6 research outputs found

    Numerical simulation of stress distribution

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    The Rogun hydropower plant is being constructed in Tajikistan, in the valley of the Vakhsh River. The construction site is located in a narrow gorge separating the Vakhsh and Surkh-Ku ridges. Most of the hydroelectric complex structures are located within a single tectonic block, which is bounded by two faults - Ionakhsh and Gulizindan, which are proximal to the Vakhsh regional fault. The study of stress distribution around the diversion tunnel was carried out by numerical simulation, which aimed to identify the stress distribution in the strongly dislocated heterogeneous rock massif before and after the tunnel creation. The underground cavity of the tunnel is a significant factor influencing the natural stress field of the rock massif. An area with critical values of the strength coefficient in the working roof, caused by the presence of a weak layer of Lower Cretaceous siltstones, is revealed in the tunnel location. The size of this area reaches two tunnel diameters. The change of stresses and their concentration around the underground working can cause deformations in the roof (collapse or rock bumps)

    Numerical simulation of stress distribution

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    The Rogun hydropower plant is being constructed in Tajikistan, in the valley of the Vakhsh River. The construction site is located in a narrow gorge separating the Vakhsh and Surkh-Ku ridges. Most of the hydroelectric complex structures are located within a single tectonic block, which is bounded by two faults - Ionakhsh and Gulizindan, which are proximal to the Vakhsh regional fault. The study of stress distribution around the diversion tunnel was carried out by numerical simulation, which aimed to identify the stress distribution in the strongly dislocated heterogeneous rock massif before and after the tunnel creation. The underground cavity of the tunnel is a significant factor influencing the natural stress field of the rock massif. An area with critical values of the strength coefficient in the working roof, caused by the presence of a weak layer of Lower Cretaceous siltstones, is revealed in the tunnel location. The size of this area reaches two tunnel diameters. The change of stresses and their concentration around the underground working can cause deformations in the roof (collapse or rock bumps)

    Shallow Landslide Susceptibility Mapping in Sochi Ski-Jump Area Using GIS and Numerical Modelling

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    The mountainous region of Greater Sochi, including the Olympic ski-jump complex area, located in the northern Caucasus, is always subjected to landslides. The weathered mudstone of low strength and potential high-intensity earthquakes are considered as the crucial factors causing slope instability in the ski-jump complex area. This study aims to conduct a seismic slope instability map of the area. A slope map was derived from a digital elevation model (DEM) and calculated using ArcGIS. The numerical modelling of slope stability with various slope angles was conducted using Geostudio. The Spencer method was applied to calculate the slope safety factors (Fs). The pseudostatic analysis was used to compute Fs considering seismic effect. A good correlation between Fs and slope angle was found. Combining these data, sets slope instability maps were achieved. Newmark displacement maps were also drawn according to empirical regression equations. The result shows that the static safety factor map corresponds to the existing slope instability locations in a shallow landslide inventory map. The seismic safety factor maps and Newmark displacement maps may be applied to predict potential landslides of the study area in the case of earthquake occurrence

    Application of GIS-based bivariate statistical methods for landslide potential assessment in Sapa, Vietnam

