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  1. 2121

    Optimal Allocation of Water Resources in Tarim River Basin Based on Engineering Pattern Optimization by HONG Liangpeng, BAI Tao, LI Jiang, LIU Dong

    Published 2024-06-01
    “…The research results show that a scheme for replacing plain reservoirs in the main streams with mountainous reservoirs has been developed and optimized. …”
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  2. 2122

    La forteresse de Sadr, une lecture géo-historique au temps des croisés by Corinne Feïss-Jehel, Jean-Michel Mouton, Claudine Piaton, Pierre-Jérôme Jehel, Jeannine Le Rhun

    Published 2011-10-01
    “…The littoral plain of Gifar offered a dune belt that was relatively flat compared to the mountains of central Sinai. This road, a main route for centuries, came under partial control of the Frankish states in 1099 with the creation of the Latin Kingdom of Jerusalem. …”
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  3. 2123

    Movement Characteristics of Typhoon Rainstorm-Triggered Debris Flow in Qinglong Gully Based on Massflow Model by XIONG Chaozheng, JI Feng, SHI Yuchuan

    Published 2023-01-01
    “…Typhoon Lekima made landfall on August 10,2019,causing a massive typhoon rainstorm-triggered debris flow in Qinglong Gully located in the middle and low mountainous area of southern Anhui.To deeply explore the movement characteristics of the typhoon rainstorm-triggered debris flow,this study identifies the characteristics,formation conditions,and source distribution of Qinglong Gully.On this basis,it builds a high-precision three-dimensional model of the study area to calculate two working conditions of the non-typhoon rainstorm and typhoon rainstorm.In addition,Massflow,the software for surface-process dynamic numerical analysis,is employed for numerical simulation and comparative analysis of debris-flow movement characteristics.The results show that the typhoon rainstorm-triggered debris flow has a faster forward speed compared with the non-typhoon rainstorm-triggered debris flow.It moves to the monitoring points j1—j5 at 600 s,100 s,1500 s,1 600 s,and 1 900 s,respectively,and the front can cause damage to the channels and buildings along the way in a short time.Three main accumulation areas are formed in the outbreak of the debris flow.The maximum accumulation thickness of the typhoon rainstorm-triggered debris flow is 3.08 m,3.80 m,and 7.75 m,and the accumulation area is 36 324.4 m<sup>2</sup>,3 700.4 m<sup>2</sup>,and 32 279.5 m<sup>2</sup>,respectively.The debris flow has the characteristics of a large height and plane range of influence,which is more likely to cause serious life and property damage to engineering buildings and residents.…”
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  4. 2124

    Modelling of Chain Process of Debris Flow Blocking River and Induced Flood Disaster in Meizoseismal Area ——A Case of Xiazhuang Gully in Wenchuan County by LUO Yuting, WANG Lijuan, MA Song, TANG Yao

    Published 2023-01-01
    “…After the Wenchuan earthquake,there has been a sharp increase in the frequency of debris flow activity,which is featured by low rainfall threshold,frequent occurrence,wide impact and strong destruction.The hazards mainly include siltation,impact,river blocking and inundation.Among them,the mudslide blocking river shows particularly prominent disaster effect,seriously threatening the improvement of mountain infrastructure,and residents' life and property safety.The research of the dynamic process of river blocking disaster chain of debris flow can provide scientific reference for debris flow hazard prevention and early warning.Based on field surveys,physical tests,remote sensing images and rainfall data for a typical watershed,a numerical simulation was conducted to study the dynamic process of the river blocking disaster chain of debris flow in Xiazhuang Gully.The simulation results show that the debris flow reaches the outlet of the basin at t=120 step;and at t=130 step the debris flow pushes forward and blocks part of the main river;at t=140 and 150 step the debris flow completely blocks the main river,forming a debris-dam with a length,width and thickness of 236.0 m,74.0 m,6.2 m and 312.0 m,79.0 m,and 7.1 m,respectively,which causes the upstream water level to rise,with an inundation depth of the upstream residential area of 3-5 m.By comparing the simulation results with the field measured data,the accuracy of the simulation reaches up to 84.9%,which indicates that the model is of good applicability to simulating the disaster chain process of landslide-debris flow-flood.…”
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  5. 2125

