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Journal articles on the topic 'Dniester'

Author: Grafiati
Published: 4 June 2021
Last updated: 3 February 2022

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1

Adamenko, Оleg. "Causes and consequences of floods in the Dniester valley." Visnyk of the Lviv University. Series Geography, no. 48 (December 23, 2014): 141–49. http://dx.doi.org/10.30970/vgg.2014.48.1302.

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Catastrophic floods in r. Dniester led to the creation of the Dniester engineering and ecological flood polygon-model sites in the Dniester within the Galician and Tysmenytsia areas centered on the village Mariyampil Galician region. Based on comprehensive studies of the Dniester area flood polygon possible to develop effective measures to prevent and reduce the negative effects of catastrophic floods and improve environmental security in the region. Key words: flood, flood Dniester ground, geoecological research.
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2

Yatsyshyn, Andriy, and Piotr Gębica. "STUDY OF THE HOLOCENE STAGE OF FORMATION OF THE DNIESTER VALLEY IN THE EASTERN CARPATHIAN FORELAND." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 11(01) (December 2020): 118–39. http://dx.doi.org/10.30970/gpc.2020.1.3204.

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The article describes the main stages of studying of the floodplain and the first floodplain terrace of the Dniester river within the Eastern Carpathian Foreland fragment of the valley, and evaluates the results of existing studies. It is discovered that during all the stages of the research morphological and morphometric parameters of the floodplain and the first floodplain terrace of the Dniester river, morphology and facie structures of the alluvial accumulations, as well as palynological analyses of biogenic accumulations buried in an alluvial series are performed. The results obtained during the palynological analyzes are used to date the erosion-accumulation cycles and to reconstruct the physical-geographical conditions of the time of the floodplain and the first floodplain formation of the Dniester terrace. The radiocarbon dating of biogenic sediments buried in alluvial series is also actively conducted at the last stage of the research. The array of geological and geomorphological information collected at the first two stages of research made it possible to establish that, first, the first floodplain terrace and floodplain were formed during the Holocene in the Dniester Valley. The first floodplain terrace (the height of which reaches 4–6 m above the Dniester riverbed) can be considered as a high floodplain which is often covered by high floods. The terrace is accumulative, but unlike all other terraces of the Dniester it is devoid of the loess cover. In the cross-sections of its accumulations the deposits of the alluvium of the channel facies builted of pebbles are exposed and covered with the alluvium of the floodplain facies composed of sands, sandy loams and loams. The total thickness of alluvium reaches 9–10 m and it doesn’t varysignificantly downstream of the Dniester. Except the Upper Dniester basin, where the thickness of the alluvium increases to 10–18 m, and the layers of peat are found. The floodplain is 4–5 m above the Dniester riverbed and is built of alluvium of the channel facies, dominated by sand and pebble series. In someplaces floodplain is covered with sandy or loamy deposits of floodplain facies. Secondly, in the Eastern Carpathian Foreland part of the Dniester valley the course of fluvial morpholitogenetic processes was regulated not only by climatic changes and neotectonic movements, but also by human economic activity. During the XIX–XX centuries especially large-scale human influence was on the Dniester riverbeds by construction of flood ramparts, reclamation canals, etc. The results of recent geomorphological research conducted within the studied fragment of the river valley particularly palynological and radiocarbon dating have significantly improved the idea of morphology, structure and history of floodplain formation and the first floodplain terrace of the Dniester. The research revealed that the accumulation of alluvium of the first floodplain terrace which is above the Dniester riverbed reaches 5,5–6,5 (7) m and started to develop in the late Pleistocene (Bølling–Allerød interstadial) (13 000–11 000 years ago (GI–1)). Presumably in the early Dryas (11 000–10 000 years ago (GS–1)), the first floodplain terrace was dissected by the meandering channel of the Dniester. The alluvial deposits that fill these large paleomeanders are still well preserved and are often exposed in the ledges of the first terrace. The further development of the floodplain and first floodplain terrace of the Dniester river was taking place in several stages such as the end of the boreal, the beginning of the atlantic, the end of the atlantic, subboreal, the beginning of the subatlantic, as well as during V–VI, X–XII and XIV–XVI centuries. These stages are identified in correlation with the cycles of humidification of the climate and the growth of fluvial activity of riverbeds (flood phases). As a result of the intensification of erosion-accumulation activity of the Dniester the two – three levels of Holocene floodplain were formed up to 4–5 m and 3–4 m high. The first traces of human activity within the studied fragment of the Dniester valley were dated by subboreal and recorded by the presence of grain pollen in the spore-pollen diagrams of Mainych (Upper Dniester Basin) and Tsvitova (Galician-Bukachiv Basin) sections. Key words: Dniester valley; floodplain; the first floodplain terrace; alluvium; phases of floods; Allerød; early Dryas; Holocene.
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3

Gazyetov, Ye І., V. І. Medinets, S. M. Snigirov, N. V. Kovaleva, and S. V. Medinets. "HYDROLOGICAL CHARACTERISTICS OF THE DNIESTER ESTUARY BY SURVEYS IN THE SUMMER’S OF 2003–2019." Odesa National University Herald. Geography and Geology 26, no. 1(38) (September 4, 2021): 28–42. http://dx.doi.org/10.18524/2303-9914.2021.1(38).234645.

