Influence of non-saturation and particle size distribution on the stiffness of granite materials

In this paper, the stiffness of two materials with the same geological origin is presented, a silty sand, called Perafita sand (D50=0.36mm) and a granite aggregate (0/12.5, D50=0.52mm). The stiffness in very small strains ( <10-5) of the compacted materials is studied by means of precision triaxi...

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Bibliographic Details
Main Author: Correia, A. Gomes (author)
Other Authors: Ferreira, Sandra Reis (author), Fleureau, Jean-Marie (author)
Format: conferencePaper
Language:eng
Published: 2007
Subjects:
Online Access:http://hdl.handle.net/1822/12280
Country:Portugal
Oai:oai:repositorium.sdum.uminho.pt:1822/12280
Description
Summary:In this paper, the stiffness of two materials with the same geological origin is presented, a silty sand, called Perafita sand (D50=0.36mm) and a granite aggregate (0/12.5, D50=0.52mm). The stiffness in very small strains ( <10-5) of the compacted materials is studied by means of precision triaxial tests (with local strain measurements). The influence of non-saturation on the stiffness is also studied through triaxial tests with measurement of negative pore water pressures. Such measurements allow the analysis of the mechanical behaviour of the unsaturated material in terms of effective stresses. For this purpose two approaches were used: the Terzaghi’s and Bishop’s approaches. The results obtained show, for each material, a unique relationship between vertical stiffness and vertical effective stress (constant void ratio = 0.5), independently of the saturation degree of the studied samples.