过刊目录

  • 2020年, 17卷, 第05期
    刊出日期:2024-06-19
      

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  • SERRANO Enrique, LóPEZ-MORENO Juan Ignacio, GóMEZ-LENDE Manuel, PISABARRO Alfonso, MARTíN-MORENO Raúl, RICO Ibai, ALONSO-GONZáLEZ Esteban
    2020, 17(05): 1013-1031.
    Seasonally frozen ground, mountain permafrost and cryogenic geomorphological processes are important components of the Pyrenean high mountains. This work presents the results of a study on the distribution of frozen ground in a marginal and paraglacial environment of temperate mountains. An inventory was made of landforms and indicators of frozen ground, and frozen ground was mapped accordingly. During 2014 and 2016 ground temperatures and thermal regimes were monitored, basal temperatures of snow-cover(BTS) were measured and a thermal map was drawn. Differential thermal behaviours were detected among different elevations and slope orientations. Periglacial processes are the most widespread, in which frost weathering and nivation, together with gelifluction and cryoturbation, are the most efficient processes; the latter two are generally linked to the presence of frozen ground. The fall in air and ground temperatures with altitude, slope orientations, and snowpack thickness and evolution determine ground thermal regimes. In the study area, three types of thermal regimes were established: climate-controlled, snowcover-controlled, and frozen ground-controlled. Seasonally frozen ground occurs across a broad range of elevation between 2650 and 3075 m asl, whereas possible permafrost only occurs above 2750 m asl.
  • GU Zhen-kui, FAN Hui, LOU Jun-peng, YANG Kun
    2020, 17(05): 1032-1044.
    Understanding the evolution of the fluvial geomorphology in an orogenic belt provides valuable insight into the relationship between upper crustal deformation and surface processes. The upper Lancang-Mekong River is in an area experiencing both uplift and erosion. The related processes provide a steady sediment supply to the lower reaches of the river and play an important role in the regional environmental changes. The Xiaohei(Weiyuan) River Basin is an important sub-basin in this area, which is characterized by large-scale topographic fluctuations, active tectonics and erosion, and anthropogenic activities. These different factors introduce numerous complexities to the local surface processes. In this study, we investigate and quantify the controls of geomorphic evolution of the Xiaohei River Basin. We located and mapped the main knick-zones within the channels and examined the main genetic factors, such as faults and stratigraphic differences. The results show that the areas with the lowest uplift rates are characterized by a low steepness index and are located in the southeastern part of the basin. The stream power of the mainstream increases downstream, with an average value of ~122 W/m. The erosional activity of the various stream channels is intense. Overall, the basin tends to expansion, with only local instances of inward contraction. Our analysis confirms that a number of the geomorphic evolutionary characteristics of the Xiaohei River Basin are transient. In addition, the future potential for the increasing the number of dams and the hydropower development in the basin may weaken the expansion trend of the basin over a long period of time.
  • Markus GASTAUER, Jan THIELE, Stefan POREMBSKI, Andreza Viana NERI
    2020, 17(05): 1045-1059.
