过刊目录

  • 2022年, 19卷, 第05期
    刊出日期:2024-06-19
      

  • 全选
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  • RHEE Hyun-Hee, SEONG Yeong-Bae, WOO Ju-Sun, Oh Changhwan, YU Byung-Yong
    2022, 19(05): 1217-1230.
    The Transantarctic Mountains are an important corridor between the East Antarctic Ice Sheet and the Western Ross Sea, where most current ice streams and outlet glaciers arise. We investigated Ricker Hills, the largest exposed mountainous region between Southern Victoria Land and Terra Nova Bay, and dated the glacial landforms using in-situ cosmogenic-nuclide 10 Be surface exposure dating to reconstruct the paleo-glacial dynamics. The surface of the Hollingsworth glacier lowered since the middle of Marine Isotope Stage(MIS) 2(22.1 ka); therefore, the Last Glacial Maximum(LGM) occurred before that period. Cosmogenic, geomorphic, and climatic records constrained the glacial surface slope to be between 5.4° and 6.8°. The ice was 270–320 m thicker at the LGM(MIS 2) than presently but did not override the top surface of the Benson Knob. Moreover, previous glacial periods such as the local LGM(MIS 4) or Penultimate Glacial Maximum(MIS 6) maintained thicker ice than the LGM(MIS 2). The Ross Ice Shelf opening during the mid-Holocene(~6 ka) caused the rapid collapse of the terminal outlet glaciers and supplied notable snow accumulation upstream, which stagnated lowering. The greatest lowering and retreat occurred during the late Holocene(2.3 ~ 0.8 ka), when elephant seal colonies thrived in the Ross Embayment.
  • Piotr Tomasz KOPY??
    2022, 19(05): 1231-1244.
    The development of erosive landforms such as rills, ditches, slits, and gullies depends on many environmental factors; thus, the rate of the development of each individual form differs. In this paper, the author presents a case study of two erosion rills located on a hiking trails(Holy Cross Mts.) resulting after 2 years of monitoring in which the process of their evolution was precisely analyzed. Once established, such landforms develop over time with variable rates and can represent multiple different stages. Moreover, the final result of the rill development hardly reminds their original form and does not allow for interpretation of the events that affected it in the recent past. Therefore, the main objective was to determine the volumetric changes of erosion rills created by the surface runoff on both sections, during two years of observation. Additional objectives included a description of the physical and meteorological parameters, important in the development process and a comparison of them to the volumetric changes of each period. Using the Structure-from-motion(Sf M) photogrammetry technique, monitoring procedures have been performed quickly offering sufficient accuracy. For direct comparison, the digital elevation model of difference(Do D) method was used, enabling the calculation of volume. The results showed that the erosion to deposition ratio was more disproportionate during storm events or periods with higher depth of rainfall. Total erosion to deposition balance for the entire monitoring period was negative and equal to 1448.84 kg or 410 Mg/ha for the first erosion rill and 1059.5 kg or 300 Mg/ha for the second rill. Both erosion rills developed differently. The first erosion rill developed by linear cut into deeper and wider form, while the other, steeper rill, evolved from plunge pools merging together into deeper and wider form.
  • LI Xia, WEI Xiao-feng, WU Jin, YIN Zhi-qiang, WAN Li-qin, SUN Hou-yun, AN Yong-long
    2022, 19(05): 1245-1262.
    Geochemical differentiation of soils has a series of consequences on plant and places pressure on the ecological environment. The quantitative evaluation of element migration in the Earth's critical zone is a challenging task. In this study, two demonstration study areas of Scutellaria baicalensis Georgi were selected, and multiple chemical weathering indexes, chemical loss fraction, mass migration coefficients and biological enrichment coefficient method were used to assess the ecological and geochemical suitability. The results show that for the element of Fe, Zn, Se, Cu, Co, Ni, Mo and Ge, the degree of weathering and soil maturation, were greater in the rhyolitic tuff area than in the Plagioclase gneiss area. In both research sites, the heavy metal level of samples in Scutellaria baicalensis Georgi did not exceed the standard limits. The plagioclase gneiss region's surface soil environment was more alkaline, and the content of soil organic matter was lower, resulting in a higher bioenrichment intensity of Ge, Co, Cu, and Se elements in Scutellaria baicalensis Georgi than in the rhyolite-tuff area. The elements of Cd, Nb, Mo, Pb and As are considerably enriched in the soil of the plagioclase gneiss area but lost by leaching in the soil of the rhyolite tuff area, which is connected to the interplay of elemental abundance and human impact in the parent materials. This study provides a good example of how to assess growth suitability of Chinese medicinal materials in the Earth's critical zone.
