Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities

The Terrestrial Photogrammetry Scanner (TEPHOS) offers the possibility to precisely monitor linear erosion features using the Structure from Motion (SfM) technique. This is a static, multi-camera array and dynamically moves the digital videoframe camera designed to obtain 3-D models of rills before...

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Main Authors: Alexander André Remke, Jesus Rodrigo-Comino, Stefan Wirtz, Johannes B. Ries
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Sensors
Subjects:
Online Access:https://www.mdpi.com/1424-8220/20/21/6254
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spelling doaj-8a7dad622b294fedbfcabfa21a1bea252020-11-25T03:37:17ZengMDPI AGSensors1424-82202020-11-01206254625410.3390/s20216254Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying CapabilitiesAlexander André Remke0Jesus Rodrigo-Comino1Stefan Wirtz2Johannes B. Ries3Department of Physical Geography, University of Trier, 54286 Trier, GermanyDepartment of Physical Geography, University of Trier, 54286 Trier, GermanyZentrum für Geoinformationswesen der Bundeswehr, 53879 Euskirchen, GermanyDepartment of Physical Geography, University of Trier, 54286 Trier, GermanyThe Terrestrial Photogrammetry Scanner (TEPHOS) offers the possibility to precisely monitor linear erosion features using the Structure from Motion (SfM) technique. This is a static, multi-camera array and dynamically moves the digital videoframe camera designed to obtain 3-D models of rills before and after the runoff experiments. The main goals were to (1) obtain better insight into the rills; (2) reduce the technical gaps generated during the runoff experiments using only one camera; (3) enable the visual location of eroded, transported and accumulated material. In this study, we obtained a mean error for all pictures reaching up to 0.00433 pixels and every single one of them was under 0.15 pixel. So, we obtained an error of about 1/10th of the maximum possible resolution. A conservative value for the overall accuracy was one pixel, which means that, in our case, the accuracy was 0.0625 mm. The point density, in our example, reached 29,484,888 pts/m². It became possible to get a glimpse of the hotspots of sidewall failure and rill-bed incision. We conclude that the combination of both approaches—rill experiment and 3D models—will make easy under laboratory conditions to describe the soil erosion processes accurately in a mathematical–physical way.https://www.mdpi.com/1424-8220/20/21/6254linear erosiongeo-sensorsTEPHOSenvironmental monitoringrunoff simulationStructure from Motion (SfM)
collection DOAJ
language English
format Article
sources DOAJ
author Alexander André Remke
Jesus Rodrigo-Comino
Stefan Wirtz
Johannes B. Ries
spellingShingle Alexander André Remke
Jesus Rodrigo-Comino
Stefan Wirtz
Johannes B. Ries
Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities
Sensors
linear erosion
geo-sensors
TEPHOS
environmental monitoring
runoff simulation
Structure from Motion (SfM)
author_facet Alexander André Remke
Jesus Rodrigo-Comino
Stefan Wirtz
Johannes B. Ries
author_sort Alexander André Remke
title Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities
title_short Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities
title_full Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities
title_fullStr Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities
title_full_unstemmed Finding Possible Weakness in the Runoff Simulation Experiments to Assess Rill Erosion Changes without Non-Intermittent Surveying Capabilities
title_sort finding possible weakness in the runoff simulation experiments to assess rill erosion changes without non-intermittent surveying capabilities
publisher MDPI AG
series Sensors
issn 1424-8220
publishDate 2020-11-01
description The Terrestrial Photogrammetry Scanner (TEPHOS) offers the possibility to precisely monitor linear erosion features using the Structure from Motion (SfM) technique. This is a static, multi-camera array and dynamically moves the digital videoframe camera designed to obtain 3-D models of rills before and after the runoff experiments. The main goals were to (1) obtain better insight into the rills; (2) reduce the technical gaps generated during the runoff experiments using only one camera; (3) enable the visual location of eroded, transported and accumulated material. In this study, we obtained a mean error for all pictures reaching up to 0.00433 pixels and every single one of them was under 0.15 pixel. So, we obtained an error of about 1/10th of the maximum possible resolution. A conservative value for the overall accuracy was one pixel, which means that, in our case, the accuracy was 0.0625 mm. The point density, in our example, reached 29,484,888 pts/m². It became possible to get a glimpse of the hotspots of sidewall failure and rill-bed incision. We conclude that the combination of both approaches—rill experiment and 3D models—will make easy under laboratory conditions to describe the soil erosion processes accurately in a mathematical–physical way.
topic linear erosion
geo-sensors
TEPHOS
environmental monitoring
runoff simulation
Structure from Motion (SfM)
url https://www.mdpi.com/1424-8220/20/21/6254
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