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2019 Vol. 38, No. 4

Display Method:
Thoughts on tunnel water inrush in changing zones of groundwater level in karst areas
ZHENG Kexun, PEI Xiongwei, ZHU Daiqiang, WU Shuyu, GUO Weixiang
2019, 38(4): 473-479. doi: 10.11932/karst20190401
Abstract:
Based on analyses of the water inrush cases in the Jiguanshan tunnel and other examples in karst areas, it is summarized that water inrush in seasonal variation zones of tunnels can be characterized by fast response, large water volume and heavy sediment load. Based on hydrogeological features of tunnels in seasonal variation zones of groundwater, they are divided into two types, general mountain tunnels and tunnels associated with synclinal structural groundwater level variation zones. The mechanisms of water inrush are presented for both types. During the preliminary investigation of tunneling in karst areas, the demarcation of karst groundwater systems and groundwater dynamic zones should be focused on to understand the characteristics of karst development. During construction and operation periods, supplementary investigation should be carried out in combination with karst exposure and water inrush, which includes rainfall monitoring, water inrush and pressure monitoring to predict the maximum water pressure and inflow. Regarding water inrush, two treatment methods, i.e. dredging and blocking, are proposed and explained. The karst caves exposed during construction should not be simply blocked and the original passage should be well maintained. The lining design of the tunnel with possible water inrush should not only consider the surrounding rock structure, but also the external water pressure. Consolidation grouting should be applied where necessary. Due to the poor reliability of the regular annular drainage system and central ditch , in case of the large inflow of water, drainage tunnel should be used to drain water.
Karst geological problems and countermeasures of the Huayingshan super-long tunnel on the Guang’an-Linshui highway
TANG Kehang, WAN Chuan, TAN Gang, CHEN Zilong
2019, 38(4): 480-487. doi: 10.11932/karst20190402
Abstract:
When highways and railways cross the karst area, appropriate route selection can reduce engineering cost, engineering diseases and environmental impacts, so the problem of crossing and avoiding will be scientifically solved. The proposed Guang’an to Linshui highway is four-lane width and of first-class standard. In the preliminary design stage, based on the engineering feasibility study, the A-line and the K-line schemes are two candidates. The Huayingshan super-long tunnel crosses karst area, which is a key construction of this project. The data available from existing G42 Shanghai-Rongshan expressway as another Huayingshan tunnel provides a basis for this study. Considering the karst development, hydrogeological conditions and the key points of highway route selection in karst areas, a varietyof auxiliary technologies were used to analyze the principle of route selection. Finally it is concluded that the K-line scheme is the optimal scheme. Through this project example, it is suggested that in the process of highway route selection in complex karst areas, the principle of "multi-comparison and careful selection" should be followed, and environmental protection should be practiced.
Application of grouting sealing technology on karst high-pressure water inrush in a deep-buried extra-long tunnel
HE Qiao, ZHU Daiqiang, ZHENG Kexun, ZHU Jianyun, HUANG Yong
2019, 38(4): 488-495. doi: 10.11932/karst20190403
Abstract:
This paper presents the application of the grouting sealing technology on karst high-pressure water inrush in a deep-buried extra-long tunnel of the highway from Dejiang to Wuchuan in Guizhou Province. Firstly, some relevant issues are addressed such as the drilling equipment, grouting material selection and implementation of this technology. For different types of high-pressure water inrush, e.g. two-hole connected, single-hole independently exposed, and single-hole independent unexposed, different methods such as drainage pressure back-blocking, grouting stopping wall combined with axial and radial blocking, and advanced pre-grouting are adopted respectively. Consequently, the problem of high-pressure karst water inrush at multiple sections of the Dejiang tunnel has been successfully solved, so that the tunneling work can be restored, the safety of the project is guaranteed, and the construction period is shortened, which yields good economic and social benefits.
