Father - Panin V.M., engineer, mind. in 1957; mother Panina A.U., office worker, d. in 1951. In 1951 he graduated from the 7th grade of secondary school and entered the Moscow Automotive Technical School, from which he graduated in 1955, having received the qualification of a technician-technologist. In 1959, after serving in the Soviet Army, he entered the evening department of the Philosophy Faculty of Moscow State University, combining his studies with work at the ZIL plant. After graduating from the faculty, he entered the graduate school of the Faculty of Philosophy. After graduating from graduate school in 1968, he was left to work at the faculty as an assistant. In 1969 he defended his Ph.D. thesis on the topic "The concept of natural science law." During his work at the faculty, he passed scientific internships twice: in the UK (University of London, 1974-75) and in the USA (State University of New York, 1984).

The greatest influence on the formation of his pedagogical and scientific views was provided by lectures and scientific contacts with leading professors of the Philosophical Faculty of Moscow State University. First of all, they include Prof. Asmus V.F., prof. Melville Yu.K., prof. Sokolov V.V., prof. Kuptsov V.I., prof. Shvyrev V.S., prof. Melyukhin S.T. and others. On the formation of scientific views Panina A.V. acquaintance with the works of the classics of the world philosophy of science had a significant impact, with many of whom he managed to establish personal contact during scientific internships. He was advised by such classics of the world philosophy of science as K. Popper, I. Lakatos, T. Kuhn, K. Gempel, M. Hessy, E. Nagel, P. Feyerabend.

Since 1968 he worked as an assistant, since 1972 as a senior lecturer, since 1975 as an associate professor at the Department of Dialectical Materialism of the Faculty of Philosophy. Currently, he works as a professor at the Department of Philosophy and Methodology of Science, Faculty of Philosophy, Moscow State University. From 1988 to 1998 he was twice elected to the post of dean of the Faculty of Philosophy of Moscow State University, at the same time heading the UMO for Philosophical Sciences. During his time in this position, under his leadership, a lot of work was done to reform philosophical education both at the faculty and through the UMO in the higher education system. During this time, the departmental structure of the faculty was radically revised, new departments and departments were opened, the staff of the faculty was updated, the curricula and programs of the main lecture courses were revised. From 1992 to 2002 headed the Department of Philosophy and Methodology of Science, in the opening of which he took an active part.

The main pedagogical and scientific interests of Panin A.V. lie in the field of ontology, theory of knowledge and philosophy and methodology of science. Together with prof. P.V. Alekseev published a series of textbooks and manuals on ontology and theory of knowledge. During his work at the faculty, he read courses of lectures on ontology and epistemology, philosophical problems of natural science, introduction to the specialty. From 1992 to present. they annually read the main cathedral course of lectures "Philosophy and Methodology of Science". In addition, he prepared and read a number of special courses on the same subject. He prepared 12 candidates of sciences.

Compositions:

• Philosophy and Science. M., 1973. (with V. I. Kuptsov, S. A. Lebedev and V. G. Borzenkov);
• Dialectical materialism and postpositivism. M. 1981;
• Criticism as a trend in Western philosophy of science // Questions of Philosophy, No. 5, 1977;
• Is the dichotomy of theoretical and empirical exhaustive in the methodology of scientific knowledge // "Scientific reports of higher education", ser. Philosophical Sciences, No. 2, 1986;
• Theory of knowledge and dialectics. / Uch. allowance. M. 1991;
• Philosophy (Textbook. Co-authored with Alekseev P.V.). M. 1996;
• Philosophy (Textbook. Co-authored with Alekseev P.V.). Ed. 3rd, revised. and additional Moscow State University, 2003 (series "Classical university textbook").

Candidate of Chemical Sciences, Assistant of the Department of Inorganic Chemistry

Candidate of Chemical Sciences, Assistant of the Department of Inorganic Chemistry,

e-mail: [email protected] website

Education

• Diploma "New complex oxides and phosphates of vanadium" 2003
• Dissertation "Synthesis and crystal structure of complex oxides of alkali and platinum metals" 2007

Labor activity

• 1998-2003 - student of the Faculty of Chemistry, Moscow State University
• 2003-2006 - PhD student, Faculty of Chemistry, Moscow State University
• 2007 - 2008 - Junior Researcher, Faculty of Chemistry, Moscow State University
• 2008 - present - assistant of the Faculty of Chemistry, Moscow State University

Awards

• 2002 - Prize named after L.M. Kovby "for the best student work in the field of radiography"
• 2008 - Encouragement Prize named after Yu.T. Struchkov "For the best scientific research in the field of crystal chemistry"
• 2011 - scholarship of the Academic Council of Moscow State University for young teachers

Administrative duties

• Chairman of the commission for term papers of the Department of Inorganic Chemistry - since 2008.
• Head of the team of teachers of the workshop on inorganic chemistry for biological classes of school No. 171 - since 2012.
• Responsible for room No. 345 at the Faculty of Chemistry - since 2011.
• Member of the training program for the personnel Olympic reserve of the Republic of Azerbaijan under the patronage of the President of the Republic of Azerbaijan - since 2011.
• Member of the Presidium of the Joint Trade Union Committee (OPK MGU), head of the food quality control group - since 2008.

