69 research outputs found
Vs sustainable development: scenarios for the future
Issues of sustainable development began to concern mankind starting from the 20th century, when mass industrialization and the depletion of natural resource potential contributed to the formulation of environmental issues at one of the leading places in scientific discourse. However, what if the goals of sustainable development would not be achieved to 2030? What other way we can identify for humanity to survive? So, the study is about the problems of studying the understanding of the term βsustainable developmentβ, considering the evolution of the formation of the concept of sustainable development and analyzing the modern goals of sustainable development for attainability. From an analysis of domestic and foreign experience, possible scenarios of the development of mankind are identified (such as 1. Creating an environmental framework, 2. Implementation of sustainable nature management practices in the conditions of natural and man-made objects, 3. Implementation of βgeoengineering projectsβ, 4. Construction of autonomous ecosystems, 5. Space exploration in search of a new planet for life, provided that the goals of sustainable development would not be achieved. It has been established that today probability of achieving all the sustainable development goals by 2030 is too small, and the indicated scenarios require, firstly, the development of science and technology, and secondly, a competent assessment of the value of nature and solving the issue of specifying property rights for natural goods
ΠΠ΅ΡΠΈΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½Π°Ρ Π΄ΠΈΠ½Π°ΠΌΠΈΠΊΠ° ΡΡΠ²ΠΎΡΠΎΡΠΎΡΠ½ΠΎΠΉ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ Π³Π»ΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠΈΠ±ΡΠΈΠ»Π»ΡΡΠ½ΠΎΠ³ΠΎ ΠΊΠΈΡΠ»ΠΎΠ³ΠΎ ΠΏΡΠΎΡΠ΅ΠΈΠ½Π° ΠΈ Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½Π½ΠΎΠ΅ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΠΎΠ΅ Π²ΠΎΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅: ΡΠΊΡΠΏΠ΅ΡΠΈΠΌΠ΅Π½ΡΠ°Π»ΡΠ½ΠΎΠ΅ ΠΎΠ±ΡΠ΅ΡΠ²Π°ΡΠΈΠΎΠ½Π½ΠΎΠ΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅
A number of studies have found an association between the increased concentration of glial fibrillar acid protein (GFAP) in blood serum in patients with various types of brain damage (ischemic stroke, traumatic brain injury, neurodegenerative and neuro-oncological diseases), as well as with a rapid decline in cognitive functions in elderly people with initially normal cognitive abilities.The objective: to