    Altitude and environmental variables such as edaphic properties are considered determinants of species distribution and community composition in mountain ecosystems. Here, we aimed to outline the effects of distinct mountain peaks, altitude and soil properties on community composition, species density, phylogenetic structure and diversity of angiosperm páramo communities from the Serra do Brigadeiro State Park, Minas Gerais, southeastern Brazil. For that, we identified all angiosperm species found in 300 plots(1 m × 1 m) from three mountain peaks, measured soil depth and analyzed soil fertility and texture in each plot. To reduce the number of soil variables and species composition, we computed principal coordinates based on soil properties and principal coordinates based on species-plot matrix for each plot. Furthermore, we computed the standard effect sizes of the mean phylogenetic pairwise distance and the mean nearest phylogenetic taxon distance for each plot to investigate differences in the degree of relatedness among coexisting species. We compared differences in response variables between peaks and modelled them in function of altitude and principle components of soil properties using mixed effect models. Species density and phylogenetic diversity differed between peaks, but, contrary to the previous findings, no relationships between species richness or phylogenetic diversity and altitude or soil properties were found, indicating that further investigations are necessary to understand the altitude-biodiversity relationship in Brazilian páramo vegetation. Community composition differed between peaks and depended on altitude, soil properties and interactions between them, indicating that upward shifting of bioclimatic conditions due to climate changes may alter communities of this ecosystem. Phylogenetic structure differed between peaks and was influenced by altitude and soil properties. As phylogenetic clustering increased with altitude, eventual upward movements of species in Brazilian páramo vegetation due to climate change may alter community composition and the degree of relatedness among coexisting species, increasing the risk of species from higher altitudes to disappear. Therefore, conservation priorities arise for higher landscape portions, where these high altitude species may find refuges.
  • Joanna Beata KOWALSKA, Bart?omiej KAJDAS, Tomasz ZALESKI
    2020, 17(05): 1058-1085.
    Six soils located within the Polish Carpathians, developed on calcium carbonate–rich sedimentary parent materials and representing various reference groups, were investigated in order to detect the lithic discontinuity. We propose using a multidirectional approach to assess the lithic discontinuity in these soils, one that includes grain size distribution, geochemical composition, heavy mineral content and micromorphology, supported by a traditional soil survey. A further aim of this process was to identify the possible admixture of allochthonous material of aeolian origin. The studied soils presented lithic discontinuities mostly at the contact of underlying calcium carbonate–rich coarsegrained slope deposits with the overlaying colluvium layer having a lower content of rock fragments. The significant changes in grain size distribution, especially in the silt and sand content, as well as high Uniformity Values and partially, high Lithological Discontinuity Index values, confirmed the occurrence of a lithic discontinuity in all studied soils. High heterogeneity in the soil profiles was also confirmed by the distribution of the major oxides; however, their distribution did not clearly indicate the lithic discontinuity. The most visible distinctions were noted from CaO content, which resulted from the deposition of carbonate-free materials(aeolian silts) and their mixing with the calcium carbonate–rich parent material. Furthermore, the analysis of heavy mineral content confirmed the allochthonous origin of the upper(and in some cases also the middle) parts of all profiles, which was manifested by the presence of highly weathering-resistant minerals such as zircon, epidote and various types of garnets. The micromorphological features of some of the studied soils showed distinctiveness within the soil profile, manifested by changes in b-fabric pattern, the occurrence and distribution of secondary carbonate and the coarse and fine coarse and fine ratio. Based on the high content of silt within the upper and middle parts of the soils, the content of Hf and Zr, as well as the higher content of weathering-resistant minerals, admixture of aeolian silt could be considered in some of the studied soils, yet with weak character. However, the dominance of minerals typical for metamorphic and igneous rocks suggested that the supply of aeolian silt was associated with loess covers rather than local sedimentary material.
  • Roya ABEDI, Tooba ABEDI
    2020, 17(05): 1084-1095.
    This study evaluated the total height of trees based on diameter at breast height by using 23 widely used height-diameter non-linear regression models for mixed-species forest stands consisting of Caucasian oak, field maple, and hornbeam from forests in Northwest Iran. 1920 trees were measured in 6 sampling plots(every sampling plot has 1 ha area). The fit of the best height–diameter models for each species were compared based on R2, Root Mean Square Error(RMSE), Akaike information criterion(AIC), standard error, and relative ranking performance criteria. In the final step, verification of results was performed by paired sample t-test to compare the observed height and estimated height. Results showed that among 23 height-diameter models, the best models were obtained from the top five ones including Modified-logistic, Prodan, Sibbesen, Burkhart, and Exponential. Comparison between the actual observed height and estimated height for Caucasian oak showed that Modified–Logistic, Prodan, Sibbesen, Burkhart, and Exponential performed better than the others, respectively(There were no statistically significant differences between observed heights and predicted height(p≥0.05)). Prodan, Modified-Logistic, Burkhart, and Loetch evaluated field maple tree height correctly, and Modified-Logistic, Burkhart, and Loetch had better fitness compared to the others for hornbeam, respectively. Although other models were introduced as appropriate criteria, they could not reliably predict the height of trees. Using the Rank analysis, the Modified-Logistic model for the Caucasian oak and Prodan model for field maple and hornbeam had the best performance. Finally, to complement the results of this study, it is suggested to assess how environmental factors such as elevation, climate parameters, forest protection policy and forest structure will modify height-diameter allometry models and will enhance the prediction accuracy of tree heights prediction in mixed stands.