Areas of scientific interest

• Crystal Chemistry of Oxide Compounds of Platinum Metals
• Framework structures with anion groups as promising cathode materials for lithium-ion batteries

Pedagogical activity

• Course "Inorganic Chemistry" (seminars, workshop) for students of the general stream of the 1st year of the Faculty of Chemistry, Moscow State University - since 2007
• Course "Inorganic Chemistry" (seminars, workshop) for 1st year undergraduate students of the Baku branch of Moscow State University - since 2009
• Course "Inorganic Chemistry" (workshop) for schoolchildren of biological classes of school No. 171 - since 2012
• Course "General and Inorganic Chemistry" (seminars) for students of the Preparatory Department of Moscow State University - since 2012
• The course "Aspects of modern inorganic chemistry for schoolchildren participating in high-level chemistry olympiads" (lectures and seminars) - since 2012. I am the author of this course, testing was carried out at the "School of Olympic Resources" of the Republic of Azerbaijan.

The main directions of educational and methodological work

• Adaptation of the system of teaching inorganic chemistry, taking into account the contingent of students (branches) and the rotational method of work.
• Inorganic chemistry within the system of high-level chemistry olympiads for schoolchildren.

Coursework in inorganic chemistry (1st year student of the Faculty of Chemistry, Moscow State University) - guidance and co-management

• Polyanina Daria - 2007
• Fetisov Evgeny - 2008
• Petukhova Anastasia - 2008
• Gubanova Svetlana - 2009
• Belova Ekaterina - 2010
• Stekolshchikova Elena - 2010
• Lobko Christina - 2011
• Sakovich Maria - 2011
• Belyaeva Maria - 2012
• Prokopkina Taisiya - 2012
• Drobot Victor - 2013
• Shigapova Anastasia - 2013
• Aksenova Vera - 2013

Publications

Created by on 23/08/2013.

Teaching aids

• R.V. Panin, I.N. One, V.P. Zlomanov. Seminars on inorganic chemistry (II semester). Methodological development for students of the Faculty of Chemistry of the Baku branch of Moscow State University. Volume 68 pages. Printing house of the Baku branch of Moscow State University. Baku, 2010.
• V.P. Zlomanov, R.V. Panin, I.N. One. Workshop on inorganic chemistry (II semester). Methodological development for students of the Faculty of Chemistry of the Baku branch of Moscow State University. Volume 61 pages. Printing house of the Baku branch of Moscow State University. Baku, 2010.
• V.P. Zlomanov, R.V. Panin, I.N. One. Inorganic chemistry. Lecture notes. Part 2. Methodological development for students of the Faculty of Chemistry of the Baku branch of Moscow State University. Volume 105 pages. Printing house of the Baku branch of Moscow State University. Baku, 2010.
• R.V. Panin. Seminars on inorganic chemistry (I semester). Methodological development for students of the Faculty of Chemistry of the Baku branch of Moscow State University. Ed. A.N. Grigoriev. Volume 111 pages. Printing house of the Baku branch of Moscow State University. Baku, 2010.
• R.V. Panin, S.Ya. Istomin, P.S. Berdonosov. Workshop on inorganic chemistry (I semester). Methodological development for students of the Faculty of Chemistry of the Baku branch of Moscow State University. Volume 105 pages. Printing house of the Baku branch of Moscow State University. Baku, 2010.
• R.V. Panin, S.Ya. Istomin, P.S. Berdonosov. Seminars on inorganic chemistry for the II semester. Methodological development for students of the Faculty of Chemistry of the Baku branch of Moscow State University. Volume 107 pages. Printing house of the Baku branch of Moscow State University. Baku, 2011.

Bykasov V. E., Chujan G. N. Geomorphology of the Bering Island Coastal Area // 5th International Conference on the Environmental Management of Enclosed Coastal Seas (EMECS–2001), Japan, Kobe, 2001.

GEOMORPHOLOGY OF THE BERING ISLAND COASTAL AREA

Valery Bykasov and Galina Chujan

The Bering Island is an elongated from south-east to north-west and tectonically upstanding block of a shelf platform that, in its turn, forms the top of a subaqueous ridge of a western part of the Aleutian island volcanic arc. The greater part of the island is occupied with a middle-high ridge (from 150 up to 750 m) that stretches from CapeMonati in the south-east to the depression of LakeSarannoe. This ridge is distinctly subdivided into two morphological parts by the watergap of the Polovinnaya and Peresheek rivers. The ridge relief is mainly denudational-tectonic. This is emphasized by a high (up to 100-250 m) shore cliff steeply breaking at the coast.

The history of development of the islands is rather peculiar. There was repeatedly observed sometimes decrease of their area, sometimes, on the contrary, its increase in several times. Anyhow, even in the second phase of Recent Pleistocene glaciation the Bering and MednyIslands represented the united land the coast line of which lay approximately along 100-200-meter isobaths. The island's recent outlines were formed about 4-5 thousand years ago after Middle Holocene climatic optimum. At present the island is slowly uplifting.

