过刊目录

  • 2021年, 18卷, 第11期
    刊出日期:2024-06-19
      

  • 全选
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  • GONG Jie, XU Cai-xian, YAN Ling-ling, ZHU Yue-hua, ZHANG Yun-xia, JIN Tian-tian
    2021, 18(11): 2803-2819.
    Understanding the trade-offs among ecosystem services(ESs) at multiple scales is a key challenge to effective environmental management. However, the scale effect of ESs trade-offs in the Qinghai-Tibetan Plateau(QTP) has received little attention. This study investigated the scale effects of ESs trade-offs in Bailongjiang Watershed(BLJW),a typical transitional ecotone from the Loess Plateau to the Tibetan Plateau with multiple ESs, intensive human activities and frequent geological disasters in the Eastern Margin of the QTP, China. Four key ESs including food supply(FS), soil conservation(SC), water conservation(WC), and habitat quality(HQ) in BLJW in 1990, 2002, and 2016 were mapped to analyze the scale effects at the watershed, county, and township scales. The results indicated varying scalerelated temporal and spatial relationships among FS, SC, WC, and HQ. The trade-offs between FS-SC and FS-WC initially increased and then decreased during 1990-2002 and 2002-2016, respectively, while the trade-offs between SC-WC, SC-HQ, HQ-WC, and HQFS first decreased and then increased at the same period. The magnitudes of the trade-offs among the four ESs are in the order of watershed scale > township scale > county scale. Among the major landuse types in BLJW, the trade-offs between WC-FS and between HQ-FS in farmland and grassland were higher than those of other land uses. There is a strong trade-off between SC-HQ in forestland and a weak trade-off between SC-WC in farmland and grassland. The trade-offs between the six ESs pairs varied and were scale-dependent mainly due to spatial heterogeneity in the landscape and in human activities. Understanding the ESs trade-offs at the watershed, county, and township scales provides a scientific basis for the formulation of environmental management strategies at appropriate spatial scales. At the BLJW watershed scale, more attention should be paid on farmland and grassland planning and its management, also, forestland should be enlarged if possible. At the county and township scales, land consolidation and planning should be paid more attention to develop ecological agricultural tourism and multi-functional landscapes for strategic spatial planning and integrated watershed management.
  • HU Xu-dong, GAO Jia-zhen, ZHOU Ming-tao, SHEN Jian, ZHAO Tong-hui
    2021, 18(11): 2820-2832.
    Slope eco-restoration has always received extensive attention as a positive way to reverse ecosystem deterioration derived from human interventions. A simplified framework is proposed to undertake a quantitative evaluation of the engineering disturbed slope eco-restoration success in the alpine region, southeast Qinghai-Tibet Plateau. The Dagu hydropower project that disturbs the local ecosystem to some certain was selected as the study area. Since August 2018, six types of slope(soil, rock, soil-rock, spoil, construction site, hardened) were served as the demonstration test for the slope eco-restoration with two years monitoring in the study area. Meanwhile, the topography, erosion, soil quality, and vegetation were selected as assessment indicators of the methodology. Finally, combined with the weighting method and the expert panel, the slope eco-restoration quality index(SERQI) was established and applied in the six slopes. The results suggested that the frost-resistant ecological substrate performed well in alpine region, and the SERQI value is in accordance with the actual monitoring level with spoil slope>soil slope>construction site slope>soil-rock slope>rock slope>hardened slope. The proposed framework could support slope eco-restoration practitioners for making a more objective and quantitative evaluation easily for the postimplementation restoration.
  • LIU Hui-chan, HE Guo-jin, PENG Yan, WANG Gui-zhou, YIN Ran-yu
    2021, 18(11): 2833-2841.
