液化                        
                
                                
                        
                            孔隙水压力                        
                
                                
                        
                            岩土工程                        
                
                                
                        
                            有效应力                        
                
                                
                        
                            地质学                        
                
                                
                        
                            剪切(地质)                        
                
                                
                        
                            土壤液化                        
                
                                
                        
                            循环应力                        
                
                                
                        
                            材料科学                        
                
                                
                        
                            复合材料                        
                
                        
                    
            作者
            
                Geoffrey R. Martin,H. Bolton Seed,Wdl Finn            
         
                    
            出处
            
                                    期刊:Journal of the Geotechnical Engineering Division
                                                         [American Society of Civil Engineers]
                                                        日期:1975-05-01
                                                        卷期号:101 (5): 423-438
                                                        被引量:563
                                
         
        
    
            
            标识
            
                                    DOI:10.1061/ajgeb6.0000164
                                    
                                
                                 
         
        
                
            摘要
            
            The mechanism of progressive pore pressure increase during undrained cyclic simple shear tests on saturated sands has been examined in detail. The concepts developed provide a better understanding of the physical processes leading to liquefaction of horizontal sand deposits during earthquakes. A quantitative relationship between volume changes occurring during drained cyclic tests and the progressive increase of pore water pressure during undrained cyclic tests has been developed. The use of this relationship enables the build-up of pore water pressure during cyclic loading to be computed theoretically using basic effective stress parameters of the sand. The application of the theory to the case of undrained cyclic simple shear tests with uniform stress controlled loading is illustrated. Values of progressive pore water pressure increases predicted theoretically agree reasonably well with the nature of pore water pressure increases observed experimentally.
         
            
 
                 
                
                    
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