过刊目录

  • 2022年, 19卷, 第12期
    刊出日期:2024-06-19
      

  • 全选
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  • ZHAO Bo, HU Kai-heng, YANG Zong-ji, LIU Qiao, ZOU Qiang, CHEN Hua-yong, ZHANG Bo, ZHANG Wei-feng, ZHU Lei, SU Li-jun
    2022, 19(12): 3323-3345.
    On 05 September 2022, an Ms 6.8(Mw 6.6) earthquake occurred in Luding County,Sichuan Province, China, with the epicenter at 29.59°N, 102.08°E and a focal depth of approximately 16.0km.Combining field investigations, high-resolution satellite images and multiple datatpes characterizing the seismogenic structure, topography and geology, this study attempts to discuss the influence of geomorphic and tectonic indexes on landslide distribution. The results show that the 2022 Luding earthquake with seismogenic fault at the Moxi fault, was a sinistral strike-slip event that triggered at least 4528landslides over an area of ~2000 km2. These landslides span a total area of 28.1 km2, and the western section of the seismogenic fault, which serves as the active wall area, is characterized by a higher landslide concentration, especially in the Wandong Basin. The seismogenic fault and lithology influence the regional distribution of landslides, and more landslides occurred closer to the seismogenic fault and in the controlling lithologies of granite and dolomite. Local topography influences the landslide occurrence position on the slope; the eastern section is prone to form landslides in the lower gorge section, and the western section is prone to form landslides in the upper-top section of the gorge. For coseismic landslides in the eastern Baryan Har block, the eastern boundary(Longmenshan fault), where the earthquakes are characterized by thrusts with slight dextral strike-slip movement, could be the primary landslide-prone area; the southern boundary, the Moxi fault and the southern segment of the Xianshuihe fault, with more intensive strikeslip movement, may be the secondary landsideprone area; and the northern boundary is the tertiary landside-prone area. Additionally, the current landslide inventory may be underestimated although this underestimation has limited influence on the results.
  • SARI Mehmet
    2022, 19(12): 3346-3371.
    Rockfalls are one of the most dangerous natural events in hilly terrains, and they substantially threaten residential areas and transport corridors in these environments. This study is aimed to analyze the risk of rockfall from a slope to nearby houses in a historical settlement with past rockfall histories. It contains numerous applications to study rockfall danger from different points of view(e.g., kinematics,numerical stability analysis, risk assessment, 2D trajectory). The rockfall kinematics revealed the statistics for different structurally controlled failure modes among the surveyed slope discontinuities,especially wedge type and block toppling were the most significant ones. Finite element analysis showed that the slope was stable under the natural condition with a safety factor of 2.19. The rockfall risk rating system calculated a medium risk for the houses downstream. Based on the field measurements, a possible rockfall profile was determined and located as an input in the 2D rockfall trajectory program. The rigid-body impact model runs utilized various shapes and sizes of blocks to simulate the rockfall events realistically. According to the 2D trajectory model results, there was no rockfall danger for the investigated downslope houses. The study showed the importance of using different analysis techniques to solve rockfall risk in protected areas based on scientific and rational approaches.
  • CAO Yi-ming, GUO Wei, WU Yu-ming, LI Lang-ping, ZHANG Yi-xing, LAN Heng-xing
    2022, 19(12): 3370-3387.
    Landslide warning models are important for mitigating landslide risks. The rainfall threshold model is the most widely used early warning model for predicting rainfall-triggered landslides. Recently,the rainfall threshold model has been coupled with the landslide susceptibility(LS) model to improve the accuracy of early warnings in the spatial domain.Existing coupled models, designed based on a matrix including predefined rainfall thresholds and susceptibility levels, have been used to determine the warning level. These predefined classifications inevitably have subjective rainfall thresholds and susceptibility levels, thus affecting the probability distribution information and eventually influencing the reliability of the produced early warning. In this paper, we propose a novel landslide warning model in which the temporal and spatial probabilities of landslides are coupled without predefining the classified levels. The temporal probability of landslides is obtained from the probability distribution of rainfall intensities that triggered historical landslides. The spatial probability of landslides is then obtained from the susceptibility probability distribution. A case study shows that the proposed probability-coupled model can successfully provide hourly warning results before the occurrence of a landslide. Although all three models successfully predicted the landslide, the probability-coupled model produced a warning zone comprising the fewest grid cells. Quantitatively, the probabilitycoupled model produced only 39 grid cells in the warning zone, while the rainfall threshold model and the matrix-coupled model produced warning zones including 81 and 49 grid cells, respectively. The proposed model is also applicable to other regions affected by rainfall-induced landslides and is thus expected to be useful for practical landslide risk management.
