FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4223646564> ?p ?o ?g. }

• W4223646564 abstract "Pore and pore network evolution of shale is critical for the evaluation the pore system in shale gas reservoirs. Thermal maturation effect acts as an indispensable role in porosity evolution. In this paper, high-temperature and high-pressure in-situ thermal simulation experiments were conducted to investigate the process and controlling factors of pore evolution in marine-continental transitional shale. Multiple methods, including scanning electron microscopy (SEM), X-ray diffraction, helium porosimetry and low-pressure N2 and CO2 adsorption were used to investigate the evolution of mineral composition and pore structure at different stages of thermal maturity. The results showed that type III organic matter (OM) generated petroleum with the thermal maturity increasing. The total organic carbon ( TOC ) decreased by 13.3% when temperature reached 607°C. At the same time, it produced numerous organic and mineral pores during hydrocarbon generation. Besides, some changes in mineral composition have occurred, especially in illite (from 11% to 31%) and kaolinite (from 89% to 69%). In general, it can divide into 3 stages (maturity, high maturity and over maturity) for shale pore system evolution with the thermal maturity increasing. In the low maturity period, large amounts of pyrolytic bitumen and oil generated to fill the pores, causing the pore system to diminish; in the high maturity period, a large number of pores were generated when oil is cracked into gas, resulting in a rapid expansion of the pore system; in the over-maturity period, the cracking of pyrolysis and hydrocarbon slowed down, allowing the pore system to stabilize. Shale pore evolution is primarily controlled by the thermal evolution of OM, and the conversion of inorganic minerals contributes less to pore evolution compared to organic matter. The high maturity period (1.2% &lt; Ro &lt; 2.0%) was the period when extensive pyrolysis and hydrocarbon generated in the Shanxi Formation shale, which contributed mostly for the pores generation and accumulation of shale gas." @default.
• W4223646564 created "2022-04-15" @default.
• W4223646564 creator A5021308713 @default.
• W4223646564 creator A5022387395 @default.
• W4223646564 creator A5045430322 @default.
• W4223646564 creator A5059606647 @default.
• W4223646564 creator A5066806764 @default.
• W4223646564 creator A5078331303 @default.
• W4223646564 creator A5088829026 @default.
• W4223646564 creator A5091699818 @default.
• W4223646564 date "2022-04-12" @default.
• W4223646564 modified "2023-09-26" @default.
• W4223646564 title "Process and Controlling Factors of Pore Evolution in Marine-Continental Transitional Black Shale—An Example From Permian Shanxi Formation in the Eastern Margin of Ordos Basin" @default.
• W4223646564 cites W2019199746 @default.
• W4223646564 cites W2021197065 @default.
• W4223646564 cites W2047305972 @default.
• W4223646564 cites W2074579280 @default.
• W4223646564 cites W2076955006 @default.
• W4223646564 cites W2110830197 @default.
• W4223646564 cites W2128873110 @default.
• W4223646564 cites W2170995602 @default.
• W4223646564 cites W2197251011 @default.
• W4223646564 cites W2395256810 @default.
• W4223646564 cites W2561230003 @default.
• W4223646564 cites W2745145532 @default.
• W4223646564 cites W2767761620 @default.
• W4223646564 cites W2891925896 @default.
• W4223646564 cites W2903415012 @default.
• W4223646564 cites W2983331167 @default.
• W4223646564 cites W2983871692 @default.
• W4223646564 cites W2990746516 @default.
• W4223646564 cites W3004085557 @default.
• W4223646564 cites W3020784381 @default.
• W4223646564 cites W3025923057 @default.
• W4223646564 cites W3026922459 @default.
• W4223646564 cites W3036133295 @default.
• W4223646564 cites W3036477896 @default.
• W4223646564 cites W3040107711 @default.
• W4223646564 cites W3041788474 @default.
• W4223646564 cites W3057751026 @default.
• W4223646564 cites W3084513121 @default.
• W4223646564 cites W3087513213 @default.
• W4223646564 cites W3088651189 @default.
• W4223646564 cites W3088957833 @default.
• W4223646564 cites W3089459273 @default.
• W4223646564 cites W3090573585 @default.
• W4223646564 cites W3092393797 @default.
• W4223646564 cites W3094286427 @default.
• W4223646564 cites W3135880125 @default.
• W4223646564 cites W3145835428 @default.
• W4223646564 cites W3176529887 @default.
• W4223646564 cites W3195485392 @default.
• W4223646564 cites W3197658528 @default.
• W4223646564 cites W3210093931 @default.
• W4223646564 cites W3211441317 @default.
• W4223646564 cites W4200208458 @default.
• W4223646564 cites W580147821 @default.
• W4223646564 doi "https://doi.org/10.3389/feart.2022.889067" @default.
• W4223646564 hasPublicationYear "2022" @default.
• W4223646564 type Work @default.
• W4223646564 citedByCount "1" @default.
• W4223646564 countsByYear W42236465642022 @default.
• W4223646564 crossrefType "journal-article" @default.
• W4223646564 hasAuthorship W4223646564A5021308713 @default.
• W4223646564 hasAuthorship W4223646564A5022387395 @default.
• W4223646564 hasAuthorship W4223646564A5045430322 @default.
• W4223646564 hasAuthorship W4223646564A5059606647 @default.
• W4223646564 hasAuthorship W4223646564A5066806764 @default.
• W4223646564 hasAuthorship W4223646564A5078331303 @default.
• W4223646564 hasAuthorship W4223646564A5088829026 @default.
• W4223646564 hasAuthorship W4223646564A5091699818 @default.
• W4223646564 hasBestOaLocation W42236465641 @default.
• W4223646564 hasConcept C101433766 @default.
• W4223646564 hasConcept C102579867 @default.
• W4223646564 hasConcept C107872376 @default.
• W4223646564 hasConcept C109007969 @default.
• W4223646564 hasConcept C114793014 @default.
• W4223646564 hasConcept C126559015 @default.
• W4223646564 hasConcept C127313418 @default.
• W4223646564 hasConcept C127413603 @default.
• W4223646564 hasConcept C138496976 @default.
• W4223646564 hasConcept C151730666 @default.
• W4223646564 hasConcept C153127940 @default.
• W4223646564 hasConcept C15744967 @default.
• W4223646564 hasConcept C158787203 @default.
• W4223646564 hasConcept C185592680 @default.
• W4223646564 hasConcept C187320778 @default.
• W4223646564 hasConcept C199289684 @default.
• W4223646564 hasConcept C2779196632 @default.
• W4223646564 hasConcept C2779899878 @default.
• W4223646564 hasConcept C36759035 @default.
• W4223646564 hasConcept C42360764 @default.
• W4223646564 hasConceptScore W4223646564C101433766 @default.
• W4223646564 hasConceptScore W4223646564C102579867 @default.
• W4223646564 hasConceptScore W4223646564C107872376 @default.
• W4223646564 hasConceptScore W4223646564C109007969 @default.
• W4223646564 hasConceptScore W4223646564C114793014 @default.
• W4223646564 hasConceptScore W4223646564C126559015 @default.
• W4223646564 hasConceptScore W4223646564C127313418 @default.
• W4223646564 hasConceptScore W4223646564C127413603 @default.

• next