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  --2010, 29 (09)   Published: 15 September 2010
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Artiles

 2010, 29 (09): -0 doi:
Full Text: [PDF 138 KB] (698)
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STRUCTURE STABILITY OF ROCK MASS ENGINEERING

ZHOU Weiyuan
 2010, 29 (09): -1753 doi:
Full Text: [PDF 803 KB] (1571)
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Firstly,the significances of rock structure and stability are introduced. Then,the methods to calculate limit bearing capacity for structure stability are presented. Finally,the basic problems on geotechnical stability,the constitutive relations and their positive-definition relations are studied. So far,the finite element method(FEM) for geotechnical structure stability could not obtain its exact solutions. However,by means of energy criteria,surplus-force reinforcement method and potential energy criteria,the solutions for engineering stability can be reasonably achieved. The following items could be preceded by FEM:limit load analysis in terms of structure failure and material failure,limit analysis of upper bound load and lower bound load of structures,nonlinear analysis of structure behaviors. The FEM is emphasized on how to solve structure stability problems for engineering projects,and on how to use energy criteria to problems of stability study for large-scale dam projects,and they could be optimized,through the context,from theory to practice. The real engineering problems are illustrated that are encountered in dam constructions during the last 40 years,and factors of safety gained from geomechanical rupture tests and rupture processes are submitted. With the corresponding achieved numerical analytical results,their factors of safety are reasonably cited in related codes or specifications. The results from these studies show that the large-scale dams in China have undergone the above-mentioned simulations,and their results are primarily verified with practical cases. Almost all of the dams are now under control and they are safe and stable.

FOUR CRITERIA OF STABILITY ANALYSIS AND ASSESSMENT OF HIGH ROCK SLOPE

LI Ning1,2,QIAN Qihu3
 2010, 29 (09): -1759 doi:
Full Text: [PDF 537 KB] (1363)
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For high rock slopes,the mechanical parameters on the potential sliding surface,the reinforcement forces needed after slope excavation,and the correlation between the calculated factor of safety and actual safety margin will directly influence engineering safety and economy. Based on back analysis methods for determining mechanical parameters of potential sliding plane and their shortcomings,the minimum value criterion of mechanical parameter selection is proposed;and the maximum reinforcement force criterion is then proposed on the basis of the equivalence of the largest reinforcement force needed and the weight of excavated rock body. Finally,the upper and lower limit criteria of the numerical results used for stability analysis and assessment are put forward and applied to engineering design based on PAN Jiazheng¢s upper and lower limit theory. It will helpfully provide designers with criteria of slope stability analysis and assessment on reinforcement scheme selection of high rock slope.

DISCUSSION ON CALCULATION METHOD OF SLOPE ROCK-SOIL LATERAL PRESSURE BASED ON FACTOR OF SAFETY WITH STRENGTH REDUCTION

ZHAO Shangyi1,ZHENG Yingren1,WANG Jianhua2,TANG Qiuyuan2
 2010, 29 (09): -1766 doi:
Full Text: [PDF 230 KB] (1104)
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The calculation method of slope rock-soil pressure is discussed. The calculation method of slope lateral pressure in the “Technical code for building slope engineering”(GB50330–2002) is not reasonable because it does not take into account the factor of safety of slope stability. The calculation factor of safety in the imbalance thrust force method is not the true stability factor of safety in reinforced slope. Thus,a new slope thrust calculation method based on the strength reduction is presented. The slope lateral pressure and imbalance thrust force can be carried out through strength reduction. In accordance with this method,the stability factor of safety of reinforced slope is equal to the factor of safety of slope thrust calculation. Analysis and comparison of the imbalance thrust force method and strength reduction method are also discussed. Through a series of case studies,the applicability of the proposed method is clearly exhibited.

