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Tytuł:
Hoard Of Olbian Coins Of ‘Borysthenes’ Type Found At Spring 2018 In The Region Of Gorodishche Town, Oblast Cherkassy, Ukraine
Skarb olbijskich monet z głową boga rzeki Borysthenes znaleziony wiosną 2018 roku w okolicach miasta Gorodišče, oblast Czerkassy, Ukraina
Autorzy:
Орлик, Василий
Коцур, Виктор
Цыганенко, Лилия
Tematy:
Olbia, Dnieper, coins, hoard
Olbia, Dniepr, monety, skarb
Pokaż więcej
Wydawca:
Łódzkie Towarzystwo Naukowe
Powiązania:
https://bibliotekanauki.pl/articles/584906.pdf  Link otwiera się w nowym oknie
Opis:
TYTUŁ ORYGINALNY: Клад ольвийских монет «борисфенов», найденный в Городищенском районе Черкасской области весной 2018 года W kwietniu 2018 roku, na południowo-wschodnim krańcu miasta Gorodišče, oblast Čerkassy, Ukraina, znaleziono około 70 brązowych monet Olbii z głową boga rzeki Borysthenes na awersie oraz toporem, łukiem, monogramem i napisem ΟΛΒΙΟ na rewersie. Znalezisko potraktowane zostało jako zespół; uznano, że mamy do czynienia ze skarbem. Istotne, że znalezisko to jest jednym z najdalej zlokalizowanych znalezisk monet nadczarnomorskiej Olbii. Z odkrytego zespołu opracowano jedynie 52 monety. Wybito je w końcu IV i pierwszej połowie III p.n.e. Monety zaliczone zostały do siedmiu grup według podziału zaproponowanego przez P.O. Karyškovskiego. Najmłodsza z opracowanych monet (z monogramem 91, według P.O. Karyškovskiego; odniesiono się również do propozycji V. Anochina, N.A. Frolovej i M. Abramzona) datowana jest, w ocenie autorów, na lata 260-250 p.n.e.; dopuszcza się jednak i inną chronologię. Dlatego też zaproponowano czas zdeponowania skarbu: druga połowa III w. p.n.e. Zwrócono uwagę, że data zdeponowania skarbu zbieżna jest z chronologią osady, którą zlokalizowano w okolicach miasta Gorodišče.
ORIGINAL TITLE: Клад ольвийских монет «борисфенов», найденный в Городищенском районе Черкасской области весной 2018 года In April 2018 an assemblage of Olbian bronze coins of Borysthenes type was found not far from the town Gorodishche, region Cherkassy, Ukraine. 52 coins were described. In opinion of authors the assemblage should be treated as the hoard.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Stratigraphic interpretation of loess in the marginal zone of the Dnieper I ice sheet and the evolution of its landscape after deglaciation (Dnieper Upland, Ukraine)
Autorzy:
Komar, M.
Łanczont, M.
Fedorowicz, S.
Gozhik, P.
Mroczek, P.
Bogucki, A.
