In order to investigate the crack propagation in quasi-brittle materials like rock, ceramic and concrete, Hillerborg and his co-researchers abstracted the fracture process zone in front of a stress free crack in terms of a "fictitious crack zone". On the fictitious crack zone, cohesive stresses distribute following a given softening relationship of stress vs. crack opening. Based on the polynomial or power series expression of cohesive crack opening displacement, the relationship of the cohesive stress vs. the crack opening displacement is established using elastic theory and integral equation, and some unknown physics variables are obtained using variation approach. The calculation results gained in this paper are close to the experimentally test ones.Fracture mechanics is one of the effectively analytic approaches to the failure behavior of materials and structures. Many investigators have focused their main attention on the crack propagation resistance and the size effect of fracture parameters of quasi-brittle materials [1][2][3] . As well known, quasi-brittle materials like ceramic, rock and concrete are widely used in engineering practice. Their basic behaviors are considerably different from metal materials with observably strain hardening behavior. It was investigated in the quasi-brittle materials that when their stresses or strains arrive at their critical values, the plots of stress vs. strain, contrary to metal materials, show a typical strain softening character [4,5] . In order to describe the crack propagation process in such a quasi-brittle material as is neither plastic nor brittle, Hillerborg, Modeer and Petersson (1976) proposed a fictitious crack model [6] in which the cohesive stresses distributed on the fracture process zone (FPZ) in front of the crack tip were taken into account for crack