A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain

Regolith, or unconsolidated materials overlying bedrock, exists as an active zone for many geological, geomorphological, hydrological and ecological processes. This zone and its processes are foundational to wide-ranging human needs and activities such as water supply, mineral exploration, forest ha...

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Autores principales: Shane Furze, Antóin M. O’Sullivan, Serge Allard, Toon Pronk, R. Allen Curry
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:d7119edf4cdd47e7a0b82f819263e8ac2021-11-11T18:50:10ZA High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain10.3390/rs132142102072-4292https://doaj.org/article/d7119edf4cdd47e7a0b82f819263e8ac2021-10-01T00:00:00Zhttps://www.mdpi.com/2072-4292/13/21/4210https://doaj.org/toc/2072-4292Regolith, or unconsolidated materials overlying bedrock, exists as an active zone for many geological, geomorphological, hydrological and ecological processes. This zone and its processes are foundational to wide-ranging human needs and activities such as water supply, mineral exploration, forest harvesting, agriculture, and engineered structures. Regolith thickness, or depth-to-bedrock (DTB), is typically unavailable or restricted to finer scale assessments because of the technical and cost limitations of traditional drilling, seismic, and ground-penetrating radar surveys. The objective of this study was to derive a high-resolution (10 m<sup>2</sup>) DTB model for the province of New Brunswick, Canada as a case study. This was accomplished by developing a DTB database from publicly available soil profiles, boreholes, drill holes, well logs, and outcrop transects (<i>n</i> = 203,238). A Random Forest model was produced by modeling the relationships between DTB measurements in the database to gridded datasets derived from both a LiDAR-derived digital elevation model and photo-interpreted surficial geology delineations. In developing the Random Forest model, DTB measurements were split 70:30 for model development and validation, respectively. The DTB model produced an <i>R</i><sup>2</sup> = 92.8%, <i>MAE</i> = 0.18 m, and <i>RMSE</i> = 0.61 m for the training, and an <i>R</i><sup>2</sup> = 80.3%, <i>MAE</i> = 0.18 m, and <i>RMSE</i> = 0.66 m for the validation data. This model provides an unprecedented resolution of DTB variance at a landscape scale. Additionally, the presented framework provides a fundamental understanding of regolith thickness across a post-glacial terrain, with potential application at the global scale.Shane FurzeAntóin M. O’SullivanSerge AllardToon PronkR. Allen CurryMDPI AGarticlebedrockregolithgeomorphologyRandom ForestLiDARmodelingScienceQENRemote Sensing, Vol 13, Iss 4210, p 4210 (2021)
institution DOAJ
collection DOAJ
language EN
topic bedrock
regolith
geomorphology
Random Forest
LiDAR
modeling
Science
Q
spellingShingle bedrock
regolith
geomorphology
Random Forest
LiDAR
modeling
Science
Q
Shane Furze
Antóin M. O’Sullivan
Serge Allard
Toon Pronk
R. Allen Curry
A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain
description Regolith, or unconsolidated materials overlying bedrock, exists as an active zone for many geological, geomorphological, hydrological and ecological processes. This zone and its processes are foundational to wide-ranging human needs and activities such as water supply, mineral exploration, forest harvesting, agriculture, and engineered structures. Regolith thickness, or depth-to-bedrock (DTB), is typically unavailable or restricted to finer scale assessments because of the technical and cost limitations of traditional drilling, seismic, and ground-penetrating radar surveys. The objective of this study was to derive a high-resolution (10 m<sup>2</sup>) DTB model for the province of New Brunswick, Canada as a case study. This was accomplished by developing a DTB database from publicly available soil profiles, boreholes, drill holes, well logs, and outcrop transects (<i>n</i> = 203,238). A Random Forest model was produced by modeling the relationships between DTB measurements in the database to gridded datasets derived from both a LiDAR-derived digital elevation model and photo-interpreted surficial geology delineations. In developing the Random Forest model, DTB measurements were split 70:30 for model development and validation, respectively. The DTB model produced an <i>R</i><sup>2</sup> = 92.8%, <i>MAE</i> = 0.18 m, and <i>RMSE</i> = 0.61 m for the training, and an <i>R</i><sup>2</sup> = 80.3%, <i>MAE</i> = 0.18 m, and <i>RMSE</i> = 0.66 m for the validation data. This model provides an unprecedented resolution of DTB variance at a landscape scale. Additionally, the presented framework provides a fundamental understanding of regolith thickness across a post-glacial terrain, with potential application at the global scale.
format article
author Shane Furze
Antóin M. O’Sullivan
Serge Allard
Toon Pronk
R. Allen Curry
author_facet Shane Furze
Antóin M. O’Sullivan
Serge Allard
Toon Pronk
R. Allen Curry
author_sort Shane Furze
title A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain
title_short A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain
title_full A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain
title_fullStr A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain
title_full_unstemmed A High-Resolution, Random Forest Approach to Mapping Depth-to-Bedrock across Shallow Overburden and Post-Glacial Terrain
title_sort high-resolution, random forest approach to mapping depth-to-bedrock across shallow overburden and post-glacial terrain
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/d7119edf4cdd47e7a0b82f819263e8ac
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