12 research outputs found
HIERARCHICAL CLUSTERIZATION AND DEEP LEARNING MODEL RANDOM FOREST OF BANKSβ STABILITY UNDER RISK CONDITIONS
Certain theoretical aspects of the stability of Russian banks under risk conditions have been studied. The relevance is due to the fact that in conditions of market uncertainty and risk, approaches to ensure the stability of banks using artificial intelligence are increasingly being used. The goal is to identify patterns between the characteristics of Assets and ROA (Return on Assets), an indicator of return on assets, and obtain a forecast value of Sberbankβs net profit. The result of the study was hierarchical clustering, as well as the generated DeepΒ Learning model Random Forest, which calculated the predicted value of the Sberbankβs net profit. The novelty lies in the fact that the work puts forward and proves the hypothesis that using the Random Forest DeepΒ learning model, a forecast of the net profit of commercial banks can be obtained, which predetermines the stability and dynamics of their development. The conclusions from the study boil down to the fact that a DeepΒ Learning model Random Forest was developed to forecast the amount of net profit, which for Sberbank for 2023 amounted to 38,631 billion rubles, which coincided with its actual value. The area of application of the results obtained is commercial banks
ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΌΠ΅ΡΠΎΠ΄ΠΈΠΊΠΈ Β«Π‘Π΅ΡΠ΅Π²ΠΎΠΉ ΡΠ°ΠΌΠΎΠΎΡΡΠ΅ΡΒ» Π΄Π»Ρ ΠΈΠ·ΡΡΠ΅Π½ΠΈΡ ΡΠΏΠ΅ΡΠΈΡΠΈΠΊΠΈ ΠΈΠ½ΡΠ΅ΡΠ½Π΅Ρ-ΡΠΎΡΠΈΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΏΠΎΠ΄ΡΠΎΡΡΠΊΠΎΠ² ΠΈ ΡΠ½ΠΎΡΠ΅ΠΉ Ρ Π½Π°ΡΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½ΡΠ΅Π»Π»Π΅ΠΊΡΠ°
Introduction. The study of specific characteristics of online socialization among adolescents and young adults with disabilities, especially intellectual disabilities, is a new and promising direction in special education that requires the development of methodological approaches and foundations for conducting research of this kind.
Methods. The study of specifics characteristics of online socialization in individuals with intellectual disabilities is associated with a description of their socialization and online-based formation, in comparison with typically developing peers. Researchers should understand online interaction as a form of alternative communication, a way of adaptation and a potential source of online risks individuals face. The Internet Userβs Self-report diagnostic tool was tested using the samples of typically developing adolescents and young adults (n = 181) and respondents of the same age with intellectual disabilities (n = 119).
Results. Testing the Internet Userβs Self-report using samples of adolescents and young adults with mental retardation and their typically developing adolescents showed that this diagnostic tool is easily understood by respondents from both groups and can identify qualitative and quantitative differences between the samples. The respondents with mental retardation show less online activity related to search for information and a low awareness of online phenomena and the phenomena of online interaction; they use the Internet as an additional field for realizing the need for communication and more aggressively protect their online interaction space from parental control.
