FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2016229493> ?p ?o ?g. }

• W2016229493 endingPage "247" @default.
• W2016229493 startingPage "237" @default.
• W2016229493 abstract "Abstract The perhydrous Batalha coal (Portugal) is found in the Cabacos and Montejunto Formation of the Oxfordian–Kimeridgian, Upper Jurassic age. From the macroscopic point of view, its appearance is similar to other perhydrous coals. Microscopically, the maceral group of huminite is the main organic component (96%), ulminite being the most important petrographic component, followed by textinite with resinite (4%) lumina filled. The huminite random reflectance is 0.33%. This coal is characterized by high H/C atomic ratio, and anomalous physical and chemical properties that are characteristic of perhydrous coals such as: (i) the absence of any correlation between reflectance and the chemical rank parameters; (ii) a lower real density than that of non-perhydrous coals; (iii) a high hydrogen content; and (iv) suppressed reflectance. Using its calorific value (moist, ash-free basis) as rank parameter, Batalha coal must be considered a subbituminous A coal. Hydrogen enrichment due to the presence of resinite has influenced the technological properties of this coal, namely: (i) reduction of the thermostability and decrease in the temperature of initial thermal decomposition due to, among other reasons, the existence of aliphatic structures with low dissociation energy bonds resulting from the presence of resinite; (ii) from the DTG profile, the volatile matter combustion and char combustion is not evident; (iii) development of chars made up of isotropic particles with angular edges, which is typical of a low rank coal; (iv) the evolution trend of gaseous compounds (CO, CO 2 and CH 4 ) during pyrolysis; and, (v) an increase in its calorific value due to its hydrogen content. The study of this coal which is interbedded in Jurassic formations in the Lusitanian Basin of Portugal is a new contribution to the assessment of the evolution of organic matter in this area." @default.
• W2016229493 created "2016-06-24" @default.
• W2016229493 creator A5006299724 @default.
• W2016229493 creator A5036883260 @default.
• W2016229493 creator A5077639564 @default.
• W2016229493 creator A5079926939 @default.
• W2016229493 creator A5081344952 @default.
• W2016229493 creator A5087441657 @default.
• W2016229493 date "2010-12-01" @default.
• W2016229493 modified "2023-09-27" @default.
• W2016229493 title "The importance of thermal behaviour and petrographic composition for understanding the characteristics of a Portuguese perhydrous Jurassic coal" @default.
• W2016229493 cites W1974344044 @default.
• W2016229493 cites W1999730965 @default.
• W2016229493 cites W2005202849 @default.
• W2016229493 cites W2014833561 @default.
• W2016229493 cites W2015083148 @default.
• W2016229493 cites W2023537349 @default.
• W2016229493 cites W2034949555 @default.
• W2016229493 cites W2045237155 @default.
• W2016229493 cites W2049481661 @default.
• W2016229493 cites W2049689904 @default.
• W2016229493 cites W2050253946 @default.
• W2016229493 cites W2054754417 @default.
• W2016229493 cites W2054767166 @default.
• W2016229493 cites W2058298989 @default.
• W2016229493 cites W2061788417 @default.
• W2016229493 cites W2077499215 @default.
• W2016229493 cites W2079737039 @default.
• W2016229493 cites W2082142605 @default.
• W2016229493 cites W2090228457 @default.
• W2016229493 cites W2092068786 @default.
• W2016229493 cites W2140605284 @default.
• W2016229493 cites W3126017275 @default.
• W2016229493 cites W4236372120 @default.
• W2016229493 cites W4253952146 @default.
• W2016229493 doi "https://doi.org/10.1016/j.coal.2010.08.012" @default.
• W2016229493 hasPublicationYear "2010" @default.
• W2016229493 type Work @default.
• W2016229493 sameAs 2016229493 @default.
• W2016229493 citedByCount "11" @default.
• W2016229493 countsByYear W20162294932012 @default.
• W2016229493 countsByYear W20162294932013 @default.
• W2016229493 countsByYear W20162294932015 @default.
• W2016229493 countsByYear W20162294932017 @default.
• W2016229493 countsByYear W20162294932019 @default.
• W2016229493 countsByYear W20162294932020 @default.
• W2016229493 countsByYear W20162294932021 @default.
• W2016229493 crossrefType "journal-article" @default.
• W2016229493 hasAuthorship W2016229493A5006299724 @default.
• W2016229493 hasAuthorship W2016229493A5036883260 @default.
• W2016229493 hasAuthorship W2016229493A5077639564 @default.
• W2016229493 hasAuthorship W2016229493A5079926939 @default.
• W2016229493 hasAuthorship W2016229493A5081344952 @default.
• W2016229493 hasAuthorship W2016229493A5087441657 @default.
• W2016229493 hasConcept C127313418 @default.
• W2016229493 hasConcept C138885662 @default.
• W2016229493 hasConcept C166957645 @default.
• W2016229493 hasConcept C17409809 @default.
• W2016229493 hasConcept C205649164 @default.
• W2016229493 hasConcept C35219183 @default.
• W2016229493 hasConcept C40231798 @default.
• W2016229493 hasConcept C41895202 @default.
• W2016229493 hasConcept C518851703 @default.
• W2016229493 hasConcept C59235061 @default.
• W2016229493 hasConcept C6494504 @default.
• W2016229493 hasConceptScore W2016229493C127313418 @default.
• W2016229493 hasConceptScore W2016229493C138885662 @default.
• W2016229493 hasConceptScore W2016229493C166957645 @default.
• W2016229493 hasConceptScore W2016229493C17409809 @default.
• W2016229493 hasConceptScore W2016229493C205649164 @default.
• W2016229493 hasConceptScore W2016229493C35219183 @default.
• W2016229493 hasConceptScore W2016229493C40231798 @default.
• W2016229493 hasConceptScore W2016229493C41895202 @default.
• W2016229493 hasConceptScore W2016229493C518851703 @default.
• W2016229493 hasConceptScore W2016229493C59235061 @default.
• W2016229493 hasConceptScore W2016229493C6494504 @default.
• W2016229493 hasIssue "3-4" @default.
• W2016229493 hasLocation W20162294931 @default.
• W2016229493 hasOpenAccess W2016229493 @default.
• W2016229493 hasPrimaryLocation W20162294931 @default.
• W2016229493 hasRelatedWork W1987982070 @default.
• W2016229493 hasRelatedWork W2018576756 @default.
• W2016229493 hasRelatedWork W2043300320 @default.
• W2016229493 hasRelatedWork W2082235444 @default.
• W2016229493 hasRelatedWork W2088675059 @default.
• W2016229493 hasRelatedWork W2169854879 @default.
• W2016229493 hasRelatedWork W2219155975 @default.
• W2016229493 hasRelatedWork W2338326138 @default.
• W2016229493 hasRelatedWork W3034131340 @default.
• W2016229493 hasRelatedWork W4252070353 @default.
• W2016229493 hasVolume "84" @default.
• W2016229493 isParatext "false" @default.
• W2016229493 isRetracted "false" @default.
• W2016229493 magId "2016229493" @default.
• W2016229493 workType "article" @default.