  • SI Guang-wu, CHEN Xiao-qing, CHEN Jian-gang, ZHAO Wan-yu, LI Shuai, LI Xiang-ning
    2022, 19(12): 3388-3406.
    Damage to rural buildings in mountainous regions caused by flash floods accounts for a significant proportion of economic losses from disasters. The unreinforced masonry(URM) wall is the most vulnerable structural element of rural buildings exposed to flash floods. The failure of a URM wall indicates damage to rural buildings in flash floods. Based on the yield line theory of out-of-plane damage of URM walls and the virtual work method,brittle failure criteria for URM walls under the impact of flash floods were established. According to the field investigation data of the 26 June 2020 flash flood event in Damawu Gully and the corresponding simulation results of FLO-2D, the disaster-causing process was analysed, and the failure criteria were validated. Three building parameters were identified to influence the flood-resistance of URM walls,including the mortar grade, the span-to-height ratio of the wall, and the number of floors of the rural building. The results showed that the cause of the 26June disaster was the diversion of a 50-year flash flood into the residential community on the alluvial fan. The affected buildings were constructed with hollow blocks and lacked flood-resistance reinforcement. The critical failure depth of a URM wall restrained at the top by ring beams(RBs) under hydrostatic load conditions is 1.17 to 1.20 times greater than that of a URM wall without RBs, and the difference is even more pronounced when lowerstrength mortar is used. The flood-resistance of a URM wall constructed with Mb 7.5 mortar and restrained by RBs is almost as strong as that of a URM wall constructed with Mb 20 mortar and without RBs. The span-to-height ratio of a URM wall should not be greater than 1.875 in this case. However,the flood-resistance of a URM wall with RB restraint is almost independent of the span-to-height ratio. The brittle fracture energy of masonry mortar is more crucial to the flood-resistance of 4-edge restrained URM walls if L/Z > 1.875. The flood-resistance of the URM wall of the first storey increases linearly with the number of floors. Single-storey rural buildings should be given priority to the use of high-grade masonry mortar and high-density blocks to improve flood-resistance. The failure criteria and the influence laws of building parameters on the flood-resistance of URM walls can provide references for flash flood mitigation and flood-resistance reinforcement of rural buildings in mountainous regions of Southwest China.
  • S.P.SATI, Shubhra SHARMA, Girish Ch.KOTHYARI, Maria ASIM, Y.P.SUNDRIYAL, Kapil MALIK, Ayush JOSH, Harsh DOBHAL, Naresh RANA, Navin JUYAL
    2022, 19(12): 3407-3431.
    Roads are the most critical means of connectivity in Himalayan villages. However, the terrain is inherently fragile with varied geological,geomorphological, ecological, and climate regimes,that result in frequent slope failure and disruption in connectivity. The risk is further to be increased by extreme events-generated hazards, which are expected to rise in frequency and magnitude with ongoing intervention, however, can improve the sustainability of road networks. The present study attempts to analyse and quantify the impacts of a major road widening project initiated in 2018 in the upper Ganga catchment, Uttarakhand Himalaya which has destabilised valley slopes along the widened segments.Also, a large quantity of excavated sediments is dumped down slopes, which is posing a threat to aquatic biodiversity. The estimates are based on Google Earth imagery of a few representative road segments recently widened in the upper Ganga catchment, which indicate a substantial increase in the landslide and unstable slope area following the road widening. The increase in unstable slope area is attributed to improper road widening approaches and poor slope management in seismically active Himalayan terrain. Further, the mean velocity plots of Persistent Scatterer Interferometric Synthetic Aperture Radar(PSInSAR) indicate that the segments undergoing road widening are coherent with areas of significant earth surface change. A broad correlation between the road width and sediment yield indicates that even a slight increase in road width can result in a large-scale mass removal from the toe of the hillslope, inflicting cascading impact on hillslopes.The study recommends a more flexible road construction approach based on the environmental and geological aspects of the terrain for sustainable road networks. Further, the impact of climate change is looming over the Himalayas, and the relation between climate change and its potential effects on the stability of slopes remains an open issue.