Influence of drainage on karst groundwater at an existing tunnel in the east-spring mountains, Chongqing
HE Suhebateer, JIANG Liangwen, ZHANG Guitong
2019, 38(4): 496-501. doi: 10.11932/karst20190404
Abstract:
The path of karst groundwater runoff is very complex, and the influence of tunnel drainage on karst groundwater is a long and complex process. Based on long-term observation data and site investigations, this paper analyzes the influence of existing tunnel drainage on karst groundwater in the east-spring mountains of Chongqing. It is concluded that the cone of depression formed by the drainage of karst groundwater from the tunnel in the horizontal flow zone can generally reach the elevation of the tunnel, while that in the tunnel in karst fractured zone remains at a certain height above the tunnel. Permeability is the key influencing factor of tunnel drainage on karst groundwater. The research results would be helpful to the selection of routes in karst areas and analysis of the influence of tunnel drainage on karst groundwater.
Karst features of the Lianhuatai hydropower station and engineering significance
LYU Yaocheng, LI Yuqiang, ZHANG Furong, JU Guanghong
2019, 38(4): 502-507. doi: 10.11932/karst20190405
Abstract:
The Lianhuatai hydropower station is located in the main valley section of the Danjiang river in Shangnan county, Shaanxi Province. Based on geological survey and exploration data, this paper presents the pattern, scale and distribution of the karst in the area of the dam and summarizes the development characteristics of the karst. The results show that karst development in the dam area is mainly controlled by lithology and geological structures. The karst is widely developed and concentrated at some places, characterized by vertical zoning and uneven spatial distribution. The influence of karst on construction mainly includes two aspects, karst seepage and karst stability, the former of which may cause the power station to fail to reach the designed normal water level. The karst caves may lower the anti-sliding stability of dam foundation. Therefore, it is suggested to set up anti-seepage curtains, and to replace and reinforce the karst caves exposed by dam foundation excavation with consolidation grouting. The influence of karst on the project can be effectively avoided with engineering treatment.
Analysis on leakage of a karst reservoir in southwestern China
XUE Wei, YUAN Zongfeng, ZHOU Mi
2019, 38(4): 508-514. doi: 10.11932/karst20190406
Abstract:
A reservoir is located in the north-central part of the Yunnan-Guizhou Plateau. The soluble rock in the reservoir area is widely distributed and the karst is developed. A nearly north-south trending fault in the middle of the reservoir area crosses both banks. To investigate the feasibility and sustainability of this reservoir, field surveys and geophysical explorations have been conducted in this area. Results suggest that the possibility of leakage to the adjacent low-lying valley is very small, to the south or downstream along the fault is also small. However, the reservoir will probably leak downstream and towards outside of the reservoir along the limestone erosion channel. The possibility of leakage to the dam downstream along the contact zone of the marble and gray-green rock or marble on the left bank is also small. Therefore, the normal water level of the reservoir may be sustained below the height of the Kc1 floor.
Karst geological conditions of the planned Ronglai reservoir in Guizhou Province
LIU Hao, TIAN Maozhong
2019, 38(4): 515-523. doi: 10.11932/karst20190407
Abstract:
The planned Ronglai reservoir is located on a karst platform between the Beipanjiang and Nanpanjiang water systems in the Pearl River basin, southwestern China. There are low-lying troughs on the left and right banks of the reservoir and large karst lakes with a number of sinkholes develop at the downstream of the chosen dam site. To further examine geological conditions of this reservoir, this work conducted the studies in terms of hydrogeological surveys, drilling, geophyical exploration and connectivity tests, involving the analyses of terrain, strata, lithology, geological structure, hydrogeological settinggy, and karst characteristics. Analytical result suggests that there will be no water leakage to occur at the bottom of the reservoir basin because of the existing impermeable rock mass. But as the two banks of the reservoir area are affected by the low groundwater level of the watershed, fault fracture zones and karst development, potential leakage remains a problem. Meanwhile, leakage can also take place along gentle-dipping rock surfaces and erosion cracks on the banks of the reservoir head. It is recommended to adopt the vertical anti-seepage method, in which the impervious standard (water permeability) is less than 3 Lu or the lower limit of the anti-seepage curtain is 10 m below the stable groundwater level. At the same time, when encountering geological defects such as caves, the threshold of this measure should be lowered to a appropriate extent.
