FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2249941408> ?p ?o ?g. }

• W2249941408 endingPage "121" @default.
• W2249941408 startingPage "114" @default.
• W2249941408 abstract "Abstract Soil degradation by processes such as soil erosion, shallow landslides, debris-flows etc. is a significant problem in mountain areas, and is a crucial issue for natural hazard assessment in mountain areas. Several soil properties, among which are the liquid and plastic limits, i.e. moisture contents for which a soil passes from the plastic to liquid state (liquid limit, LL) and from the semisolid to plastic state (PL, plastic limit), have been proposed as indicators for soil vulnerability to degradation processes, both of natural and anthropogenic origin. In this research we investigated the liquid and plastic limits of the main soil groups of World Reference Base for Soil Resources (WRB) classification present in Aosta Valley (N–W Italian Alps) from a pedogenic perspective. In particular, we compared 1) soils at different stages of development; and 2) different genetic horizons. Our main aim was to provide and interpret data on soils' consistency and mechanical behavior that may be used as indexes for the assessment of soil vulnerability. Despite its relatively small area, the Aosta Valley is characterized by a wide range of soil types. Sixty-two soils with different profile evolution stages, representative of 7 WRB soil groups, were investigated and LL and PL in genetic horizons were studied at the soil type and genetic horizons level. In general, soil consistency was largely determined by the organic matter content (both in topsoils and organic matter-enriched subsurface horizons), but in spodic horizons and some C horizons a role of poorly crystalline and pedogenic iron oxides was observed too. Considering the vulnerability to consistency loss, that can result in erosion processes and overall soil degradation, surface horizons were generally less vulnerable, as could be expected on the basis of previous research, i.e. showed higher LL and PL values, than the deeper ones, generally characterized by a reduction of soil consistency. Therefore, topsoil could receive higher water inputs while still preserving their consistency and strength. This was not confirmed in Podzols, where the organic matter enrichment of spodic horizons determined a discontinuity in physical properties between the E horizons (more vulnerable) and the underlying, spodic ones. The same trend was observed for Calcisols with a deep cemented Bkm horizon. The research provided a novel overview on LL and PL in the common soil types present in the Alpine region, integrating the already existing research on topsoil vulnerability to degradation processes (erosion, consistency losses, losses of strength), and the regional soil database. The use of LL and PL as indicators of soil physical quality was approached with a pedogenic perspective, which might be helpful for a better definition of hazard assessment at the regional scale." @default.
• W2249941408 created "2016-06-24" @default.
• W2249941408 creator A5000932879 @default.
• W2249941408 creator A5013676868 @default.
• W2249941408 creator A5040953050 @default.
• W2249941408 creator A5051778738 @default.
• W2249941408 date "2015-12-01" @default.
• W2249941408 modified "2023-09-26" @default.
• W2249941408 title "Liquid and plastic limits of mountain soils as a function of the soil and horizon type" @default.
• W2249941408 cites W1974948747 @default.
• W2249941408 cites W1975654131 @default.
• W2249941408 cites W1979295289 @default.
• W2249941408 cites W1982507535 @default.
• W2249941408 cites W1992195814 @default.
• W2249941408 cites W1994951306 @default.
• W2249941408 cites W1995823735 @default.
• W2249941408 cites W2002173304 @default.
• W2249941408 cites W2019602586 @default.
• W2249941408 cites W2034956097 @default.
• W2249941408 cites W2049517593 @default.
• W2249941408 cites W2053282958 @default.
• W2249941408 cites W2060983129 @default.
• W2249941408 cites W2067550468 @default.
• W2249941408 cites W2068681816 @default.
• W2249941408 cites W2078685747 @default.
• W2249941408 cites W2079288125 @default.
• W2249941408 cites W2092492673 @default.
• W2249941408 cites W2106687660 @default.
• W2249941408 cites W2106823745 @default.
• W2249941408 cites W2125830490 @default.
• W2249941408 cites W2127529521 @default.
• W2249941408 cites W2156388478 @default.
