过刊目录

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

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  • Pawe? MIKU?, Bart?omiej WY?GA
    2020, 17(06): 1281-1293.
    Studies presenting long-term observations of the recruitment and mobility of large wood in mountain watercourses are scarce, but they can considerably contribute to the knowledge of river/riparian forest interactions and the assessment of flood hazard resulting from wood mobility during floods. Widespread dieback of riparian forest along the headwater course of Kamienica Stream in the Polish Carpathians, caused by bark beetle infestation of spruce trees, has raised concerns about potential increases of large wood recruitment to the stream and of the flood hazard to downstream valley reaches. In October 2009, 429 trees growing along three sections of the stream were tagged with numbered metal plates and monitored over 10 years to determine the timing and causes of their delivery to the channel and the lengths of their displacement during individual flood events. Moreover, in 2012 the mode of location of wood deposits and a degree of wood decay were determined in the second-to fourth-order stream reaches. The monitoring of tagged trees indicated that trees were recruited to the channel during highintensity meteorological and hydrological events,mostly as a result of bank erosion during floods or windthrow. With 22% of tagged trees recruited to the channel during 10 years, the rate of turnover of the riparian trees was estimated at 45 years. As the riparian area is overgrown with trees with ages up to~160 years, the rate evidences substantial intensification of large wood recruitment to the channel in the recent period. Results of large wood inventory and the 10-year-long monitoring of tagged trees indicated variable mobility of large wood along the upper course of the stream. Wood mobility was negligible in the second-order stream reach, very small in the third-order reach, and greater, but still limited in the fourth-order reach. Wood is transported longer distances only during major floods.However, the advanced state of decay of most pieces leads to their disintegration during floods, precluding distant transport. Thus, large wood retained in the upper stream course does not constitute an important flood hazard to downstream, inhabited valley reaches.
  • Jana GáFRIKOVá, Milan ZVARíK, Peter HANAJíK, Marek Sú?OVSKY, Ivana VYKOUKOVá
    2020, 17(06): 1294-1309.
    Perturbations caused by windstorms usually lead to the harvesting and clearcutting of fallen trees and wood debris, especially in the areas of managed forest ecosystems. Induced shifts in soils due to management practices play a crucial role in the restoration and maintaining of key ecosystem services.This paper focuses on topsoil chemical properties in relation to vegetation type(trees, shrubs and herbs)evolving at windstorm damaged(in 2004) areas with former Norway spruce(Picea abies) forests in the Tatra Mts. region(Slovakia). We assessed the content of topsoil organic matter fractions(extractives,holocellulose(HC) and lignin(Lig)), carbon in microbial biomass(C_(mic)), soil organic matter(SOM)and the content of elements N, C, H and S. The study plots represent different types of post-windthrow disturbance history/regime: wooden debris extraction(EXT), wooden debris not extracted(NEX), wooden debris extraction followed by wildfire(FIR), affected by the windstorm in 2014 with the subsequent wooden debris extraction(REX) and unaffected(REF). Our results revealed significant differences among sites in the content of dichloromethane extractives(EXT vs. REX and FIR), acetone extractives(NEX vs. EXT, FIR and REF), ethanol extractives(FIR vs. EXT, NEX and REF), water extractives(FIR vs. REX, NEX) and C_(mic)(EXT vs.NEX, FIR and REF). The topsoil of Vaccinium myrtillus and Picea abies showed a higher ratio of C/N, N/Lig, and Lig/HC compared to Rubus idaeus,Avenella flexuosa, Calamagrostis villosa, and Larix decidua. The content of N, C, H and S varied between topsoil with shrubs(Vaccinium myrtillus, Rubus idaeus) and grasses(Avenella flexuosa,Calamagrostis villosa). A positive correlation between soil organic matter(SOM) and polar extractives(r=0.81) and a negative correlation between SOM and HC(r=-0.83) was revealed. The carbon content in microbial biomass(C_(mic)) is positively correlated with acid soluble lignin(ASL)(r=0.85). We also identified a strong correlation between Klason lignin(KL) and the Lig/HC ratio(r=0.97).