The island’s geological structure conditions considerable differences in the formation of shore and near-shore forms of relief of its southern (the Pacific) and northern (the Bering Sea) coasts, there being a well-expressed bench all over the shore. These relief forms differ in geomorphological structure as well as, correspondingly, in lithodynamic peculiarities of sedimentation. As a rule, the island southern part shores are high and precipitous with a lot of almost impassable areas and non-passages. Here the cliffs are very active and they are the source of supply of fragmental product into the coastal area. The shore line of the island northern part is rimmed with a wide strand up to 100-200 m.

Generally, the following total regularities of geomorphological structure and matter distribution in the beach area are noted for the shore of the whole island. All the recent area of ​​beaches is formed mainly owing to washout of shore cliffs and alluvial drifts of rivers and creeks. As far as the island is slowly uplifting, the bench area is well developed all over its shore. In this area the speed of waves becomes slower and the material brought from the depth remains here not reaching the beach area. For the same reason there are no well-expressed stormy breakers. Thus, any significant dynamic differentiation of sediments of the shore area is not observed. By the way, this is confirmed by the data received by us from the analysis of mineralogical composition of sandy fraction and petrographic composition of pebbly material. The obtained data confirmed these general regularities of formation and development of the BeringIsland shore area.

GEOMORPHOLOGY OF THE COASTAL ZONE OF BERING ISLAND

Bering Island is a tectonically uplifted block of the shelf plate, elongated from the southeast to the northwest, which, in turn, forms the top of the underwater ridge of the western part of the Aleutian island volcanic arc. Most of the island is occupied by a medium-altitude, from 150 to 750 m, ridge, which, stretching from Cape Monati in the southeast to the depression of Lake Sarannoy, is clearly divided by the through valley of the Polovinnaya and Isthmus rivers into two morphological parts. The relief of the ridge is mostly denudation-tectonic, which is emphasized by a high, up to 100–250 m, coastal ledge, steeply dropping to the sea coast.

The history of the development of the islands is quite peculiar. A decrease in their area was repeatedly observed, then, on the contrary, its increase by several times. In any case, even in the second phase of the Upper Pleistocene glaciation, the Bering and Medny Islands were a single land, the coastline of which ran along approximately 100-200-meter isobaths. The modern shape of the island took about 4-5 thousand years ago after the Middle Holocene climatic optimum. The island is currently experiencing a slow uplift.

The geological structure of the island causes, in the presence of a well-defined bench along the entire coast, significant differences in the formation of coastal and coastal landforms of its southern (Pacific) and northern (Bering Sea) coasts both in terms of geomorphological structure and, accordingly, in terms of lithodynamic features of sedimentation. The shores of the southern part of the island are usually high, steep, with a large number of difficult sections and impassable areas. The cliffs here are very active and serve as sources of detrital material entering the coastal zone. The coastline of the northern part of the island is bordered by a wide, up to 100–200 m, strip of beach.

In general, for the coast of the entire island, the following general patterns of geomorphological structure and distribution of matter in the beach area are noted. The entire modern zone of beaches was formed mainly due to the erosion of coastal ledges and the alluvial removal of rivers and streams. Since the island experiences a slow uplift, the bench zone is well developed along its entire coast. In this zone, the wave velocity is damped and the material drawn from the depth remains here before reaching the beach zone. For the same reason, there is no clear manifestation of storm surges. That is, no significant dynamic differentiation of sediments in the beach zone is observed. Which, by the way, is also confirmed by the data of our analysis of the mineralogical composition of the sandy fraction and the petrographic composition of the pebble material, which confirmed these general patterns in the formation and development of the coastal zone of Bering Island.

How should the timekeeping system be regulated in Russia? Cancel or keep daylight savings time? Andrei Panin, Candidate of Sciences, an employee of the Faculty of Geography of Moscow State University, expressed his opinion in the article "".

Readers of "RG" this problem found a lively response. We propose to continue the discussion about what configuration of time zones would be optimal for Russia. Andrey Panin is ready to answer your questions and comment on the proposals.

A little about our expert:

Panin Andrey Valerievich. Born in 1966 in Moscow. As a schoolboy, he came to the Faculty of Geography of Moscow State University, and so he stayed here. In 1991 he defended his PhD thesis. He worked on expeditions in Yakutia, the Krasnoyarsk Territory, Tuva, as well as throughout the European part of the country from Murmansk to Stavropol. Published three monographs (co-authored), about a hundred scientific articles in various publications, more than half of them in peer-reviewed journals, Russian and English. She is finishing her doctorate, but her passion for the popularization of scientific knowledge unexpectedly got in her way. Over the past year, he has collaborated with several central newspapers.

One of the topics of cooperation is the problem of time calculation in Russia. According to the scientist, this problem is more likely from the field of not science, but practice - the rational organization of life: "I want that in the country where I live myself, and my children will live after me, life was built on some reasonable principles. Therefore I put aside my unfinished doctoral thesis and write about time zones."