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  --2005, 24 (17)   Published: 01 September 2005
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2005-17期目录

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 2005, 24 (17): -3002 doi:
Full Text: [PDF 71 KB] (769)
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2005-17期目录

CRITERIA FOR STRENGTH AND STRUCTURAL FAILURE OF ROCKS BASED ON ENERGY DISSIPATION AND ENERGY RELEASE PRINCIPLES BASED ON ENERGY DISSIPATION AND ENERGY RELEASE PRINCIPLES

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 2005, 24 (17): -3010 doi:
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The intrinsic relations between energy dissipation,energy release,and strength and abrupt structural failure of rocks during failure process are discussed. It is emphasized that the failure of rock is a process in which energy dissipation and energy release occur simultaneously. The energy,part of work done by external forces,dissipates to produce damage and irreversible deformation inside rock and makes the material deteriorate and its strength drop down eventually. The strain energy released in rock volume plays the pivotal role of abrupt structural failure of rock. The concepts of energy dissipation,energy release,strength loss and abrupt structural failure of rock are defined. On the basis of these concepts,the criteria for strength and abrupt structural failure of rock are proposed. The critical stresses at the time of abrupt structural failure of rock under various stress states can be determined by these principles. The energy criteria have been applied to analyzing the failure condition of surrounding rock masses of a circular tunnel in practice.

CONSTITUTIVE MODEL OF SATURATED-UNSATURATED CLAY AND ITS NUMERICAL SIMULATION

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 2005, 24 (17): -3016 doi:
Full Text: [PDF 109 KB] (2248)
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Based on laboratory data of unsaturated flow in clay,the constitutive model of unsaturated flow coupled model for clay considering plastic strain hardening and Hoek-Brown model is applied to simulate the swelling and shrinking behavior of clay shaft during excavation,concrete lining stage and long time ventilation. With the help of numerical simulation,the flow process in clay from initial saturated to desaturated and then to resaturated is stated. Furthermore,the sensitivity analysis of Biot coefficient,capillary pressure and water relative permeability with saturation degree is discussed;and the results show that the hydraulic parameters have effects on unsaturated zone in surrounding rock mass,especially the water relative permeability,while the mechanical behavior of clay has low effect on unsaturated flow law in surrounding rock mass.

THEORY AND METHOD ON LIFE DIAGNOSIS IN IMPORTANT HYDRAULIC ENGINEERINGS

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 2005, 24 (17): -3022 doi:
Full Text: [PDF 56 KB] (1489)
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Some hydraulic engineerings have serious hidden troubles or lose their function. By absorbing advanced theories and methods from America etc.,and combining the features in China,the theory system on life diagnosis is put forward for the important hydraulic engineerings. This system includes three rules,namely safety rule,engineering benefit rule,ecology and environment rule. Based on the above rules,this paper proposes the theories,methods and technologies on life diagnosis for the important hydraulic engineerings.

PARALLEL FINITE ELEMENT ANALYSIS BASED ON ELEMENT-BY-ELEMENT METHOD AND ITS APPLICATION

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 2005, 24 (17): -3028 doi:
Full Text: [PDF 111 KB] (1425)
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In 3D finite element analysis of structure failure process,large scale numerical analysis has increased the demand for high-performance computing. The element-by-element(EBE) method for distributed memory processors(DMP) is formulated based on the Jacobi-preconditioned conjugate gradient(J-PCG) method. For data exchange,a scheme which only gathers and scatters necessary data is advised to make EBE method available for distributed-memory parallel computers. In this way,it will dramatically reduce data exchange and consequently improve efficiency of parallel computing. At the same time,the formation of global stiffness matrix can be avoided;greatly reducing the requirement for the storage,and the assignment of jobs can be done automatically. A 3D parallel finite element code is developed using MPICH and C/C++ language. Numerical tests on cantilever beam indicate that they are correct. Then it is applied to the finite element analysis of Xiluodu arch dam project and numerical analysis of fracture process of four-point shear test based on grid refining technology. It is the same in essence for EBE method and domain decomposition in task allocation. The results show that for the analysis of the 3D irregular and complicated structures like arch dams,the finite element EBE method is effective and reliable

PARAMETER IDENTIFICATION OF CONSTITUTIVE MODEL FOR HARD ROCK UNDER HIGH IN-SITU STRESS CONDITION USING PARTICLE SWARM OPTIMIZATION ALGORITHM

