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Research Article | Open Access

Permeability of coarse silts using dissipation tests in cone penetration test: Case study, Finninmäki testing site

Mohammad Sadegh Farhadi( )Eetu PöyryTim Tapani Länsivaara
Research Center TERRA, TERRA-Geo group, Faculty of Built Environment, Tampere University, Korkeakoulunkatu 5, 33720 Tampere, Finland
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Abstract

Dissipation tests were performed at the Finninmäki testing site, Tampere, Finland, through the cone penetration test (CPTu). In these tests, both contractive and dilative behaviors were observed. The parameter t 50 , the time when 50 % of initial pore pressure, u 2 , dissipates, was computed for the tests using three methods proposed in literature. Then, soil permeability, k, was estimated following two approaches, using either t 50 -based empirical equations or CPTu-based methods. It was observed that the t 50 values interpreted from the three methods were considerably different. The differences in the estimated t 50 values led to considerably variable k estimations approximated by the t 50 -based empirical equations. On the other hand, the CPTu-based k estimates were considerably different from the t 50 -based estimations. Besides, three undisturbed soil samples were taken by the 132 mm TUNI tube sampler in the field. These samples were used in the lab to measure the soil permeability, k, experimentally. Comparison of the experimental measurements with the k estimates highlighted the significance of the improvement required for the available empirical equations to estimate k for the studied coarse silts.

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AIMS Geosciences
Pages 885-906

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Cite this article:
Farhadi MS, Pöyry E, Länsivaara TT. Permeability of coarse silts using dissipation tests in cone penetration test: Case study, Finninmäki testing site. AIMS Geosciences, 2025, 11(4): 885-906. https://doi.org/10.3934/geosci.2025038

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Web of Science

Received: 13 March 2025
Revised: 17 June 2025
Accepted: 19 August 2025
Published: 15 December 2025
©2025 the Author(s), licensee AIMS Press.

This is an open access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0)