ANALYTICAL SOLUTION TO TEMPERATURE FIELDS OF TUNNEL IN COLD REGION CONSIDERING LINING AND INSULATION LAYER

XIA Caichu1,2,ZHANG Guozhu1,2,XIAO Suguang1,2
 2010, 29 (09): -1773 doi:
Full Text: [PDF 291 KB] (1134)
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The problem of time-dependent heat conduction for tunnel in cold region with nonhomogeneous outer boundary conduction is transformed into both transient heat conduction with convection boundary condition of air temperature changed with sinusoid and steady heat conduction. Using the separation of variables and Laplace transform technique can obtain analytical solution to temperature fields of tunnel with insulation layer in cold region. The analytical solutions of the annual mean temperature and temperature amplitude can be obtained by energy conservation and experiential method considering heat conduction/convection between the tunnel ground and the air flow in the tunnel. Temperature of lining varies with both tunnel depth and annual mean temperature linearly. When the annual mean temperature is below 0 ℃ and the tunnel depth is less than 80 m,5 cm thick insulation layer alone can not satisfy the anti-freezing requirements. As the increase in thickness of insulation layer,lining temperature presents an upward trend,but the growth rate has gradually decreased;when the thickness of insulation layer is more than 5 cm,the increase in the thickness of insulation to improve the lining temperature is not economical. The insulation thickness can be calculated by engineering analogy and analytical solution based on climate and terrain conditions with piecewise calculation. Accuracy of the analytical solution is examined by comparing the calculated results with measured results. It is found that the calculated values agree well with those measured in the field.

NUMERICAL ANALYSIS OF INFLUENCE OF STRESS-DILATANCY DEPENDENCE OF POROSITY ON THERMO-GAS-MECHANICAL COUPLING IN CO2 INJECTION IN STRATUM

ZHANG Yujun,ZHANG Weiqing
 2010, 29 (09): -1781 doi:
Full Text: [PDF 283 KB] (1013)
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Introducing the existing empirical relationships into a coupled thermo-gas-mechanical model,the porosity and the permeability of rock mass are regarded as functions of mean effective stress and volumetric strain resulted from shear dilation;and a corresponding two-dimensional finite element code is developed. Taking an assumed geological storage system consisted of an under-part reservoir and an upper-part caprock as an analytic object,the numerical simulation of the coupled thermo-gas-mechanical process in the rock mass during CO2 injection is conducted under three cases of different porosities and permeabilities. The calculation results show that the distributions and changes in porosities,pore air pressures,displacements,stresses,zones of tensile and shear failure in the rock mass are obviously different in three cases. Therefore,it is more accurate to consider porosity and permeability of rock as functions of stress,especially reckoning in the effect of volumetric strain resulted from shear dilation than to consider them as constants.

FAILURE PROBABILITY AND STRENGTH SIZE EFFECT OF QUASI-BRITTLE MATERIALS

ZHANG Ming,LU Yujie,YANG Qiang
 2010, 29 (09): -1789 doi:
Full Text: [PDF 263 KB] (1290)
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The failure probability and the average strength of quasi-brittle materials such as rock,concrete,etc.,have size effect due to the heterogeneity,and the statistical approach is of importance in the research of this problem. A statistical model for the strength size effect is established based on the weakest link model and the Poisson¢s distribution of defects during the failure process of materials. The general expressions of the failure probability and the strength size effect are derived for the case of uniaxial compression. From these expressions,it is known that,with respect to volume,the failure probability is monotonically increasing and the strength is monotonically decreasing. The strength varies very slowly and thus may be regarded as constant when the volume becomes very large within usual limited scope. As for defect-free perfect materials,the issue of size effect does not longer exist. The Weibull distribution and the lognormal distribution are then introduced into the general expressions,respectively. The applicability of these expressions is demonstrated with the results of some typical uniaxial compressive strength tests of eight kinds of rocks. It can be found that the two distributions are able to describe the size effect of quasi-brittle materials,with less strength given by using Weibull distribution at the same volume. The difference between the strengths from these two distributions is somewhat slight when the specimen volume is near the reference volume. The expression using the lognormal distribution can give more accurate strengths throughout the volume range,which is valuable in the strength evaluation through indoor test with small specimens. It is also concluded that the lognormal distribution can be used in the research of strength size effect by statistical approach as a simple improvement of the classical Weibull size effect theory.

