Predictions of coefficient of consolidation from CPTU dissipation tests in Quaternary clays

The coefficient of consolidation (c _v or c _h) is an important parameter in both geotechnical and geo-environmental engineering, measuring the flow characteristics of soils. In China, conventionally it is obtained from the oedometer test, which is time consuming and of limited accuracy due to inevitable sample disturbance. These difficulties can be overcome by in situ pizeocone dissipation tests which provide continuous measurements of pore water pressure with time. In this paper, existing methods for interpreting coefficient of consolidation in clays from piezocone dissipation tests are briefly reviewed. Piezocone tests were undertaken at different sites in the Jiangsu province of China and piezocone dissipation tests conducted at different penetration depths. Based on the reference c _v values determined from the laboratory oedometer tests, comparisons with existing interpretation methods were undertaken. It is shown that the Teh and Houlsby’s interpretation method has a much higher accuracy for determining the coefficient of consolidation of Quaternary clay deposits while the values of c _h obtained by the CPTU method are in the range of back-analyzed field values.