Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed

This study aimed to assess the ability of using visible and near-infrared reflectance (Vis–NIR) spectroscopy to quantify soil erodibility factor (<i>K</i>) rapidly in an ecologically restored watershed. To achieve this goal, we explored the performance and transferability of the develope...

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Main Authors: Qinghu Jiang, Yiyun Chen, Jialiang Hu, Feng Liu
Format: Article
Language:English
Published: MDPI AG 2020-09-01
Series:Remote Sensing
Subjects:
Online Access:https://www.mdpi.com/2072-4292/12/18/3103
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spelling doaj-f82f7bbd213c4419ac0a65764f06e56d2020-11-25T03:40:10ZengMDPI AGRemote Sensing2072-42922020-09-01123103310310.3390/rs12183103Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored WatershedQinghu Jiang0Yiyun Chen1Jialiang Hu2Feng Liu3Key Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, ChinaSchool of Resource and Environmental Science, Wuhan University, No.129 Luoyu Road, Wuhan 430079, ChinaChina Railway Fifth Survey and Design Institute Group Co., Ltd., Beijing 102600, ChinaKey Laboratory of Aquatic Botany and Watershed Ecology, Wuhan Botanical Garden, Chinese Academy of Sciences, Wuhan 430074, ChinaThis study aimed to assess the ability of using visible and near-infrared reflectance (Vis–NIR) spectroscopy to quantify soil erodibility factor (<i>K</i>) rapidly in an ecologically restored watershed. To achieve this goal, we explored the performance and transferability of the developed spectral models in multiple land-use types: woodland, shrubland, terrace, and slope farmland (the first two types are natural land and the latter two are cultivated land). Subsequently, we developed an improved approach by combining spectral data with related topographic variables (i.e., elevation, watershed location, slope height, and normalized height) to estimate <i>K</i>. The results indicate that the calibrated spectral model using total samples could estimate <i>K</i> factor effectively (<i>R</i><sup>2</sup><sub>CV</sub><i> </i>= 0.71, <i>RMSE</i><sub>CV</sub> = 0.0030 Mg h Mj<sup>−1</sup> mm<sup>−1</sup>, and <i>RPD</i><sub>CV</sub> = 1.84). When predicting <i>K</i> in the new samples, models performed well in natural land soils (<i>R</i><sup>2</sup><sub>P</sub> = 0.74, <i>RPD</i><sub>P</sub> = 1.93) but failed in cultivated land soils (<i>R</i><sup>2</sup><sub>P</sub> = 0.24, <i>RPD</i><sub>P</sub> = 0.99). Furthermore, the developed models showed low transferability between the natural and cultivated land datasets. The results also indicate that the combination of spectral data with topographic variables could slightly increase the accuracies of <i>K</i> estimation in total and natural land datasets but did not work for cultivated land samples. This study demonstrated that the Vis–NIR spectroscopy could be used as an effective method in predicting <i>K</i>. However, the predictability and transferability of the calibrated models were land-use type dependent. Our study also revealed that the coupling of spectrum and environmental variable is an effective improvement of <i>K</i> estimation in natural landscape region.https://www.mdpi.com/2072-4292/12/18/3103soil erodibilityvisible and near-infrared reflectance spectroscopymodel transferabilitymodel improvementwatershed landscapes
collection DOAJ
language English
format Article
sources DOAJ
author Qinghu Jiang
Yiyun Chen
Jialiang Hu
Feng Liu
spellingShingle Qinghu Jiang
Yiyun Chen
Jialiang Hu
Feng Liu
Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed
Remote Sensing
soil erodibility
visible and near-infrared reflectance spectroscopy
model transferability
model improvement
watershed landscapes
author_facet Qinghu Jiang
Yiyun Chen
Jialiang Hu
Feng Liu
author_sort Qinghu Jiang
title Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed
title_short Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed
title_full Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed
title_fullStr Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed
title_full_unstemmed Use of Visible and Near-Infrared Reflectance Spectroscopy Models to Determine Soil Erodibility Factor (<i>K</i>) in an Ecologically Restored Watershed
title_sort use of visible and near-infrared reflectance spectroscopy models to determine soil erodibility factor (<i>k</i>) in an ecologically restored watershed
publisher MDPI AG
series Remote Sensing
issn 2072-4292
publishDate 2020-09-01
description This study aimed to assess the ability of using visible and near-infrared reflectance (Vis–NIR) spectroscopy to quantify soil erodibility factor (<i>K</i>) rapidly in an ecologically restored watershed. To achieve this goal, we explored the performance and transferability of the developed spectral models in multiple land-use types: woodland, shrubland, terrace, and slope farmland (the first two types are natural land and the latter two are cultivated land). Subsequently, we developed an improved approach by combining spectral data with related topographic variables (i.e., elevation, watershed location, slope height, and normalized height) to estimate <i>K</i>. The results indicate that the calibrated spectral model using total samples could estimate <i>K</i> factor effectively (<i>R</i><sup>2</sup><sub>CV</sub><i> </i>= 0.71, <i>RMSE</i><sub>CV</sub> = 0.0030 Mg h Mj<sup>−1</sup> mm<sup>−1</sup>, and <i>RPD</i><sub>CV</sub> = 1.84). When predicting <i>K</i> in the new samples, models performed well in natural land soils (<i>R</i><sup>2</sup><sub>P</sub> = 0.74, <i>RPD</i><sub>P</sub> = 1.93) but failed in cultivated land soils (<i>R</i><sup>2</sup><sub>P</sub> = 0.24, <i>RPD</i><sub>P</sub> = 0.99). Furthermore, the developed models showed low transferability between the natural and cultivated land datasets. The results also indicate that the combination of spectral data with topographic variables could slightly increase the accuracies of <i>K</i> estimation in total and natural land datasets but did not work for cultivated land samples. This study demonstrated that the Vis–NIR spectroscopy could be used as an effective method in predicting <i>K</i>. However, the predictability and transferability of the calibrated models were land-use type dependent. Our study also revealed that the coupling of spectrum and environmental variable is an effective improvement of <i>K</i> estimation in natural landscape region.
topic soil erodibility
visible and near-infrared reflectance spectroscopy
model transferability
model improvement
watershed landscapes
url https://www.mdpi.com/2072-4292/12/18/3103
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