Discussion. The presented data open up promising directions of research in the field of online socialization of students with developmental disabilities, including (a) primary screening within the framework of the primary disease in comparison with typically developing peers, (b) in-depth study of age ranges within nosologies and identification of age differences within nosological groups, and (c) differentiated study comparing different nosological categories and identifying intergroup differences.ΠΠ²Π΅Π΄Π΅Π½ΠΈΠ΅. ΠΠ·ΡΡΠ΅Π½ΠΈΠ΅ ΡΠΏΠ΅ΡΠΈΡΠΈΠΊΠΈ ΡΠ΅ΡΠ΅Π²ΠΎΠΉ ΡΠΎΡΠΈΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΏΠΎΠ΄ΡΠΎΡΡΠΊΠΎΠ² ΠΈ ΡΠ½ΠΎΡΠ΅ΠΉ Ρ ΠΠΠ ΠΈ, Π² ΡΠ°ΡΡΠ½ΠΎΡΡΠΈ, Ρ Π½Π°ΡΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½ΡΠ΅Π»Π»Π΅ΠΊΡΠ° ΡΠ²Π»ΡΠ΅ΡΡΡ Π½ΠΎΠ²ΡΠΌ ΠΈ ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Π½ΡΠΌ Π½Π°ΠΏΡΠ°Π²Π»Π΅Π½ΠΈΠ΅ΠΌ Π² ΡΠΏΠ΅ΡΠΈΠ°Π»ΡΠ½ΠΎΠΉ ΠΏΡΠΈΡ
ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈ Π½ΡΠΆΠ΄Π°Π΅ΡΡΡ Π² ΡΠ°Π·ΡΠ°Π±ΠΎΡΠΊΠ΅ ΠΌΠ΅ΡΠΎΠ΄ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΏΠΎΠ΄Ρ
ΠΎΠ΄ΠΎΠ² ΠΈ ΠΌΠ΅ΡΠΎΠ΄ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΎΡΠ½ΠΎΠ² ΠΏΡΠΎΠ²Π΅Π΄Π΅Π½ΠΈΡ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ ΠΏΠΎΠ΄ΠΎΠ±Π½ΠΎΠ³ΠΎ ΡΠΎΠ΄Π°.