  • LIAN Ji-jian, ZHANG Shu-guang, HE Jun-ling
    2022, 19(05): 1263-1273.
    Atomizing rainfall caused by flood discharge of high dams poses a great threat to the safety of powerhouse and ecological environment. As an indispensable means, numerical calculation is widely used in the safety design of discharge structures. The distribution of rainfall intensity is closely related to the trajectory nappe shape, jet trajectory distances, the splashed water droplet diameter and its velocity, and the spatial distribution of downstream nappe wind. In this paper, an experimental result is used to verify the improved stochastic splash mathematical model under different bucket types and discharge conditions, and the sensitivity of downstream rainfall intensity distribution to the shape of trajectory nappe, discharge flow, spatial distribution of downstream nappe wind, and the corresponding relationship between the droplet diameter and its splashing velocity is analyzed. The results show that the calculation accuracy of downstream rainfall intensity distribution is significantly improved when the above factors are taken into consideration. It is found that the bucket type and flood discharge rate play the greatest role in the rainfall intensity distribution, followed by the downstream nappe wind distribution, and finally the corresponding relationship between the diameter and velocity of splash droplets. Therefore, these factors should be considered comprehensively when the rainfall intensity distribution of flood discharge atomization is calculated. This study can help us to understand the influence factors of flood discharge atomization more deeply and predict the distribution of flood discharge atomization rainfall intensity more accurately.
  • JAWADI Hussain Ali, IQBAL Mohammad Wasim, NASERI Mohammad, FARAHMAND Asadullah, AZIZI Abdul Haseeb, EQRAR Mohammad Naiem
    2022, 19(05): 1274-1291.
    Groundwater contamination has been on the rise in Afghanistan. It has become a major concern among the policy makers. This paper aims to propose practical options for the management of nitrate contamination in one of Afghanistan's groundwater polluted provinces, Kabul. The management framework utilized Mann-Kendall and Sen Slope tests to detect nitrate trend and geostatistical analysis option in Arc GIS 10.5 to assess the nitrate change. To explore the impact of various management options, a number of legislative documents were reviewed. The results indicate a decline in the nitrate storage of Kabul aquifers from 108 mg/L in 2005 to 0.044 mg/L in 2010.Considering the whole period of the study, the results show that the nitrate volumes remain lower than the nitrate concentration range proposed by World Health Organization(50 mg/L). Groundwater dynamics in Kabul aquifers were influenced by nitrate derived from precipitation and nitrate input from root zones in agricultural areas. Finally, different management options for groundwater pollution from nitrate and corresponding authorities, incorporated urban, rural and agriculture, were proposed. It is expected that this study will help policy makers to better manage the nitrate storage of Kabul aquifers by implementing the proposed management options.
  • HAN Jin-hua, ZHANG Zhao-hui, WANG Zhi-hui
    2022, 19(05): 1292-1306.
