过刊目录

  • 2023年, 20卷, 第08期
    刊出日期:2024-06-19
      

  • 全选
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  • ZHANG Qi-yuan, HU Kai-heng, LIU Shuang, LIU Wei-ming
    2023, 20(08): 2107-2132.
    The regional distribution of landslide dams can provide valuable insights into the interactions among various factors, including lithology, topography, climate, and fluvial landforms in tectonically active mountains. Himalayan rivers are frequently impacted by large-scale landslide damming, which profoundly influence fluvial geomorphology. In this study, we identified 1652 landslide dams in four major rivers of Bhutan and its surrounding area by remote sensing interpretation. Notably, approximately 71% of these landslide dams are found in regions composed of quartzite or gneiss. Fault-related tectonic activity plays a significant role in governing the distribution of these landslide dams, as approximately 83% of the mapped landslide dams are found within a 10 km radius of the nearest fault. The majority of the identified landslide dams are situated in areas with relatively modest local relief, ranging from 227 m to 327 m. These dams tend to cluster in the tributaries, and the stream power of almost 95% of them is typically below 1×10~6 kg m~2 s~(-3). Our data, combining the erosion rate and kernel density map of the landslide dams, reveals that regions with high erosion rates do not consistently align with the major high-density distribution of landslide dams. It is shown that the distribution of landslide dams is strongly influenced by the valley form. In comparison to U-shaped valleys, V-shaped valleys exhibit a higher density of landslide dams. Intriguingly, we also find a positive correlation between the landslide-dam distribution density and the erosion rate only in relatively arid regions with mean annual rainfall less than 500 mm. Moreover, the length of the upstream reach protected by the knickpoint associated with both lithology and landslide damming is about three times longer than that protected by the knickpoint associated only with landslide damming.
  • XIONG Bo-bo, YANG Shi-jie, ZHAO Bing-qin, LU Xiao-chun, TIAN Bin, LI Cheng, WU Xuan-xuan, TU Xiao-long
    2023, 20(08): 2133-2148.
    High-density resistivity imaging method is widely used in landslide monitoring. The resistivity of rock and soil is closely related to factors, such as porosity, moisture content, saturation and temperature. In this study, the resistivity test was designed to investigate the influence of physical factors and pore solution components on the resistivity of landslide soil. Experimental and analytical results find that both moisture content and volumetric water content varies greatly under the same resistivity. At different temperatures, soil resistivity exhibits great changes. Under the same temperature, the ion concentration and species in pore solutions have great influence on soil resistivity. Based on the test results and grey correlation analysis,this study established a resistivity model by considering porosity, saturation, temperature and ion concentration. The study lays a foundation for the high-density resistivity method to measure the moisture content of landslides.
  • NIGRELLI Guido, CHIARLE Marta
    2023, 20(08): 2149-2163.
    Alps are an important geographical area of the European continent and, in this area, temperature increase is most evident. However, the 1991-2020 climate normal in the Alps has still not been thoroughly investigated. Aiming to fill this gap with a focus on high-elevation environments, minimum and maximum daily air temperature acquired by 23 automatic weather station were used. The results show that the mean annual values of minimum and maximum temperature for the 1991-2020 climate normal in the Alps are-2.4°C and 4.4°C, respectively, with a warming rate of 0.5°C/10 years. The mean annual temperature comparison between 1961-1990 and 1971-2000, 1961-1990 and 1981-2010, 1961-1990 and 1991-2020 climate normal show an increase of 0.3°C, 0.5°C and 0.9°C, respectively. The results also confirm that seasonal and annual temperatures are rising through the whole Alpine arc, mainly in summer and autumn. This work highlights that annual minimum and maximum temperature do not seem to be affected by a positive elevation-dependent warming. Instead, a positive elevation-dependent warming in the maximum values of the annual minimum temperature was found. If anthropogenic emissions maintain the trend of the last decades, the expected mean annual temperature of the 2001-2030 climate normal is-0.2°C, with an increase of 0.5°C if compared to the 1991-2020 climate normal and with an increase of 1.5°C if compared to the 1961-1990 climate normal.This study highlights the warming rate that is now present in the European Alps, provides indications on the warming rate that will occur in the coming years and highlights the importance of carrying out investigations that consider not only the last 30-year climate normal, but also the most recent 30-year climate normal by comparing them with each other.
