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an engineering geological characterisation of tropical clays - GBV

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125<br />

Plate 7.8. Oedometer consolidation testing in this study.<br />

The British St<strong>an</strong>dard consolidation testing procedure adopted in this study is very similar in<br />

principle to the one-dimensional consolidation test specified by the ASTM Designation<br />

D2435. However, the ASTM st<strong>an</strong>dard incorporates either a fixed-ring type or floating-ring<br />

type <strong>of</strong> consolidation cell, with minimum specimen dimensions <strong>of</strong> 50 mm diameter <strong>an</strong>d 12,5<br />

mm thickness; <strong>an</strong>d a minimum height to diameter ratio <strong>of</strong> 1:2,5. In addition, a copper disc is<br />

also used for the deformation calibration <strong>of</strong> the apparatus, while <strong>an</strong> initial seating load <strong>of</strong> 2,5-<br />

5,0 kPa is usually applied to the soil specimen depending on the s<strong>of</strong>tness <strong>of</strong> the soil. In<br />

practice, a st<strong>an</strong>dard loading sequence <strong>of</strong> pressures consist <strong>of</strong> 5, 12,5; 25, 50, 100, 200, 400,<br />

800 kPa, even though smaller increments could be used on very s<strong>of</strong>t soils (BS 1377: 1975;<br />

ASTM D2435-70).<br />

7.4.5 Analysis <strong>of</strong> consolidation test data<br />

A graphical <strong>an</strong>alysis <strong>of</strong> consolidation test data obtained for black <strong>clays</strong> made use <strong>of</strong><br />

conventional log-time method. However, both log-time <strong>an</strong>d square-root-time methods were<br />

employed in the graphical <strong>an</strong>alysis <strong>of</strong> test data for the more silty red clay soils, whose early<br />

portion <strong>of</strong> log- time/ settlement curves depart from the conventional shape as derived from<br />

theoretical relationships (Fig. 7.17). Determination <strong>of</strong> the do point corresponding to 0%<br />

primary consolidation was therefore not possible. The departure from conventional shape<br />

could be attributed to the relatively much higher permeability (k = 7,57E-11 to 7,33E-9) <strong>of</strong><br />

the red soils which caused rapid settlement immediately after initial loading, so that the initial

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