Abstract
Organic soil is characterised by high compressibility and should be improved so that it can be used for construction. The use of every method of soil improvement requires knowledge of the compressibility parameters. One of these parameters is the constrained modulus. The constrained modulus can be determined using laboratory or in-situ tests. In this study, the constrained modulus of organic soil was determined using oedometer and piezocone tests (CPTU). The author analysed subsoil under an approximately 250 m section of a designed road in north-eastern Poland. The constrained modulus of organic soil sampled from four different depths was determined in oedometer tests. Piezocone tests were conducted at 18 points located every 15 m along the length of the section concerned. To determine the constrained modulus based on the cone resistance from CPTU tests, the knowledge of the α and αM coefficients is needed. For the tested soil, the optimal range of the α coefficient from 0.4 to 0.7 was determined. The αM coefficient ranged from 0.4 to 0.8. The value of the constrained modulus of organic soil obtained from the oedometer tests, depending on the effective stress, ranged from approximately 100 kPa to 400 kPa. The constrained modulus of the tested soil decreased with depth, which both research methods proved.
Highlights
Construction of structures on organic soils is avoided whenever possible
The objective of this study was to determine the constrained modulus of organic soil from oedometer and piezocone penetration tests
The cone resistances qtav were calculated using Formula (2) for the values of cone resistance qcav and water pressure u2av averaged within a separate layer
Summary
Construction of structures on organic soils is avoided whenever possible. rapid development has made construction works on organic soils increasingly inevitable. Organic soils should be improved so that they can be used for construction (Rahman et al, 2016). Determining the parameters of organic soil may be very difficult due to its variable properties even within one deposit (Lechowicz & Szymański, 2002; Zainorabidin & Wijeyesekera, 2008) or its ability to change properties with time (Huat et al, 2005). For these reasons, organic soil should be tested in detail and its parameters should be carefully determined using various methods
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