ΠΠ΅ΡΠΎΠ΄Ρ. ΠΠ·ΡΡΠ΅Π½ΠΈΠ΅ ΡΠΏΠ΅ΡΠΈΡΠΈΠΊΠΈ ΡΠ΅ΡΠ΅Π²ΠΎΠΉ ΡΠΎΡΠΈΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ Π»ΠΈΡ Ρ Π½Π°ΡΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½ΡΠ΅Π»Π»Π΅ΠΊΡΠ° ΡΠ²ΡΠ·Π°Π½ΠΎ Ρ ΠΎΠΏΠΈΡΠ°Π½ΠΈΠ΅ΠΌ ΠΎΡΠΎΠ±Π΅Π½Π½ΠΎΡΡΠ΅ΠΉ ΠΈΡ
ΡΠΎΡΠΈΠ°Π»ΠΈΠ·Π°ΡΠΈΠΎΠ½Π½ΠΎ-ΡΠ΅ΡΠ΅Π²ΠΎΠ³ΠΎ ΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΡ, Π² ΡΡΠ°Π²Π½Π΅Π½ΠΈΠΈ Ρ Π½ΠΎΡΠΌΠ°ΡΠΈΠ²Π½ΠΎ ΡΠ°Π·Π²ΠΈΠ²Π°ΡΡΠΈΠΌΠΈΡΡ ΡΠ²Π΅ΡΡΡΠ½ΠΈΠΊΠ°ΠΌΠΈ ΠΏΡΠ΅Π΄ΠΏΠΎΠ»Π°Π³Π°ΡΡΠΈΠΌ ΠΏΠΎΠ½ΠΈΠΌΠ°Π½ΠΈΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°ΡΠ΅Π»Π΅ΠΌ ΠΈΠ½ΡΠ΅ΡΠ½Π΅Ρ-Π²Π·Π°ΠΈΠΌΠΎΠ΄Π΅ΠΉΡΡΠ²ΠΈΡ ΠΊΠ°ΠΊ ΡΠΎΡΠΌΡ Π°Π»ΡΡΠ΅ΡΠ½Π°ΡΠΈΠ²Π½ΠΎΠΉ ΠΊΠΎΠΌΠΌΡΠ½ΠΈΠΊΠ°ΡΠΈΠΈ, ΡΠΏΠΎΡΠΎΠ±Π° Π°Π΄Π°ΠΏΡΠ°ΡΠΈΠΈ ΠΈ ΠΏΠΎΡΠ΅Π½ΡΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΠΈΡΡΠΎΡΠ½ΠΈΠΊΠ° ΡΠ΅ΡΠ΅Π²ΡΡ
ΡΠΈΡΠΊΠΎΠ² Π»ΠΈΡΠ½ΠΎΡΡΠΈ. ΠΠ΅ΡΠΎΠ΄ΠΈΡΠ΅ΡΠΊΠΈΠΉ ΠΈΠ½ΡΡΡΡΠΌΠ΅Π½ΡΠ°ΡΠΈΠΉ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½ Π°Π²ΡΠΎΡΡΠΊΠΎΠΉ ΠΌΠ΅ΡΠΎΠ΄ΠΈΠΊΠΎΠΉ Β«Π‘Π΅ΡΠ΅Π²ΠΎΠΉ ΡΠ°ΠΌΠΎΠΎΡΡΠ΅ΡΒ», Π°ΠΏΡΠΎΠ±ΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠΉ Ρ ΡΡΠ°ΡΡΠΈΠ΅ΠΌ 181 ΡΠ΅ΡΠΏΠΎΠ½Π΄Π΅Π½ΡΠ° ΠΏΠΎΠ΄ΡΠΎΡΡΠΊΠΎΠ²ΠΎΠ³ΠΎ ΠΈ ΡΠ½ΠΎΡΠ΅ΡΠΊΠΎΠ³ΠΎ Π²ΠΎΠ·ΡΠ°ΡΡΠ° Ρ Π½ΠΎΡΠΌΠ°ΡΠΈΠ²Π½ΡΠΌ ΡΠ°Π·Π²ΠΈΡΠΈΠ΅ΠΌ ΠΈ 119 ΡΠ΅ΡΠΏΠΎΠ½Π΄Π΅Π½ΡΠΎΠ² ΡΠ΅Ρ