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Problem Statement and Purpose. The Lower Dniester delta and the Dniester estuary are very important because they are natural filters of the river water from pollution and suspended matter, as well as they are the habitat of a large number species of flora and fauna. The construction of reservoirs on the Dniester River in past completely changed the hydrological regime of the river itself and of the Dniester estuary. For these reasons a constant environmental monitoring of the aquatic environment are required. Since 2002 Odessa I. I. Mechnikov National University has been carrying out a wide range of environmental studies in the Dniester estuary, one of aspects of which is observation of hydrological characteristics. The purpose of this paper is to study long-term changes in transparency, temperature and electrical conductivity of the Dniester estuary water in the summer periods of 2003–2019. Materials & Methods. Measurements of transparency, temperature and electrical conductivity of water in the Dniester estuary in the indicated years were carried out according to standard methods at 19 ecological stations. Statistical processing, analysis and mapping of the measurements results were conducted in EXCEL, ARCGIS, SURFER software’s. Data analysis was based on a graphical representation of the spatial distribution of characteristics, as well as by identifying the features of long-term changes in these characteristics. Main Results and Conclusions. On the basis of the summer surveys during 2003–2019 more than double decrease of water transparency mean values in the Dniester estuary has been established. It was found that the maximum transparency values were observed in the central parts of the estuary, far from settlements. For theseyears, an increase of the mean water temperature for the estuary northern part and its decrease in the middle and southern parts has been recorded. Also, for the summer period of these years, an increase of the mean water electrical conductivity in all parts of the estuary was established. The established features of spatial distribution of hydrological characteristics indicate to the river runoff, intrusion of seawater into the estuary, and wind activity as the determining factors in formation of the estuary hydrological regime. Recorded long-term trends of the means transparency values decreasing and the means temperature and electrical conductivity increasing of the Dniester estuary water in the summer of 2003–2019 are considered as consequences of the river discharge decreasing due to long-term climatic changes over Europe and man regulation of river flow.
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4

Tomeniuk, O. "Yuriy Polians’kyi as a researcher of terraces of Dniester river." Visnyk of the Lviv University. Series Geography, no. 38 (December 15, 2010): 340–56. http://dx.doi.org/10.30970/vgg.2010.38.2287.

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Yuriy Polians’kyi’s contribution to the investigation of geologic and geomorphologic structure of Dniester River on the basis of detailed analysis of his scientific publications was characterized. Works of the scientists who were the predecessors and the successors of Yuriy Polians’kyi in the field of study of terraces of Upper and Middle currents of Dniester River also was analyzed. The principal achievements of Yuriy Polians’kyi that have got the further development in present geomorphology were corroborated at the article. Key words: floodplain terrace, alluvium, Pleistocene, relative elevation, geological and geomorphological researches, Dniester, Podillya.
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5

A. Chebanova, Lydia, Lyudmila A. Novikova, Lyudmila K. Ushakova, and Irina A. Karnilovi. "Migration Processes in the Trans-Dniester Region of the Republic of Moldova and Their Impact on the Socio-Economic Situation." International Journal of Engineering & Technology 7, no. 3.15 (August 13, 2018): 226. http://dx.doi.org/10.14419/ijet.v7i3.15.18677.

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The purpose of the study is revealing the content and causes of migration processes in Trans-Dniester Region and their impact on the socio-economic situation in the region. From this perspective the main objectives of the study consisted in disclosing the reasons of considerable population outflow over the past two decades, the study of the peculiarities of different forms of migration in Trans-Dniester Region, identifying trends in migration of population, regulation of the migration mechanism at the present stage, the assessment of the current system of migration flows accounting in Trans-Dniester Region and the definition of its optimization directions. Particular attention is paid to the consideration of the migration scale and the main areas of emigration. The loss of immigration attractiveness of the region and outflow of highly qualified young and active population from Trans-Dniester Region causes a steady reduction in the population, creates a significant imbalance in the demographic structure of the population (in terms of age and profession). Besides, the Trans-Dniester Region turned out to be actively involved in migration processes due to its relative geographical proximity to both Russia and the EU countries. Currently, the predominant role is played by labor migration.
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6

Brusak, Vitaliy, and Sofia Paljanycja. "Non-living nature monuments of Halych-Dniester region: state of protection and perspectives of geotouristic application." Visnyk of the Lviv University. Series Geography, no. 47 (November 27, 2014): 30–41. http://dx.doi.org/10.30970/vgg.2014.47.814.

