过刊目录

  • 2024年, 21卷, 第03期
    刊出日期:2024-06-19
      

  • 全选
    |
  • G.Wilson FERNANDES, Letícia RAMOS, Dario C.PAIVA, Jéssica CUNHA-BLUM, Vanessa Matos GOMES, Daniel NEGREIROS
    2024, 21(03): 719-738.
    Land use change and occupation have led to modifications in the environment causing loss of biodiversity and ecosystem services throughout the planet. Some environments with high economic relevance, such as the ferruginous campo rupestre(rupestrian grassland known as Canga in Brazil), are even more susceptible to severe impacts due to their extreme habitat conditions and low resilience. The determination of reference ecosystems based on the intrinsic characteristics of the ecosystem is essential for conservation as well as to the implementation of ecological restoration. We proposed the reference ecosystem of the three main types of habitats of the ferruginous campo rupestre based on their floristic composition. We described the floristic composition of each habitat and evaluated the physicochemical properties of the soils and the relationship between plants and soils. All three habitats showed high diversity of plant species and many endemic species, such as Chamaecrista choriophylla, Cuphea pseudovaccinium, Lychnophora pinaster, and Vellozia subalata. The distribution of vegetation was strongly related with the edaphic characteristics, with a set of species more adapted to high concentration of base saturation, fine sand, organic carbon, and iron, while another set of species succeeded in more acidic soils with higher S and silt concentration. We provide support for the contention that the ferruginous campo rupestre is a mosaic of different habitats shaped by intrinsic local conditions. Failure to recognize the floristic composition of each particular habitat can lead to inappropriate restoration, increased habitat homogenization and increased loss of biodiversity and ecosystem services. This study also advances the knowledge base for building the reference ecosystem for the different types of ferruginous campo rupestre habitats, as well as a key database for highlighting those species contribute most to community assembly in this diverse and threatened tropical mountain ecosystem.
  • MACUROVá Tereza, ?KARPICH Václav
    2024, 21(03): 734-753.
    Mountain streams act as conveyors of sediments within the river continuum, where the physical transport of sediments between river reaches through the catchment or between individual parts(e.g., between hillslopes and channels) of the catchment is assumed. This study focused on sediment connectivity analysis in the Slaví? River catchment in the Moravskoslezské Beskydy Mts in the eastern part of the Czech Republic. The connectivity index and connectivity index target modelling were combined with an analysis of anthropogenic interventions. Additionally, field mapping, grain size of bed sediments and stream power analysis were used to obtain information about connectivity in the catchment. Based on the analysis and obtained results, terrain topography is the current main driving factor affecting the connectivity of sediment movement in the Slaví? River catchment. However, the modelling provided valuable information about high sediment connectivity despite different recent land use conditions(highly forested area of the catchment) than those in historical times from the 16th to 19th centuries when the Slaví? River catchment was highly deforested and sediment connectivity was probably higher. The analysis of anthropogenic interventions, field mapping,grain size of bed sediments and stream power analysis revealed more deceleration of sediment movement through the catchment, decreased sediment connectivity with bed erosion, and gradual river channel process transformation in some reaches. Field mapping has identified various natural formations and human-induced changes impacting the longitudinal and lateral connectivity in the Slaví? River. For instance, embankments along 48% of the river's length, both on the right and left banks, significantly hinder lateral sediment supply to the channel. Stream power index analysis indicates increased energy levels in the flowing water in the river's upper reaches(up to 404.8 W m~(-2)). This high energy is also observed in certain downstream sections(up to 337.6 W m~(-2)), where it is influenced by human activities. These conditions lead to intensified erosion processes, playing a crucial role in sediment connectivity. Similar observations were described in recent studies that pointed out the longterm human interventions on many streams draining European mountains, where a decrease in sediment connectivity in these streams is linked with sediment deficits and the transformation of processes forming channels.
  • SATIR Onur, TOSUN Busra, COSKUN OZYOL Funda, OZDEMIR Omer Faruk, BERBEROGLU Suha
    2024, 21(03): 754-767.
