C185592680 @default.
• W2780138694 hasConceptScore W2780138694C195702682 @default.
• W2780138694 hasConceptScore W2780138694C199289684 @default.
• W2780138694 hasConceptScore W2780138694C2777615417 @default.
• W2780138694 hasConceptScore W2780138694C2779096232 @default.
• W2780138694 hasConceptScore W2780138694C2779851234 @default.
• W2780138694 hasConceptScore W2780138694C2983155866 @default.
• W2780138694 hasConceptScore W2780138694C531131001 @default.
• W2780138694 hasConceptScore W2780138694C548895740 @default.
• W2780138694 hasConceptScore W2780138694C5900021 @default.
• W2780138694 hasConceptScore W2780138694C6494504 @default.
• W2780138694 hasConceptScore W2780138694C78762247 @default.
• W2780138694 hasConceptScore W2780138694C81803558 @default.
• W2780138694 hasConceptScore W2780138694C83365034 @default.
• W2780138694 hasLocation W27801386941 @default.
• W2780138694 hasOpenAccess W2780138694 @default.
• W2780138694 hasPrimaryLocation W27801386941 @default.
• W2780138694 hasRelatedWork W109165701 @default.
• W2780138694 hasRelatedWork W112182015 @default.
• W2780138694 hasRelatedWork W1536106891 @default.
• W2780138694 hasRelatedWork W2018377848 @default.
• W2780138694 hasRelatedWork W2077346396 @default.
• W2780138694 hasRelatedWork W2089635000 @default.
• W2780138694 hasRelatedWork W2138066017 @default.
• W2780138694 hasRelatedWork W2352465799 @default.
• W2780138694 hasRelatedWork W2780138694 @default.
• W2780138694 hasRelatedWork W2892034786 @default.
• W2780138694 hasVolume "72" @default.

• next