identify the relationship between delayed cognitive recovery and changes in serum GFAP concentration in the perioperative period in patients operated for various oncological diseases.Subjects and Methods. The study included 30 patients who underwent surgical treatment for prostate cancer, colorectal cancer and pancreatic cancer under combined general anesthesia.The inclusion criteria were the expected duration of the operation over 300 minutes and the age over 60 years. GFAP was determined in plasma by enzyme immunoassay before anesthesia, the next day after surgery and on the 4thβ5th day. Neuropsychological testing was performed before surgery and on the 4thβ5th postoperative day. Delayed cognitive recovery was defined as a decrease in the composite z-score of more than one standard deviation (SD) compared to the preoperative assessment.Correlation analysis was performed between changes in the composite z-score (in absolute values) and the difference in GFAP concentration between the outcome and the first postoperative day, the outcome and the 4thβ5th postoperative day and the first and 4thβ5th postoperative days.Results. In five cases (16.6%), a decrease in the composite z-score > 1 SD was revealed indicating a delayed cognitive recovery. In the remaining 25 (83.4%) patients, changes in the composite z-score were less than one standard deviation. The median concentration of GFAP in patients with delayed cognitive recovery was 0.13 [0.1; 0.14] before surgery, 0.12 [0.09; 0.14] the day after surgery and 0.16 [0.05; 0.19] on the 4thβ5th day after surgery. In patients without cognitive impairment, the concentration of GFAP was 0.15 [0.125; 0.184] before surgery, 0.15 [0.121; 0.163] 24 hours after surgery and 0.13 [0.079; 0.151] on the 4thβ5th day after surgery. The correlation values between changes in the composite z-score and the difference in GFAP concentrations were: between the outcome and the first postoperative day β rs = 0.107, p = 0.37, outcome and the 4thβ5th postoperative day β rs = 0.134, p = 0.37, the first and 4thβ5th postoperative days β rs = 0.21, p = 0.37.Discussion. There was no statistically significant difference in GFAP levels between patients with delayed cognitive recovery and patients without cognitive impairment. There was also no correlation between the difference in GFAP concentrations in plasma before surgery and 24 hours after, before surgery and on the 4thβ5th day of the postoperative period and the composite z-score.Conclusions. The use of GFAP to predict cognitive decline associated with surgical treatment of colorectal cancer, prostate cancer and pancreatic cancer under general anesthesia is not yet possible.