  • Joanna Beata KOWALSKA, Tomasz ZALESKI, Ryszard MAZUREK
    2020, 17(06): 1310-1332.
    Seven soil profiles developed on calcium carbonate–rich slope deposits in the Polish Carpathians were studied in order to: i) determine the micromorphological features of heterogeneous soils formed in a carbonate depositional environment, and ii) track primary and secondary calcium carbonate forms and their distribution in such stratified soils.Three cases of soils with different arrangements of calcium carbonate were distinguished, controlled mostly by slope processes. For instance, the increasing content and random distribution of angular and subangular rock fragments found in the overall soil matrix and the irregular coarse: fine size limit suggested different intensities of accumulation and mixing of soil material transported along the slope. Slope processes, together with the calcium carbonate content, mineralogical characteristics and texture influenced the type and arrangement of the bfabric pattern. The calcium carbonate distribution within the soils, besides the obvious inheritance from parent material, was governed by the translocation and mixing of deposits on slopes. The climatic conditions prevailing in the area favour the development of secondary forms of calcium carbonate.However, only three of the seven studied profiles contained pedogenic forms of calcium carbonate, yet they were distributed randomly. The occurrence,distribution and preservation of secondary carbonates depended on the content of primary calcium carbonate and soil features such as texture. The transported material down the slope may indicate a very low content of primary calcium or lack thereof,hence its pedogenic forms could not be created.
  • YANG Chao, SU Zheng-an, FAN Jian-rong, FANG Hai-dong, SHI Liang-tao, ZHANG Jian-hui, HE Zhou-yao, ZHOU Tao, WANG Xiao-yi
    2020, 17(06): 1333-1344.
    Both tillage erosion and water erosion are severe erosional forms that occur widely on sloping agricultural land. However, previous studies have rarely considered the process of landform change due to continuous simulation experiments of alternating tillage erosion and water erosion. To identify such changes, we applied a scouring experiment(at a 60 L min~(-1) water discharge rate based on precipitation data from the local meteorological station and the catchment area in the Yuanmou County, Yunnan Province, China) and a series of simulated tillage experiments where plots were consecutively tilled 5,10, and 15 times in rotation(representing 5 yr, 10 yr,and 15 yr of tillage) at slope gradients of 5°, 10°, and 20°. Close-range photogrammetry(CRP) employing an unmanned aerial vehicle(UAV) and a real-time kinematic global positioning system(RTK-GPS) was used to measure landform changes, and highresolution digital elevation models(DEMs) were generated to calculate net soil loss volumes.Additionally, the CRP was determined to be accurate and applicable through the use of erosion pins. The average tillage erosion rates were 69.85, 131.45, and 155.34 t·hm~(-2)·tillage pass~(-1), and the average water erosion rates were 1892.52, 2961.76, and 4405.93 t·hm~(-2)·h~(-1) for the 5°, 10°, and 20° sloping farmland plots, respectively. The water erosion rates increased as tillage intensity increased, indicating that tillage erosion accelerates water erosion. Following these intensive tillage treatments, slope gradients gradually decreased, while the trend in slope gradients increased in runoff plots at the conclusion of the scouring experiment. Compared to the original plots(prior to our experiments), interactions between tillage and water erosion caused no obvious change in the landform structure of the runoff plots, while the height of all the runoff plots decreased. Our findings showed that both tillage erosion and water erosion caused a pseudo-steady-state landform evolutionary mechanism and resulted in thin soil layers on cultivated land composed of purple soil in China.
  • LIU Lei, LIU Ben-hong, LI Wei, ZHANG Yi
    2020, 17(06): 1345-1359.