TRANSMISSION ATTRIBUTES OF BLASTING SEISMIC WAVE IN INTERFACE AND JUDGEMENT OF INTERFACE OBLIQUITY

WANG Guanshi1,HU Shili1,LI Guirong1,LI Shihai2
 2010, 29 (09): -1798 doi:
Full Text: [PDF 370 KB] (1016)
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Seismic waves are converted into two different types of transmission waves such as P wave and SV wave when seismic wave oblique incident goes through the rock mass interface. At the same time,wave field polarity is altered by rock mass interface. The non-filling interface is simplified as a spring model. Propagation characteristics of blasting seismic wave are analyzed by the spring model. The results show that interface stiffness and the variation of incidence angle can be effectively reflected by waveform transformation of seismic wave in interface and variation of the ratio of peak amplitude values between P wave and SV wave and variation of polarization angle. The ratio of peak values between P wave and SV wave and polarization angle can be calculated by analyzing the field test results. The relationship between polarization angle and incidence angle and transmission coefficient of interface is studied. Interface obliquity can be calculated by analyzing the ratio of peak amplitude values between P wave and SV wave and variation of polarization angle of different survey points that are obtained by field experiment. The field experiment and theoretical results indicate that interface obliquity can be determined by the ratio of peak values between P wave and SV wave and variation of polarization angle at different survey points.

APPLICATION OF NON-THICKNESS THREE-NODE JOINT ELEMENT TO CRACK PROPAGATION SIMULATION

QI Jinghua,ZHANG Zhennan,GE Xiurun,QIU Yiping
 2010, 29 (09): -1806 doi:
Full Text: [PDF 2335 KB] (1197)
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It is difficult to describe the thickness of joint with a constant in practical engineering. In order to model the mechanical behaviors of joints conveniently,a non-thickness three-node joint element is proposed on the basis of the existed three-node joint element;and the stiffness matrix of non-thickness three-node element is deduced. For it shares the same nodes with original three-node triangle element,the non-thickness three-node joint element is adopted to model crack propagation without remeshing or adjustment of the original mesh. Another advantage is that the cracked body is meshed without considering its geometry integrity and the existence of joints or pre-existed crack in the procedure of mesh generation;and then the triangular element intersected by crack or joint is automatically transformed into the three-node joint element to represent pre-existed cracks. These make the numerical simulation of crack propagation highly convenient and efficient. After the maximum strain failure criterion is chosen to determine whether the element is intersected by the extended crack or not,the extended crack is located in the model based on hypothesis of the direction of crack propagation perpendicular to the direction of the extended crack passing through the centroid of the triangle element. By simulating the marble plates with double parallel cracks subjected to uniaxial compressive loads,it is shown that the simulated results are in good agreement with the experimental results,so as to show that the present method is valid and feasible in rock crack propagation simulation.

EXPERIMENTAL RESEARCH ON MECHANICAL PROPERTIES OF DEEP-BURIED MARBLE UNDER DIFFERENT UNLOADING RATES OF CONFINING PRESSURES

QIU Shili,FENG Xiating,ZHANG Chuanqing,ZHOU Hui,SUN Feng
 2010, 29 (09): -1817 doi:
Full Text: [PDF 473 KB] (1606)
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In order to understand exactly the influence of unloading rate on mechanical properties of rock,the unloading confining pressure tests under different unloading rates are carried out,which use new loading path and operation method. Thus the disadvantageous effect on test process of the results is reduced. And the deep-buried marble samples cored from Jinping II hydropower station are tested. Based on a new description variable presented as strain-pressure compliance,the influences of the unloading confining pressure path are analyzed on the axial and volume deformations and strengths. The results indicate that the unloading rates of the confining pressure have significant influence on the deformation of Jinping marble,and the initial confining pressure levels mainly control the corresponding influence rules. There are obvious differences in the dilatant processes between the unloading confining pressure tests and triaxial compression tests. In unloading confining pressure tests,the limited bearing loads under the range of unloading rates between 0.01 MPa/s and 1.0 MPa/s are higher than those in the conventional triaxial compression tests under the loading rate of 0.5 MPa/s. Limited bearing capacity increases along with the rise of unloading rates,and increases 10%–15% at the rate of 1.0 MPa/s.

