The downward spiral entangling soil sealing and hydrogeological disasters

The frequency of occurrence of hydrogeological disasters (HGDs), as well as the persistence of their impacts, are not evenly distributed. Hazardous areas, by definition, are more prone to extreme events, while in densely urbanized regions, the impacts of these events tend to be more severe. The obje...

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Published in:Environmental Research Letters
Main Authors: Alessio Gatto, Federico Martellozzo, Stefano Clo’, Lorenzo Ciulla, Samuele Segoni
Format: Article
Language:English
Published: IOP Publishing 2024-01-01
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ad5fa1
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author Alessio Gatto
Federico Martellozzo
Stefano Clo’
Lorenzo Ciulla
Samuele Segoni
author_facet Alessio Gatto
Federico Martellozzo
Stefano Clo’
Lorenzo Ciulla
Samuele Segoni
author_sort Alessio Gatto
collection DOAJ
container_title Environmental Research Letters
description The frequency of occurrence of hydrogeological disasters (HGDs), as well as the persistence of their impacts, are not evenly distributed. Hazardous areas, by definition, are more prone to extreme events, while in densely urbanized regions, the impacts of these events tend to be more severe. The objective of this study is to investigate statistical relationships between urban and natural environment features and HGD occurrences. Taking Italian provinces as a comprehensive case study, we assessed the coefficient of determination, the χ ^2 test, and the p -value to determine the degree of statistical correlation between impact indicators and 57 hazard/risk/land management indicators, such as extension of at-risk areas or soil sealing. We discovered that HGDs persistence and frequency correlate best with an indicator describing the amount of soil sealing (i.e. urbanized soil) in medium-hazard areas. Building on that, a further dynamic analysis was carried out to investigate whether soil sealing trends changed significantly after the provinces were struck by HGDs. Our findings hold significant implications, challenging current policy norms. European directives and Italian national laws impose strict development restrictions in ‘high-hazard’ areas, but generally allow for urbanization in ‘medium-hazard’ areas, with only minor limitations. Moreover, a paradoxical positive urbanization trend is observed in the most sensitive areas, greater than in safer areas and generally unchanged after HGDs. This outcome highlights a critical gap in risk perception that reflects into territorial planning, decision-making processes, and existing policies.
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spelling doaj-art-4d03b82a3d044e9db9fce67c613b2fdf2025-08-20T00:37:47ZengIOP PublishingEnvironmental Research Letters1748-93262024-01-0119808402310.1088/1748-9326/ad5fa1The downward spiral entangling soil sealing and hydrogeological disastersAlessio Gatto0https://orcid.org/0000-0001-6635-6171Federico Martellozzo1https://orcid.org/0000-0002-3142-2543Stefano Clo’2https://orcid.org/0000-0003-2901-7458Lorenzo Ciulla3Samuele Segoni4https://orcid.org/0000-0002-6030-1046Department of Earth Sciences, Università degli Studi di Firenze , Firenze, ItalyDepartment of Economics and Business Sciences, Università degli Studi di Firenze , Firenze, ItalyDepartment of Economics and Business Sciences, Università degli Studi di Firenze , Firenze, ItalyDepartment of Economics and Business Sciences, Università degli Studi di Firenze , Firenze, ItalyDepartment of Earth Sciences, Università degli Studi di Firenze , Firenze, ItalyThe frequency of occurrence of hydrogeological disasters (HGDs), as well as the persistence of their impacts, are not evenly distributed. Hazardous areas, by definition, are more prone to extreme events, while in densely urbanized regions, the impacts of these events tend to be more severe. The objective of this study is to investigate statistical relationships between urban and natural environment features and HGD occurrences. Taking Italian provinces as a comprehensive case study, we assessed the coefficient of determination, the χ ^2 test, and the p -value to determine the degree of statistical correlation between impact indicators and 57 hazard/risk/land management indicators, such as extension of at-risk areas or soil sealing. We discovered that HGDs persistence and frequency correlate best with an indicator describing the amount of soil sealing (i.e. urbanized soil) in medium-hazard areas. Building on that, a further dynamic analysis was carried out to investigate whether soil sealing trends changed significantly after the provinces were struck by HGDs. Our findings hold significant implications, challenging current policy norms. European directives and Italian national laws impose strict development restrictions in ‘high-hazard’ areas, but generally allow for urbanization in ‘medium-hazard’ areas, with only minor limitations. Moreover, a paradoxical positive urbanization trend is observed in the most sensitive areas, greater than in safer areas and generally unchanged after HGDs. This outcome highlights a critical gap in risk perception that reflects into territorial planning, decision-making processes, and existing policies.https://doi.org/10.1088/1748-9326/ad5fa1soil sealingurbanizationpoliciesnatural disasterslandslideflood
spellingShingle Alessio Gatto
Federico Martellozzo
Stefano Clo’
Lorenzo Ciulla
Samuele Segoni
The downward spiral entangling soil sealing and hydrogeological disasters
soil sealing
urbanization
policies
natural disasters
landslide
flood
title The downward spiral entangling soil sealing and hydrogeological disasters
title_full The downward spiral entangling soil sealing and hydrogeological disasters
title_fullStr The downward spiral entangling soil sealing and hydrogeological disasters
title_full_unstemmed The downward spiral entangling soil sealing and hydrogeological disasters
title_short The downward spiral entangling soil sealing and hydrogeological disasters
title_sort downward spiral entangling soil sealing and hydrogeological disasters
topic soil sealing
urbanization
policies
natural disasters
landslide
flood
url https://doi.org/10.1088/1748-9326/ad5fa1
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