    Acid Mine Drainage(AMD) from coal mining is a serious environmental issue which affects water quality, ecology, and the overall landscape of the basin. A large number of coal mine tailings in the mountainous regions of Guizhou Province, China were unattended and iron-rich AMD was directly discharged to the rivers. This discharge leaves the river ―yellow‖ and heavily polluted. This study tries to find an efficient and economical method for treating iron-rich AMD. We sampled AMD water in two sites: Yangliujie town of Duyun city(hereafter, called Yangliujie), and Xinglong Coal Mine, Duliu town of Guiding county(hereafter, called Xinglong). We performed iron removal laboratory experiment with Cement-Bentonite Agent(CBA, 80% cement and 20% bentonite) in 500 mL AMD water from Yangliujie, scale-up experiment in 15 L AMD water from both Yangliujie and Xinglong, and engineering application in Xinglong respectively. Laboratory experiment results showed the iron removal rate can reach 99.8% and the removal rate depends on the CBA dosage and the treatment time. In the scale-up experiment, we found that Fe concentration could be reduced from 587.0 to 0.2 mg/L when adding 20 g/L CBA to the AMD water and aerating for 3 hours. As sampled water in Xinglong has a very high Fe concentration(Fe 1019.8 mg/L) and the concentration varies with seasons, it is not economical to add the CBA directly to the AMD water. Considering the abundant and cheap limestone resources in Guizhou, we used a twostep treatment method, first we added CaCO_3 to raise the pH, and then we took the supernatant liquor and added CBA to the liquor. It was shown that 15 g/L of CBA was a good dosage for iron removal with Fe concentration being reduced from 1019.8 to 0.3 mg/L when CaCO_3 was used to raise the pH. The best treatment realized over 99.9% iron removal, 99.2% NH_3-N removal, 98.9% CODMn removal, and heavy metals in the treated water were reduced to under the limit stipulated in the ―Environmental Quality Standards of Surface Water in China‖. Thus in the engineering application, we used this two-step treatment method. After the treatment, the pH of the iron-rich AMD(pH 2.86, Fe 2624.6 mg/L) increased to 8.53, the concentration of Fe was reduced to 59.5 mg/L, NH_3-N decreased from 16.15 to less than 0.05 mg/L, COD_(Mn) decreased from 323.33 to 24.57 mg/L, heavy metals except Fe and Mn were reduced to under the limit of surface water. In conclusion, the use of CBA can effectively remove Fe and other heavy metals from the iron-rich AMD and adjust the pH value to the range of a natural water body.
  • KHAN Humaira, BAIG Siddique Ullah
    2020, 17(06): 1360-1373.
    The high mountains of northern Pakistan comprise the western section of the Hindu KushKarakoram-Himalayas(HKH) region of South and Central Asia. They are home to some rare and endangered species of fauna and flora which form an important link in the biodiversity of the region as a whole. Increasing population and changing life styles in recent decades have brought unprecedented pressures on the biodiversity of this region. Along with the government, the non-governmental organizations(NGOs) and communities have a crucial role to play in conserving biodiversity. In this regard,a number of undertakings to protect depleting species have been initiated by governmental and nongovernmental entities. These efforts are commendable and some have produced positive results, but many exist on a small scale and, with a few exceptions, are not self-sustaining. This paper reports on some of these initiatives of conserving big mammal species like the Astor markhor, Blue sheep,Himalayan brown bear, Himalayan ibex and Snow leopard, with the aim of collating and highlighting them, identifying gaps in conservation and suggesting a way forward so as to promote conservation projects on a larger and more sustainable basis.
  • SCHEIBLER Erica E, FERNáNDEZ CAMPóN Florencia, LAGOS SILNIK Susana, WELLNITZ Todd
    2020, 17(06): 1374-1388.
