У статті йдеться про антропосистему роману Ю. Муш- кетика «На брата брат», яка представлена двома великими групами: реа- ліонімами (імена реальних історичних персоналій) та авторськими іменами (використовуються для іменування вигаданих персонажів). Установлено, що зафіксовані в тексті твору імена персонажів мають різну генетичну спря- мованість. Відповідно до етимологічної належності конкретного імені героя, виділено такі групи за походженням: грецькі, латинські, давньоєврейські та слов’янські імена. Власні імена персонажів роману «На брата брат» відобра- жають унікальний історико-культурний портрет козацької доби в Україні XVII–XVIII ст. із притаманним їй своєрідним багатонаціональним складом іменникá. Досліджено, що письменник використовує моделі однокомпонент- ного, двокомпонентного та трикомпонентного іменування героїв твору. Роз- глянуто однокомпонентні імена, які є найбільш частотними в тексті роману та представлені назвами у формі одного імені або одного прізвища, які часто а...

RUSSIAN ACADEMY OF SCIENCES Department of Earth Sciences Institute of Water Problems Scientific Council RAN Russian Foundation for Basic Research Russian National Committee of the International Association of Hydraulic Research DINAMICS AND THERMIC OF RIVERS, BASINS AND COASTAL SEAS VI Conference PROCEEDINGS 22-26 November 2004 Moscow, Russia DYNAMICS OF SOME ITALIAN RIVER MOUTHS FOR THE PAST 10.000 years (THE HOLOCENE PERIOD) * Piero Bellotti and Publio Valeri University of Rome «La Sapienza», Department of Earth Sciences, Rome Italy Dipartimento di Scienze della Terra, Università di Roma «La Sapienza, Roma, Italia) At present, many italian rivers form deltas, in microtidal regime, with different morphological and dynamic characteristics. There are four main types of river deltas in Italy [1] (Fig. 1): 1) delta of limited size, single and unstable distributary channel, and deposits from silt to gravel. These deltas are formed on the narrow shelves in the mouth of rivers with limited drainage basin (river Centa and Crati); 2) delta of limited size, with multiple distributary channels, sediment from clay to sand. Such delta formed in protected areas with moderately steep shelf in the mouths of small rivers (river Isonzo); 3) delta of medium size, single and stable distributary channel, in most cases, and deposits from silt to sand. These deltas are formed on the broad shelf in the mouths of rivers with basin area allo >10.000 km2. These rivers form large strand plain (river Arno, Ombrone, Tiber, Volturno, Tagliamento); 4) delta of large size with many and unstable distributary channels and sediment from clay to sand. Such delta formed in the wide shelf with a weak slope (River Po). Deltas are formed when Vm> Vr, where Vm - volume of sediment receipts at the mouth of river, and Vr- amount of sediment carried away by sea processes. In non-tidal deltas for the time interval Δt relationship exists ± ΔVf = Vd ± Vo-Vi [6], where ΔVf - change in the volume of the fan, Vd- volume of river sediments coming from all delta distributaries, Vo - the amount of sediment carried by the wawes , Vi - the amount of sediment carried offshore or by river plume or by density flow. Let us assume that γd - density of river water, and γb - the density of the receiving waters of the reservoir; if γd<γb, sediments are transported in the river buoyancy low, and if γd>γb, in the form of density flow. In marine deltas last condition mets only in exceptional floods, and in the Italian deltas is observed only in the delta of the river Crati [8]. In the absence of relative sea level rise (the sum of eustatic sea level rise and land subsidence) delta extends when ΔVf >0 and is subjected to erosion if ΔVf<0. With a significant relative sea-level rise happens drowning of the sediment prism Va in the process of accumulation. In the interval Δt when ΔVf>0 delta extends, if ΔVf >Va, and shifts to the land if ΔVf >Va. Stratigraphic studies on the Italian deltas [2-4, 7] discover that in the process of their development during the Holocene changed fisiographic and dynamic conditions of their formation. Sea levels in the early Holocene, at the end of the last glacial maximum was at 30 m below the present. In the northern part of the Adriatic Sea (shelf with a weak slope) away from the recent mouths already formed a large system of barrier-lagoon-estuary, which receives runoff of various rivers such as the Po, Tagliamento, Adige and Isonzo. On the coast of the Tyrrhenian Sea rivers flow into large rias, partially protected from the sea by sand bars. There rivers built longitudinal delta structures. On most wide shelves, river mouths were already in rias and the delta building not happened. Despite the progressive decrease of eustatic sea-level rise, the mouth shifted landwards until about 6,000 years ago, when sea level began to change, as in the present conditions (1-1.5 mm / year). During this period, estuaries almost everywhere presented broad lagoons or bays, partially bordered by sand barriers. Within