  • GUO Xiao-hua, FORMAN Steven, WANG Yuan-yuan, ZHANG Yu-feng, LIU Xin-yu
    2023, 20(08): 2164-2180.
    The Yellow River is usually assumed to record tectonic activities and climatic changes; however, a systematic study was lack in the sedimentology, stratigraphy, geomorphology and geochronology for the entire Yellow River though various geologic scholars have conducted numerous works in individual basins. This review focused on well-preserved fluvial terrace sequences that formed along this river on northeastern(NE) Tibetan Plateau and Ordos Block over the past 2.6 Ma. After comparing numerous initial incision ages at different segments along the Yellow River, we found out that the youngest initial incision may occur at ca. 150 ka at the Longyang Gorge. The Yellow River may transit from multiple separated endorheic drainages to an entire external drainage after 150 ka, which may cause differentiations in the apparent incision rates before and after 150 ka; thus apparent net incision rates were calculated respectively for the Yellow River before 150 ka and the drainage network post 150 ka. Apparent net incision rates prior to 0.15 Ma were calculated as 0.15, 0.29, 0.10, 0.12 and 0.03 mm/a respectively in Tongde-Xunhua, Lanzhou-Linxia basins, Heishan, Jinshan and Fenwei-Sanmen Gorges in this review, which mainly reflected Kunhuang-Gonghe Tectonic Event, generated by the Indo-Asian collision and diminishing as the NE Tibetan Plateau eastward extruding at ca. 1.8-0.15 Ma. Apparent net incision rates post 0.15 Ma were calculated respectively for NE Tibetan Plateau and Ordos Block, considering their different base level. On NE Tibetan Plateau, four fluvial degradational phases were identified between ca.105~70, 53~40, 25~16 and 12~6 ka associated with terrace levels respectively, at average elevations of 96, 40, 20 and 10.5 meters above the current river level(m arl) within a range of 5 ~ 96 m arl; and four broad periods in the last 150 ka on Ordos Block: possibly marine oxygen isotope stage(MIS) 5, ca. 118 to 72 ka, most of MIS 3, ca. 44~28 ka, transition from LGM to last deglacial ca. 20 to 16 ka, and 4~3 ka at average elevations of 67.5, 26, 19 and 11.5 m arl. These degradational phases post 0.15 Ma were associated with multiple processes including enhanced fluvial discharge with an increase in monsoonal precipitation and/or melt water in deglaciation.
  • ZHAO Xin-yue, ZHAO Mao-qiang, WANG Pan-pan, DAI Yu-quan, PU Wan-qiu, HUANG Cheng-min
    2023, 20(08): 2181-2196.
    Since natural restoration combined with artificial auxiliary measures may achieve a relatively rapid restoration effect at a lower cost, it has become an essential measure for the ecological restoration of rock slopes. Previous studies have focused heavily on the relationship between substrate nutrients and water conditions and the development of mosses on the rock surface, but quantitative characterization of substantial effect of rock surface texture(e.g., microrelief) on moss growth is absent. The undulating microrelief on the rock surface can increase the heterogeneity of the microhabitat, which may be an important factor affecting the development of mossdominated biocrusts. In this study, the roughness of rock surfaces, moss coverage and biomass, weight and major nutrient contents of soils within the biocrusts were measured in the western mountainous area of Sichuan Province, Southwest China to further examine the role of rock surface microrelief in the biocrusts. The results showed that three main factors affecting the development of the biocrusts were bryophyte emergence, soil accumulation, and lithology. The presence of moss accelerates soil formation on rock surfaces and lead to the accumulation of nutrients so that all parts of the moss-dominated biocrusts system can develop synergistically. It was found that a microrelief structure with a roughness between 1.5 and 2.5 could gather soil and bryophyte propagules effectively, which may have a strong relationship with the angle of repose. When the roughness is 1.5, the corresponding undulation angle is very close to the theoretical minimum value of the undulation angle calculated according to the relationships between the undulation angle of the protrusion, slope and angle of repose.
  • SUI Qi-ru, CHEN Qin-huang, WANG Dan-dan, TAO Zhi-gang
    2023, 20(08): 2197-2213.