    Small water bodies are critical for maintaining freshwater biodiversity, but are among the least investigated aquatic environments. We examined physical and chemical variables at two reaches in Arroyo Tambillos, a small, high-elevation Andean stream, in NW Mendoza province, Argentina,across four seasons to examine how local factors and seasonality affected the structure of the macroinvertebrate community. The Arroyo Tambillos community was numerically dominated by ephemeropterans(mainly Massartellopsis irarrazavali) while the dipteran Chironomidae were the most species rich. Total macroinvertebrate abundance was highest in summer, driven mainly by taxa that were secondary in dominance(Austrelmis sp. and Andesiops peruvianus), while richness did not differ between seasons. However, benthic composition was different in Fall 2013(March)compared to other seasons, largely because of the increased abundance of Chironomidae. Canonical correspondence analysis discriminated Chironomidae species distributions in Fall 2013 by substrate type(i.e., big and small boulder substrate). By contrast,discharge, velocity, and depth were the variables which most affected the macroinvertebrate abundance and distributions. Contrary to our expectations, most community changes observed occurred in fall instead of summer. Nivo-kryal stream communities like the one described here have become increasingly important for conserving mountain stream biodiversity as anthropogentic impacts and climate change increasingly impact lower stream reaches. Therefore, monitoring high-altitude streams like the Arroyo Tambillos may be critical for preventing the future loss of unique and sensitive stream biota.
  • SUN Jin-jin, WANG Peng-bin, TONG Yong-shang, HAO Yuan-yuan, HE You-long, WANG Hai-bo, YU Xiao-jun
    2020, 17(06): 1387-1398.
    Alpine meadows, comprising the main ecosystem of the Three-River Source Region, play an important role in the economic development of western pastoral areas. To determine whether the grazing level was too intense or the nutrient-carrying capacity of the meadows was overloaded, and to offer solutions in Maqin County, Qinghai Province, China,the meadows carrying capacity was determined by combining grass-yield and nutrients data for different seasons across different meadows. The results showed that the levels of crude protein(CP), ether extract(EE), ash, soluble sugars(SS), gas production, and energy value of forage in the summer–autumn grazing meadows were higher than those of the winter–spring meadows. Neutral detergent fiber(NDF) and acid detergent fiber(ADF) of forage in the summer–autumn grazing meadows were lower than those of the winter–spring meadows. We found that no pastures were overloaded with metabolizable energy(ME) for the whole year but digestible crude protein(DCP) was overloaded in winter–spring. And there were differences in the amount carrying capacity(forage yield) of seasonal grazing meadows for the different herds, the overload types were annual overloading(herd A), overloaded in summer–autumn(herd B), overloaded in winter–spring(herd C), and not overloaded(herd D). Compared with the previous grazing mode, theoretical carrying capacity, DCP carrying capacity, and ME carrying capacity of herd A increased by 20, 19, and 27 sheep units, respectively,after optimization; herd B: 36, 31, and 45 sheep units,respectively; herd C: 28, 23, and 44 sheep units,respectively; and herd D: 43, 40, and 61 sheep units,respectively. In the Three-River Source Region and similar alpine pastoral areas, the grassland-livestock structure should be optimized to improve grassland vegetation status and increase the theoretical carrying capacity.
  • LUO Song-ping, HE Bing-hui, ZENG Qing-ping, LI Nan-jie, YANG Lei
    2020, 17(06): 1398-1409.
