FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4386701604> ?p ?o ?g. }

• W4386701604 endingPage "108910" @default.
• W4386701604 startingPage "108910" @default.
• W4386701604 abstract "Slopes with clay-rich, deeply weathered soils, such as those present in the Flysch Zone of Lower Austria, are prone to landslide processes. Even though generally being of low magnitude and velocity, they can cause substantial economic losses and threaten settlements as well as infrastructure. Previous studies have demonstrated the importance of sub-surface information to further increase our understanding on landslide processes and triggers in different areas as well as to support any decision makers to determine any appropriate landslide mitigation measures. The combination of direct and indirect methods thereby has proven to be an adequate methodology, yet case studies are still needed to develop a universal strategy for the investigation of clay-rich landslides. In this study, we applied Electrical Resistivity Tomography (ERT) and Dynamic Probing Medium (DPM) to further investigate the complex Hofermühle landslide in the Flysch Zone of Lower Austria in order to improve our knowledge on sub-surface conditions. The focus is on the initially activated main landslide area, which has already formed earth-flow-like processes in the past. The methodology facilitated a representative characterization of the sub-surface. We were able to approximate the geometry and depth of slip surfaces, as well as the transition to bedrock, allowing us to delimit those parts of the slope which are likely to fail and, respectively be re-activated in the future. The results show that a range of thicknesses can be found in the investigated part of the Hofermühle landslide. In particular, near the surface, which has been altered by creep displacement and also by anthropogenic alteration, the resistivity is more variable compared to deeper, presumably less disturbed, layers. Furthermore, it is assumed that clay particles are transported with the surface runoff and deposited in the surroundings of the drainage channels, resulting in lower resistivity values and higher saturation at this locations. The location of the slip surface is interpreted to be on the surface of the bedrock, where there is a highly disturbed, clay-rich mass with no interbedded layers. Layers with lower resistivity directly above the bedrock indicate weathered material and remolding of materials during creep." @default.
• W4386701604 created "2023-09-14" @default.
• W4386701604 creator A5020198886 @default.
• W4386701604 creator A5033503685 @default.
• W4386701604 creator A5053356806 @default.
• W4386701604 creator A5092860876 @default.
• W4386701604 date "2023-11-01" @default.
• W4386701604 modified "2023-09-28" @default.
• W4386701604 title "Internal structure of an active landslide based on ERT and DP data: New insights from the Hofermühle landslide observatory in Lower Austria" @default.
• W4386701604 cites W135871549 @default.
• W4386701604 cites W184755470 @default.
• W4386701604 cites W1948971016 @default.
• W4386701604 cites W1967387860 @default.
• W4386701604 cites W2002626751 @default.
• W4386701604 cites W2019622179 @default.
• W4386701604 cites W2038949065 @default.
• W4386701604 cites W2056563787 @default.
• W4386701604 cites W2089095990 @default.
• W4386701604 cites W2089314377 @default.
• W4386701604 cites W2114688767 @default.
• W4386701604 cites W2120556002 @default.
• W4386701604 cites W2172220975 @default.
• W4386701604 cites W2215567916 @default.
• W4386701604 cites W2322327419 @default.
• W4386701604 cites W2461193358 @default.
• W4386701604 cites W2494443411 @default.
• W4386701604 cites W2570396043 @default.
• W4386701604 cites W2601397486 @default.
• W4386701604 cites W2836445908 @default.
• W4386701604 cites W2890417872 @default.
• W4386701604 cites W2901030745 @default.
• W4386701604 cites W2903734548 @default.
• W4386701604 cites W2994285514 @default.
• W4386701604 cites W3033840892 @default.
• W4386701604 cites W3111657584 @default.
• W4386701604 cites W3130626645 @default.
• W4386701604 cites W3168352768 @default.
• W4386701604 cites W3179387966 @default.
• W4386701604 cites W3210561348 @default.
• W4386701604 cites W4223579124 @default.
• W4386701604 cites W4231535762 @default.
• W4386701604 cites W4294935206 @default.
• W4386701604 cites W4302095194 @default.
• W4386701604 cites W4322217381 @default.
• W4386701604 cites W4324057221 @default.
• W4386701604 doi "https://doi.org/10.1016/j.geomorph.2023.108910" @default.
• W4386701604 hasPublicationYear "2023" @default.
• W4386701604 type Work @default.
• W4386701604 citedByCount "0" @default.
• W4386701604 crossrefType "journal-article" @default.
• W4386701604 hasAuthorship W4386701604A5020198886 @default.
• W4386701604 hasAuthorship W4386701604A5033503685 @default.
• W4386701604 hasAuthorship W4386701604A5053356806 @default.
• W4386701604 hasAuthorship W4386701604A5092860876 @default.
• W4386701604 hasBestOaLocation W43867016041 @default.
• W4386701604 hasConcept C109007969 @default.
• W4386701604 hasConcept C114793014 @default.
• W4386701604 hasConcept C119599485 @default.
• W4386701604 hasConcept C121332964 @default.
• W4386701604 hasConcept C127313418 @default.
• W4386701604 hasConcept C127413603 @default.
• W4386701604 hasConcept C137527640 @default.
• W4386701604 hasConcept C186295008 @default.
• W4386701604 hasConcept C187320778 @default.
• W4386701604 hasConcept C195268267 @default.
• W4386701604 hasConcept C199927954 @default.
• W4386701604 hasConcept C2779452743 @default.
• W4386701604 hasConcept C60591178 @default.
• W4386701604 hasConcept C65865001 @default.
• W4386701604 hasConcept C69990965 @default.
• W4386701604 hasConcept C97355855 @default.
• W4386701604 hasConceptScore W4386701604C109007969 @default.
• W4386701604 hasConceptScore W4386701604C114793014 @default.
• W4386701604 hasConceptScore W4386701604C119599485 @default.
• W4386701604 hasConceptScore W4386701604C121332964 @default.
• W4386701604 hasConceptScore W4386701604C127313418 @default.
• W4386701604 hasConceptScore W4386701604C127413603 @default.
• W4386701604 hasConceptScore W4386701604C137527640 @default.
• W4386701604 hasConceptScore W4386701604C186295008 @default.
• W4386701604 hasConceptScore W4386701604C187320778 @default.
• W4386701604 hasConceptScore W4386701604C195268267 @default.
• W4386701604 hasConceptScore W4386701604C199927954 @default.
• W4386701604 hasConceptScore W4386701604C2779452743 @default.
• W4386701604 hasConceptScore W4386701604C60591178 @default.
• W4386701604 hasConceptScore W4386701604C65865001 @default.
• W4386701604 hasConceptScore W4386701604C69990965 @default.
• W4386701604 hasConceptScore W4386701604C97355855 @default.
• W4386701604 hasLocation W43867016041 @default.
• W4386701604 hasOpenAccess W4386701604 @default.
• W4386701604 hasPrimaryLocation W43867016041 @default.
• W4386701604 hasRelatedWork W2007030016 @default.
• W4386701604 hasRelatedWork W2014956389 @default.
• W4386701604 hasRelatedWork W2147357873 @default.
• W4386701604 hasRelatedWork W2621423033 @default.
• W4386701604 hasRelatedWork W2746380321 @default.
• W4386701604 hasRelatedWork W2749824284 @default.
• W4386701604 hasRelatedWork W2783228585 @default.
• W4386701604 hasRelatedWork W3173057511 @default.

• next