2021
DOI: 10.52321/geolbalc.50.1.37
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Liquefaction potential assessment of saturated loess

Abstract: Usually, soils with mainly fine grain-sized content, as loess, are considered to have low liquefaction potential. Regardless of this, many researchers have analyzed and presented much field evidence that silty soil (in particular loess) liquefaction occurred under certain conditions. In Bulgaria, the first loess river terrace (T1) within the Danube River lowland areas is covered by low plasticity silty loess with a thickness of 10–12 m. Тhe groundwater level is often located between 5 m and 8 m in depth so tha… Show more

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Cited by 7 publications
(6 citation statements)
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“…As a summary, the comparative analysis strongly supports the efficacy of both the CSC and DSM methods, highlighting their ability to significantly improve ground foundation performance. These techniques are invaluable assets in geotechnical engineering and construction, particularly in regions susceptible to seismic activity, where they contribute to both structural stability and seismic resistance (Karastanev, Tchakalova, 2021;Minkov et al, 1981).…”
Section: Design and Calculationsmentioning
confidence: 99%
“…As a summary, the comparative analysis strongly supports the efficacy of both the CSC and DSM methods, highlighting their ability to significantly improve ground foundation performance. These techniques are invaluable assets in geotechnical engineering and construction, particularly in regions susceptible to seismic activity, where they contribute to both structural stability and seismic resistance (Karastanev, Tchakalova, 2021;Minkov et al, 1981).…”
Section: Design and Calculationsmentioning
confidence: 99%
“…Jalil et al [23] studied liquefaction in Palu as the cause of massive mudflows. Karastanev & Tchakalova [24] assessed the liquefaction potential of saturated loess. Uyanik [25] analyzed the soil liquefaction based on soil and earthquake parameters.…”
Section: Overview Of Some Previous Researchmentioning
confidence: 99%
“…1) покриващи стария релеф от заравнени повърхнини, четвърта, трета и втора надзаливни тераси на р. Дунав. Еоличните седименти са изградени от типичен льос (Minkov, 1968;Philipov, Mikova, 1986;Philipov, 1990;Tchakalova, Karastanev, 2019;Karastanev, Tchakalova, 2021), смесени с алувиалните чакъли, пясъци, глини и склоновите материали. Неогенът е представен от праховопесъчливи глини, глинести варовици и прахов глинест пясък.…”
Section: геоложки условияunclassified