FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1965241036> ?p ?o ?g. }

• W1965241036 endingPage "922" @default.
• W1965241036 startingPage "911" @default.
• W1965241036 abstract "Based on the pyrolysis products for the Jurassic low-mature coal under programmed temperature, and chemical and carbon isotopic compositions of natural gas from the Kuqa Depression, the genetic origin of natural gas was determined, and then a gas filling model was established, in combination with the geological background of the Kuqa Depression. The active energy of CH4, C2H6 and C3H8 was gotten after the data of pyrolysis gas products under different heating rates (2°C/h and 20°C/h) were fitted by the Gas Oil Ratio (GOR) Isotope Model soft. When the frequency factor (Af) was chosen as 1×1014, the active energy of CH4, C2H6 and C3H8 was 58 kcal/mol, 57 kcal/mol and 54 kcal/mol, respectively. The distributive ranges of the δ13C1, δ13C2 and δ13C3 values for the pyrolysis gas products are –35.9‰ to –30.7‰, –26.2‰ to –21.3‰ and –26.4‰ to –22.7‰, respectively. All of the natural gases from the Kuqa Depression are dominated by hydrocarbon gases, with the high gas dryness (C1/C1–4) at the middle and northern parts of the depression and the low values at both east and west sides and the southern part. The carbon isotopes of methane and its homologs as a typical coal-type gas are enriched in 13C, and the distributive range of the δ13C1, δ13C2 and, δ13C3 value is –32‰ to –38‰, –22‰ to –24‰ and –20‰ to –22‰, respectively, with the carbon isotopes of gaseous alkanes being less negative with the carbon number. With the ethane being enriched in 13C the increasing tendency of the geological reserve of natural gas in the Kuqa Depression is observed. This observed change is consistent with the results of pyrolysate gas yield of coal as a potential gas source in the Kuqa Depression, suggesting natural gas was thermally derived from the humic organic matters and the carbon isotopes of gaseous alkanes would coarsely predict the geological reserve of gas in the Kuqa Depression. Through the simulation of kinetic processes of gas generation for the Jurassic coal in the Kuqa Depression, the gas in the Kela 2 gas field would get the threshold of gas expulsion after 27 Ma, be expelled out of source rocks as “pulse action”, and then filled in the gas reservoir. The peak gas-filling history took place during the past 2 Ma." @default.
• W1965241036 created "2016-06-24" @default.
• W1965241036 creator A5005439774 @default.
• W1965241036 creator A5043362888 @default.
• W1965241036 creator A5063285358 @default.
• W1965241036 creator A5068916530 @default.
• W1965241036 creator A5073272634 @default.
• W1965241036 creator A5085670380 @default.
• W1965241036 date "2011-08-01" @default.
• W1965241036 modified "2023-09-27" @default.
• W1965241036 title "Kinetic Model of Gaseous Alkanes Formed from Coal in a Confined System and Its Application to Gas Filling History in Kuqa Depression, Tarim Basin, Northwest China" @default.
• W1965241036 cites W1965231386 @default.
• W1965241036 cites W1967567810 @default.
• W1965241036 cites W1975872459 @default.
• W1965241036 cites W1976346396 @default.
• W1965241036 cites W1980433970 @default.
• W1965241036 cites W2006717745 @default.
• W1965241036 cites W2014070369 @default.
• W1965241036 cites W2019483389 @default.
• W1965241036 cites W2022999977 @default.
• W1965241036 cites W2025270360 @default.
• W1965241036 cites W2030310824 @default.
• W1965241036 cites W2030785057 @default.
• W1965241036 cites W2033268728 @default.
• W1965241036 cites W2039000423 @default.
• W1965241036 cites W2051269582 @default.
• W1965241036 cites W2063068316 @default.
• W1965241036 cites W2071197737 @default.
• W1965241036 cites W2076749715 @default.
• W1965241036 cites W2077541114 @default.
• W1965241036 cites W2079240626 @default.
• W1965241036 cites W2080002668 @default.
• W1965241036 cites W2156204090 @default.