  • Mohammad Mehdi HOSSEINZADEH, Saeedeh MATSH BEYRANVAND, Reza ESMAILI
    2020, 17(05): 1096-1105.
    Powerful alluvial rivers in the northern Alborz mountain ranges erode river banks due to having high slopes. Most of these rivers flow in forest areas. In this research, the rate of the river bank erosion was examined using the exposed roots of the trees. For this purpose, 8 reaches of Lavij Stream were investigated. To determine the first year of root exposure, two sets of macroscopic and microscopic indicators were utilized. Accordingly, the rate of the stream bank erosion was estimated. The results were analyzed by using statistical test, which showed insignificant differences between the two groups of indicators. Due to its more abundance(frequency) on the margins and easy detection of its root through the exposure(macroscopic and microscopic) indicators, Alnus glutinosa(black alder) species could be more easily and accurately analyzed as compared with any other tree species in the region. The mean erosion rate of the riverbank using the extruded roots was estimated to be 0.08 m/yr. The hydrological analyses of flood flows showed that 95% of Lavij Stream bank erosion was caused by the river bank full discharges with a return period of 1-3 years.
  • XIAO Yuan-ming, YANG Lu-cun, NIE Xiu-qing, LI Chang-bin, XIONG Feng, ZHOU Guo-ying
    2020, 17(05): 1106-1114.
    Biodiversity distribution patterns are a basic and long-standing but crucial aspect of ecology research. These patterns form the primary source of data used to develop biodiversity protection practices, especially in mountain ecosystems. Shrubs comprise one of the main types of vegetation on the Qinghai–Tibetan Plateau, where they serve vital ecological functions. In this study, we used a community phylogenetic approach to examine the distribution patterns of shrub communities along the longitudinal and latitudinal gradients on the northeastern Qinghai–Tibetan Plateau. We observed significant latitudinal trends in both the phylogenetic diversity(PD) and net relatedness index(NRI) values of shrub communities, such that the former decreased and the latter increased with increasing latitude. However, no significant PD, NRI and nearest taxon index(NTI) distribution patterns were observed along a longitudinal gradient. A further analysis revealed that the combination of temperature-related and precipitation-related climate variables most strongly affected the PD, NRI and NTI values of shrub communities, indicating that the latitudinal patterns in the PD, NRI and NTI of a shrub community may be determined mainly by interactions with these climate factors.
  • Bimal Raj SHRESTHA, Binu TIMSINA, Zuzana MüNZBERGOVá, Tomá? DOSTáLEK, Prakash GAUDEL, Tej B.BASNET, Maan B.ROKAYA
    2020, 17(05): 1115-1138.