    The Tibetan Plateau is known as the "Asian water tower", and changes in its surface water distribution are important indicators of global climate change and the regional response to these changes. Dynamic monitoring of the surface water on the Tibetan Plateau is an important part of the research on the functions of the "third pole" of the earth and the Asian water tower. With the support of the Google Earth Engine cloud platform, this study used a spectral index-based fast extraction method to obtain surface water data from multi-temporal Landsat(Landsat 4, 5, and 8) satellite remote sensing images. Based on the extracted surface water data, we analyzed the spatiotemporal variations in the surface water of the Tibetan Plateau from 1980 s to 2019. In this study, surface water area refers to the maximum coverage area of the surface water extracted from remote sensing images for one year, hereafter referred to as the surface water area. The results show that since 1980 s, the overall surface water area of the Tibetan Plateau has increased, but not in a linear fashion. After a slight decrease from 1980 s to 1995, the surface water area of the Tibetan Plateau increased steadily, except for a slight decrease in 2015, which may have been caused by the El Ni?o phenomenon. In terms of spatiotemporal distribution, different patterns exist in the various ecological regions of the Tibetan Plateau. The Inner ecological region had the greatest changes of surface water area among the ten ecological regions, accounting for 71.0% of the total surface water area increase from 1980 s to 2019. The surface water bodies in the cold desert and the dry-winter subtropical climatic regions underwent the most changes, with their coefficients of variation being more than 20%. This study can provide data support for dynamic monitoring of surface water in the Tibetan Plateau.
  • NIGRELLI Guido, CHIARLE Marta
    2021, 18(11): 2842-2853.
    Air temperature in the European Alps shows warming over recent decades at an average rate of 0.3 °C/10 years, thereby outpacing the global warming rate of 0.2 °C/10 years. The periglacial environment of the Alps is particularly important for several aspects(i.e. hydropower production, tourism, natural hazards, indicator of global warming). However, there is a lack of specific and updated studies relating to temperature change in this environment. In order to fill this gap, the recent temperature trends in the periglacial environment of the Alps were analyzed. Mean/maximum/minimum daily air temperatures recorded by 14 land-based meteorological stations were used, and the temperature indices for the period 1990-2019 were calculated. The periglacial environment of the Alps showed a warming rate of 0.4 °C/10 years, 0.6 °C/10 years and 0.8 °C/10 years for the mean/maximum/minimum temperatures, respectively. These warming rates are higher than that observed for the entire Alpine area. In 2050 many glaciers of the Alps below 3000 m altitude are expected to be extinct, and all the areas previously occupied by glaciers will become periglacial. In order to manage and adapt to these changes, more in-depth climate analyses are needed. This is necessary for all the mountainous areas of the world, which are undergoing similar changes.
  • SUN Xiao-fei, YUAN Lin-guo, ZHOU Ying-zhi, SHAO Huai-yong, LI Xian-feng, ZHONG Ping
    2021, 18(11): 2854-2869.
    Vegetation coverage recovery after the Wenchuan earthquake has important implications for preventing post-seismic geohazards and soil erosion. However, spatiotemporal changes in vegetation coverage recovery and its driving factors have not been sufficiently studied in the quake-hit areas. This paper aims to analyze vegetation coverage recovery and its driving factors in the quake-hit areas using monadic linear regression, coefficient of variation, and geographical detector. First, we used Moderateresolution Imaging Spectroradiometer(MODIS) data to calculate the vegetation coverage from 2008 to 2018 in the quake-hit areas. Second, we assessed the trend and stability of vegetation recovery in the quake-hit areas based on vegetation coverage. Finally, combined with topography, climate, soil type, vegetation type, and human activities in the quake-hit areas, the driving factors affecting vegetation coverage recovery were analyzed. The results showed that the vegetation coverage level in the quake-hit areas recovered about 90% of that before the earthquake. Vegetation coverage recovery was mainly improved in a stepwise manner: increasing and then stabilizing, then increasing and stabilizing again. Elevation, soil type, and road density were the main factors affecting vegetation coverage recovery, and the interaction among all factors positively strengthened their impacts on vegetation coverage recovery. In addition, the results also revealed the categories that were conducive to vegetation coverage recovery among the same environmental factors and can provide a scientific reference for vegetation coverage recovery in the quake-hit areas.
  • ZHANG Heng-shuo, ZHA Tong-gang, YU Yang, JI Xiao-dong, JESúS Rodrigo-Comino
    2021, 18(11): 2870-2887.
