FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1736033808> ?p ?o ?g. }

• W1736033808 endingPage "839" @default.
• W1736033808 startingPage "823" @default.
• W1736033808 abstract "We present a new numerical approach for simulating geomorphic and stratigraphic processes that combines open-channel flow with non-uniform sediment transport law and semi-empirical diffusive mass wasting. It is designed to facilitate modelling of surface processes across multiple space- and time-scales, and under a variety of environmental and tectonic conditions. The physics of open-channel flow is primarily based on an adapted Lagrangian formulation of shallow-water equations. The interaction between flow and surface geology is performed by a non-uniform total-load sediment transport law. Additional hillslope processes are simulated using a semi-empirical method based on a diffusion approach. In the implementation, the resolution of flow dynamics is made on a triangulated grid automatically mapped and adaptively remeshed over a regular orthogonal stratigraphic mesh. These new methods reduce computational time while preserving stability and accuracy of the physical solutions. In order to illustrate the potential of this method for landscape and sedimentary system modelling, we present a set of three generic experiments focusing on assessing the influence of contrasting erodibilities on the evolution of an active bedrock landscape. The modelled ridges morphometrics satisfy established relationships for drainage network geometry and slope distribution, and provide quantitative information on the relative impact of hillslope and channel processes, sediment discharge and alluviation. Our results suggest that contrasting erodibility can stimulate autogenic changes in erosion rate and influence the landscape morphology and preservation. This approach offers new opportunities to investigate joint landscape and sedimentary systems response to external perturbations. The possibility to define and track a large number of materials makes the implementation highly suited to model source-to-sink problems where material dispersion is the key question that needs to be addressed, such as natural resources exploration and basin analysis. Copyright © 2014 John Wiley & Sons, Ltd." @default.
• W1736033808 created "2016-06-24" @default.
• W1736033808 creator A5059231746 @default.
• W1736033808 creator A5060187619 @default.
• W1736033808 date "2014-12-16" @default.
• W1736033808 modified "2023-10-12" @default.
• W1736033808 title "Combined hillslope diffusion and sediment transport simulation applied to landscape dynamics modelling" @default.
• W1736033808 cites W111123141 @default.
• W1736033808 cites W1505152330 @default.
• W1736033808 cites W1533766981 @default.
• W1736033808 cites W1537353194 @default.
• W1736033808 cites W1606571603 @default.
• W1736033808 cites W1606765290 @default.
• W1736033808 cites W1663975594 @default.
• W1736033808 cites W1920174585 @default.
• W1736033808 cites W1971670210 @default.
• W1736033808 cites W1972168971 @default.
• W1736033808 cites W1973493124 @default.
• W1736033808 cites W1976700595 @default.
• W1736033808 cites W1976972127 @default.
• W1736033808 cites W1976989609 @default.
• W1736033808 cites W1979634530 @default.
• W1736033808 cites W1987144912 @default.
• W1736033808 cites W1988537420 @default.
• W1736033808 cites W1991491828 @default.
• W1736033808 cites W1996283133 @default.
• W1736033808 cites W2004243894 @default.
• W1736033808 cites W2008179277 @default.
• W1736033808 cites W2011475523 @default.
• W1736033808 cites W2011679124 @default.
• W1736033808 cites W2016597687 @default.
• W1736033808 cites W2019595634 @default.
• W1736033808 cites W2021905555 @default.
• W1736033808 cites W2025017677 @default.
• W1736033808 cites W2033345860 @default.
• W1736033808 cites W2035207306 @default.
• W1736033808 cites W2037836810 @default.
• W1736033808 cites W2037971711 @default.
• W1736033808 cites W2040513229 @default.
• W1736033808 cites W2050693654 @default.
• W1736033808 cites W2051466016 @default.
• W1736033808 cites W2052717221 @default.
• W1736033808 cites W2057075002 @default.
• W1736033808 cites W2059054619 @default.
• W1736033808 cites W2060702643 @default.
• W1736033808 cites W2066288156 @default.
• W1736033808 cites W2074633921 @default.
• W1736033808 cites W2076744895 @default.
• W1736033808 cites W2080667544 @default.
• W1736033808 cites W2083963037 @default.
• W1736033808 cites W2086747528 @default.
• W1736033808 cites W2088402813 @default.
• W1736033808 cites W2090652217 @default.
• W1736033808 cites W2091819642 @default.
• W1736033808 cites W2095079529 @default.
• W1736033808 cites W2097187375 @default.
• W1736033808 cites W2105290847 @default.
• W1736033808 cites W2109287321 @default.
• W1736033808 cites W2111204986 @default.
• W1736033808 cites W2111552444 @default.
• W1736033808 cites W2119059793 @default.
• W1736033808 cites W2119429580 @default.
• W1736033808 cites W2119534769 @default.
• W1736033808 cites W2120923020 @default.
• W1736033808 cites W2121484925 @default.
• W1736033808 cites W2126310354 @default.
• W1736033808 cites W2128421631 @default.
• W1736033808 cites W2132355961 @default.
• W1736033808 cites W2132745343 @default.
• W1736033808 cites W2132970916 @default.
• W1736033808 cites W2139482396 @default.
• W1736033808 cites W2140403093 @default.
• W1736033808 cites W2146175595 @default.
• W1736033808 cites W2153109963 @default.
• W1736033808 cites W2153978805 @default.
• W1736033808 cites W2155863509 @default.
• W1736033808 cites W2165415867 @default.
• W1736033808 cites W2166976873 @default.
• W1736033808 cites W2170801163 @default.
• W1736033808 cites W2319440775 @default.
• W1736033808 cites W2320485088 @default.
• W1736033808 cites W2495403608 @default.
• W1736033808 cites W3021568154 @default.
• W1736033808 cites W4205698215 @default.
• W1736033808 cites W4214813356 @default.
• W1736033808 doi "https://doi.org/10.1002/esp.3674" @default.
• W1736033808 hasPublicationYear "2014" @default.
• W1736033808 type Work @default.
• W1736033808 sameAs 1736033808 @default.
• W1736033808 citedByCount "29" @default.
• W1736033808 countsByYear W17360338082015 @default.
• W1736033808 countsByYear W17360338082016 @default.
• W1736033808 countsByYear W17360338082017 @default.
• W1736033808 countsByYear W17360338082018 @default.
• W1736033808 countsByYear W17360338082019 @default.
• W1736033808 countsByYear W17360338082020 @default.
• W1736033808 countsByYear W17360338082021 @default.
• W1736033808 countsByYear W17360338082022 @default.

• next