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The list of non-living nature geological, geomorphological, hydrological monuments of Halych National Park in Halych-Dniester region is submitted in this article and its current state of protection is characterized. The opportunities of application of non-living nature monuments in recreation and tourism activities of Halych National Park are analyzed. The network of one-day and multi-day geotouristic trails are developed. The perspectives of creation of National geopark “Halych-Dniester region” are regarded. Key words: monuments of non-living nature, geological, geomorphological and hydrological monuments of nature, geotouristic trails, National geopark, Halych-Dniester region, Halych National Park.
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7

Bosatikova, Nadezhda. "Summer in the Trans-Dniester." Index on Censorship 22, no. 4 (April 1993): 16–18. http://dx.doi.org/10.1080/03064229308535542.

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8

Kravchuk, Yaroslav, and Yuriy Zinko. "STEPAN RUDNITSKY'S STUDIES OF THE PODILLYA RELIEF: ITS MORPHOLOGY, GENESIS AND HISTORY OF DEVELOPMENT." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 09 (01) (September 25, 2019): 3–20. http://dx.doi.org/10.30970/gpc.2019.1.2796.

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S. Rudnitsky’s research continued in Podillya; he went on studying the morphology of genesis and history of the relief of the Carpathian and pre-Carpathian Dniester basins. Many years of expeditionary research (1903-1912) resulted in the monograph “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester”, which was recommended for publication at the meeting of the Mathematical & Nature Descriptive section of the Shevchenko Scientific society (NTSh) on April 17, 1912. This work provides detailed morphographic and morphometric characteristics of the Galician Podillya relief. The monograph also reports on the formation of the Dniester basin river system, geological structure, paleogeomorphology, as well as morphological & genetic problems. In studying the Podilsky Dniester Basin, S. Rudnytsky made numerous conclusions on the problems of morphological regionalization, the relief history, in particular the formation of the Dniester valley and its Podilsky tributaries, which have not lost their relevance to this day. We can distinguish the following major points among the main findings of S. Rudnitsky's research of morphogenesis and the evolution of the Podilsky Dniester basin relief: (1) Geomorphological division of the Galician Podillya with districts allocation: Roztochya, Vereshchytsky-Shchyrets lowland, Mykolayiv-Bobretskyi “horbovyna” (land surface with hills) (Pidopillya), Opilsky “horbovyna”, Podnistriya, Podillya and Gogoloro-Kremenetsk Ridge; (2) Clarification of the history of individual regions development: the erratic Scandinavian material in Roztochya is mixed (Scandinavian-Carpathian); it is deposited by fluvia-glacial flows and represented up to altitudes of 380 m; (3) In the periglacial Pleistocene period, almost all the sands of the main areas had eolian processes; (4) Confirmation of the Podillya geological division into western and eastern with five morphological bands, proposed by W. Teisseyre; (5) Justification of the morphotectonic scheme of Podillya development, connected with tectonic elevations of the Hologoro-Kremenets Ridge, which caused the current inclination of the Podolsk hills to Southeast-East; (6) Statement that the tectonic lines of Berdo-Nârul and Kovalivka-Smykivtsi characterize the Paleozoic Platform of Podillya as a typical tectonic horst; (7) Detailed description of the Dniester “rinyshcha” (alluvial deposits) with the Carpathian material present in Podniester, Opil and Podillya itself, which are present as a strip at a distance of 14-20 km from the modern Dniester river bed; (8) Based on literary sources and his own research, the scientist came to the conclusion that there is “eolian” loess in the “rinyshcha”, sands and alluvial clay; (9) It is argued that the old Nadnistryan rivers cannot be older than the planation surfaces of the Carpathians and Pre-Carpathians; (10) Formation of the Dniester valley pattern in Pliocene and Pleistocene, which determined the direction of the flows of the left tributaries and their capture by the Western (Zakhidny) Bug river sources. Finally, in his “Prerequisites for Studying Morphology of the Podilsky Catchment Area of the Dniester” S. Rudnitsky managed to use a complex morphogenetic approach to studying the region relief for the first time geomorphological literature: from standardized morphological descriptions through systematization of the morphological structure of the region to the historical genetic interpretation of the main features of relief morphology. Key words: morphological districts; Dniester catchment area (basin); Naddnistriansky “rinyshcha” (alluvial deposits); glacial erratic material; fluvia-glacial deposits; free and entrenched meanders; “horbovyna” (land surface with hills); Podillya.
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9

Jacyshyn, A. "The principal stages high pliocene and low pleistocene morpho and lithogenesis of the Dniester basin in the Halician Dniester region." Visnyk of the Lviv University. Series Geography, no. 38 (December 15, 2010): 379–94. http://dx.doi.org/10.30970/vgg.2010.38.2290.

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The principal stages of high Pliocene and low Pleistocene history of the Dniester basin development in Halicia and Ivano-Frankivsk region on the basis of the detailed morphological, morphometric analysis of the Dniester terraces as well as its Carpathian streams and the analysis of cut terraces. The fundamental geomorphological research of Loyeva, Krasna rivers levels has been done and some determined provisions about their structure, development and time of formation were defined. Paleogeographic events are related with the stages of isotopic-oxygen scale, paleomagnetic rappers, stratigraphic horizons of loess and soil series of the Halician Dniester region. Key words: level of Krasna river, level of Loyeva river, terrace, isotopic-oxygen stage, tectonic raising, erosive cutting, alluvium accumulation.
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10

Yatsyshyn, Andriy, Maciej Bąbe, Danuta Olszewska-Nejbert, Andriy Bogucki, and Kateryna Dran. "Lithological characteristics of the alluvium of the seventh terrace of the Dniester River in the Kunysivtsi and Ivane-Puste sections (Podillia-Dniester region)." Visnyk of the Lviv University. Series Geography, no. 42 (October 15, 2013): 367–78. http://dx.doi.org/10.30970/vgg.2013.42.1897.

