Wednesday, 29 September 2021

Geotechnical Engineering

 πŸ‘‰ Active earth pressure in loose state is larger than the active earth pressure in dense state.

πŸ‘‰ Passive earth pressure in dense state is larger than the passive earth pressure in loose state.

πŸ‘‰ By compacting the soil, active earth pressure decreases but passive earth pressure increases.

πŸ‘‰Soils deposited by wind are called Aeolian soil.

πŸ‘‰All types of soils carried and deposited by water are known as Alluvial deposits.

πŸ‘‰Lacustrine soils are soil deposited in lake beds.

πŸ‘‰Marine deposits are formed when the flowing water carries soils to oceans or sea.

πŸ‘‰Loess is a loose deposit of wind blown silt that has been weakly cemented with calcium carbonate and montmorillonite.

πŸ‘‰Marl is a very fine grained calcium carbonated soil of marine origin.

πŸ‘‰Peat is a highly organic soil, consisting almost entirely of vegetative matter in varying states of decomposition, brown to black in colour, possessing an organic odour.

πŸ‘‰Peat and Muck are organic clay.

πŸ‘‰Volume of solids will remain same in fill and borrow pit.

πŸ‘‰For a sandy soil with soil grains spherical in shape and uniform in size the theoretical void ratio is 0.91.