  • KHARUK Viacheslav I., PETROV Il’ya A., IM Sergei T., GOLYUKOV Alexey S., DVINSKAYA Maria L., SHUSHPANOV Alexander S.
    2022, 19(12): 3426-3443.
    We hypothesize that in mountain windy habitat trees formed clusters(hedges) as adaptive structures for seedlings' rooting, survival, and tress' upslope migration. We studied hedges formed by Siberian pine(Pinus sibirica du Tour) and larch(Larix sibirica Ledeb.) within the treeline ecotone in southern Siberian Mountains, investigated hedges formation, evolution, habitat amelioration, and analyzed tree's growth index(GI) dependence on the eco-climate variables(air temperature, precipitation,soil moisture, wind speed) and relief features(elevation, aspect, slope steepness, and terrain curvature). We conducted a ground survey, measured biometrical parameters of trees and hedges,determined species composition and tree physiognomy, soil types and nutrient contents, and sampled wood cores and applied dendrochronology for trees' GI analysis. With high-resolution satellite scenes for hedge detection and upslope migration, we found that winter winds and soil moisture are the main constraints of trees' settlement and growth.Hedge formation always links with wind-sheltered microtopography features(boulders,local depressions or felled trees). Once the first tree is established, a positive feedback is aroused that facilitates seedling rooting and in-hedge habitat amelioration. Trees form a streamlined dense “common crown” that mitigates adverse winter wind influence. Hedges always orient along the prevailing winds, and trees' uphill migration occurs by seedlings establishment within the leeward hedge side. Hedge growth facilitates soil formation and fertilization. The concentration of nutrients(K, P, N and S) within hedges exceeds the background by 1.5-5.5 times.Hedge extension leads to increased snow accumulation that mitigates the influence of desiccation and snow abrasion and mitigates seasonal water stress. In the extremely harsh windy habitat, inhedge trees present in mat, prostrate or krummholz forms. With warming, tree stems and even twigs turn upright. Notably that GI dependence on the wind speed is insignificant until prostrated trees get turning upright. Since that, the negative correlation between GI and wind speed is arisen with subsequent decrease since hedges form streamlined crown. Hedge growth also leads to a “phytofield” formation(i.e.,grasses, lichen, moss and small bushes growth)around the hedges that, in its turn, encourages seedling rooting which is about triple more efficient than outside the phytofield. Larch, in comparison with Siberian pine, is less often formed hedges. GI of both species is stimulated by warmer air temperature in the beginning of the growth season. Meanwhile,larch GI has stronger response to elevated temperatures and less dependent on soil moisture.This indicates larch is a potential substitute of Siberian pine in a warmer and dryer climate. Hedges in warming climate evolve into closed stands due to both in-hedge tree growth and filling gaps between hedges by different tree species.
  • Luis D.LLAMBI, Luis E.GáMEZ, Roxibell PELAYO, Carmen J.AZóCAR, Jesús E.TORRES, Nelson J.MáRQUEZ, Monica B.BERDUGO, Francisco CUESTA, Lirey A.RAMIREZ
    2022, 19(12): 3441-3464.
    Tropical alpine ecosystems exhibit outstanding plant diversity and endemism while being particularly sensitive to the impacts of climate change. Although understanding spatiotemporal changes in plant species composition, richness and community structure along tropical alpine altitudinal gradients is of primary importance, both the functional and historical/biogeographic dimensions of vegetation diversity remain largely unexplored. We used Generalized Linear Models and multivariate analyses to assess changes in species, growth forms,and biogeographic groups richness and abundance, in response to habitat variables along an elevation gradient in seven summits(3800 to 4600 m asl) in the Venezuelan Andes, studied using the standardized approach of the GLORIA-Andes monitoring network.The habitat variables assessed were soil temperature(-10 cm),soil organic matter,slope inclination,and substrate cover.We found 113 species,representing72 genera,32 families,13 growth forms,and seven biogeographic origins,that included 25%of endemic elements.We observed richer vegetation,both in terms of species and growth forms,in summits with higher soil temperatures and higher SOM content,as well as higher biogeographic origin richness with increasing soil temperatures.The presence of holarctic elements increased toward higher elevations,while the occurrence of austral antarctic elements increased toward lower elevations.Our results indicate that biogeographic and functional approaches to vegetation diversity capture well the effect of abiotic filtering on community structuring in these tropical alpine environments.These findings constitute an important baseline for monitoring vegetation dynamics linked to climate change in the Venezuelan Andes by highlighting the functional and historical perspective on vegetation analyses,in contrast with more traditional approaches,based only on taxonomic species diversity.