    Butterflies are widely studied due to their key ecosystem functions. For this reason, they are used in ecosystem assessment, formulating conservation plans and in raising the environmental awareness. Quantification of different factors affecting diversity of butterflies is important for their effective conservation. In this study, we investigated abiotic and biotic factors affecting species richness and community composition of butterflies along an elevational gradient in Manang region, central Nepal. We also tested if butterfly species follow the Bergmann's rule. A total of 57 butterfly species belonging to 39 genera and 8 families were recorded in the study area. Out of a total of 127 plant species identified in the study region, only 67 plant species were visited by butterflies as nectar sources. Species richness of butterflies increased with increasing elevation. Species richness was significantly higher in places with shrubs compared to other places and also in autumn than in summer. Species richness of butterflies also depended on composition of plant species occurring at the localities. Butterfly species composition varied among sampling localities. It was also determined by habitat type, elevation, sampling time, plant species and interactions of elevation × time. The relationship between butterfly size and elevation was in the opposite direction than expected according to the Bergmann's rule. In conclusion, protection of butterfly diversity can only be achieved by protecting different habitats across the diverse physiography of the region and different plant species, in particular herbs and shrubs. Our results do not support the Bergmann's rule for butterflies along an elevational gradient in our region.
  • HUANG Qiu-xiang, XU Xiang-tao, P.H.S.W.KULATILAKE, LIN Feng
    2020, 17(05): 1128-1148.
    This case study is about a landslide that occurred after 4 days of heavy rainfall, in the morning of June 29, 2012, in Cengong County, Guizhou Province of China, geographical coordinated 108°20′-109°03′E, 27°09′-27°32′N, with an estimated volume of 3.3×106 m3. To fully investigate the landslide process and formation mechanism, detailed geotechnical and geophysical investigations were performed including borehole drilling, sampling, and laboratory tests coupled with monitoring of displacement. Also, a combined seepage-slope stability modeling was performed to study the behavior of the landslide. After the heavy rainfall event, the sliding process started in this area. The landslide development can be divided into different parts. The man-made fill area, spatially distributed in the south side of the landslide area with low elevations, slid first along the interface between the slope debris and the strongly weathered bedrock roughly in the EW direction. Consequently, due to severe lateral shear disturbance, the slope in the main sliding zone slid next towards the SW direction, along the sliding surface developed within the strongly weathered calcareous shale formation located at a depth of 25-35 m. This means it was a rainfall triggered deep-seated landslide. Finally, retrogressive failure of a number of upstream blocks occurred, which moved in more than one direction. The initial failure of the man-made fill area was the ‘engine' of the whole instability framework. This artificial material with low permeability, piled up in the accumulation area of surface and sub-surface and destroyed the drainage capacity of the groundwater. The numerical modeling results agreed with the analysis results obtained from the laboratory and field investigations. A conceptual model is given to illustrate the formation mechanism and development process of the landslide.
  • ZHOU Ze-Hua, LYU Yan, SU Sheng-rui, LIU Shi-jie, ZHAO Hui, LI Peng, ZHOU Yang
    2020, 17(05): 1143-1165.
    Analyzing large prehistoric rock avalanches provides significant data for evaluating the disaster posed by these relatively infrequent but destructive geological events. This paper attempts to study the characteristics and dynamics of the Ganqiuchi granitic rock avalanche, in the middle of the northern margin of Qinling Mountains, 30 km to the south of Xi'an, Shaanxi Province, China. In plane view, this rock avalanche is characterized by source area, accumulation area and dammed lake area. Based on previous studies, historical records and regional geological data, the major trigger of the Ganqiuchi rock avalanche is considered to be a strong paleo-earthquake with tremendous energy. The in situ deposit block size distributions of the intact rock mass and the debris deposits are presented and analyzed by using a simple model for estimating the number of fragmentation cycles that the blocks underwent. The results show that the primary controlling factor of the fragmentation process is the pre-existing fractures, and there is a relationship between the potential energy and the fragmentation energy: the latter is approximately 20% of the former. Based on the dynamic discrete element technique, the study proposes a four-stage model for the dynamic course of the Ganqiuchi rock avalanche:(1) failing;(2) highspeed sliding;(3) collision with obstacles;(4) decelerated sliding, which has implication for hazard assessment of the potential rock avalanches in China and other countries with similar geological setting.