SEISMIC MULTI-FRACTAL CHARACTERISTICS IN MINES AND SEISMICITY PREDICTION

TANG Lizhong1,2,K. W. XIA2,LI Xibing1
 2010, 29 (09): -1824 doi:
Full Text: [PDF 274 KB] (1001)
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The characteristics of the fractal of seismicity in mines play an important role in the establishment of a nonlinear dynamics of seismicity in mines for prediction of seismicity. With seismic data detected in Dongguashan Copper mine,the fractal dimensions of spatial distributions of seismic hypocenters were calculated in the generalized correlation integral,and the fractal dimensions of energy of seismic events were calculated in the relation between b-values in the Gutenberg-Richter law. The fractal structures of seismicity in the mine and their temporal spectra were researched by means of multi-fractal theory,combining with the mining activities and mining engineering structures. The results show that seismicity in the mine has multi-fractal,and the heterogeneity of fractal structure of seismicity is of mining activity and engineering structure. Only if the fractal structure of seismicity in a space for fractal calculation is relative homogeneous,its fractal dimensions can be adopted to effectively predict seismicity. This space for the fractal calculation generally has few sorts of mining activities and simplex engineering structure,and the fractal dimensions of spatial distribution of seismic epicenters reflect the state of the induced seismicity. The temporal spectrum has an obvious precursor of main shock and is suitable for seismicity prediction,but the has no obvious precursor of main shock and is not suitable for seismicity prediction.

EXPERIMENTAL RESEARCH ON DYNAMIC RESPONSE OF CONSEQUENT ROCK SLOPE UNDER SEISMIC LOADING


AI Chang1,FENG Chun1,LI Shihai1,ZHAO Anping2
 2010, 29 (09): -1832 doi:
Full Text: [PDF 621 KB] (1056)
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Based on the similarity theory,a mechanical model of consequent rock slope is established. The design idea and method of the explosion model test are introduced. Using detonating cord as the explosive sources,the deformation and breakage pattern of the archetype slope under near field seismic loading are studied and the effects of the retaining structure are estimated with underwater explosion model test. The test results show that the major deformation pattern of consequent rock slope near field seismic is interlayer sliding in jointed rock mass. The breakage pattern is sliding and fracturing caused by elastic wave. The distribution of the peak compressive stress of the gravity retaining wall is changed in different heights and presents bell-shaped distribution,which increases at first and then decreases. Test results and the in-situ investigation in Wenchuan after earthquake show that the retaining structures play an important role in the stability of slope.

STUDY OF DISTRIBUTION FEATURES OF STRESS REDUCTION COEFFICIENT IN LIQUEFACTION EVALUATION

HAN Chao1,2,ZHOU Yanguo1,2,LING Daosheng1,2,CHEN Yunmin1,2
 2010, 29 (09): -1839 doi:
Full Text: [PDF 387 KB] (990)
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To investigate the distribution features of rd under different types of excitations,firstly FLAC3D is used to calibrate the results of dynamic centrifuge tests on saturated sand;and then the validated numerical model is used to study the variation of rd curves with soil depth under seismic and harmonic excitations. The results show that the proposed empirical equation of rd is fairly accurate in non-liquefied cases;whereas larger differences exist between the distribution of shear stresses and the predicted values by empirical equation in liquefied cases. Besides,the duration of seismic excitation also influences rd,where the generation level of pore water pressure and the softening degree of soil are major factors. As for the effect of seismic input frequency,it is closely related to the predominant frequency of the site;i.e. the closer the two frequencies become,the more drastic the variation of rd curve is. Therefore,the effects of seismic motion and site conditions should be considered when the Seed-Idriss equation is used to calculate CSR in liquefaction evaluation.

GLOBAL STABILITY ANALYSIS OF SLOPE BASED ON DECISION- MAKING MODEL OF MULTI-ATTRIBUTE AND INTERVAL NUMBER

XU Xinghua,SHANG Yuequan,WANG Yingchao
 2010, 29 (09): -1849 doi:
Full Text: [PDF 608 KB] (1018)
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In order to study the status of global stability of a slope,the decision-making model of multi-attribute and interval number is constructed to carry out global stability analysis of slope. With this method,the research process can be realized. According to the actual geological conditions and the situation of engineering sections of Guanjia slope,the set of influence factors and research objects are established,and the decision-making model of multi-attribute and interval number is adopted,and the safe and stable states of slope are back analyzed. Moreover,the macroscopic signs of slope failure are referenced to perform comparison and verification. The research results show that through the model solution,the interval of global stability factor which can characterize the changing situation of global stability of slope ranges from 0.927 to 1.032,and the probability of sliding instability or failure is up to 70%. The slope,which has poor global stability and low safety level,is in an unstable state,and the tread of deformation expansion and sliding instability is obvious. In addition,the current active state of slope indicates that it has high possibility of sliding instability or failure. In order to maintain safety,stability and reliability of slope,it is noted that comprehensive treatment should be carried out for the slope. Thus it is shown that the decision-making model of multi-attribute and interval number can provide a feasible technical platform for state feedback and prevention countermeasures of slope disaster,which has positive guiding significance.