ΠΆΠ΅ Π²ΠΎΠ·ΡΠ°ΡΡΠΎΠ² Ρ Π½Π°ΡΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½ΡΠ΅Π»Π»Π΅ΠΊΡΠ°.
Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. ΠΠΏΡΠΎΠ±Π°ΡΠΈΡ ΠΌΠ΅ΡΠΎΠ΄ΠΈΠΊΠΈ Β«Π‘Π΅ΡΠ΅Π²ΠΎΠΉ ΡΠ°ΠΌΠΎΠΎΡΡΠ΅ΡΒ» Ρ ΡΡΠ°ΡΡΠΈΠ΅ΠΌ Π²ΡΠ±ΠΎΡΠΎΠΊ ΠΏΠΎΠ΄ΡΠΎΡΡΠΊΠΎΠ² ΠΈ ΡΠ½ΠΎΡΠ΅ΠΉ Ρ ΡΠΌΡΡΠ²Π΅Π½Π½ΠΎΠΉ ΠΎΡΡΡΠ°Π»ΠΎΡΡΡΡ ΠΈ ΠΈΡ
Π½ΠΎΡΠΌΠ°ΡΠΈΠ²Π½ΠΎ ΡΠ°Π·Π²ΠΈΠ²Π°ΡΡΠΈΡ
ΡΡ ΡΠ²Π΅ΡΡΡΠ½ΠΈΠΊΠΎΠ² ΠΏΠΎΠΊΠ°Π·Π°Π»Π°, ΡΡΠΎ Π΄Π°Π½Π½ΡΠΉ ΠΈΠ½ΡΡΡΡΠΌΠ΅Π½ΡΠ°ΡΠΈΠΉ Π΄ΠΎΡΡΡΠΏΠ΅Π½ Π΄Π»Ρ Π²ΡΠΏΠΎΠ»Π½Π΅Π½ΠΈΡ ΡΠ΅ΡΠΏΠΎΠ½Π΄Π΅Π½ΡΠ°ΠΌ ΠΎΠ±Π΅ΠΈΡ
Π³ΡΡΠΏΠΏ ΠΈ ΠΏΡΠΈΠΌΠ΅Π½ΠΈΠΌ Π΄Π»Ρ Π²ΡΡΠ²Π»Π΅Π½ΠΈΡ ΠΊΠ°ΡΠ΅ΡΡΠ²Π΅Π½Π½ΠΎ-ΠΊΠΎΠ»ΠΈΡΠ΅ΡΡΠ²Π΅Π½Π½ΡΡ
ΡΠ°Π·Π»ΠΈΡΠΈΠΉ ΠΌΠ΅ΠΆΠ΄Ρ Π²ΡΠ±ΠΎΡΠΊΠ°ΠΌΠΈ. Π£ ΡΠ΅ΡΠΏΠΎΠ½Π΄Π΅Π½ΡΠΎΠ² Ρ ΡΠΌΡΡΠ²Π΅Π½Π½ΠΎΠΉ ΠΎΡΡΡΠ°Π»ΠΎΡΡΡΡ Π½Π°Π±Π»ΡΠ΄Π°ΡΡΡΡ ΠΌΠ΅Π½ΡΡΠ°Ρ Π°ΠΊΡΠΈΠ²Π½ΠΎΡΡΡ Π² Π‘Π΅ΡΠΈ ΠΏΠΎ ΠΏΠΎΠΈΡΠΊΡ ΠΈΠ½ΡΠΎΡΠΌΠ°ΡΠΈΠΈ, Π½ΠΈΠ·ΠΊΠ°Ρ ΠΎΡΠ²Π΅Π΄ΠΎΠΌΠ»Π΅Π½Π½ΠΎΡΡΡ ΠΎ ΡΠ΅ΡΠ΅Π²ΡΡ
ΡΠ²Π»Π΅Π½ΠΈΡΡ
ΠΈ ΡΠ΅Π½ΠΎΠΌΠ΅Π½Π°Ρ
ΡΠ΅ΡΠ΅Π²ΠΎΠ³ΠΎ Π²Π·Π°ΠΈΠΌΠΎΠ΄Π΅ΠΉΡΡΠ²ΠΈΡ, ΠΈΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΠ½ΡΠ΅ΡΠ½Π΅ΡΠ° ΠΊΠ°ΠΊ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡΠ΅Π»ΡΠ½ΠΎΠ³ΠΎ ΠΏΠΎΠ»Ρ ΡΠ΅Π°Π»ΠΈΠ·Π°ΡΠΈΠΈ Π²ΡΡΠ°ΠΆΠ΅Π½Π½ΠΎΠΉ ΠΏΠΎΡΡΠ΅Π±Π½ΠΎΡΡΠΈ Π² ΠΎΠ±ΡΠ΅Π½ΠΈΠΈ ΠΈ Π±ΠΎΠ»Π΅Π΅ Π°Π³ΡΠ΅ΡΡΠΈΠ²Π½Π°Ρ Π·Π°ΡΠΈΡΠ° ΡΠ²ΠΎΠ΅Π³ΠΎ ΡΠ΅ΡΠ΅Π²ΠΎΠ³ΠΎ ΠΏΡΠΎΡΡΡΠ°Π½ΡΡΠ²Π° ΠΎΡ Π²ΠΌΠ΅ΡΠ°ΡΠ΅Π»ΡΡΡΠ²Π° ΡΠΎΠ΄ΠΈΡΠ΅Π»Π΅ΠΉ.