    Bryophyte communities have been widely used to monitor and assess heavy metal pollution in soil, air and water. However, the unique value of acrocarpous moss in monitoring environmental pollution and the harm of non-metallic sulfur to human health caused by carbonate manganese mining were seldom considered in previous studies. This study investigated the heavy metal and sulfur pollution level by soil and moss sample collection in Changgou manganese ore and its surrounding environment in the Zunyi area, Guizhou Province, China. By means of cluster analysis, diversity analysis, correlation analysis and redundancy analysis, the relationship between dominant moss communities and major pollutants were analyzed. The results showed that there were pollutants such as iron(Fe), manganese(Mn), cadmium(Cd), sulfur(S) and others in the 500 meters buffer zone centered on Changgou manganese ore. The ore sorting area and waste rock accumulation area were considered as the most seriously polluted, followed by the ore outlet area and ore transport line, at last the miners' living area and vegetable planting area were the least polluted. A total of 23 species of moss communities were identified in the Changgou manganese ore area, among which 9 were dominant, including Bryum blindii Bruch & Schimp.(Bry.bli),Weissia planifolia Dix(Wei.pla)-Bry.bli, Bryum caespiticium Hedw.(Bry.cae), Bryum pallescens Schleicher ex Schw?gr.(Bry.pal), Didymodon longicostatus X. J. Li et Iwats(Did.lon), Weissia brachycarpa(Nees & Hornsch.) Jur.(Wei.bra), Trichostomum brachydontium Bruch.(Tri.bra), Bryum argenteum Hedw.(Bry.arg) Wei.bra and Bryum algovicum Sendt.ex M?ll. Hal.(Bry.alg), all of which are from the acrocarp species. Bry.cae showed a strong tolerance to S, Did.lon to Fe, Bry.pal to Cd and Bry.bli to Mn. There was a significant correlation between the main polluting elements and the dominant bryophyte community(P<0.05), indicating a high biological indicator value. Together, our results can provide the scientific basis for soil pollution monitoring and human health risk assessment in carbonate manganese mining areas.
  • ZHANG Bo, LI Xue-mei, LI Chao, NYIRANSENGIYUMVA Christine, QIN Qi-yong
    2022, 19(05): 1307-1323.
    Investigating the interrelation between snow and vegetation is essential to explain the response of alpine ecosystems to climate change. Based on the MOD10 A1 daily cloud-free snow product and MOD13 A1 NDVI(normalized difference vegetation index) data, this study analysed the spatial and temporal patterns of snow phenology including snow onset date, snow end date, snow cover days, and vegetation phenology including the start of growing season, the end of growing season and the length of growing season in the Chinese Tianshan Mountainous Region(CTMR) from 2002 to 2018, and then investigated the snow phenological effects on the vegetation phenology among different ecogeographic zones and diverse vegetation types. The results indicated that snow onset date was earlier at higher elevations and later at lower elevations, while snow end date showed opposite spatial distribution characteristics. The end of growing season occurred later on the northwest slope of the CTMR and the Yili Valley. The earliest end of growing season was in the middle part of the CTMR. A long growing season was mainly distributed along the northern slope and the Yili Valley, while a short growing season was concentrated in the middle part of the CTMR. The response of vegetation phenology to changes in snow phenology varied among vegetation types and ecogeographic zones. The effect of snow phenology on vegetation phenology was more significant in IID5(Yili Valley) than in the other ecogeographic zones. A negative correlation was observed between the start of growing season and snow end date in nearly 54.78% of the study area, while a positive correlation was observed between the start of growing season and the snow end date in 66.85% of the study area. The sensitivity of vegetation phenology to changes in snow cover varied among different vegetation types. Snow onset date had the greatest effect on the start of growing season in the four vegetation cover types(alpine meadows, alpine steppes, shrubs, and alpine sparse vegetation), whereas the snow cover days had the least impact. Snow end date had the greatest impact on the end of growing season in the alpine steppes and shrub areas. The study results are helpful for understanding the vegetation dynamics under ongoing climate change, and can benefit vegetation management and pasture development in the CTMR.
  • WANG Ya-fei, DUAN Wen-biao, QU Mei-xue, CHEN Li-xin, LAN Hang-yu, YANG Xi-feng, MENG Si-jing, CHEN Jia
    2022, 19(05): 1324-1335.
