Paleoclimate and Environment Evolution |
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Experimental Study on Rheological Properties of Neogene Red-bed Soft Rock |
LIU Xiao-wei1,2, CHEN Wen-wu1,2, ZHANG Fan-yu1,2, YUAN Peng-bo1,2, HAN Wen-feng1,3 |
1.Ministry of Education Key Laboratory of Mechanics on Disaster and Environment in Western China, Lanzhou University, Lanzhou 730000, China;
2.School of Civil Engineering and Mechanics, Lanzhou University, Lanzhou 730000, China;
3.Department of Civil Engineering, Tianjin College of Urban Construction, Tianjin 300381, China |
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Abstract Rheological property is a major controlling factor for rock mass stability. By a set of rheological experiments, the creep and relaxation curves of Neogene red-bed soft rock are obtained, whose variation process can be classified as three change stages. Compared with argillaceous siltstone, Neogene silty mudstone has lower strength, larger creep and longer time to stabilization. Based on scientific analysis and comparative study, rheological curves of red-bed soft rock are in accord with Burgers rheological model. Using Marquardt algorithm, the rheological parameters of red-bed soft rock under different test conditions were obtained. The rheological parameters of red-bed soft rock are far lower than those of the hard rock, which indicates that Neogene argillaceous siltstone and silty mudstone have remarkable rheological property. All these parameters can be applied to characterize the rheological properties of red-bed soft rock.
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Received: 10 April 2012
Published: 20 September 2012
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