What is the importance of Atterberg limits?
This is very important when trying to build with or build on these type of materials. The two commonly determined Atterberg Limits represent the moisture contents at which a specific soil’s behavior changes from solid to plastic (Plastic Limit) and from plastic to liquid (Liquid Limit).Click to see full answer. Also know, why is the…
This is very important when trying to build with or build on these type of materials. The two commonly determined Atterberg Limits represent the moisture contents at which a specific soil’s behavior changes from solid to plastic (Plastic Limit) and from plastic to liquid (Liquid Limit).Click to see full answer. Also know, why is the plastic limit important?The plastic limit (PL) is the water content, in percent, at which a soil can no longer be deformed by rolling into 3.2 mm (1/8 in.) Those limit of soil are very important property of fine grained soil and its Value is used to classify fine grained soil and calculate activity of clays and toughness index of soil.Secondly, what is the importance of liquid limit and plastic limit in soil classification? Liquid Limit is the water content at which soil changes from a plastic to a liquid state, when the soil specimen is just fluid enough for a groove to close when jarred in a specified manner. Plastic Limit is the water content at the change from a plastic to a semisolid state. In respect to this, what is the importance of liquid limit? Value of liquid limit is used to classify fine grained soil. It gives us information regarding the state of consistency of soil on site. Liquid limit of soil can be used to predict the consolidation properties of soil while calculating allowable bearing capacity & settlement of foundation.What is meant by plastic limit?Plastic limit is the water content in clay soil below Which it stop to behave like a plastic material. it starts to crumble when rolled in threads of 3 mm diameter. At this water content, the soil losses its plasticity. Liquid limit of clay soil is the water content at which soil change from plastic to liquid states.