• W2249941408 doi "https://doi.org/10.1016/j.catena.2015.07.021" @default.
• W2249941408 hasPublicationYear "2015" @default.
• W2249941408 type Work @default.
• W2249941408 sameAs 2249941408 @default.
• W2249941408 citedByCount "20" @default.
• W2249941408 countsByYear W22499414082017 @default.
• W2249941408 countsByYear W22499414082018 @default.
• W2249941408 countsByYear W22499414082019 @default.
• W2249941408 countsByYear W22499414082020 @default.
• W2249941408 countsByYear W22499414082021 @default.
• W2249941408 countsByYear W22499414082022 @default.
• W2249941408 countsByYear W22499414082023 @default.
• W2249941408 crossrefType "journal-article" @default.
• W2249941408 hasAuthorship W2249941408A5000932879 @default.
• W2249941408 hasAuthorship W2249941408A5013676868 @default.
• W2249941408 hasAuthorship W2249941408A5040953050 @default.
• W2249941408 hasAuthorship W2249941408A5051778738 @default.
• W2249941408 hasBestOaLocation W22499414082 @default.
• W2249941408 hasConcept C116973930 @default.
• W2249941408 hasConcept C127313418 @default.
• W2249941408 hasConcept C14036430 @default.
• W2249941408 hasConcept C159176650 @default.
• W2249941408 hasConcept C159390177 @default.
• W2249941408 hasConcept C159750122 @default.
• W2249941408 hasConcept C160934017 @default.
• W2249941408 hasConcept C187320778 @default.
• W2249941408 hasConcept C1965285 @default.
• W2249941408 hasConcept C2524010 @default.
• W2249941408 hasConcept C33923547 @default.
• W2249941408 hasConcept C39432304 @default.
• W2249941408 hasConcept C76886044 @default.
• W2249941408 hasConcept C78458016 @default.
• W2249941408 hasConcept C86803240 @default.
• W2249941408 hasConceptScore W2249941408C116973930 @default.
• W2249941408 hasConceptScore W2249941408C127313418 @default.
• W2249941408 hasConceptScore W2249941408C14036430 @default.
• W2249941408 hasConceptScore W2249941408C159176650 @default.
• W2249941408 hasConceptScore W2249941408C159390177 @default.
• W2249941408 hasConceptScore W2249941408C159750122 @default.
• W2249941408 hasConceptScore W2249941408C160934017 @default.
• W2249941408 hasConceptScore W2249941408C187320778 @default.
• W2249941408 hasConceptScore W2249941408C1965285 @default.
• W2249941408 hasConceptScore W2249941408C2524010 @default.
• W2249941408 hasConceptScore W2249941408C33923547 @default.
• W2249941408 hasConceptScore W2249941408C39432304 @default.
• W2249941408 hasConceptScore W2249941408C76886044 @default.
• W2249941408 hasConceptScore W2249941408C78458016 @default.
• W2249941408 hasConceptScore W2249941408C86803240 @default.
• W2249941408 hasLocation W22499414081 @default.
• W2249941408 hasLocation W22499414082 @default.
• W2249941408 hasOpenAccess W2249941408 @default.
• W2249941408 hasPrimaryLocation W22499414081 @default.
• W2249941408 hasRelatedWork W2031900686 @default.
• W2249941408 hasRelatedWork W2040084316 @default.
• W2249941408 hasRelatedWork W2092492673 @default.
• W2249941408 hasRelatedWork W2249941408 @default.
• W2249941408 hasRelatedWork W2355014288 @default.
• W2249941408 hasRelatedWork W2365297795 @default.
• W2249941408 hasRelatedWork W2790785622 @default.
• W2249941408 hasRelatedWork W2980470657 @default.
• W2249941408 hasRelatedWork W3036482061 @default.
• W2249941408 hasRelatedWork W3045510106 @default.
• W2249941408 hasVolume "135" @default.
• W2249941408 isParatext "false" @default.
• W2249941408 isRetracted "false" @default.
• W2249941408 magId "2249941408" @default.

• next