    Alpine mountain ecosystem shows strong interactions between abiotic and biotic parameters. They also receive high attention from human activities(natural tourism, trekking, skiing, etc.). However, as the potential disturbance risk areas in alpine mountains are increasing, it is necessary to understand the relationship between environmental factors and plant communities. This is also the key consideration for the coming international events such as the Winter Olympic Games, which could generate uncontrolled ecosystem issues not previously studied. The Yin Mountains in Chongli district, Zhangjiakou City, Hebei Province, China will be the core area of the 2022 Winter Olympic Games. We hypothesize that disturbances will be caused, therefore, the previous relationships between the habitat factors and plant community and the main environmental limiting factors before hosting them must be assessed to design future restoration plans. Therefore, we used the two-way indicator species analysis(TWINSPAN) and market basket analysis(MBA) for vegetation classification in 91 sampling plots. Plant community and relationships among environmental variables(altitude, slope position, aspect, direction, inclination, soil porosity, soil bulk density, organic matter content and soil pH) were investigated through the trend correspondence(DCA) and canonical correspondence analyses(CCA). Also, the TWINSPAN was used to classify the vegetation into 6 different groups. CCA analysis showed that i) the spatial variation of soil moisture and the content of soil organic matter are the main factors limiting the development of shrub and herb communities; ii) the distribution of different forest communities was mainly affected by terrain factors(altitude, aspect and slope position); iii) the dynamic changes of vegetation communities in different altitudes were affected by the fluctuation of environmental factors and human disturbance, and the shrubs and herbaceous plants in mid-to-high altitude areas(above 1400 m) generally show the process of transformation from the pioneer community to transitional community in the competition. We concluded that under the strong interference of human activities in the core construction area of the Olympic venues, higher damage intensity and lower resilience in the low altitude area is observed compared with the pioneer community. Whereas in the low altitude area(below 1400 m) with a fragile ecological environment, although the plant diversity and coverage are poor, the potential impact and damage degree of the Olympic Games are greatly reduced due to the distance from the construction area of the core venues and good resilience. This information can help land managers and policymakers to anticipate human disturbances on plant communities and support guiding the most efficient ecological restoration after the Winter Olympic Games in 2022.
  • Jung-Hwan YOON, Young-Nam KIM, Kye-Hoon KIM, M.B.KIRKHAM, Hyuck Soo KIM, Jae E.YANG
    2021, 18(11): 2888-2899.
    The steeply sloping agricultural highlands in Korea have severe soil erosion. Estimation of both soil erosion and sedimentation in these highlands is necessary to make plans for soil-conservation measures, but it is not feasible using existing soilerosion models. This study measured the site-specific concentrations of ~(137) Cs and ~(210) Pbex on both a highland slope(33% slope) and a reference site(undisturbed flat area) to estimate soil erosion and redistribution.The use of the fallout radionuclide(FRN) method was evaluated to see if it is a suitable method for characterizing soil erosion. Results were compared with those obtained with the Universal Soil Loss Equation(USLE), which is an empirical model that estimates annual soil erosion. The average concentrations of ~(137) Cs and ~(210) Pbex at the reference site were 11.57±0.24 Bq kg~(-1) and 59.74±4.2 Bq kg~(-1), respectively. Concentrations of ~(137) Cs and ~(210) Pbex in the experimental slope were 16.4% and 10.8%, respectively, of those at the reference site. Radionuclide inventories were lower at the upper point of the slope than those at the basal point of the slope. Concentrations of ~(137) Cs and ~(210) Pbex were significantly correlated with available phosphorus, organic matter, CEC, and exchangeable cations. Estimation of soil redistribution rate using ~(137) Cs and ~(210) Pbex showed site-specific variations at different points along the slope, and respective ranges were-17.46~-207.51 and 1.55~-581.38 Mg ha~(-1) yr~(-1), which indicated that more erosion was assessed by ~(210) Pbex than by ~(137) Cs. Redistribution analysis showed that soil erosion occurred along the entire slope, except for the bottom point of the slope where 1.55 Mg ha~(-1) yr~(-1) of sediment accumulated. The USLE provided a single value of the average annual soil loss in the entire slope,which was either 166 or 398 Mg ha~(-1) yr~(-1), depending on the soil erodibility factor(soil series factor and calculated factor from soil sample analysis) used in the model. We conclude that the FRN method using ~(137) Cs and ~(210) Pbex radionuclides can be used to assess soil erosion and redistribution in steeply sloping agricultural highlands. Verification of soil-erosion values using the FRN method and soil-erosion models has been controversial, but it merits further study at many locations with different soils, topography, and management practices.