  • FRASCA Marco, VACHA Damiano, CHICCO Jessica, TROILO Fabrizio, BERTOLO Davide
    2020, 17(05): 1161-1171.
    In the warm summer of 2017, a landslide failed from the south-east side of the Col des Clochettes on the top of the underlying Trajo Glacier. The study area is at an elevation of about 3500 m a.s.l. in the Gran Paradiso Massif and can be hardly reached by walking from Cogne(Aosta Valley, NW Italy). Studies conducted by field surveys, photogrammetry(structure from motion) and satellite images analysis, integrated with the evaluation of data from meteorological stations have been used to reconstruct the phenomenon and infer its causes. The site is very complex to be studied especially due to logistic problems, therefore, measurements and observations that are common practice in other landslides are very difficult to apply here. So, many of the results achieved are not adequately supported by field studies. Anyway, the following factors could have affected the stability of the slope: i) the tectonic structure of the area, which is reflected on the morphology and on the geomechanics characteristics of the rock masses; ii) the meteorological conditions during 3 months before the main failure, resulting in an extremely high temperature compared to historical data. Moreover, the analysis of multitemporal satellite images allowed to recognize that it was not a single landslide but that the phenomenon is articulated over time in at least five failures in about 2 months. Moreover, several predisposing factors may have been playing an important role in causing the instability: the degradation of permafrost(probably affecting rock mass due to the circulation of warm air and water in the discontinuity systems), the alternance of the freeze-thaw cycles and the availability of a considerable amount of water from rainfalls and nival fusion infiltrating deeply in the rock mass. More common causes such as rains and earthquakes have been excluded.
  • WANG Lan-sheng, WANG Xiao-qun, SHEN Jun-hui, YIN Guan, CUI Jie, XU Xiang-ning, ZHANG Zhi-long, WAN Tao, WEN Li-wang
    2020, 17(05): 1172-1191.
    In 1999, Diexi paleo-dammed lake(2349 m a.s.l.) was discovered around Diexi town along the Minjiang River in Sichuan province. Diexi is located where the eastern edge of the Tibetan Plateau and the Sichuan Basin meet. The dammed lake was formed during the Last Glacial Maximum of the Late Pleistocene(~30,000 years ago) and began to empty about 15,000 years ago. The lacustrine sediments(up to 240 m thick) preserve abundant paleoenvironment information. In this paper, a mass of oxygen isotopes and 14 C dating from drilled cores are analyzed and discussed. The δ18 O curve on the paleo climate from this section is comparable with the coeval paleo climatic curves of ice cores and karsts in China and others. Furthermore, the physical model testing has confirmed that the disturbed zones in the core are caused by strong earthquakes occurred at least 10 times, which implies strong crustal deformation, as an important driving force, affecting climate change. This study provides a new window to observe East Asian monsoon formation, paleoenvironmental evolution and the global climate change.
  • LIU Bo, HU Xie-wen, HE Kun, HE Shu-heng, SHI Hong-bin, LIU Ding-yi
    2020, 17(05): 1188-1209.