    Mountainous regions have disadvantages in economic development because of harsh physical and climatic conditions. However, winter tourism activities are one of the key components for supporting economic development in the highlands. Establishing a ski resort area supports direct and indirect employment in a region, and it stops immigration from mountainous regions to other places. This research aimed to assess the potential ski areas using a multi criteria evaluation technique in the Van region which is located in the eastern part of Türkiye. In this context, snow cover duration, sun effect, slope, slope length, elevation, population density, distance from main roads and lake visibility were used as input factors in the decision making process. Each factor was standardized using a fuzzy technique based on existing well-known ski centers in Türkiye. The weight of inputs was defined by applying a survey to the professional skiers. The most important factors were detected as transportation opportunities and snow covers whereas, the least important factors were elevation and population density. Additionally, lake visibility was very important to make a difference from other existing facilities in the region. Therefore, it was included as constraints and lake visible areas were extracted at the final stage of the research. Potential ski areas were mapped in three levels as professional, intermediate and beginner skiers. One of the suitable areas was selected as a sample projection and for the 3D simulation of the ski investment area. Potential costs and benefits were discussed. It was found that a ski tourism area investment can be amortized in 3 years in the region.
  • Shakil Ahmad ROMSHOO, Ummer AMEEN, Mustafa Hameed BHAT, Tariq ABDULLAH
    2024, 21(03): 768-789.
    Himalayan glaciers are shrinking rapidly, especially after 2000. Glacier shrinkage, however, shows a differential pattern in space and time, emphasizing the need to monitor and assess glacier changes at a larger scale. In this study, changes of 48 glaciers situated around the twin peaks of the Nun and Kun mountains in the northwestern Himalaya, hereafter referred to as Nun-Kun Group of Glaciers(NKGG), were investigated using Landsat satellite data during 2000-2020. Changes in glacier area, snout position, Equilibrium Line Altitude(ELA), surface thickness and glacier velocity were assessed using remote sensing data supplemented by field observations. The study revealed that the NKGG glaciers have experienced a recession of 4.5%±3.4% and their snouts have retreated at the rate of 6.4±1.6 m·a~(-1). Additionally, there was a 41% increase observed in the debris cover area during the observation period. Using the geodetic approach, an average glacier elevation change of-1.4±0.4 m·a~(-1) was observed between 2000 and 2012. The observed mass loss of the NKGG has resulted in the deceleration of glacier velocity from 27.0±3.7 m·a~(-1) in 2000 to 21.2±2.2 m·a~(-1) in 2020. The ELA has shifted upwards by 83.0±22 m during the period. Glacier morphological and topographic factors showed a strong influence on glacier recession. Furthermore, a higher recession of 12.9%±3.2% was observed in small glaciers, compared to 2.7%±3.1% in larger glaciers. The debris-covered glaciers showed lower shrinkage(2.8%±1.1%) compared to the clean glaciers(9.3%±5%). The glacier depletion recorded in the NKGG during the last two decades, if continued, would severely diminish glacial volume and capacity to store water, thus jeopardizing the sustainability of water resources in the basin.
  • Johndale Rein T.BULLONG, Jim P.SILVERIO, Joanna I.ALAFAG, Maricel A.GURON, Jones T.NAPALDET
    2024, 21(03): 786-804.
    The scientific community faces the challenge of measuring progress toward biodiversity targets and indices have been traditionally used. However, recent inventories in secondary tropical mountain forests using traditional biodiversity indices have yielded results that are indistinct with primary ones. This shows the need to develop complementary indices that goes beyond species count but integrates the distribution and conservation status of the species. This study developed endemicity and conservation importance index for tropical forest that incorporated the distribution and conservation status of the species. These indices were applied to Mt. Natoo, a remnant primary mossy forest in Buguias, Benguet, Philippines, that resulted to endemicity index of 81.07 and conservation importance index of 42.90. Comparing these with secondary forest sites with comparable Shannon-Wiener, Simpson, Evenness and Margalef's indices, our endemicity and conservation indices clearly differentiates primary forest(our study site) with higher values from secondary forests with much lower values. Thus, we are proposing these indices for a direct but scientifically-informed identification of specific sites for conservation and protection in tropical forests. Additionally, our study documented a total of 168 vascular plant species(79 endemic and 12 locally threatened species) in Mt. Nato-o. Majority are of tropical elements for both generic and species levels with some temperate elements that could be attributed to the site's high elevation and semi-temperate climate. These are important baseline information for conservation plans and monitoring of tropical mossy forests.
  • JIN Lu, CHEN Jun, CAI Yu, KONG Yecheng, WANG Yongfeng, DUAN Zheng
    2024, 21(03): 805-819.
