FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2049131837> ?p ?o ?g. }

• W2049131837 abstract "[1] Seamounts and volcanic islands are regions of the seafloor where pressure gradients, caused by temperature variations, are large enough to drive fluid flow. Compaction in surrounding sedimentary aprons, formed during mass wasting of these features, drives fluid flow as well. In seamount environments a complex flow pattern evolves as effects of compaction and free convection interact. We use transient finite element modeling to explore fluid flow and pore pressure in a volcanic edifice and its surrounding sedimentary apron to determine the hydrogeologic and pore pressure regime. Models are based on geophysical cross sections of the Hawaiian Islands and include the volcanic edifice, sedimentary apron, and underlying oceanic crust. Models simulate growth of the volcanic island, flexure of the oceanic crust due to loading, and formation of the sedimentary apron. High sedimentation rates of up to 1 mm/yr during volcanic building cause compaction in the sedimentary apron, and the weight of the edifice compacts the pelagic sediment beneath it; compaction-driven flow dominates flow patterns. Excess pore pressures are highest during the beginning of volcanic construction and decline through the remainder of the simulation. As sedimentation decreases, compaction-driven and buoyancy-driven flow both control flow patterns. When sedimentation stops, pore pressure dissipates, and buoyancy-driven flow dominates the flow regime. Pore pressure ratios indicate that under certain parameter conditions, pore pressure may exceed lithostatic, leading to unstable edifice conditions. Although fluid velocities are small (q < 0.5 cm/yr), the hydrologic regime has important implications for slope stability, volcanic spreading, sedimentation processes, and geochemical transport." @default.
• W2049131837 created "2016-06-24" @default.
• W2049131837 creator A5021270219 @default.
• W2049131837 creator A5076217516 @default.
• W2049131837 date "2004-02-01" @default.
• W2049131837 modified "2023-09-23" @default.
• W2049131837 title "Transient hydrogeologic models for submarine flow in volcanic seamounts: 1. The Hawaiian Islands" @default.
• W2049131837 cites W1482367149 @default.
• W2049131837 cites W1495519640 @default.
• W2049131837 cites W1525269631 @default.
• W2049131837 cites W1964332514 @default.
• W2049131837 cites W1964576280 @default.
• W2049131837 cites W1968028981 @default.
• W2049131837 cites W1968087724 @default.
• W2049131837 cites W1971910394 @default.
• W2049131837 cites W1972133069 @default.
• W2049131837 cites W1975523684 @default.
• W2049131837 cites W1985011582 @default.
• W2049131837 cites W1987908336 @default.
• W2049131837 cites W1988239312 @default.
• W2049131837 cites W1993066972 @default.
• W2049131837 cites W2006270629 @default.
• W2049131837 cites W2010975107 @default.
• W2049131837 cites W2015445406 @default.
• W2049131837 cites W2017370998 @default.
• W2049131837 cites W2020788784 @default.
• W2049131837 cites W2020896503 @default.
• W2049131837 cites W2024826611 @default.
• W2049131837 cites W2038703090 @default.
• W2049131837 cites W2048075105 @default.
• W2049131837 cites W2048572409 @default.
• W2049131837 cites W2049199841 @default.
• W2049131837 cites W2055044852 @default.
• W2049131837 cites W2059983526 @default.
• W2049131837 cites W2061650077 @default.
• W2049131837 cites W2072751239 @default.
• W2049131837 cites W2079026875 @default.
• W2049131837 cites W2086509057 @default.
• W2049131837 cites W2091806628 @default.
• W2049131837 cites W2093453195 @default.
• W2049131837 cites W2093824165 @default.
• W2049131837 cites W2101842711 @default.
• W2049131837 cites W2102595079 @default.
• W2049131837 cites W2102729179 @default.
• W2049131837 cites W2107440173 @default.
• W2049131837 cites W2108893738 @default.
• W2049131837 cites W2111248120 @default.
• W2049131837 cites W2122084993 @default.
• W2049131837 cites W2129426845 @default.
• W2049131837 cites W2143729170 @default.
• W2049131837 cites W2148628311 @default.
• W2049131837 cites W2151370956 @default.
• W2049131837 cites W2160455456 @default.
• W2049131837 cites W2170384715 @default.
• W2049131837 cites W2315026256 @default.
• W2049131837 doi "https://doi.org/10.1029/2003jb002401" @default.
• W2049131837 hasPublicationYear "2004" @default.
• W2049131837 type Work @default.
• W2049131837 sameAs 2049131837 @default.
• W2049131837 citedByCount "1" @default.
• W2049131837 crossrefType "journal-article" @default.
• W2049131837 hasAuthorship W2049131837A5021270219 @default.
• W2049131837 hasAuthorship W2049131837A5076217516 @default.
• W2049131837 hasBestOaLocation W20491318371 @default.
• W2049131837 hasConcept C102579867 @default.
• W2049131837 hasConcept C114793014 @default.
• W2049131837 hasConcept C117485682 @default.
• W2049131837 hasConcept C120806208 @default.
• W2049131837 hasConcept C127313418 @default.
• W2049131837 hasConcept C135559958 @default.
• W2049131837 hasConcept C17409809 @default.
• W2049131837 hasConcept C187320778 @default.
• W2049131837 hasConcept C5900021 @default.
• W2049131837 hasConcept C6494504 @default.
• W2049131837 hasConcept C8058405 @default.
• W2049131837 hasConceptScore W2049131837C102579867 @default.
• W2049131837 hasConceptScore W2049131837C114793014 @default.
• W2049131837 hasConceptScore W2049131837C117485682 @default.
• W2049131837 hasConceptScore W2049131837C120806208 @default.
• W2049131837 hasConceptScore W2049131837C127313418 @default.
• W2049131837 hasConceptScore W2049131837C135559958 @default.
• W2049131837 hasConceptScore W2049131837C17409809 @default.
• W2049131837 hasConceptScore W2049131837C187320778 @default.
• W2049131837 hasConceptScore W2049131837C5900021 @default.
• W2049131837 hasConceptScore W2049131837C6494504 @default.
• W2049131837 hasConceptScore W2049131837C8058405 @default.
• W2049131837 hasIssue "B2" @default.
• W2049131837 hasLocation W20491318371 @default.
• W2049131837 hasOpenAccess W2049131837 @default.
• W2049131837 hasPrimaryLocation W20491318371 @default.
• W2049131837 hasRelatedWork W1510632934 @default.
• W2049131837 hasRelatedWork W2021049577 @default.
• W2049131837 hasRelatedWork W2046905393 @default.
• W2049131837 hasRelatedWork W2139994190 @default.
• W2049131837 hasRelatedWork W2148628311 @default.
• W2049131837 hasRelatedWork W2203665432 @default.
• W2049131837 hasRelatedWork W2800679694 @default.
• W2049131837 hasRelatedWork W2985110962 @default.
• W2049131837 hasRelatedWork W3210313583 @default.
• W2049131837 hasRelatedWork W4253875906 @default.

• next