Π ΡΡΠ΄Π΅ ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠΉ Π±ΡΠ»Π° ΠΎΠ±Π½Π°ΡΡΠΆΠ΅Π½Π° ΡΠ²ΡΠ·Ρ ΠΌΠ΅ΠΆΠ΄Ρ ΠΏΠΎΠ²ΡΡΠ΅Π½Π½ΠΎΠΉ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠ΅ΠΉ Π³Π»ΠΈΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠΈΠ±ΡΠΈΠ»Π»ΡΡΠ½ΠΎΠ³ΠΎ ΠΊΠΈΡΠ»ΠΎΠ³ΠΎ ΠΏΡΠΎΡΠ΅ΠΈΠ½Π° (GFAP) Π² ΡΡΠ²ΠΎΡΠΎΡΠΊΠ΅ ΠΊΡΠΎΠ²ΠΈ Ρ ΠΏΠ°ΡΠΈΠ΅Π½ΡΠΎΠ² Ρ ΡΠ°Π·Π»ΠΈΡΠ½ΡΠΌΠΈ Π²Π°ΡΠΈΠ°Π½ΡΠ°ΠΌΠΈ ΠΏΠΎΡΠ°ΠΆΠ΅Π½ΠΈΡ Π³ΠΎΠ»ΠΎΠ²Π½ΠΎΠ³ΠΎ ΠΌΠΎΠ·Π³Π° (ΠΈΡΠ΅ΠΌΠΈΡΠ΅ΡΠΊΠΈΠΌ ΠΈΠ½ΡΡΠ»ΡΡΠΎΠΌ, ΡΡΠ°Π²ΠΌΠ°ΡΠΈΡΠ΅ΡΠΊΠΈΠΌ ΠΏΠΎΠ²ΡΠ΅ΠΆΠ΄Π΅Π½ΠΈΠ΅ΠΌ Π³ΠΎΠ»ΠΎΠ²Π½ΠΎΠ³ΠΎ ΠΌΠΎΠ·Π³Π°, Π½Π΅ΠΉΡΠΎΠ΄Π΅Π³Π΅Π½Π΅ΡΠ°ΡΠΈΠ²Π½ΡΠΌΠΈ ΠΈ Π½Π΅ΠΉΡΠΎΠΎΠ½ΠΊΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΠΌΠΈ Π·Π°Π±ΠΎΠ»Π΅Π²Π°Π½ΠΈΡΠΌΠΈ), Π° ΡΠ°ΠΊΠΆΠ΅ Ρ Π±ΡΡΡΡΡΠΌ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΠ΅ΠΌ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΡ
ΡΡΠ½ΠΊΡΠΈΠΉ Ρ ΠΏΠΎΠΆΠΈΠ»ΡΡ
Π»ΡΠ΄Π΅ΠΉ c ΠΈΡΡ
ΠΎΠ΄Π½ΠΎ Π½ΠΎΡΠΌΠ°Π»ΡΠ½ΡΠΌΠΈ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΠΌΠΈ ΡΠΏΠΎΡΠΎΠ±Π½ΠΎΡΡΡΠΌΠΈ.Π¦Π΅Π»Ρ: Π²ΡΡΠ²ΠΈΡΡ Π²Π·Π°ΠΈΠΌΠΎΡΠ²ΡΠ·Ρ ΠΌΠ΅ΠΆΠ΄Ρ Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½Π½ΡΠΌ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΠΌ Π²ΠΎΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅ΠΌ ΠΈ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΠ΅ΠΌ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ GFAP ΡΡΠ²ΠΎΡΠΎΡΠΊΠΈ ΠΊΡΠΎΠ²ΠΈ Π² ΠΏΠ΅ΡΠΈΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΌ ΠΏΠ΅ΡΠΈΠΎΠ΄Π΅ Ρ ΠΏΠ°ΡΠΈΠ΅Π½ΡΠΎΠ², ΠΎΠΏΠ΅ΡΠΈΡΠΎΠ²Π°Π½Π½ΡΡ
ΠΏΠΎ ΠΏΠΎΠ²ΠΎΠ΄Ρ ΡΠ°Π·Π»ΠΈΡΠ½ΡΡ
ΠΎΠ½ΠΊΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΈΡ
Π·Π°Π±ΠΎΠ»Π΅Π²Π°Π½ΠΈΠΉ.ΠΠ°ΡΠ΅ΡΠΈΠ°Π» ΠΈ ΠΌΠ΅ΡΠΎΠ΄Ρ. Π ΠΈΡΡΠ»Π΅Π΄ΠΎΠ²Π°Π½ΠΈΠ΅ Π²ΠΊΠ»ΡΡΠ΅Π½ΠΎ 30 ΠΏΠ°ΡΠΈΠ΅Π½ΡΠΎΠ², ΠΏΠ΅ΡΠ΅Π½Π΅ΡΡΠΈΡ
ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠ²Π½ΠΎΠ΅ Π»Π΅ΡΠ΅Π½ΠΈΠ΅ ΠΏΠΎ ΠΏΠΎΠ²ΠΎΠ΄Ρ ΡΠ°ΠΊΠ° ΠΏΡΠ΅Π΄ΡΡΠ°ΡΠ΅Π»ΡΠ½ΠΎΠΉ ΠΆΠ΅Π»Π΅Π·Ρ, ΠΊΠΎΠ»ΠΎΡΠ΅ΠΊΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°ΠΊΠ° ΠΈ ΡΠ°ΠΊΠ° ΠΏΠΎΠ΄ΠΆΠ΅Π»ΡΠ΄ΠΎΡΠ½ΠΎΠΉ ΠΆΠ΅Π»Π΅Π·Ρ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ
ΠΊΠΎΠΌΠ±ΠΈΠ½ΠΈΡΠΎΠ²Π°Π½Π½ΠΎΠΉ ΠΎΠ±ΡΠ΅ΠΉ Π°Π½Π΅ΡΡΠ΅Π·ΠΈΠΈ. ΠΡΠΈΡΠ΅ΡΠΈΡΠΌΠΈ Π²ΠΊΠ»ΡΡΠ΅Π½ΠΈΡ Π±ΡΠ»ΠΈ ΠΎΠΆΠΈΠ΄Π°Π΅ΠΌΠ°Ρ ΠΏΡΠΎΠ΄ΠΎΠ»ΠΆΠΈΡΠ΅Π»ΡΠ½ΠΎΡΡΡ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ Π±ΠΎΠ»Π΅Π΅ 300 ΠΌΠΈΠ½ ΠΈ Π²ΠΎΠ·ΡΠ°ΡΡ Π±ΠΎΠ»Π΅Π΅ 60 Π»Π΅Ρ. GFAP ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ»ΠΈ Π² ΠΏΠ»Π°Π·ΠΌΠ΅ ΠΈΠΌΠΌΡΠ½ΠΎΡΠ΅ΡΠΌΠ΅Π½ΡΠ½ΡΠΌ Π°Π½Π°Π»ΠΈΠ·ΠΎΠΌ Π΄ΠΎ Π²Π²Π΅Π΄Π΅Π½ΠΈΡ Π°Π½Π΅ΡΡΠ΅Π·ΠΈΠΈ, Π½Π° ΡΠ»Π΅Π΄ΡΡΡΠΈΠΉ Π΄Π΅Π½Ρ ΠΏΠΎΡΠ»Π΅ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ ΠΈ Π½Π° 4β5-Π΅ ΡΡΡ. ΠΠ΅ΠΉΡΠΎΠΏΡΠΈΡ