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 2005, 24 (17): -3034 doi:
Full Text: [PDF 113 KB] (1723)
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Particle swarm optimization (PSO) algorithm is a stochastic global optimization technique and has become the hotspot of evolutionary computation because of its excellent performance and simplicity for implementation. In light of the fact that it is hard to determine the parameters of a constitutive model—cohesion weakening and frictional strengthening (CWFS) model,which performs excellently in modeling the extent and depth of brittle failure zone for hard rock under high in-situ stress condition,a new method is presented to identify parameters of CWFS model using PSO. At first,the stochastic values of parameters are initialized and the difference in failure zone between the value computed and the datum measured is regarded as fitness value to evaluate quality of the parameters. Then the parameters are updated continually using PSO until the optimal parameters are found. Thus parameters are identified adaptively during computation. The results of applications to two real tunnels,i.e.,Mine-by tunnel in Canada and Taipingyi tunnel in China,show that the method is feasible and efficient for identifying constitutive parameters and predicting the extent and depth of brittle failure of hard rock under high in-situ stress condition with high precision.

COLLAPSE SIMULATION AND ANALYSIS OF CYPRESS VIADUCT DURING LOMA PRIETA EARTHQUAKE

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 2005, 24 (17): -3044 doi:
Full Text: [PDF 256 KB] (1366)
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The collapse of the Cypress Viaduct is employed to test the following structural collapse analysis model:a mixed hinge model based on generalized functions is proposed to describe discontinuous displacements;the governing equations are built in the current unstressed configuration;a Lagrange multiplier approach is adopted for the analysis of collisions. After both the viaduct parameters and the ground acceleration recorded at Emeryville are input to the corresponding program,the changing coordinates of each member end during the collapse process are obtained. Visualized clearly by the Visualization of Dynamic Demo Show,the collapse process is consistent with the speculation of the Earthquake Engineering Research Center from UC Berkeley,which proves the validity and utility of the present models. Based on the results,some issues,such as the reason of the collapse,sharp changes of the frame accelerations when collisions happen,and the effects of earthquake lasting times on the weak parts of the structures,are discussed.

2D ELASTOPLASTIC FINITE ELEMENT ANALYSIS FOR COUPLED HYDRO- MECHANICAL PROCESSES IN SATURATED-UNSATURATED MEDIA

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 2005, 24 (17): -3051 doi:
Full Text: [PDF 213 KB] (1101)
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The stress equilibrium equation,the continuity equation for water and the elastoplastic matrix are established. By using the Galerkin method,all the governing equations are discretized in the space domain and time domain respectively;and a two-dimensional FEM code for coupled hydro-mechanical elastoplastic analysis of saturated-unsaturated porous medium is developed. By introducing one set of special computation equations related to the unsaturated state,a numerical computation is carried out for the assumed coupled hydro-mechanical problem in an unsaturated soil body. The displacements,the pore pressures,the effective principal stresses,the flow velocities and the plastic zones at different times in the soil body are investigated;and the validity of the code is tested and verified qualitatively.

RELATIONSHIP BETWEEN LANDSLIDE PROBABILITY AND RAINFALL IN THREE GORGES RESERVOIR AREA

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 2005, 24 (17): -3056 doi:
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The Three Gorges Reservoir area is located at the upper reaches of the Yangtze River,where the geological hazards occur with high frequency,especially the major landslides are fully developed at the bank slopes along the river. These landslides are characterized by great amount,extensive distribution and big magnitude,often causing serious loss and casualty in local areas. How to predict landslides is the key to prevent hazards and reduce economical loss and casualties. The rainfall is the dominant exterior factor triggering the landslides. Based on statistic analysis of the data of 112 landslides(volume≥104 m3),the relationship between landslide and rainfall is derived. It is suggested that the temporal prediction criterion of landslides in the local area be established by the maximum 24-hour rainfall. In terms of the characteristics of landform,lithology,geological structures etc.,the Three Gorges Reservoir area is divided into two parts for landslides prediction. Using the maximum 24-hour rainfall in 72 hours as the prediction index,the occurrence probabilities of landslides are determined in different rainfall conditions for the two subareas. The distinct difference of landslides probabilities between the two subareas indicates that their different mechanism of rainfall induced landslides. Based on the coupling analysis of the geology and meteorology,it is possible to improve the precision of the landslide forecast.

