Erosional response of granular material in landscape models
<p>Tectonics and erosion–sedimentation are the main processes responsible for shaping the Earth's surface. The link between these processes has a strong influence on the evolution of landscapes. One of the tools we have for investigating coupled process models is analog modeling. Here we...
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doaj-6a4e42dbf8344fbe951f7e9ea700fca72020-11-25T04:05:12ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2020-11-01897399310.5194/esurf-8-973-2020Erosional response of granular material in landscape modelsR. Reitano0C. Faccenna1C. Faccenna2F. Funiciello3F. Corbi4F. Corbi5S. D. Willett6Dipartimento di Scienze, Laboratory of Experimental Tectonics, Università “Roma Tre”, Rome, 00146, ItalyDipartimento di Scienze, Laboratory of Experimental Tectonics, Università “Roma Tre”, Rome, 00146, ItalyDepartment of Geological Sciences, Jackson School of Geosciences, The University of Texas at Austin, Austin, TX, USADipartimento di Scienze, Laboratory of Experimental Tectonics, Università “Roma Tre”, Rome, 00146, ItalyDipartimento di Scienze, Laboratory of Experimental Tectonics, Università “Roma Tre”, Rome, 00146, ItalyIstituto di Geologia Ambientale e Geoingegneria – Consiglio Nazionale delle Ricerche, Rome, ItalyDepartment of Earth Sciences, ETH Zürich, Sonneggstrasse 5, 8092 Zurich, Switzerland<p>Tectonics and erosion–sedimentation are the main processes responsible for shaping the Earth's surface. The link between these processes has a strong influence on the evolution of landscapes. One of the tools we have for investigating coupled process models is analog modeling. Here we contribute to the utility of this tool by presenting laboratory-scaled analog models of erosion. We explore the erosional response of different materials to imposed boundary conditions, trying to find the composite material that best mimics the behavior of the natural prototype. The models recreate conditions in which tectonic uplift is no longer active, but there is an imposed fixed slope. On this slope the erosion is triggered by precipitation and gravity, with the formation of channels in valleys and diffusion on hillslope that are functions of the analog material. Using digital elevation models (DEMs) and a laser scan correlation technique, we show model evolution and measure sediment discharge rates. We propose three main components of our analog material (silica powder, glass microbeads and PVC powder; PVC: polyvinyl chloride), and we investigate how different proportions of these components affect the model evolution and the development of landscapes. We find that silica powder is mainly responsible for creating a realistic landscape in the laboratory. Furthermore, we find that varying the concentration of silica powder between 40 <span class="inline-formula">wt %</span> and 50 <span class="inline-formula">wt %</span> (with glass microbeads and PVC powder in the range 35 <span class="inline-formula">wt %</span>–40 <span class="inline-formula">wt %</span> and 15 <span class="inline-formula">wt %</span>–20 <span class="inline-formula">wt %</span>, respectively) results in metrics and morphologies that are comparable with those from natural prototypes.</p>https://esurf.copernicus.org/articles/8/973/2020/esurf-8-973-2020.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
R. Reitano C. Faccenna C. Faccenna F. Funiciello F. Corbi F. Corbi S. D. Willett |
spellingShingle |
R. Reitano C. Faccenna C. Faccenna F. Funiciello F. Corbi F. Corbi S. D. Willett Erosional response of granular material in landscape models Earth Surface Dynamics |
author_facet |
R. Reitano C. Faccenna C. Faccenna F. Funiciello F. Corbi F. Corbi S. D. Willett |
author_sort |
R. Reitano |
title |
Erosional response of granular material in landscape models |
title_short |
Erosional response of granular material in landscape models |
title_full |
Erosional response of granular material in landscape models |
title_fullStr |
Erosional response of granular material in landscape models |
title_full_unstemmed |
Erosional response of granular material in landscape models |
title_sort |
erosional response of granular material in landscape models |
publisher |
Copernicus Publications |
series |
Earth Surface Dynamics |
issn |
2196-6311 2196-632X |
publishDate |
2020-11-01 |
description |
<p>Tectonics and erosion–sedimentation are the main processes responsible for shaping the Earth's surface. The link between these processes has a strong
influence on the evolution of landscapes. One of the tools we have for investigating coupled process models is analog modeling. Here we contribute
to the utility of this tool by presenting laboratory-scaled analog models of erosion. We explore the erosional response of different materials to
imposed boundary conditions, trying to find the composite material that best mimics the behavior of the natural prototype. The models recreate
conditions in which tectonic uplift is no longer active, but there is an imposed fixed slope. On this slope the erosion is triggered by precipitation
and gravity, with the formation of channels in valleys and diffusion on hillslope that are functions of the analog material. Using digital elevation
models (DEMs) and a laser scan correlation technique, we show model evolution and measure sediment discharge rates. We propose three main components of
our analog material (silica powder, glass microbeads and PVC powder; PVC: polyvinyl chloride), and we investigate how different proportions of these components affect the
model evolution and the development of landscapes. We find that silica powder is mainly responsible for creating a realistic landscape in
the laboratory. Furthermore, we find that varying the concentration of silica powder between 40 <span class="inline-formula">wt %</span> and 50 <span class="inline-formula">wt %</span> (with glass microbeads and PVC
powder in the range 35 <span class="inline-formula">wt %</span>–40 <span class="inline-formula">wt %</span> and 15 <span class="inline-formula">wt %</span>–20 <span class="inline-formula">wt %</span>, respectively) results in metrics and morphologies that are comparable with
those from natural prototypes.</p> |
url |
https://esurf.copernicus.org/articles/8/973/2020/esurf-8-973-2020.pdf |
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