STRONG MOTION RECORDS OF WENCHUAN Ms8.0 EARTHQUAKE FROM DIGITAL STRONG EARTHQUAKE NETWORKS IN SICHUAN AND ITS NEIGHBOURING REGIONS

 2010, 29 (09): -1858
Full Text: [PDF 844 KB] (1218)
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The thrust-dextral slip motion of Longmenshan tectonic belt resulted in Wenchuan Ms8.0 earthquake occurred on May 12,2008. 133 groups of three-component acceleration records were collected by digital strong earthquake networks in Sichuan Province. By using these original records and some strong motion records from digital strong earthquake networks in Shaanxi and Gansu provinces,the contour lines of acceleration peak values were drawn;and they show that the anomalistic ellipse-shaped contour lines of acceleration peak values along the long axis in NE direction conform to the distribution of earthquake response intensity. The attenuation of the acceleration records shows obvious directivity effect and hanging wall effect;i.e. the peak acceleration decayed relatively slower in NE direction of the rupture propagation than in SW direction. The attenuation of peak acceleration also decayed slower on the fault hanging wall in NW direction than that in SE direction;the systemic relative higher phenomenon of the peak acceleration attenuation was more remarkable in Yingxiu—Beichuan section of the causative fault;and it can be relative to fracture pattern and progress of seismic source. Another phenomenon is that the ratio of vertical peak ground value to horizontal one near the causative fault is obviously higher than that in the seismic far-field;and the ratio is about 1.0 near the faults,which is great different with the 2/3 from Code for seismic design of buildings(GB50011–2001). Furthermore,with fault distance increasing,the peak acceleration gradually shifted to the long-period in the acceleration response spectrum,which is more obvious beyond a distance of 200 km to the causative faults;but in the near-fault distance of 100 km,there is a large velocity pulse.

(1. College of Mining Technology,Taiyuan University of Technology,Taiyuan,Shanxi 030024,China;2. Institute of Mining Technology,Taiyuan University of Technology,Taiyuan,Shanxi 030024,China)
 2010, 29 (09): -1866
Full Text: [PDF 322 KB] (974)
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Great changes in pore structure and quantity of coal may occur as the pyrolysis temperature rises. To study the change laws,a mercury intrusion method was adopted to measure and analyze the pore structure parameters of the solid products of flame coal pyrolysis,which were generated in vacuum system with temperatures from 300 ℃ to 600 ℃ and in high temperature steam state at 600 ℃;the pore fractal dimensions were calculated under different temperatures;and pore properties of solid products under two different pyrolysis ways were compared. The results indicate that:(1) Under conventional pyrolysis,the total pore volume and porosity of Heidaigou coal decreased from 300 ℃ to 400 ℃ and increased from 400 ℃ to 600 ℃;the increasing rate is the greatest from 500 ℃ to 600 ℃;the specific surface area increased progressively from 300 ℃ to 600 ℃. But for Zichang coal,the total pore volume and porosity increased from 300 ℃ to 400 ℃ and then decreased from 400 ℃ to 500 ℃ and increased from 500 ℃ to 600 ℃;the increasing rate is the greatest from 300 ℃ to 400 ℃;the specific surface area decreased progressively from 300℃ to 600 ℃. (2) Under conventional pyrolysis,large pores were the major parts of pore volume,micropore and transition pore were the major parts of the specific surface area. (3) Under high temperature steam pyrolysis,the large pores were the major parts of pore volume;the proportion of large pores of Zichang coal was 99.91%;micropores and transition pores were the major parts of the specific surface area of Heidaigou coal;the large pores were the major parts of specific surface area of Zichang coal. (4) Compared with conventional pyrolysis,the permeability of solid products of high temperature steam pyrolysis was greater;and compared with inert gas injection,it is the best method in the coal situ-pyrolysis application. These results can provide a scientific basis and theoretical guidance for the issue that coal pore structure changes with temperature during coal situ-pyrolysis.