  • Ivan KUSHNOV, Evgeny ABAKUMOV, Rustam TEMBOTOV, Timur NIZAMUTDINOV
    2022, 19(12): 3458-3478.
    Rapid deglaciation is one of the most important challenges in the Earth science today. One reason of this is specific supraglacial sediments –cryoconites, which represent carbon-containing dust with organomineral matter and living organisms.Investigation of physical and chemical characteristics of cryoconites in the Central Caucasus is necessary in order to understand their influence on alpine territories biogeochemical cycles, pollution and development in conditions of intensive glacial melting and active anthropogenic influence. For this research cryoconites as well as moraines, soil-like bodies and soils have been sampled from the alpine Bezengi Glacier and adjacent Khulamo-Bezengi Gorge. Key physicochemical features(pH values, total organic carbon content, microbial respiration, particle-size distribution) as well as content of trace elements have been defined in sampled materials and several pollution indices(Geoaccumulation index,Contamination factor and Degree of pollution) have been calculated. Results obtained show low values of total organic carbon in cryoconites(max. 0.23%) but high values(max. 7.54%) in top horizon of soils located in floodplain, indicating its active fluvioglacial transfer which may further accelerate the development of soils. Microbiological activity in the studied soils was mostly influenced by additional input of labile organic carbon from cryoconites with water flows. Particle-size distribution was similar among the studied cryoconites, indicating dominance of sand fraction(up to 85.28%) while studied soils showed higher variability due to influence of weathering. Among the trace elements, cryoconites were mostly polluted by Zn(max. 85.70 mg·kg-1)which corresponds to high pollution according to pollution indices; Pb(max. 24.90 mg·kg-1) and Cu(max. 17.40 mg·kg-1), up to moderate pollution level.Redistribution of polluted cryoconite material as well as local anthropogenic activities increased pollution of periglacial soils by Zn(max. 89.20 mg·kg-1), Pb(max.15.00 mg·kg-1) and Cu(max. 12.80 mg·kg-1), which was also proven by the pollution indices with up to high level of pollution.
  • Rubén MARTíNEZ-CAMILO, Manuel MARTíNEZ-MELéNDEZ, Nayely MARTíNEZ-MELéNDEZ, Derio Antonio JIMéNEZ-LóPEZ, Mauricio JOSé-RíOS
    2022, 19(12): 3475-3494.
    Unraveling the factors that determine variation of diversity in tropical mountain systems is a topic for debate in plant ecology. This is especially true in areas where topography is complex due to volcano elevational gradients and where forests are vulnerable to human activity. In this study we used a set of climatic(temperature, rainfall, and radiation solar), topographic(elevation, slope aspect, and slope orientation) and human disturbance variables to determine their effect on diversity and composition patterns of a tree community, considering three slope aspects of a tropical volcano in southeastern Mexico.We sampled trees in seventy 0.1-ha plots distributed on three slope aspects of the Tacaná volcano along an elevational gradient of 1500 to 2500 m. We determined diversity patterns(general tree richness,exponential of Shannon index, and pioneer species richness) with linear regression models, and for beta diversity, we used a dissimilarity index(within and between elevational bands 100 m wide). The effect of a set of environmental and human disturbance variables on tree diversity and community composition was analyzed with general linear models and multivariate analyses, respectively. We registered 2,949 individual trees belonging to 176 species and 58families. The average species richness and alpha diversity per plot were 13(standard deviation ±6) and 9(±5), respectively. General tree richness and alpha diversity increased in the middle part(unimodal patterns) of the elevational gradient, but pioneer species richness decreased linearly with elevation.The variance explained by general linear models was greater in richness(32%) than in alpha diversity(25.3%). The most important predictor variables were temperature(elevational gradient), which explained the unimodal pattern(richness and alpha diversity increase at intermediate levels of temperature), and slope orientation, which explained the increase in richness and alpha diversity toward the geographic north. Only temperature had a significant effect on pioneer species diversity(22%). For community composition, all the predictor variables evaluated had a significant effect, but the most important were slope aspect and temperature. Assemblages were almost completely different in plots that were farther apart along the elevation gradient and had different slope aspects. Finally, the forests at lower elevations(1500– 1900 m) were those that had the most human disturbance. Our study reveals the importance of considering a set of environmental variables related to climate, topography(e.g., slope aspect), and human disturbance to understand variation in diversity and composition of a tree community on a tropical volcano. With this information, we believe that it is important to implement conservation and restoration measures in the forests of the lower parts of the Tacaná volcano, complemented by studies that contribute to designing better conservation strategies.
