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Title:Mean grain size as a function of spectral amplitude: a new regression law for marine sediment cores
Authors:ID Zanette, Nelly (Author)
ID Battelino, Darinka (Author)
ID Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo Univerze v Mariboru (Copyright holder)
Files:.pdf Acta_geotechnica_Slovenica_2006_Zanette,_Battelino_Mean_grain_size_as_a_function_of_spectral_amplitude_a_new_regression_law_for_marine_s.pdf (437,86 KB)
MD5: 0E57722175DEE75F72DDD117D4507452
PID: 20.500.12556/dkum/c4837314-63f3-47a9-b7eb-97fbc29fb6c0
 
URL http://fgserver3.fg.um.si/journal-ags/2006-1/article-2.asp
 
Language:English
Work type:Scientific work
Typology:1.01 - Original Scientific Article
Organization:FGPA - Faculty of Civil Engineering, Transportation Engineering and Architecture
Abstract:Geophysics has been developed in order to supply indicative estimations in soil mechanics like the grain size distribution of finely grained soils as day, silt and fine sands. The paper describes the attempt to characterize porous and saturated marine sediments with a non destructive technique which is the acoustic wave, in order to determine the correlation with geotechnical measurements. The characterization of physical parameters of marine sediments was based on research methods which permit to describe the parameters defining different types of sediment and zones of sedimentation; to determine fundamental parameters that influence the propagation of the acoustic waves in saturated and porous means; to define quick and indicative methods for characterization of physical parameters of analysed means. The acoustic measurements were carried out at SACLANT-NATO of La Spezia (I), where the Vertical Multi Sensor Core Logger (V-MSCL) was used. The results of acoustic tests were compared to the grain size curves of the sediments and the propagation characteristics such as velocity, density, porosity and absorption of experimentally determined data. The analyses are based 011 various mathematical models presented in. literature, in order to predict and to describe physical mechanisms of the wave propagation using a simplification of the sediment structure. The target of the study was to determine a new mathematical law that linked the mean grain size to a directly measurable parameter such as the spectral amplitude, and to offer the possibility to obtain the first indicative value of the sediment mean grain size. The determined exponential law represents an innovative and quick approach to determine a physical characteristic of saturated and porous sediments such as the grain size in a non destructive way based on the spectral analysis of the wave propagation form.
Keywords:soil mechanics, marine sediments, finely grained soil, acoustic waves, grain size curve
Publication status:Published
Publication version:Version of Record
Year of publishing:2017
Number of pages:str. 28-34
Numbering:Letn. 3, št. 1
PID:20.500.12556/DKUM-70502 New window
ISSN:1854-0171
UDC:624.131
ISSN on article:1854-0171
COBISS.SI-ID:10531094 New window
NUK URN:URN:SI:UM:DK:FRDMFJ2Z
Copyright:Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo Univerze v Mariboru
Publication date in DKUM:17.05.2018
Views:1211
Downloads:174
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Categories:Misc.
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Record is a part of a journal

Title:Acta geotechnica Slovenica
Shortened title:Acta geotech. Slov.
Publisher:Fakulteta za gradbeništvo, prometno inženirstvo in arhitekturo Univerze v Mariboru
ISSN:1854-0171
COBISS.SI-ID:215987712 New window

Secondary language

Language:Slovenian
Title:Granulometrija kot funkcija spektralne amplitude: nov regresisjki za kon za morske sedimente
Abstract:V članku je prikazana geofizikalna metoda, katera omogoča analizo poroznih, saturiranih morskih sedimentov z uporabo širjenja akustičnega valovanja in primerjava dobljenih rezultatov z rezultati konvencionalnih geomehanskih preiskav. Akustične meritve so bile izdelane v SACLANT-NATO v kraju Spezija (1), z uporabo Vertikal Multi Senzor Core Logger (V-MSCL). Rezultati akustične preiskave so bili primerjani z granulometrijskimi krivuljami analiziranih morskih sedimentov in karakteristikami širjenja valov, kot so hitrost in dušenje valovanja ter poroznost materiala. Analiza rezultatov je bila izdelana na osnovi različnih matematičnih modelov, podanih v literaturi, s katerimi bi bilo možno določiti fizikalno odvisnost med širitvijo valovanja v poroznem, saturiranem materialu in njegovo granulometrijo. Rezultat študije je nov pristop, ki omogoča iz izmerjenih vrednosti spektralne amplitude oziroma spektralne analize širjenja valov v poraznem in saturiranem materialu, neposredno določanje velikosti posameznih zrnc z matematično eksponentno funkcijo.
Keywords:geomehanika, morski sedimenti, drobno zrnate zemljine, akustični valovi, krivulja zrnavosti


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  1. Acta geotechnica Slovenica

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