12 research outputs found

    HIERARCHICAL CLUSTERIZATION AND DEEP LEARNING MODEL RANDOM FOREST OF BANKS’ STABILITY UNDER RISK CONDITIONS

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    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 Sberbank’s 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 Sberbank’s 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

    ИспользованиС ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊΠΈ Β«Π‘Π΅Ρ‚Π΅Π²ΠΎΠΉ самоотчСт» для изучСния спСцифики ΠΈΠ½Ρ‚Π΅Ρ€Π½Π΅Ρ‚-социализации подростков ΠΈ юношСй с Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½Ρ‚Π΅Π»Π»Π΅ΠΊΡ‚Π°

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    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 User’s 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 User’s 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.Π’Π²Π΅Π΄Π΅Π½ΠΈΠ΅. Π˜Π·ΡƒΡ‡Π΅Π½ΠΈΠ΅ спСцифики сСтСвой социализации подростков ΠΈ юношСй с ΠžΠ’Π— ΠΈ, Π² частности, с Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½Ρ‚Π΅Π»Π»Π΅ΠΊΡ‚Π° являСтся Π½ΠΎΠ²Ρ‹ΠΌ ΠΈ пСрспСктивным Π½Π°ΠΏΡ€Π°Π²Π»Π΅Π½ΠΈΠ΅ΠΌ Π² ΡΠΏΠ΅Ρ†ΠΈΠ°Π»ΡŒΠ½ΠΎΠΉ психологии ΠΈ нуТдаСтся Π² Ρ€Π°Π·Ρ€Π°Π±ΠΎΡ‚ΠΊΠ΅ мСтодологичСских ΠΏΠΎΠ΄Ρ…ΠΎΠ΄ΠΎΠ² ΠΈ мСтодичСских основ провСдСния исслСдований ΠΏΠΎΠ΄ΠΎΠ±Π½ΠΎΠ³ΠΎ Ρ€ΠΎΠ΄Π°. ΠœΠ΅Ρ‚ΠΎΠ΄Ρ‹. Π˜Π·ΡƒΡ‡Π΅Π½ΠΈΠ΅ спСцифики сСтСвой социализации Π»ΠΈΡ† с Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½Ρ‚Π΅Π»Π»Π΅ΠΊΡ‚Π° связано с описаниСм особСнностСй ΠΈΡ… социализационно-сСтСвого становлСния, Π² сравнСнии с