Abstract

Landscape topography is a critical factor affecting soil formation and plays an important role in determining soil properties on the earth surface, as it regulates the gravity-driven soil movement induced by runoff and tillage activities. The recent application of Light Detection and Ranging (LiDAR) data holds promise for generating high spatial resolution topographic metrics that can be used to investigate soil property variability. In this study, fifteen topographic metrics derived from LiDAR data were used to investigate topographic impacts on redistribution of soil and spatial distribution of soil organic carbon (SOC). Specifically, we explored the use of topographic principal components (TPCs) for characterizing topography metrics and stepwise principal component regression (SPCR) to develop topography-based soil erosion and SOC models at site and watershed scales. Performance of SPCR models was evaluated against stepwise ordinary least square regression (SOLSR) models. Results showed that SPCR models outperformed SOLSR models in predicting soil redistribution rates and SOC density at different spatial scales. Use of TPCs removes potential collinearity between individual input variables, and dimensionality reduction by principal component analysis (PCA) diminishes the risk of overfitting the prediction models. This study proposes a new approach for modeling soil redistribution across various spatial scales. For one application, access to private lands is often limited, and the need to extrapolate findings from representative study sites to larger settings that include private lands can be important.

Highlights

  • Soil redistribution exerts significant impacts on soil organic carbon (SOC) stocks and dynamics

  • Topographic metrics and soil property information were calculated for the 230 locations

  • We found that the stepwise principal component regression (SPCR) models The coefficients of determination h(ra2)dbthyecobmesptaprrinegdiSctOioCnsdaenndsittyheprSeOdiLcStioRnr models showed the poorest performances at the watershed scale. to observation increased from: 1) 0.60 in SOLSRf and 0.52 in SOLSRr to 0.66 in SPCR, and 2) Nash-Sutcliffe efficiency (NSE) increased from 0.21 in SOLSRf and 0.16 in SOLSRr to 0.59 in SPCR; while RSR reduced from 0.87 in SOLSRf and 0.91 in SOLSRr to 0.64 in SPCR

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Summary

Introduction

Soil redistribution (erosion and deposition) exerts significant impacts on soil organic carbon (SOC) stocks and dynamics. Carbon (C) sequestration and SOC distribution are influenced by gravity-driven soil movement induced by water erosion[4,5,6]. Tillage erosion causes a considerable net downslope movement of soil particles and leads to a within-field soil variation[10]. Both water and tillage erosion are significantly affected by landscape topography, which determines the locations of erosional and depositional sites[11]. Effective soil erosion regulation and C dynamic investigation in agricultural lands calls for a better understanding of topographic controls on soil erosion and movements

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