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The main lithological characteristics of the sands, gravels and pebbly deposits in the particular layers of the seventh terrace of the Dniester River in the investigated part of its Podillian valley have been analyzed. The texture and the granulometrical and petrographical composition of the sands, gravels and pebbly materials has been described, including the roundness of the grains and some other features. The conditions of sedimentation of the alluvial sands, gravels and pebbly deposits of the seventh terrace of the Dniester River have been reconstructed and direction of the palaeo-Dniester flow and some other features interpreted. Key words: terraces over the canyon, alluvium, granulometrical composition, petrographical composition, sandstone, aleurolite, quartz, siliceous rocks, roundness.
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11

Strutsinska, Olena. "Landscape and soils of coastal areas of Dniester estuary." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2014): 344–55. http://dx.doi.org/10.30970/vgg.2013.44.1242.

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This article reveals landscape and soils characteristics of coastal areas of the Dniester estuary. Peculiar emphasis is made on the connection established between landscape- and soil formation processes and composition of soils allocated on different hypsometric levels of “coast-to-shore” zone of the estuary. Key words: Dniester estuary, coast-to-shore zones, landscape, soil formation, soils.
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12

Chernyavskyy, M., and P. Telish. "Geographic aspects of optimization forests of Upper Dniester Beskids on close to nature forestry." Visnyk of the Lviv University. Series Geography 2, no. 40 (December 12, 2012): 224–36. http://dx.doi.org/10.30970/vgg.2012.40.2114.

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Proved system of measures aimed at the reconstruction of the derivatives forest Upper Dniester Beskydy. Within the high-altitude forest zones and high-altitude landscape areas the tree stands options, targeted measures to approximate the natural forest and the recommended methods of felling have been proposed. Key words: Upper Dniester Beskids, high-altitude forest zones, forest harvesting methods, the target stands.
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13

Adamenko, Oleg, Denis Zorin, Natalia Zorina, and Kateryna Radlovska. "GEOECOLOGICAL STATE OF BISTRIZA-TLUMACH’S AND PRYDNIESTER-POKUTSKIY HIGHLIGHTS." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRANIAN CARPATHIANS AND ADJACENT AREAS, no. 09 (01) (September 25, 2019): 21–33. http://dx.doi.org/10.30970/gpc.2019.1.2800.

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Abstract. The anthropogenic environmental changes over the past decade have become global for the entire globe. They deeply penetrate into all components of the environment - the lithosphere, the geomorphosphere, the hydropower and the atmosphere, the soil and vegetation, alter the physical fields of the Earth and the Cosmos, transforming the original natural landscapes into natural and human-made geosystems and endangering human health and life. Especially sensitive to changes are the least protected natural landscapes on the territories of the nature reserve fund - natural monuments, nature reserves, regional parks, national natural parks, natural and biosphere reserves. The article deals with the issues of technogenic influence on the part of the territory of the Dniester Regional Landscape Park - Bistriza-Tlumach’s and Prydniester-Pokutskiy hills of the Prut-Dniester interfluve in Ivano-Frankivsk region. The authors carried out an ecological assessment of the environmental components of the specified territory - geological environment, relief, hydro- and atmosphere, soil and vegetation cover. Recommendations on the reduction of anthropogenic influence by introducing geoinformation technology of environmental protection, its modeling and forecasting are offered. Most of the study area has a generally normal ecological status. There are favorable conditions along the Dniester Canyon, where the oxygen content in the atmospheric air is higher than the average. Within a short distance of the Dniester Canyon from the north-west to the southeast, lanes of satisfactory condition stretch. Within them, five sites of complex ecological status have been identified. The comparison of the obtained data of the ecological assessment of the heights on the right riverside with the adjacent territory on the left riverside of the Dniester – located there National Nature Park “Dniester Canyon” showed that practically all geo-ecological structures of the right bank have their continuation on the left riverside. It follows that the Dnistrovsky Regional Landscape Park should be transferred to the category of nature reserve fund “National Nature Park” and be combined with the National Park “Dnistrovsky Canyon”. Keywords: environmental assessment; geoecological state; environmental components; inter-rivers; hills; anthropogenic influence; GIS-technologies.
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14

Telish, Pavlo. "Structure of forests fund of regional landscape park “Upper-Dniester Beskids”, it anthropogenic transformation and ways to optimization." Visnyk of the Lviv University. Series Geography, no. 42 (October 15, 2013): 342–49. http://dx.doi.org/10.30970/vgg.2013.42.1889.