Π½ΠΎΡ€ΠΌΠ°Ρ‚ΠΈΠ²Π½ΠΎ Ρ€Π°Π·Π²ΠΈΠ²Π°ΡŽΡ‰ΠΈΠΌΠΈΡΡ свСрстниками ΠΏΡ€Π΅Π΄ΠΏΠΎΠ»Π°Π³Π°ΡŽΡ‰ΠΈΠΌ ΠΏΠΎΠ½ΠΈΠΌΠ°Π½ΠΈΠ΅ исслСдоватСлСм ΠΈΠ½Ρ‚Π΅Ρ€Π½Π΅Ρ‚-взаимодСйствия ΠΊΠ°ΠΊ Ρ„ΠΎΡ€ΠΌΡ‹ Π°Π»ΡŒΡ‚Π΅Ρ€Π½Π°Ρ‚ΠΈΠ²Π½ΠΎΠΉ ΠΊΠΎΠΌΠΌΡƒΠ½ΠΈΠΊΠ°Ρ†ΠΈΠΈ, способа Π°Π΄Π°ΠΏΡ‚Π°Ρ†ΠΈΠΈ ΠΈ ΠΏΠΎΡ‚Π΅Π½Ρ†ΠΈΠ°Π»ΡŒΠ½ΠΎΠ³ΠΎ источника сСтСвых рисков личности. ΠœΠ΅Ρ‚ΠΎΠ΄ΠΈΡ‡Π΅ΡΠΊΠΈΠΉ инструмСнтарий прСдставлСн авторской ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊΠΎΠΉ Β«Π‘Π΅Ρ‚Π΅Π²ΠΎΠΉ самоотчСт», Π°ΠΏΡ€ΠΎΠ±ΠΈΡ€ΠΎΠ²Π°Π½Π½ΠΎΠΉ с участиСм 181 рСспондСнта подросткового ΠΈ юношСского возраста с Π½ΠΎΡ€ΠΌΠ°Ρ‚ΠΈΠ²Π½Ρ‹ΠΌ Ρ€Π°Π·Π²ΠΈΡ‚ΠΈΠ΅ΠΌ ΠΈ 119 рСспондСнтов Ρ‚Π΅Ρ… ΠΆΠ΅ возрастов с Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΠ΅ΠΌ ΠΈΠ½Ρ‚Π΅Π»Π»Π΅ΠΊΡ‚Π°. Π Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚Ρ‹. Апробация ΠΌΠ΅Ρ‚ΠΎΠ΄ΠΈΠΊΠΈ Β«Π‘Π΅Ρ‚Π΅Π²ΠΎΠΉ самоотчСт» с участиСм Π²Ρ‹Π±ΠΎΡ€ΠΎΠΊ подростков ΠΈ юношСй с умствСнной ΠΎΡ‚ΡΡ‚Π°Π»ΠΎΡΡ‚ΡŒΡŽ ΠΈ ΠΈΡ… Π½ΠΎΡ€ΠΌΠ°Ρ‚ΠΈΠ²Π½ΠΎ Ρ€Π°Π·Π²ΠΈΠ²Π°ΡŽΡ‰ΠΈΡ…ΡΡ свСрстников ΠΏΠΎΠΊΠ°Π·Π°Π»Π°, Ρ‡Ρ‚ΠΎ Π΄Π°Π½Π½Ρ‹ΠΉ инструмСнтарий доступСн для выполнСния рСспондСнтам ΠΎΠ±Π΅ΠΈΡ… Π³Ρ€ΡƒΠΏΠΏ ΠΈ ΠΏΡ€ΠΈΠΌΠ΅Π½ΠΈΠΌ для выявлСния качСствСнно-количСствСнных Ρ€Π°Π·Π»ΠΈΡ‡ΠΈΠΉ ΠΌΠ΅ΠΆΠ΄Ρƒ Π²Ρ‹Π±ΠΎΡ€ΠΊΠ°ΠΌΠΈ. Π£ рСспондСнтов с умствСнной ΠΎΡ‚ΡΡ‚Π°Π»ΠΎΡΡ‚ΡŒΡŽ Π½Π°Π±Π»ΡŽΠ΄Π°ΡŽΡ‚ΡΡ мСньшая Π°ΠΊΡ‚ΠΈΠ²Π½ΠΎΡΡ‚ΡŒ Π² Π‘Π΅Ρ‚ΠΈ ΠΏΠΎ поиску ΠΈΠ½Ρ„ΠΎΡ€ΠΌΠ°Ρ†ΠΈΠΈ, низкая ΠΎΡΠ²Π΅Π΄ΠΎΠΌΠ»Π΅Π½Π½ΠΎΡΡ‚ΡŒ ΠΎ сСтСвых явлСниях ΠΈ Ρ„Π΅Π½ΠΎΠΌΠ΅Π½Π°Ρ… сСтСвого взаимодСйствия, использованиС Π˜Π½Ρ‚Π΅Ρ€Π½Π΅Ρ‚Π° ΠΊΠ°ΠΊ Π΄ΠΎΠΏΠΎΠ»Π½ΠΈΡ‚Π΅Π»ΡŒΠ½ΠΎΠ³ΠΎ поля