FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2995590561> ?p ?o ?g. }

• W2995590561 endingPage "1091" @default.
• W2995590561 startingPage "1080" @default.
• W2995590561 abstract "Abstract Due to its significance for gas hydrate accumulation, the gas hydrate stability zone (GHSZ) is an essential condition for successful gas hydrate exploration and is usually controlled by three main factors: gas components, geothermal gradient, and permafrost thickness. Based on the core and conventional log data of gas hydrate potential region, the CSMHYD program was adopted to simulate the influences of above three factors on the thickness of the GHSZ. When the gas components of the gas hydrate were CH 4 , C 2 H 6 , and C 3 H 8 , with the CH 4 percentage ranging from 50% to 100%, the average GHSZ thickness can reach 1000 m according to the forward simulation results. When the gas hydrate was composed of CH 4 and one of C 2 H 6 , C 3 H 8 , H 2 S, and CO 2 , the influence order of the above four gases on the thickness of GHSZ is as follows: H 2 S ＞ C 2 H 6 ＞ C 3 H 8 ＞ CO 2 . Under the gas components of 90% CH 4 , 5% C 2 H 6, and 5% C 3 H 8 , the thickness of GHSZ decreased rapidly as the geothermal gradient increased following an exponential relation with a correlation of 99.92% and increased slowly as permafrost thickness increased following a linear relation with a correlation of 99.9%. In addition, the thickness of a gas hydrate favorable reservoir was determined by comprehensive log methods as 500 m. We conclude that a reservoir within 500 m below the permafrost layer is favorable for gas hydrate reservoir formation." @default.
• W2995590561 created "2019-12-26" @default.
• W2995590561 creator A5012413334 @default.
• W2995590561 creator A5021169746 @default.
• W2995590561 creator A5041439668 @default.
• W2995590561 creator A5056450584 @default.
• W2995590561 creator A5063074043 @default.
• W2995590561 creator A5082003061 @default.
• W2995590561 date "2019-12-10" @default.
• W2995590561 modified "2023-10-15" @default.
• W2995590561 title "A preliminary study of the gas hydrate stability zone in a gas hydrate potential region of China" @default.
• W2995590561 cites W1963619621 @default.
• W2995590561 cites W1970399460 @default.
• W2995590561 cites W1986184972 @default.
• W2995590561 cites W1986692954 @default.
• W2995590561 cites W1992379608 @default.
• W2995590561 cites W2003673844 @default.
• W2995590561 cites W2005343684 @default.
• W2995590561 cites W2008205066 @default.
• W2995590561 cites W2010178797 @default.
• W2995590561 cites W2013282701 @default.
• W2995590561 cites W2018523834 @default.
• W2995590561 cites W2020312486 @default.
• W2995590561 cites W2022008377 @default.
• W2995590561 cites W2032657589 @default.
• W2995590561 cites W2036409439 @default.
• W2995590561 cites W2049719154 @default.
• W2995590561 cites W2058004520 @default.
• W2995590561 cites W2059409472 @default.
• W2995590561 cites W2062022304 @default.
• W2995590561 cites W2063405400 @default.
• W2995590561 cites W2063846068 @default.
• W2995590561 cites W2086165554 @default.
• W2995590561 cites W2098552708 @default.
• W2995590561 cites W2102114010 @default.
• W2995590561 cites W2108011640 @default.
• W2995590561 cites W2108046206 @default.
• W2995590561 cites W2118883207 @default.
• W2995590561 cites W2131741495 @default.
• W2995590561 cites W2132940782 @default.
• W2995590561 cites W2162086856 @default.
• W2995590561 cites W2182725300 @default.
• W2995590561 cites W2186936048 @default.
• W2995590561 cites W2261522619 @default.
• W2995590561 cites W2328059996 @default.
• W2995590561 cites W2520254131 @default.
• W2995590561 cites W2748926671 @default.
• W2995590561 cites W2768131036 @default.
• W2995590561 cites W2772129814 @default.
• W2995590561 cites W2788737361 @default.
• W2995590561 cites W2804487343 @default.
• W2995590561 cites W2885629140 @default.
• W2995590561 cites W2886011293 @default.
• W2995590561 cites W2899692264 @default.
• W2995590561 cites W2926000640 @default.
• W2995590561 cites W2951684143 @default.
• W2995590561 doi "https://doi.org/10.1002/ese3.569" @default.
• W2995590561 hasPublicationYear "2019" @default.
• W2995590561 type Work @default.
• W2995590561 sameAs 2995590561 @default.
• W2995590561 citedByCount "3" @default.
• W2995590561 countsByYear W29955905612020 @default.
• W2995590561 countsByYear W29955905612022 @default.
• W2995590561 crossrefType "journal-article" @default.
• W2995590561 hasAuthorship W2995590561A5012413334 @default.
• W2995590561 hasAuthorship W2995590561A5021169746 @default.
• W2995590561 hasAuthorship W2995590561A5041439668 @default.
• W2995590561 hasAuthorship W2995590561A5056450584 @default.
• W2995590561 hasAuthorship W2995590561A5063074043 @default.
• W2995590561 hasAuthorship W2995590561A5082003061 @default.
• W2995590561 hasBestOaLocation W29955905611 @default.
• W2995590561 hasConcept C100402318 @default.
• W2995590561 hasConcept C111368507 @default.
• W2995590561 hasConcept C111766609 @default.
• W2995590561 hasConcept C127313418 @default.
• W2995590561 hasConcept C15098985 @default.
• W2995590561 hasConcept C178790620 @default.
• W2995590561 hasConcept C185592680 @default.
• W2995590561 hasConcept C199289684 @default.
• W2995590561 hasConcept C2781060337 @default.
• W2995590561 hasConcept C5900021 @default.
• W2995590561 hasConcept C8058405 @default.
• W2995590561 hasConceptScore W2995590561C100402318 @default.
• W2995590561 hasConceptScore W2995590561C111368507 @default.
• W2995590561 hasConceptScore W2995590561C111766609 @default.
• W2995590561 hasConceptScore W2995590561C127313418 @default.
• W2995590561 hasConceptScore W2995590561C15098985 @default.
• W2995590561 hasConceptScore W2995590561C178790620 @default.
• W2995590561 hasConceptScore W2995590561C185592680 @default.
• W2995590561 hasConceptScore W2995590561C199289684 @default.
• W2995590561 hasConceptScore W2995590561C2781060337 @default.
• W2995590561 hasConceptScore W2995590561C5900021 @default.
• W2995590561 hasConceptScore W2995590561C8058405 @default.
• W2995590561 hasFunder F4320311687 @default.
• W2995590561 hasFunder F4320321001 @default.
• W2995590561 hasFunder F4320321012 @default.
• W2995590561 hasFunder F4320322665 @default.
• W2995590561 hasFunder F4320337504 @default.

• next