    Earthquakes can cause violent liquefaction of the soil, resulting in unstable foundations that can cause serious damage to facilities such as buildings, roads, and dikes. This is a primary cause of major earthquake disasters. Therefore, the discrimination and prediction of earthquake-induced soil liquefaction has been a hot issue in geohazard research. The soil liquefaction assessment is an integral part of engineering practice. This paper evaluated a dataset of 435 seismic sand liquefaction events using machine learning algorithms. The dataset was analyzed using seven potential assessment parameters. Ten machine learning algorithms are evaluated for their ability to assess seismic sand liquefaction potential, including Linear Discriminant Analysis(LDA), Quadratic Discriminant Analysis(QDA), Naive Bayes(NB), KNearest Neighbor(KNN), Artificial Neural Network(ANN), Classification Tree(CT), Support Vector Machine(SVM), Random Forest(RF), e Xtreme Gradient Boosting(XGBoost), Light Gradient Boosting Machine(Light GBM). A 10-fold cross-validation(CV) method was used in the modeling process to verify the predictive performance of the machine learning models. The final percentages of significant parameters that influenced the prediction results were obtained as Cyclic Stress Ratio(CSR) and Shear-Wave Velocity( VS1) with 56% and 38%, respectively. The final machine learning algorithms identified as suitable for seismic sand liquefaction assessment were the CT, RF, XGBoost algorithms, with the RF algorithm performing best.
  • LI Xia, ZHU Wan-ze, WANG Wen-wu, MA Sheng-lan, SHENG Zhe-liang, SHU Shu-miao
    2023, 20(08): 2214-2227.
    Bauhinia faberi via. Microphylla(BFM) is an important tree species for vegetation restoration in the dry valley of southwestern China. However, there were few studies on the application of arbuscular mycorrhizal fungi(AMF) in improving the drought adaptation of BFM. In order to investigate the response of BFM to water stress(WS), we tested four inoculation treatments((no AMF, Control), Glomus mosseae(GM), Glomus intraradices(GI), Glomus mosseae + Glomus intraradices(GMI)) in pots, experimented under three field water holding capacity(WHC) of 70%, 50% and 30%. The changes of seedling survival rate(SR), AMF relative root length colonization rate(Col), growth, photosynthetic parameters, water status and leaf nutrients were examined. The results showed that under 30% WHC drought conditions, SR with dual inoculation of AMF was not higher than with single inoculation of GM, suggesting that increasing the diversity of AMF did not definitely improve plant SR, and that the species of inoculated AMF might have an important impact on SR. The sensitivity of dual inoculated Col to water stress was lower than that of single inoculation, which was more favorable for dual inoculated BFM seedlings adapting to drought environment. The overall drought resistance ability(D) also showed that dual inoculation of AMF improved plant drought adaptation compared with single inoculation, which was related to the higher Col of dual inoculated AMF. This study is of practical importance to promote vegetation restoration in arid areas in a cost-effective and environmentally friendly manner.
  • WANG Jian-yong, ZHANG Zhi-xiang
    2023, 20(08): 2228-2241.
    Several plant micro-reserves were established to preserve the vegetation in local mountain areas during the construction of the Yanqing competition zone of the 2022 Beijing Winter Olympics. The spatial patterns of the main species in one of the micro-reserves and the factors affecting these patterns were characterized in this study. The distribution of arbor species was found to be mostly aggregated, especially at fine scales(< 5 m). Minor species were found to be more aggregated than the major species in each forest layer. The spatial patterns were found to be affected by habitat heterogeneity, intraspecific relationships, interspecific competition, and seed dispersal limitation. Habitat heterogeneity was found to affect large-scale spatial patterns, and its effects were observed throughout population development. Interspecific competition is another factor affecting the distribution of the species, and its effects were stronger during the later stages of population development. Habitat heterogeneity was found to affect competition among species and is key for species coexistence. Both these processes are affected by the seed dispersal limitation, and intraspecific relationships are a legacy of seed dispersal. The point patterns can be used as a tool for the initial assessment of the status of communities within micro-reserves. The consideration of these relationships in the development, management, and formulation of policies for micro-reserves in mountainous areas will facilitate the achievement of conservation goals. The careful consideration of habitat conditions when selecting sites for micro-reserves establishment can promote species conservation.