    The ice phenology of alpine lakes on the Tibetan Plateau(TP) is a rapid and direct responder to climate changes, and the variations in lake ice exhibit high temporal frequency characteristics. MODIS and passive microwave data are widely used to monitor lake ice changes with high temporal resolution. However, the low spatial resolutions make it difficult to effectively quantify the freeze-melt dynamics of lakes. This work used Sentinel-1 synthetic aperture radar(SAR) data to derive highresolution ice maps(about 6 days), then with the aid of Sentinel-2 optical images to quantify freeze-melt processes in three typical lakes on the TP(e.g. Selin Co, Ayakekumu Lake, and Nam Co). The results showed that three lakes had an average annual ice period of 125-157 days and a complete ice cover period of 72-115 days, from 2018 to 2022. They exhibit different ice phenology patterns. Nam Co is characterized by repeated episodes of freezing,melting, and refreezing, resulting in a prolonged freeze-up period. Meanwhile, the break-up period of Nam Co lasts for a longer duration(about 19 days), and the break-up exhibits a smooth process. Similarly, Ayakekumu Lake showed more significant inter-annual fluctuations in the freeze-up period, with deviations of up to 28 days observed among different years. Compared to the other two lakes, Selin Co experienced a relatively short freeze-up and break-up period. In short, Sentinel-1 SAR data can effectively monitor the weekly and seasonal variations in lake ice on the TP. Particularly, this data facilitates quantification of the freeze-melt dynamics.
  • QIN Xiaochun, NI Anchen, YANG Dongxiao, XING Wenhu, LIU Shiliang
    2024, 21(03): 820-835.
    During the highway construction, a large number of spoil areas will be generated while a large amount of waste slag and soil could not be rationally utilized. Besides, the vegetation recovery is slow in the spoil areas due to the soil depletion. Aiming at recycling the solid waste, the sieved engineering waste slag with local red clay and corn straw biochar was supplied to solve the problem of insufficient nutrients in engineering waste slag and soil. In addition, planting experiments of alfalfa(Medicago sativa L.) and Amorpha fruticosa L. combined with physical and chemical experiments were carried out to prove the feasibility of the novel improved substrate for the reclamation of spoil areas. The results show that the substrate's improvement effect is mainly affected by the soil to slag ratio and the biochar content. The improvement effect of soil matrix in highway spoil area decreases with the increase of the waste slag content, especially when the soil-slag ratio is less than 3, and the promotion of plants is limited. On the contrary, the improvement effect is proportional to the biochar content(3%-8%). But it is noted that the Cu and Pb in the soil will exceed the clean limit corresponding to the Nemero soil pollution index level when the biochar content is 8%. Therefore, it is recommended that the soil-slag ratio should be ≥3, and the biochar content should reach 3%-5%. This research provides experimental basis and technical support for utilizing solid waste resources in the reclamation of highway spoil areas.
  • PANG Jinghao, LIANG Shen, LIU Yabin, LI Shengwei, WANG Shu, ZHU Haili, LI Guorong, HU Xiasong
    2024, 21(03): 835-849.
    Artificial vegetation restoration is the main measure for vegetation restoration and soil and water conservation in alpine mine dumps on the Qinghai–Tibet Plateau, China. However, there are few reports on the dynamic changes and the influencing factors of the soil reinforcement effect of plant species after artificial vegetation restoration under different recovery periods. We selected dump areas of the Delni Copper Mine in Qinghai Province, China to study the relationship between the shear strength and the peak displacement of the root–soil composite on the slope during the recovery period, and the influence of the root traits and soil physical properties on the shear resistance characteristics of the root–soil composite via in situ direct shear tests. The results indicate that the shear strength and peak displacement of the rooted soil initially decreased and then increased with the increase of the recovery period. The shear strength of the rooted soil and the recovery period exhibited a quadratic function relationship. There is no significant function relationship between the peak displacement and the recovery period. Significant positive correlations(P < 0.05) exists between the shear strength of the root–soil composite and the root biomass density, root volume density, and root area ratio, and they show significant linear correlations(P < 0.05). There are no significant correlations(P > 0.05) between the shear strength of the root–soil composite and the root length density, and the root volume ratio of the coarse roots to the fine roots. A significant negative linear correlation(P < 0.05) exists between the peak displacement of the rooted soil and the coarse-grain content, but no significant correlations(P > 0.05) with the root traits, other soil physical property indices(the moisture content and dry density of the soil), and slope gradient. The coarse-grain content is the main factor controlling the peak displacement of the rooted soil.
  • WEI wenyu, LIU Ya, ZHANG Lixia, LI Lanhai
    2024, 21(03): 850-866.
