Experimental Study on Effects of Deterioration of Grains on Deformation and Strength Characteristics of Soils

Doctoral Thesis / Dissertation from the year 2010 in the subject Engineering - Geotechnology course: Civil Engineering language: English abstract: With growing infrastructure developments in hilly areas and due toeconomical constraints of using locally available rockfill materials for construction of embankments practicing engineers must be acquainted with geotechnical response of non-conventional granular soils. These materials are most likely to disintegrate with time due to physical and chemical weathering. In general the laboratory investigations on durability characteristics of such materials are only made through simple slaking tests. However studies examining the effects of slaking-induced disintegration of soil grains on thegeotechnical engineering analysis and design parameters are rather limited. This is essentially due to the reason that the grains of standard laboratory sands are mostly durable and hence the stress-strain response is considered to be unaffected by the presence of water.In order to explore the possible effects of deterioration of soil grains on static and dynamic properties of granular soils a series of consolidated drained torsional shear tests on various crushed soft rocks were performed under saturated and dry conditions and compared with a well reported Toyoura silica sand consisting of durable grains. Due to the sensitivity of crushed rockfill todeteriorate upon water-submergence test under dry conditions represented the response of a soil with intact grains whereas a similar test under saturated condition simulated the potential reduction in strength and stiffness of the soil with time. From the grain size distributions determined after each test a degradation index was defined to quantify the degree of disintegration of grains.Strength and deformation properties determined from monotonic as well as cyclic shear tests were then compared with this index. Possible correlations of water-induced deterioration of soil g