    Physics Features of TRU-Fueled VHTRs by Tom G. Lewis, Pavel V. Tsvetkov

    Published 2009-01-01
    “…The current waste management strategy for spent nuclear fuel (SNF) mandated by the US Congress is the disposal of high-level waste (HLW) in a geological repository at Yucca Mountain. Ongoing efforts on closed-fuel cycle options and difficulties in opening and safeguarding such a repository have led to investigations of alternative waste management strategies. …”
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  6. 2126

    ANTHROPOGENIC LOAD ON WATER BODIES IN THE UPPER OB BASIN IN DIFFERENT WATER CONTENT PERIODS: THE DYNAMICS AND THE FORECAST by Natalya V. Stoyashcheva

    Published 2020-06-01
    “…It was revealed that the highest wastewater dilution ratio (over 1000 times) is characteristic of mountainous rivers of the Republic of Altai, Altai Kray and the north of Tomsk oblast. …”
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  9. 2129

    New glacier thickness and bed topography maps for Svalbard by W. van Pelt, T. Frank

    Published 2025-01-01
    “…Specifically, we model large glaciers with the Parallel Ice Sheet Model (PISM) at 500 m resolution, while we resolve smaller mountain glaciers at 100 m resolution using the physics-informed deep-learning-based Instructed Glacier Model (IGM). …”
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  10. 2130

    Rudy Kelly’s Eyes: Chris Hedges and Joe Sacco’s Days of Destruction, Days of Revolt by Øyvind Vågnes

    Published 2015-08-01
    “….; migrant workers assigned to pick tomatoes in worker camps in Florida; and individuals suffering from and resisting mountain-top removal by coal companies in West Virginia. …”
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  14. 2134

    Estimates of vertical tectonic stress in the northwest Ethiopian plateau using topography and gravity data by Muluken Kassa

    Published 2025-01-01
    “…The Lake Tana and areas adjacent to the Lake Tana, including the Debre Tabor Graben, Guna, Choke, and Guguftu mountains, are characterized by negative vertical tectonic stress. …”
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  15. 2135

    Luke’s Divine Call of Jesus. Part One by Robert Lee Williams

    Published 2024-07-01
    “…Then come two times of prayer (9:18, 29), the first prior to and the second on the occasion of visible transformation on a mountain, the “transfiguration,” regarding Jesus’ prophetic role and his coming suffering. …”
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  17. 2137

    Calculation of Flood Recurrence of Delibekirli Basin (Kırıkhan/Hatay) using Statistical and Deterministic Methods and Modeling with HEC-RAS by Mahsum Bozdoğan, Ergin Canpolat

    Published 2024-07-01
    “…In this study, the flood risk potential of the Delibekirli Stream Basin, which is located in the central part of the Amanos Mountains and has flood records in 2014 and 2015, was revealed by statistical and deterministic methods. …”
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  18. 2138

    Weathering Processes and Mechanisms of Low-Grade Metamorphic Rock following Freeze-Thaw Processes by Guopeng Wu, Kai Cui, Pei Wang, Wenwu Chen

    Published 2023-01-01
    “…Examples of such materials are slate and phyllite, which are employed approximately mountainous permafrost zones. In order to study the weathering processes and mechanisms in low-grade metamorphic rock following freeze-thaw weathering processes, the freeze-thaw cycles were applied. …”
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  19. 2139

    Estimating the Geological Strength Index (GSI) in Regional Seismic-Landslide Zonation Using the Empirical Regression Model by M. E. Mirabedini, E. Haghshenas, N. Ganjian

    Published 2022-01-01
    “…An empirical regression model was presented to estimate the Geological Strength Index (GSI) with an implication on geological quadrangle of Gorgan region at Alborz mountains range (north of Iran). Two main sets of data were applied in this study: (1) geomorphological data including the slope height, aspect, and distance from faults and distance from thrusts and (2) the physical and mechanical properties of rocks including the unit weight, uniaxial compressive strength (σci), and the petrographic constant (mί) of intact rock. …”
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  20. 2140