• W1965241036 doi "https://doi.org/10.1111/j.1755-6724.2011.00494.x" @default.
• W1965241036 hasPublicationYear "2011" @default.
• W1965241036 type Work @default.
• W1965241036 sameAs 1965241036 @default.
• W1965241036 citedByCount "14" @default.
• W1965241036 countsByYear W19652410362012 @default.
• W1965241036 countsByYear W19652410362013 @default.
• W1965241036 countsByYear W19652410362014 @default.
• W1965241036 countsByYear W19652410362015 @default.
• W1965241036 countsByYear W19652410362016 @default.
• W1965241036 countsByYear W19652410362017 @default.
• W1965241036 countsByYear W19652410362018 @default.
• W1965241036 countsByYear W19652410362019 @default.
• W1965241036 countsByYear W19652410362021 @default.
• W1965241036 countsByYear W19652410362022 @default.
• W1965241036 countsByYear W19652410362023 @default.
• W1965241036 crossrefType "journal-article" @default.
• W1965241036 hasAuthorship W1965241036A5005439774 @default.
• W1965241036 hasAuthorship W1965241036A5043362888 @default.
• W1965241036 hasAuthorship W1965241036A5063285358 @default.
• W1965241036 hasAuthorship W1965241036A5068916530 @default.
• W1965241036 hasAuthorship W1965241036A5073272634 @default.
• W1965241036 hasAuthorship W1965241036A5085670380 @default.
• W1965241036 hasConcept C104779481 @default.
• W1965241036 hasConcept C107872376 @default.
• W1965241036 hasConcept C109007969 @default.
• W1965241036 hasConcept C126559015 @default.
• W1965241036 hasConcept C127313418 @default.
• W1965241036 hasConcept C140205800 @default.
• W1965241036 hasConcept C151730666 @default.
• W1965241036 hasConcept C158787203 @default.
• W1965241036 hasConcept C159985019 @default.
• W1965241036 hasConcept C17409809 @default.
• W1965241036 hasConcept C178790620 @default.
• W1965241036 hasConcept C185059815 @default.
• W1965241036 hasConcept C185592680 @default.
• W1965241036 hasConcept C192562407 @default.
• W1965241036 hasConcept C199289684 @default.
• W1965241036 hasConcept C2777207669 @default.
• W1965241036 hasConcept C2994520453 @default.
• W1965241036 hasConcept C36759035 @default.
• W1965241036 hasConcept C516920438 @default.
• W1965241036 hasConcept C518851703 @default.
• W1965241036 hasConcept C59427239 @default.
• W1965241036 hasConceptScore W1965241036C104779481 @default.
• W1965241036 hasConceptScore W1965241036C107872376 @default.
• W1965241036 hasConceptScore W1965241036C109007969 @default.
• W1965241036 hasConceptScore W1965241036C126559015 @default.
• W1965241036 hasConceptScore W1965241036C127313418 @default.
• W1965241036 hasConceptScore W1965241036C140205800 @default.
• W1965241036 hasConceptScore W1965241036C151730666 @default.
• W1965241036 hasConceptScore W1965241036C158787203 @default.
• W1965241036 hasConceptScore W1965241036C159985019 @default.
• W1965241036 hasConceptScore W1965241036C17409809 @default.
• W1965241036 hasConceptScore W1965241036C178790620 @default.
• W1965241036 hasConceptScore W1965241036C185059815 @default.
• W1965241036 hasConceptScore W1965241036C185592680 @default.
• W1965241036 hasConceptScore W1965241036C192562407 @default.
• W1965241036 hasConceptScore W1965241036C199289684 @default.
• W1965241036 hasConceptScore W1965241036C2777207669 @default.
• W1965241036 hasConceptScore W1965241036C2994520453 @default.
• W1965241036 hasConceptScore W1965241036C36759035 @default.
• W1965241036 hasConceptScore W1965241036C516920438 @default.
• W1965241036 hasConceptScore W1965241036C518851703 @default.
• W1965241036 hasConceptScore W1965241036C59427239 @default.

• next