DEFORMATION PREDICTION OF ADJACENT PIPELINE DUE TO NON-UNIFORM CONVERGENCE OF SHIELD TUNNELLING IN LAYERED SOILS

ZHANG Zhiguo1,2,3,HUANG Maosong2,ZHANG Mengxi1,WANG Weidong4
 2010, 29 (09): -1876
Full Text: [PDF 412 KB] (787)
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The elastic layered soil model is adopted to consider the soil non-homogeneous characters. The oval- shaped soil deformation model is imposed to the tunnel opening boundaries,and the boundary element method based on displacement-controlled technique is presented to analyze the free soil displacement. The displacement- controlled method is put forward to predict the deformation of adjacent pipeline due to non-uniform convergence of shield tunnelling in multi-layered soils. The accuracy of the proposed method is demonstrated with the displacement-controlled finite element numerical analysis and existing centrifuge model tests. The results indicate that the solution of the free soil deformation is rather important to estimate the effects on adjacent pipeline. It is also shown that the soil non-homogeneity,neglected in previous methods,has a significant influence on the deformation behaviors of municipal pipelines induced by tunnelling in multi-layered soils. The proposed method may provide a theoretical basis for proposing correctly protective measurements of existing pipelines influenced by adjacent underground construction.

NUMERICAL SIMULATION OF SHRUB ROOTS FOR SLOPE PROTECTION EFFECTS ON LOESS AREA OF NORTHEAST QINGHAI—TIBETAN PLATEAU

LI Guorong1,HU Xiasong1,MAO Xiaoqing2,ZHU Haili1,NI Sanchuan1,QIAO Na1, YU Qinqin1,CHEN Guichen3
 2010, 29 (09): -1884
Full Text: [PDF 296 KB] (1051)
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To study the relationship between shrub roots and slope stability in loess area of northeast Qinghai— Tibetan plateau,four shrubs Caragana korshinskii,Atriplex canescens,Zygophyllum xanthoxylon and Nitraria tangutorum were planted on the slopes of the test area in Xining basin. The mechanical strength tests of root-soil composite systems were carried out and the increasing effect of slope stability of four two-year growth shrubs were simulated with two-dimensional finite element method. The results show that the horizontal and vertical displacements of four shrubs root-soil composite systems are obviously smaller than those of soil without roots. The order of four two-year growth period shrubs in the course of deformation in magnitude is Caragana korshinskii,Atriplex canescens,Zygophyllum xanthoxylon and Nitraria tangutorum. Lateral roots and main roots of shrubs play a part in reinforcement and anchorage in the soil,which increase the shear strength and the cohesion of the soil,thus the plastic area and the shearing stress concentration area can be reduced. The results of factors of safety of the slope in the testing area show that,compared with the safety factor of soil without roots,the increments of the safety factor of the related slope of the four shrubs root-soil composite systems of the four shrubs are 80.5%(Atriplex canescens),48.7%(Caragana korshinskii),22.1%(Zygophyllum xanthoxylon) and 8.0%(Nitraria tangutorum),respectively. The achievements can be taken as criteria for choosing shrubs for protecting slope and preventing shallow landslide,collapsing and debris flow in loess area of northeast Qinghai—Tibetan plateau.

FAILURE CRITERION OF ANISOTROPIC SAND WITH METHOD OF MACRO-MESO INCORPORATION

LI Xuefeng1,2,HUANG Maosong1,2,QIAN Jiangu1,2
 2010, 29 (09): -1892
Full Text: [PDF 315 KB] (1114)
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With the method of macro-meso incorporation,a failure criterion of anisotropic sand is proposed. A new anisotropic state variable is properly defined by two invariables of a joint tensor combined by loading direction tensor and fabric tensor from the mesoscopic point of view;then a failure criterion of anisotropic sand is put forward by introducing the new anisotropy state variable into macroscopic equation. In view of the relationship between fabric and stress state,the proposed criterion not only can describe the effect of mesostructure on material anisotropy under conditions of non-rotating and rotating stresses,but also has the clear physical significance parameters. Verifying the proposed criterion with a series of experimental data,the results show that the effects of mesostructure on anisotropic strength and peak friction angle are well captured by the proposed criterion under three-dimensional condition;and the adaptability and validity of the method can be confirmed from the comparison and analysis of calculated results.