these lagoons whose a lot of river mouths. Tyrrhenian rivers carry their deposits directly into the lagoon and built lagoon-delta complexes [1], in other cases, the deposits flowed into the lagoon not regularly, depending on the movement of channels, the most active in areas with severe land subsidence. In the northern part of the Adriatic Sea, the lagoon system was already formed, and it formed separate delta protrusions [4]. At the mouth of the river Crati river sediments interspersed lagoon clays. About 3,000 years ago, all major Italian river has flowed into the sea, partially filling the lagoon, but has not yet formed a stable marine delta systems. Many small rivers long maintained lagunar mouths, that disappeared only by drying lagoons. In the Etruscan period appear the first extensions of the delta, but only in the Roman Empire Period and in the Tyrrhenian and Adriatic seas appear first stable delta bodies, near which there were still large lagoon during the early Middle Ages the Tyrrhenian delta (all single channel) were subjected to partial erosion; in the delta complex of the Po River (with many and unstable channels), some bodies partially were destroyed, partly forwarded in the sea. In XV-XVI centuries delta moving into a phase of active progradation, which lasts until the XIX century. In the mouths of the Tyrrhenian rivers formed delta with beach ridges. Po Delta forwarded into the sea more than 15 kilometers, forming a multi channel system. It confirms the excess energy of the river compared with the energy of waves. At the mouth of the river Centa, delta shifted producing temporary separation of the main channel into two branches. At the mouth of the river Crati began formation of the modern delta and recurrent floods crossed the ancient coastal bars, and the remains of the lagoon turned into swamp (in the lagoon to the III century was the port). In XX century the progress of the delta ends everywhere, and in some cases even a partial retreat of delta lobes begins. By stratigraphic data can be established that between the beginning of the Holocene and the time 6.000 years ago, occur condition ΔVf<Va, in connection with the last phase of eustatic sea level rise. For the last 6.000 years the value Va at eustatic rise becomes small, but it remains significant at the mouths of rivers Po and Crati as a result of strong subsidence. However, for the period 6000-3000 years ago, at the mouth of the Po river changed dynamics of the delta, and for SΔVf>Va (S characterizes majority of mouths) was a phase of progress; at the mouth of the river Crati similar phase was not, as the formation of the delta, apparently occurred under ΔVf ~ Va. In Tyrrhenian mouths value of Va was small, ΔVf values were sufficient to advance of lagoon deltas. Over the last 3,000 years, despite an increase in the values of Vo and Vi, corresponding to the position of sea level in the all mouths, the values ΔVf increase and development of deltas occur anywhere under the conditions ΔVf>Va. Especially in the second half of the XX century occurs condition ΔVf >> Va, which corresponds to the most intense phase of progress of the major deltas Italy. Later there were still periods of negative values ΔVf, defined by data of erosion of the delta lobes. Changes ΔVf in this period is mainly dependent on the fluctuations of Vd to the result of the change of different climatic phases or human impact. REFERENCES Bellotti Р. Il modello morfo-sedimentario dei maggiori delta tirrenici. Boll. Soc. Geol. It 2000. 119. 777-792. Bellotti Р., Chiocci F.L., Milli S., Tortora Р., Valeri P. Sequence stratigraphy and depositional setting of the Tiber Delta: integration of high resolution seismics, well-logs and archeological data. Journ. Sedim. Res. 1994. 64 B. 416-432. Bellotti Р., Caputo C., Davoli L., Evangelista S., Pugliese F. Evolutionary Dynamics of the Crati River Delta (Italy). Proc. VI Int. Conf. MEDCOAST’03, 7-11 Oct. 2003. Ravenna, 2003. 1805-1816. Bondesan М., Favero V., Vinals M.J. New evidence on the evolution of the Po delta coastal plain during the Holocene. Quatemary International. 1995. 29/30. 105-110. Roveri М., Correggiati A, Asioli A., Trincardi F. Evoluzione dei sistemi deltizio e costieri in Adriatico settentrionale. Abs Volume GEOITALLA. 5-9 Sept. 1997. 1997. 4142. Mikhailova M. Merphodynamics and morphometry of nontidal protruding river deltas. I.A H R. Symp. River. Coastal and Estuarine Morphodynamics, 6-10 Sept. 1999. Genova. Piccazzo М., Firpo М., Ivaldi R., Arobba D. Il delta del Fiume Centa (Liguria occidentale): Un esempio di modificazione recente del clima e del paesaggio. Il Quaternario. 1994. 7. 293-298. Ricci Lucchi F., Coltella A., Gabbianelli G., Rossi S., Normark W.R. The Crati submarine fan, Ionian Sea. Geo-Marine Letters. 1984. 3. 71-77. Fig. 1. Scheme of distribution of the main Italian rivers On four inset shows four types of deltas, described in the text. Percentages indicate the average slope of the underwater platforms near the mouth