  • Agumassie Genet GELA, Daniel Ayalew MENGISTU, Daniel Asfaw BEKELE
    2023, 20(08): 2242-2262.
    Soil erosion and the subsequent sedimentation are serious environmental problems. Improper land management coupled with intense rainfall has complicated the problem in the Ethiopian highlands. Consequently, soil loss costs a profound amount of the national GDP and deters land productivity. Quantifying soil loss and prioritizing areas for conservation is imperative for proper planning and resource management. Therefore, this study aimed at estimating the mean annual soil loss rate of Gilgel Abay watershed which has critical implications on Lake Tana and Abbay River(Upper Blue Nile River), using RUSLE and morphometric analysis methods. Datasets including rainfall, soil, Digital Elevation Model and land use/land cover were used to generate important parameters required for the soil loss estimation. Data collected through field observation, consultation with experts and document analysis were used for validation purposes. The results of the study reveal that the watershed experienced an average soil loss rate of 39.8 t ha~(-1) yr~(-1). Subsequently, nearly 25%(37,038 ha) of the watershed is threatened by moderate to very severe soil loss. Among the four sub watersheds, sub watershed 3(S3) and sub watershed 4(S4), which consist of about 65%(105,000 ha) of the total area of the study watershed, experienced an annual soil loss rate of over 30 t ha~(-1) yr~(-1). The amount of soil loss that the study watershed has experienced is above the soil loss tolerance level of Ethiopia(2-18 t ha~(-1) yr~(-1)) and the tropical region(10 t ha~(-1) yr~(-1)). Similarly, the results of morphometric analysis showed that the studied watershed has S-shaped hypsometric curve, an indication for maturity stage of landscape development. The studied watershed is also characterized by a non-circular shaped drainage with rugged and dissected topography that contributes to high flash flood, peak discharge and incidence of soil loss. The result of both models signified that S3 and S4 are highly susceptible to soil erosion. Therefore, these two sub watersheds need priority for soil and water conservation(SWC) measures. Furthermore, the study demonstrated the importance of the integration of different models in the identification of soil erosion prone areas and prioritization for the proper implementation of SWC measures.
  • Zeshan ALI, Mudassar IQBAL, Ihsan Ullah KHAN, Muhammad Umer MASOOD, Muhammad UMER, Muhammad Usama Khan LODHI, Muhammad Atiq Ur Rehman TARIQ
    2023, 20(08): 2263-2281.
    Climate change strongly influences the available water resources in a watershed due to direct linkage of atmospheric driving forces and changes in watershed hydrological processes. Understanding how these climatic changes affect watershed hydrology is essential for human society and environmental processes. Coupled Model Intercomparison Project phase 6(CMIP6) dataset of three GCM's(BCC-CSM2-MR, INM-CM5-0, and MPIESM1-2-HR) with resolution of 100 km has been analyzed to examine the projected changes in temperature and precipitation over the Astore catchment during 2020-2070. Bias correction method was used to reduce errors. In this study, statistical significance of trends was performed by using the Man-Kendall test. Sen's estimator determined the magnitude of the trend on both seasonal and annual scales at Rama Rattu and Astore stations. MPI-ESM1-2-HR showed better results with coefficient of determination(COD) ranging from 0.70-0.74 for precipitation and 0.90-0.92 for maximum and minimum temperature at Astore, Rama, and Rattu followed by INM-CM5-0 and BCC-CSM2-MR. University of British Columbia Watershed model was used to attain the future hydrological series and to analyze the hydrological response of Astore River Basin to climate change. Results revealed that by the end of the 2070s, average annual precipitation is projected to increase up to 26.55% under the SSP1-2.6, 6.91% under SSP2-4.5, and decrease up to 21.62% under the SSP5-8.5. Precipitation also showed considerable variability during summer and winter. The projected temperature showed an increasing trend that may cause melting of glaciers. The projected increase in temperature ranges from-0.66°C to 0.50°C, 0.9°C to 1.5°C and 1.18°C to 2°C under the scenarios of SSP1-2.6, SSP2-4.5 and SSP5-8.5, respectively. Simulated streamflows presented a slight increase by all scenarios. Maximum streamflow was generated under SSP5-8.5 followed by SSP2-4.5 and SSP1-2.6. The snowmelt and groundwater contributions to streamflow have decreased whereas rainfall and glacier melt components have increased on the other hand. The projected streamflows(2020-2070) compared to the control period(1990-2014) showed a reduction of 3%-11%, 2%-9%, and 1%-7% by SSP1-2.6, SSP2-4.5, and SSP5-8.5, respectively. The results revealed detailed insights into the performance of three GCMs, which can serve as a blueprint for regional policymaking and be expanded upon to establish adaption measures.
