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A New Empirical Correlation Between Pressuremeter Modules (Em) and Shear Wave Velocity (Vs) for Clay Soils

dc.authorscopusid 15768634400
dc.authorscopusid 35739305500
dc.authorscopusid 57211276011
dc.authorwosid Akkaya, İsmail/Q-3778-2018
dc.contributor.author Akkaya, Ismail
dc.contributor.author Ozvan, Ali
dc.contributor.author Ozvan, Elif E.
dc.date.accessioned 2025-05-10T17:34:54Z
dc.date.available 2025-05-10T17:34:54Z
dc.date.issued 2019
dc.department T.C. Van Yüzüncü Yıl Üniversitesi en_US
dc.department-temp [Akkaya, Ismail] Van Yuzuncu Yil Univ, Dept Geophys Engn, Van, Turkey; [Ozvan, Ali] Van Yuzuncu Yil Univ, Dept Geol Engn, Van, Turkey; [Ozvan, Elif E.] Cukurova Univ, Inst Nat & Appl Sci, Adana, Turkey en_US
dc.description.abstract The pressuremeter (PMT) and standard penetration (SPT) tests are the most common in situ tests used for determining the engineering properties of soils and rocks. PMT method can be used to determine the deformation and strength properties of soil or very blocky rock masses. PMT procedure is time-consuming and expensive, and it requires advanced testing equipment. Both SPT and PMT methods also require drilling to be performed in the area. The shear wave velocity (V-s) is a parameter obtained using active and passive seismic methods and provides insight into the strength properties of the soil and rock. V-s is easy to obtain with these methods and can be determined in all kinds of field conditions. Due to the difficulties experienced during many types of in-situ tests, numerous empirical equations for the soil or rock units have been proposed in the literature that are based on V-s. In this paper, correlations of Menard Deformation Modules (E-M) with the corrected SPT blow counts (SPT-N-60) and shear wave velocity (V-s) data were conducted. For this purpose, parameters of the pressuremeter were defined as a function of two variables. In order to determine the relationship between the results of these field tests and the results obtained from high-consolidated clayey soils with high and low plasticity properties, 10 boreholes with a depth of 15 m were drilled and in-situ tests were carried out at diverse depths. In addition, seismic measurements were performed at the same locations and depth-based V-s velocity data was obtained. It was concluded that E-M could be predicted as a function of SPT-N60 and V-s values, and the predictions had relatively high R-2 values of 0.77 and 0.75, respectively. This study thereby introduces to the literature empirical equations between E-M and V-s for the first time. As soil properties are heterogeneous and anisotropic, it has been shown that it is more appropriate to use the equations produced from logarithmic and exponential relations in both single and multiple statistical analysis. (C) 2019 Elsevier B.V. All rights reserved. en_US
dc.description.woscitationindex Science Citation Index Expanded
dc.identifier.doi 10.1016/j.jappgeo.2019.103865
dc.identifier.issn 0926-9851
dc.identifier.issn 1879-1859
dc.identifier.scopus 2-s2.0-85074115541
dc.identifier.scopusquality Q2
dc.identifier.uri https://doi.org/10.1016/j.jappgeo.2019.103865
dc.identifier.uri https://hdl.handle.net/20.500.14720/13956
dc.identifier.volume 171 en_US
dc.identifier.wos WOS:000500374300009
dc.identifier.wosquality Q3
dc.language.iso en en_US
dc.publisher Elsevier en_US
dc.relation.publicationcategory Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı en_US
dc.rights info:eu-repo/semantics/closedAccess en_US
dc.subject Pressuremeter Test en_US
dc.subject Standard Penetration Test en_US
dc.subject Shear Wave Velocity en_US
dc.subject Clay Soil en_US
dc.subject Correlation en_US
dc.title A New Empirical Correlation Between Pressuremeter Modules (Em) and Shear Wave Velocity (Vs) for Clay Soils en_US
dc.type Article en_US

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