Tematy:
loess
palaeosol
Dnieper
Pleistocene
palaeogeography
palynology
luminescence dating
Pokaż więcej
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Powiązania:
https://bibliotekanauki.pl/articles/2060425.pdf  Link otwiera się w nowym oknie
Opis:
Litho-, pedo- and palynological analyses constrained by radiometric dating of two loess-palaeosol sequences, Nahirne and Velyka Andrusivka, exposed in a cliff at the eastern edge of the Dnieper Upland, Ukraine, document regional environmental changes in the western marginal zone of the Dnieper lobe. The postglacial loess sedimentation cycle was initiated during MIS 8, immediately after the ice sheet recession. On the basis of palaeorelief analysis, subsequent morphogenetic stages of the original postglacial relief, associated with the modifying and masking role of the loess, and destructive slope processes were reconstructed. Periglacial steppe with consistently present scattered trees formed the Pleistocene landscape in the Middle Dniester area during the last three glacial periods. In such an environment, the following loess beds, correlated with marine isotope stages (MIS), were deposited: Dnieper (dn) - MIS 8, Tyasmyn (ts) - MIS 6, Uday (ud) - MIS 4 and Bug (bg) - MIS 2. During the last two warm periods: Kaydaky (kd) - MIS 7 and Pryluky (pl) - MIS 5, the landscape was not fully forested. As a result, the individual palynological features of these soils show a diverse character. The TL and OSL dates form a sequence with numerous inversions that are difficult to interpret. Although these data do not significantly influence the interpretation, they show that: 1) there are loesses that undoubtedly formed after the maximum extent of the ice sheet by short-distance transport of dust material from local fresh glacial deposits and the underlying Paleogene rocks; 2) date distortions result from the activities of an exceptionally rich pedofauna that has contaminated the material not only in the soil sections of the profile but also in the adjacent loess. It is possible to delimit a few stages of pedofaunal activity in each of the soil units.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Diprion pini L. (Hymenoptera, Symphyta, Diprionidae) population dynamics in the Low Dnieper region
Autorzy:
Nazarenko, Serhii
Meshkova, Valentyna
Kolienkina, Maryna
Wydawca:
The Committee on Forestry Sciences and Wood Technology of the Polish Academy of Sciences and the Forest Research Institute in Sekocin Stary
Cytata wydawnicza:
Meshkova, Valentyna & Nazarenko, Serhii & Kolienkina, Maryna. (2019). Diprion pini L. (Hymenoptera, Symphyta, Diprionidae) population dynamics in the Low Dnieper region. Folia Forestalia Polonica. 61. 22-29. 10.2478/ffp-2019-0002.
Opis:
Pine sawflies (Hymenoptera, Symphyta, Diprionidae) are the most spread foliage browsing insects of pine forests in Europe, especially monovoltinous European pine sawfly Neodiprion sertifer (Geoffroy, 1785) and common pine sawfly Diprion pini (Linnaeus, 1758), which develops in one or two generations per year depending on weather. The outbreaks of both pine sawflies are the most frequent and intensive in the Steppe zone of Ukraine, especially in the Low Dnieper region, where pine forest (Pinus sylvestris Linnaeus and Pinus pallasiana D. Don) was planted on moving sands in the sixties of the 20th century. This research is aimed at the evaluation of the parameters for D. pini outbreak dynamics in the Low Dnieper region. Outbreak severity, specific foci area and mean score of stand threat by D. pini were evaluated from the regional statistical reports. In the regional scale for 1979–2017, notable outbreaks of D. pini were registered in 1982, 1993, 2002, 2006 and 2017. An interval between maximums was from 4 to 11 years, in average 9 years. The growth of foci area in 1979–1998 as compared to 1999–2017 as well as correlation between pine stand area and annual area of this pest’s foci in different forests was not statistically significant. Graphical analysis of dynamics of D. pini focal area for 2010–2017 was done based on individual threat levels. Our study confirms the fact of three outbreaks for this period in three forest and hunting enterprises (FHE), two outbreaks in one FHE and one outbreak in one FHE. An interval between the outbreaks makes three or six years. The causes of such shortening of interval are discussed.
Dostawca treści:
Repozytorium Centrum Otwartej Nauki
Artykuł
Tytuł:
The application of fault seal analysis at the Solokha field, Dnieper-Donets Basin, Ukraine – case studies
Autorzy:
Okrepkyi, O.
Tiapkina, A.