Application of the tracer test in karst hydrogeological prospecting: An example of Heilongtan, Lijiang, Yunnan
HAN Xiao, CHEN Xin, ZHENG Kexun, LIU Sheng
2019, 38(4): 524-531. doi: 10.11932/karst20190408
Abstract:
The purpose of this work was to investigate the connection between groundwater and the surrounding springs in the recharge area of the Jiuzihai depression, Lijiang, Yunnan Province, and to provide scientific basis for spring water restoration. Using the artificial chemical tracer method a large-scale groundwater tracer test has been conducted with potassium iodide as tracer. Based on the experimental data, the seepage velocity of groundwater was calculated and the characteristics of the groundwater system in Heilongtan springs area were analyzed. The results show that the groundwater in the Jiuzihai depression is significantly connected with Heilongtan and Gucheng springs, while not connected with Qingxi springs and Bailanghua springs. The seepage velocity of groundwater from Jiuzihai to Heilongtan and Gucheng is around 405.86-1,077.84 m· d-1 and 349.96-629.09 m· d-1, respectively. The Jiuzihai depression is the main recharge area of the groundwater system of the Heilongtan springs area, which can also be used as an effective injection site for the restoration of Heilongtan springs. After receiving the recharge, it is mainly transported to area around Heilongtan-Gucheng by deep karst pipelines, of which the Heilongtan springs are the discharge area of the groundwater system.
Simulation of karst groundwater balance in the Westshan mountains, Heqing county, Yunnan Province
LIU Ruitong, WANG Jinguo, ZHOU Yun, HUANG Hua, CHEN Changsheng
2019, 38(4): 532-538. doi: 10.11932/karst20190409
Abstract:
The karst groundwater in the Westshan mountains of Heqing county is an important water resource for local residents. To carry out studies on groundwater balance, flow simulation and the karst groundwater dynamics is of great significance to improve management of the karst groundwater in this area. Based on available data, the physiography, lithology, structure, and hydrogeology of the area are analyzed and the karst groundwater system is demarcated. Numerical simulation is conducted, the result of which is compared with the conventional water balance method. The results show that the karst groundwater system in the study area can be reasonably divided into six sub-systems. The recharge and discharge of each karst subsystem are largely balanced, and the discharge is dominated by a concentrating manner, which accounts for 67%-92% of the total amount. The connectivity test confirms the existence of karst pipelines in the subsystem V, in which the difference between the simulated discharge and the measured spring discharge is minimal, indicating that the model considering the concentrated drainage is more suitable.
Formation mechanism of the karst spring in Dalongjing, Zhijin, Guizhou Province
MAO Jicheng, LIU Hong, ZUO Shuangying, HU Xuan
2019, 38(4): 539-545. doi: 10.11932/karst20190410
Abstract:
The Dalongjing karst spring system lies in Chadian township, Zhijin, Guizhou Province. This work attempts to clarify its formation mechanism and the relevant relationship between groundwater recharge and drainage by investigations to the terrain, landform, and chemical analysis. Results show that this big karst spring system formed in a limestone area with low mountains and hills. It is formed during the Range-basin and the Wujiang periods when the area have experienced a persistent river incision and strong karstifiction. As a result, karst depressions and funnels extensively developed between surface peak clusters on the Shangzhai platform and the water holes in the middle area. In addition, atmospheric rainwater enters the underground along the sinkhole, producing southward runoffs at a natural gradient. During this process, the water flow is gradually concentrated in the karst cave voids, and in turn the karst space is gradually expanded by means of physical and chemical erosions. Finally, the water is collected in the Longdonggou and discharges to the ground surface in a concentrating manner, resulting in the Dalongjing karst springs and the Dalongjing water system
Dynamic characteristics of karst water in underground rivers during dry seasons at the Yangniu village, Huaxi district, Guiyang
DAI Tianhao, WANG Zhongmei, CHEN Yao, ZHANG Yadi, JIANG Jianxu, ZOU Lei
2019, 38(4): 546-551. doi: 10.11932/karst20190411
Abstract:
The area around Yangniu village, Huaxi district, Guiyang City is characterized by well-developed karst, abundant groundwater, and valley landforms with complex tectonic deformation. The objective of this study is to investigate the underground river flow, water level changes and groundwater contamination in dry seasons in this region. Based on data from field investigations, actual measurements and laboratory experiments, the dynamic characteristics of the flow, water level, water quality, water temperature and pH value of the underground river are analyzed using CAD drawing and Excel data statistics. The results show that the seasonal adjustment coefficient of the karst water in the underground river of Yangniu village is 6.83 and the average flow is 0.102 m3·s-1, which is in a stable state. The water level change amplitude is 2.7, which is also stable. Moreover the water temperature and pH exhibit a gentle increasing trend. According to the Groundwater Quality Standard (GB/T 14848-2017), the groundwater quality in this area is of class III-V and is not fit for drinking purpose. This study can provide reference for the development and utilization of groundwater resources and environment assessment and protection in this area.
