Writings Of Professor Research Articles

Вклад трудов профессора Н.Н. Клодницкого (1868–1939) в становление учения о природной очаговости чумы

Вклад трудов профессора Н.Н. Клодницкого (1868–1939) в становление учения о природной очаговости чумы

DOCTRINAL POSITION OF THE INDEPENDENCE OF THE JUDICIARY IN WORKS OF V. I. ANICHINA

The article is in memory of Vera Ivanovna Anishina, Doctor of Law, Professor of the Russian State University of Justice, Chairman of the 2nd Judicial Collegium for Administrative Cases of the Supreme Court of the Russian Federation. The author of the article highlights the basic doctrinal provisions of the independence of the judiciary in the writings of Professor V.I. Anishina, highlights the scientist's contribution to improving the mechanism of the judge's responsibility in the Russian Federation. Many topical issues are being touched on the judiciary in the Russian Federation. The author analyzes numerous works of the scientist in the field of the principles of the administration of justice and discloses the content of the principles of independence and independence of judges. Conclusions are drawn about the need to change the system of principles of law, by adding new ones. The idea of a new qualitative approach to the formation of a system of constitutional and legal ideas of the modern development of the judiciary in the Russian Federation is being put forward. Based on the assumption of the need to reform the system of bringing the judge to justice, ideas are offered regarding the mechanism for bringing the judge to legal responsibility on the basis of the ideas of Judge V.I. Anishina, who participated in the consideration of the complaints of judges, deprived of the status of a judge and appealing decisions of the qualification collegiums of judges and the highest qualification board of judges in the country's highest judicial body, other scientists and international experience. It is concluded that the mechanism of judicial responsibility must be enshrined in the federal law "On the responsibility of a judge in the Russian Federation". Current conclusions, having elements of scientific novelty, made by the author in the work, correlate with the available sources on the topic of the research, supported by theoretical research.

Стадії ґрунтотворення підвісних ґрунтів Верховинського вододільного хребта Українських Карпат

It was found out that suspended soils in Verkhovyna Dividing Range in Ukrainian Carpathians are intrazonal ones and are formed near dense sandstones outcrops in Krosnenska zone provided excess moisture of flushing type of water regime. Suspended soils are located within the mountain-forest and subalpine zones under moss lichen communities. They form habitats ranging from 0.1 to 1.0 square meter, oval and oblong shaped with the highest capacity of organic horizon in the central part with gradual reduction to the periphery. Suspended soils in Ukrainian Carpathians were mentioned for the first time in writings of Professor A. Zrazhevskyi. Formation of suspended soils in dense sandstones within Verkhovyna Dividing Range can occur in two ways: initial (primary) soil development and settlement of moss lichen communities from adjacent soil areas. Main stages of formation of soils under research are detected analyzing the succession of plant communities and morphological features of each section. Initial stage begins with the settlement of alga, bacteria, fungi, actinomyces, lichens (crustose and foliose) in centres of soil formation and formation of humified layer of dark gray colour up to 2 cm thick. Moss settlement on the developed organo-mineral layer and formation of organic (peat) horizon marks the beginning of development stage. Soils under research with formed organic horizon up to 10 cm thick are to be classified as initial suspended soils. The development stage is accompanied by accumulation of defunct organic remains (peat formation) and expansion of organic horizon (Td+T). Soils formed in Krosnenska zone in mild wind-blown sandstones with organic horizon more than 10 cm thick are at the stage of equilibrium functioning. It is advisable to define these soils as peat-suspended soils. Suspended soils are not represented in the nomenclature list of soils of Ukraine, that encourages conducting more detailed research on their classification. Patterns of distribution of soils under research and stages of soil formation were found out. Key words: Verkhovyna Diving range, suspended soils, the formation of peat, genesis, stages of soil formation.

The Learned Writings of Professor G.I. Tunkin

AbstractNo Abstract

Bibliography of the Writings of Professor K. H. Connell

Bibliography of the Writings of Professor K. H. Connell

Industrialisation and the U.N. Economic Commission for Africa

There has been a marked change in recent years in the climate of ideas about industrialisation in developing economies and it is fortunately no longer necessary to argue in favour of industrialisation in opposition to another approach to economic development. Yet it is still necessary to continue to state the basic case, particularly since Africa is industrially the least developed of all the continents. The doctrine that industry is the key to economic development is of comparatively recent origin. Its antecedents are the writings of Professor G. Myrdal and Dr R. Prebisch and the practical achievements of the U.S.S.R. and Japan.

A list of the published writings of professor R. W. Zandvoort

A list of the published writings of professor R. W. Zandvoort

Laminar Moulds in Cellulose Acetate for the Study of Rock and Mineral Structures

The preparation and utility of laminar collodion moulds for recording relief features in natural surfaces of fossil plants is well known from the writings of Professor A. G. Nathorst (1). Equally familiar is the technique of Professor J. Walton (2) for making cellulose acetate “peels” from ground and etched surfaces of rocks containing carbonized remains of vegetable tissues. More recently, similar methods have been adopted by Dr. S. Leclercq (3) for studying fossil corals, by Professor A. E. Trueman (4) for examining ammonites, and by Dr. J. K. S. St. Joseph (5) and Dr. J. Weir for the analysis of fossil brachiopods. In these several cases, ground and etched specimens were prepared, from which cellulose nitrate or cellulose acetate moulds were taken. Hitherto, however, no corresponding technique appears to have been used either for research upon inorganic rock-structures or for the investigation of surface relief-characters of minerals.

Life and Writings of Professor F. E. L. Beal

Life and Writings of Professor F. E. L. Beal

3. Contact-Phenomena of some Scottish Olivine-Diabases

In the second and third numbers of the ninth volume of Tschermdk's Mineralogische und petrographische Mittheilungen, I published the results of an examination of some “dolerites” from the Carboniferous basin of the Firth of Forth, the material for which I obtained through the kindness of Prof. Archibald Geikie. It is true most of the “dolerites” are already well known through the valuable writings of Professor A. Geikie and Mr Allport, but a special study of the modifications of the rock in the different parts of any one volcanic mass has not yet been the subject of any paper. Having elicited many facts of petrological interest, I purpose giving in this communication a short account of my investigations.