BANK SLOPE TYPES AND ROCK MASS STRUCTURAL FEATURES IN NEW FENGJIE COUNTY,THREE GORGES RESERVOIR REGION

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 2005, 24 (17): -3063 doi:
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After impoundment up to 139 m elevation in the Three Gorges Reservoir in June 2003,many geological hazards were triggered inevitably. Lots of deformation and failure phenomenon on the bank slope are dooming in new Fengjie,a county located on the Yangtze River. The complexity and diversity of deformation and failure modes of the bank slope bring many difficulties to effectively prevent instability of the bank slope and to release the threat to lives. Based on the research on rock and soil sort of the bank slope and its structural characteristics,the bank slope,which is 21.7 km long totally in 175 m elevation,is divided into 21 sections. The sections are researched respectively on the lithology,obliquity,direct relationship between slope and terrain,interrelation of different rocks and soils,and then,they are reduced to 13 structural types. Through detailed field investigation on the characteristics of the 13 structural types of the bank slopes,6 potential deformation and failure patterns are presented,such as bending-cracking-toppling,shearing-sliding,sphenoid falling-sliding and weathering-flake for rock bank slope,cambered sliding and part sliding-falling for gravel-clay bank slope. These 6 possible patterns will provide guidance for choosing proper protection measures so as to maintain stability of the bank slope.

INTELLIGENT INVERSION OF CREEPING PARAMETERS OF LEFT BANK HIGH SLOPE SHALE ROCK MASSES AT LONGTAN HYDROPOWER STATION

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 2005, 24 (17): -3070 doi:
Full Text: [PDF 209 KB] (1427)
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Based on the comprehensive analysis of the creep experimental data of left bank slope shale samples at Longtan Hydropower Station and the weathered degree of rock masses,rock characteristics and joint distribution in local area,a creep model of shale rock masses of the left bank is set up. The uniform design method and FLAC3D are used to simulate the excavation and creeping process on the simplified geological model of the No.72 test-tunnel,which is located in the central portion of the left bank high slope. With the deformation monitoring data of the No.72 test-tunnel as the aim,the intelligent inversion is made for the creeping parameters by way of combined neural network and genetic algorithm. With these parameters,numerical simulation is conducted. Results indicate that the monitoring displacements not used in inversion are similar to the calculated displacements. This reveals the reasonability of the rheology model and parameters of left bank high slope shale rock masses of Longtan Hydropower Station as well as the important bridging function of intelligent displacement back analysis in the process of the transition from creeping experimental parameters of small-scale rock masses to those of the local large-scale rock masses.

STUDY ON EFFECT OF GEOSTRESS ON PERMEABILITY
OF FRACTURED ROCK MASS

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 2005, 24 (17): -3071 doi:
Full Text: [PDF 148 KB] (1457)
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Rock mass always exists in the fields of geostress and seepage,so it is important to study the effect of geostress on the permeability of rock mass. Firstly,the basic rule of seepage in fissured rock mass and the mechanism of the effect are studied. Then the in-situ geostress measurement and high water pressure test are made combining with an engineering project in Gansu Province. Investigations into joints on ground surface and in borehole are done;and the geostress and permeability coefficient of this area are obtained. By nonlinear regression analysis the change law is found that with the increase of geostress the permeability coefficient will decrease with negative exponential trend.

ANALYSIS OF MECHANISM OF ROCK FAILURE DUE TO
FREEZE-THAW CYCLING AND MECHANICAL TESTING
STUDY ON FROZEN-THAWED ROCKS

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 2005, 24 (17): -3076 doi:
Full Text: [PDF 134 KB] (1584)
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The rock failure due to freeze-thaw weathering is a main engineering problem which often occurs in the rock engineering in cold regions. The process of the rock failure due to freezing and thawing and the effect factors are systematically analyzed,also the mechanism of rock failure due to freezing and thawing is studied. The process of freezing and thawing failure of two types of rocks is studied by experiments;and two basic modes of rock deterioration are found;i. e.,the scaling mode and fracturing mode. In addition to providing reliable experimental foundation for studying the damage and fracture due to freezing and thawing,the uniaxial compression tests of two types of rocks subjected to different cycles of freezing and thawing were conducted in room temperature(about 20 ℃);and the fitting relations of the uniaxial compressive strength and elastic modulus respectively with the cycles of freezing and thawing are formulated.