ΠΎΠ»ΠΎΠ³ΠΈΡΠ΅ΡΠΊΠΎΠ΅ ΡΠ΅ΡΡΠΈΡΠΎΠ²Π°Π½ΠΈΠ΅ Π²ΡΠΏΠΎΠ»Π½ΡΠ»ΠΈ Π΄ΠΎ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ ΠΈ Π½Π° 4β5-ΠΉ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΉ Π΄Π΅Π½Ρ. ΠΠ°ΠΌΠ΅Π΄Π»Π΅Π½Π½ΠΎΠ΅ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΠΎΠ΅ Π²ΠΎΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅ ΠΎΠΏΡΠ΅Π΄Π΅Π»ΡΠ»ΠΈ ΠΊΠ°ΠΊ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΠ΅ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ½ΠΎΠ³ΠΎ z-Π±Π°Π»Π»Π° Π±ΠΎΠ»Π΅Π΅ ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΡΡΠ°Π½Π΄Π°ΡΡΠ½ΠΎΠ³ΠΎ (SD) ΠΎΡΠΊΠ»ΠΎΠ½Π΅Π½ΠΈΡ ΠΏΠΎ ΡΡΠ°Π²Π½Π΅Π½ΠΈΡ Ρ ΠΏΡΠ΅Π΄ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠΉ ΠΎΡΠ΅Π½ΠΊΠΎΠΉ. ΠΠΎΡΡΠ΅Π»ΡΡΠΈΠΎΠ½Π½ΡΠΉ Π°Π½Π°Π»ΠΈΠ· ΠΏΡΠΎΠ²ΠΎΠ΄ΠΈΠ»ΠΈ ΠΌΠ΅ΠΆΠ΄Ρ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡΠΌΠΈ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ½ΠΎΠ³ΠΎ z-Π±Π°Π»Π»Π° (Π² Π°Π±ΡΠΎΠ»ΡΡΠ½ΡΡ
Π·Π½Π°ΡΠ΅Π½ΠΈΡΡ
) ΠΈ ΡΠ°Π·Π½ΠΈΡΠ΅ΠΉ Π² ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ GFAP ΠΌΠ΅ΠΆΠ΄Ρ ΠΈΡΡ
ΠΎΠ΄ΠΎΠΌ ΠΈ ΠΏΠ΅ΡΠ²ΡΠΌ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌ Π΄Π½Π΅ΠΌ, ΠΈΡΡ
ΠΎΠ΄ΠΎΠΌ ΠΈ 4β5-ΠΌ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌ Π΄Π½Π΅ΠΌ ΠΈ ΠΏΠ΅ΡΠ²ΡΠΌ ΠΈ 4β5-ΠΌ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌΠΈ Π΄Π½ΡΠΌΠΈ.Π Π΅Π·ΡΠ»ΡΡΠ°ΡΡ. Π 5 (16,6%) ΡΠ»ΡΡΠ°ΡΡ
Π²ΡΡΠ²Π»Π΅Π½ΠΎ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΠ΅ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ½ΠΎΠ³ΠΎ z-Π±Π°Π»Π»Π° > 1 SD, ΡΡΠΎ ΡΠΊΠ°Π·ΡΠ²Π°Π»ΠΎ Π½Π° Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½Π½ΠΎΠ΅ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΠΎΠ΅ Π²ΠΎΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅. Π£ ΠΎΡΡΠ°Π»ΡΠ½ΡΡ
25 (83,4%) ΠΏΠ°ΡΠΈΠ΅Π½ΡΠΎΠ² ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ½ΠΎΠ³ΠΎ z-Π±Π°Π»Π»Π° Π±ΡΠ»ΠΈ ΠΌΠ΅Π½Π΅Π΅ ΠΎΠ΄Π½ΠΎΠ³ΠΎ ΡΡΠ°Π½Π΄Π°ΡΡΠ½ΠΎΠ³ΠΎ ΠΎΡΠΊΠ»ΠΎΠ½Π΅Π½ΠΈΡ. ΠΠ΅Π΄ΠΈΠ°Π½Π° ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΈ GFAP Ρ ΠΏΠ°ΡΠΈΠ΅Π½ΡΠΎΠ² Ρ Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½Π½ΡΠΌ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΠΌ Π²ΠΎΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅ΠΌ ΡΠΎΡΡΠ°Π²ΠΈΠ»Π° 0,13 [0,1; 0,14] Π΄ΠΎ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ, 0,12 [0,09; 0,14] Π½Π° ΡΠ»Π΅Π΄ΡΡΡΠΈΠΉ Π΄Π΅Π½Ρ ΠΏΠΎΡΠ»Π΅ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ ΠΈ 0,16 [0,05; 0,19] Π½Π° 4β5-Π΅ ΡΡΡ ΠΏΠΎΡΠ»Π΅ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ. Π£ ΠΏΠ°ΡΠΈΠ΅Π½ΡΠΎΠ² Π±Π΅Π· ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΡ
