Do You Know?
👉Sand drains reduces the length of drainage path resulting in acceleration of consolidation.
👉High volume change in clay is due to presence of Montmorillonite clay.
👉Loose sand and normally consolidated clay (OCR = 1) have similar stress strain curve in triaxial compression.
👉Dense sand and over-consolidated clay (OCR>1) have similar stress strain curves.
👉Stoke's Law: Sedimentation of soil particles in water with a constant velocity is known as terminal velocity.
Stoke's Law is applicable for spheres of diameter between 0.2 mm and 0.0002 mm
👉Terzaghi's theory of consolidation considers only primary consolidation and not valid for secondary consolidation.
👉Final consolidation(Ultimate consolidation settlement) does not depend upon drainage conditions.
👉Coefficient of consolidation is inversely proportional to liquid limit.
👉Compression index of clay is related to its index properties, especially the liquid limit
According to Terzaghi and Peck
Cc = 0.009 (L.L-10) for undisturbed soils
👉The compression index for the over consolidated clay stratum (which is called as recompression index) is smaller as compared to other given soils.
👉When a soil is heavily over-consolidated its stress-strain curve has a sharp peak. It shows brittle behaviour.
Thankyou sir
ReplyDelete