  • Brijesh KUMAR, Dipankar ROY, Venkataraman LAKSHMI
    2022, 19(12): 3487-3503.
    The hydrology of Himalayan region is influenced by temperature lapse rate (TLAPS) and precipitation lapse rate (PLAPS).Therefore,hydrological modeling considering TLAPS and PLAPS is crucial to manage the water resources in these terrains.In this research,Himalayan Gandak River basin is considered as the study area where TLAPS and PLAPS vary significantly due to high altitude of Himalayas.To assess the impact of TLAPS and PLAPS on water balance components,Soil Water Assessment Tool (SWAT) model was calibrated (2000-2007) and validated (2008-2014) on daily time step for three projects i.e.,Reference Project (RP),Snowmelt Project (SP) and distributed elevation band snowmelt project (SWAT-ETISM).The analysis discloses that SWAT-ETISM model (which has TLAPS and PLAPS parameters) outperforms the RP and the SP models in predicting streamflow with improved statistical indicators R~2=0.88,NSE=0.84 and PBIAS=11.9.Furthermore,it was observed that SWAT-ETISM model comprehensively improved the streamflow statistics by improving the snow water equivalent and water balance components through the consideration of TLAPS and PLAPS values for the region.Hence,the proposed SWAT-ETISM model can be used for estimation of the water budget at the high-altitude and data scarce alpine Himalayan regions and worldwide,where PLAPS and TLAPS are substantial due to altitudinal variation.
  • LI Pan-pan, WANG Bing, YANG Yan-fen, LIU Guo-bin
    2022, 19(12): 3503-3516.
    Nitrogen deposition will alleviate the nitrogen limitation in terrestrial ecosystems and greatly affect vegetation growth, thereby soil erosion.It is important to clarify the effects of nitrogen addition to the plant roots and soil properties on the soil erosion process. A nitrogen addition experiment was conducted in the grassland dominated by Bothriochloa ischaemum(Linn.) Keng(BI), which has received 0, 2.5, 5, and 10 g N m-2 yr-1(N0, N2.5, N5and N10, respectively) for three consecutive years.Then, a total of 150 undisturbed soil samples were collected(including bare soil control) and subjected to flowing water to test their soil detachment capacities under six shear stress levels(10.2 Pa to 29.9 Pa).Three-year nitrogen addition increased the soil bulk density, soil cohesion and nitrate nitrogen while decreasing the saturated hydraulic conductivity, soil water-stable aggregates, soil organic carbon, total nitrogen and ammonium nitrogen. The root mass density and root diameter decreased with nitrogen addition. And the root length, surface area and volume density of the N0 and N5 treatments were larger than those of the other treatments, while the plant roots were significantly inhibited by N10.Additionally, the soil detachment capacity(Dc) and rill erodibility(Kr) of the N0 and N5 treatments were significantly less than those of the N2.5 and N10treatments, of which the Dc(0.020 kg m-2 s-1) of the N0 treatment was 69.0%, 24.3% and 66.8% less than that of the N2.5, N5 and N10 treatments, respectively.The Kr of the N0 treatment was 0.0012 s m-1, which was 72.1%, 25.0% and 70.0% less than that of the others. This study implies that an increase in nitrogen addition likely exacerbates soil erosion in the early(approximately 2.5 g N m-2 yr-1) and late phases(more than 10 g N m-2 yr-1). However, when the nitrogen addition rate is approximately 5 g m-2 yr-1, soil erosion may be inhibited because of the responses of the plant roots and soil to nitrogen addition.