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The present structure of the forest fund of regional park “Upper-Dniester Beskids” for the purpose of selecting of the optimal mode use of forest resources was investigated. Intensive forest management during the twentieth century led to adverse changes in the structure of the forest fund of landscape park. Distribution of forest of park by protection category and land category was analyzed. Species composition and age structure of forests of regional landscape parks were clarified. The degree of anthropogenic transformation of forest of park was identified. Optimization measures which should be carried out on the basis of functional zoning of the regional landscape park “Upper-Dniester Beskids” were proposed to improve the modern structure of the forest fund. Key words: regional landscape park “Upper-Dniester Beskids”, structure of forest fund, anthropogenic transformation, ways to optimization.
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15

Bogucki, A., R. Dmytruk, and I. Dumas. "Natural environments of period of the formation of Dubno paleosoil in Halych-Dniester region." Visnyk of the Lviv University. Series Geography, no. 39 (November 15, 2011): 35–43. http://dx.doi.org/10.30970/vgg.2011.39.2160.

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In the article have been suggested the analysis of main lithology-petrography characteristics of Dubno paleosoil complex in Halych-Dniester region. The natural environments of period of the formation of paleosoil have been reconstructed, based on mollusc fauna analysis. The analysis of correlation between the cultural layers Upper Palaeolithic and Dubno paleosoil complex and also solifluction layers complex has been provided. Key worlds: paleosoil, Halych-Dniester region, Palaeolithic, solifluction, molluscs fauna.
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16

Kolisnyk, A. V. "Current situation of water quality Dniester River basin in transboundary areas." Ukrainian hydrometeorological journal, no. 16 (October 29, 2017): 202–8. http://dx.doi.org/10.31481/uhmj.16.2015.27.

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Introduction. Today there are significant problems of transboundary pollution of the Dniester River basin in Ukraine, including within the Vinnitska oblast. Purpose. The aim is to assess the current state of the watercourses of the Dniester River basin in transboundary areas with the Republic of Moldova, within the Vinnytska oblast by 2013. Methods. Evaluation of current watercourses quality in Dnister basin was performed based on the Methodology of environmental assessment of watercourses quality for the relevant category and on the Methods integrated assessment of groundwater contamination. Results. The results of water quality evaluation of the river Dniester basin in cross-border areas are assigned to them "satisfactory" and "bad" (the average and maximum environmental indices) features state and "dirty" and "dirty" qualifications purity by the Method of environmental assessment of watercourses quality in the relevant categories. By the Method of integral estimation of water courses contamination within the basin of river Dnister in Vinnytska oblast contamination status changed from "harmless" to "intensive". This shows a significant contamination of the river Dniester water basin. Conclusion. In order to improve the ecological state of the river basin it is necessary to conduct comprehensive monitoring of rivers, set GDS the priority given indicators of water quality, improve the culture of land and water use in watersheds. Priority execution of these measures should be in parts of the basin, characterized by the worst quality. Improvement of the situation with river Dnister basin in the cross-border region with Republic of Moldova should only be done on the state level with help of Euroregion "Dniester" initiative.
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Sinika, Vitalij Stepanovich, Nikolai Petrovich Telnov, and Oksana Alexandrovna Zakordonets. "Scythian barrow № 4 of the «Sluiceway» group on the left bank of the Lower Dniester." Samara Journal of Science 6, no. 2 (June 1, 2017): 108–13. http://dx.doi.org/10.17816/snv201762203.

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The paper publishes materials obtained during the study of Scythian barrow 4 of the Sluiceway group on the left bank of the Lower Dniester in 2016. The main burial, almost completely robbed in antiquity, was surrounded by a ring ditch with two ruptures - in the northwest and southeast. At the western extremity of the northern arch of the ditch a horses skull was found. Secondary burial of the barrow remained undisturbed. It was done in an oblong pit. Such constructions have not been fixed in the Danube-Dniester steppes so far, except for a pit of similar proportions, excavated in the barrow 5 of the same cemetery as the published complex. The analysis of the funeral rite and a few preserved inventories demonstrates that both burials belonged to ordinary members of the Scythian community. At the same time, the gold holder and bronze earring from the secondary burial have practically no analogies in the Scythian complexes of the steppes of the North-Western Black Sea Region. A nail-shaped earring from the secondary grave testifies to the cultural impulse from the population of the Middle Dniester Region (forest-steppe), reflected in the finery of the Scythians on the left bank of the Lower Dniester in the second half of the 4th century BC.
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18

Burshtynska, K., V. Shevchuk, S. Tretyak, and V. Vekliuk. "MONITORING OF THE RIVERBEDS OF RIVERS DNIESTER AND TISZA OF THE CARPATHIAN REGION." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B7 (June 21, 2016): 177–82. http://dx.doi.org/10.5194/isprsarchives-xli-b7-177-2016.

