FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1898490411> ?p ?o ?g. }

• W1898490411 endingPage "6738" @default.
• W1898490411 startingPage "6732" @default.
• W1898490411 abstract "Abstract Large amounts of methane (CH 4 ) are known to be emitted from permafrost environments during the autumn freeze‐in, but the specific soil conditions leading up to these bursts are unclear. Therefore, we used an ultrawide band ground‐penetrating radar in Northeast Greenland in autumn 2009 to estimate the volumetric composition inside the soil through dielectric characterization from 200 to 3200 MHz. Our results suggest a compression of the gas reservoir during the phase transition of soil water, which is accompanied by a peak in surface CH 4 emissions. About 1 week thereafter, there seems to be a decompression event, consistent with ground cracking which allows the gas reservoir to expand again. This coincides with the largest CH 4 emission, exceeding the summer maximum by a factor of 4. We argue that these complementary measurement techniques are needed to come to an understanding of tundra CH 4 bursts connected to soil freezing." @default.
• W1898490411 created "2016-06-24" @default.
• W1898490411 creator A5010598856 @default.
• W1898490411 creator A5038404251 @default.
• W1898490411 creator A5040849275 @default.
• W1898490411 creator A5061370990 @default.
• W1898490411 creator A5065945384 @default.
• W1898490411 creator A5073439066 @default.
• W1898490411 creator A5076213437 @default.
• W1898490411 creator A5080231261 @default.
• W1898490411 date "2015-08-24" @default.
• W1898490411 modified "2023-10-01" @default.
• W1898490411 title "Methane emission bursts from permafrost environments during autumn freeze‐in: New insights from ground‐penetrating radar" @default.
• W1898490411 cites W1547310551 @default.
• W1898490411 cites W1967527530 @default.
• W1898490411 cites W1990184879 @default.
• W1898490411 cites W2005648470 @default.
• W1898490411 cites W2016917133 @default.
• W1898490411 cites W2020803217 @default.
• W1898490411 cites W2051414711 @default.
• W1898490411 cites W2052231490 @default.
• W1898490411 cites W2069756757 @default.
• W1898490411 cites W2076827910 @default.
• W1898490411 cites W2077390592 @default.
• W1898490411 cites W2097161880 @default.
• W1898490411 cites W2097441736 @default.
• W1898490411 cites W2106247170 @default.
• W1898490411 cites W2123726127 @default.
• W1898490411 cites W2127041725 @default.
• W1898490411 cites W2144764688 @default.
• W1898490411 cites W2147715656 @default.
• W1898490411 cites W2157423959 @default.
• W1898490411 cites W2158769179 @default.
• W1898490411 cites W2159053543 @default.
• W1898490411 cites W2160023238 @default.
• W1898490411 cites W2338795959 @default.
• W1898490411 cites W4241837466 @default.
• W1898490411 doi "https://doi.org/10.1002/2015gl065034" @default.
• W1898490411 hasPublicationYear "2015" @default.
• W1898490411 type Work @default.
• W1898490411 sameAs 1898490411 @default.
• W1898490411 citedByCount "28" @default.
• W1898490411 countsByYear W18984904112016 @default.
• W1898490411 countsByYear W18984904112017 @default.
• W1898490411 countsByYear W18984904112018 @default.
• W1898490411 countsByYear W18984904112019 @default.
• W1898490411 countsByYear W18984904112020 @default.
• W1898490411 countsByYear W18984904112021 @default.
• W1898490411 countsByYear W18984904112022 @default.
• W1898490411 countsByYear W18984904112023 @default.
• W1898490411 crossrefType "journal-article" @default.
• W1898490411 hasAuthorship W1898490411A5010598856 @default.
• W1898490411 hasAuthorship W1898490411A5038404251 @default.
• W1898490411 hasAuthorship W1898490411A5040849275 @default.
• W1898490411 hasAuthorship W1898490411A5061370990 @default.
• W1898490411 hasAuthorship W1898490411A5065945384 @default.
• W1898490411 hasAuthorship W1898490411A5073439066 @default.
• W1898490411 hasAuthorship W1898490411A5076213437 @default.
• W1898490411 hasAuthorship W1898490411A5080231261 @default.
• W1898490411 hasBestOaLocation W18984904111 @default.
• W1898490411 hasConcept C111368507 @default.
• W1898490411 hasConcept C114793014 @default.
• W1898490411 hasConcept C125069764 @default.
• W1898490411 hasConcept C127313418 @default.
• W1898490411 hasConcept C15098985 @default.
• W1898490411 hasConcept C178790620 @default.
• W1898490411 hasConcept C185592680 @default.
• W1898490411 hasConcept C2780155556 @default.
• W1898490411 hasConcept C39432304 @default.
• W1898490411 hasConcept C41008148 @default.
• W1898490411 hasConcept C516920438 @default.
• W1898490411 hasConcept C518008717 @default.
• W1898490411 hasConcept C554190296 @default.
• W1898490411 hasConcept C71813955 @default.
• W1898490411 hasConcept C76155785 @default.
• W1898490411 hasConcept C91586092 @default.
• W1898490411 hasConceptScore W1898490411C111368507 @default.
• W1898490411 hasConceptScore W1898490411C114793014 @default.
• W1898490411 hasConceptScore W1898490411C125069764 @default.
• W1898490411 hasConceptScore W1898490411C127313418 @default.
• W1898490411 hasConceptScore W1898490411C15098985 @default.
• W1898490411 hasConceptScore W1898490411C178790620 @default.
• W1898490411 hasConceptScore W1898490411C185592680 @default.
• W1898490411 hasConceptScore W1898490411C2780155556 @default.
• W1898490411 hasConceptScore W1898490411C39432304 @default.
• W1898490411 hasConceptScore W1898490411C41008148 @default.
• W1898490411 hasConceptScore W1898490411C516920438 @default.
• W1898490411 hasConceptScore W1898490411C518008717 @default.
• W1898490411 hasConceptScore W1898490411C554190296 @default.
• W1898490411 hasConceptScore W1898490411C71813955 @default.
• W1898490411 hasConceptScore W1898490411C76155785 @default.
• W1898490411 hasConceptScore W1898490411C91586092 @default.
• W1898490411 hasFunder F4320325128 @default.
• W1898490411 hasIssue "16" @default.
• W1898490411 hasLocation W18984904111 @default.
• W1898490411 hasOpenAccess W1898490411 @default.
• W1898490411 hasPrimaryLocation W18984904111 @default.
• W1898490411 hasRelatedWork W2133694882 @default.

• next