  • SUN Tao, YANG Yan-mei, WANG Ze-gen, YONG Zhi-wei, XIONG Jun-nan, MA Guo-li, LI Jie, LIU Ao
    2023, 20(08): 2282-2297.
    Protecting the ecological security of the Qinghai-Tibet Plateau(QTP) is of great importance for global ecology and climate. Over the past few decades, climate extremes have posed a significant challenge to the ecological environment of the QTP. However, there are few studies that explored the effects of climate extremes on ecological environment quality of the QTP, and few researchers have made quantitative analysis. Hereby, this paper proposed the Ecological Environmental Quality Index(EEQI) for analyzing the spatial and temporal variation of ecological environment quality on the QTP from 2000 to 2020, and explored the effects of climate extremes on EEQI based on Geographically and Temporally Weighted Regression(GTWR) model. The results showed that the ecological environment quality in QTP was poor in the west, but good in the east. Between 2000 and 2020, the area of EEQI variation was large(34.61% of the total area), but the intensity of EEQI variation was relatively low and occurred mainly by a slightly increasing level(EEQI change range of 0.05-0.1). The overall ecological environment quality of the QTP exhibited spatial and temporal fluctuations, which may be attributed to climate extremes. Significant spatial heterogeneity was observed in the effects of the climate extremes on ecological environment quality. Specifically, the effects of daily temperature range(DTR), number of frost days(FD0), maximum 5-day precipitation(RX5day), and moderate precipitation days(R10) on ecological environment quality were positive in most regions. Furthermore, there were significant temporal differences in the effects of consecutive dry days(CDD), consecutive wet days(CWD), R10, and FD0 on ecological environment quality. These differences may be attributed to variances in ecological environment quality, climate extremes, and vegetation types across different regions. In conclusion, the impact of climate extremes on ecological environment quality exhibits complex patterns. These findings will assist managers in identifying changes in the ecological environment quality of the QTP and addressing the effects of climate extremes.
  • LI Feng-jiao, LIAO Xia, LIU Jia-ming, JIANG Li-li, WANG Meng-di, LIU Jin-feng
    2023, 20(08): 2298-2314.
    A favorable tourism image of high-quality mountain scenic spots(HQMSS) is crucial for tourism prosperity and sustainability. This paper establishes a framework for investigating the tourism image based on cognitive-emotion theory and uses natural language processing(NLP) tools to clarify the cognition, emotion, and overall tourist image of the HQMSS in China from the perspective of tourist perception. This paper examines the multi-dimensional spatial differentiation of China's overall image, including province, scenic spot scales, as well as the spatial pattern of the overall comprehensive tourism image. Strategies for comprehensively improving HQMSS's tourism image are also formulated. The results show that:(1) The cognitive image of Chinese HQMSS is categorized into core and marginal images, and the core images such as scenery and cable car are the expression of the uniqueness of mountainous scenic spots. Additionally, the cognitive image is classified into six dimensions: tourism environment, tourism supporting facilities, tourism experience, tourism price, tourism service, and tourism safety.(2) Positive emotions are the dominant mood type of HQMSS in China, followed by neutral emotions, with negative emotions being the least frequent. Emotional images vary across dimensions, with tourism environment and tourism experience evoking relatively higher emotion.(3) The spatial pattern of HQMSS for each dimension at the national, provincial, and scenic scales is diversifying. This article provides a multidimensional perspective for investigating the tourism image of mountainous scenic spots, proposes targeted recommendations to improve the overall image of HQMSS in China, and can greatly contribute to the sustainable development of mountain tourism.