    There is a strong link between vegetation and environmental factors. Therefore, to elucidate how the stoichiometric characteristics of plants respond to different habitats, we studied organic carbon(C) and total nitrogen(N) stoichiometry characteristics of plants in four different habitats of two different natural Korean pine forests. Three of the habitats(gaps, mounds, and pits) were formed via tree uprooting, whereas an undisturbed site(closed canopies) was used as a control. The followings were our main findings:(1) the organic carbon content of more than half of the 12 picked plants showed significant differences in different habitats. Most of the plants in pit-mound complexes exhibited lower organic carbon contents than plants in gaps and closed canopies;(2) there was no significant differences in the total nitrogen content in 13 of the 25 groups of plant samples;(3) interestingly, the C/N of the sample groups with significant differences in total nitrogen also showed significant differences;(4) there was no significant variations in the stoichiometric characteristics of plants that grew in gaps; however, the variations among plants that grew in pits and mounds were significant;(5) through redundancy analysis(RDA), we find that the main factors effecting the C and N stoichiometric characters of the plants were plants own regulation and the change of photosynthetically active radiation(PAR). In conclusion, the C and N stoichiometric characteristics of plants did not respond to gap formations, but they did strongly respond to pit-mound complex formations. Photosynthetically active radiation was the most important effective factor to plants in the four habitats.
  • PENG Si-li, GE Zhi-wei, LIU Gang-cai, MAO Ling-feng
    2022, 19(05): 1336-1347.
    Microbial functional and structural patterns and drivers along elevational gradients have recently received increasing attention. In this study, we examined soil bacterial and fungal community diversity, compositions, and microbial activities(i.e., soil basal respiration and extracellular enzyme activities) across an elevational gradient from 1148 m to 2080 m(consists of six elevations) in the Yuanmou dry-hot valley located in Southwest China. Environmental factors, including soil temperature, moisture content, p H, soil organic carbon(SOC), total nitrogen(TN), the C/N ratio, total phosphorus(TP), and aboveground plant biomass were also determined. The results showed that soil bacterial alpha diversity(Shannon index) was unaffected by elevation, whereas fungal alpha diversity firstly increased significantly from 1148 m to 1539 m but did not increase further at higher elevations. Bacterial Shannon index was significantly correlated with SOC, whereas fungal Shannon index was remarkably associated with soil temperature. Microbial activity, beta diversities and community composition varied with elevation, but none of them showed a consistent trend. Monte Carlo test revealed that soil moisture followed by temperature, and p H, were the primary drivers of bacterial community composition. Soil fungal community composition significantly depended on soil moisture. Overall, our study suggested bacterial diversity and composition were determined by climatic(moisture and temperature) and edaphic properties(SOC and p H), while fungal diversity and composition were structured mainly by climatic factors. These findings may contribute to a better understanding of microbial responses along elevational gradients in this semi-arid region.
  • LI Xiao-juan, LIU Xin, ZHANG Han-yue, BAO Wei-kai
    2022, 19(05): 1348-1356.
    Climate is a key factor to determine the pattern of ecosystems; however, the latitudinal patterns of climatic variables in the arid and semiarid areas remain largely unclear when compared to humid areas. The topography of the dry valleys of southwestern China plays an important role in the formation of climate. However, its impact on the climate remains qualitative. In this study, eight climatic variables from 12 meteorological stations were analyzed to explore their latitudinal patterns in the wet and dry seasons from 1961 to 2019. We also quantified the effects of local topography(RH10) on the climatic variables. The results were as follows: sunshine duration, total solar radiation, average temperature, and evaporation decreased significantly, and wind speed increased significantly with increasing latitude in the annual, wet, and dry seasons(P<0.001). Relative humidity and precipitation decreased significantly with increasing latitude in the wet season(P<0.001), and no obvious change pattern was observed in the dry season. Aridity index significantly decreased(toward dryness) with increasing latitude in the wet season and increased in the dry season(P<0.001). Wind speed had a significantly positive relationship with topography(RH10)(P<0.01), whereas precipitation and aridity index were negatively associated with topography in the wet season and positively associated with topography in the dry season. Dryness was positively associated with RH10 in the wet season, and negatively in the dry season. The results of our research could provide new perspectives for understanding the relationship between topography and drought in the dry valleys of southwestern China.
  • GUO Fu-yun, MENG Xing-min, QI Tian-jun, DIJKSTRA Tom, THORKILDSEN Jarsve Kristine, YUE Dong-xia, CHEN Guan, ZHANG Yi, DOU Xiao-dong, SHI Peng-qing
    2022, 19(05): 1357-1369.