Ρ€Π΅Π°Π»ΠΈΠ·Π°Ρ†ΠΈΠΈ Π²Ρ‹Ρ€Π°ΠΆΠ΅Π½Π½ΠΎΠΉ потрСбности Π² ΠΎΠ±Ρ‰Π΅Π½ΠΈΠΈ ΠΈ Π±ΠΎΠ»Π΅Π΅ агрСссивная Π·Π°Ρ‰ΠΈΡ‚Π° своСго сСтСвого пространства ΠΎΡ‚ Π²ΠΌΠ΅ΡˆΠ°Ρ‚Π΅Π»ΡŒΡΡ‚Π²Π° Ρ€ΠΎΠ΄ΠΈΡ‚Π΅Π»Π΅ΠΉ. ΠžΠ±ΡΡƒΠΆΠ΄Π΅Π½ΠΈΠ΅ Ρ€Π΅Π·ΡƒΠ»ΡŒΡ‚Π°Ρ‚ΠΎΠ². ΠŸΡ€Π΅Π΄ΡΡ‚Π°Π²Π»Π΅Π½Π½Ρ‹Π΅ Π΄Π°Π½Π½Ρ‹Π΅ ΠΎΡ‚ΠΊΡ€Ρ‹Π²Π°ΡŽΡ‚ ряд пСрспСктивных Π½Π°ΠΏΡ€Π°Π²Π»Π΅Π½ΠΈΠΉ исслСдования Π² ΠΏΡ€Π΅Π΄ΠΌΠ΅Ρ‚Π½ΠΎΠΉ области сСтСвой социализации ΠΎΠ±ΡƒΡ‡Π°ΡŽΡ‰ΠΈΡ…ΡΡ с Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΠ΅ΠΌ развития: 1) ΠΏΠ΅Ρ€Π²ΠΈΡ‡Π½Ρ‹ΠΉ скрининг Π² Ρ€Π°ΠΌΠΊΠ°Ρ… Π²Π΅Π΄ΡƒΡ‰Π΅Π³ΠΎ Π½Π°Ρ€ΡƒΡˆΠ΅Π½ΠΈΡ ΠΏΠΎ ΡΡ€Π°Π²Π½Π΅Π½ΠΈΡŽ с Π½ΠΎΡ€ΠΌΠ°Ρ‚ΠΈΠ²Π½ΠΎ Ρ€Π°Π·Π²ΠΈΠ²Π°ΡŽΡ‰ΠΈΠΌΠΈΡΡ свСрстниками; 2) ΡƒΠ³Π»ΡƒΠ±Π»Π΅Π½Π½ΠΎΠ΅ исслСдованиС ΠΏΠΎ возрастным Π΄ΠΈΠ°ΠΏΠ°Π·ΠΎΠ½Π°ΠΌ Π² Ρ€Π°ΠΌΠΊΠ°Ρ… ΠΎΠ΄Π½ΠΎΠΉ Π½ΠΎΠ·ΠΎΠ»ΠΎΠ³ΠΈΠΈ ΠΈ выявлСниС возрастных Ρ€Π°Π·Π»ΠΈΡ‡ΠΈΠΉ Π²Π½ΡƒΡ‚Ρ€ΠΈ ΠΎΠ΄Π½ΠΎΠΉ нозологичСской Π³Ρ€ΡƒΠΏΠΏΡ‹; 3) Π΄ΠΈΡ„Ρ„Π΅Ρ€Π΅Π½Ρ†ΠΈΡ€ΠΎΠ²Π°Π½Π½ΠΎΠ΅ исслСдованиС ΠΏΠΎ ΡΡ€Π°Π²Π½Π΅Π½ΠΈΡŽ Ρ€Π°Π·Π½Ρ‹Ρ… нозологичСских ΠΊΠ°Ρ‚Π΅Π³ΠΎΡ€ΠΈΠΉ ΠΈ Π²Ρ‹ΡΠ²Π»Π΅Π½ΠΈΡŽ ΠΌΠ΅ΠΆΠ³Ρ€ΡƒΠΏΠΏΠΎΠ²Ρ‹Ρ… Ρ€Π°Π·Π»ΠΈΡ‡ΠΈΠΉ

    Geochemical composition of sediment samples from Krasnov field in the Mid Atlantic Ridge

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    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 2) Grain size composition of bottom sediments from Core SO201-2-101, Shirshov Ridge, Bering Sea

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    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
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