Tematy:
Dnieper-Donets Basin
Fault Seal Analysis (FSA)
hydrocarbon traps
Pokaż więcej
Wydawca:
Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie. Wydawnictwo AGH
Powiązania:
https://bibliotekanauki.pl/articles/184614.pdf  Link otwiera się w nowym oknie
Opis:
The Solokha gas field is one of the most valuable hydrocarbon fields in the central axial part of the Dnieper-Donets Basin (DDB). Every new exploration well there has to be highly validated in order to reduce possible drilling risks. In this study, the characteristics of faults, as possible seals, are analysed, based on the latest well and 3D seismic data. Evaluating fault seal risk is a constitutive factor in hydrocarbon exploration and production. For this reason, to reduce uncertainty in the faults’ leaking facilities, we used a couple of known approaches, such as juxtaposition analysis, with building Allan diagrams, to determine the relationship between sand-sand juxtaposition and the occurrence of hydrocarbons-bearing sands. We used the Shale Gouge Ratio (SGR) calculation with prediction of clay content distribution along the faults, pressure data analysis, seismic at tributes modelling and self-organized map clustering analysis for accurate delineation of sand bodies shape. This represents a complex research method of integration of high-quality depth processing with seismic structural and stratigraphic interpretation and, also, geological modeling. In this paper, we assessed the Jurassic and Visean faults of the Solokha gas field, according to their fluid cross-flow facilities. This research will provide valuable information about the presence of prospective places for hydrocarbon accumulation and will likely impact the well staking process for the upcoming drilling.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Diprion pini L. (Hymenoptera, Symphyta, Diprionidae) population dynamics in the Low Dnieper region
Autorzy:
Meshkova, Valentyna
Nazarenko, Serhii
Kolienkina, Maryna
Tematy:
Diprion pini
Low Dnieper sands
outbreak severity
outbreak frequency
Pokaż więcej
Wydawca:
Instytut Badawczy Leśnictwa
Powiązania:
https://bibliotekanauki.pl/articles/2044139.pdf  Link otwiera się w nowym oknie
Opis:
Pine sawflies (Hymenoptera, Symphyta, Diprionidae) are the most spread foliage browsing insects of pine forests in Europe, especially monovoltinous European pine sawfly Neodiprion sertifer (Geoffroy, 1785) and common pine sawfly Diprion pini (Linnaeus, 1758), which develops in one or two generations per year depending on weather. The outbreaks of both pine sawflies are the most frequent and intensive in the Steppe zone of Ukraine, especially in the Low Dnieper region, where pine forest (Pinus sylvestris Linnaeus and Pinus pallasiana D. Don) was planted on moving sands in the sixties of the 20th century. This research is aimed at the evaluation of the parameters for D. pini outbreak dynamics in the Low Dnieper region. Outbreak severity, specific foci area and mean score of stand threat by D. pini were evaluated from the regional statistical reports. In the regional scale for 1979–2017, notable outbreaks of D. pini were registered in 1982, 1993, 2002, 2006 and 2017. An interval between maximums was from 4 to 11 years, in average 9 years. The growth of foci area in 1979–1998 as compared to 1999–2017 as well as correlation between pine stand area and annual area of this pest’s foci in different forests was not statistically significant. Graphical analysis of dynamics of D. pini focal area for 2010–2017 was done based on individual threat levels. Our study confirms the fact of three outbreaks for this period in three forest and hunting enterprises (FHE), two outbreaks in one FHE and one outbreak in one FHE. An interval between the outbreaks makes three or six years. The causes of such shortening of interval are discussed.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Large and small reservoirs of Ukraine
Autorzy:
Khilchevskyi, Valentyn
Grebin, Vasyl
Dubniak, Sergiy
Zabokrytska, Myroslava
Bolbot, Hanna
Tematy:
Dnieper cascade
Dniester reservoir
rent
reservoir
river basin district
Ukraine
Pokaż więcej
Wydawca:
Instytut Technologiczno-Przyrodniczy
Powiązania:
https://bibliotekanauki.pl/articles/2073741.pdf  Link otwiera się w nowym oknie
Opis:
This article is a continuation of the topic of artificial water bodies in Ukraine, which was started in our previous publication in 2020. It was devoted to accounting and monitoring of ponds at the local and national levels. Reservoirs play important role in water supply for various sectors of the economy. For this reason, much more attention is paid to reservoirs by the State Agency of Water Resources of Ukraine (Ukr. Derzhavne ahentstvo vodnykh resursiv Ukrainy), the Ministry of Ecology and Natural Resources of Ukraine (Ukr. Ministerstvo ekolohii ta pryrodnykh resursiv Ukrainy), scientists and specialists. The main tasks of the article are: to establish patterns of territorial distribution of reservoirs in administrative regions and river basins districts; to identify the role of large and small reservoirs in the balance of river runoff regulation. There are 1054 reservoirs in Ukraine, so it can be considered a country rich in reservoirs. The volume of the cascade of six reservoirs on the Dnieper River and the Dniester Reservoir is 85%, other reservoirs – 15% of the total number. At the same time, there are 1047 other reservoirs (middle, small and very small), which provide for regional needs and which have their own patterns of distribution throughout the country. The main trend in their creation was water supply of industrial regions, in particular Kharkiv, Donetsk, Dnipropetrovsk and others. About 28% of reservoirs are leased. These reservoirs also require clear accounting and monitoring at the national level, attention from water management and environmental organizations.