    Numerous large-scale fragmented bedrock landslides developed along major fault system is a world-wide phenomenon, which are often characterized with repeated reactivation throughout histories. Due to the large-scale and deep-seated features, it is normally difficult to control such landslides, which in turn pose great threat to local residents and infrastructures. Therefore, monitoring and forecasting these gigantic landslides has become a key protocol for risk reduction. This paper introduces such a typical massive landslide, named Yahuokou landslide, besides Min River in Zhouqu County, Gansu Province, China. Reactivated on July 16, 2019 with a volume of approximately 4×106 m3, moving slowly and transitionally starting from top part, its toe had partially blocked the Min River and destroyed roads and houses eventually by August 11, 2019. As to emergency response for such huge slowmoving landslide, there is no standard national protocols. Therefore, how to make effective emergency decision has become a challenge. Based on previous experiences, integrated multi-methods,including UAV imagery interpretation, we applied GNSS monitoring and field investigations in the early stages of landsliding, in order to assist the decisionmaking. The results show that the movement path of the current displacement is consistent with that of the 1989 reactivation event, and the slide body was separated into three relatively independent blocks with different sliding velocities and responses to rainfall. The upper and lower blocks appeared less affected by rainfall, while the middle block responded more to the changes in precipitations. It proves that the combined approaches using a variety of monitoring techniques can play an effective role in the monitoring of rapidly deformed transitional largescale landslides, and can also provide a set of reference methods for the emergency disposal of similar landslide hazards.
  • ZHANG Fu-ling, DENG Mao-lin, YI Qing-lin, LU Shu-qiang, ZHENG Wei-jun, HUANG Hai-feng, ZHU Xing
    2022, 19(05): 1370-1385.
    Since the first impoundment of the Three Gorges Reservoir(TGR) in China in 2003, more than 5000 landslides including potential landslides were identified. In this paper, a deep-seated active landslide in TGR area was analyzed. Fourteen years' monitoring data and field investigations from 2006 to 2020 were used to analyze the deformation characteristics, influencing factors, and meteohydrological thresholds. The landslide showed a none-overall periodic movement pattern featuring acceleration during long-duration rainfall and rapid transition to constant creep after rainfall events. Two secondary sliding masses, No. 1 and No. 2, were defined via field investigation. The reservoir has no impact on the deformation whereas long-duration-low-intensity rainfall is the main factor. At present, the cumulative displacements of the main sliding mass range from 0.9 to 3.2 m, and the deformation during the rainy season is gradually increasing. The boundary of this landslide was formed, and the boundary of No. 2 sliding mass became obvious. The probability of the failure of sliding mass No. 2 is very high under the conditions of continuous rainfall. The 15-day antecedent rainfall combined with 4-day cumulative rainfall could be the rainfall threshold which could be associated with the groundwater level S1 of 294 m above sea level for forecasting large deformation of Tanjiawan landslide.
  • ZHANG Jing, BROWN Colin, WALDRON Scott, YADAV Lava, ZHUOGA De-qing
    2022, 19(05): 1386-1403.
    Smallholder livelihoods in agricultural areas in Tibet Autonomous Region, China(Tibet for short) have traditionally been based on subsistence mixed crop-livestock systems. Like many parts of China and the developing world, rural Tibet is undergoing rapid change in agricultural development, boosted by links with the off-farm sector. However, the agricultural transition process in Tibet has not been linear, is affected by policies particular to the region, and varies significantly for different categories of rural actors. This paper analyses heterogeneity of household types in agricultural areas of southern Tibet and how household structures and characteristics result in different agricultural development pathways. Data is drawn from a stratified random survey of 144 households in three townships in southern Tibet and analysed through three methods: cluster analysis, bio-economic modelling, and analysis of household perceptions and attitudes to change. The analysis allows for the identification of three key household types – semisubsistence, pluriactive and semi-commercial – organised along a continuum of intensification, commercialisation, specialisation and productivity. The study demonstrates the diversity of household farming systems in Tibet which in turn highlights the need for disaggregated analysis and tailored development policies and strategies. However, the analysis also reveals commonalities in development paths between groups, where all farm types are more interested in pursuing income and livelihood goals through an increase in productivity than through an increase in scale. Farmers in all systems choose to retain agriculture as a base from which to pursue livelihood strategies, especially through off-farm activities. Accounting for this household heterogeneity is important on several levels. First, it provides more granular detail on the process of development in rural areas of Tibet that have been very difficult to access in English literature especially in recent years. Second, the characteristics of the case study in agricultural areas of Tibet – especially the mixed agricultural-pastoral systems, high levels of seasonality, heavy state investment and increased integration with the other regions of China-may contribute to the broader agricultural development study. Third, policymakers in the central and local governments may be interested in how the household heterogeneity may affect – or be affected by – policies to increase agricultural productivity, intensify systems, change the composition of crop-livestock systems, promote rural-urban transformation and pursue environmental objectives, especially grassland degradation.