STUDY OF MECHANICAL BEHAVIORS OF INTERFACE BETWEEN COARSE-GRAINED SOIL AND CONCRETE BY SIMPLE SHEAR TEST

PENG Kai1,2,ZHU Jungao1,2,ZHANG Dan3,WU Xiaoyu3
 2010, 29 (09): -1900
Full Text: [PDF 270 KB] (1244)
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The mechanical behaviors of interface between coarse-grained soil and concrete were investigated by simple shear tests with both bentonite slurry and mixed soil slurry(bentonite mixed with cement grout). In addition,the mechanical behaviors of interface were analyzed with different slurries. The results show that the relation curves between shear stress and shear strain exist strain softening,and strain hardening appears with bentonite slurry or without slurry,when mixed soil slurry exists;and the position of peak strength is mainly related to normal stress and cement content. The more the cement content is,the larger the strength becomes. The value of friction angle with 40 percent cement grouts is 3.2 times higher than that with 10 percent cement grouts,the strength accounts for 84 percent of the interface strength without slurry. The shear displacement increases with increasing normal stress and cement content at the same height in shear failure state. Shear dilatation is significant when the surface without slurry in small normal stress state,while shear contraction is significant with the bentonite slurry and the mixted soil slurry. Compared the sample with height of 100 mm to that with height of 30 mm,the errors of friction angle and horizontal displacement are about 3% and 6%,respectively,when the maximum grain size is 20 mm,which shows that the height of sample affects the strength and deformation to some extent. In addition,the friction angle reduces by 4.8%,i.e. 1.9°,compared to the maximum grain size of 60 mm.

STUDY OF EQUIVALENT SUCTION OF UNSATURATED LOESS

HU Zaiqiang,LIU Lanlan,LI Hongru,JIAO Lijie,WANG Junxing
 2010, 29 (09): -1906
Full Text: [PDF 246 KB] (824)
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As an essential portion of basic framework of soil mechanics,strength theory of saturated soils has been well developed and widely used in geotechnical engineering. However,unsaturated soils have a wide distribution and display more complex behaviours compared with saturated soils in engineering practice. Until now the research activities in the field of unsaturated soils have been still in the academic stage because of the difficulty of suction measurement. To solve this problem,the equivalent suction has been proposed and validated recently. Based on the principle of equivalence of deformation and the stress-strain curves obtained from triaxial compression tests of intact saturated and unsaturated loess,a determination method of equivalent suction is proposed. The nonlinear relationship formula between equivalent suction and degree of saturation is proposed;and the correctness of this exponential function relationship is verified. Based on testing results,the influence of water content on shear strength is analyzed;and shear strength formula of unsaturated soils is established. It provides a new feasible method for application of unsaturated soil theory to engineering practice.

DENSITY-SATURATION-DEPENDENT AIR-WATER PERMEABILITY FUNCTION OF UNSATURATED LOESS

LIU Fengyin1,ZHANG Zhao1,ZHOU Dong2
 2010, 29 (09): -1914
Full Text: [PDF 238 KB] (868)
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The coefficient of permeability of unsaturated soil is a key parameter in performing seepage analysis in saturated/unsaturated soils. However,both the degree of saturation and the dry density influence the coefficient of permeability of unsaturated soil. A series of experiments are performed by using the improved measurement apparatus under different infiltration steps and various initial dry densities of unsaturated remoulded loess specimens. According to the results,the relationships among degree of saturation,dry density,coefficients of air and water permeability are analyzed. A new density-saturation-dependent air-water permeability function is put forward based on the above relationships;and it can not only determine the coefficient of water permeability but also quantitatively describe the mutual influence of movement of both air and water in the void of unsaturated soil. Finally,the new experiment is provided to verify the proposed permeability function. It is shown that the predicted curves are in good accordance with the experimental data.

FORMATION MECHANISM AND NUMERICAL SIMULATION OF LONGITUDINAL CRACKS IN WETLAND SECTION OF QINGHAI—TIBET HIGHWAY

MAO Xuesong,HOU Zhongjie,WANG Weina,LU Lu
 2010, 29 (09): -1921
Full Text: [PDF 336 KB] (865)
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To understand the formation mechanism of longitudinal crack of Qinghai—Tibet highway in permafrost region,the mechanical model of longitudinal cracks in subgrade is constructed during freezing and thawing processes by numerical simulation,based on the in-situ observation of thick ice layer in the cross-section K3020+200 and the testing data of temperature field in the cross-section K3016+000. The formation process of thick pure ice layer under road shoulder and its effect on subgrade stability are analyzed. The observation in the cross-section K3020+200 shows that the thick pure ice layer exists under road shoulder and natural ground surface. The time-history curves of ground temperature at different depths in the cross-section K3016+000 show that the change in ground temperature is larger near the ground surface;the change in temperature in subgrade lags behind that at ground surface;the upper limits of permafrost at road shoulder and slope toe decrease by ground surface water infiltration from road shoulder,slope and slope toe,i.e. the distribution of upper limits presents arch shape. The results show that the infiltration of ground surface water leads directly to the formation of thick pure ice layer;the formation and thawing of thick pure ice layer are immediate causes of nonuniform deformation of subgrade and formation of longitudinal cracks.

