A hybrid data–model approach to map soil thickness in mountain hillslopes

<p>Soil thickness plays a central role in the interactions between vegetation, soils, and topography, where it controls the retention and release of water, carbon, nitrogen, and metals. However, mapping soil thickness, here defined as the mobile regolith layer, at high spatial resolution remai...

Full description

Bibliographic Details
Main Authors: Q. Yan, H. Wainwright, B. Dafflon, S. Uhlemann, C. I. Steefel, N. Falco, J. Kwang, S. S. Hubbard
Format: Article
Language:English
Published: Copernicus Publications 2021-10-01
Series:Earth Surface Dynamics
Online Access:https://esurf.copernicus.org/articles/9/1347/2021/esurf-9-1347-2021.pdf
id doaj-b7f5afb52c9e4efdba351503bb80d242
record_format Article
spelling doaj-b7f5afb52c9e4efdba351503bb80d2422021-10-11T06:01:17ZengCopernicus PublicationsEarth Surface Dynamics2196-63112196-632X2021-10-0191347136110.5194/esurf-9-1347-2021A hybrid data–model approach to map soil thickness in mountain hillslopesQ. Yan0H. Wainwright1B. Dafflon2S. Uhlemann3C. I. Steefel4N. Falco5J. Kwang6S. S. Hubbard7Earth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USAEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USAEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USAEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USAEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USAEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USADepartment of Geosciences, University of Massachusetts Amherst, Amherst, MA, USAEarth and Environmental Science Area, Lawrence Berkeley National Laboratory, Berkeley, CA, USA<p>Soil thickness plays a central role in the interactions between vegetation, soils, and topography, where it controls the retention and release of water, carbon, nitrogen, and metals. However, mapping soil thickness, here defined as the mobile regolith layer, at high spatial resolution remains challenging. Here, we develop a hybrid model that combines a process-based model and empirical relationships to estimate the spatial heterogeneity of soil thickness with fine spatial resolution (0.5 m). We apply this model to two aspects of hillslopes (southwest- and northeast-facing, respectively) in the East River watershed in Colorado. Two independent measurement methods – auger and cone penetrometer – are used to sample soil thickness at 78 locations to calibrate the local value of unconstrained parameters within the hybrid model. Sensitivity analysis using the hybrid model reveals that the diffusion coefficient used in hillslope diffusion modeling has the largest sensitivity among all input parameters. In addition, our results from both sampling and modeling show that, in general, the northeast-facing hillslope has a deeper soil layer than the southwest-facing hillslope. By comparing the soil thickness estimated between a machine-learning approach and this hybrid model, the hybrid model provides higher accuracy and requires less sampling data. Modeling results further reveal that the southwest-facing hillslope has a slightly faster surface soil erosion rate and soil production rate than the northeast-facing hillslope, which suggests that the relatively less dense vegetation cover and drier surface soils on the southwest-facing slopes influence soil properties. With seven parameters in total for calibration, this hybrid model can provide a realistic soil thickness map with a relatively small amount of sampling dataset comparing to machine-learning approach. Integrating process-based modeling and statistical analysis not only provides a thorough understanding of the fundamental mechanisms for soil thickness prediction but also integrates the strengths of both statistical approaches and process-based modeling approaches.</p>https://esurf.copernicus.org/articles/9/1347/2021/esurf-9-1347-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Q. Yan
H. Wainwright
B. Dafflon
S. Uhlemann
C. I. Steefel
N. Falco
J. Kwang
S. S. Hubbard
spellingShingle Q. Yan
H. Wainwright
B. Dafflon
S. Uhlemann
C. I. Steefel
N. Falco
J. Kwang
S. S. Hubbard
A hybrid data–model approach to map soil thickness in mountain hillslopes
Earth Surface Dynamics
author_facet Q. Yan
H. Wainwright
B. Dafflon
S. Uhlemann
C. I. Steefel
N. Falco
J. Kwang
S. S. Hubbard
author_sort Q. Yan
title A hybrid data–model approach to map soil thickness in mountain hillslopes
title_short A hybrid data–model approach to map soil thickness in mountain hillslopes
title_full A hybrid data–model approach to map soil thickness in mountain hillslopes
title_fullStr A hybrid data–model approach to map soil thickness in mountain hillslopes
title_full_unstemmed A hybrid data–model approach to map soil thickness in mountain hillslopes
title_sort hybrid data–model approach to map soil thickness in mountain hillslopes
publisher Copernicus Publications
series Earth Surface Dynamics
issn 2196-6311
2196-632X
publishDate 2021-10-01
description <p>Soil thickness plays a central role in the interactions between vegetation, soils, and topography, where it controls the retention and release of water, carbon, nitrogen, and metals. However, mapping soil thickness, here defined as the mobile regolith layer, at high spatial resolution remains challenging. Here, we develop a hybrid model that combines a process-based model and empirical relationships to estimate the spatial heterogeneity of soil thickness with fine spatial resolution (0.5 m). We apply this model to two aspects of hillslopes (southwest- and northeast-facing, respectively) in the East River watershed in Colorado. Two independent measurement methods – auger and cone penetrometer – are used to sample soil thickness at 78 locations to calibrate the local value of unconstrained parameters within the hybrid model. Sensitivity analysis using the hybrid model reveals that the diffusion coefficient used in hillslope diffusion modeling has the largest sensitivity among all input parameters. In addition, our results from both sampling and modeling show that, in general, the northeast-facing hillslope has a deeper soil layer than the southwest-facing hillslope. By comparing the soil thickness estimated between a machine-learning approach and this hybrid model, the hybrid model provides higher accuracy and requires less sampling data. Modeling results further reveal that the southwest-facing hillslope has a slightly faster surface soil erosion rate and soil production rate than the northeast-facing hillslope, which suggests that the relatively less dense vegetation cover and drier surface soils on the southwest-facing slopes influence soil properties. With seven parameters in total for calibration, this hybrid model can provide a realistic soil thickness map with a relatively small amount of sampling dataset comparing to machine-learning approach. Integrating process-based modeling and statistical analysis not only provides a thorough understanding of the fundamental mechanisms for soil thickness prediction but also integrates the strengths of both statistical approaches and process-based modeling approaches.</p>
url https://esurf.copernicus.org/articles/9/1347/2021/esurf-9-1347-2021.pdf
work_keys_str_mv AT qyan ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT hwainwright ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT bdafflon ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT suhlemann ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT cisteefel ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT nfalco ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT jkwang ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT sshubbard ahybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT qyan hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT hwainwright hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT bdafflon hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT suhlemann hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT cisteefel hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT nfalco hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT jkwang hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
AT sshubbard hybriddatamodelapproachtomapsoilthicknessinmountainhillslopes
_version_ 1716828437216231424