Π½Π°ΡΡΡΠ΅Π½ΠΈΠΉ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΡ GFAP ΡΠΎΡΡΠ°Π²ΠΈΠ»Π° 0,15 [0,125; 0,184] Π΄ΠΎ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ, 0,15 [0,121; 0,163] ΡΠ΅ΡΠ΅Π· 24 ΠΏΠΎΡΠ»Π΅ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ ΠΈ 0,13 [0,079; 0,151] Π½Π° 4β5-Π΅ ΡΡΡ ΠΏΠΎΡΠ»Π΅ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ. ΠΠ½Π°ΡΠ΅Π½ΠΈΡ ΠΊΠΎΡΡΠ΅Π»ΡΡΠΈΠΈ ΠΌΠ΅ΠΆΠ΄Ρ ΠΈΠ·ΠΌΠ΅Π½Π΅Π½ΠΈΡΠΌΠΈ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ½ΠΎΠ³ΠΎ z-Π±Π°Π»Π»Π° ΠΈ ΡΠ°Π·Π½ΠΈΡΠ΅ΠΉ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΉ GFAP ΡΠΎΡΡΠ°Π²ΠΈΠ»ΠΈ: ΠΌΠ΅ΠΆΠ΄Ρ ΠΈΡΡ
ΠΎΠ΄ΠΎΠΌ ΠΈ ΠΏΠ΅ΡΠ²ΡΠΌ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌ Π΄Π½Π΅ΠΌ β rs = 0,107, p = 0,37, ΠΈΡΡ
ΠΎΠ΄ΠΎΠΌ ΠΈ 4β5-ΠΌ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌ Π΄Π½Π΅ΠΌ β rs = 0,134, p = 0,37, ΠΏΠ΅ΡΠ²ΡΠΌ ΠΈ 4β5-ΠΌ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΡΠΌΠΈ Π΄Π½ΡΠΌΠΈ β rs = 0,21, p = 0,37.ΠΠ±ΡΡΠΆΠ΄Π΅Π½ΠΈΠ΅. ΠΠ΅ Π²ΡΡΠ²Π»Π΅Π½ΠΎ ΡΡΠ°ΡΠΈΡΡΠΈΡΠ΅ΡΠΊΠΈ Π·Π½Π°ΡΠΈΠΌΠΎΠΉ ΡΠ°Π·Π½ΠΈΡΡ Π² ΡΡΠΎΠ²Π½ΡΡ
GFAP ΠΌΠ΅ΠΆΠ΄Ρ ΠΏΠ°ΡΠΈΠ΅Π½ΡΠ°ΠΌΠΈ Ρ Π·Π°ΠΌΠ΅Π΄Π»Π΅Π½Π½ΡΠΌ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΠΌ Π²ΠΎΡΡΡΠ°Π½ΠΎΠ²Π»Π΅Π½ΠΈΠ΅ΠΌ ΠΈ ΠΏΠ°ΡΠΈΠ΅Π½ΡΠ°ΠΌΠΈ Π±Π΅Π· ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΡ
Π½Π°ΡΡΡΠ΅Π½ΠΈΠΉ. Π’Π°ΠΊΠΆΠ΅ Π½Π΅ ΠΎΠ±Π½Π°ΡΡΠΆΠ΅Π½ΠΎ ΠΊΠΎΡΡΠ΅Π»ΡΡΠΈΠΈ ΠΌΠ΅ΠΆΠ΄Ρ ΡΠ°Π·Π½ΠΈΡΠ΅ΠΉ ΠΊΠΎΠ½ΡΠ΅Π½ΡΡΠ°ΡΠΈΠΉ GFAP Π² ΠΏΠ»Π°Π·ΠΌΠ΅ Π΄ΠΎ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ ΠΈ ΡΠ΅ΡΠ΅Π· 24 Ρ ΠΏΠΎΡΠ»Π΅, Π΄ΠΎ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΈ ΠΈ Π½Π° 4β5-Π΅ ΡΡΡ ΠΏΠΎΡΠ»Π΅ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠΎΠ½Π½ΠΎΠ³ΠΎ ΠΏΠ΅ΡΠΈΠΎΠ΄Π° ΠΈ ΠΊΠΎΠΌΠΏΠΎΠ·ΠΈΡΠ½ΡΠΌ z-ΡΡΠ΅ΡΠΎΠΌ.ΠΡΠ²ΠΎΠ΄Ρ. ΠΡΠΏΠΎΠ»ΡΠ·ΠΎΠ²Π°Π½ΠΈΠ΅ GFAP Π΄Π»Ρ ΠΏΡΠΎΠ³Π½ΠΎΠ·ΠΈΡΠΎΠ²Π°Π½ΠΈΡ ΡΠ½ΠΈΠΆΠ΅Π½ΠΈΡ ΠΊΠΎΠ³Π½ΠΈΡΠΈΠ²Π½ΡΡ
ΡΡΠ½ΠΊΡΠΈΠΉ, ΡΠ²ΡΠ·Π°Π½Π½ΠΎΠ³ΠΎ Ρ ΠΎΠΏΠ΅ΡΠ°ΡΠΈΠ²Π½ΡΠΌ Π»Π΅ΡΠ΅Π½ΠΈΠ΅ΠΌ ΠΊΠΎΠ»ΠΎΡΠ΅ΠΊΡΠ°Π»ΡΠ½ΠΎΠ³ΠΎ ΡΠ°ΠΊΠ°, ΡΠ°ΠΊΠ° ΠΏΡΠ΅Π΄ΡΡΠ°ΡΠ΅Π»ΡΠ½ΠΎΠΉ ΠΆΠ΅Π»Π΅Π·Ρ ΠΈ ΡΠ°ΠΊΠ° ΠΏΠΎΠ΄ΠΆΠ΅Π»ΡΠ΄ΠΎΡΠ½ΠΎΠΉ ΠΆΠ΅Π»Π΅Π·Ρ Π² ΡΡΠ»ΠΎΠ²ΠΈΡΡ
ΠΎΠ±ΡΠ΅ΠΉ Π°Π½Π΅ΡΡΠ΅Π·ΠΈΠΈ, ΠΏΠΎΠΊΠ° Π½Π΅ ΠΏΡΠ΅Π΄ΡΡΠ°Π²Π»ΡΠ΅ΡΡΡ Π²ΠΎΠ·ΠΌΠΎΠΆΠ½ΡΠΌ
Magmatism and metallogeny of the transverse structures of the North Urals
