Assessing Soil Degradation in Agricultural Landscapes of Semi‐Arid Tropics Using Proximal and Remote Sensing‐Based Diffuse Reflectance Spectroscopy

ABSTRACT Monitoring soil degradation using the soil degradation index (SDI) is a complex process. Typically, multiple soil parameters are measured under laboratory conditions to create such a composite parameter. Because conventional soil testing methods are tedious and time‐consuming, frequent monitoring of soil degradation through SDI continues to be a challenging task. With diffuse reflectance spectroscopy (DRS) emerging as a rapid soil testing method, the major objective of this study is to examine the DRS approach for estimating SDIs in a degradation‐prone dryland landscape of Maharashtra, India. Accordingly, surface soil samples were collected from 141 locations and 20 different soil parameters were measured in these samples. Six key parameters were identified to formulate the SDI following a minimum dataset (MDS) approach: soil organic carbon content (SOC), soil erodibility index (eMCR), available S, available Mn, the ratio between exchangeable Ca to Mg and silt content. Spectral reflectance data collected under laboratory conditions and those extracted from multispectral imaging data from Sentinel‐2 L2A over the visible to infrared (VNIR) region were used to estimate SDIs and its six indicators by calibrating two popular chemometric models: support vector regression (SVR) and feature selection‐based partial‐least‐squares regression (PLSR FS ). Results showed that the SDI values could be estimated from the laboratory‐measured DRS data with the coefficient of determination ( R 2 ) value of 0.81 and root‐mean‐squared error (RMSE) value of 0.03. Similarly, chemometric models also performed well for the MSI data ( R 2 = 0.52; RMSE = 0.04). Although the laboratory‐based DRS approach provided greater estimation accuracy, low RMSE values associated with the MSI data showed that SDI may be effectively mapped for the entire study area at high spatial resolution (~10 m for Sentinel‐2 L2A data). Correlation analyses between mapped SDI and crop yield further showed yield declines with increasing soil degradation for different rainfed crops, while no such trends were observed for the irrigated crops, suggesting that irrigation management in dryland areas may circumvent land degradation challenges.

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Journal
Soil Use and Management
Published
2025-04-01
DOI
https://doi.org/10.1111/sum.70101
Primary Topic
Soil Geostatistics and Mapping
Type
article
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article

Assessing Soil Degradation in Agricultural Landscapes of Semi‐Arid Tropics Using Proximal and Remote Sensing‐Based Diffuse Reflectance Spectroscopy

Nagaraju Budama, Sourav Roy, Bhabani S. Das, Nagarjuna N. Reddy et al.
Soil Use and Management
Soil Geostatistics and Mapping
article

Assessing Soil Degradation in Agricultural Landscapes of Semi‐Arid Tropics Using Proximal and Remote Sensing‐Based Diffuse Reflectance Spectroscopy

Nagaraju Budama, Sourav Roy, Bhabani S. Das, Nagarjuna N. Reddy, M.L. Jat, A. Venkataradha, Kaushal K. Garg, Israr Majeed, P. Niranjan, Ramesh Singh, K. H. Anantha
article en

Abstract

ABSTRACT Monitoring soil degradation using the soil degradation index (SDI) is a complex process. Typically, multiple soil parameters are measured under laboratory conditions to create such a composite parameter. Because conventional soil testing methods are tedious and time‐consuming, frequent monitoring of soil degradation through SDI continues to be a challenging task. With diffuse reflectance spectroscopy (DRS) emerging as a rapid soil testing method, the major objective of this study is to examine the DRS approach for estimating SDIs in a degradation‐prone dryland landscape of Maharashtra, India. Accordingly, surface soil samples were collected from 141 locations and 20 different soil parameters were measured in these samples. Six key parameters were identified to formulate the SDI following a minimum dataset (MDS) approach: soil organic carbon content (SOC), soil erodibility index (eMCR), available S, available Mn, the ratio between exchangeable Ca to Mg and silt content. Spectral reflectance data collected under laboratory conditions and those extracted from multispectral imaging data from Sentinel‐2 L2A over the visible to infrared (VNIR) region were used to estimate SDIs and its six indicators by calibrating two popular chemometric models: support vector regression (SVR) and feature selection‐based partial‐least‐squares regression (PLSR FS ). Results showed that the SDI values could be estimated from the laboratory‐measured DRS data with the coefficient of determination ( R 2 ) value of 0.81 and root‐mean‐squared error (RMSE) value of 0.03. Similarly, chemometric models also performed well for the MSI data ( R 2 = 0.52; RMSE = 0.04). Although the laboratory‐based DRS approach provided greater estimation accuracy, low RMSE values associated with the MSI data showed that SDI may be effectively mapped for the entire study area at high spatial resolution (~10 m for Sentinel‐2 L2A data). Correlation analyses between mapped SDI and crop yield further showed yield declines with increasing soil degradation for different rainfed crops, while no such trends were observed for the irrigated crops, suggesting that irrigation management in dryland areas may circumvent land degradation challenges.

Soil Use and ManagementVol. 41(2)
Indian Institute of Technology Kharagpur (IN), Indian Council of Agricultural Research (IN), International Crops Research Institute for the Semi-Arid Tropics (IN)
Openalex Percentile: Top 88%
Soil Geostatistics and Mapping
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