The nomenclature for hydrogeological instability risks includes four main risks, which are distinguished according to the risk causes : 1) hydrogeological risk, that is slowly caused by natural factors (e.g. collapse landslides in a calcareous cliff in uninhabited areas and erosion along a marly-calcareous slope) in environments where human activities are minimal, i.e. woods, forests and mountain pastures; 2) hydraulic-pedological farming risk, that implies the occurrence of landslides in every winter and is caused by incorrect crop selection, not suitable for the soil and climate parameters (e.g. on a hilly slope with a clay vertisol type with a landslide having different fronts, when the arable land is cultivated with a cereal-legume crop rotation), or the presence of springs with missing drainage in clay soils with a high gradient; 3) hydraulic-infrastructural risk, that is caused by the building up of infrastructures not suitable for the surrounding environment, as they change the downflow of shallow water; 4) hydraulic-infrastructural-pedological-management risk, that is caused by crop operations not suitable for soil and crop parameters, where the selected cultivated plant species are suitable for the environment and field improvements change water downflow (e.g. in soils along hilly calcarenite slopes cultivated with olive orchards, where up-down soil tillage causes shallow water erosion).

Salvatore Raimondi, Antonio Comparetti, Carlo Greco, Davide Puccio (2022). Nomenclature for Hydrogeological Instability Risks. In Encyclopedia E, topic review, Subjects "Area Studies", Entry Collection "Environmental Sciences" (pp. 1-10). MDPI (Multidisciplinary Digital Publishing Institute).

Nomenclature for Hydrogeological Instability Risks

Salvatore Raimondi;Antonio Comparetti
;
Carlo Greco;
2022-01-25

Abstract

The nomenclature for hydrogeological instability risks includes four main risks, which are distinguished according to the risk causes : 1) hydrogeological risk, that is slowly caused by natural factors (e.g. collapse landslides in a calcareous cliff in uninhabited areas and erosion along a marly-calcareous slope) in environments where human activities are minimal, i.e. woods, forests and mountain pastures; 2) hydraulic-pedological farming risk, that implies the occurrence of landslides in every winter and is caused by incorrect crop selection, not suitable for the soil and climate parameters (e.g. on a hilly slope with a clay vertisol type with a landslide having different fronts, when the arable land is cultivated with a cereal-legume crop rotation), or the presence of springs with missing drainage in clay soils with a high gradient; 3) hydraulic-infrastructural risk, that is caused by the building up of infrastructures not suitable for the surrounding environment, as they change the downflow of shallow water; 4) hydraulic-infrastructural-pedological-management risk, that is caused by crop operations not suitable for soil and crop parameters, where the selected cultivated plant species are suitable for the environment and field improvements change water downflow (e.g. in soils along hilly calcarenite slopes cultivated with olive orchards, where up-down soil tillage causes shallow water erosion).
25-gen-2022
soil management, sustainable development, environmental sustainability, Soil Cadastre, best practices, agricultural mechanisation
Salvatore Raimondi, Antonio Comparetti, Carlo Greco, Davide Puccio (2022). Nomenclature for Hydrogeological Instability Risks. In Encyclopedia E, topic review, Subjects "Area Studies", Entry Collection "Environmental Sciences" (pp. 1-10). MDPI (Multidisciplinary Digital Publishing Institute).
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/10447/532456
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