FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2010384430> ?p ?o ?g. }

• W2010384430 endingPage "11" @default.
• W2010384430 startingPage "1" @default.
• W2010384430 abstract "Iron–minerals–water interactions are of primary importance in the contexts of underground structure engineering (e.g. reactive barriers or deep geological storage) and for the understanding of secondary alteration processes in primitive meteorites. To improve our understanding of these systems, we determine the mineralogical transformations induced by the association of iron and silicates during a cooling through an experimental simulation of iron–clay interactions with a step-by-step procedure in the range of 90 °C to 40 °C. The run products and solutions are well characterised, by means of different techniques (X-ray diffraction, scanning and transmission electron microscopy, manocalcimetry, inductively coupled plasma optical emission spectrometry and ion chromatography), and the thermodynamic data concerning Fe-bearing phyllosilicates are well-tested comparing the modelling and experimental results. Therefore, the main mineralogical modifications observed include the remarkable formation of cronstedtite and greenalite, as well as the formation of magnetite at all temperatures, along with a significant dissolution of quartz, mixed-layer illite–smectite clays, illite (affecting more than 70% of each mineralogical phase) and a partial alteration of chlorite, kaolinite and dolomite. The experimental results confirm the reaction path predicted by thermodynamic modelling, i.e. the formation of iron-rich T–O phyllosilicates (cronstedtite and greenalite) and magnetite at the expense of metal iron and silicates. Both the experimental and thermodynamic results presented in this study provide important constraints to well predict the impact of nuclear waste canister corrosion in a claystone media and to better understand secondary alteration processes, which could also affect the mineralogical and chemical composition of primitive meteorites." @default.
• W2010384430 created "2016-06-24" @default.
• W2010384430 creator A5002394983 @default.
• W2010384430 creator A5013217472 @default.
• W2010384430 creator A5024808382 @default.
• W2010384430 creator A5025778239 @default.
• W2010384430 creator A5031128770 @default.
• W2010384430 creator A5050745575 @default.
• W2010384430 creator A5089322493 @default.
• W2010384430 date "2014-11-01" @default.
• W2010384430 modified "2023-10-09" @default.
• W2010384430 title "Iron–clay interactions: Detailed study of the mineralogical transformation of claystone with emphasis on the formation of iron-rich T–O phyllosilicates in a step-by-step cooling experiment from 90 °C to 40 °C" @default.
• W2010384430 cites W1622535263 @default.
• W2010384430 cites W1973254267 @default.
• W2010384430 cites W1976299022 @default.
• W2010384430 cites W1980180529 @default.
• W2010384430 cites W1989197278 @default.
• W2010384430 cites W1991972851 @default.
• W2010384430 cites W2001021373 @default.
• W2010384430 cites W2001356524 @default.
• W2010384430 cites W2003461155 @default.
• W2010384430 cites W2005557231 @default.
• W2010384430 cites W2024659512 @default.
• W2010384430 cites W2028294441 @default.
• W2010384430 cites W2036129894 @default.
• W2010384430 cites W2038248875 @default.
• W2010384430 cites W2042470192 @default.
• W2010384430 cites W2043828500 @default.
• W2010384430 cites W2046004406 @default.
• W2010384430 cites W2054666458 @default.
• W2010384430 cites W2063796742 @default.
• W2010384430 cites W2068857519 @default.
• W2010384430 cites W2079421544 @default.
• W2010384430 cites W2082584843 @default.
• W2010384430 cites W2091537829 @default.
• W2010384430 cites W2111062559 @default.
• W2010384430 cites W2113574130 @default.
• W2010384430 cites W2123094330 @default.
• W2010384430 cites W2126058984 @default.
• W2010384430 cites W2127309440 @default.
• W2010384430 cites W2132925139 @default.
• W2010384430 cites W2142800389 @default.
• W2010384430 cites W2158194642 @default.
• W2010384430 cites W2320567613 @default.
• W2010384430 cites W2328021513 @default.
• W2010384430 cites W2330516177 @default.
• W2010384430 cites W2334540651 @default.
• W2010384430 cites W2350692534 @default.
• W2010384430 doi "https://doi.org/10.1016/j.chemgeo.2014.08.010" @default.
• W2010384430 hasPublicationYear "2014" @default.
• W2010384430 type Work @default.
• W2010384430 sameAs 2010384430 @default.
• W2010384430 citedByCount "33" @default.
• W2010384430 countsByYear W20103844302014 @default.
• W2010384430 countsByYear W20103844302015 @default.
• W2010384430 countsByYear W20103844302016 @default.
• W2010384430 countsByYear W20103844302017 @default.
• W2010384430 countsByYear W20103844302018 @default.
• W2010384430 countsByYear W20103844302019 @default.
• W2010384430 countsByYear W20103844302020 @default.
• W2010384430 countsByYear W20103844302021 @default.
• W2010384430 countsByYear W20103844302022 @default.
• W2010384430 countsByYear W20103844302023 @default.
• W2010384430 crossrefType "journal-article" @default.
• W2010384430 hasAuthorship W2010384430A5002394983 @default.
• W2010384430 hasAuthorship W2010384430A5013217472 @default.
• W2010384430 hasAuthorship W2010384430A5024808382 @default.
• W2010384430 hasAuthorship W2010384430A5025778239 @default.
• W2010384430 hasAuthorship W2010384430A5031128770 @default.
• W2010384430 hasAuthorship W2010384430A5050745575 @default.
• W2010384430 hasAuthorship W2010384430A5089322493 @default.
• W2010384430 hasConcept C127313418 @default.
• W2010384430 hasConcept C127413603 @default.
• W2010384430 hasConcept C151730666 @default.
• W2010384430 hasConcept C17409809 @default.
• W2010384430 hasConcept C191897082 @default.
• W2010384430 hasConcept C192562407 @default.
• W2010384430 hasConcept C199289684 @default.
• W2010384430 hasConcept C2776432453 @default.
• W2010384430 hasConcept C2777781897 @default.
• W2010384430 hasConcept C2777844515 @default.
• W2010384430 hasConcept C2779429093 @default.
• W2010384430 hasConcept C2779870107 @default.
• W2010384430 hasConcept C2779899878 @default.
• W2010384430 hasConcept C2780786144 @default.
• W2010384430 hasConcept C40212044 @default.
• W2010384430 hasConcept C42360764 @default.
• W2010384430 hasConcept C88380143 @default.
• W2010384430 hasConceptScore W2010384430C127313418 @default.
• W2010384430 hasConceptScore W2010384430C127413603 @default.
• W2010384430 hasConceptScore W2010384430C151730666 @default.
• W2010384430 hasConceptScore W2010384430C17409809 @default.
• W2010384430 hasConceptScore W2010384430C191897082 @default.
• W2010384430 hasConceptScore W2010384430C192562407 @default.
• W2010384430 hasConceptScore W2010384430C199289684 @default.
• W2010384430 hasConceptScore W2010384430C2776432453 @default.
• W2010384430 hasConceptScore W2010384430C2777781897 @default.
• W2010384430 hasConceptScore W2010384430C2777844515 @default.

• next