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Volume 6 – Geotechnical Manual, Site Investigation and Engineering ...

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Chapter 6 SLOPE STABILITY<br />

Table 6.1 Undrained Shear Strength <strong>and</strong> Consistency of Cohesive Soils<br />

Consistency<br />

Undrained Shear<br />

Strength, S u (kPa)<br />

Visual Identification<br />

Very soft < 12 Thumb can penetrate more than 25 mm<br />

Soft 12 <strong>–</strong> 25 Thumb can penetrate about 25 mm<br />

Medium 25 -50<br />

Thumb can penetrate with moderate<br />

effort<br />

Stiff 50 <strong>–</strong> 100 Thumb will indent soil about 8 mm<br />

Very stiff 100 <strong>–</strong> 200<br />

Thumb will not indent but readily indent<br />

with thumbnail<br />

(After Terzaghi & Peck <strong>and</strong> ASTM D2488-90)<br />

6.4.2.2 Long-term<br />

Long-term stability analysis is normally carried out using effective stress analysis with drained shear<br />

strength parameters. For cohesive or clayey soil, total stress analysis (for short-term) in addition to<br />

the effective stress analysis (for long-term) are carried out to determine the most critical factor of<br />

safety. As granular or s<strong>and</strong>y soils are more permeable than cohesive or clayey soils, drainage of<br />

excess pore pressure in s<strong>and</strong>y soil occurs much more rapidly. Hence, only effective stress analysis is<br />

usually required.<br />

Effective stress analysis requires the estimation of the drained strength parameters c’, φ’ <strong>and</strong> pore<br />

pressures. For pure free draining s<strong>and</strong>s, φ = φ’ <strong>and</strong> c = 0. Under conditions of steady seepage, the<br />

phreatic line can be obtained from the flow net.<br />

Some common drained strength parameters, φ' <strong>and</strong> c’ adopted in the slope analysis are as follows:-<br />

Table 6.2 Typical Drained Parameters For Effective Stress Analysis<br />

Soil type Effective friction angle φ‘ Effective cohesion c’<br />

Well compacted soil 28 o <strong>–</strong> 30 o 2 <strong>–</strong> 5 kPa<br />

Residual soil grade V to VI 30 o <strong>–</strong> 32 o 5 <strong>–</strong> 10kPa<br />

Residual soil grade IV to V 32 o <strong>–</strong> 35 o 10 <strong>–</strong> 15kPa<br />

Note:-<br />

• The values above are just for references. Test shall be carried out before any<br />

analysis is carried out. It is advisable to limit the cohesion to not more than<br />

15kPa even with lab test results. The cohesion shows in test are sometimes<br />

apparent <strong>and</strong> the changes are subjected to external factors i.e., weathering<br />

process etc<br />

• Description of grade of residual soil:<br />

Grade VI = residual soil : Grade V = completely weathered rock ; Grade IV =<br />

highly weathered<br />

6.5 CIRCULAR ARC ANALYSIS<br />

6.5.1 General Principles<br />

Figure 6.4 shows a potential slide mass defined by a predetermined circular arc slip surface. If the<br />

shear resistance of the soil along the slip surface exceeds that necessary to provide equilibrium, the<br />

mass is stable. If the shear resistance is insufficient, the mass is unstable. Thus, the stability or<br />

instability of the mass depends on its weight, the external forces acting on it, the shear strengths<br />

March 2009 6-5

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