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These lecture notes delve into the plasticity and structure of soil, covering key concepts like liquid limit, plastic limit, shrinkage limit, and activity. They provide a comprehensive overview of atterberg limits, their determination, and their significance in soil mechanics. The notes also include practical examples and references to relevant standards and literature.
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developed a method to describe the^ consistency of fine‐grained soils
with varying moisture contents.
-^ The behavior of soil can be divided into four basic states—
solid, semisolid, plastic, and liquid.^ jbmamburam_CIEN 3113_2nd Sem AY 2024‐
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U.S. Army Corps of Engineers (1949)^ proposed an
empirical equation^ of the form. • Equation (4.3) generally yields good results for the
number of blows between 20 and 30. jbmamburam_CIEN 3113_2nd Sem AY 2024‐
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liquid limit^ that is popular in Europeand Asia is the Fall Cone Method^ (British Standard—BS1377).
-^ In this test the liquid limit is defined as the moisture content at whicha standard cone of^ apex angle 30°
and^ weight of 0.78 N (80 gf)^ will penetrate a distance^ d = 20 mm^ in 5 seconds jbmamburam_CIEN 3113_2nd Sem AY 2024‐
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3.2 mm (1/8 in.) diameter. jbmamburam_CIEN 3113_2nd Sem AY 2024‐
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Shrinkage Limit.
-^ ASTM D427 – Test Method for Shrinkage Factors of Soils by theMercury Method (Withdrawn 2008). •^ ASTM^ D4943^ ‐^ Standard^ Test
Method^ for^ Shrinkage^ Factors
of Cohesive Soils by the Water Submersion Method.jbmamburam_CIEN 3113_2nd Sem AY 2024‐
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to^ the^ corresponding^ change^
in moisture content. jbmamburam_CIEN 3113_2nd Sem AY 2024‐
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and linear shrinkage at given^ moisture contents (w)^ can be calculated as: • Linear shrinkage • Typical values of shrinkage limit for some clay mineralsjbmamburam_CIEN 3113_2nd Sem AY 2024‐
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