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Sprawozdania Archeologiczne 70 (2018)
Revisiting the Neolithic chronology of the Dnieper steppe region with consideration of a reservoir effect for human skeletal material
Autorzy:
Kotova, Nadezhda
Wydawca:
Instytut Archeologii i Etnologii Polskiej Akademii Nauk
Powiązania:
Bodyanskiy A. V. and Kotova N. S. 1994. Vovnigskiy 2 pozdneneoliticheskiy mogilnik. In Arkheologichni pamyatki ta istoriya starodavnogo peselennya Ukrainy 1, Lutsk: Vezha, 98-110
Kotova N. and Tuboltsev O. 2013. The Neolithic site Kizlevy 5 in the Dnieper rapids region (Ukraine) (= Atti Della Societá per La Preistoria e Protostoria Della Regione Friuli-Venezia Giulia 18, 2010-211), Trieste: Museo Civico di Storia Naturale, 33-52
Kotova N. S. and Tuboltsev O. V. 1992. Pozdniaya surskaya kul’tura i yeye okruzheniye. Drevnosti Stepnogo Prichernomor’ya i Kryma 3, 8-23
Danilenko V. N. 1974. Eneolit Ukrainy: etnoistoricheskoe issledovanie, Kiev: Naukova Dumka
Bodyanskiy A. V. 1959. Neolitichniy mogilnik bilya Nenasitietskogo poroga, Arkheologiya 5, 163-172
Chernykh Ye. N. 1966. Perviye spektral’niye issledovaniya medi dnepro-donetskoy kul’tury, Kratkiye soobshcheniya Instituta arkheologii AN SSSR, 106, 66-68
Kotova N. S. 2010. Chronology and periodization of the Surskaja Neolithic culture, Studia Archaeologica et Mediaevalia 11, 67-90
Toscev G. N. 2005. Die neolithische Nekropole Mamaj-Gora im unternen Dneprgebiet. Godisnjak 34, 21-39
Borić D., French C. and Dimitrijević V. 2008. Vlasac revisited: formation processes, stratigraphy and dating, Documenta Praehictorica 35, 261-288
Kotova N. S. 2003. Neolithization in Ukraine (= British Archaeological Reports. International Series 1109), Oxford: Archaeopress
Rudinskiy M. Ya. 1956. Pershiy Vovnizkiy pizdnoneolitichniy mogilnik, AP Arkheologichni pam’yatki URSR 6, 152–161
Lillie M., Henderson R., Budd Ch. and Potekhina I. 2016. Factors influencing the Radiocarbon Dating of Human Skeletal Remains from the Dnieper River System: Archaeological and Stable Isotope Evidence of Diet from the Epipaleolithic to Eneolithic Periods, Radiocarbon 58(4), 741-753
Telegin D. Ya., Lillie M. C., Potekhina I. D. and Kovaliukh M. M. 2003. Settlement and economy in Neolithic Ukraine: a new chronology, Antiquity 77 (279), 456-470
Kotova N. S. and Kravchenko S. N. 1992. Noviye neoliticheskiye mogilniki v Nadporozhie. In Neoliticheskiye pamyatniki Stepno Ukrainy, Kiev: Institut Arkheologii Akademii Nauk Ukrainy, 21-26
Lillie M., Budd Ch. and Potekhina I. 2011. Stable isotope analysis of prehistoric populations from the cemeteries of the middle and lower Dnieper Basin, Ukraine. Journal of Archaeological Science 38, 57-68
Lillie M., Budd Ch., Potekhina I. and Hedges R. 2009. The radiocarbon reservoir effect: new evidence from the cemeteries of the middle and lower Dnieper basin, Ukraine, Journal of Archaeological Science 36, 256-264
Telegin D. Ya. and Potekhina I. 1987. Neolithic cemeteries and population in the Dnieper Basin (= British Archaeological Reports. International Series 383), Oxford: Archaeopress
Kotova N. S. 1994. Mariupoloskaya kulturno-istoricheskaya oblast’. In Arkheologichni pamyatki ta istoriya starodavnogo naselennya Ukrainy 1, Kovel: Vezha, 1-143
Telegin D. Ya. 1990. Novyye raskopki poseleniya Kamennaya Mogila v Priazov’ye. In Problemy arkheologii Severnogo Prichernomor’ya (k 100-letiyu osnovaniya Khersonskogo muzeya drevnostey), Tezisy dokladov yubileynoy konferentsii, Kherson, 31-33
Sprawozdania Archeologiczne
Kotova N., Tubоltsev O., Kiosak D., Spitsyna L., Makhortykh S., Tinner W., Nielsen E. H. and Dzhos V. 2017. Preliminary results of excavations at the multilayer Kamyana Mohila 1 site (2011-2012). In S. Makhortykh, A. de Capitani (eds.), Archaeology and palaeoecology of the Ukrainian steppe, Kyiv: Maidan