ANALYSIS OF ROCK MASS STABILITY IN TUNNEL AND UNDERGROUND ENGINEERING BASED ON YIELD APPROACH INDEX

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 2005, 24 (17): -3083 doi:
Full Text: [PDF 168 KB] (1399)
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In many cases,it is necessary to realize the importance of the stability discrepancy among the points which are all close to the yield state in the principal stresses space. So the YAI(yield approach index) concept is presented,which denotes the yield approach degree or the difference of the stability of some points in the Haigh-Westergaard space compared with the relative safe point;and the method and rule are provided for the choice of relative safe point. The whole analysis is limited in the frame of plastic theory. This concept allows the possibility of describing the stability state and the progressing transition between stability and instability state of each element or point. So evolution of the stability state of surrounding rock mass in the process of loading can be simulated. The yield approach function is derived out based on the Mohr-Coulomb yield criterion. Finally,a case study is presented to which YAI is applied.

TIME SERIES EVOLUTION MODEL FOR DEFORMATION
MODULUS OF GEOLOGICAL DEFECT

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 2005, 24 (17): -3088 doi:
Full Text: [PDF 95 KB] (932)
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Geological defects existing extensively in foundations often do harms to the safety of buildings. At the same time,construction of large-scale structures leads to variation of the natural geological condition. And in some cases,the geological defects may deteriorate with the construction of structures,which will bring adverse impacts on the normal operation of the buildings. Deformation modulus of the geological defect is a key parameter that reflects its deformation and strength character,so deformation modulus of the geological defect is used to study its evolvement rules. The theory,which is to build time series evolution model for geological defect by use of monitoring data,is presented. Then based on Elman recurrent neural networks,the detailed process to build time series evolution model for geological defect is proposed. The application shows that the proposed method is effective.

CLASSIFIED ANALYSIS OF CSAMT SECTION IN EMBEDDED TUNNEL EXPLORATION AT ABA SECTION OF FIRST STAGE OF WEST LINE PROJECT OF SOUTH-TO-NORTH WATER TRANSFER

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 2005, 24 (17): -3094 doi:
Full Text: [PDF 167 KB] (1266)
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The first stage of the west route project of the South-to-North Water Transfer,which diverts water from the upper Yangtze River into the upper Yellow River,is located in the east edge of Qinghai—Tibet Plateau where the regional geological conditions are very complex. Active faults are distributed over the project zone,and strata are strongly folded. Through CSAMT exploration,the distribution of faults and groundwater are qualitatively analyzed;and the stability of embedded is evaluated. According to regional geology background,sedimentary rock modes and condition and physical features of rocks,the characters of CSAMT section to explore the strata structure,fault and groundwater condition are analyzed. The CSAMT section is classified into 4 types,accounting for 54.75 percent,38.75 percent,3.75 percent,2.75 percent respectively in the 40 kilometer long surveying line. Each mode reflects different geological condition. For type 1 with wide high resistance area,CSAMT section changes sparsely and gradually,r :2 000–10 000 W· m. Type 2,wide low resistance area,CSAMT section also changes sparsely and gradually,but the resistance reduces from the ground surface to deep zone,r :1 000–50 W·m. For type 3 with wide high resistance area,the resistance increases from the ground surface to deep zone,r :50–1 000 W·m. For type 4 with low resistance strip,r<300 W·m. The geological interpretation is that the wide high resistance area(type 1 and type 3 ) reflects that the groundwater is not abundant in the sandrock and slate stratum. The large region of low resistance anomaly(type 2) reflects the hydraulic permeability and water reservoir of deep rocks are better than the superficial rocks. Low resistance anomaly depends on ground water conditions and lithologic characters,not on tectonic movement. Sandrock filled with water may appear low resistance anomaly. According to groundwater condition,when the tunnel is excavated,these low resistance anomaly made of moderate to thick-bedded sandrock may cause water gushing but the amount of water which may affect the safety of tunnel is not much. The low resistance strip (type 4)which reflects fault and its crushed belt will affect the excavation of tunnel.