  • ZHANG Xuan-yun, ZHANG Shi-chao, LIU Jing-yu, RAN Na, ZHANG Xiang, NING Qi-wen
    2023, 20(08): 2315-2343.
    The natural and economic conditions of agricultural resources vary greatly in China, especially in hilly and mountainous areas. The phenomenon of land fragmentation has become increasingly prominent, so that large-scale operations cannot be fully achieved in a short period of time, and the centralized and continuous scale of operations cannot be realized in China. In addition, with increasingly strict farmland protection and agricultural land use control systems, the issues of nongrain production and nonagricultural cultivated land use have become increasingly restricted. Thus, it is quite necessary to determine the appropriate scale of operations and the means to achieve moderately scaled operations for the new business entities. On the basis of microsurvey data for 108 new citrus-planting business entities in the modern agricultural park in the Chongqing's Jiangjin District, an area with long citrus-planting history, we measured the moderate scale of new citrus-planting business entities to maximize profit using a translog growth model. According to the projection pursuit model, we evaluated the suitability conditions of citrus planting in garden land, woodland, grassland, and general cultivated land in the study area. We then explored the potential for new moderate-scale business entities within different farming radii. The results showed that large-scale planting conditions of citrus in garden land, forest land, grassland, and general cultivated land in the study area were suitable, and the proportion of high-suitable and mediumsuitable land was 73.42%. Under the existing social and economic conditions, the moderate scale of new citrus-planting business entities in the study area was 1.8–2.7 hm~2. In particular, its rankings from large to small were agricultural enterprises(17.19–25.78 hm~2), farmer cooperatives(16.88–25.33 hm~2), big growers and breeders(6.39–9.59 hm~2), and family farms(5.02–7.53 hm~2). In the sample of 108 households,only 47.22% of the entities achieved moderate-scale operation, of which 25% of the entities achieved a scale greater than moderate operation. However, 52.78% of the entities achieved a scale of less than moderate operation. These entities would have to transfer the surrounding adjacent garden land, forest land, grassland, or general cultivated land to achieve largescale land management. The land area of the adjacent gardens in a 1000 m farming radius could meet the moderate-scale operation demand of the vast majority of new business entities. For the vast majority of new business entities, the land area of the adjacent woodland, grassland, and general cultivated land could supplement the garden land to achieve moderate-scale operation in a 500 m farming radius. If the land area with moderate suitability and high suitability is prioritized, the land area in the adjacent gardens in the 1000 m farming radius could meet the moderate-scale operation demand for the vast majority of new business entities. Within the 500 m farming radius, the vast majority of new business entities have achieved moderate-scale operations if the land area adjacent to forest land, grassland, and general arable land was supplemented by gardens; however, a few entities could not achieve moderate-scale operations. From the village perspective, gardens were prioritized. Sixteen villages had planting areas and planting suitability that exceeded the average level of the study area, accounting for 23.53%. If combined with the reserve potential of the garden land, eight villages could improve their potential, accounting for 11.76%. Therefore, the conditions of large-scale citrus planting in the study area should be further improved, and the scale expansion of new citrus-planting business entities should receive additional scientific guidance.
  • JIN Tao, CHEN Yang, SHU Bo, GAO Min, QIU Jian
    2023, 20(08): 2344-2357.
    The Da-Xiao Liangshan mountains are critical ecological function areas and essential ecological barriers in the upper reaches of the Yangtze River in China. This study selected a total of six periods of land use land cover(LULC) data from 1995 to 2020, to estimate the ecosystem service value(ESV) and analyzed its spatiotemporal evolution and topographic gradient divergence. The results showed that:(1) The ESV increased by 1.1 billion yuan, with an increase rate of 1.47% from 1995 to 2020. Two time periods, 2005–2010 and 2015–2020, showed more significant increases than other periods.(2) The elevation and slope of mountainous areas determine the type of land use and further influence the spatial pattern of ESV.(3) Although woodland and grassland are the main land use types of the study area(more than 90%), the hydrological regulation function of the water area partially compensated for the impact of the encroachment of the built-up area on the ESV of grassland.(4) The spatial distribution of ESVs showed an inverted V-shaped characteristic as the topographic gradient increased, with the dominant position being the 5th topographic gradient zone. Finally, this study provided relevant recommendations for ecosystem protection and optimization. The findings of this study clarified the influence of topographical factors on the spatial differentiation of ESV and provided novel insights into ecosystem protection.