  • Fred KALANZI, Prossy ISUBIKALU, Florence Birungi KYAZZE, Lawrence Justus Baguma ORIKIRIZA, Clement OKIA, Isaac KIYINGI
    2022, 19(05): 1404-1418.
    This study was intended to understand how smallholder farmers' modifications improved agroforestry technologies' usability in Uganda's Mt. Elgon region. We used a case study approach to understand how smallholder farmers' contextual realities informed their modifications and enhanced the usability of agroforestry technologies. Data was collected over four months of frequent and regular interaction with the cases using formal and informal methods that included in-depth interviews, conversations, discussions, and direct observations. Emerging themes and patterns were identified from the comprehensively reduced data. In addition, respondents' direct quotes were used to emphasize the reasons for the modifications. The findings showed that smallholder farmers modified the recommended technologies to suit their biophysical and socio-economic realities. Differences and similarities in modifications existed among cases across the agroforestry technologies. The modifications were mainly done to diversify tree uses, optimize space utilization, and minimize production costs for farming households. These findings imply a need to critically examine the smallholder farmers' modifications to make agroforestry technologies applicable and compliant to their contexts. This will inform the re-invention of technologies that will quickly diffuse into the community for broader impact. Findings also emphasize the need to rethink the linear model of technology transfer mainly applied in agroforestry technology development and dissemination because it offers limited space for the much-needed feedback from smallholder farmers.
  • WU Hong-gang, PAI Li-fang
    2022, 19(05): 1419-1436.
    Despite the continuous advancements of engineering construction in high-intensity areas, many engineering landslides are still manufactured with huge thrust force, and double-row piles are effective to control such large landslides. In this study, large shaking table test were performed to test and obtain multi-attribute seismic data such as feature image, acceleration, and dynamic soil pressure. Through the feature image processing analysis, the deformation characteristics for the slope reinforced by double-row piles were revealed. By analyzing the acceleration and the dynamic soil pressure time domain, the spatial dynamic response characteristics were revealed. Using Fast Fourier Transform and half-power bandwidth, the damping ratio of acceleration and dynamic soil pressure was obtained. Following that, the Seism Signal was used to calculate the spectral displacement of the accelerations to obtain the regional differences of spectral displacement. The results showed that the overall deformation mechanism of the slope originates from tension failure in the soil mass. The platform at the back of the slope was caused by seismic subsidence, and the peak acceleration ratio was positively correlated with the relative pile heights.The dynamic soil pressure of the front row piles showed an inverted "K"-shaped distribution, but that of the back row piles showed an "S"-shaped distribution. The predominant frequency of acceleration was 2.16 Hz, and the main frequency band was 0.7-6.87 Hz; for dynamic soil pressure, the two parameters became 1.15 Hz and 0.5-6.59 Hz, respectively. In conclusion, dynamic soil pressure was more sensitive to dampening effects than acceleration. Besides, compared to acceleration, dynamic soil pressure exhibited larger loss factors and lower resonance peaks. Finally, back row pile heads were highly sensitive to spectral displacement compared to front row pile heads. These findings may be of reference value for future seismic designs of double-row piles.
  • MENG Wei, HE Chuan, WU Fang-yin, YANG Wen-bo, KOU Hao, ZHOU Zi-han, GUO De-ping, MENG Hai-long
    2022, 19(05): 1437-1455.