    Soil degradation caused by soil erosion is one of the world's most critical environmental issues. Soil erosion in the Tianshan Mountains has caused various environmental problems in the surrounding areas. This study used remote sensing data to analyze the distribution of the factors influencing soil erosion, and the revised universal soil loss equation(RUSLE) to calculate the total amount and distribution characteristics of soil erosion in the Tianshan Mountains in 2019. Due to the large error of RUSLE in soil erosion estimation in mountainous areas, this study modified RUSLE equation based on the characteristics of snow cover in the Tianshan Mountains. The results show that the average soil erosion was 1690.3 t/(km~2·year), of which insignificant erosion, slight erosion and moderate erosion accounted for 42,8%, 22.4% and 9.9%, respectively. Severe erosion and above accounted for 13.3%. The accuracy of the soil erosion modulus calculated by the RUSLE was only 61.9%, with an average error of 1631.9 t/(km~2·year). The average error of the double-coefficient correction method was 1259.1 t/(km~2·year), and the average error of the modified formula method was reduced by 40.3% compared with the RUSLE, reaching 973.7 t/(km~2·year), and its accuracy reached 76.2%. Very severe erosion and catastrophic erosion are distributed on mountain ridges with higher elevation and on the northern area with higher precipitation. Snow cover has a certain inhibitory effect on soil erosion, and snow cover in alpine mountains is a factor that cannot be ignored in soil erosion research. The improvement of the RUSLE by the modified formula method can more accurately calculate the soil erosion modulus in the Tianshan Mountains in order to provide accurate soil erosion control recommendations for different erosion areas.
  • JIAO Weizhi, ZHANG Ming, LI Peng, XIE Junjin, PANG Haisong, LIU Fuxing, YANG Long
    2024, 21(03): 867-881.
    Red clay landslides are widely distributed worldwide, resulting in severe loss of life and property. Although rainfall-induced red clay slopes have received extensive attention, the role of cracks in the evolutionary process of red clay slopes and their connection to failure mechanisms is still poorly understood. A comprehensive approach integrating field investigation, laboratory tests, and numerical simulations was conducted to study the 168 red clay landslides in Xinshao County, China. The results show that red clay is prone to forming cracks at high moisture content due to its low swelling and high shrinkage properties. The failure mode of red clay slopes can be summarized in three stages: crack generation, slope excavation, and slope failure. Furthermore, the retrospective analysis and numerical simulations of the typical landslide in Guanchong indicated that intense rainfall primarily impacts the shallow layer of soil within approximately 0.5 m on the intact slope. However, cracks change the pattern of rainfall infiltration in the slope. Rainwater infiltrates rapidly through the preferential channels induced by the cracks rather than uniformly and slowly from the slope surface. This results in a significant increase in both the depth of infiltration and the saturated zone area of the cracked slope, reaching 3.8 m and 36.2 m2, respectively. Consequently, the factor of safety of the slope decreases by 13.4% compared to the intact slope, ultimately triggering landslides. This study can provide valuable insights into understanding the failure mechanisms of red clay slopes in China and other regions with similar geological settings.
  • WANG Tong, LIU Xianfeng, HOU Zhaoxu, XU Jiahang, ZHANG Jun, YUAN Shengyang, JIANG Guanlu, HU Jinshan
    2024, 21(03): 882-900.
    Rock slope with horizontal-layered fractured structure(HLFS) has high stability in its natural state. However, a strong earthquake can induce rock fissure expansion, ultimately leading to slope failure. In this study, the dynamic response, failure mode, and spectral characteristics of rock slope with HLFS under strong earthquake conditions were investigated based on the large-scale shaking table model test. On this basis, multiple sets of numerical calculation models were further established by UDEC discrete element program. Five influencing factors were considered in the parametric study of numerical simulations, including slope height, slope angle, bedding-plane spacing and secondary joint spacing as well as bedrock dip angle. The results showed that the failure process of rock slope with HLFS under earthquake action is mainly divided into four phases, i.e., the tensile crack of the slope shoulder joints and shear dislocation at the top bedding plane, the extension of vertical joint cracks and increase of shear displacement, the formation of step-through sliding surfaces and the instability, and finally collapse of fractured rock mass. The acceleration response of slopes exhibits elevation amplification effect and surface effect. Numerical simulations indicate that the seismic stability of slopes with HLFS exhibits a negative correlation with slope height and angle, but a positive correlation with bedding-plane spacing, joint spacing, and bedrock dip angle. The results of this study can provide a reference for seismic stability evaluation of weathered rock slopes.
