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  4. Multi-scale soil salinization dynamics from global to pore scale : a review
 
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Multi-scale soil salinization dynamics from global to pore scale : a review

Citation Link: https://doi.org/10.15480/882.13413
Publikationstyp
Review Article
Date Issued
2024-12
Sprache
English
Author(s)
Shokri, Nima  
Geohydroinformatik B-9  
Hassani, Amirhossein  
Sahimi, Muhammad  
TORE-DOI
10.15480/882.13413
TORE-URI
https://hdl.handle.net/11420/49447
Journal
Reviews of geophysics  
Volume
62
Issue
4
Article Number
e2023RG000804
Citation
Reviews of Geophysics 62 (4): e2023RG000804 (2024-12)
Publisher DOI
10.1029/2023rg000804
Scopus ID
2-s2.0-85205282996
Publisher
Wiley
Soil salinization refers to the accumulation of water-soluble salts in the upper part of the soil profile. Excessive levels of soil salinity affects crop production, soil health, and ecosystem functioning. This phenomenon threatens agriculture, food security, soil stability, and fertility leading to land degradation and loss of essential soil ecosystem services that are fundamental to sustaining life. In this review, we synthesize recent advances in soil salinization at various spatial and temporal scales, ranging from global to core, pore, and molecular scales, offering new insights and presenting our perspective on potential future research directions to address key challenges and open questions related to soil salinization. Globally, we identify significant challenges in understanding soil salinity, which are (a) the considerable uncertainty in estimating the total area of salt-affected soils, (b) geographical bias in ground-based measurements of soil salinity, and (c) lack of information and data detailing secondary salinization processes, both in dry- and wetlands, particularly concerning responses to climate change. At the core scale, the impact of salt precipitation with evolving porous structure on the evaporative fluxes from porous media is not fully understood. This knowledge is crucial for accurately predicting soil water loss due to evaporation. Additionally, the effects of transport properties of porous media, such as mixed wettability conditions, on the saline water evaporation and the resulting salt precipitation patterns remain unclear. Furthermore, effective continuum equations must be developed to accurately represent experimental data and pore-scale numerical simulations.
Subjects
pore scale processes
saline water evaporation
soil health
soil salinization
DDC Class
550: Earth Sciences, Geology
Funding(s)
Projekt DEAL  
Publication version
publishedVersion
Lizenz
https://creativecommons.org/licenses/by/4.0/
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Reviews of Geophysics - 2024 - Shokri - Multi‐Scale Soil Salinization Dynamics From Global to Pore Scale A Review.pdf

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