    To explore the water table and water inflow after tunnel excavation in a vertically stratified phreatic aquifer, approximate analytical solutions for the steady-state water table and water inflow of a drained tunnel in a vertically stratified phreatic aquifer were obtained based on the Dupuit assumptions and the integral method. By comparing the approximate analytical solutions with numerical solutions, it was found that the relative error of the approximate analytical solution for the water table elevation is less than 10%, and the relative error of the approximate analytical solution for the water inflow is approximately 25%. The sources of the above errors are as follows:(1) At the lateral boundary of water replenishment, the water surface should be tangent to the horizontal line, but the water surface for the approximate analytical solutions has a gradient.(2) At the vertical boundaries near the tunnel, the total head is variable, but the total head for the approximate analytical solutions is assumed to be constant.(3) The Dupuit assumptions are applied in the flow domain near the tunnel. Although the relative errors of the approximate analytical solutions for the water table elevation and water inflow are evident, the lowered water table is reflected in the approximate analytical solutions.
  • YU Fang-wei
    2022, 19(05): 1456-1463.
    This paper presents a generalized dilatancy angle equation of granular soil to cover not only the drained tests but also the undrained tests by introducing a generalized structure of soil: soil skeleton formed by soil particles and the fluid in soil voids, under the assumptions of the incompressibility of soil particles and the compressibility of the fluid in soil voids. For the drained tests, the generalized dilatancy angle equation of granular soil would be degenerated to its current dilatancy angle equation. However, for the undrained tests, the generalized dilatancy angle equation of granular soil was derived with a λ parameter that was related to the stress-strain state of soil and the nature of the fluid in soil voids. The λ parameter was determined by the initial dilatancy angles of granular soil at the onset of shearing on the same initial state of the soil in the drained and undrained tests. In addition, the generalized dilatancy angle equation of granular soil was verified for application in calculation of the dilatancy angles of sands in the drained and undrained tests.
  • ZHANG Wen-gang, WU Jia-hao, GU Xin, HAN Liang, WANG Lin
    2022, 19(05): 1464-1474.
    The safety of embankments under seismic conditions is a primary concern for geotechnical engineering societies. The reliability analysis approach offers an effective tool to quantify the safety margin of geotechnical structures from a probabilistic perspective and has gained increasing popularity in geotechnical engineering. This study presents an approach for probabilistic stability analysis of embankment slopes under transient seepage considering both the spatial variability of soil parameters and seismic randomness. The spatial varying soil parameters are firstly characterized by the random field theory, where a large number of random field samples of the soil parameters can be readily generated. Then, the factor of safety(FS) of the embankment slope under seismic conditions corresponding to each random field sample is evaluated through performing seismic stability analysis based on the pseudo-static method. A hypothetical embankment example is adopted in this study for illustration, and the influences of shear strength parameters, seismic coefficient, and the external water level on the embankment slope failure probability are systematically investigated. Results show that the coefficient of variation of the friction angle and the horizontal scale of fluctuation have more significant effects on the embankment slope failure probability. Besides, the seismic coefficient also affects the embankment slope failure probability considerably. For a given external water level, the failure probability corresponding to the downstream slope of the embankment is larger than that in the upstream slope.
  • CHEN Si-yu, YANG Li-yun, YANG Ai-yun, HUANG Chen, XIE Huan-zhen
    2022, 19(05): 1475-1486.
    Pyramid cut blasting is an essential form of inclined hole cut blasting, but the in-situ stress effect of pyramid cut blasting is rarely studied. Based on the research background of pyramid cut blasting in a deep rock mass, the size, volume, and fragment size distribution of the blasting cavity before and after uniaxial compression were analysed by a model test. Otherwise, the damage and effective stress of the pyramid cut blasting were analysed with LS-DYNA numerical simulation. The results show that the damage and fragmentation of pyramid cut blasting are not only affected by blasting stress wave and blasting gas, but also affected by uniaxial compression. Under the influence of uniaxial compression, the blasting stress wave and blasting gas are more likely to damage the rock mass parallel to the uniaxial compression direction near the connecting line of blasting hole, and make the volume of cavity larger and the fragment rate lower. Additionally, uniaxial compression has a prominent influence during the middle and late stages of blasting.