  • LI Guang, LIU Shuai-qi, MA Feng-shan, GUO Jie, HUI Xin
    2023, 20(08): 2358-2369.
    Long-term field monitoring finds that serious surface subsidence can still occur even if the high strength cemented fill method is adopted. Combining the results of numerical simulations with global position system(GPS) monitoring, we took a typical filling mining mine with a steeply inclined ore body as an example, and explored its ground subsidence mechanism. The results show that the ground subsidence caused by the mining of steep ore body is characterized by two settlement centers and a significantly uneven spatial distribution, which is visibly different from ground subsidence characteristic of the coal mine. The subsidence on the hanging wall is much larger than that on the footwall, and the settlement center tends to move to the hanging wall with the increase of mining depth. The backfill improves the strength and surrounding rock bearing capacity, which leads to a lag of about 3 years of the subsidence. However, under the actions of continuous and repeated mining disturbances, the supporting effect of the backfill can only reduce the amplitude of the deformation, but it cannot prevent the occurrence of settlement.
  • DENG Jie, ZHAO Jian-jun, LAI Qi-yi, LI Ai-nong, XIE Ming-li, LI Qing-miao, ZHAO Xiao
    2023, 20(08): 2370-2387.
    The deformation and failure of mining slopes in layered rocks predominantly result from shear landslides. However, the instability process of the Pusa rock avalanche in Guizhou, China, revealed a unique damage phenomenon: prominent breaking and toppling of rock blocks occurred in the central section of the mountain, with a lack of commonly observed shear landslide features. This paper aims to investigate the underlying reasons behind this distinctive damage pattern. The study employs various methods including geological survey, UAV aerial survey, physical simulation, and discrete element numerical simulation. The findings indicate that the geological conditions, characterized by a hard upper layer and a soft lower layer along with underground mining activities, play a significant role in triggering the landslide. Furthermore, the presence of a columnar structured rock mass emerges as the primary factor influencing the instability of the Pusa rock avalanche. To elucidate the mining failure mechanism of the rock mass with vertical joints, we propose a "subsidence-buckling" failure model. Following the subsidence and collapse of the roof rock mass in the goaf, the columnar rock mass in the upper and middle portions of the slope undergoes deflection and deformation, forming a three-hinged arch structure. This structural configuration converts the pressure exerted by the overlying rock mass into both vertical pressure and lateral thrust. Under the influence of external loads, the slope experiences buckling failure, ultimately leading to instability upon fragmentation. By shedding light on these findings, this study contributes to a better understanding of the spatiotemporal evolution of mining slope fractures and their impact on slope stability.
  • ZHANG Xiu-lian, ZHANG Fang, WANG Ya-zhe, TAO Zhi-gang, ZHANG Xiao-yun
    2023, 20(08): 2388-2404.
    The strength of water-bearing rock cannot be obtained in real time and by nondestructive experiments, which is an issue at cultural relics protection sites such as grotto temples. To solve this problem, we conducted a near-infrared spectrum acquisition experiment in the field and laboratory uniaxial compression strength tests on sandstone that had different water saturation levels. The correlations between the peak height and peak area of the nearinfrared absorption bands of the water-bearing sandstone and uniaxial compressive strength were analyzed. On this basis, a strength prediction model for water-bearing sandstone was established using the long short-term memory full convolutional network(LSTM-FCN) method. Subsequently, a field engineering test was carried out. The results showed that:(1) The sandstone samples had four distinct characteristic absorption peaks at 1400, 1900, 2200, and 2325 nm. The peak height and peak area of the absorption bands near 1400 nm and 1900 nm had a negative correlation with uniaxial compressive strength. The peak height and peak area of the absorption bands near 2200 nm and 2325 nm had nonlinear positive correlations with uniaxial compressive strength.(2) The LSTM-FCN method was used to establish a strength prediction model for water-bearing sandstone based on near-infrared spectroscopy, and the model achieved an accuracy of up to 97.52%.(3) The prediction model was used to realize non-destructive, quantitative, and real-time determination of uniaxial compressive strength; this represents a new method for the non-destructive testing of grotto rock mass at sites of cultural relics protection.