EFFECTS OF MECHANISM AND RIGIDITY OF FAULT SURFACE
ON STRONG GROUND MOTION

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 2005, 24 (17): -3101 doi:
Full Text: [PDF 163 KB] (1338)
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The distribution of near-fault strong ground motion during Chi-Chi earthquake (Mw7.6) has two remarkable characters:(1) the distribution of horizontal peak acceleration,peak velocity and displacement along the fault is asymmetric and the effect of hanging-wall is distinct;(2) the distribution of acceleration,velocity and displacement are inconsistent. Based on theoretical analysis of focal mechanism and research on medium rigidity of fault,a model of finite source of Chi-Chi earthquake is established;and then the ground motion of the model is simulated. The distribution characteristics of simulation is similar to that of ground motion monitored by instruments. Without considering the site condition,the rigidity of fault surface affects acceleration and velocity value of near-site strong ground motion to some extent,the peak ground acceleration and velocity are respectively in proportional to media rigidity — and . Furthermore,the parameters of focal mechanism,such as dislocation,obliquity,rupture mode,have remarkable influence on distribution of strong ground motion. The uneven distribution of strong ground motion near the source is attributed to the complexity of source by former researchers. But our studies result in a farther conclusion,that the mechanism and rigidity of fault surface are the main factors resulting in uneven distribution of strong ground motion near the source,and the complexity of source has relationship with the mechanism and rigidity of fault surface.

ESTIMATION OF COARSE AGGREGATE SIZE DISTRIBUTION
FROM TWO-DIMENSIONAL SECTION

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 2005, 24 (17): -3107 doi:
Full Text: [PDF 144 KB] (1224)
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Coarse aggregate size distribution is important for the research on concrete strength analysis. Usually it can not be obtained without cutting a part of concrete down. A new method based on conditional probabilistic method is introduced. Application of “estimation of three-dimensional size distribution from two-dimensional section” is presented to direct estimation of three-dimensional size distribution. Analysis for a two-dimensional section using digital images is compared with the test of conventional mechanical sieving. The study demonstrates that this new method is a convenient and accurate technique for particle size distribution analysis.

STUDY ON IMPACT OF FOCAL MECHANISM
ON LONG-PERIOD GROUND MOTIONS

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 2005, 24 (17): -3113 doi:
Full Text: [PDF 169 KB] (1589)
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The study of long-period ground motions is significant to seismic design of large-scale engineering structures. The digital broad-band seismic records of strong earthquake swarm obtained in Jiashi,Xinjiang,China,in 1997 are used to study the impact of earthquake magnitude and focal mechanism on long-period ground motions. The results show that:(1) Earthquake magnitude has strong effects on the long-period ground motions. Larger earthquake has more long-period ground motion contents. (2) Compared with the strike-slip earthquakes,the oblique-faulting earthquakes have more long-period contents in vertical component. (3) The long-period horizontal acceleration response spectra of strike-slip earthquakes are higher than those of the normal-faulting earthquakes.

SIMULATION OF DEFORMATION BEHAVIOR OF ROCK MATERIAL UNDER TRIAXIAL COMPRESSION BASED ON SLIDING CRACK MODEL

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 2005, 24 (17): -3119 doi:
Full Text: [PDF 169 KB] (995)
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Based on the sliding crack model and the energy balance during crack growth,the deformation properties of the granite under triaxial compression are simulated at the confining pressures of 20,50 and 80 MPa respectively. It is shown that the simulated results agree well with the experimental results. The work in the paper can present an available method to quantitatively analyze the deformation properties of rock material under triaxial compression by using crack model.

LIFE-CYCLE RELIABILITY MANAGEMENT OF STRUCTURES

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 2005, 24 (17): -3125 doi:
Full Text: [PDF 69 KB] (918)
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The performance of structures is a time-variant process with large amount of uncertainties as well as the load and environmental effects on them. The reliability of a specific structure should be managed considering not only a generic design but also the inspection and maintenance strategies during its life-cycle. In the paper,firstly the advantages and limitations of the time-variant reliability theory currently used in structural design are discussed. Then the concept of life-cycle reliability management is introduced. A framework considering risk optimization and safety constraint is proposed for life-cycle reliability management. Several important theoretic issues are discussed,including the definition and usage of time-dependent reliability and dynamic reliability index,the expression of life-cycle cost and the Bayesian decision analysis,etc.. The framework stresses the importance of information updating during the structural life-cycle,and keeps consistent with current design practice.