The relevance of research.Technological sensors (sensors of load, pressure, liquid temperature, solution yield, liquid density) are used for monitoring data of technical operations of well drilling, various types repair of well, exploration drilling in the oil and gas industry on drilling and repair of all types of wells. Modern sensors are small in size and manufactured on the basis of nanoelectromechanical systems to increase sensitivity. They include constituent elements, nano beams and nano plates. These elements operate at high temperatures and are subjected to mechanical loads of various kinds. Increasing the strength of these elements is undoubtedly an urgent task. The main aim of the research is to build a mathematical model on the basis of Timoshenko kinematic hypothesis and the modified couple stress theory of a sensing element in the form of a beam, a nano-electro-mechanical sensor under the action of mechanical and thermal fields;to develop methodology for obtaining the ...

Розглядаються теоретичні аспекти феномену памʼяті в літературному творі, а також культурні коди, які проявляються в художніх текстах

Kulinyak Nazar Ivanovich. National and European Modernist Components of the Anton Rudnytsky's Individual Style. The article deals with the creative personality of one of the leading musicians of Ukrainian culture of the 20th century-Anton Rudnitsky, a composer, conductor, symphonist, pianist, critic, an active social and cultural figure, whose creative path took place in two artistic paradigms: the European and American continuum. Through the prism of the study of the artist's creative becoming period in a wide range of modern modernist tendencies of European culture (V. Barvinsky, V. Kurts, L. Syrota), later, during studying in Germany (F. Shreker, F. Bouton, K. Zaks, G. Abert), the leading composer's stylistic orientations were formed (B. Bartko, M. Ravel, I. Strvinsky, A. Senberg) and the radical level of their application in the author's creative intentions in various planes of activity (vocal cycle "Chinese flute" on the tests of Li Bo, Atonal Sonata for piano op.11, "Three Hymns for the Hour of Industry" for bass and orchestra, Symphony No. 1). While systematizing the genre palette in order to identify the priority directions and the specifics of A. Rudnytsky's genre and stylistic thesaurus (vocal, choral, vocal-symphonic, stage, instrumental compositions, etc.) both in Ukrainian and in the foreign period, the leading signs of his composer's handwriting are revealed with the prevalence of the Avant-Garde and Modernist tendencies embedded in a specific national ground. However, the stylistic dynamics of the composer's handwriting gradually transforms from radical Avant-Garde quest to Romantic-Impressionistic and folkloristic tendencies that characterize the work of the American period, primarily associated with choral, cantata oratorical and operatic genres.

Актуальность работы обусловлена необходимостью выяснения роли пирокластического материла в формировании угленосных отложений и геохимического фона редких элементов в углях. Цель: выяснение природы тонштейна из угольного пласта Новый-1а Харанорского буроугольного месторождения. Объекты: угли и тонштейн пласта Новый-1а Харанорского месторождения. Методы: отбор проб из пласта Новый-1а Харанорского месторождения угля; масс-спектрометрия с индуктивно связанной плазмой (ICP-MS), атомно-эмиссионная спектрометрия с индуктивно связанной плазмой (ICP-AES), инструментальный нейтронно-активационный анализ (ИНАА); минеральный состав изучен методами оптической микроскопии, сканирующей электронной микроскопии, рентгенофазовым анализом. Результаты. В ходе исследования был изучен тонштейн из угольного пласта Новый-1а Харанорского буроугольного месторождения. Минеральный состав, структурно-текстурные и геохимические особенности тонштейна позволили установить его апопепловый генезис. Комплекс критерие...