Atterberg Limits
Liquid Limit Test | Plastic Limit Test
Atterberg’s limits tests
A fine-grained soil can exist in any of several states; which state depends on the amount of water in the soil system. When water is added to a dry soil, each particle is covered with a film of adsorbed water. If the addition of water is continued, the thickness of the water film on a particle increases. Increasing the thickness of the water films permits the particles to slide past one another more easily. The behavior of the soil, therefore, is related to the amount of water in the system. Approximately sixty years ago, A. Atterberg defined the boundaries of four states in terms of "limits" as follows:
Procedure for Determination of Liquid Limit | Procedure for Determination of Plastic Limit These limits have since been more definitely defined by A. Casagrande as the water contents which exist under the following conditions: The water content at which the soil has such a small shear strength that it flows to close a groove of standard width when jarred in a specified manner. The Liquid Limit, also known as the upper plastic limit, is the water content at which soil changes from the liquid state to a plastic state. OR It is the minimum moisture content at which a soil flows upon application of very small shear force. Liquid Limit (LL or wL) ‑ the water content, in percent, of a soil at the arbitrarily defined boundary between the semi‑liquid and plastic states. |
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Liquid limit is defined as “ the moisture content at which soil changes from liquid state to plastic state” Or According to Casagrande Liquid Limit Test it is also defined as “ the moisture content at which two sides of a groove come close together for a distance of 12.7 mm under the impact of 25 number of blows” Or According to fall cone test method Liquid Limit is also defined as “the moisture content at which the cone( fall cone test) penetrates with in the soil for 1 cm when falls freely for 5 seconds. The water content at which the soil begins to crumble when rolled into threads of specified size. The Plastic Limit, also known as the lower plastic limit, is the water content at which a soil changes from the plastic state to a semisolid state. Plastic Limit (PL or wP) ‑ the water content, in percent, of a soil at the boundary between the plastic and semi‑solid states. It is defined as “The moisture content at which the soil behaves like a plastic material is called plastic limit” Or It may also be defined as “The moisture content at which the soil changes from plastic state to semi solid state" Or “The moisture content at which the soil begins to crumble when rolled up into a thread of 3 mm in diameter”
Or “The maximum water content at which the reduction in water content will not cause decrease in total volume of soil but the increase in moisture content will cause an increase in moisture content” Or It is also defined as “the lowest water content at which the soil are still completely saturated”
Or
Ip = LL – PL |
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