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    ΠΠΊΡ‚ΡƒΠ°Π»ΡŒΠ½ΠΎΡΡ‚ΡŒ. ΠŸΡ€ΠΎΠ³Π½ΠΎΠ·ΠΈΡ€ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΈ минимизация послСдствий стихийных бСдствий ΡΠ²Π»ΡΡŽΡ‚ΡΡ ваТнСйшими Π·Π°Π΄Π°Ρ‡Π°ΠΌΠΈ для ΠΏΡ€Π°Π²ΠΈΡ‚Π΅Π»ΡŒΡΡ‚Π² Π²ΠΎ всСм ΠΌΠΈΡ€Π΅, Π²ΠΊΠ»ΡŽΡ‡Π°Ρ Π’ΡŒΠ΅Ρ‚Π½Π°ΠΌ. Оползни ΡΠ²Π»ΡΡŽΡ‚ΡΡ ΠΎΠ΄Π½ΠΈΠΌ ΠΈΠ· Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ распространСнных Π²ΠΈΠ΄ΠΎΠ² стихийных бСдствий Π²ΠΎ Π’ΡŒΠ΅Ρ‚Π½Π°ΠΌΠ΅, особСнно Π² сСвСрных Π³ΠΎΡ€Π½Ρ‹Ρ… провинциях, Ρ‡Ρ‚ΠΎ ΠΏΡ€ΠΈΠ²ΠΎΠ΄ΠΈΡ‚ ΠΊ Π·Π½Π°Ρ‡ΠΈΡ‚Π΅Π»ΡŒΠ½Ρ‹ΠΌ чСловСчСским ΠΆΠ΅Ρ€Ρ‚Π²Π°ΠΌ ΠΈ ΠΌΠ°Ρ‚Π΅Ρ€ΠΈΠ°Π»ΡŒΠ½ΠΎΠΌΡƒ ΡƒΡ‰Π΅Ρ€Π±Ρƒ. Π’ этом исслСдовании для ΠΎΡ†Π΅Π½ΠΊΠΈ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»ΡŒΠ½ΠΎΠ³ΠΎ развития ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ Π² Ρ€Π°ΠΉΠΎΠ½Π΅ Π¨Π°ΠΏΠ°, провинция Π›Π°ΠΎΠΊΠ°ΠΉ, ΠΏΡ€ΠΈΠΌΠ΅Π½ΡΠ»ΠΈΡΡŒ статистичСскиС ΠΌΠ΅Ρ‚ΠΎΠ΄Ρ‹, с использованиСм Π³Π΅ΠΎΠΈΠ½Ρ„ΠΎΡ€ΠΌΠ°Ρ†ΠΈΠΎΠ½Π½Ρ‹Ρ… систСм (Π“Π˜Π‘). Для Ρ€Π΅ΡˆΠ΅Π½ΠΈΡ поставлСнной Π·Π°Π΄Π°Ρ‡ΠΈ Π±Ρ‹Π»ΠΎ ΠΎΡ‚ΠΎΠ±Ρ€Π°Π½ΠΎ Π΄Π΅Π²ΡΡ‚ΡŒ Ρ„Π°ΠΊΡ‚ΠΎΡ€ΠΎΠ², ΠΎΠΏΡ€Π΅Π΄Π΅Π»ΡΡŽΡ‰ΠΈΡ… ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΡƒΡŽ Π²ΠΎΡΠΏΡ€ΠΈΠΈΠΌΡ‡ΠΈΠ²ΠΎΡΡ‚ΡŒ Π½Π° рассматриваСмой Ρ‚Π΅Ρ€Ρ€ΠΈΡ‚ΠΎΡ€ΠΈΠΈ: высота Π½Π°Π΄ ΡƒΡ€ΠΎΠ²Π½Π΅ΠΌ моря, расстояниС Π΄ΠΎ Π΄ΠΎΡ€ΠΎΠ³, ΠΊΡ€ΡƒΡ‚ΠΈΠ·Π½Π° склонов, расстояниС ΠΎΡ‚ Ρ€Π°Π·Π»ΠΎΠΌΠΎΠ², срСднСмСсячноС количСство осадков, Π²Π΅Ρ€Ρ‚ΠΈΠΊΠ°Π»ΡŒΠ½ΠΎΠ΅ расчлСнСниС Ρ€Π΅Π»ΡŒΠ΅Ρ„Π°, зСмлСпользованиС, Ρ‚ΠΈΠΏ ΠΊΠΎΡ€Ρ‹ вывСтривания ΠΈ расстояниС Π΄ΠΎ эрозионной сСти. Основная Ρ†Π΅Π»ΡŒ исслСдования Π·Π°ΠΊΠ»ΡŽΡ‡Π°Π΅Ρ‚ΡΡ Π² ΠΏΠΎΠ΄Π³ΠΎΡ‚ΠΎΠ²ΠΊΠ΅ ΠΊΠ°Ρ€Ρ‚ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»ΡŒΠ½ΠΎΠ³ΠΎ развития ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ для Ρ€Π°ΠΉΠΎΠ½Π° Π¨Π°ΠΏΠ°. ΠšΡ€ΠΎΠΌΠ΅ Ρ‚ΠΎΠ³ΠΎ, Π²Ρ‹ΠΏΠΎΠ»Π½Π΅Π½Π½Ρ‹Π΅ Ρ€Π°Π±ΠΎΡ‚Ρ‹ продСмонстрировали ΡΡ„Ρ„Π΅ΠΊΡ‚ΠΈΠ²Π½ΠΎΡΡ‚ΡŒ ΠΈΡΠΏΠΎΠ»ΡŒΠ·ΠΎΠ²Π°Π½Π½Ρ‹Ρ… статистичСских ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΎΠ² ΠΏΡ€ΠΈ ΠΎΡ†Π΅Π½ΠΊΠ΅ восприимчивости Ρ‚Π΅Ρ€Ρ€ΠΈΡ‚ΠΎΡ€ΠΈΠΈ ΠΊ ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΠΎΠΌΡƒ процСссу. ΠžΠ±ΡŠΠ΅ΠΊΡ‚ΠΎΠΌ исслСдования являСтся оползнСвая Π²ΠΎΡΠΏΡ€ΠΈΠΈΠΌΡ‡ΠΈΠ²ΠΎΡΡ‚ΡŒ Π² Ρ€Π°ΠΉΠΎΠ½Π΅ Π¨Π°ΠΏΠ° ΠΏΡ€ΠΎΠ²ΠΈΠ½Ρ†ΠΈΠΈ Π›Π°ΠΎΠΊΠ°ΠΉ (Π’ΡŒΠ΅Ρ‚Π½Π°ΠΌ). ΠœΠ΅Ρ‚ΠΎΠ΄Ρ‹: статистичСскиС ΠΌΠ΅Ρ‚ΠΎΠ΄Ρ‹ с использованиСм Π“Π˜Π‘, Π²ΠΊΠ»ΡŽΡ‡Π°Ρ ΠΌΠ΅Ρ‚ΠΎΠ΄ ΡΠΎΠΎΡ‚Π½ΠΎΡˆΠ΅Π½ΠΈΡ частотностСй (Π°Π½Π³Π». Frequency