FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2003139655> ?p ?o ?g. }

• W2003139655 endingPage "11000" @default.
• W2003139655 startingPage "10983" @default.
• W2003139655 abstract "Ridge crest hydrothermal systems are generally characterized by high heat fluxes and a permeable top which allows fluids to flow freely across the seafloor. The basic patterns of flow and heat transport in such systems are poorly known especially at high Rayleigh numbers. We present the results of a laboratory study using a wide‐aspect ratio, open‐top Hele‐Shaw cell heated from below. The model is an analog for two‐dimensional hydrothermal convection. The onset of convection occurs at a Rayleigh number Ra = 20.4 in good agreement with numerical predictions. Above onset, the spacing of upwelling plumes decreases quickly with the Rayleigh number before reaching an asymptotic limit in the range 0.2–0.3 above Ra ≈ 125. Periodic unsteady flow is first observed at Ra ≈ 47 and is a result of small thermals that are advected horizontally in the bottom boundary layer. The amplitude, frequency, and irregularity of oscillations increase with the Rayleigh number. Unsteadiness can also result from the repeated formation of new plumes accompanied by the merging of plumes elsewhere in the model. Above Ra ≈ 590, the flow patterns show no dominant frequency and are chaotic. In the unsteady regime the frequency of oscillations scales as Ra 1.92 and the Nusselt number scales as Ra 0.91 above Ra ≈ 200. These relationships are in close agreement with theoretical scalings for high Rayleigh number porous convection, Nu ∝ Ra and ƒ ∝ Ra 2 . Assuming vigorous mid‐ocean ridge systems can be approximated by flow through a Darcy porous media, our results predict that upwelling sites will be spaced at about half the depth of circulation. This is compatible with observations on the Endeavour segment of the Juan de Fuca Ridge. Our results also predict that ridge crest hydrothermal systems with Nusselt numbers of 10–500, will exhibit unsteady flow at periods of ∼500–0.2 years. Unsteady convection has not yet been observed, perhaps because highly permeable flow channels stabilize the flow in real systems." @default.
• W2003139655 created "2016-06-24" @default.
• W2003139655 creator A5024274753 @default.
• W2003139655 creator A5038878385 @default.
• W2003139655 date "2001-06-10" @default.
• W2003139655 modified "2023-10-13" @default.
• W2003139655 title "Laboratory studies of high Rayleigh number circulation in an open‐top Hele‐Shaw cell: An analog to mid‐ocean ridge hydrothermal systems" @default.
• W2003139655 cites W121624279 @default.
• W2003139655 cites W1968593934 @default.
• W2003139655 cites W1968681582 @default.
• W2003139655 cites W1969726119 @default.
• W2003139655 cites W1973680512 @default.
• W2003139655 cites W1976785776 @default.
• W2003139655 cites W1977308675 @default.
• W2003139655 cites W1978156800 @default.
• W2003139655 cites W1994134090 @default.
• W2003139655 cites W1996525097 @default.
• W2003139655 cites W1997921817 @default.
• W2003139655 cites W2001747122 @default.
• W2003139655 cites W2002278475 @default.
• W2003139655 cites W2003005196 @default.
• W2003139655 cites W2003754165 @default.
• W2003139655 cites W2004094496 @default.
• W2003139655 cites W2004625570 @default.
• W2003139655 cites W2007116652 @default.
• W2003139655 cites W2011856326 @default.
• W2003139655 cites W2014674255 @default.
• W2003139655 cites W2017154790 @default.
• W2003139655 cites W2018115470 @default.
• W2003139655 cites W2023366799 @default.
• W2003139655 cites W2023488081 @default.
• W2003139655 cites W2036258155 @default.
• W2003139655 cites W2037680752 @default.
• W2003139655 cites W2042362098 @default.
• W2003139655 cites W2044395857 @default.
• W2003139655 cites W2045580715 @default.
• W2003139655 cites W2046491644 @default.
• W2003139655 cites W2051170103 @default.
• W2003139655 cites W2052880187 @default.
• W2003139655 cites W2054509582 @default.
• W2003139655 cites W2055044852 @default.
• W2003139655 cites W2061672437 @default.
• W2003139655 cites W2064969558 @default.
• W2003139655 cites W2071698372 @default.
• W2003139655 cites W2078099897 @default.
• W2003139655 cites W2082697422 @default.
• W2003139655 cites W2084712840 @default.
• W2003139655 cites W2102243269 @default.
• W2003139655 cites W2121983062 @default.
• W2003139655 cites W2122963397 @default.
• W2003139655 cites W2156437513 @default.
• W2003139655 cites W2158818323 @default.
• W2003139655 cites W2160462823 @default.
• W2003139655 cites W2163842229 @default.
• W2003139655 cites W2167034012 @default.
• W2003139655 cites W2167544181 @default.
• W2003139655 cites W2169729655 @default.
• W2003139655 cites W2170258733 @default.
• W2003139655 doi "https://doi.org/10.1029/2000jb900470" @default.
• W2003139655 hasPublicationYear "2001" @default.
• W2003139655 type Work @default.
• W2003139655 sameAs 2003139655 @default.
• W2003139655 citedByCount "20" @default.
• W2003139655 countsByYear W20031396552012 @default.
• W2003139655 countsByYear W20031396552013 @default.
• W2003139655 countsByYear W20031396552015 @default.
• W2003139655 countsByYear W20031396552017 @default.
• W2003139655 countsByYear W20031396552018 @default.
• W2003139655 countsByYear W20031396552019 @default.
• W2003139655 countsByYear W20031396552020 @default.
• W2003139655 crossrefType "journal-article" @default.
• W2003139655 hasAuthorship W2003139655A5024274753 @default.
• W2003139655 hasAuthorship W2003139655A5038878385 @default.
• W2003139655 hasBestOaLocation W20031396551 @default.
• W2003139655 hasConcept C106836276 @default.
• W2003139655 hasConcept C10899652 @default.
• W2003139655 hasConcept C120665830 @default.
• W2003139655 hasConcept C121332964 @default.
• W2003139655 hasConcept C127313418 @default.
• W2003139655 hasConcept C130230704 @default.
• W2003139655 hasConcept C151730666 @default.
• W2003139655 hasConcept C156622251 @default.
• W2003139655 hasConcept C165205528 @default.
• W2003139655 hasConcept C182748727 @default.
• W2003139655 hasConcept C196558001 @default.
• W2003139655 hasConcept C32277403 @default.
• W2003139655 hasConcept C38349280 @default.
• W2003139655 hasConcept C46244369 @default.
• W2003139655 hasConcept C48880136 @default.
• W2003139655 hasConcept C54791560 @default.
• W2003139655 hasConcept C57879066 @default.
• W2003139655 hasConcept C8058405 @default.
• W2003139655 hasConceptScore W2003139655C106836276 @default.
• W2003139655 hasConceptScore W2003139655C10899652 @default.
• W2003139655 hasConceptScore W2003139655C120665830 @default.
• W2003139655 hasConceptScore W2003139655C121332964 @default.
• W2003139655 hasConceptScore W2003139655C127313418 @default.
• W2003139655 hasConceptScore W2003139655C130230704 @default.

• next