The article contains summarized results of the study of Late Paleozoic-Mesozoic magmatic complexes of the North Urals; there are three age levels of the plume-type intraplate magmatism: Permian-Triassic alkaline-acid (Torasoveysky, Levdievsky, Pon'insky complexes), Triassic-Jurassic trappean (Musyursky, Yatyinsky complexes), and Jurassic-Cretaceous alkaline-basite (Yalyayakhinsky, Marunsky, and Osoveisky complexes). The author shows their confinement to transverse disjunctive structures discordant to the general submeridional structure of the folded system. For the first time the author provides results of studying the isotope age of magmatites and describes their geochemical and metallogenic specializations. Thus, the Late Permian-Early Triassic stage is characterized by the manifestation of alkaline-acidic magmatism and associated mineralization of rare metal-albitite (Ta-Nb-Th-U) with gold and platinoids (Taykeusky, Longotsky deposits), quartz-fluorite and carbonatefluorite (Amderminsky deposit), and gold-copper-molybdenum-porphyry (Levdievsky manifestation) formations. The ore objects of the Triassic-Jurassic stage due to the magmatism of trappean type are represented by small objects of gold-porphyry (Petropavlovsky deposit) formation, as well as by deposits of crystal, Iceland spar
(Khasavarka, Pelin-gichey deposit) and agates (Harbeysky-Yagodny manifestation). The productivity of alkaline-basite-ultrabasite magmatism formations, attributed to manifestations of mantle and crust-mantle types, is of interest primarily for their probable diamond content (Nemziyakhinsky complex). In addition, alkalinebasite magmatism is promising for the manifestations of mercury, tungsten-mercury (Malotal'beysky, Sfinks manifestations), gold-quartz-sulfide with platinoids (Penzengoyakhinsky manifestation and others) and quartz-antimonite (Verkhnekhanmeisky, Slavkino ore manifestations) formations. The author makes a conclusion on the connection between the magmatism of the Urals and the processes that occurred in the foundation of the West Siberian plate
METHODOLOGICAL TOOLS TO ENSURE THE COMPLETENESS OF THE NON-RENEWABLE RESOURCES USE IN AN ENVIRONMENTALLY SUSTAINABLE SUBSOIL USE
The relevance of the study. One of the main conditions for environmentally sustainable subsoil use is to minimize the depletion of mineral resources. It involves the most efficient and complete development of reserves of exploited mineral deposits. At the same time, the loss and dilution rates in mining remain high. On average, in the mining industry, the amount of losses is determined in 10β50 %. Positive changes in solving this problem are very small due to the lack of the effective guidelines aimed at the completeness of the study of subsoil resources. The purpose of the study is to develop methodological tools to ensure the full use of non β renewable resources.