Ratio method - FR), ΠΌΠ΅Ρ‚ΠΎΠ΄ Π°Π½Π°Π»ΠΈΠ·Π° ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΠΎΠΉ восприимчивости (Π°Π½Π³Π». Landslide Susceptibility Analysis method - LSA) ΠΈ ΠΌΠ΅Ρ‚ΠΎΠ΄ статистичСского индСкса (Π°Π½Π³Π». Statistical Index method - SI). Π Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚Ρ‹. Π‘Ρ‹Π»ΠΈ построСны ΠΊΠ°Ρ€Ρ‚Ρ‹ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»ΡŒΠ½ΠΎΠ³ΠΎ развития ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ для исслСдуСмой Ρ‚Π΅Ρ€Ρ€ΠΈΡ‚ΠΎΡ€ΠΈΠΈ, которая Π±Ρ‹Π»Π° Ρ€Π°Π·Π΄Π΅Π»Π΅Π½Π° Π½Π° ΠΏΡΡ‚ΡŒ Π·ΠΎΠ½: ΠΎΡ‡Π΅Π½ΡŒ Π½ΠΈΠ·ΠΊΠΎΠ³ΠΎ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»Π°, Π½ΠΈΠ·ΠΊΠΎΠ³ΠΎ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»Π°, срСднСго ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»Π°, высокого ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»Π° ΠΈ ΠΎΡ‡Π΅Π½ΡŒ высокого ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»Π°. ΠŸΠ»ΠΎΡ‰Π°Π΄ΡŒ ΠΏΠΎΠ΄ ΠΊΡ€ΠΈΠ²ΠΎΠΉ ошибок Π±Ρ‹Π»Π° использована для ΠΎΡ†Π΅Π½ΠΊΠΈ достовСрности этих ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ. ΠŸΡ€ΠΎΡ†Π΅Π½Ρ‚Ρ‹ успСха ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ для Ρ‚Ρ€Π΅Π½ΠΈΡ€ΠΎΠ²ΠΎΡ‡Π½Ρ‹Ρ… Π΄Π°Π½Π½Ρ‹Ρ… ΡΠΎΡΡ‚Π°Π²Π»ΡΡŽΡ‚ 74,60 % (FR), 70,82 % (LSA) ΠΈ 76,36 % (SI). ΠŸΡ€ΠΎΡ†Π΅Π½Ρ‚Ρ‹ прогнозирования ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ для Π΄Π°Π½Π½Ρ‹Ρ… тСстирования ΡΠΎΡΡ‚Π°Π²Π»ΡΡŽΡ‚ 77,01 % (FR), 74,36 % (LSA) ΠΈ 78,11 % (SI). ΠžΡ†Π΅Π½ΠΊΠ° эффСктивности ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ ΠΏΠΎΠΊΠ°Π·Π°Π»Π°, Ρ‡Ρ‚ΠΎ всС Ρ‚Ρ€ΠΈ ΠΌΠ΅Ρ‚ΠΎΠ΄Π° ΡΠ²Π»ΡΡŽΡ‚ΡΡ эффСктивными для ΠΎΡ†Π΅Π½ΠΊΠΈ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»ΡŒΠ½ΠΎΠ³ΠΎ развития ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΠΎΠ³ΠΎ процСсса Π² Ρ€Π°ΠΉΠΎΠ½Π΅ исслСдования. Π Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚Ρ‹ исслСдований ΠΈΠΌΠ΅ΡŽΡ‚ ΠΈΡΠΊΠ»ΡŽΡ‡ΠΈΡ‚Π΅Π»ΡŒΠ½ΠΎ Π²Π°ΠΆΠ½ΠΎΠ΅ Π·Π½Π°Ρ‡Π΅Π½ΠΈΠ΅ для планирования зСмлСпользования ΠΈ экономичСского развития, Π° Ρ‚Π°ΠΊΠΆΠ΅ для ΠΌΠΈΠ½ΠΈΠΌΠΈΠ·Π°Ρ†ΠΈΠΈ ΡƒΡ‰Π΅Ρ€Π±Π° ΠΎΡ‚ ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ.The relevance. Predicting and minimizing the impact of natural disasters are critical tasks for governments worldwide, including Vietnam. Landslides are one of the most frequent types of natural disasters in Vietnam, especially in the northern mountainous provinces, resulting in