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Gold Science and Technology ›› 2020, Vol. 28 ›› Issue (3): 430-441.doi: 10.11872/j.issn.1005-2518.2020.03.151

• Mining Technology and Mine Management • Previous Articles     Next Articles

Fatigue Damage Analysis of Fractured Sandstone Based on Nuclear Magnetic Resonance T2 Spectrum

Siyu MAO(),Ping CAO(),Jianxiong LI,Chuanjing OU   

  1. School of Resources and Safety Engineering,Central South University,Changsha 410083,Hunan,China
  • Received:2019-09-06 Revised:2020-02-26 Online:2020-06-30 Published:2020-07-01
  • Contact: Ping CAO E-mail:632776568@qq.com;pcao_csu@sina.com

Abstract:

In the process of underground mining and tunnel construction,the rock is mostly in the process of repeated loading and unloading,and the macro-cracks and micro-defects in the rock mass itself will continue to expand under fatigue loading and eventually lead to many accidents.Therefore,it is of great engineering significance to study the micro-defects of fractured rock masses under fatigue loading.In the previous studies, acoustic emission and CT scanning technology were mainly used to reflect the change of microscopic damage through AE number or CT number, which obtained good results.The porosity measured by nuclear magnetic resonance technology can also be used to show the damage of rock samples,but it is currently mainly used in uniaxial compression loading.In this experiment,yellow sandstone specimens with five fracture inclination angles (0°,15°,30°,45°,60°) were selected.Firstly,uniaxial compression experiments were performed to measure the uniaxial compressive strength of fractured sandstone at various angles.Then carry out fatigue loading experiments,and select the upper limit fatigue loading stresses based on the measured uniaxial compressive strength to be 19.1 MPa,25.6 MPa and 30.3 MPa,respectively.The internal porosity of each fractured sandstone before and after 30 fatigue cycles under each upper limit stress was measured with nuclear magnetic resonance instruments.Combined with the analysis of T2 spectrum measured by nuclear magnetic resonance instrument,it is found that with the increase of the upper limit stress,the total area of T2 spectrum and the accumulation of porosity in fractured sandstone have increased significantly.This shows that its internal damage increases with the increase of the upper limit stress,and then combined with the T2 spectral area for quantitative analysis,it was found that the spectral area of the small pores in the T2 spectrum changed only slightly with the increase of the upper limit stress,while the spectral area of large pores increases exponentially with the increase of the upper limit stress.No matter from the angle of the change of the ratio of large pores (to the total pores) to the fatigue upper limit stresses under different inclination angles,or from the angle of the change of the ratio of large pores under different fatigue upper limit stresses to the angle of fracture inclination,similar rules are obtained.Therefore,it can be concluded that the change of large pores is the main factor that causes the total porosity of fractured sandstones to increase after fatigue loading,and then the curve of the ratio of the proportion of large holes to the upper limit fatigue stress ratio after fatigue loading at various inclination cracks is fitted.The fitting coefficients of sandstones at various inclination angles are very high,which shows that the change law of internal damage can be well displayed.Considering the effect of initial damage of rock samples on fatigue loading,two types of damage variables based on the ratio of large pores to total pores were defined to study the impact of fatigue upper limit stress on the fatigue damage of sandstones with different fracture inclination angles.According to the relationship curves between the two damage variables,the upper limit stress ratio and the upper limit stress,the change of the defined damage variable can be well projected. Further analysis can show the intensity change of the sandstones with different fracture inclination angles,that is,the damage intensity of the fractured rock sample that tends to be gentle will eventually be greater than that of the fractured rock sample with a sharp increase in damage. Finally,combining the probability density function of Weibull distribution and generalized Hook’s law,it is deduced from the theoretical formula that it is reasonable to use pores to study sandstone fatigue damage.Combining the results of previous studies and this experiment,it was found that the porosity can well reflect the microscopic damage of rock samples in both uniaxial compression experiments and fatigue loading experiments.