ΠΠ±ΡΡΠΆΠ΄Π΅Π½ΠΈΠ΅ ΡΠ΅Π·ΡΠ»ΡΡΠ°ΡΠΎΠ². ΠΡΠ΅Π΄ΡΡΠ°Π²Π»Π΅Π½Π½ΡΠ΅ Π΄Π°Π½Π½ΡΠ΅ ΠΎΡΠΊΡΡΠ²Π°ΡΡ ΡΡΠ΄ ΠΏΠ΅ΡΡΠΏΠ΅ΠΊΡΠΈΠ²Π½ΡΡ
Π½Π°ΠΏΡΠ°Π²Π»Π΅Π½ΠΈΠΉ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΡ Π² ΠΏΡΠ΅Π΄ΠΌΠ΅ΡΠ½ΠΎΠΉ ΠΎΠ±Π»Π°ΡΡΠΈ ΡΠ΅ΡΠ΅Π²ΠΎΠΉ ΡΠΎΡΠΈΠ°Π»ΠΈΠ·Π°ΡΠΈΠΈ ΠΎΠ±ΡΡΠ°ΡΡΠΈΡ
ΡΡ Ρ Π½Π°ΡΡΡΠ΅Π½ΠΈΠ΅ΠΌ ΡΠ°Π·Π²ΠΈΡΠΈΡ: 1) ΠΏΠ΅ΡΠ²ΠΈΡΠ½ΡΠΉ ΡΠΊΡΠΈΠ½ΠΈΠ½Π³ Π² ΡΠ°ΠΌΠΊΠ°Ρ
Π²Π΅Π΄ΡΡΠ΅Π³ΠΎ Π½Π°ΡΡΡΠ΅Π½ΠΈΡ ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ Ρ Π½ΠΎΡΠΌΠ°ΡΠΈΠ²Π½ΠΎ ΡΠ°Π·Π²ΠΈΠ²Π°ΡΡΠΈΠΌΠΈΡΡ ΡΠ²Π΅ΡΡΡΠ½ΠΈΠΊΠ°ΠΌΠΈ; 2) ΡΠ³Π»ΡΠ±Π»Π΅Π½Π½ΠΎΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΏΠΎ Π²ΠΎΠ·ΡΠ°ΡΡΠ½ΡΠΌ Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π°ΠΌ Π² ΡΠ°ΠΌΠΊΠ°Ρ
ΠΎΠ΄Π½ΠΎΠΉ Π½ΠΎΠ·ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈ Π²ΡΡΠ²Π»Π΅Π½ΠΈΠ΅ Π²ΠΎΠ·ΡΠ°ΡΡΠ½ΡΡ
ΡΠ°Π·Π»ΠΈΡΠΈΠΉ Π²Π½ΡΡΡΠΈ ΠΎΠ΄Π½ΠΎΠΉ Π½ΠΎΠ·ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠΉ Π³ΡΡΠΏΠΏΡ; 3) Π΄ΠΈΡΡΠ΅ΡΠ΅Π½ΡΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ ΡΠ°Π·Π½ΡΡ
Π½ΠΎΠ·ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
ΠΊΠ°ΡΠ΅Π³ΠΎΡΠΈΠΉ ΠΈ Π²ΡΡΠ²Π»Π΅Π½ΠΈΡ ΠΌΠ΅ΠΆΠ³ΡΡΠΏΠΏΠΎΠ²ΡΡ
ΡΠ°Π·Π»ΠΈΡΠΈΠΉ
Geochemical composition of sediment samples from Krasnov field in the Mid Atlantic Ridge
This paper is dedicated to the geochemical studies of two bottom sediment cores that were taken during cruise 28 of the R/V Professor Logachev in the Mid-Atlantic Ridge (MAR) 16Β°38'N area in 2006. The chemical compositions of background metalliferous and ore (ore-bearing) carbonate sediments are presented and inter-element correlations are examined. Individual episodes are distinguished in the accumulation history of the ore-bearing and metalliferous sediments on the basis of element factor analysis
(Table 7) Chemical composition of bottom sediments from Core SO201-2-101, Shirshov Ridge, Bering Sea
(Table 2) Grain size composition of bottom sediments from Core SO201-2-101, Shirshov Ridge, Bering Sea
Analysis of lithology, grain-size composition, clay minerals, and geochemistry of Upper Pleistocene bottom sediments from the submarine Shirshov Ridge (Bering Sea) showed that the Yukon-Tanana terrane of the Central Alaska was main source area of the sediments. Sedimentary material was transported by the Yukon River through Beringia up to the shelf break, where they were entrained by a strong north-west sea current. Lithological data revealed several pulses of ice-rafted debris deposition roughly synchronous with Heinrich events and periods of weaker bottom current intensity. Based on geochemical results we distinguished intervals of an increase in paleoproductivity and extension of the oxygen minimum zone. Our results suggest that there were three stages of deposition driven by glacioeustatic sea-level fluctuations and glacial cycles in Alaska