  • LU Jiahui, LUO Junjie, HUANG Xiangyun, HONG Junliang, HE Yan Xin, ZHOU Fulin
    2024, 21(03): 901-920.
    Seismic isolation is an effective strategy to mitigate the risk of seismic damage in tunnels. However, the impact of surface-reflected seismic waves on the effectiveness of tunnel isolation layers remains under explored. In this study, we employ the wave function expansion method to provide analytical solutions for the dynamic responses of linings in an elastic half-space and an infinite elastic space. By comparing the results of the two models, we investigate the seismic isolation effect of tunnel isolation layers induced by reflected seismic waves. Our findings reveal significant differences in the dynamic responses of the lining in the elastic half-space and the infinitely elastic space. Specifically, the dynamic stress concentration factor(DSCF) of the lining in the elastic half-space exhibits periodic fluctuations, influenced by the incident wave frequency and tunnel depth, while the DSCF in the infinitely elastic space remain stable. Overall, the seismic isolation application of the tunnel isolation layer is found to be less affected by surfacereflected seismic waves. Our results provide valuable insights for the design and assessment of the seismic isolation effect of tunnel isolation layers.
  • CAO Ting, WANG Pingyi, QIU Zhenfeng, LIU Jie
    2024, 21(03): 918-931.
    Impulse waves that are generated by landslides in narrow reservoir areas threaten the stability of buildings and bank slopes. To discuss the action process and evolution law of the wave pressure on bank slopes, a three-dimensional physical model test that considers impulse waves generated by landslides was performed, and factors including landslide width, thickness, slope angles of the sliding surface, and bank slope angle were considered. Based on wave forms on the bank slopes, wave pressure curve characteristics, and peak value, the action process of wave pressure could be divided into the following stages: maximum pulsating pressure stage, wave impact stage(when waves break), and stationary pulsation stage. It was found that wave breaking is dependent on the value of the surf similarity parameter ξ. The distribution pattern of impact pressure decays linearly on both sides of the maximum impact pressure point, and the attenuation degree decreases when it attains 40% of the maximum value. Thus, it is proposed that the prediction formula for the maximum effective impact pressure of the bank slope be related to the reciprocal of wave steepness, relative water depth, and slope rate. The prediction formula provides strong theoretical support for early safety warning and for predicting the bank slope under impulse waves generated by landslides.
  • HE Ligeng, TAN Longmeng, YANG Xingguo, ZHOU Jiawen, LIAO Haimei
    2024, 21(03): 932-951.
    Granular debris plays a significant role in determining damming deposit characteristics. An indepth understanding of how variations in grain size distribution(GSD) and geometric configurations impact the behavior of granular debris during the occurrence of granular debris is essential for precise assessment and effective mitigation of landslide hazards in mountainous terrains. This research aims to investigate the impact of GSD and geometric configurations on sliding and damming properties through laboratory experiments. The geometric configurations were categorized into three categories based on the spatial distribution of maximum volume: located at the front(Type Ⅰ), middle(Type Ⅱ), and rear(Type Ⅲ) of the granular debris. Our experimental findings highlight that the sliding and damming processes primarily depend on the interaction among the geometric configuration, grain size, and GSD in granular debris. Different sliding and damming mechanisms across various geometric configurations induce variability in motion parameters and deposition patterns. For Type Ⅰ configurations, the front debris functions as the critical and primary driving component, with energy dissipation primarily occurring through inter-grain interactions. In contrast, Type Ⅱ configurations feature the middle debris as the dominant driving component, experiencing hindrance from the front debris and propulsion from the rear, leading to complex alterations in sliding motion. Here, energy dissipation arises from a combination of inter-grain and grain-substrate interactions. Lastly, in Type Ⅲ configurations, both the middle and rear debris serve as the main driving components, with the rear sliding debris impeded by the front. In this case, energy dissipation predominantly results from grainsubstrate interaction. Moreover, we have quantitatively demonstrated that the inverse grading in damming deposits, where coarse grain moves upward and fine grain moves downward, is primarily caused by grain sorting due to collisions among the grains and between the grain and the base. The impact of grain on the horizontal channel further aids grain sorting and contributes to inverse grading. The proposed classification of three geometric configurations in our study enhances the understanding of damming properties from the view of mechanism, which provides valuable insights for related study about damming granular debris.