Karst hydrogeology and risk assessment of the Huali tunnel
TIAN Zutao, ZHANG Jun
2019, 38(4): 552-558. doi: 10.11932/karst20190412
Abstract:
The Huali tunnel on the Wengan-Kaiyang railway is a key engineering site, which is complicated by sinkholes, shafts, karst springs,and underground rivers. In this work, the lithologic combination of aquifers, distribution of soluble rock mass and karst water of this karst tunnel are studied by geological investigation, borehole drilling, field measurement, laboratory tests of physical and mechanical parameters and electrical geophysical prospecting. Results show that, (1) The karst groundwater system in the tunnel area can be divided into two hydrogeological units, a non-soluble rock system composed of argillaceous siltstone and a soluble rock system composed of limestone.(2) The normal tunnel water inflow is predicted to be 32,126.4 m3· d-1,and the maximum gushing water amount in the rainy season should be designed as 2 to 6 times of that in the normal condition.(3) The overall risk of karst water gushing is moderate, while the section with extremely high risk accounts for 16% of the total length.
Stability assessment of the spoil ground on the Liupanshui-Weining expressway in Guizhou Province
SHEN Mingxiang, LUO Hongming, LIU Zhipeng, MU Risheng, PENG Kunjie
2019, 38(4): 559-564. doi: 10.11932/karst20190413
Abstract:
Taking the 140m spoil ground on the right side of K89+250 from Liupanshui to Weining expressway in Guizhou Province as research object, the drainage capacity, the stability of retaining wall and slope are evaluated by site investigation and calculation and the stability of the spoil ground is evaluated. The results show that the peak discharge of the spoil ground is 0.874 m3· s-1, which is less than the maximum discharge capacity of 1.95 m3· s-1of the drainage ditch. The local stability coefficient of the spoil ground slope is 1.404 and the overall stability coefficient is 1.360 under normal operating conditions. The local stability coefficient is 1.303 and the overall stability coefficient is 1.172 under abnormal operating conditions. Anti-sliding stability of the retaining wall is greater than 1.3, anti-overturning stability is greater than 1.5, and the base stress is less than 250 kPa of foundation bearing capacity. Consequently, dimensions of drainage ditches can meet the drainage requirements of the spoil ground. The overall and local stability of the spoil ground slope under different working conditions can meet the requirements of stability and safety, and the anti-sliding stability, anti-overturning stability and bearing capacity of retaining wall also can meet the requirements of stability and safety. It is recommended to plant grass on the slope to improve the interception and drainage of the spoil ground and reduce the soil erosion on the slope.
Mechanism of geological hazards in the middle Permian collapse in the Wulingshan mountains of Guizhou Province
CHENG Pengxiang, LI Zongfa
2019, 38(4): 565-572. doi: 10.11932/karst20190414
Abstract:
The objective of this work is to analyze the mechanism of geological hazards of middle Permian collapse in the Wulingshan mountains, Guizhou Province. Based on field investigation and available geological data, it is found that the middle Permian strata in this area is mainly distributed on both banks of Wujiang river and its tributaries. The typical river valley terrain essentially causes the collapse. According to the analysis, the unloading action leads to the formation of vertical fractures in rock mass. These unloading fractures expand steadily under the combination of gravity, water erosion and dissolution, and other external forces, forming the boundary of dangerous rock mass. In the meantime, the unloading fractures together with independent structural planes such as layers and joints cut rock mass into independent dangerous rock masses, which leads to collapse. Three main types of failure modes of the Permian collapse in the region are proposed, unloading-stretching-overturn, unloading-stretching-sliding, and unloading-stretching-falling, of which the first type dominates the collapse in the study area.
