6 research outputs found
Numerical simulation of stress distribution
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
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
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
ΠΠΊΡΡΠ°Π»ΡΠ½ΠΎΡΡΡ. ΠΡΠΎΠ³Π½ΠΎΠ·ΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ ΠΈ ΠΌΠΈΠ½ΠΈΠΌΠΈΠ·Π°ΡΠΈΡ ΠΏΠΎΡΠ»Π΅Π΄ΡΡΠ²ΠΈΠΉ ΡΡΠΈΡ
ΠΈΠΉΠ½ΡΡ
Π±Π΅Π΄ΡΡΠ²ΠΈΠΉ ΡΠ²Π»ΡΡΡΡΡ Π²Π°ΠΆΠ½Π΅ΠΉΡΠΈΠΌΠΈ Π·Π°Π΄Π°ΡΠ°ΠΌΠΈ Π΄Π»Ρ ΠΏΡΠ°Π²ΠΈΡΠ΅Π»ΡΡΡΠ² Π²ΠΎ Π²ΡΠ΅ΠΌ ΠΌΠΈΡΠ΅, Π²ΠΊΠ»ΡΡΠ°Ρ ΠΡΠ΅ΡΠ½Π°ΠΌ. ΠΠΏΠΎΠ»Π·Π½ΠΈ ΡΠ²Π»ΡΡΡΡΡ ΠΎΠ΄Π½ΠΈΠΌ ΠΈΠ· Π½Π°ΠΈΠ±ΠΎΠ»Π΅Π΅ ΡΠ°ΡΠΏΡΠΎΡΡΡΠ°Π½Π΅Π½Π½ΡΡ
Π²ΠΈΠ΄ΠΎΠ² ΡΡΠΈΡ
ΠΈΠΉΠ½ΡΡ
Π±Π΅Π΄ΡΡΠ²ΠΈΠΉ Π²ΠΎ ΠΡΠ΅ΡΠ½Π°ΠΌΠ΅, ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎ Π² ΡΠ΅Π²Π΅ΡΠ½ΡΡ
Π³ΠΎΡΠ½ΡΡ
ΠΏΡΠΎΠ²ΠΈΠ½ΡΠΈΡΡ
, ΡΡΠΎ ΠΏΡΠΈΠ²ΠΎΠ΄ΠΈΡ ΠΊ Π·Π½Π°ΡΠΈΡΠ΅Π»ΡΠ½ΡΠΌ ΡΠ΅Π»ΠΎΠ²Π΅ΡΠ΅ΡΠΊΠΈΠΌ ΠΆΠ΅ΡΡΠ²Π°ΠΌ ΠΈ ΠΌΠ°ΡΠ΅ΡΠΈΠ°Π»ΡΠ½ΠΎΠΌΡ ΡΡΠ΅ΡΠ±Ρ. Π ΡΡΠΎΠΌ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΈ Π΄Π»Ρ ΠΎΡΠ΅Π½ΠΊΠΈ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ Π² ΡΠ°ΠΉΠΎΠ½Π΅ Π¨Π°ΠΏΠ°, ΠΏΡΠΎΠ²ΠΈΠ½ΡΠΈΡ ΠΠ°ΠΎΠΊΠ°ΠΉ, ΠΏΡΠΈΠΌΠ΅Π½ΡΠ»ΠΈΡΡ ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΌΠ΅ΡΠΎΠ΄Ρ, Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ Π³Π΅ΠΎΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΎΠ½Π½ΡΡ
ΡΠΈΡΡΠ΅ΠΌ (ΠΠΠ‘). ΠΠ»Ρ ΡΠ΅ΡΠ΅Π½ΠΈΡ ΠΏΠΎΡΡΠ°Π²Π»Π΅Π½Π½ΠΎΠΉ Π·Π°Π΄Π°ΡΠΈ Π±ΡΠ»ΠΎ ΠΎΡΠΎΠ±ΡΠ°Π½ΠΎ Π΄Π΅Π²ΡΡΡ ΡΠ°ΠΊΡΠΎΡΠΎΠ², ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΡΡΠΈΡ
ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΡΡ Π²ΠΎΡΠΏΡΠΈΠΈΠΌΡΠΈΠ²ΠΎΡΡΡ Π½Π° ΡΠ°ΡΡΠΌΠ°ΡΡΠΈΠ²Π°Π΅ΠΌΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ: Π²ΡΡΠΎΡΠ° Π½Π°Π΄ ΡΡΠΎΠ²Π½Π΅ΠΌ ΠΌΠΎΡΡ, ΡΠ°ΡΡΡΠΎΡΠ½ΠΈΠ΅ Π΄ΠΎ Π΄ΠΎΡΠΎΠ³, ΠΊΡΡΡΠΈΠ·Π½Π° ΡΠΊΠ»ΠΎΠ½ΠΎΠ², ΡΠ°ΡΡΡΠΎΡΠ½ΠΈΠ΅ ΠΎΡ ΡΠ°Π·Π»ΠΎΠΌΠΎΠ², ΡΡΠ΅Π΄Π½Π΅ΠΌΠ΅ΡΡΡΠ½ΠΎΠ΅ ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²ΠΎ ΠΎΡΠ°Π΄ΠΊΠΎΠ², Π²Π΅ΡΡΠΈΠΊΠ°Π»ΡΠ½ΠΎΠ΅ ΡΠ°ΡΡΠ»Π΅Π½Π΅Π½ΠΈΠ΅ ΡΠ΅Π»ΡΠ΅ΡΠ°, Π·Π΅ΠΌΠ»Π΅ΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅, ΡΠΈΠΏ ΠΊΠΎΡΡ Π²ΡΠ²Π΅ΡΡΠΈΠ²Π°Π½ΠΈΡ ΠΈ ΡΠ°ΡΡΡΠΎΡΠ½ΠΈΠ΅ Π΄ΠΎ ΡΡΠΎΠ·ΠΈΠΎΠ½Π½ΠΎΠΉ ΡΠ΅ΡΠΈ. ΠΡΠ½ΠΎΠ²Π½Π°Ρ ΡΠ΅Π»Ρ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π·Π°ΠΊΠ»ΡΡΠ°Π΅ΡΡΡ Π² ΠΏΠΎΠ΄Π³ΠΎΡΠΎΠ²ΠΊΠ΅ ΠΊΠ°ΡΡ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ Π΄Π»Ρ ΡΠ°ΠΉΠΎΠ½Π° Π¨Π°ΠΏΠ°. ΠΡΠΎΠΌΠ΅ ΡΠΎΠ³ΠΎ, Π²ΡΠΏΠΎΠ»Π½Π΅Π½Π½ΡΠ΅ ΡΠ°Π±ΠΎΡΡ ΠΏΡΠΎΠ΄Π΅ΠΌΠΎΠ½ΡΡΡΠΈΡΠΎΠ²Π°Π»ΠΈ ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΠΎΡΡΡ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½Π½ΡΡ
ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ² ΠΏΡΠΈ ΠΎΡΠ΅Π½ΠΊΠ΅ Π²ΠΎΡΠΏΡΠΈΠΈΠΌΡΠΈΠ²ΠΎΡΡΠΈ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ ΠΊ ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΠΎΠΌΡ ΠΏΡΠΎΡΠ΅ΡΡΡ. ΠΠ±ΡΠ΅ΠΊΡΠΎΠΌ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ ΡΠ²Π»ΡΠ΅ΡΡΡ ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²Π°Ρ Π²ΠΎΡΠΏΡΠΈΠΈΠΌΡΠΈΠ²ΠΎΡΡΡ Π² ΡΠ°ΠΉΠΎΠ½Π΅ Π¨Π°ΠΏΠ° ΠΏΡΠΎΠ²ΠΈΠ½ΡΠΈΠΈ ΠΠ°ΠΎΠΊΠ°ΠΉ (ΠΡΠ΅ΡΠ½Π°ΠΌ). ΠΠ΅ΡΠΎΠ΄Ρ: ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈΠ΅ ΠΌΠ΅ΡΠΎΠ΄Ρ Ρ ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ΠΌ ΠΠΠ‘, Π²ΠΊΠ»ΡΡΠ°Ρ ΠΌΠ΅ΡΠΎΠ΄ ΡΠΎΠΎΡΠ½ΠΎΡΠ΅Π½ΠΈΡ ΡΠ°ΡΡΠΎΡΠ½ΠΎΡΡΠ΅ΠΉ (Π°Π½Π³Π». Frequency Ratio method - FR), ΠΌΠ΅ΡΠΎΠ΄ Π°Π½Π°Π»ΠΈΠ·Π° ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΠΎΠΉ Π²ΠΎΡΠΏΡΠΈΠΈΠΌΡΠΈΠ²ΠΎΡΡΠΈ (Π°Π½Π³Π». Landslide Susceptibility Analysis method - LSA) ΠΈ ΠΌΠ΅ΡΠΎΠ΄ ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΠΈΠ½Π΄Π΅ΠΊΡΠ° (Π°Π½Π³Π». Statistical Index method - SI). Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΡΠ»ΠΈ ΠΏΠΎΡΡΡΠΎΠ΅Π½Ρ ΠΊΠ°ΡΡΡ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΎΠΏΠΎΠ»Π·Π½Π΅ΠΉ Π΄Π»Ρ ΠΈΡΡΠ»Π΅Π΄ΡΠ΅ΠΌΠΎΠΉ ΡΠ΅ΡΡΠΈΡΠΎΡΠΈΠΈ, ΠΊΠΎΡΠΎΡΠ°Ρ Π±ΡΠ»Π° ΡΠ°Π·Π΄Π΅Π»Π΅Π½Π° Π½Π° ΠΏΡΡΡ Π·ΠΎΠ½: ΠΎΡΠ΅Π½Ρ Π½ΠΈΠ·ΠΊΠΎΠ³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π°, Π½ΠΈΠ·ΠΊΠΎΠ³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π°, ΡΡΠ΅Π΄Π½Π΅Π³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π°, Π²ΡΡΠΎΠΊΠΎΠ³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π° ΠΈ ΠΎΡΠ΅Π½Ρ Π²ΡΡΠΎΠΊΠΎΠ³ΠΎ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»Π°. ΠΠ»ΠΎΡΠ°Π΄Ρ ΠΏΠΎΠ΄ ΠΊΡΠΈΠ²ΠΎΠΉ ΠΎΡΠΈΠ±ΠΎΠΊ Π±ΡΠ»Π° ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½Π° Π΄Π»Ρ ΠΎΡΠ΅Π½ΠΊΠΈ Π΄ΠΎΡΡΠΎΠ²Π΅ΡΠ½ΠΎΡΡΠΈ ΡΡΠΈΡ
ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ. ΠΡΠΎΡΠ΅Π½ΡΡ ΡΡΠΏΠ΅Ρ
Π° ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ Π΄Π»Ρ ΡΡΠ΅Π½ΠΈΡΠΎΠ²ΠΎΡΠ½ΡΡ
Π΄Π°Π½Π½ΡΡ
ΡΠΎΡΡΠ°Π²Π»ΡΡΡ 74,60 % (FR), 70,82 % (LSA) ΠΈ 76,36 % (SI). ΠΡΠΎΡΠ΅Π½ΡΡ ΠΏΡΠΎΠ³Π½ΠΎΠ·ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ Π΄Π»Ρ Π΄Π°Π½Π½ΡΡ
ΡΠ΅ΡΡΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠΎΡΡΠ°Π²Π»ΡΡΡ 77,01 % (FR), 74,36 % (LSA) ΠΈ 78,11 % (SI). ΠΡΠ΅Π½ΠΊΠ° ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΠΎΡΡΠΈ ΠΌΠΎΠ΄Π΅Π»Π΅ΠΉ ΠΏΠΎΠΊΠ°Π·Π°Π»Π°, ΡΡΠΎ Π²ΡΠ΅ ΡΡΠΈ ΠΌΠ΅ΡΠΎΠ΄Π° ΡΠ²Π»ΡΡΡΡΡ ΡΡΡΠ΅ΠΊΡΠΈΠ²Π½ΡΠΌΠΈ Π΄Π»Ρ ΠΎΡΠ΅Π½ΠΊΠΈ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ ΠΎΠΏΠΎΠ»Π·Π½Π΅Π²ΠΎΠ³ΠΎ ΠΏΡΠΎΡΠ΅ΡΡΠ° Π² ΡΠ°ΠΉΠΎΠ½Π΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ. Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ ΠΈΠΌΠ΅ΡΡ ΠΈΡΠΊΠ»ΡΡΠΈΡΠ΅Π»ΡΠ½ΠΎ Π²Π°ΠΆΠ½ΠΎΠ΅ Π·Π½Π°ΡΠ΅Π½ΠΈΠ΅ Π΄Π»Ρ ΠΏΠ»Π°Π½ΠΈΡΠΎΠ²Π°Π½ΠΈΡ Π·Π΅ΠΌΠ»Π΅ΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΡ ΠΈ ΡΠΊΠΎΠ½ΠΎΠΌΠΈΡΠ΅ΡΠΊΠΎΠ³ΠΎ ΡΠ°Π·Π²ΠΈΡΠΈΡ, Π° ΡΠ°ΠΊΠΆΠ΅ Π΄Π»Ρ ΠΌΠΈΠ½ΠΈΠΌΠΈΠ·Π°ΡΠΈΠΈ ΡΡΠ΅ΡΠ±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
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