Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands
The spatial and temporal monitoring of soil organic carbon (SOC), and other soil properties related to soil erosion, is extremely important, both from the environmental and economic perspectives. Sentinel-2 (S2) and Landsat-8 (L8) time series increase the probability to observe bare soil fields in c...
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doaj-830efbedbb6444278433e34d09a8c53e2021-09-09T13:54:59ZengMDPI AGRemote Sensing2072-42922021-08-01133345334510.3390/rs13173345Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on CroplandsFabio Castaldi0Institute of BioEconomy, National Research Council of Italy (CNR), Via Giovanni Caproni 8, 50145 Firenze, ItalyThe spatial and temporal monitoring of soil organic carbon (SOC), and other soil properties related to soil erosion, is extremely important, both from the environmental and economic perspectives. Sentinel-2 (S2) and Landsat-8 (L8) time series increase the probability to observe bare soil fields in croplands, and thus, monitor soil properties over large regions. In this regard, this work suggests an automated pixel-based approach to select only pure soil pixels in S2 and L8 time series, and to make a synthetic bare soil image (SBSI). The SBSIs and the soil properties measured in the framework of the European LUCAS survey were used to calibrate SOC, clay, and CaCO<sub>3</sub> prediction models. The results highlight a high correlation between laboratory soil spectra and the SBSIs median spectra, especially for the SBSI obtained by a three-year S2 collection, which provides satisfactory results in terms of SOC prediction accuracy (RPD: 1.74). The comparison between S2 and L8 results demonstrated the higher capability of the S2 sensor in terms of SOC prediction accuracy, mainly due to the greater spatial resolution of the bands in the visible region. Whereas, neither S2 nor L8 could accurately predict the clay and CaCO<sub>3</sub> content. This is because of the low spectral and spatial resolution of their SWIR bands that prevent the exploitation of the narrow spectral features related to these two soil attributes. The results of this study prove that large S2 time series can estimate and monitor SOC in croplands using an automated pixel-based approach that selects pure soil pixels and retrieves reliable synthetic soil spectra.https://www.mdpi.com/2072-4292/13/17/3345time seriesmulti-temporalmosaickingbare soilSOCclay |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
Fabio Castaldi |
spellingShingle |
Fabio Castaldi Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands Remote Sensing time series multi-temporal mosaicking bare soil SOC clay |
author_facet |
Fabio Castaldi |
author_sort |
Fabio Castaldi |
title |
Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands |
title_short |
Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands |
title_full |
Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands |
title_fullStr |
Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands |
title_full_unstemmed |
Sentinel-2 and Landsat-8 Multi-Temporal Series to Estimate Topsoil Properties on Croplands |
title_sort |
sentinel-2 and landsat-8 multi-temporal series to estimate topsoil properties on croplands |
publisher |
MDPI AG |
series |
Remote Sensing |
issn |
2072-4292 |
publishDate |
2021-08-01 |
description |
The spatial and temporal monitoring of soil organic carbon (SOC), and other soil properties related to soil erosion, is extremely important, both from the environmental and economic perspectives. Sentinel-2 (S2) and Landsat-8 (L8) time series increase the probability to observe bare soil fields in croplands, and thus, monitor soil properties over large regions. In this regard, this work suggests an automated pixel-based approach to select only pure soil pixels in S2 and L8 time series, and to make a synthetic bare soil image (SBSI). The SBSIs and the soil properties measured in the framework of the European LUCAS survey were used to calibrate SOC, clay, and CaCO<sub>3</sub> prediction models. The results highlight a high correlation between laboratory soil spectra and the SBSIs median spectra, especially for the SBSI obtained by a three-year S2 collection, which provides satisfactory results in terms of SOC prediction accuracy (RPD: 1.74). The comparison between S2 and L8 results demonstrated the higher capability of the S2 sensor in terms of SOC prediction accuracy, mainly due to the greater spatial resolution of the bands in the visible region. Whereas, neither S2 nor L8 could accurately predict the clay and CaCO<sub>3</sub> content. This is because of the low spectral and spatial resolution of their SWIR bands that prevent the exploitation of the narrow spectral features related to these two soil attributes. The results of this study prove that large S2 time series can estimate and monitor SOC in croplands using an automated pixel-based approach that selects pure soil pixels and retrieves reliable synthetic soil spectra. |
topic |
time series multi-temporal mosaicking bare soil SOC clay |
url |
https://www.mdpi.com/2072-4292/13/17/3345 |
work_keys_str_mv |
AT fabiocastaldi sentinel2andlandsat8multitemporalseriestoestimatetopsoilpropertiesoncroplands |
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1717759520039501824 |