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Building Design and Construction Handbook - Merritt - Ventech!

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6.40 SECTION SIX<br />

terms the shear strength of soils can be divided into two broad categories: granular<br />

(nonplastic) soils <strong>and</strong> cohesive (plastic) soils.<br />

Granular Soil. These types of soil are nonplastic <strong>and</strong> include gravels, s<strong>and</strong>s, <strong>and</strong><br />

nonplastic silt such as rock flour. A granular soil develops its shear strength as a<br />

result of the frictional <strong>and</strong> interlocking resistance between the individual soil particles.<br />

Granular soils, also known as cohesionless soils, can only be held together<br />

by confining pressures <strong>and</strong> will fall apart when the confining pressure is released<br />

(i.e., c� � 0). The drained shear strength (effective stress analysis) is of most<br />

importance for granular soils. The shear strength of granular soils is often measured<br />

in the direct shear apparatus, where a soil specimen is subjected to a constant<br />

vertical pressure (� ) while a horizontal force is applied to the top of the shear box<br />

�n<br />

so that the soil specimen is sheared in half along a horizontal shear surface (see<br />

Fig. 6.10). By plotting the vertical pressure (� ) versus shear stress at failure (� ƒ),<br />

�n<br />

the effective friction angle (��) can be obtained. Because the test specifications<br />

typically require the direct shear testing of soil in a saturated <strong>and</strong> drained state, the<br />

shear strength of the soil is expressed in terms of the effective friction angle (��).<br />

Granular soils can also be tested in a dry state, <strong>and</strong> the shear strength of the soil<br />

is then expressed in terms of the friction angle (�). In a comparison of the effective<br />

friction angle (��) from drained direct shear tests on saturated cohesionless soil<br />

<strong>and</strong> the friction angle (�) from direct shear tests on the same soil in a dry state, it<br />

has been determined that �� is only 1 to 2� lower than �. This slight difference is<br />

usually ignored <strong>and</strong> the friction angle (�) <strong>and</strong> effective friction angle (��) are<br />

typically considered to mean the same thing for granular (nonplastic) soils.<br />

Table 6.12 presents values of effective friction angles for different types of granular<br />

(nonplastic) soils. An exception to the values presented in Table 6.12 are granular<br />

soils that contain appreciable mica flakes. A micaceous s<strong>and</strong> will often have<br />

a high void ratio <strong>and</strong> hence little interlocking <strong>and</strong> a lower friction angle. In summary,<br />

for granular soils, c� � 0 <strong>and</strong> the effective friction angle (��) depends on:<br />

1. Soil Type (Table 6.12). S<strong>and</strong> <strong>and</strong> gravel mixtures have a higher effective friction<br />

angle than nonplastic silts.<br />

2. Soil Density. For a given granular soil, the denser the soil, the higher the effective<br />

friction angle. This is due to the interlocking of soil particles, where at a<br />

FIGURE 6.10 Direct shear apparatus.

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