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  4. Negative correlation between soil salinity and soil organic carbon variability
 
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Negative correlation between soil salinity and soil organic carbon variability

Citation Link: https://doi.org/10.15480/882.9571
Publikationstyp
Journal Article
Date Issued
2024-04-30
Sprache
English
Author(s)
Hassani, Amirhossein  
Smith, Pete  
University of Aberdeen, Aberdeen, United Kingdom
Shokri, Nima  
Geohydroinformatik B-9  
TORE-DOI
10.15480/882.9571
TORE-URI
https://hdl.handle.net/11420/47457
Journal
Proceedings of the National Academy of Sciences of the United States of America  
Volume
121
Issue
18
Citation
Proceedings of the National Academy of Sciences of the United States of America 121 (18): e2317332121 (2024)
Publisher DOI
10.1073/pnas.2317332121
Scopus ID
2-s2.0-85191640138
Publisher
PNAS
Soil organic carbon (SOC) is vital for terrestrial ecosystems, affecting biogeochemical processes, and soil health. It is known that soil salinity impacts SOC content, yet the specific direction and magnitude of SOC variability in relation to soil salinity remain poorly understood. Analyzing 43,459 mineral soil samples (SOC < 150 g kg-1) collected across different land covers since 1992, we approximate a soil salinity increase from 1 to 5 dS m-1 in croplands would be associated with a decline in mineral soils SOC from 0.14 g kg-1 above the mean predicted SOC ([Formula: see text] = 18.47 g kg-1) to 0.46 g kg-1 below [Formula: see text] (~-430%), while for noncroplands, such decline is sharper, from 0.96 above [Formula: see text] = 35.96 g kg-1 to 4.99 below [Formula: see text] (~-620%). Although salinity's significance in explaining SOC variability is minor (<6%), we estimate a one SD increase in salinity of topsoil samples (0 to 7 cm) correlates with respective [Formula: see text] declines of ~4.4% and ~9.26%, relative to [Formula: see text] and [Formula: see text]. The [Formula: see text] decline in croplands is greatest in vegetation/cropland mosaics while lands covered with evergreen needle-leaved trees are estimated with the highest [Formula: see text] decline in noncroplands. We identify soil nitrogen, land cover, and precipitation Seasonality Index as the most significant parameters in explaining the SOC's variability. The findings provide insights into SOC dynamics under increased soil salinity, improving understanding of SOC stock responses to land degradation and climate warming.
Subjects
biogeochemistry
carbon cycle
environmental impact
soil organic carbon
soil salinity
DDC Class
630: Agriculture and Related Technologies
570: Life Sciences, Biology
550: Earth Sciences, Geology
Publication version
publishedVersion
Lizenz
https://creativecommons.org/licenses/by/4.0/
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hassani-et-al-2024-negative-correlation-between-soil-salinity-and-soil-organic-carbon-variability.pdf

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