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Cosmogenic soil production rate calculator

To understand the rates at which soils form from bedrock, it is important to know the rates at which the bedrock surface lowers (the apparent erosion rate, which is assumed to be constant). Previous models that calculate apparent erosion rates using measured concentrations of cosmogenic radionuclide...

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Detalles Bibliográficos
Autores principales: Rodés, Ángel, Evans, Daniel L.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Elsevier 2019
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6994705/
https://www.ncbi.nlm.nih.gov/pubmed/32021816
http://dx.doi.org/10.1016/j.mex.2019.11.026
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author Rodés, Ángel
Evans, Daniel L.
author_facet Rodés, Ángel
Evans, Daniel L.
author_sort Rodés, Ángel
collection PubMed
description To understand the rates at which soils form from bedrock, it is important to know the rates at which the bedrock surface lowers (the apparent erosion rate, which is assumed to be constant). Previous models that calculate apparent erosion rates using measured concentrations of cosmogenic radionuclides rely on the assumption that the bulk density of the soil which forms as a product of bedrock erosion either equals that of the bedrock itself or is constant with depth down the soil profile. This assumption fails to recognise that soils have significantly lower densities that might not be constant with depth. The model presented here allows for the calculation of isotopically-derived soil production rates, considering the bulk density profile of the soil overlying the bedrock surface. This calculator, which can be run both in MATLAB® and GNU Octave©, represents a novel and significant contribution to the derivation of soil production rates.
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spelling pubmed-69947052020-02-04 Cosmogenic soil production rate calculator Rodés, Ángel Evans, Daniel L. MethodsX Earth and Planetary Science To understand the rates at which soils form from bedrock, it is important to know the rates at which the bedrock surface lowers (the apparent erosion rate, which is assumed to be constant). Previous models that calculate apparent erosion rates using measured concentrations of cosmogenic radionuclides rely on the assumption that the bulk density of the soil which forms as a product of bedrock erosion either equals that of the bedrock itself or is constant with depth down the soil profile. This assumption fails to recognise that soils have significantly lower densities that might not be constant with depth. The model presented here allows for the calculation of isotopically-derived soil production rates, considering the bulk density profile of the soil overlying the bedrock surface. This calculator, which can be run both in MATLAB® and GNU Octave©, represents a novel and significant contribution to the derivation of soil production rates. Elsevier 2019-11-28 /pmc/articles/PMC6994705/ /pubmed/32021816 http://dx.doi.org/10.1016/j.mex.2019.11.026 Text en © 2019 The Authors http://creativecommons.org/licenses/by/4.0/ This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/).
spellingShingle Earth and Planetary Science
Rodés, Ángel
Evans, Daniel L.
Cosmogenic soil production rate calculator
title Cosmogenic soil production rate calculator
title_full Cosmogenic soil production rate calculator
title_fullStr Cosmogenic soil production rate calculator
title_full_unstemmed Cosmogenic soil production rate calculator
title_short Cosmogenic soil production rate calculator
title_sort cosmogenic soil production rate calculator
topic Earth and Planetary Science
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6994705/
https://www.ncbi.nlm.nih.gov/pubmed/32021816
http://dx.doi.org/10.1016/j.mex.2019.11.026
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