  • GUO Junqi, XI Wenfei, YANG Zhiquan, SHI Zhengtao, HUANG Guangcai, YANG Zhengrong, YANG Dongqing
    2024, 21(03): 952-972.
    Landslide hazard susceptibility evaluation takes on critical significance in early warning and disaster prevention and reduction. In order to solve the problems of poor effectiveness of landslide data and complex calculation of weights for multiple evaluation factors in the existing landslide susceptibility evaluation models, in this study, a method of landslide hazard susceptibility evaluation is proposed by combining SBAS-InSAR(Small Baseline Subsets-Interferometric Synthetic Aperture Radar) and SSA-BP(Sparrow Search Algorithm-Back Propagation) neural network algorithm. The SBAS-InSAR technology is adopted to identify potential landslide hazards in the study area, update the cataloging data of landslide hazards, and 11 evaluation factors are chosen for constructing the SSA-BP model for training and validation. Baihetan Reservoir area is selected as a case study for validation. As indicated by the results, the application of SBAS-InSAR technology, combined with both ascending and descending orbit data, effectively addresses the incomplete identification of landslide hazards caused by geometric distortion of single orbit SAR data(e.g., shadow, overlay, and perspective contraction) in deep canyon areas, thereby enabling the acquisition of upto-date landslide hazard data. Moreover, in comparison to the conventional BP(Back Propagation) algorithm, the accuracy of the model constructed by the SSA-BP algorithm exhibits a significant increase, with mean squared error and mean absolute error reduced by 0.0142 and 0.0607, respectively. Additionally, during the process of susceptibility evaluation, the SSA-BP model effectively circumvents the issue of considerable manual interventions in calculating the weight of evaluation factors. The area under the curve of this model reaches 0.909, surpassing BP(0.835), random forest(0.792), and the information value method(0.699). The risk of landslide occurrence in the Baihetan Reservoir area is positively correlated with slope, surface temperature, and deformation rate, while it is negatively correlated with fault distance and normalized difference vegetation index. Geological lithology exerts minimal influence on the occurrence of landslides, with the risk being low in forest land and high in grassland. The method proposed in this study provides a useful reference for disaster prevention and mitigation departments to perform landslide hazard susceptibility evaluations in deep canyon areas under complex geological conditions.
  • ZHANG Shengrui, ZHANG Tongyan, JU Hongrun, WANG Yingjie
    2024, 21(03): 973-986.
    Tourism resources that span provincial boundaries in China play a pivotal role in regional development, yet effective governance poses persistent challenges. This study addresses this issue by constructing a comprehensive database of transboundary natural tourism resources(TNTR) through amalgamation of diverse data sources. Utilizing the Getis-Ord Gi*, kernel density estimation, and geographical detectors, we scrutinize the spatial patterns of TNTR, focusing on both named and unnamed entities, while exploring the influencing factors. Our findings reveal 7883 identified TNTR in China, with mountain tourism resources emerging as the predominant type. Among provinces, Hunan boasts the highest count, while Shanghai exhibits the lowest. Southern China demonstrates a pronounced clustering trend in TNTR distribution, with the spatial arrangement of biological landscapes appearing more random compared to geological and water landscapes. Western China, characterized by intricate terrain, exhibits fewer TNTR, concurrently unveiling a significant presence of unnamed natural tourism resources. Crucially, administrative segmentation influences TNTR development, generating disparities in regional goals, developmental stages and intensities, and management approaches. In response to these variations, we advocate for strengthening the naming of the unnamed transboundary tourism resources, constructing a geographic database of TNTR for government and establishing a collaborative management mechanism based on TNTR database. Our research contributes to elucidating the intricate landscape of TNTR, offering insights for tailored governance strategies in the realm of cross-provincial tourism resource management.
  • MOUJANE Said, ALGOUTI Ahmed, ALGOUTI Abdellah, FARAH Abdelouahed, ABOULFARAJ Abdelfatah, NAFOURI Imane
    2024, 21(03): 987-1003.
