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| A whole process creeping model of salt rock under uniaxial compression based on inverse S function |
| WANG Junbao1,LIU Xinrong2,SONG Zhanping1,ZHAO Baoyun3,JIANG Bin3,HUANG Tianzhu3 |
(1. School of Civil Engineering,Xi?an University of Architecture and Technology,Xi?an,Shaanxi 710055,China;
2. School of Civil Engineering,Chongqing University,Chongqing 400045,China;3. Department of Civil Engineering and Architecture,Chongqing University of Science and Technology,Chongqing 401331,China) |
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Abstract In order to study the creeping properties of salt rock,uniaxial compression creeping tests under different axial stresses were carried out on salt rock specimens. The test results indicate that the creep strain and the steady creeping rate of salt rock both increase gradually and exponentially with the increasing of axial stress. The creeping process of salt rock is nonlinear with respect to the axial stress and creeping time. The higher the axial stress level and the longer the creeping time,the more obvious the nonlinear characteristic. To determine the long term strength of salt rock,an improved inflection point method for steady creeping rate-stress curve was proposed. The long term strength of salt rock determined with the method is very close to that obtained from the inflection point method for isochronous stress-strain curves. The new method can provide some insight into the similar studies. A new whole process creeping model for rocks under uniaxial compression was established by taking the inverse of S shaped function. The creeping test results of salt rock were used to evaluate the reasonability of the creeping model. The comparison of prediction curves and the test results shows that not only the primary creeping stage and steady creeping stage under the low stress level,but also the whole creep process(the primary creep stage,steady creep stage and accelerated creep stage) under the high stress level of salt rock can be described by this model. The new creeping model can accurately reflect the three stages of rock creeping with a unified expression,and overcome the shortcomings of the combined component model which is segmented. In addition,the expression of the model is very simple and convenient for application.
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