  • QIU An-ni, ZHANG Yan-jun, WANG Gen-xu, CUI Jun-fang, SONG Yuan-xin, SUN Xiang-yang, CHEN Li
    2022, 19(12): 3517-3532.
    Subsurface stormflow is a dominant runoff mechanism in steep humid mountainous areas. An insite measurement of subsurface stormflow suggests that the bedrock surface plays an important role in the runoff generation and routing process, which was rarely adopted in hydrological modelling studies. To improve the runoff simulation performance, the bedrock surface topographic index is introduced, and a modified TOPMODEL based on the bedrock surface topographic index is developed to simulate the runoff.The modified TOPMODEL is applied to the Huangbengliu(HBL), a steep watershed in Gongga Mountain, and proved to be more appropriate for the HBL watershed, especially for peak simulation. The Nash-Sutcliffe model efficiency(NSE) is improved from 0.24 to 0.58 in the calibration period and from 0.40 to 0.62 in the verification period. The result of this study can advance the understanding of the mechanism of flash floods and contribute flood control and disaster prevention in the HBL watershed and similar areas.
  • ZHANG Bin, ZHANG Mao-sheng, SUN Ping-ping, LIU Hao, FENG Li
    2022, 19(12): 3533-3547.
    Resistivity is used to evaluate soil water content (SWC),which has the advantages of not causing soil disturbance and in low price.It is an effective way to assess the SWC variability.This paper aims to evaluate the variability of loess slope SWC through the change of resistivity.It provides a simple way for long term SWC monitoring to solve the expensive cost of deploying moisture sensors.In this context,geoelectric and environmental factors such as soil temperature and SWC were monitored for three years.The prediction model of apparent resistivity and SWC was calibrated.The post processing of geoelectric data was introduced.In addition,the SWC collected by Time-Domain Reflectometry (TDR) was used to verify the feasibility of electrical resistivity tomography (ERT) data.The SWC variability in the process of rainfall,the evolution of four seasons,and the alternation of drying and wetting were evaluated.The research results show that:i) the SWC monitored by ERT and TDR can reflect the response and hysteretic effect of water content at 0.5-3.0 m depth.ii) The moisture content monitored by ERT reflects that the soil is relatively wet in summer and autumn and dry in winter and spring.iii) From 2017 to 2020,the SWC increased in August,and the soil became dry in January.iv) Two areas with high SWC and three areas with low SWC on loess slope are reflected by resistivity.The outcome can provide the change information of SWC to a great extent without excavating boreholes.
  • HE Ling, DENG Yu-song, TANG Qiu-yue, LIAO Da-lan, WANG Chao, DUAN Xiao-qian
    2022, 19(12): 3548-3567.
    Benggang erosion is caused by a special type of gully erosion in southern China that seriously endangers the local ecology and environment. In this study, typical Benggang collapsing-wall soils were used as the study area to investigate the effects of different initial moisture contents and dicranopteris linearis root weight densities, as well as their interactions on disintegration in orthogonal test method. The results showed that the rate of soil disintegration decreased as a linear function of the initial moisture content. The soil disintegration rate tended to rise and then fall as the root weight density increased, reflecting an optimum root weight density of 0.75-1.00 g/100 cm3. The incorporation of dicranopteris linearis roots was most effective for soil consolidation in the shallow layers of soil. In addition,the disintegration rate of the collapsing-wall soils increases as the soil layer deepened. The dicranopteris linearis root system and initial moisture content had an interactive effect that was more pronounced in deeper soils. However, the combined effect of these processes was always dominated by the initial moisture content. Moderate initial soil moisture content(0.20-0.24 g/g) and the addition of a high root density in dicranopteris linearis(0.75-1.00 g/100 cm3) were the optimal combinations that reduced the disintegration rate. In conclusion, maintaining a suitable natural moisture content in collapsing-wall soils and taking measures that use plants to consolidate soil can effectively prevent and control the occurrence of Benggang erosion. The results of this study provided further insight into the factors that influence soil disintegration and offered a scientific basis for soil erosion management in the southern China.
  • LONG Yin-ping, CHEN Gong-yan, MA Qin-min, CHEN Jun
    2022, 19(12): 3568-3581.
