Soil health assessments increasingly rely on indicators to infer soil functions and ecosystem services; however, the extent to which these indicators accurately represent water-related soil processes remains uncertain. This study investigates the relationships between soil properties and provision of water regulation ecosystem services across three contrasting pedo-climatic regions in Austria, Italy, and Tunisia. Using 315 soil profiles, we applied a process-based soil–water model to quantify infiltration, runoff triggering, groundwater recharge, and crop water stress index under representative climatic conditions. We evaluated commonly used soil indicators, including saturated hydraulic conductivity, available water content, bulk density, organic matter content, clay content, saturated soil water content, soil depth, and macroporosity. Pairwise correlation and multiple linear regression analyses were employed to assess interactions between soil properties and soil water balance components. Results show that indicator–process relationships vary considerably across sites and are often non-linear, with specific correlations reflecting local combinations of soil texture, structure, profile development, and climate. For example, in the Marchfeld region (Austria), infiltration exhibited a strong positive correlation with bulk density (, ), while the crop water stress index showed a significant negative correlation with soil depth ( 0.35, ). In the Bologna area (Italy), the study also indicated that groundwater recharge was positively correlated with soil macro-porosity (, ), whereas macro-porosity exhibited a strong negative correlation with flux-to …

Soil indicators for ecosystem services: a focus on water regulation

Yosef B. A.;Basile A.;Ungaro F.;Bancheri M.
2026

Abstract

Soil health assessments increasingly rely on indicators to infer soil functions and ecosystem services; however, the extent to which these indicators accurately represent water-related soil processes remains uncertain. This study investigates the relationships between soil properties and provision of water regulation ecosystem services across three contrasting pedo-climatic regions in Austria, Italy, and Tunisia. Using 315 soil profiles, we applied a process-based soil–water model to quantify infiltration, runoff triggering, groundwater recharge, and crop water stress index under representative climatic conditions. We evaluated commonly used soil indicators, including saturated hydraulic conductivity, available water content, bulk density, organic matter content, clay content, saturated soil water content, soil depth, and macroporosity. Pairwise correlation and multiple linear regression analyses were employed to assess interactions between soil properties and soil water balance components. Results show that indicator–process relationships vary considerably across sites and are often non-linear, with specific correlations reflecting local combinations of soil texture, structure, profile development, and climate. For example, in the Marchfeld region (Austria), infiltration exhibited a strong positive correlation with bulk density (, ), while the crop water stress index showed a significant negative correlation with soil depth ( 0.35, ). In the Bologna area (Italy), the study also indicated that groundwater recharge was positively correlated with soil macro-porosity (, ), whereas macro-porosity exhibited a strong negative correlation with flux-to …
2026
Istituto per i Sistemi Agricoli e Forestali del Mediterraneo - ISAFOM
Istituto per la BioEconomia - IBE
modelling, hydraulic properties, runoff, groundwater recharge, ecosystem services, soil health
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/583030
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