ANALYSIS OF BLASTING TREMOR IMPACT ON ROADWAY
STABILITY IN COAL MINING

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 2005, 24 (17): -3131 doi:
Full Text: [PDF 563 KB] (1281)
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Based on the model for the initiation of coal-gas outbursts developed by J. Litwiniszyn,this paper briefly describes the mining conditions that lead to the coal bumps and a study of the impact on roadway stability caused by dynamic loading of blasting tremor in Zhaogezhuang Coal Mine. A mechanical model is described to analyze the mechanism of coal bumps induced by blasting tremor in deep mining. The FLAC2D is used to analyze the tremor impact on deep excavations and responses of different kinds of support systems in Zhaogezhuang Mine. The material properties are determined by examinations carried out in the mine. The study indicates that the blasting tremor can not only cause the stress redistribution,but also induce decreasing of frictional force between the coal seam and surrounding rock. The results of numerical simulations show that the behavior of the rock mass-support system under the dynamic load and confirm the possible damages to the excavation. The U-shaped steel yielding support system is proved to be efficient to offer superior protection in bursting region to the bolt and net system.

FUNCTIONS OF CHECK DAM AGAINST DEBRIS FLOW:COMPARISON OF TWO WATERSHEDS OF JIANGJIA GULLY,YUNNAN,CHINA

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 2005, 24 (17): -3137 doi:
Full Text: [PDF 257 KB] (1438)
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Debris flow activity has recently caused serious property damage as well as loss of life in Yunnan,Southwest China. Moreover,ground failure caused by debris flow needs a long time to be recovered. The hazards of debris flow can be prevented or released by some engineering countermeasures such as erosion control. The check dam is one of the most effective structures to control the debris flow in the original area. Based on the examination of Architectonic geology,engineering geology,rock mechanics and remote sensing geology,two major tributary gullies(one with check dams but the other without) of Jiangjia Gully in Yunnan Province,are compared in three aspects (channel longitudinal gradient,stability of lateral slopes and trailing edge of channel,soil erosion by debris flow) to prove that check dam or check dam series can:(1) effectively uplift the basic level of erosion of debris-flow channel;(2) reduce the longitudinal gradient of the debris-flow channel,and accordingly velocity slowed down and energy dissipated;(3) fix the channel and stabilize the slope so as to facilitate or restore the growth of the vegetation. In addition,several problems,needed to be taken into account during the design of check dam,are also discussed.

OCCURRENCE,GEOLOGY AND GEOMORPHY CHARACTERISTICS AND ORIGIN OF QIANJIANGPING LANDSLIDE IN THREE GORGES RESERVOIR AREA AND STUDY ON ANCIENT LANDSLIDE CRITERION

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 2005, 24 (17): -3146 doi:
Full Text: [PDF 121 KB] (3127)
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Qianjiangping landslide (2.4×107 m3),which occurred in the Three Gorges Reservoir area on July 13,2003,is one of the serious landslide disasters in this area after impounding. Also,it caused a serious loss of lives and property. According to the tracking survey on this landslide,quite a number of information about the landslide is obtained. This paper,firstly,introduces the location,geological background,occurrence and the emergency monitoring of the landslide,and elucidates its typical geologic and geomorphic characteristics,such as its plane shape of dust pan,boundary,longitudinal tensile crack in landslide body and geological structure and so on. Secondly,combined with the first-hand data,the origin of Qianjiangping landslide is analyzed by utilizing the theories of geomorphy and engineering geology mechanics. The result shows that the vulnerable geological structure of landslide body and concentrated rainfall mainly cause this landslide,while the rise of Qingganhe River and excavation accelerate the occurrence to some degree. Finally,the methods of field identifying of ancient (or old) landslide in reservoir area are discussed in term of the geologic and geomorphic characteristics of Qianjiangping landslide.

CONSTITUTIVE MODEL OF PLASTIC COMPACTION
FOR POROUS CHALK

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 2005, 24 (17): -3154 doi:
Full Text: [PDF 312 KB] (1101)
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Chalk is a typical material with high porosity. The experimental results suggest that the chalk behavior can be modeled in terms of elastoplastic model with two plastic deformation mechanisms:plastic compaction (pore collapse) and plastic shearing. Porosity plays an important role in the chalk plastic behavior. In other words,the effect of porosity needs to be taken into account in the modelling of chalk plastic behavior,especially in the modelling of chalk plastic compaction. Based on the concept,a new constitutive model,which is based on the Gurson criterion,is proposed for the description of plastic compaction behaviors in porous chalks. In general,the model predictions are in satisfactory agreement with the experimental results.