    Soil microbial communities and enzyme activities play key roles in soil ecosystems. Both are sensitive to changes in environmental factors,including seasonal temperature, precipitation variations and soil properties. To understand the interactive mechanisms of seasonal changes that affect soil microbial communities and enzyme activities in a subtropical masson pine(Pinus massoniana) forest, we investigated the soil microbial community structure and enzyme activities to identify the effect of seasonal changes on the soil microbial community for two years in Jinyun Mountain National Nature Reserve, Chongqing, China. The soil microbial community structure was investigated using phospholipid fatty acids(PLFAs). The results indicated that a total of 36 different PLFAs were identified, and 16:0 was found in the highest proportions in the four seasons, moreover, the total PLFAs abundance were highest in spring and lowest in winter. Bacteria and actinomycetes were the dominant types in the study area. Seasonal changes also had a significant(P < 0.05) influence on the soil enzyme activity. The maximum and minimum values of the invertase and catalase activities were observed in autumn and winter, respectively. However, the maximum and minimum values of the urease and phosphatase acid enzymatic activities were found in spring and winter, respectively. Canonical correspondence analysis(CCA) analysis revealed that the seasonal shifts in soil community composition and enzyme activities were relatively more sensitive to soil moisture and temperature, but the microbial community structure and enzyme activity were not correlated with soil pH in the study region. This study highlights how the seasonal variations affect the microbial community and function(enzyme activity)to better understand and predict microbial responses to future climate regimes in subtropical area.
  • Suched LIKITLERSUANG, Kittikhun KOUNYOU, Gayuh Aji PRASETYANING TIYAS
    2020, 17(06): 1410-1422.
    An understanding of how different land covers affect soil erosion caused by rainfall is necessary in mountainous areas. The land cover usually plays an important role in controlling landslide hazards associated with these terrains. This paper presents the results of a field experiment where several types of land covers were placed on a full-scale embankment as erosion control. An 8 m wide, 21 m long, and 3 m high embankment with a 45° side-slope was built with lateric soil. The soil was compacted under a relative compaction of 70% to simulate a natural soil slope. Two sides of the embankment were divided into six land cover areas, with three different areas of bare soil, and one each of a geosynthetic cementitious composite mat(GCCM), vetiver grass,and a combination of GCCM and vegetation. Soil erosion and moisture levels were monitored for each land cover area during six natural rainfall events encountered over the experimental period. Field results were compared with a numerical simulation and empirical soil loss equation. The results revealed that the GCCM gave the best erosion control immediately after installation, but vetiver grass also exhibited good erosion control six months postconstruction.
  • KUANG Qian, YUAN Quan-zhi, HAN Ji-chong, LENG Rong, WANG Yu-shuang, ZHU Ke-hong, LIN Shuo, REN Ping
    2020, 17(06): 1423-1437.
    Alpine grassland is the typical vegetation in the eastern Qinghai–Tibetan Plateau, which has important ecological service functions, and also supports the development of alpine stock farming. In recent years, under both the natural and human disturbance, alpine grasslands in this area have appeared to different degrees of desertification. A diagnosis of the desertification degree serves as the basis for grassland ecological restoration. This study constructs a comprehensive index based on remote sensing called alpine grassland desertification index(AGDI) to monitor the areas and degree of desertification. The most relevant indicators of desertification, namely, vegetation fraction, aboveground biomass, soil moisture, and land surface temperature, were selected to establish AGDI. The geographical detector is used to reselect and assess these indicators. The results show that the overall verification accuracy of AGDI is 82.05%. In particular, the accuracy of identifying severe desertification is the highest. Our study confirms that the desertification of alpine grasslands in the eastern Qinghai–Tibetan Plateau is characterized by fragmentation. Thus, Landsat-8 OLI data with a spatial resolution of 30 m is more suitable than MODIS data for alpine grasslands desertification monitoring. The research results can provide a methodological reference for monitoring desertification of alpine grasslands and other grassland regions in the world.
  • ZHAO Xun, WANG Yun-sheng, WANG Shi-yuan, ZHAO Bo, ZENG Lu, LIU Yu, FENG Qian-qian
    2020, 17(06): 1438-1451.