significant loss of life and property. In this study, the GIS-based bivariate statistical methods were applied for assessing landslide potential in Sapa district, Laocai province, Vietnam. For assessing landslide susceptibility, nine landslide-related factors were selected, including elevation, distance to roads, slope, distance to faults, average monthly precipitation, relative relief, land use, crust weathering, and distance to drainage. The main aim of this study is to prepare landslide potential maps for the study area. In addition, the study also demonstrated the effectiveness of bivariate statistical methods for landslide susceptibility assessment. Object of the study is the landslide susceptibility in Sapa district, Laocai province, Vietnam. Methods: GIS-based bivariate statistical methods including frequency ratio, landslide susceptibility analysis, and statistical index. Results. Landslide potential maps were prepared using GIS-based bivariate statistical methods. The study area is divided into five landslide potential zones: very low, low, moderate, high, and very high. The area under the curve of the receiver operating characteristic (AUCROC) was used to evaluate the performance of these models. The success rates of the models for the training data are 74,60 % frequency ratio, 70,82 % landslide susceptibility analysis and 76,36 % statistical index. The prediction rates of the models for the testing data are 77,01 % frequency ratio, 74,36 % landslide susceptibility analysis and 78,11 % statistical index. The performance evaluation of the models revealed that all three techniques are efficient in assessing landslide potential in the study area. Study results are critical for land use planning and economic development, as well as minimizing landslide-related damage

    Abstracts of The Second Eurasian RISK-2020 Conference and Symposium

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    This abstract book contains abstracts of the various research ideas presented at The Second Eurasian RISK-2020 Conference and Symposium.The RISK-2020 Conference and Symposium served as a perfect venue for practitioners, engineers, researchers, scientists, managers and decision-makers from all over the world to exchange ideas and technology about the latest innovation developments dealing with risk minimization
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