    The "5.12" Wenchuan earthquake in 2008 triggered a large number of co-seismic landslides. The rear boundary or cracks of co-seismic landslide are generally located at the steep free surface of thin or thick mountains. Dynamic process of this kind of landslides could be divided into two parts: the seismic dynamic response of the slope and the movement process of rock mass. Taking the Laoyingyan rockslide as an example, the amplification effect was studied by single-degree-of-freedom system analysis method. Besides, the dynamic process of landslide under seismic loading was simulated by the finite difference method(FDM) and discrete element method(DEM). The amplification coefficient of the rockslide to seismic wave is 1.25. The results show that the critical sliding surface of the Laoyingyan rockslide was formed at the 23 th seconds under the action of seismic wave. At the same time, tension failure occurred at the rear edge of the sliding mass and shear failure occurred at the front edge. The maximum displacement was 0.81 m and the initial velocity was 2.78 m/s. During the initiation process of the rockslide, the rock mass firstly broke down along the joints which are along the dip of the rock stratum, and then collapsed bodily along the secondary structural planes. In the process of movement, the maximum velocity of rock mass was 38.24 m/s. After that, the rock mass underwent multiple collisions, including contact, deceleration to 0 and speed recovery after rebound. Finally, due to the constant loss of energy, the rocks stopped and accumulated loosely at the foot of the slope. The longest distance of movement was about 494 m. Besides, the smaller the damping ratio, the farther the rock mass moved. Compared with the results without considering the amplification factor, the movement distance of landslide by considering the amplification factor was more accurate. The study of the Laoyingyan rockslide is helpful to strengthen our field identification of potential co-seismic rockslides. At the same time, understanding its movement and accumulation process can help us better predict the hazard scope of the co-seismic rockslides, and provide a reference for the design of treatment projects.
  • SU Fang, YIN Ya-juan
    2020, 17(05): 1206-1220.
    Achieving sustainable livelihood is the ultimate goal of poverty alleviation efforts in mountainous areas, and selecting an optimal livelihood strategy for different poverty-type farmers greatly improves farmers' livelihood capital, resists livelihood risks, and promotes sustainable development. For farmers, optimal livelihood strategy means better employment opportunities, higher family income(or better income structure), and stronger employability or development potential. This paper classifies different types of farmers' poverty on the basis of a quantitative evaluation of farmers' livelihood capital in the Qin-ba Mountain Area in South-Shaanxi by using the k-means clustering method and subsequently the fuzzy evaluation method to evaluate the effectiveness of farmers' livelihood strategies. Then, the multi-attribute decision-making model is used to analyze the selection of optimal livelihood strategies for different poverty-type farmers. The results suggest a significant difference in the selection of the optimal livelihood strategy for different poverty-type farmers. Farmers without financial and human capital choose to "go out to work," farmers lacking natural capital choose to "acquire social insurance and government relief," farmers without physical capital choose to "use loans," and farmers lacking social capital choose to "use savings." Studying the selection of optimal livelihood strategies for different poverty-type farmers can help to propose targeted sustainable livelihood optimization programs for farmers and accelerate efforts to overcome poverty in mountainous areas.
  • HAN Hui-qing, LIU Yue, GAO Hong-juan, ZHANG Ying-jia, WANG Zhe, CHEN Xiao-qiao
    2020, 17(05): 1221-1236.
    Under the influence of various natural and human factors, the relationship between the ecosystem services provided for human beings by a karst ecosystem is becoming increasingly complex, profoundly limiting the effective and sustainable development of the social economy and ecosystem protection in karst areas. Taking Guizhou, China as an example, which includes both karst(including five different landforms) and non-karst area, the study explored and compared the tradeoff and synergy between ecosystem services in both terrain types. The results showed higher change rates of water yield and soil retention in karst areas than those in non-karst areas, with only small differences in the carbon storage and crop production change. The ecosystem service relationships in the karst area from 1995 to 2005 were consistent with the relationships in the non-karst area. However, differences were observed in most of these relationships from 2005 to 2015. The relationships between ecosystem services in different karst landforms from 1995 to 2005 remained the same, but there are differences found in the relationships of ecosystem services from 2005 to 2015. The trade-off and synergistic relationships between ecosystem services in the different landforms were closely related to the changes of climate and land use, particularly related to rainfall, rainfall erosivity, farmland, and forestland.
  • ZHANG Yu-xin, WANG Yu-kuan, FU Bin, DIXIT Amod Mani, CHAUDHARY Suresh, WANG Shan
    2020, 17(05): 1235-1250.
