FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000027802> ?p ?o ?g. }

• W2000027802 endingPage "340" @default.
• W2000027802 startingPage "325" @default.
• W2000027802 abstract "Interpretations of regolith and soil thickness in the context of landscape evolution are typically based on the notion that thickness is controlled by the interaction of weathering rates and erosion and tuned to topography. On sideslopes of the Ouachita Mountains, Arkansas, however, there is a high degree of local spatial variability that is largely unrelated to topography. This indicates nonequilibrium in the sense that there is no evidence of a balance between rates of weathering and removal, as is postulated in some conceptual models in geomorphology and pedology. Johnson's soil thickness model is applied as an alternative to interpret local variations in regolith thickness. At the study sites, regolith thickness is not generally related to slope, curvature, elevation, or pedogenic development in the solum. This indicates that variability in thickness is related chiefly to processes and controls acting in the lower regolith, below the solum. The primary controls of variability are local lithological variation, variable structural resistance associated with fractures and bedding planes in strongly tilted Paleozoic sedimentary parent material, and point‐centered pedological influences of trees. A steady state regolith may be relatively rare. Results of this study suggest that an equilibrium regolith thickness is most likely in uniform lithology with a high degree of lithologic purity, less likely in interbedded sedimentary rocks, and more unlikely still if the latter are titled and fractured. Equilibrium thickness would also be more likely where the effects of bioturbation are more areally uniform (as opposed to the point‐centered effects of individual trees) and where the biomantle is above the weathering front." @default.
• W2000027802 created "2016-06-24" @default.
• W2000027802 creator A5010359463 @default.
• W2000027802 creator A5025777199 @default.
• W2000027802 creator A5065002336 @default.
• W2000027802 creator A5078393722 @default.
• W2000027802 date "2005-05-01" @default.
• W2000027802 modified "2023-10-16" @default.
• W2000027802 title "Nonequilibrium Regolith Thickness in the Ouachita Mountains" @default.
• W2000027802 cites W1480646436 @default.
• W2000027802 cites W1556967983 @default.
• W2000027802 cites W1972383019 @default.
• W2000027802 cites W1975386817 @default.
• W2000027802 cites W1978710003 @default.
• W2000027802 cites W1981710965 @default.
• W2000027802 cites W1982455662 @default.
• W2000027802 cites W1998996427 @default.
• W2000027802 cites W2001982791 @default.
• W2000027802 cites W2007489936 @default.
• W2000027802 cites W2019912218 @default.
• W2000027802 cites W2023622578 @default.
• W2000027802 cites W2031755626 @default.
• W2000027802 cites W2042845797 @default.
• W2000027802 cites W2046726092 @default.
• W2000027802 cites W2047078616 @default.
• W2000027802 cites W2057424406 @default.
• W2000027802 cites W2059075294 @default.
• W2000027802 cites W2064762548 @default.
• W2000027802 cites W2065335930 @default.
• W2000027802 cites W2066240087 @default.
• W2000027802 cites W2068658906 @default.
• W2000027802 cites W2073359425 @default.
• W2000027802 cites W2079324534 @default.
• W2000027802 cites W2079854736 @default.
• W2000027802 cites W2084047592 @default.
• W2000027802 cites W2087130443 @default.
• W2000027802 cites W2100610731 @default.
• W2000027802 cites W2115422473 @default.
• W2000027802 cites W2120295188 @default.
• W2000027802 cites W2152015161 @default.
• W2000027802 cites W2322832855 @default.
• W2000027802 cites W2334461786 @default.
• W2000027802 cites W3156882853 @default.
• W2000027802 doi "https://doi.org/10.1086/428808" @default.
• W2000027802 hasPublicationYear "2005" @default.
• W2000027802 type Work @default.
• W2000027802 sameAs 2000027802 @default.
• W2000027802 citedByCount "46" @default.
• W2000027802 countsByYear W20000278022012 @default.
• W2000027802 countsByYear W20000278022013 @default.
• W2000027802 countsByYear W20000278022014 @default.
• W2000027802 countsByYear W20000278022015 @default.
• W2000027802 countsByYear W20000278022016 @default.
• W2000027802 countsByYear W20000278022019 @default.
• W2000027802 countsByYear W20000278022021 @default.
• W2000027802 countsByYear W20000278022022 @default.
• W2000027802 countsByYear W20000278022023 @default.
• W2000027802 crossrefType "journal-article" @default.
• W2000027802 hasAuthorship W2000027802A5010359463 @default.
• W2000027802 hasAuthorship W2000027802A5025777199 @default.
• W2000027802 hasAuthorship W2000027802A5065002336 @default.
• W2000027802 hasAuthorship W2000027802A5078393722 @default.
• W2000027802 hasConcept C114793014 @default.
• W2000027802 hasConcept C121332964 @default.
• W2000027802 hasConcept C122792734 @default.
• W2000027802 hasConcept C127313418 @default.
• W2000027802 hasConcept C138170599 @default.
• W2000027802 hasConcept C144027150 @default.
• W2000027802 hasConcept C153018869 @default.
• W2000027802 hasConcept C159390177 @default.
• W2000027802 hasConcept C159750122 @default.
• W2000027802 hasConcept C169212394 @default.
• W2000027802 hasConcept C17409809 @default.
• W2000027802 hasConcept C184269829 @default.
• W2000027802 hasConcept C2777232088 @default.
• W2000027802 hasConcept C2816523 @default.
• W2000027802 hasConcept C40724407 @default.
• W2000027802 hasConcept C41642174 @default.
• W2000027802 hasConcept C6494504 @default.
• W2000027802 hasConcept C86803240 @default.
• W2000027802 hasConcept C87355193 @default.
• W2000027802 hasConceptScore W2000027802C114793014 @default.
• W2000027802 hasConceptScore W2000027802C121332964 @default.
• W2000027802 hasConceptScore W2000027802C122792734 @default.
• W2000027802 hasConceptScore W2000027802C127313418 @default.
• W2000027802 hasConceptScore W2000027802C138170599 @default.
• W2000027802 hasConceptScore W2000027802C144027150 @default.
• W2000027802 hasConceptScore W2000027802C153018869 @default.
• W2000027802 hasConceptScore W2000027802C159390177 @default.
• W2000027802 hasConceptScore W2000027802C159750122 @default.
• W2000027802 hasConceptScore W2000027802C169212394 @default.
• W2000027802 hasConceptScore W2000027802C17409809 @default.
• W2000027802 hasConceptScore W2000027802C184269829 @default.
• W2000027802 hasConceptScore W2000027802C2777232088 @default.
• W2000027802 hasConceptScore W2000027802C2816523 @default.
• W2000027802 hasConceptScore W2000027802C40724407 @default.
• W2000027802 hasConceptScore W2000027802C41642174 @default.
• W2000027802 hasConceptScore W2000027802C6494504 @default.

• next