FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2132043686> ?p ?o ?g. }

• W2132043686 endingPage "125" @default.
• W2132043686 startingPage "105" @default.
• W2132043686 abstract "In situ produced 10Be and 26Al, measured in 40 sediment samples collected from the Iron and Granite Mountain piedmonts, eastern Mojave Desert, provide a unique view of piedmont modification processes and process rates over the 103 to 105 year time scale. Cosmogenic nuclide-based models suggest that the Iron and Granite Mountains generate 0.11–0.13 and 0.082–0.097 m3 of sediment per year per meter of rangefront, respectively. The sediment moves down the piedmont in an active transport layer (ATL), which is 20 to 30 cm thick (based on visual observations, measurements of depth to a buried B-horizon, cosmogenic nuclide data, and maximum ephemeral channel depths). Sediment in this layer is well-mixed vertically and horizontally on the 102 year time scale, indicating that the small ephemeral channels, which dominate the piedmont surface migrate quickly. Interpretive models of increasing nuclide activities at depth in two pits suggest steady sediment deposition on the piedmont (at rates between 17–21 and 38–45 m Ma−1) until the late Pleistocene epoch, when a discontinuity to markedly lower nuclide activities in the isotopically well-mixed active transport layer suggests that deposition stopped, a significant change in piedmont behavior. Nuclide activities in 10 amalgamated surface samples, each collected along a different 4-km-long transect, increase steadily away from the mountain front. Thus, we infer that sediment is uniformly dosed by cosmic rays as it is transported down the Iron and Granite Mountain piedmonts. Interpretive models suggest that long-term average sediment speeds down the Iron and Granite Mountain piedmonts are a few decimeters to a meter per year." @default.
• W2132043686 created "2016-06-24" @default.
• W2132043686 creator A5003372017 @default.
• W2132043686 creator A5027616747 @default.
• W2132043686 creator A5037488197 @default.
• W2132043686 creator A5065669012 @default.
• W2132043686 creator A5069756627 @default.
• W2132043686 date "2002-06-01" @default.
• W2132043686 modified "2023-10-14" @default.
• W2132043686 title "Quantifying sediment transport on desert piedmonts using 10Be and 26Al" @default.
• W2132043686 cites W1489089526 @default.
• W2132043686 cites W1986054052 @default.
• W2132043686 cites W1990613401 @default.
• W2132043686 cites W1994131355 @default.
• W2132043686 cites W2002473398 @default.
• W2132043686 cites W2009943538 @default.
• W2132043686 cites W2016055802 @default.
• W2132043686 cites W2020038340 @default.
• W2132043686 cites W2029466114 @default.
• W2132043686 cites W2031755626 @default.
• W2132043686 cites W2035178161 @default.
• W2132043686 cites W2038908314 @default.
• W2132043686 cites W2066941285 @default.
• W2132043686 cites W2074006941 @default.
• W2132043686 cites W2076212076 @default.
• W2132043686 cites W2080461854 @default.
• W2132043686 cites W2087899885 @default.
• W2132043686 cites W2093570562 @default.
• W2132043686 cites W2098797024 @default.
• W2132043686 cites W2099338989 @default.
• W2132043686 cites W2127273188 @default.
• W2132043686 cites W2131642202 @default.
• W2132043686 cites W2149128668 @default.
• W2132043686 cites W2168133538 @default.
• W2132043686 cites W2175637255 @default.
• W2132043686 cites W2313255370 @default.
• W2132043686 cites W2320432250 @default.
• W2132043686 cites W4253495497 @default.
• W2132043686 cites W4300496685 @default.
• W2132043686 doi "https://doi.org/10.1016/s0169-555x(01)00192-1" @default.
• W2132043686 hasPublicationYear "2002" @default.
• W2132043686 type Work @default.
• W2132043686 sameAs 2132043686 @default.
• W2132043686 citedByCount "66" @default.
• W2132043686 countsByYear W21320436862012 @default.
• W2132043686 countsByYear W21320436862013 @default.
• W2132043686 countsByYear W21320436862014 @default.
• W2132043686 countsByYear W21320436862015 @default.
• W2132043686 countsByYear W21320436862016 @default.
• W2132043686 countsByYear W21320436862017 @default.
• W2132043686 countsByYear W21320436862018 @default.
• W2132043686 countsByYear W21320436862019 @default.
• W2132043686 countsByYear W21320436862020 @default.
• W2132043686 countsByYear W21320436862022 @default.
• W2132043686 crossrefType "journal-article" @default.
• W2132043686 hasAuthorship W2132043686A5003372017 @default.
• W2132043686 hasAuthorship W2132043686A5027616747 @default.
• W2132043686 hasAuthorship W2132043686A5037488197 @default.
• W2132043686 hasAuthorship W2132043686A5065669012 @default.
• W2132043686 hasAuthorship W2132043686A5069756627 @default.
• W2132043686 hasConcept C101140149 @default.
• W2132043686 hasConcept C111309251 @default.
• W2132043686 hasConcept C111368507 @default.
• W2132043686 hasConcept C11413529 @default.
• W2132043686 hasConcept C114793014 @default.
• W2132043686 hasConcept C121332964 @default.
• W2132043686 hasConcept C127313418 @default.
• W2132043686 hasConcept C17409809 @default.
• W2132043686 hasConcept C177571023 @default.
• W2132043686 hasConcept C187320778 @default.
• W2132043686 hasConcept C2816523 @default.
• W2132043686 hasConcept C41008148 @default.
• W2132043686 hasConcept C44870925 @default.
• W2132043686 hasConcept C62520636 @default.
• W2132043686 hasConcept C64297162 @default.
• W2132043686 hasConcept C65589250 @default.
• W2132043686 hasConcept C69661492 @default.
• W2132043686 hasConcept C76886044 @default.
• W2132043686 hasConcept C76947770 @default.
• W2132043686 hasConceptScore W2132043686C101140149 @default.
• W2132043686 hasConceptScore W2132043686C111309251 @default.
• W2132043686 hasConceptScore W2132043686C111368507 @default.
• W2132043686 hasConceptScore W2132043686C11413529 @default.
• W2132043686 hasConceptScore W2132043686C114793014 @default.
• W2132043686 hasConceptScore W2132043686C121332964 @default.
• W2132043686 hasConceptScore W2132043686C127313418 @default.
• W2132043686 hasConceptScore W2132043686C17409809 @default.
• W2132043686 hasConceptScore W2132043686C177571023 @default.
• W2132043686 hasConceptScore W2132043686C187320778 @default.
• W2132043686 hasConceptScore W2132043686C2816523 @default.
• W2132043686 hasConceptScore W2132043686C41008148 @default.
• W2132043686 hasConceptScore W2132043686C44870925 @default.
• W2132043686 hasConceptScore W2132043686C62520636 @default.
• W2132043686 hasConceptScore W2132043686C64297162 @default.
• W2132043686 hasConceptScore W2132043686C65589250 @default.
• W2132043686 hasConceptScore W2132043686C69661492 @default.
• W2132043686 hasConceptScore W2132043686C76886044 @default.
• W2132043686 hasConceptScore W2132043686C76947770 @default.

• next