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Mohajerani method: Tool for determining the liquid limit of soils using fall cone test results with strong correlation with the Casagrande test

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27120%2F20%3A10246511" target="_blank" >RIV/61989100:27120/20:10246511 - isvavai.cz</a>

  • Výsledek na webu

    <a href="https://reader.elsevier.com/reader/sd/pii/S001379522031749X?token=AED89DC04C6BF848F54F48483EB55037D7DB3E1A9EA5239F25971841C10BD4535F1017CA5AC9A0B4F6CA1105AA2E8D1B" target="_blank" >https://reader.elsevier.com/reader/sd/pii/S001379522031749X?token=AED89DC04C6BF848F54F48483EB55037D7DB3E1A9EA5239F25971841C10BD4535F1017CA5AC9A0B4F6CA1105AA2E8D1B</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.enggeo.2020.105852" target="_blank" >10.1016/j.enggeo.2020.105852</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Mohajerani method: Tool for determining the liquid limit of soils using fall cone test results with strong correlation with the Casagrande test

  • Popis výsledku v původním jazyce

    The European Standard EN ISO 17892-12:2018 describes the means of determining the liquid limit (LL) of soils using two independent test methods: the Casagrande percussion cup and fall cone test. The first method is characterized mainly by its universality and the second by its simplicity. However, these two methods are known to provide different results. The higher the LL, the greater is the difference between the results. In 2019, Shimobe and Spagnoli established a correlation between the Casagrande and fall cone tests for soils with LL &lt; 150%, based on an analysis of over 100 experimental datasets. However, further studies are required for soils with LL &gt; 150%. Mohajerani method, which combines the universality of the former method and the simplicity of the latter, is applicable for such soils. The main objective of the study was to apply the Mohajerani method to determine the LLs based on fall cone test results and to compare them with those of the Casagrande test (soft base), with focus on soils with LL &gt; 150%. The experimental results showed that for high plasticity soil (containing bentonite, etc.), the differences in the LL between the Casagrande and fall cone tests are significant (ab to relative ratio 30%), and some modification of the fall cone test evaluation is required. This study confirmed excellent agreement between the LL evaluated using the Mohajerani method (i.e., modification of the fall cone test evaluation) and that obtained from the Casagrande test, even for soils with higher LLs. Furthermore, the fall cone test results were used to determine the plastic limit (PL) for those soils with LLs within 20-50% for which the Casagrande LL and standard fall cone LL were correlated (where the latter was not modified by the Mohajerani method). Determination of the PL for these types of soils via the fall cone test results offers credible results comparable to those of the standard thread rolling test.

  • Název v anglickém jazyce

    Mohajerani method: Tool for determining the liquid limit of soils using fall cone test results with strong correlation with the Casagrande test

  • Popis výsledku anglicky

    The European Standard EN ISO 17892-12:2018 describes the means of determining the liquid limit (LL) of soils using two independent test methods: the Casagrande percussion cup and fall cone test. The first method is characterized mainly by its universality and the second by its simplicity. However, these two methods are known to provide different results. The higher the LL, the greater is the difference between the results. In 2019, Shimobe and Spagnoli established a correlation between the Casagrande and fall cone tests for soils with LL &lt; 150%, based on an analysis of over 100 experimental datasets. However, further studies are required for soils with LL &gt; 150%. Mohajerani method, which combines the universality of the former method and the simplicity of the latter, is applicable for such soils. The main objective of the study was to apply the Mohajerani method to determine the LLs based on fall cone test results and to compare them with those of the Casagrande test (soft base), with focus on soils with LL &gt; 150%. The experimental results showed that for high plasticity soil (containing bentonite, etc.), the differences in the LL between the Casagrande and fall cone tests are significant (ab to relative ratio 30%), and some modification of the fall cone test evaluation is required. This study confirmed excellent agreement between the LL evaluated using the Mohajerani method (i.e., modification of the fall cone test evaluation) and that obtained from the Casagrande test, even for soils with higher LLs. Furthermore, the fall cone test results were used to determine the plastic limit (PL) for those soils with LLs within 20-50% for which the Casagrande LL and standard fall cone LL were correlated (where the latter was not modified by the Mohajerani method). Determination of the PL for these types of soils via the fall cone test results offers credible results comparable to those of the standard thread rolling test.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    20701 - Environmental and geological engineering, geotechnics

Návaznosti výsledku

  • Projekt

  • Návaznosti

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2020

  • Kód důvěrnosti údajů

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Údaje specifické pro druh výsledku

  • Název periodika

    Engineering Geology

  • ISSN

    0013-7952

  • e-ISSN

  • Svazek periodika

    278

  • Číslo periodika v rámci svazku

    1

  • Stát vydavatele periodika

    NL - Nizozemsko

  • Počet stran výsledku

    8

  • Strana od-do

    1-8

  • Kód UT WoS článku

    000589411800025

  • EID výsledku v databázi Scopus

    2-s2.0-85092051083