    Studying the characteristics of a prehistoric giant landslide and ascertaining its relationship with palaeo-seismic events could provide useful information on the role of regional tectonic activities in hillslope evolution. Here, a giant palaeoseismic landslide(GPSL), namely, the Luanshibao(LSB) landslide, located on the eastern margin of the Qinghai-Tibet Plateau, was investigated to ascertain its characteristics and occurrence age. The relationship between occurrence age and palaeoseismic episodes was also discussed by using 14 C dating on the adjacent active faults, including the regional Yidun-Litang-Dewu(YD-LT-DW) fault zone,which crossed the LSB landslide. The dating of multiple samples acquired from palaeo-seismic trenches revealed that at least 5 palaeo-seismic episodes had occurred in the vicinity of the LSB landslide over the last 5000 years. The occurrence age of the LSB landslide(3635 ± 387 a BP) coincides with palaeo-seismic episode I, and the LSB landslide is convincingly inferred to have been triggered during episode I, which reached a seismic intensity(Chinese scale) of at least degree VII near the LSB landslide during failure. The timing of a second reactivation phase coincides with palaeo-seismic episode IV,which occurred at 2100-2200 a BP. The study could provide reference for studying the regional palaeoseismic activities and palaeo landslide evolution near the Litang area.
  • FAN Ji-hui, GALOIE Majid, MOTAMEDI Artemis
    2020, 17(06): 1452-1461.
    This paper aims to numerically investigate the impact of the combination of groynes and vertical piers on mitigating the amplitude and celerity of dam break wave-front. First, a robust numerical model based on the Finite Volume Method(FVM) with the Harten, Lax and van Leer(HLL) approximate Reimann's solver's technique is developed and validated with other research studies. Then many different scenarios including group of piers, group of groynes with different shapes and combination of groynes and piers are considered for dam break flow modeling. The final results showed that group of piers alone or group of groynes alone have no significant effects on the wave-front depth and celerity but, combination of L-head groyne with piers can decrease the amplitude and celerity of the dam break wavefront or flood wave. In this case, a blockage zone between the groynes and intensive backwater effects behind them were observed.
  • Nabin DHUNGANA, Nisha SILWAL, Suraj UPADHAYA, Chiranjeewee KHADKA, Sunil Kumar REGMI, Dipesh JOSHI, Samjhana ADHIKARI
    2020, 17(06): 1462-1475.
    Climate change has major impacts on the livelihoods of forest-dependent communities. The unpredictable weather conditions in rural Nepal have been attributed to a changing climate. This study explored the climate change adaptation and coping strategies that rural communities adopt for the conservation of natural resources and livelihoods in the mid-hills of Nepal. This paper explored major climatic hazards, assessed different coping and adaptation measures, and barrier faced to climate change adaptation based on perceptions by forest-dependent communities. We conducted focus group discussions, questionnaire surveys, and semistructured interviews with local communities and stakeholders. The results showed that rural communities had experienced significant impacts of climate change and variability. In response, they are practicing diverse coping and adaptation strategies,including the construction of bioengineering structures and planting different species that grow quickly and establish promptly.
  • Stella GIANNAKOPOULOU, Dimitris KALIAMP AKOS
    2020, 17(06): 1475-1490.
    The concept of benefaction, as shaped in the pre-industrial society, has been altered and replaced by the modern term of sponsoring. The verbal transformation emerges from a deep cultural shift. Focusing on the dipole of benefactionsponsoring, we examine the cultural transition from the traditional communities of long duration to the modern societies of consumption, taking the Greek mountainous regions as an example. We investigate the cultural shift that generates the metastasis from the communities of benefaction to the modern brandplaces that consume their own cultural heritage,mainly, at the altar of the tourism industry. Modern society has adopted the concept of sponsoring, for the grace of which, culture has to prove evidence of economic value, in order to survive. In the extremely competitive frame of the free-market economy,mountain regions appear vulnerable. The selling and buying of their culture are tempting and attractive under a constantly shrinking welfare-state and narrowing development opportunities. It depends on local and national society to rediscover and regenerate those social mechanisms able to create culture or let the modern consumption-oriented forces prevail. However, authentic principles of benefaction may form an alternative perspective for social reorganization.
  • WANG Yi, ZHU Ying-ming, YU Mao-jun, XU Jing
    2020, 17(06): 1491-1508.