    The integration of remote sensing and geographic information system(GIS) was employed in this study to delineate the structural lineaments within the eastern section of the Ouarzazate Basin, situated between the southern front of the Central High Atlas and the northern slopes of the Eastern Anti-Atlas(also known as the Saghro Massif). To achieve this objective, Landsat 8 Operational Land Imager(OLI) and Shuttle Radar Topography Mission(SRTM) data were used. Principal Component Analysis(PCA) was computed and a directional filter was applied to the first PCA and the panchromatic band(B8). Additionally, shading was applied to the SRTM data in four directions; N0°, N45°, N90°, N135°. After removing of the nongeological linear structures, the results obtained, using the automatic extraction method, allowed us to produce a synthetic map that included 1251 lineaments with an average length of 1331 m and was dominated by NE-SW, ENE-WSW and E-W directions, respectively. However, the high lineament density is clearly noted in the Anti-Atlas(Saghro Massif) and at the level of the northern part, extending from the Ait Ibrirne to Arg-Ali Oubourk villages. High lineament density can always be found around the major faults affecting this area. The data collected during the field investigations and from geological maps show that the major direction of the faults and structural accidents range mostly between N45°, N70° and N75°. The correlation of remote sensing results with those collected in the field shows a similarity and coincidence with each other. From these results, it is possible to consider the automatic extraction method as a supplementary kind that can serve classical geology by quickly enriching it with additional data. As shown in this work, this method provides more information when applied in arid areas where the fields are well outcropped.
  • LIU Dongqiao, SUN Jie, MENG Wen, HE Manchao, ZHANG Chongyuan, LI Ran, CAO Binghao
    2024, 21(03): 1004-1018.
    To investigate the influence mechanism of geostress on rockburst characteristics, three groups of gneiss rockburst experiments were conducted under different initial geostress conditions. A high-speed photography system and acoustic emission(AE) monitoring system were used to monitor the entire rockburst process in real time. The experimental results show that when the initial burial depth increases from 928 m to 1320 m, the proportion of large fracture scale in rockburst increases by 154.54%, and the AE energy increases by 565.63%, reflecting that the degree and severity of rockburst increase with the increase of burial depth. And then, two mechanisms are proposed to explain this effect, including(i) the increase of initial geostress improves the energy storage capacity of gneiss, and then, the excess energy which can be converted into kinetic energy of debris ejection increases, consequently, a more pronounced violent ejection phenomenon is observed at rockburst;(ii) the increase of initial geostress causes more sufficient plate cracks of gneiss after unloading of σh, which provides a basis for more severe ejection of rockburst. What's more, a precursor with clear physical meaning for rockburst is proposed under the framework of dynamic response process of crack evolution. Finally, potential value in long term rockburst warning of the precursor obtained in this study is shown via the comparison of conventional precursor.
  • LI Dejian, FU Junwen, LI Hekai, CHENG Xiao, ZHAO Lianheng, ZHANG Yingbin, PENG Xinyan
    2024, 21(03): 1019-1035.
    In practical engineering, due to the noncontinuity characteristics of joints in rock slopes, in addition to plane failure, stepped sliding failure may occur for intermittently jointed rock slopes. Especially for intermittently bedding jointed rock slopes, the correlation and difference in strength parameters between joints and rock bridges, along with the various failure modes and intermittency of rock bridges, contribute to the complexity of stepped failure modes and the unpredictability of failure regions. Based on the upper-bound limit analysis method and multisliders step-path failure mode, considering the shear and tensile failure of rock bridges and the weakened relationship between the strength parameters of rock bridges and jointed surfaces, by introducing the modified M-C failure criterion and the formula for calculating the energy consumption of tensile failure of rock bridges, two failure mechanisms are constructed to obtain the safety factor(Fs) of intermittently jointed rock slopes. The sequential quadratic programming method is used to obtain the optimal upper-bound solution for Fs. The influence of multiple key parameters(slope height H, horizontal distance L, Slope angle β, shear strength parameters of the rock bridge φr and cr, Dimensionless parameter u, weakening coefficients of the internal friction angle and cohesion between the rock bridges and joint surfaces Kφ and Kc) on the stability analysis of intermittently jointed rock slopes under the shear failure mode of rock bridges as well as under the tensile failure mode is also explored. The reliability of the failure mechanisms is verified by comparative analysis with theoretical results, numerical results, and landslide cases, and the variation rules of Fs with each key parameter are obtained. The results show that Fs varies linearly with φ_r and cr of the rock bridge and with K_φ and K_c, whereas F_s changes nonlinearly with H and L. In particular, with the increase in K_φ and K_c, Fs increases by approximately 52.78% and 171.02% on average, respectively. For rock bridge tensile failure, Fs shows a nonlinearly positive correlation with φ_r, c_r, K_φ and K_c. In particular, with the increase in K_φ and K_c, Fs increases by approximately 13% and 61.69% on average, respectively. Fs decreases rapidly with increasing slope gradient β and decreasing dimensionless parameter μ. When K_φ and K_c are both less than 1.0, the stepped sliding surface occurs more easily than the plane failure surface, especially in the case of tensile failure of the rock bridge. In addition, rock slopes with higher strength parameters, taller heights, and greater weakening coefficients are prone to rock bridge tension failure with lower Fs, and more attention should be given to the occurrence of such accidents in actual engineering.