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The paper analyses the causes of riverbed shifts of the rivers Dniester and Tisza of the Carpathian region. Among these reasons are mostly climate, physical and geographical, and anthropogenic factors, including frequent floods, weak rocks and soils, logging, and removal of gravel and sand materials out of the channels. The research considers the transition of the Dniester and Tisza rivers from mountaineous area into the lowland. The analysis of these shifts has been carried out on the 100 km long sections over a 100-year period. We used topographic maps and space images, as well as special geological and soil maps, as materials for this research. We have determined that the shifts of the Dniester and Tisza riverbeds can reach up to 500-1000 m in some sections. We also analyze the risks and dangers that follow such shifts.
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Burshtynska, K., V. Shevchuk, S. Tretyak, and V. Vekliuk. "MONITORING OF THE RIVERBEDS OF RIVERS DNIESTER AND TISZA OF THE CARPATHIAN REGION." ISPRS - International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLI-B7 (June 21, 2016): 177–82. http://dx.doi.org/10.5194/isprs-archives-xli-b7-177-2016.

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The paper analyses the causes of riverbed shifts of the rivers Dniester and Tisza of the Carpathian region. Among these reasons are mostly climate, physical and geographical, and anthropogenic factors, including frequent floods, weak rocks and soils, logging, and removal of gravel and sand materials out of the channels. The research considers the transition of the Dniester and Tisza rivers from mountaineous area into the lowland. The analysis of these shifts has been carried out on the 100 km long sections over a 100-year period. We used topographic maps and space images, as well as special geological and soil maps, as materials for this research. We have determined that the shifts of the Dniester and Tisza riverbeds can reach up to 500-1000 m in some sections. We also analyze the risks and dangers that follow such shifts.
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Romanchuk, A., and N. Romanenko. "Intercultural Communication in the Carpathian-Dniester Region during the Early Hallstatt Period." Scientific Research and Development. Modern Communication Studies 9, no. 4 (August 3, 2020): 31–34. http://dx.doi.org/10.12737/2587-9103-2020-31-34.

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The article considers some issues of intercultural communication in the between archaic societies of the Carpathian-Dniester region. Using the method of comparative-historical analysis the authors examine the nature and characteristics of affiliate networks, which served as the basis for intercultural communication in the Early Hallstatt period (XII-X centuries B.C.). One of the factors that determined the complexity and non-linearity of the processes of intercultural communication is location of the Carpathian-Dniester region at the crossroad of several “cultural worlds”. The authors stress that although archeological data confirm the presence of intercultural communication, it was not accompanied by the movement of actual material objects, ceramics itself, between the cultures. Accordingly, this requires a search for mechanisms that explain the processes of intercultural communications in the archaic societies of the Early Hallstatt period of Carpathian-Dniester region.
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Kovalchuk, О. М., V. A. Marareskul, D. S. Zakharov, and T. F. Obadă. "Early Pliocene Sturgeons and Bony Fishes from the Dniester Valley (Republic of Moldova) / Осетровые и костистые рыбы раннего плиоцена из долины Днестра (Республика Молдова)." Vestnik Zoologii 49, no. 1 (February 1, 2015): 49–56. http://dx.doi.org/10.1515/vzoo-2015-0005.

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Abstract A fossil fish remnants from the Early Pliocene strata of the Dniester valley (Republic of Moldova) are described in the paper. Seven species, belonging to 6 genera, 4 families and 4 orders (Acipenseriformes, Cypriniformes, Siluriformes, Esociformes) were identified in Nikolskoe and Uyutnoe localities. All of them are analogues of extant taxa. A brief review of development of the freshwater fish fauna in the Lower Dniester Basin during the Early Pliocene is presented.
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Simonenko, Sergey Olegovich. "New Sarmatian grave on the left bank of the Lower Dniester." Samara Journal of Science 8, no. 3 (August 5, 2019): 173–78. http://dx.doi.org/10.17816/snv201983210.

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In 2018, a secondary Sarmatian burial with an impressive inventory (molded pot, pottery jug, silver earring, necklace of beads) was discovered in the Scythian mound in the course of the study of the barrow group Garden near the Glinoe village, Slobodzeya region, on the left bank of the Lower Dniester. Orientation of the buried head to the south-southeast is quite rare in the North-West Black Sea region. The cult of fire is fixed by the finds of three burned pebbles from the left to the head. A handmade pot combines features known for the dishes of a given cultural and chronological period. At the same time, the wave-like ornament in the upper part of the body was fixed only once on a similar vessel in the Danube-Dniester interfluve. Of particular interest is a pottery jug from the complex. Such forms were not previously known in the North-West Black Sea region. The closest analogies to the vessel come from the sites of the Volga-Don interfluve. Earrings identical to those found in the published grave are widely represented in the materials of the Prut-Dniester interfluve, the Middle and Lower Dniester. Necklaces of various shapes and beads belong to the most mass material received by the Sarmatians from ancient centers. The burial dates back to the 2nd century based on the analysis of the grave goods.
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Bacal, Petru, and Nicolae Boboc. "Economic and Financial Aspects of Water Management in the Dniester Basin (The Sector of the Republic of Moldova)." Present Environment and Sustainable Development 9, no. 1 (May 1, 2015): 33–45. http://dx.doi.org/10.1515/pesd-2015-0002.