Danilenko V. N. 1986. Kamyana Mohyla, Kiev: Naukova Dumka
Kotova N. S. 2015. Drevneyshaya keramika Ukrainy, Kiyev, Kharkov: Maydan
Lillie M. C. and Richards M. 2000. Stable isotope analysis and dental evidence of diet at the Mesolithic–Neolithic transition in Ukraine, Journal of Archaeological Science 27, 965-972
Opis:
ill. ; 25 cm
il. ; 25 cm
Comparison of radiocarbon dates for human and animal bones from Neolithic cemeteries of the Dnieper region has demonstrated the necessity of using only the non-human material for determining the ages of these sites. This approach has made significant corrections to the dating of the Neolithic cultures in the Ukrainian steppe from the late 6th to the early 5th millennia calBC. The revision of the chronological position of some Surskoy Culture cemeteries (Vovnigi 3, Vovnigi 1, the first stage of Vilnyanka, the first and second stages of Yasinovatka 1) has resulted in more precise dates than previous estimates (about 5350-4950 calBC), and the latest date of occupation of the Surskoy Culture at sites in this region has likewise been revised to about 4900-4800 calBC. According the correction, period 1b of the Azov-Dnieper Culture is dated at about 5750-4900 calBC. The second peraiod of the Azov-Dnieper Culture should be dated around 4900-4700 calBC
Dostawca treści:
RCIN - Repozytorium Cyfrowe Instytutów Naukowych
Książka
Tytuł:
An integrated approach for landslide hazard assessment: A case study of the Middle Dnieper Basin, Ukraine
Autorzy:
Ivanik, Olena
Fonseca, Joana
Shabatura, Oleksandr
Khomenko, Ruslan
Hadiatska, Kateryna
Kravchenko, Dmytro
Tematy:
Dnieper River basin
electrical resistivity tomography
ERT
infrared thermography
IRT
landslide hazards
Pokaż więcej
Wydawca:
Instytut Technologiczno-Przyrodniczy
Powiązania:
https://bibliotekanauki.pl/articles/2073724.pdf  Link otwiera się w nowym oknie
Opis:
Ukraine is characterised by active natural hazards processes within different structural, tectonic and landscape zones. In Middle Dnieper basin region mass movement processes have great impact on people’s livelihoods and infrastructure. These processes occur on the slopes with different geological structure. The determining causes include lithologic and stratigraphic conditions, hydrogeological regime, structural and textural peculiarities of rocks and the geomorphology of the slopes. Landslide inventory database has been developed based on long-term observations of more than 400 landslides and landslide-prone areas. This paper takes efforts forward by combining different geological and geophysical methods to advance the current understanding of landslide phenomena and contributing towards a better informed assessment of landslide hazard and risk. The developed methodology is implemented in a test sites of Kyiv region, covering an area of 18.3 km2 situated in the Middle Dnieper basin. Electrical Resistivity Tomography, Self-Potential and Infrared Thermography techniques were employed to investigate the lithostratigraphic sequences, the geometry of landslide body and potential mass movement. The results presented here confirm the potential of using an integrated approach that combines different field data to better plan mitigation activities and measures for the effective land management. This study will be useful in increasing the safety aspects of the infrastructures and lives and also for planning of research and developmental activities.
Dostawca treści:
Biblioteka Nauki
Artykuł
Wyświetlanie 1-10 z 35

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