  • BAI Yu-shi, LIU Mu-xing, YI Jun, ZHANG Hai-lin
    2021, 18(11): 2900-2914.
    Soil water content(SWC) plays a crucial role in simulating hydrological process, guiding reforestation and controlling soil erosion in mountainous regions. Spatial-temporal variability of SWC increases the difficulty of quantifying SWC pattern in the prediction of soil moisture. Temporal stability analysis of SWC can reduce the labor consuming and simplify the costly field monitoring. This study aimed to evaluate the temporal stability of SWC at hourly, daily and monthly temporal periods and its controlling factors at a hillslope in the Three Gorges region. The SWC of five soil depths was monitored at 5 topographic locations(toe, lower, middle, upper and top slope positions) along a 170 m hillslope in the Three Gorges region(110°04' ~112°04' E, 29°53'~31°34' N), Yichang City, Hubei Province, China from May 4 th, 2018 to May 3 rd, 2019. The results showed that the coefficient of variation of SWC ranged from 4% to 49%, which increased with rising soil depth within 40 cm but thereafter decreased. However, the high Spearman's rank coefficients(P<0.05) indicated strong temporal stability at three temporal periods. The representative locations(RLs)varied in the different soil depths, which were toe, upper and middle slope positions at 0~40, 40~60 and 60~80 cm depths of the investigated hillslope, respectively. Saturated hydraulic conductivity served as a dominant factor controlling the temporal stability of SWC. The result advances our thorough understanding of hydrology and soil water resource in the Three Gorges region.
  • OU Xiao-lin, CHEN Zhi-biao, CHEN Zhi-qiang, LIANG Mei-xia, CHEN Hai-bin
    2021, 18(11): 2915-2928.
    Rare earth elements(REEs) are widely applied in high-tech fields. However, their increasing presence in the food chain poses significant risks to human health. At present, little is known about the effects of organic matter on the distribution of ionadsorbed REEs in soil aggregates during ecological restoration. Red soil derived from coarse-grained granite in Southern China is both prone to ecosystem degradation from soil erosion and rich in REEs. Understanding the distribution of REEs in soil aggregates undergoing ecological restoration is helpful to formulate effective measures for controlling the environmental migration of REEs. Four sites that had undergone different durations/degrees of ecological restoration were selected in the areas to analyze. REEs concentration of six different aggregates sizes(<0.25, 0.25-0.5, 0.5-1, 1-2, 2-5, and >5 mm) were analyzed and the enrichment coefficients were calculated in 4 sample sites of severe-degraded ecosystem in Changting County, Fujian Province, Southern China. The results showed that the total rare earth elements(TREEs)concentration in the aggregates increased from 213 mg kg~(-1) to 528 mg kg~(-1) with the extension of the ecological restoration time. At the initial stages of ecological restoration, there was no significant difference in the TREEs concentration among the six aggregates sizes. However, in the middle and late stages of restoration, the concentration of TREEs increased significantly with the decrease of aggregate size. The concentration of individual REEs showed three changing trends with sizes of aggregates during ecological restoration, respectively: 1) no obvious regular change(S_1), 2) a V-shaped change trend(S_2), and 3) increasing concentration with the decrease of aggregate size(S_3 and S_4). Ce and Eu showed a positive and negative anomaly in the soil aggregates, respectively. Moreover, the light rare earth elements(LREEs) were enriched, while the heavy rare earth elements(HREEs) were depleted during the initial stages, and the HREEs were enriched during the middle and late stages of restoration. The correlation coefficient between organic matter and REEs in aggregates was generally low; however, LREEs showed a stronger correlation with organic matter than that of HREEs during the initial stages of ecological restoration. The correlation between organic matter and HREEs gradually increased and even exceeded that of LREEs with on-going ecological restoration. The distribution of REEs concentration in degraded soil aggregates in Southern China showed obvious variability with the ecological restoration time.