    It is necessary to understand vegetation dynamics and their climatic controls for sustainable ecosystem management. This study examines the vegetation dynamics and the effect of climate change on vegetation growth in the pristine conditions of 58 woodland National Nature Reserves(NNRs) located in the upper Yangtze River basin(UYRB) in China which are little influenced by human activities. Changes in the normalized difference vegetation index(NDVI), precipitation, and temperature in the selected NNRs were observed and analyzed for the period between 1999 and 2015. The relationship between time-lag effect of climate and changes in the NDVI were assessed using Pearson correlations. The results showed three major trends. 1) The NDVI increased during the study period; this indicates an increase in the amount of green vegetation, especially due to the warmer climate during the growing season. The NDVIs in March and September were significantly affected by the temperature of the previous months. Spring temperatures increased significantly(P < 0.05) and there was a delay between climatic factors and their effect on vegetation, which depended on the previous season. In particular, the spring temperature had a delayed effect on the NDVI in summer. 2) The way in which vegetation responds to climatic factors varied significantly across the seasons. Temperature had a greater effect on the NDVI in spring and summer and the effect was greater at higher altitudes. A similar trend was observed for precipitation, except for altitudes of 1000–2000 m. 3) Temperature had a greater effect on the NDVI in spring and autumn at higher altitudes. The same trend was observed for precipitation in summer. These findings suggest that the vegetation found in NNRs in the upper reaches of the Yangtze River was in good condition between 1999 and 2015 and that the growth and development of vegetation in the region has not been adversely affected by climate change. This demonstrates the effectiveness of nature reserves in protecting regional ecology and minimizing anthropogenic effects.
  • ZHANG Jian-jing, NIU Jia-yong, FU Xiao, CAO Li-cong, XIE Qiang
    2020, 17(05): 1251-1269.
    As a combined supporting structure, the anchor cable and lattice beam have a complex interaction with the slope body. In order to investigate the seismic behaviors of the slope reinforced by anchor cable and lattice beam, a largescale shaking table test was carried out on a slope model(geometric scale of 1:20) by applying recorded and artificial seismic waves with different amplitudes. The acceleration and displacement of the slope, the displacement of lattice beam and the axial force of anchor cable were obtained to study the interaction between the slope and the supporting structure. The test results show that:(1) the acceleration responses of the slope at different relative elevations display obvious nonlinear characteristics with increasing of the peak ground acceleration(PGA) of the inputted seismic waves, and the weak intercalated layer has a stronger effect on acceleration amplification at the upper part of the slope than that at the lower part of the slope;(2) the frequency component near the second dominant frequency is significantly magnified by the interaction between the slope and the supporting structure;(3) the anchor cables at the upper part of the slope have larger peak and residual axial forces than that at the lower part of the slope, and the prestress loss of the anchor cable first occurs at the top of the slope and then passes down;(4) the peak and residual displacements inside the slope and on the lattice beam increase with the increase of relative elevation. When the inputted PGA is not greater than 0.5 g, the combined effect of anchor cable and lattice beam is remarkable for stabilizing the middle and lower parts of the potential sliding body. The research results can provide a reference for the seismic design of such slope and the optimization of supporting structure.
  • ZHU Hong-wei, YAO Ling-kan, XU Guang-xing
    2020, 17(05): 1269-1280.
    The stability and seismic behavior of geosynthetic-reinforced embankments during the earthquake is not well known. In this paper, the damage types of embankments were summarized, and the seismic stability of reinforced embankment were analyzed through an earthquake damage investigation in the Wenchuan earthquake region. Then, large-scale shaking table model tests were performed on the geosynthetic-reinforced embankment. The results show that the damage level of the reinforced embankment was almost less than that of the unreinforced embankment. The peak seismic earth pressure was nonlinear along the height of the embankment, the largest peak seismic earth pressure was roughly in the middle of the embankment slope. The peak ground accelerations(PGA) amplification factor first showed an increasing pattern and then a decreasing pattern with the increase of elevation, but there was a final increasing trend along the height of the reinforced embankment. The results can help to establish the proper design of the reinforcement embankments under earthquake conditions.