This paper presents the use of dilatometer test to determine the type and state of organic soils. The results of dilatometer tests perfomed in organic subsoils, composed of peat, gyttja layers as well as organic mud, located at the Antoniny, Koszyce and Nielisz sites are shown. The analysis of test results indicates that the correction for material index (ID) proposed by Larsson can be used for tested organic soils. Based on proposed modification of Larsson’s chart the type and state of organic soils can be determined.
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