  • ZHOU Zhi-xiong, ZHOU Feng-xi, ZHANG Ming-li, LEI Bing-bing, MA Zhao
    2021, 18(11): 2929-2945.
    In the past several decades, the trend of rainfall have been significantly increasing in the Qinghai–Tibet Plateau, which inevitably leads to a change in the surface energy balance processes and thermal-moisture status of the permafrost active layers. However, the influence of mechanisms and associated effects of increasing rainfall on active layers are still poorly understood. Therefore, in this study, a validated coupled numerical water–vapor–heat model was applied for simulating the surface energy components, liquid and vapor water migration, and energy transfer within the permafrost active layer under the action of increasing rainfall in the case of an especially wet year. The obtained results demonstrate that the surface heat flux decreases with the increase in rainfall, and the dominant form of energy exchange between the ground and atmosphere becomes the latent heat flux, which is beneficial for the preservation of permafrost. The increasing rainfall will also cause the migration of liquid and vapor water, and the migration of liquid will be more significant. The liquid and vapor water migration caused by the increasing rainfall is also accompanied by energy transfer. With the increase in rainfall, the decrease in total soil heat flux directly leads to a cooling effect on the soil, and then the upper limit of the frozen soil rises, which alleviates the degradation of permafrost. These results provide further insights into engineering structures, regional ecological climate change, hydrology, and environmental issues in permafrost regions.
  • ZHANG Qi-bing, MO Cao-hu, ZHAO Di, JIANG Zong-li, CHEN Zhe-fu, WU Kun-peng, ZHANG Zhen
    2021, 18(11): 2946-2959.
    Glaciers in the central Qilian Mountains provide important water resources for the arid Hexi corridor and Qaidam Basin; however, changes in these glaciers interact with climate change. Twentyfour bi-static image pairs of TerraSAR-X add-on for Digital Elevation Measurement(TanDEM-X) data, in addition to a Shuttle Radar Topography Mission-C/X band digital elevation model, and the technology of iterative differential synthetic aperture radar interferometry were used to carry out glacier elevation change analysis in the central Qilian Mountains in China during 2000–2014. Glacier elevation changed with an average rate of(-0.47±0.06) m yr~(-1), while changes in elevation of(-0.51±0.06) m yr~(-1) and(-0.44±0.06) m yr~(-1) were found in the northern(including the Zoulangnan, Tuolai, and Tuolainan mountains) and southern(including the Shulenan and Hark mountains) regions, respectively. Summer mean temperature has risen by 0.51°C(10 yr)~(-1) in the northern region and 0.48°C(10 yr)~(-1) in the southern region during 1989–2014; however, the change in amplitude of annual precipitation was 2.69 mm yr~(-1) in the northern region and 4.77 mm yr~(-1) in the southern region for the same period. These changes can be ascribed as major driving factors for the differences in the changes in glacial elevation in the northern and southern regions. Four types of glaciers existed in the region when considering the change in elevation of the glacial tongue and variation in the position of the glacial terminus: surging, advancing, intensively retreating, and slightly retreating glaciers. If elevation decreased more than 20 m on the part of glacier tongue, the glacier terminus position had commonly retreated more than 100 m.
  • DEY Litan, JAN Chyan-Deng, WANG Ji-Shang
    2021, 18(11): 2960-2970.
