Least-squares fitting of the linear Mohr envelope
- 1 February 1982
- journal article
- Published by Geological Society of London in Quarterly Journal of Engineering Geology
- Vol. 15 (1) , 55-56
- https://doi.org/10.1144/gsl.qjeg.1982.015.01.07
Abstract
Introduction Mohr's hypothesis proposes that when shear failure along a plane takes place, the normal stress σ and the shear stress τ acting on that plane have a characteristic functional relationship. This function relating τ and σ, it is proposed, depends on the material and can be represented on the στ plane by a line defining the critical values of α and τ for shear failure. In practice this critical line is constructed tangen-tially to Mohr circles representing different combinations of principal stresses applied to specimens of a particular material and is therefore referred to as the Mohr envelope. For some materials a straight Mohr envelope with the equation τ = c + μσ appears from the results of triaxial testing. Furthermore in the routine testing of some materials (e.g. soils) a straight line envelope is sometimes assumed a priori. In such tests small deviations of the Mohr circles from the envelope are attributed to errors and a best-fitting straight line is used to obtain the parameters (μ, c ) necessary to characterize the properties of the material. We describe here a procedure for calculating a best-fitting straight Mohr envelope from data consisting of the applied principal stresses (i.e. from the Mohr circles). The concept of best-fit used The criterion used for selecting the envelope of best fit is illustrated in Fig. 1. By means of a least-squares fit we represent the Mohr envelope by a straight line τ = c + μσ- subject to the condition that SThis publication has 3 references indexed in Scilit:
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