STUDY ON JI′AN LANDSLIDE CHARACTERS AND ORIGIN IN WANZHOU CHONGQING

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 2005, 24 (17): -3159 doi:
Full Text: [PDF 202 KB] (1145)
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At 9:00 5th September 2004,the worst new landslide in the history of Chongqing,China since 1949 occurred in Ji′an village Wanzhou City. Seven people were killed or injured by the landslide. The landslide destroyed an important local market town,the highway and the expressway under construction,and left a thousand of people homeless. There are great losses of life and economy in the landslide. The landslide is 1 247 m long,394 m wide in average with 7.0×106 m3 in volume and 0.7 km2 in area. On the basis of field investigation and study,the geologic environment and characters of Ji′an landslide are studied in detail. According to the environment characters and occurring process of Ji′an landslide,the geologic origin and the environment origin are researched. The conclusion is that the Ji′an landslide is a new consequent rock landslide of traction type in Jurassic. The hydrogeological structure type is the crucial factor;the geological structure type is the control factor;the valley development and evolvement type is the affecting factor;and the high intense and large rainfall is the triggering factor. At last,it is suggested to strengthen the landslide triggering mechanism study and landslide monitor.

FLEXIBILITY OF VISCO-ELASTOPLASTIC MODEL TO
RHEOLOGICAL CHARACTERISTICS OF ROCK AND SOLUTION
OF RHEOLOGICAL PARAMETER

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 2005, 24 (17): -3165 doi:
Full Text: [PDF 90 KB] (1224)
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By comparison of Burgers model with visco-elastoplastic model,this paper considers visco-
elastoplastic model is adaptive to all kinds of rock rheological characteristics,while Burgers model is only suitable to rather soft rock. Due to taking the relationship between s and ss into account,constitutive equations of visco-elastoplastic model are presented by segmented functions. When s <ss in the visco-elastoplastic model,creep never causes infinite deformation and relaxation wouldn′t result in stress disappearing. When s ≥ss,deformation caused by creeping will last all along,but stress caused by relaxation never decreases to zero. The Burgers model,regardless of relationship between s and ss,holds deformation to infinite as long as s is not equal to zero,which is contradictory to the rheological characteristics of rock. Moreover,according to triaxial creep test of rock samples,authors fit the curve of -t of the gray-yellow miliolite from fault of Zhaogezhuang Coal Mine respectively by visco-elastoplastic model and Burgers model and obtain their rheological parameters by least squares procedure. The fitting results show that the visco-elastoplastic model is more suitable than the Burgers model to describe rock rheological characteristics.

EXPERIMENTAL STUDY OF ROCK FAILURE PRECURSOR USING SIMULATED TIDE STRESS—LOAD/UNLOAD RESPONSE RATIO (LURR) AND ACCELERATING ENERGY RELEASE (AER)

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 2005, 24 (17): -3172 doi:
Full Text: [PDF 161 KB] (1091)
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High LURR values and observations of Accelerating Moment/Energy Release (AMR/AER) prior to large earthquakes have suggested that intermediate-term earthquake prediction is possible. The LURR and AMR/AER have a similar physical origin. Experiments are very important in exploring the deformation and fracture of earth rock. Acoustic emission experiments of rock failure under triaxial stress have been conducted. The technique of acoustic emission is an important approach to reveal the micro-mechanism of deformation and failure of rocks. In order to simulate the rock in the earth crust the specimens were loaded by the combined action of a constant stress,intended to simulate tectonic loading,and a small sinusoidal disturbance stress,analogous to the Earth tide induced by the sun and the moon. Lots of acoustic emission during the entire loading was recorded. Each acoustic emission signal is characterized by the time,the three coordinates of the hypocenter and the amplitude,which is able to indicate the occurrence time,location and magnitude of every damage (micro-crack) in the specimen. In this paper LURR and AER are carried out in detail using the AE records. The results show that high LURR and AER occur before the macro fracture of the specimens. The experimental results confirm that LURR and AER are two macroscopic failure precursors of rock,which could be served as the experimental support of critical point hypothesis and foundation of earthquake prediction.