    The rheological behaviors of highly concentrated fine particle suspensions(clay-silt-water mixtures) and coarse particle suspensions(coarse particles within a fine particle suspension) were investigated in this study. Experimental results demonstrated that the Bingham Fluid Model with two rheological parameters, Bingham yield stress and viscosity, well characterized the rheological behavior of fine particle suspensions at shear rates between 4 and 20 s~(-1). The inclusion of coarse particles within a fine particle suspension induced an enhancement to the rheological parameters. The rheological parameters of a coarse particle suspension not only depend on its total particle fraction but also on its relative fine/coarse particle fractions. Empirical equations of these two parameters were proposed, quantitatively related to both fine and coarse particle fractions. Results indicated that the Bingham yield stress and viscosity are much more(an order larger) sensitive to changes in fine particle fraction than to changes in coarse particle fraction.
  • HUANG Xiao-rong, ZHOU Xing-yu, YOU Jin-jun, YANG Qing, WANG Yan-jun, MA Kai
    2021, 18(11): 2971-2981.
    The Dujiangyan Project, located at the junction of the upstream of the Minjiang River and Chengdu Plain, Sichuan Province, China, is an irrigation system project as important as the Great Wall in the history of China. Without dam structures, this project has been continuously playing its crucial role in diverting water for irrigation, separating sediments, and controlling flood for 2275 years. In this study, the predicaments of the Dujiangyan Project under the background of rapid urbanization and social economic development were summarized by conducting the field research and using the Indicators of Hydrological alteration(IHA) method: excessive diversion of water, disruption of hydrological pulses, erosion and deposition imbalance and conflicts between power generation and water supply. These contradictions have led to the weakening of the function of automatic water diversion and sand removal in the Dujiangyan Project. Considering the influence of climate change and strong human activities, we pointed out the challenges faced by the millennium ancient weir in balancing human and environmental water usage and project operation and management based on the simulation results of the hydrological model. The corresponding suggestions about strengthening agricultural water saving, generating artificial flood peak were provided to protect and continue to maintain the function of the Dujiangyan Project.
  • YANG Fan, LU Hui, YANG Kun, HUANG Guang-wei, LI Yi-shan, WANG Wei, LU Ping, TIAN Fu-qiang, HUANG Yu-gang
    2021, 18(11): 2982-3002.
    The Nu-Salween River(NSR), the longest free-flow river in Southeast Asia, plays an irreplaceable role in social development and ecological protection. The lower NSR region is particularly valuable as it is inhabited by approximately 6.7 million people. The basin has limited hydraulic conservancy infrastructure and insufficient ability to cope with climate change risks. Studying the hydrological characteristics and changes in the basin provides the scientific basis for rational protection and development of the basin. However, owing to the limitation of observation data, previous studies have focused on the local area and neglected the study of the lower reaches, which is not enough to reflect the spatial characteristics of the entire basin.In this study, the ECMWF 5 th generation reanalysis data(ERA5) and Multi-Source Weighted-Ensemble Precipitation(MSWEP) were applied to develop a geomorphology-based hydrological model(GBHM) for reconstructing hydrological datasets(i.e. GBHMERA5 and GBHM-MSWEP). The reconstructed datasets covering the complete basin were verified against the gauge observation and compared with other commonly used streamflow products, including Global Flood Awareness System v2.1, GloFASReanalysis dataset v3.0, and linear optimal runoff aggregate(LORA). The comparison results revealed that GBHM-ERA5 is significantly better than the other four datasets and provides a good reproduction of the hydrological characteristics and trends of the NSR. Detailed analysis of GBHM-ERA5 revealed that:(1) A multi-year mean surface runoff represented 39% of precipitation over the basin during 1980–2018, which had low surface runoff in the upstream, while areas around the Three Parallel Rivers Area and the estuary had abundant surface runoff.(2) The surface runoff and discharge coefficient of variations in spring were larger than those in other seasons, and the interannual variation in the downstream was smaller than that in the upstream and midstream regions.(3) More than 70% of the basin areas showed a decreasing trend in the surface runoff, except for parts of Nagqu, south of Shan State in Myanmar, and Thailand, where surface runoff has an increasing trend.(4) The downstream discharge has dropped significantly at a rate of approximately 680 million cubic metres per year, and the decline rate is greater than that of upstream and midstream, especially in summer. This study provides a data basis for subsequent studies in the NSR basin and further elucidates the impact of climate change on the basin, which is beneficial to river planning and promotes international cooperation on the water-and eco-security of the basin.