    Satellite-based precipitation observations with high spatiotemporal resolution are essential for studying rainfall-induced natural hazards, especially in alpine and canyon areas of the southeastern Tibetan Plateau, which are prone to such hazards yet sparsely gauged. Here, we evaluated precipitation estimated from the Chinese Fengyun-4A meteorological satellite(FY-4A AGRI) versus the Integrated Multi-satellitE Retrievals for GPM(IMERG), by using rain gauge data collected in the Parlung Zangbo Basin from May through September in both 2018 and 2019. Our results showed that(1)FY-4A AGRI generated smaller values of RMSE(root mean square error) on hourly to daily scales, and larger correlation coefficients(R-values) and smaller RMSE values for both moderate and heavy rain,indicating its greater accuracy at rainfall estimation,which is most likely due to the denser rain gauge network at a finer temporal scale used when calibrating FY-4A AGRI;(2) Both satellite products underestimated the volume of moderate and heavy rain, with the larger degree of underestimation by FY-4A AGRI, which could lower their performance in flood monitoring and forecasting;(3) Worse performance and greater inconsistency between the two products were observed in high-elevation areas,perhaps because of orographic cloud effects in these mountainous areas; and(4) Both products revealed that the Gangrigabu Range blocked incoming water vapor from the southwest monsoon, with a better representation of the spatial pattern and spatial variability produced by IMERG. To improve precipitation estimation, the effects of complex terrain should be explicitly incorporated into the retrieval algorithms, with more gauged observations in a denser network and at a finer temporal scale needed to robustly calibrate the satellite-based estimates.
  • WANG Sheng, YAO Tan-dong, PU Jian-chen
    2022, 19(12): 3582-3597.
    Understandinng how futurre climate chaange impacts glaciers is crrucial to suustainable water supplies aand water resource managements..A calibrated ddegree-day glaacier mass baalance model and a volume-aarea scaling approach wwere coupledd to quantitativeely assess thhe effect off future climate change onn the ice volume in thhe Beida RRiver catchment,Northeast TTibetan Plateeau.The ressults show that future mean mass loss off all glaciers will reach to 0.6628±0.058,00.676±0.058 aand 0.765±0.074×10~8 m~3 yr~(-1) under RCP 2.6,4.5 and 8.5,respectivvely,with 81%-996.2%ice voluume losses by the end off 21~(st) century.Fuuture mass balance tennds to be mmore negative unntil 2050 undder RCP 2.6,uuntil 2060 unnder RCP 4.5,annd until 21000 under RCPP 8.5.Glacierrs in the catchmment are likely experienciing or will soon experience the most inteense ice loss,,which may lead to negativee impact onn water resoources after the tipping poiint around 2015-2035.IIn the RCP 8.5scenario,thhe summer mass balancee decreases with elevvation at the altitudinal beelt of 4650~55050 m a.s.l.duee to the variaation of elevaation structurre caused by acceelerating glaciers shrrinkage.Fuurther,the simulations aree sensitive tto the parammeterization scheme of glaccier area andd air tempeerature.The projjections havee the potentiaal to significanntly improve ourr understandiings of glacieer regime oveer data-poor regiions.
  • MAGADáN-DíAZ Marta, RIVAS-GARCíA Jesús I.
    2022, 19(12): 3597-3614.
    Spain is the country with the most Biosphere Reserves in the world,52,and Asturias,with 7,ranks first among the single-province Autonomous Communities.The tourist interest in these natural spaces is increasing,but little or nothing is known about how the residents of these natural spaces perceive the tourist impacts.The main objective of this research was to evaluate the residents'perceived changes in protected mountain areas in Asturias concerning the environmental,sociocultural,and economic dimensions related to tourism activity with survey methods and various quantitative tools.The findings obtained were the following:firstly,there were significant differences between the residents'sociodemographic characteristics and their perceptions of tourism impacts;secondly,there were positive relationships between the residents'perceived tourism economic,environmental and sociocultural impacts and their general attitude towards tourism development;and thirdly,the more positive the residents'attitude towards tourism development,the more likely residents actively support its further development.The findings indicate the willingness of residents to get involved and participate in the tourism activity,so policymakers should implicate residents in decisionmaking on local tourism development.In conclusion,long-term monitoring of residents'evolution of their perceptions and attitudes is necessary to achieve sustainable tourism development.