TIME SERIES EVOLUTION FORECASTING MODEL OF SLOPE DEFORMATION BASED ON MULTIPLE FACTORS

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 2005, 24 (17): -3180 doi:
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A lot of factors such as topography,geological conditions and rainfall influence slope deformation. The importance of rainfall is difficult to determine. Based on the analysis of the multiple factors of slope deformation and observation of monitoring deformations,a statistic method to correlate slope deformation and rainfall was developed including the hysteresis of rainfall. Whereafter,by applying observation to ordinary statistic model comprising rainfall,temperature and time factor,the main factors affecting slope deformation were extracted by stepwise regression. According to the factors extracted and time series observation,a recursion model was obtained with multilayer recursion analysis method of dynamic system forecasting. At the end,a time series evolution forecasting model of slope deformation was presented combining with regression model and recursion model. The model syncretizes the merits of regression analysis and recursive analysis for enhancing the capability of forecasting evolution of slope deformation. Through comparison between the forecasting and the observation of monitoring deformations,the deformation and stability of slope can be monitored. The engineering case analysis indicates that the model is effective and has big value for forecasting of slope deformation.

PROBABILITY ANALYSIS OF RELATIONSHIP BETWEEN LANDSLIDE
AND RAINFALL IN CHONGQING AREA

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 2005, 24 (17): -3185 doi:
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Historical data of landslide and rainfall of 577 landslides in several decades are analyzed and the hydrogeology conditions in Chongqing area are introduced in detail. The relationship between rainfall and landslide is investigated in respects of time distribution,intraday rainfall,rainstorm,comparison of time between landslides and rainfall,and comparison between the days with rainfall and those with continuous rainfall within ten days before the landslide;and several conclusions are drawn which prove that the relationship between rainfall and landslide is close. The quantity of landslide has direct ratio with rainfall. Landslide usually occurs within four days after a rainfall and within one day after a rainstorm. On the assumption that rainfall begins to infiltrate into soil when rainfall is 3 mm,if there is 3-day continuous rainfall,the possibility of landslide is very high.

IMPROVED CUBIC COVERING METHOD FOR FRACTAL
DIMENSIONS OF A FRACTURE SURFACE OF ROCK

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 2005, 24 (17): -3192 doi:
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Description of fracture surface of rock is the base of evaluating its mechanical behavior. Ways to determine the fractal dimensions of a fracture surface are essential for a better understanding of its complete topographic characteristics. Triangular prism surface area method,projective covering method and cubic covering method are three widely used methods at present. Both the triangular prism surface area and projective covering methods cannot avoid the problem of approximate estimation of the real area surrounded by four points on the fracture surface,because the four points considered seldom lie on a plane. Such approximate calculations will certainly result in error. However,the cubic covering method can assure that every step is accurate. Therefore,it can be regarded as a reliable method for direct determination of the fractal dimension of a fracture surface. In this paper,a laser profilometer is employed to measure the topography of a rock fracture surface. Based on cubic covering method for the fractal dimensions of a fracture surface of rock,a new method named improved cubic covering method is proposed. Cubic covering method and improved cubic covering method are applied to computing fractal dimensions of the same fracture surface of rock. The results show that the improved cubic covering method not only has the advantage of the cubic covering method,but also has more convenient computing process.

ANALYSIS OF DIFFERENCE IN THERMAL STATE BETWEEN
SOUTH FACED SLOPE AND NORTH FACED SLOPE OF RAILWAY EMBANKMENT IN PERMAFROST REGION

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 2005, 24 (17): -3197 doi:
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As for the engineering construction in permafrost regions,the change of local permafrost environment,induced by human events,influences permafrost much more than the climate warming. The settlement on south faced slope is usually more than that on north faced slope,as indicated that the thawing of permafrost under south faced slope is acuter. Based on observed data in Beiluhe test site of Qinghai-Tibet Railway,the difference in thermal state between south faced slope and north faced slope was analyzed. The results indicate that the difference of ground-atmosphere heat transfers between south faced slope and north faced slope is very obvious and the annual mean temperature at a 0.5 m depth on south faced slope could be higher than that on north faced slope by over 3℃. The higher temperature on south faced slope is greatly attributed to high temperature during winter time. The fact that the annual ranges of ground temperatures near embankment surfaces are all greater than those near nature ground surface shows that the ground-atmosphere heat exchange of embankment surface is beyond that of nature ground surface. This kind of difference in thermal state may result in asymmetric thermal regime in embankment,and underlying soil as well. As a result,possible unevenly transverse deformation may appear.

薛强博士论文摘要

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 2005, 24 (17): -3201 doi:
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薛强博士论文摘要
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