Application of the landsonar to detecting hidden hazards of tunnel base on high-speed railway in karst areas
WANG Zefeng, ZHONG Shihang
2019, 38(4): 573-577. doi: 10.11932/karst20190415
Abstract:
It is reported that uneven subsidence and floor bulge occurred in the joint test stages of the Malazhai tunnel of the Shanghai-Kunming railway and Gaotian tunnel of the Guiyang-Guangzhou railway, implying potential geologic hazards there. In order to find out the cause of this phenomenon and the quality of grouting, landsonar method was used to detect the karst sections of these tunnels. Results show that there are many medium and small karst caves below the tunnel foundation, which are interconnected by several sets of medium to small faults extending below the tunnel foundation. During rainy seasons, intense change of water pressure surrounding the tunnel caused uneven subsidence and floor bulge. To remove such a hidden hazard, the fractured zone and grouting zone were identified according to landsonar data and a treatment plan was determined, which has been verified by its implementation.
Geophysical characteristics and geological interpretation of karst strata
TANG Kexuan, ZHAO Nan
2019, 38(4): 578-583. doi: 10.11932/karst20190416
Abstract:
To investigate the karst development characteristics in a water conservancy project area in Yunnan Province, a geophysical survey using transient electromagnetic and microtremor detection methods has been conducted. Analysis of the survey data shows that karstification can cause inhomogeneity of the physical properties in carbonate strata; the karst development in the engineering area is significantly affected by the structural plane and lithology distribution of the rock and it shows a certain layering in the vertical direction. The strong weathering zone and the fracture zone is often accompanied by the development of karst with the presence of large scale or discrete low resistivity and low wave velocity anomalies. Erosion along fractures can change the electrical parameters of the rock to a very large extent, but the impact on its elastic parameters is relatively low. The discrete coefficients of electrical and elastic parameters of rock can be used to characterize the resistance to erosion and weathering of rock mass as well as the degree of karst development. In combination with the magnitude and distribution of physical properties of rock, these coefficients can effectively help to analyze the karst development and nature of its filling material.
Analysis of foundation selection of a water-transmission aqueduct across a karst area in Guizhou Province
XIE Hongjian, WU Qingwen, YANG Wen
2019, 38(4): 584-590. doi: 10.11932/karst20190417
Abstract:
A water-transmission aqueduct crosses a karst area of Guizhou Province, which may cause engineering geological problems such as karst collapse and instability of slopes. On the basis of geological and geophysical surveys and drilling property of joints and cracks and their effects on karst are analyzed using the geological outline method, and the stability of buried karst caves is assessed. Standard semi-quantitative analysis and 2D- and 3D FEM analyses containing joints and fractures are performed to further examine the stability of karst caves under overlying loads from the perspectives of displacement, stress distribution, development of plastic zones and failure modes. Research shows that the stress of the roof of the karst cave beneath the project site is similar to that of a loaded beam at depth, in which joints and fractures can have a great impact on the stability of the roof. Shearing and extension are easy to occur along these discontinuities. Based on such analysis, a proper type of foundation is recommended for the long-term safety and stability of the planned aqueduct.