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Abstract The main topics presented in this paper are following:1 Essence and the tools of the economic mechanism of management of water resources; 2 Taxes on water consumption; 3 Tariffs for services of water supply and sewerage; 4 administrative penalties for infringements of use and protection of water resources; 5 The grants for the rational use and protection of water. In the Dniester Basin have been concentrated the majority of water resources, of urban, industrial and agricultural centers. Thus, this basin holds over 90% of water consumption, most of which are captured from surface sources and used by industrial enterprises from the left bank of Dniester, especially by Thermoelectric Plant (TEP) from Dnestrovsk. On the right bank of Dniester it is noted communal enterprises, agricultural and food industry, and in most of the localities water is captured from groundwater sources. Actual amount of water tax is very low, which conditioned the increased of water consumption and irrational use of these limited resources
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Boiko, A. I., O. V. Lobodzinskyi, and О. I. Lukіanets. "СALCULATED CHARACTERISTICS OF THE AVERAGE ANNUAL RUNOFF OF THE RIGHT-BANK AND LEFT-BANK PARTS OF THE RIVER BASIN DNIESTER TO THE CITY OF ZALISHCHYKY." Hydrology, hydrochemistry and hydroecology, no. 3 (58) (2020): 58–72. http://dx.doi.org/10.17721/2306-5680.2020.3.6.

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The Dniester River is the second longest and most watery river in Ukraine, which is characterized by heterogeneity and diversity of conditions for the formation of water flow, both in terms of its length and numerous tributaries. The right-bank and left-bank parts of the Dniester River basin are quite different in terms of physical and geographical conditions, drainage network density, water regime and river water content. The object of the study is the average annual water flow of the rivers of the Dniester River basin, the subject is its calculated characteristics of different probabilities of exceeding. The purpose of the study is to analyze, systematize, generalize and compare the calculated characteristics of the average annual water flow of rivers of the right-bank and left-bank parts of the Dniester basin. Input data is based on the average annual river water discharge from 50 stream flow measuring stations in the Dniester River basin (to Zalishchyky). The data bank was formed from the beginning of observations until 2016. 89% of 28 right-bank stream flow measuring stations have a continuous series of more than 50 years, and 86% of 22 left-bank stream flow measuring stations have a continuous series of observations of more than 50 years. As for the catchment areas of rivers in the closing areas, the right bank is dominated by small ones – 64% of 28 stations have an area of less than 500 km2 and 25% – from 500 to 1,000 km2. 37% of 22 stations on the left bank have a catchment area of less than 500 km2 and 41% – from 500 to 1,000 km2. According to statistical criteria, the series of observations of the average annual river water discharge in both parts were mainly homogeneous and representative. Analytical distribution curves were calculated by the method of moments, as the coefficients of variation do not exceed 0.50. Generalization and comparison of the calculated characteristics of the average annual water flow of different probabilities of exceeding the rivers of the right-bank and left-bank parts of the Dniester basin have shown that the smallest scatter of certain analytical ordinates is observed for the probability of exceeding 50%, the transition coefficients from the norm are close to 1. The greatest spread of variation of ordinates is observed at extreme probabilities of excess of distributions, that is 0,01 % and 99 %. Analysis of the ranges of variability of transition coefficients from the norm of average annual water consumption has shown that the intensity of their change in the region of rare probabilities (0.01, 0.1, 1 %%) on the left bank is more significant than on the right bank of the Dniester basin. As for low-water supplies (95, 97, 99 %%), their ranges of variability coincide in both studied parts.
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Snigirov, Sergii, Yuriy Kvach, Oleksandr Goncharov, Roman Sizo, and Sergiy Sylantyev. "Hydrology and parasites: What divides the fish community of the lower Dniester and Dniester estuary into three?" Estuarine, Coastal and Shelf Science 217 (February 2019): 120–31. http://dx.doi.org/10.1016/j.ecss.2018.11.022.

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26

Yatsyshyn, Andriy, Maciej Bąbe, Danuta Olszewska-Nejber, Andriy Bogucki, and Stephania Vas’kiv. "Lithological and sedimentological characteristics of the alluvium of the sixth terrace of the Dniester river (Loyeva level) in the Torhanovychi 2 section." Visnyk of the Lviv University. Series Geography, no. 41 (September 17, 2013): 382–95. http://dx.doi.org/10.30970/vgg.2013.41.2011.

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The main lithological characteristics of the alluvium of the sandy-gravelly bed of the sixth terrace of the Dniester river (Loyeva level) at environs of Sambir was analysed, in particular textural elements, granulometric and petrographic composition of the gravelly material (enclosing coarse sands, granules, pebbles, cobbles and boulders), its roundness, and the orientation of grains. The conditions of sedimentation of the studied alluvial sandy-gravelly bed of the sixth terrace of the Dniester river (Loyeva level) were reconstructed. Key words: granulometric composition, petrographic composition, roundness, sorting, imbrication, braided channel, depositional conditions.
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Konstantynenko, L. "ORDOVICIAN STRATIGRAPHY OF THE NEAR-DNIESTER REGION." Tectonics and Stratigraphy, no. 38 (December 8, 2011): 42–50. http://dx.doi.org/10.30836/igs.0375-7773.2011.92230.