ANALYSIS OF VERTICAL VIBRATIONS OF A RIGID FOUNDATION RESTING ON SATURATED POROELASTIC HALF-SPACE SUBJECTED TO INCIDENT PLANE WAVES

WANG Peng1,CAI Yuanqiang1,2,ZENG Chen1
 2010, 29 (09): -1928
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An investigation is put into the vertical dynamic responses of a rigid circular foundation on the poroelastic soil excited by incident fast P1 waves and SV waves. The radiation field and rigid-body scattering field are introduced in order to consider the dynamic interaction between the foundation and the underlying soil,as well as the scattering phenomena caused by the existence of the foundation. The motion of the soil is supposed to be governed by Biot¢s dynamic poroelastic theory,while the boundary conditions along the contact surface between the soil and the bottom of the foundation are assumed to be perfectly bonded for the skeleton and hydraulically drained for the fluid. Combining with the mixed boundary-value condition and the dynamic equilibrium equation of the foundation,the expression of the vertical dynamic amplitude of the foundation,subjected to the incident plane waves,is obtained by solving the control equations using Hankel integral transforms. The influences of incident angle,the mass of the foundation and the permeability of the soil on the vertical vibrations of the foundation are thus determined through numerical simulations. Significant differences are found between the responses of the foundation,which is excited by fast P1 waves and SV waves,respectively.

FIELD TEST STUDY OF REINFORCED EMBANKMENT SUPPORTED BY CAST-IN-SITU THIN-WALL TUBULAR PILES

XIA Tangdai1,2,WANG Mei1,2,SHOU Xuan1,2,WU Ming3,4,5
 2010, 29 (09): -1936
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To validate the working mechanism of reinforced embankment supported by cast-in-situ thin-wall tubular piles,field test has been performed in a highway section from Jiujiang to Xiaotang around Guangzhou City. Test results show that tubular pile has a large vertical bearing capacity,and punching failure happens to most piles in static tests. Moreover,the bearing capacity of single tubular pile composite foundation is also large with small settlements. Tests still suggest that soil arching effect and tension membrane effect are the two key factors influencing the load transfer mechanism. The pile-soil stress ratio varies with the embankment loads and differential settlements between piles and soil. The total settlement of tubular pile composite foundation under embankment load is small. Differential settlements are found between soil above pile cap and soil among piles,respectively,and increase of this difference can reflect the degree of soil arching effect. In addition,excess pore water pressure,which is induced by embankment loads,turns up slightly and decreases rapidly along depth. It is nearly zero at the depth of 6.0 m. The lateral deformation of embankment is small,and decreases rapidly along depth;and it reaches its peak value at the depths of 3.0 to 4.5 m.

STUDY OF UNSATURATED COMPACTED SOIL CONSIDERING INFLUENCE OF END EFFECT BY TRIAXIAL TEST

DONG Jianjun1,SHAO Longtan2
 2010, 29 (09): -1944
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In the unsaturated compacted soil triaxial tests under controlled suction conditions,the digital image measurement technique is used,with which the strength and deformation behaviours of unsaturated compacted soil can be studied by considering the influence of end effect. The comparison of test results of the overall specimen and 1/3 zone in the middle of specimen under controlled suction reflects that end effect has a little influence on 1/3 zone in the middle of specimen;the test result of this part can better stand for the actual deformation properties of unsaturated soil;and it provides credible test data for the study of unsaturated soil stress-strain relationship. The end effect has great influence on parameters of shear strength formula,when using the double-stress state variable method to analyze the shear strength. The elastoplastic model of Alonso for unsaturated soil is adopted to further analyze the influence of end effect on numerical calculation.

 2010, 29 (09): -1946
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 2010, 29 (09): -1948
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