Optimization of pile foundation for high-rise buildings in deep-covered karst areas
LI Xiang, YIN Ji, WEI Jiaqi, WEI Maji
2019, 38(4): 591-599. doi: 10.11932/karst20190418
Abstract:
High-rise buildings, with a height over 150 m, commonly require high bearing capacity of the foundation and a pile-raft foundation is generally adopted. The pile foundation located in the deep-covered karst area should make full use of the bearing capacity of overlying strata and try to avoid the unstable section of the karst to optimize the use of pile foundation. Taking a 177 m-high building project in a deep-covered karst area as an example this paper presents the details of optimized design of pile foundation, large-scale construction and post-grouting at pile tips. Using the scheme of pile tip post-grouting and design of long- and short-piles, lengths of piles under the tower building is optimized from 40 m to 28 m under the core-tube zone and 23 m under the non-core-tube zone. Load tests and subsidence observations show that the vertical ultimate bearing capacity of single pile and foundation stiffness meet the designed requirement, and the differential settlement of foundation is very small, indicating that the post-grouting technology can effectively improve the bearing capacity of piles and the foundation stiffness. Adoption of long-short pile foundation can reduce differential settlement remarkably. Pile post-grouting technology can be recommended in high-rise building projects in deep-covered karst areas to make full use of the bearing capacity of overlying strata above the karstand reduce or avoid the risk of pile foundation across karst zones.
A new technology of reinforcement by cast-in-place pile foundation in karst areas
DU Hailong, HE Moli, LUO Xiaobin, BIN Bin, ZHAO Tiejun
2019, 38(4): 600-606. doi: 10.11932/karst20190419
Abstract:
To solve the defect of pile foundation of high buildings on karst foundation, this paper proposes a controllable pressure-tight grouting technology that uses low slump plastic concrete to reinforce the defect pile foundation. This technology uses a special high-pressure pump to form an effective pile diameter to improve pile foundation defects, which presses low slump with a strength of no less than 20 MPa and a slump of no more than 50mm into the strong karst development stratum. By means of in-situ tests and full-scale construction, a complete set of construction technology has been developed, which can be effectively applied to the treatment of bearing layer defects of pile foundation in limestone areas.
Technologies to deal with karst caves beneath pile foundation of the big bridge on the Laos-China railway
LI Qiang, Qin Yushun
2019, 38(4): 607-611. doi: 10.11932/karst20190420
Abstract:
This work studies the techniques to deal problems associated with karst caves beneath the pile foundation of Nam Song bridge in the Laos-China railway. Many kinds of factors are considered such as construction safety, quality, work duration, cost, environment and forms of karst caves. Based on data derive from the construction site, comparative analyses are performed in the strengths and weaknesses as well as practicability of the macadam back-filling method (e.g. wall-building by throwing and filling clay and rubble) and follow-up steel casing method and their combination in dealing with karst caves of various shapes. Results show that for small empty caves and moderate caves fully or partially filled caves, the first method can deal with the karst caves rapidly, efficiently and economically. For moderate empty karst caves, large karst caves and caves with big channels of underground rivers, the combination of the two methods permit to solve the problems during construction such as low efficiency, hole collapse risk, concrete over pouring, and steel casing deformation by extrusion, to overcome the construction risk owing to the karst cave in an economical and efficient manner. Based on these study results, this paper proposes the feasible options and key technologies deal with karst caves beneath bridge pile foundation in karst areas.
Effect of microbial mineralization on red clay
CHEN Jun, SHI Pengchao, BAI Wensheng, WU Zhonghu, YANG Heng
2019, 38(4): 612-618. doi: 10.11932/karst20190421
Abstract:
The technology of microbial mineralization was applied to the modification of red clay, in which the metabolites of bacillus pasteurii were used. Routine physical index tests were carried out on the red clay samples to analyze the changes of water content, density, specific gravity, porosity ratio and particle size by the modification. The shear strength of soil was determined by triaxial undrained shear tests. The microstructure of red clay was observed by SEM. The results show that the Bacillus pasteurii can induce the precipitation and cementation of calcium carbonate to fill voids of red clay effectively, and the soil sample was the best after 10 days of curing with constant temperature. With the addition of bacteria and the occurrence of microbial mineralization, the physical properties of the red clay changed significantly, and the internal friction angle and cohesion of the sample increased. Analysis of SEM images shows that calcium carbonate crystals were generated in the red clay sample which filled in the pores of the soil and strengthen the connection between soil particles.