  • ZUO Shi, ZHAO Lianheng, HU Shihong
    2024, 21(03): 1036-1047.
    Only simplified two-dimensional model and a single failure mode are adopted to calculate the ultimate pullout capacity(UPC) of anchor cables in most previous research. This study focuses on a more comprehensive combination failure mode that consists of bond failure of an anchorage body and failure of an anchored rock mass. The three-dimensional ultimate pullout capacity of the anchor cables is calculated based on the Hoek-Brown failure criterion and variation analysis method. The numerical solution for the curvilinear function in fracture plane is obtained based on the finite difference theory, which more accurately reflects the failure state of the anchor cable, as opposed to that being assumed in advance. The results reveal that relying solely on a single failure mode for UPC calculations has limitations, as changes in parameter values not only directly impact the UPC value but also can alter the failure model and thus the calculation method.
  • YU Bo, TAI Shengping, ZHENG Kexun, CHEN Shiwan, HAN Xiao, WANG Senlin, ZUO Shuangying
    2024, 21(03): 1048-1057.
    Karst sinkholes with natural negative landform provide favorable conditions for the pumped storage reservoir construction for less excavation work. However, the construction of the reservoir would plug the natural karst channels for water and air, which would cause remarkable air pressure in karst channels when the groundwater level fluctuates. A large laboratory simulation test was carried out to study the air pressure variation of a reservoir built on the karst sinkhole. The air pressure in the karst channel and inside the model was monitored during the groundwater rising and falling process. Result showed that the variation of air pressure in the karst channel and the surrounding rock exhibited a high degree of similarity. The air pressure increased rapidly at the initial stage of water level rising, followed by a slight decrease, then the air pressure increased sharply when the water level approached the top of the karst cave. The initial peak of air pressure and the final peak of air pressure were defined, and both air pressure peaks were linearly increasing with the water level rising rate. The negative air pressure was also analyzed during the drainage process, which was linearly correlated with the water level falling rate. The causes of air pressure variation in karst channels of a pumped storage reservoir built on the karst sinkhole were discussed. The initial rapid increase, then slight decrease and final sudden increase of air pressure were controlled by the combined effects of air compression in karst channel and air seepage into the surrounding rock. For the drainage process, the instant negative air pressure and gradual recovering of air pressure were controlled by the combined effects of negative air pressure induced by water level falling and air supply from surrounding rock. This work could provide valuable reference for the reservoir construction in karst area.
  • CHENG Yun, SONG Zhanping, XU Zhiwei, YANG Tengtian, TIAN Xiaoxu
    2024, 21(03): 1058-1074.
    The deformation in sedimentary rock induced by train loads has potential threat to the safe operation of tunnels. This study investigated the influence of stratification structure on the infrared radiation and temporal damage mechanism of hard siltstone. The uniaxial compression tests, coupled with acoustic emission(AE) and infrared radiation temperature(IRT) were conducted on siltstones with different stratification effects. The results revealed that the stratigraphic structure significantly affects the stress-strain response and strength degradation characteristics. The mechanical parameters exhibit anisotropy characteristics, and the stratification effect exhibits a negative correlation with the cracking stress and peak stress. The failure modes caused by the stratification effect show remarkable anisotropic features, including splitting failure(Ⅰ: 0°-22.50°, Ⅱ: 90°), composite failure(45°), and shearing failure(67.50°). The AE temporal sequences demonstrate a stepwise response characteristic to the loading stress level. The AE intensity indicates that the stress sensitivity of shearing failure and composite failure is generally greater than that of splitting failure. The IRT field has spatiotemporal migration and progressive dissimilation with stress loading and its dissimilation degree increases under higher stress levels. The stronger the stratification effect, the greater the dissimilation degree of the IRT field. The abnormal characteristic points of average infrared radiation temperature(AIRT) variance at local stress drop and peak stress can be used as early and late precursors to identify fracture instability. Theoretical analysis shows that the competitive relationship between compaction strengthening and fracturing damage intensifies the dissimilation of the infrared thermal field for an increasing stress level. The present study provides a theoretical reference for disaster warnings in hard sedimentary rock mass.