فرمولاسیون تعادل فاز دو فازی و نمودار فاز برای سیستم تغییر شکل پلاستیکی تحت شرایط تنش غیر هیدرواستاتیک: فرمولاسیون و تأیید

On the basis of a widely used approximation that the constitutive relationships between deviatoric stress and deviatoric elastic strain are linear, and the elastic coefficients depend only on pressure and temperature, a formula of the general chemical potential was derived in this paper. The result was found to be similar to that in hydrostatic thermodynamics as long as we substitute temperature T with an effective quantity Teff, which has the unit of temperature, and pressure P with another effective quantity Peff, which has the unit of pressure. The expressions of Teff and Peff are correlated with deviatoric elastic strain, elastic coefficients and the pressure and temperature partial derivatives of elastic coefficients. It is through the correlation between Teff and Peff and deviatoric quantities that the influence of deviatoric stress on phase equilibrium and phase transformation is imposed. In classical solid mechanics, the mechanical properties of a solid body are usually divided into two classes: volumetric properties and deviatoric properties. In addition, the deviatoric properties are thought to be affected by volumetric properties, but the volumetric properties are not influenced by deviatoric properties. Thus, the deviatoric and volumetric properties are standing unequal in classical solid mechanics. In contrast, the irrational inequality between volumetric and deviatoric properties has been successfully removed in the formulism proposed in this paper. For an isotropic solid system, the general Clausius-Clapyron relation was further deduced, which can be used to quantitatively calculate the shift in transition pressure caused by deviatoric stress. As an example of application, as well as verification, the formulism proposed in this paper was employed to quantitatively interpret the scatter in transition pressure of the α-ω transformation of titanium observed in experiments, which was commonly thought to have a relationship with non-hydrostatic stresses, but comprehensive quantitative theoretical interpretations are still needed.