  • LI Yuan-zheng, SHEN Jun-hui, ZHANG Wei-xin, ZHANG Kai-qiang, PENG Zhang-hai, HUANG Meng
    2023, 20(08): 2405-2421.
    The scientific and fair positioning of monitoring locations for surface displacement on slopes is a prerequisite for early warning and forecasting. However, there is no specific provision on how to effectively determine the number and location of monitoring points according to the actual deformation characteristics of the slope. There are still some defects in the layout of monitoring points. To this end, based on displacement data series and spatial location information of surface displacement monitoring points, by combining displacement series correlation and spatial distance influence factors, a spatial deformation correlation calculation model of slope based on clustering analysis was proposed to calculate the correlation between different monitoring points, based on which the deformation area of the slope was divided. The redundant monitoring points in each partition were eliminated based on the partition's outcome, and the overall optimal arrangement of slope monitoring points was then achieved. This method scientifically addresses the issues of slope deformation zoning and data gathering overlap. It not only eliminates human subjectivity from slope deformation zoning but also increases the efficiency and accuracy of slope monitoring. In order to verify the effectiveness of the method, a sand-mudstone interbedded CounterTilt excavation slope in the Chongqing city of China was used as the research object. Twenty-four monitoring points deployed on this slope were monitored for surface displacement for 13 months. The spatial location of the monitoring points was discussed. The results show that the proposed method of slope deformation zoning and the optimized placement of monitoring points are feasible.
  • CHEN Jing-yi, CHEN Xiao-qing, SONG Dong-ri, LV Ming, GUO Han-qing, SADEGHI Hamed
    2023, 20(08): 2422-2435.
    The simple-shear condition is closer to reality than the direct-shear condition for simulating the mechanical behavior of vegetated soil slope under shallow failure. However, study on simple-shear characteristics for vegetated slope is still insufficient, and there lacks intuitive comparison of characteristics between these two shear conditions. In this study, large-scale simple-shear and direct-shear experiments were conducted on soil permeated by roots of Amorpha fruticosa to investigate the shear strength and stiffness. The stress-displacement relationship of each sample was obtained and further normalized to unify the influence of root content. The results reveal that the direct-shear condition overestimates the shear strength of root-permeated soils(by 41%) and thus the estimation of slope stability based on the parameters of direct-shear condition is not conservative. Furthermore, the initial stiffness of root-permeated soil under simple-shear condition is 34% lower than that under direct-shear condition. The higher strength and stiffness under direct-shear condition are caused by the following reasons: the shear plane does not have the lowest strength, the shear area is decreasing, and the shear zone is thinner. The significant deformation(lower stiffness) revealed by the simple-shear condition facilitates the application of early warning for vegetated shallow landslides.
  • Yavuz ABUT, Ilknur BOZBEY, Ece KURT BAL
    2023, 20(08): 2436-2452.
    In this paper the use of lime stabilized subgrade for low volume roads in two regions with high mountains and different frost penetration conditions in Türkiye was investigated in terms of design, performance, and cost. Pavements on unstabilized and stabilized subgrade were designed for two regions(Izmir and Van), covering all climate variations. The resilient modulus of the lime stabilized subgrade with different soil pulverization levels for non-freezing and freezing conditions were taken from a previous laboratory study. Frost effects were considered in pavement design using two different approaches, including limited subgrade frost penetration method and reduced subgrade strength method. Detailed application and evaluation were performed for all steps. Lime stabilized subgrades significantly reduced the thickness of base courses, and the benefit of lime stabilization was highly dependent on soil pulverization level. A detailed cost analysis on the unstabilized and stabilized cases found that the use of lime stabilization in the subgrade provided significant initial cost savings. Comparative analysis by using the AASHTO(1993) method and KENPAVE software, and quantity effect of soil pulverization level on the performance of low volume roads from a service life perspective, show that subgrade resilient modulus can be estimated. It is also possible to make correct performance estimation in the field. The results of the study show that lime stabilization is a good solution for low volume roads in the mountainous regions of Türkiye.