Mechanical properties of microorganism solidified red clay immobilized by activated carbon in Guiyang
YANG Heng, CHEN Jun, BAI Wensheng, GAO Bin, SHI Pengchao
2019, 38(4): 619-626. doi: 10.11932/karst20190422
Abstract:
Although microorganisms can solidify soil, its consolidation strength needs to be enhanced further. This work proposed a combination of immobilized microbial technology and microbial induced calcium carbonate precipitation technology (MICP). In this method, about 0, 4%, 7%, 10%, 15% of activated carbon is uniformly mixed with the remolded red clay, and the soil is solidified by MICP, then conventional triaxial compression tests are performed on soil samples. At the same time, comparison tests of generating calcium carbonate in the liquid bottle with or without the cement solution under the same conditions are carried out. By means of scanning electron microscopy analysis, the mechanical properties of the sample, the role of activated carbon in the MICP process, and the microstructure are obtained. The test results show that in the process of microbial solidification of soil, activated carbon acts as a carrier for immobilized microorganisms, which plays a role of the “enhancing effect” on microorganisms during the MICP process, and increases calcium carbonate production during microbial induced calcium carbonate precipitation. The presence or absence and content of the soil have an important influence on the microbial solidified soil. Combined with the change of water film thickness, filling of pores and cementation by calcium carbonate, the effective C value of the shear strength of red clay is greatly increased, the effective φ value is reduced, and the peak shear stress is increased. These changes demonstrate that adding activated carbon can optimize the biomineralization environment, and pose a certain control effect on the crystal structure and morphology during crystallization. Consequently, a block with a certain structure with activated carbon as the "core" is formed, and the mechanical properties of the soil are enhanced. This research would be valuable for future microbial geotechnical technology and engineering applications.
Experimental study on creep behavior of red clay of existing foundation in Guiyang City
ZHANG Yaodan, SHA Yunbin, CHRN Jun, GAO Bin, WU Zhonghu
2019, 38(4): 627-634. doi: 10.11932/karst20190423
Abstract:
In order to further understanding the creep characteristics of red clay in the existing foundation, a uniaxial creep consolidation and triaxial creep tests were carried out in the laboratory respectively, with samples collected from the Guizhou Aluminum Plant, Guiyang City. Then a uniaxial creep empirical equation and Singh-Mitchell model were established based on the test data. The results show that under unidirectional consolidation there is a linear relationship between t/s and t, with a very high correlation coefficient. Because of the high correlation, the parameter b of the uniaxial creep equation can be used to assess total settlement in an uniaxial consolidation condition. The Singh-Mitchell three-parameter creep model established can better express the stress-strain and time relation of tested soil in the range of 25% to 100% deviatoric stress. At the same time, the SEM images show that with the increase of vertical pressure, the pore area and the number of micro particles of the red clay decrease, while the particle area gets larger, and the three-dimensional porosity grows in the uniaxial consolidation test, indicating that the change of the clay particle pores on a micro scale can be used to explain the macro phenomenon.
Microstructure and fractal characteristics of red clay particles in existing foundation based on SEM images
CHEN Taixu, CHEN Jun, SHA Yunbin, BAI Wensheng, WU Zhonghu, WANG Tingting
2019, 38(4): 635-642. doi: 10.11932/karst20190424
Abstract:
The IPP (Image-Pro Plus) software was used to extract and process the information of SEM images of three kinds of existing red clay in a factory, Guizhou Province, which helps to make qualitative description and quantitative analysis to the microstructure of the soil from the study site. In addition, the fractal theory is applied to analyze the SEM images, and the method of calculating the three-dimensional fractal dimension of particles in the IPP software is proposed. The results show that,(1) The parameters of shear strength increase with the growing number of microparticles and the ratio of particle morphology, and decrease with the average area of particles. (2) The distribution and morphology of particles have obvious fractal characteristics, with fractal dimensions between 2 and 3. The parameters of shear strength increase with the increase of particle distribution and fractal dimension of particle morphology. (3) It is feasible to use the IPP software to calculate the three-dimensional fractal dimension of soil particles. Compared with the method of building three-dimensional models, this method is simple and easy to use, and its analysis results are reliable.