The results obtained in the course of research are as follows: the tendency of systematic overstatement of reserves is revealed. This requires clarification of the coefficients of transfer of reserves to higher categories. The necessity for increasing the reliability of geological information both in geological study of subsoil and in operational exploration is proved. The expediency of the advanced geological study of mineral resources in the process of field development is substantiated. The method of its efficiency evaluation is specified. This method considers the effect due to the increase in the completeness of the use of mineral resources. The effect formed by increasing the level of the mining operations safety and the effect of increasing the level of investment attractiveness of the object of subsoil use are also considered.
Applying the results. The developed methodological tools aimed at minimizing the depletion of non-renewable natural resources, contains proposals for detailing the amount of mineral resources and improving the reliability of geological information. These tools will allow subsoil users to achieve an increase in the completeness of subsoil use, providing an ecological and economic effect
Economic evaluation of mineral resources potential of solid minerals with a view to the national resource mode
The article presents the results of the revaluation of the mineral resource potential objects of the Northern and Subpolar Ural Khanty-Mansiysk Autonomous Okrug β Ugra with the national resource of the regime. The aim of presented research is the development of theory and methodology of complex study and evaluation of mineral resources in the Northern, polar and Arctic territories in various stages of geological survey and development of uncertainty and risks. Author's method of accounting the national resource regime for the economic evaluation of the prospects of the mineral and raw materials potential is presented. In the course of the research were used, income, comparative approaches to the economic valuation and analyzed method abstract generic values of the (potential value), applied theoretical apparatus of the institutional theory. As a result of research, the following conclusions were made: underreporting of existing methods of economic evaluation of mineral-raw potential environmental and including institutional risks leads to incorrect results; a widely used procedure of assessment of country risks, based on applications of credit ratings and contain high share of subjectivity; the evaluation of a national resource of the regime showed high institutional risks in comparison with other countries, actively exploiting mineral resources, which indicates the need for a substantial change of the state commodity policies with a view to reducing institutional risks; the conducted economic revaluation showed the usefulness of involving in economic circulation of the facilities of mineral-raw potential of the KhMAO-Ugra only in the case of system development of the region; a revalued mineral and raw material potential is able to meet only local requirements for raw materials part of the industrial potential of the Ural region and the adjacent areas and only under the condition of construction of new of appropriate transport and energy infrastructure
THE PRODUCTION OF THE MINERAL BASE IN THE URAL PART OF HANTI-MANSIYSK IN THE AUTONOMOUS REGION OF YUGRA
The necessity of reproduction process intensification Urals Mountains is proved in the clause. There are presented maden mineral resources potential value estimation of Hunty-Mansiysk autonomous region β Ugra`s mountain part and the author's methodical approach to reproduction process regulation of the mineral resources base, realized in conditions HMAO β Ugra`s Ural part
Modern Challenges for Oil and Gas Education
Today, in education in general and in higher education in particular, there is no more pressing problem than the organization of the educational process in the context of a pandemic that all universities in the world are facing. Also, there are no universal recipes for how to organize educational and scientific processes in a university without losing quality. The authors share their experience on how to restructure the work of teachers with students in the context of distance communication, organize the work of an educational portal, conduct training sessions, internships, state final certification, create motivational remuneration for the teaching staff. The article concludes that the challenges of the pandemic to higher education made it possible to find algorithms for interaction between students and teachers in the online environment, showed the need to improve the methodological qualifications of teachers, motivational and psychological support for participants in the educational process, accelerate the development of digital resources
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