Key words: fractured sandstone, fatigue loading, nuclear magnetic resonance, microscopic damage, fatigue strength, damage variable

CLC Number: 

  • TU443

Fig.1

Yellow sandstone sample and test design flow chart"

Fig.2

Schematic diagram and results of uniaxial compression loading test"

Fig.3

Schematic diagram fatigue loading curve"

Fig.4

NMR spectra of all samples"

Fig.5

T2 distribution and cumulative porosity curve before and after fatigue loading of sandstone"

Table 1

Comparison of nuclear magnetic resonance spectrum area of 0° fractured rock samples before and after fatigue loading"

岩样代号编号小孔谱面积疲劳加载后增幅大孔谱面积疲劳加载后增幅
疲劳前疲劳后疲劳前疲劳后
0-1917 765.157 865.13+1.29%6 088.456 530.75+7.26%
27 562.448 187.28+8.26%1 420.061 969.82+38.71%
37 209.697 990.78+10.83%5 592.666 159.69+10.14%
0-2618 025.266 854.49-14.59%2 408.643 473.45+44.21%
28 205.958 446.64+2.93%2 653.975 242.45+97.53%
36 612.318 041.24+21.61%2 721.096 020.57+121.26%
0-3118 019.327 611.89-5.08%2 626.235 901.92+124.73%
28 022.078 509.59+6.08%1 850.364 751.84+156.81%
37 888.177 936.17+0.61%2 687.425 587.12+107.90%

Fig.6

Variation of the proportion of large pores with fatigue upper limit stress under different fracture inclination angles"

Fig.7

Variation of the proportion of large pores with fracture inclination angle under different fatigue upper limit stresses"

Fig.8

Fitting curve of the proportion of large pores with fatigue upper limit stress ratio in fractured sandstone with different inclination angles"

Table 2

Characteristics of fitting equation of proportion of large pores with fatigue upper limit stress"

裂隙倾角/(°)拟合曲线方程拟合系数R2X=0.96的拟合数值
0y=0.15421+0.58142*x3.338360.972900.66156
15y=0.14508+0.44167*x10.392120.972410.43406
30y=0.15864+0.50032*x5.4260.999700.55955
45y=0.17174+0.34557*x3.101330.935110.47622
60y=0.13469+0.55907*x6.468360.998310.56402

Table 3

Correlation equation of damage variable D of fractured sandstone with different inclination angles"

裂隙倾角/(°)D与上限应力比的关系D与上限应力(σmax)的关系
0D0=1.14599*x3.33836D0=1.14599*(σmax/39.58)3.33836
15D15=1.52838*x10..39212D15=1.52838*(σmax/33.66)10..39212
30D30=1.24796*x5.426D30=1.24796*(σmax/35.75)5.426
45D45=1.13495*x3.10133D45=1.13495*(σmax/37.72)3.10133
60D60=1.30219*x6.46836D60=1.30219*(σmax/36.51)6.46836

Fig.9

Damage variable curves of fractured sandstone with different inclination angles"

Table 4

Correlation equation of damage variable D′ of fractured sandstone with different inclination angles"

裂隙角度/(°)D′与上限应力比的关系D′与上限应力(σmax)的关系
0D0′=0.2331+0.8789*x3.33836

D0′=0.2331+0.8789*

(σmax/39.58)3.33836

15D15′=0.3342+1.0175*x10.39212

D15′=0.3342+1.0175*

(σmax/33.66)10..39212

30D30′=0.2835+0.8941*x5.426

D30′=0.2835+0.8941*

(σmax/35.75)5.426

45D45′=0.3606+0.7257*x3.10133

D45′=0.3606+0.7257*

(σmax/37.72)3.10133

60D60′=0.2388+0.9912*x6.46836

D60′=0.2388+0.9912*

(σmax/36.51)6.46836

Fig.10

Variation curve of the proportion of large pores with porosity"

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