  • Ujwal Deep SAHA, Sohini NEOGY, Jhikmik KAR, Uttam MUKHOPADHYAY
    2021, 18(11): 3003-3024.
    Rishi Khola, a sub-watershed of Teesta river, traverses along the Main Central Thrust(MCT) with a multitude of litho units and structural entities. This study examines the impact of tectonic and lithologic controls in configuring the catchment characteristics of Rishi Khola, Sikkim, India. Corrected SRTM 30 m DEM and Landsat 8 satellite image have been used for extracting the river network, preparing the sub-catchments, the longitudinal profile and thereby calculating the morphotectonic indices. An aggregated tectonic index(ATI) has been prepared to map the intensity of tectonic perturbations in the fluvial environment using the entropy weightage method(EWM) and Weighted Linear Combination(WLC). The undulating nature of the longitudinal profile with prominent knick points confirms the presence of tectonic disturbances and lithological variations. From all the computed morphotectonic indices and the ATI, it has been evident that the region has experienced surface deformations. When viewed at the entire catchment, the morphotectonic indices suggest ample responses to the tectonic perturbations due to the dominance of lithology-controlled hill slope processes and fluvial erosion. The spatiality of the tectonic sensitiveness is rather concentrated into certain pockets of differential stress field formed due to fault thrusting of the Himalayas. The study chiefly focuses on the peculiarity of the watershed which displays a complex response of tectonic and rock structure; wherein the proposed methodology has been successful in excavating such complex responses around the Himalayan thrusts.
  • CIECHA?SKI Ariel
    2021, 18(11): 3025-3040.
    Transport-based social exclusion is currently a serious social problem in Poland, and one which is apparently most severe at the level of the county(Polish powiat) in the south-east of the country, including the Beskid Niski and Bieszczady Mountains. A deeper illustration of this problem requires both observation of changes in the suburban public-transport network and the identification of areas in which this has deteriorated significantly in quantity and quality. The chosen starting point for the research was therefore 1990, as a year in which – on the one hand – the Polish economy was already shifted to the new free-market principles; while – on the other – state PKS(Przedsi?biorstwo Komunikacji Samochodowej) non-urban bus transport enterprises still dominated public transport. The endpoint of the study is then the beginning of 2019(the author's research year). The article introduced here seeks to identify and present cartographically the changes affecting the public-transport network in the study area over the last 30 years, as well as to point to possible consequences of these processes. The background of the described changes is also discussed as are the observed consequences of what is taking place.
  • ZHAO Mei-feng, WANG De-gen
    2021, 18(11): 3041-3057.
    Interregional migration has broad and farreaching impacts on regional urbanization process in ethnic minority areas of Southwest China. The previous literature of interregional migration paid less attention on the ethnic minority areas with fragile geographical feature and marginal socio-economic context in the developing world due to the dearth of reliable data. Based on the 2015 national 1% population sampling survey at the village/community scale, taking Yulong Naxi Autonomous County, Yunnan Province, China as the case study, this paper analyzed the spatial differentiation pattern. The results showed that:(1) migration in Yulong Naxi Autonomous County exhibited obvious spatial differentiation characteristics in terms of population aggregation, population loss, migration direction, and migration activity;(2) the overall spatial differentiation of migration exhibited a "layer + sector" pattern in Yulong Naxi Autonomous County: the first layer was active areas with net inflows(< 20 km from the seat of the county government), the second layer was inactive areas(within 20–60 km of the seat of the county government), and the third layer was a mixed "layer + sector" zone(> 60 km to the seat of the county government), comprised of inactive areas and active areas with net outflows;(3) the spatial differentiation pattern of migration was highly correlated with the regional contexts including the regional economic development, regional transportation accessibility and regional social development, while regional physical geographical factors had insignificant relationships with the migration pattern.
  • XIE Qi-jun, SU Li-jun, BAI Hao, TANG Hao, ZHANG Chong-lei, YU Fang-wei
    2021, 18(11): 3058-3068.
