Please use this identifier to cite or link to this item: https://doi.org/10.15480/882.3258
Publisher DOI: 10.1073/pnas.2013771117
Title: Predicting long-term dynamics of soil salinity and sodicity on a global scale
Language: English
Authors: Hassani, Amirhossein 
Azapagic, Adisa 
Shokri, Nima 
Keywords: global scale modeling; machine learning; soil salinity; soil salinization; soil sodicity
Issue Date: 14-Dec-2020
Source: Proceedings of the National Academy of Sciences of the United States of America 52 (117): 33017-33027 (2020-12-29)
Abstract (english): 
Knowledge of spatiotemporal distribution and likelihood of (re)occurrence of salt-affected soils is crucial to our understanding of land degradation and for planning effective remediation strategies in face of future climatic uncertainties. However, conventional methods used for tracking the variability of soil salinity/sodicity are extensively localized, making predictions on a global scale difficult. Here, we employ machine-learning techniques and a comprehensive set of climatic, topographic, soil, and remote sensing data to develop models capable of making predictions of soil salinity (expressed as electrical conductivity of saturated soil extract) and sodicity (measured as soil exchangeable sodium percentage) at different longitudes, latitudes, soil depths, and time periods. Using these predictive models, we provide a global-scale quantitative and gridded dataset characterizing different spatiotemporal facets of soil salinity and sodicity variability over the past four decades at a ∼1-km resolution. Analysis of this dataset reveals that a soil area of 11.73 Mkm2 located in nonfrigid zones has been salt-affected with a frequency of reoccurrence in at least three-fourths of the years between 1980 and 2018, with 0.16 Mkm2 of this area being croplands. Although the net changes in soil salinity/sodicity and the total area of salt-affected soils have been geographically highly variable, the continents with the highest salt-affected areas are Asia (particularly China, Kazakhstan, and Iran), Africa, and Australia. The proposed method can also be applied for quantifying the spatiotemporal variability of other dynamic soil properties, such as soil nutrients, organic carbon content, and pH.
URI: http://hdl.handle.net/11420/8481
DOI: 10.15480/882.3258
ISSN: 0027-8424
Journal: Proceedings of the National Academy of Sciences of the United States of America 
Institute: Geohydroinformatik B-9 
Document Type: Article
More Funding information: This study was funded by the UK Research Councils (grant no. EP/K011820/1), the Institute of Geo-Hydroinformatics at Hamburg University of Technology, and the Presidential Doctoral Scholarship Award at The University of Manchester.
License: CC BY 4.0 (Attribution) CC BY 4.0 (Attribution)
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