  • ZHANG Yong-gan, LIU Si-hong, DENG Gang, FANG Bin-xin, ZHANG Yan-yi, LU Yang
    2022, 19(12): 3615-3626.
    The use of clay-gravel mixtures(i.e.,adding excavated or natural gravel particles into clay soil matrix) as the main filling materials is increasing in the anti-seepage system of high Earth Core Rockfill Dams(ECRDs). With the continuous construction of high ECRDs in the Chinese plateaus and cold regions,it is of great urgency and importance to understand the physical and mechanical characteristics of compacted clay-gravel mixtures under freeze-thaw action. To this end, laboratory freezing-thawing tests,computed tomography(CT), and triaxial compression tests were conducted to evaluate the effects of freezethaw cycles on moisture loss, pore structure characteristics,stress-strain behavior,failure strength, elastic modulus, cohesion, and internal friction angle of compacted clay-gravel mixtures. The results demonstrate that, 1) the freeze-thaw cycle significantly changed the mechanical characteristics of the clay-gravel mixture samples, but the shape of the stress-strain curve is less sensitive to it. 2) The failure strength of samples exhibits a significant decrease after the first freeze-thaw cycle, but shows a certain increase as the number of freeze-thaw cycles increases from 1 to 2.3) The elastic modulus of samples first decreases and then increases with increasing freeze-thaw cycle, and the most severe deterioration was observed after the first freeze-thaw cycle. 4) Regardless of the number of freeze-thaw cycles, there is a linear relationship between failure strength and elastic modulus for a sample that has suffered freeze-thaw weathering. 5) The cohesion of samples decreases firstly and then slightly increases with increasing freeze-thaw cycles, while the internal friction angle is hardly affected.
  • YU Fang-wei, ZHAO Chuang, LIU Wei-chen
    2022, 19(12): 3627-3644.
    This paper presents an experimental study on single particle breakage behavior of crushable weathered sands by a number of single particle uniaxial compression tests to comprehensively investigate the characteristics of single particle breakage, the probability of survival of single particle,and the effects of particle size and weathering on single particle strengths. The behavior of single particle under uniaxial compression falls into the mixed five phases: damage by chipping, elastic deformation, fragmentation by partial fracture,breakage by splitting,and the residuals,demonstrating the complexity and variability of the tensile strengths of single particles. The behavior of single particle breakage was quantified herein by the initial fracture and failure strengths of single particle.The probability of survival decreased as the characteristic stresses increased. An increase in the particle size or weathering number of single particle resulted in a reduction in the probability of survival of single particle. For a given probability of survival, the difference in the initial fracture characteristic stress and failure characteristic stress decreased with increasing particle size but showed a complex change with increasing weathering number. The probability of survival showed greater variability for the normalized initial fracture characteristic stress than for the normalized failure characteristic stress,implying that the initial fracture stresses of single particles diverged more than the failure stresses of the particles. The average initial fracture and failure characteristic stresses, and the initial fracture and failure characteristic stresses corresponding to 1/e(37%) survival of single particles decreased while increasing particle size or weathering number, but the decrease showed a sharper rate for smaller single particles with a lower weathering number. The ln-ln coordinates showed a linear representation of the failure characteristic stress and particle size, verifying the applicability of Weibull theory to single particle breakage. However, weathering resulted in downward translation and slight rotation of the linear relation of the failure characteristic stress and particle size in the ln-ln coordinates.
  • TONG Xin-hao, LIAN Jing, ZHANG Liang
    2022, 19(12): 3645-3660.
    This paper aims to investigate the seismic motion characteristics of bedrock and overburden layer slope with the prototype model taken from slopes in the Zheduo Mountain in Northwest Plateau of Sichuan Province,China.Based on dimensional analysis and similarity principle,two model tests with different slope angles were carried out.A transfer function analysis method was proposed to interpret the results from shaking table tests.After eliminating trend terms and signal filtering,the time-domain acceleration was transformed into frequency domain.Then the transfer function was calculated by an average periodic chart.The variation of transfer function from different positions was analyzed by Pearson correlation coefficient,and the least square iteration method was used for modal analysis.The effect of seismic intensity on the dynamic response was highlighted.It is found that the transfer function obviously changes when the slopes are destroyed.Results from modal analysis show that the natural frequency decreases with the increase of the excitation intensity,and the damping ratio increases due to slope damage.