    The performance of a structurally dissipating rock-shed(SDR) depends largely on the capacity of its energy dissipators. At present, most energy dissipators are made of metals, which dissipate energy by unrecoverable plastic deformation. Therefore, they are not able to recover their energydissipation capacity after deformation under rockfall impact. However, a rockfall usually disintegrates into pieces when it rolls down from a higher position and results in multiple rockfall impacts. An energy dissipator with self-recovery capability is therefore more suitable for ensuring the safety of SDRs. Replacing metal with polyurethane(a hyperelastic material with remarkable self-recovery capability) can provide self-recovery capability for energy dissipators, making them more suitable for resisting multiple rockfall impacts. In this work, polyurethane was manufactured into two types of energy dissipators: cylindrical and cubical. Full-scale falling rock impact tests and dynamic numerical simulations were conducted to study the mechanical response of the energy dissipators. In addition, in order to ensure the accuracy of the simulation, the dynamic mechanical properties of the polyurethane were tested and its dynamic constitutive model was established. The experimental and simulation tests have clarified the advantages of the polyurethane energy dissipator. We also summarized the practical considerations in the design of energy dissipators.
  • WAN Yu-hao, ZHAO Xiao-yan, LING Si-xiang, LI Jin, ZENG Cai-yun, BERND Wünnemann
    2021, 18(11): 3069-3081.
    Phyllite fragments are essential for accumulating and generating talus slope at the toes of hillslopes, however, how they are linked to slope failure remains unknown. This paper reports the directional arrangement of phyllite fragments(DAPF) in phyllite talus slope at the eastern margin of the Tibetan Plateau. Field investigation, mathematical statistics and model experiments were performed in order to systematically understand the influencing factors, which include fragment shape, flat ratio, dip angle(α), and fine particle content(c). The results show that the quadrilateral fragment generates a similar imbricate structure more easily than the triangular and rod fragments in the phyllite talus slope. Additionally, the flat phyllite fragments easily accumulate as imbricated structures on the phyllite talus slope. When the dip angle(α) is in the range of 20°– 30°, the minimum orientation ratio(P) is more than 50%, which means that the DAPF phenomenon is more obvious in the phyllite talus slope. For the fine particle content(c) at the same dip angle(α), the minimum orientation ratio(P) is 54%, and the minimum orientation ratio(P) correlates positively with the fine particle content(c). Therefore, compared with the homogeneous talus slope, the phyllite talus slope displays a special DAPF phenomenon. This study provides a valuable reference and presents novel knowledge for risk assessment and engineering design against the phyllite talus slope failure mechanism.
  • CHOU Ya-ling, WANG Li-jie
    2021, 18(11): 3082-3098.
    In seasonally frozen soil regions, freezingthawing action and hydrothermal effect have strong influence on physical and mechanical behavior of shallow soil. A field experiment on the Loess Plateau in Northwest China was carried out to analyze the freezing-thawing process and hydrothermal characteristics of shallow soil considering the climate influence. The results show that the maximum seasonal freezing depth under bare ground surface in this area is from 20 cm to 50 cm. The ground temperature shows a similar changing trend with air temperature, but it has lagged behind the air temperature, and the ground temperature amplitude exponentially decreases with the increase of soil depth. The seasonally frozen soil has experienced four typical stages: unfrozen period, alternate freezing period, freezing period and alternate thawing period. The freezing-thawing process is characterized by unidirectional freezing and bidirectional thawing. The water content of shallow soil is significantly affected by air temperature, evaporation and precipitation, and the soil water content shows a "low-high-low" changing trend with the increase of depth. The soil temperature and water content interact with each other, and are often coupled. The variation trend of soil moisture with time is consistent with the change trend of the ground temperature with time in each soil layer, and the degree of consistency is higher in the near surface soil than that in the lower layer. Also, the spatial-temporal characteristics of soil moisture and temperature is that the volumetric water content and ground temperature of near surface soil have strong variability, and the range value Ka and coefficient of variation Cv of soil water content and ground temperature in different seasons show a decreasing trend with the increase of depth.