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Evolution of Soil Porosity in Loess-Palaeosol Sequences of the Ebro Valley, NE Iberia

Carlos A. Torres-Guerrero,Daniela Álvarez Morales,Frank Preusser,José Ramón Olarieta,Rosa M. Poch

SSRN Electronic Journal（2023）

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Abstract
•The microstructure of Loess of the Ebro Valley is manly affected by two processes: compaction by freeze–thaw or weight load and the bioturbation.•The bioturbation structures are presents during the most stable periods.•Carbonates and gypsum act as cementing agents, providing stability in the Loess structure.
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Key words
soil porosity,ebro valley,loess-palaeosol
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