    The scientific analyses of the spatial patterns of regional eco-environment livability, along with the explorations of the correlations between ecoenvironments and population and economic activity distributions, are of major significance in the guidance of the coordinated development between social economies, natural resources, and environments. In this study, the topography, climate,hydrology, land cover, air quality, and the dangers presented by natural hazards in the study area were investigated in order to establish an evaluation model for the regional eco-environmental livability. Then,the observed spatial patterns and regional differences in the eco-environmental livability, as well as their relationships with the distributions of population and economic activities in Zhejiang Province, were investigated. The results showed that the ecoenvironmental livability in Zhejiang Province displayed a gradual decreasing trend from southwest to northeast, as well as from the mountains to the hills, valleys, and plains areas. During the compartmentalization of the eco-environmental livability, it was observed that the lowest livable area covered the largest population, accounting for approximately 29.64% of the total population in the study area. The higher livable areas covered the widest land areas, accounting for approximately 26.15% of the total area. Moreover, it was found that the eco-environmental livability in the mountain areas was higher than that in the plain areas in Zhejiang Province. Furthermore, the ecoenvironmental livability was found to have a significant exponential relationship with the population and GDP densities of Zhejiang Province,with the R~2 of the curve-fittings reaching 0.835 and 0.656, respectively. However, it was determined that the coefficient of the exponential function was negative, which indicated that a strong negative relationship existed between the eco-environmental livability and densities of the population and economic activities. It was assumed that the impacts of anthropogenic factors were the fundamental causes of this negative correlation. This study introduced two new factors(air quality and natural hazards) into the evaluation framework of eco-environmental livability.As a result, a more comprehensive model was established for the evaluation of eco-environmenta livability in certain segments of the study area Additionally, the correlation between ecoenvironment livability and human activities was discussed in-depth, which can potentially provide theoretical and practical guidance for the implementation of eco-livability in China, and possibly even those of other vast developing countries.
  • WANG Zhen-yu, GU Dong-ming, ZHANG Wen-gang
    2020, 17(06): 1509-1522.
    Slope failure due to improper excavation is one of common engineering disasters in China. To explore the failure mechanism of soil slope induced by toe excavation, especially to investigate the influence of excavation unloading path and rate on slope stability, a numerical slope model was built via particle flow code PFC2 D. The development of crack and strain during excavation were obtained and used to evaluate the deformation characteristics.Furthermore, excavation types representing different unloading paths and rates were compared in terms of crack number and strain level. Results indicate that crack number and strain level induced by horizontal column excavation are much greater than those of vertical column excavation and oblique excavation.The crack number and strain level increase with excavation unloading rate. Besides, the feasibility of taking the average strain of slope surface and the average value of maximum strain along monitoring lines to represent the global deformation characteristics were discussed. This study can provide a theoretical guidance for slope monitoring and preliminary optimal selection of excavation scheme in the design and construction of slope engineering.
  • Diganta KUMAR, Bhagawat Pran DUARAH
    2020, 17(06): 1523-1540.
    The Subansiri, a major tributary of the Brahmaputra with its catchment area(35763 km~2)spreading almost entirely in the Eastern Himalayas across almost all the major and local tectonic features in the area witnesses large numbers of seismic events.Active tectonic indices like relief and slope, drainage pattern, longitudinal profile, valley profile,hypsometry, valley asymmetry factors and transverse topographic symmetry index, stream length gradient,valley floor-height ratio extracted from SRTM 3 arcsecond data prove that the evolving basin morphology has substantial contribution from the Himalayan tectonics. Seismic data are incorporated in the study to establish the potentially active tectonic elements in the catchment area. The study shows that the western part of the Subansiri River Basin is profoundly tilted towards north in the upper catchment and towards east in the lower and middle part of the catchment.The predominant tectonic movements in the western part of the basin caused the tilting of the basin towards north in the upstream and towards east in the middle and lower parts.