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28

Gladchi, V., Gh Duca, N. Goreaceva, E. Bunduchi, and A. Lis. "Chemical Composition from the Dniester River Tributaries." Chemistry Journal of Moldova 8, no. 1 (June 2013): 23–32. http://dx.doi.org/10.19261/cjm.2013.08(1).03.

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29

Koroleva, E. A. "Paleolithic art of the carpathian-dniester region." Archaeology, Ethnology and Anthropology of Eurasia 39, no. 1 (March 2011): 34–42. http://dx.doi.org/10.1016/j.aeae.2011.06.004.

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30

Kolstø, Pål, Andrei Edemsky, and Natalya Kalashnikova. "The Dniester conflict: Between irredentism and separatism." Europe-Asia Studies 45, no. 6 (January 1993): 973–1000. http://dx.doi.org/10.1080/09668139308412137.

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31

Levitski, O. G., and L. V. Sîrbu. "CONSIDERATIONS ON THE CURRENT STATE OF ART AND PRIORITIES IN THE STUDY OF THE CHIŞINĂU—CORLĂTENI CULTURE OF THE CARPATHIAN-DNIESTER AREA (the 12th—10th Centuries BC)." Archaeology and Early History of Ukraine 27, no. 2 (June 22, 2018): 458–68. http://dx.doi.org/10.37445/adiu.2018.02.35.

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The study gives a brief presentation of the history of research of grooved Hallstatt culture of the Carpathian-Dniester area represented by a local variant called Chişinău—Corlăteni, and the current state of art of knowledge of the main cultural. A special attention is paid to the achievements in studying of general issues of the Early Hallstatt period in the Carpathian-Dniester region. The final part of the study proposes more specified directions of research in the present domain taking in consideration the actual debated questions on Chişinău—Corlăteni culture, among which problems of genesis, evolution, and historical destiny of the culture bearers could be mentioned.
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32

Ivanova, Svetlana V., and Gennadiy N. Toschev. "The Middle-Dniester Cultural Contact Area of Early Metal Age Societies. The Frontier of Pontic and Baltic Drainage Basins in the 4Th/3Rd-2Nd Millennium Bc." Baltic-Pontic Studies 20, no. 1 (June 1, 2015): 337–406. http://dx.doi.org/10.1515/bps-2017-0008.

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Abstract The paper discusses the taxonomy and autogenesis of the cycle of early ‘barrow cultures’ developed by the local communities of the Middle Dniester Area or, in a broader comparative context, the north-western Black Sea Coast, in the 4th/3rd-2nd millennium BC. The purpose of the study is to conduct an analytical and conceptual entry point to the research questions of the Dniester Contact Area, specifically the contacts between autochthonous ‘Late Eneolithic’ communities (Yamnaya, Catacomb and Babyno cultures) and incoming communities from the Baltic basin. The discussion of these cultures continues in other papers presented in this volume of Baltic-Pontic Studies.
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Greben, V., and K. Mudra. "USE OF A REGIONAL CLIMATE MODEL (REMO) FOR WATER FLOW TRENDS EVALUATION IN THE DNIESTER RIVER BASIN." Bulletin of Taras Shevchenko National University of Kyiv. Geography, no. 70-71 (2018): 22–28. http://dx.doi.org/10.17721/1728-2721.2018.70.4.

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In order to confirm the possibility of predictive climate models using for the flow modelling in the Dniester river basin, the REMO climate model was verified. The verification was carried out on the basis of comparison of the simulated values and data from the hydrological observation network. The data of 28 hydrological stations on the Dniester and its tributaries were used. The reference period for testing the model was from 1971 to 2000. In total, 11 136 values of the average monthly and 917 values of the average annual water flow were used. According to the results of the conducted research, it was found that in most cases, the average annual flow value, taken from the model REMO, is lower, compared with the data from the hydrological observation network. The mean annual flow in the Dniester basin according to the hydrological observation network is 9.25 l/s∙km2, based on the model REMO – 8.27 l/s∙km2. In order to reduce the deviations of the predicted values, it was proposed to use a correction factor, it can reduce the percentage of deviations from the measured values by half. The assessment of the relationship between the data from the hydrological observation network and model values was carried out on the basis of determining the coefficient of pair correlation with the subsequent calculation of the regression equation. It was found that the correlation coefficient for a pair of data of the average long-term value – measured and model – is close to 1, which confirms the possibility of modelling not only for certain designated areas but also for individual hydrological stations. This research shows that the model REMO reliably predicts water flow changes in the Dniester river basin, taking into account the peculiarities of flow formation in different parts of the studied basin.
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KOST’, Maria, Halyna MEDVID, Vasyl HARASYMCHUK, Olga TELEGUZ, Iryna SAKHNYUK, and Orysia MAYKUT. "Geochemical characteristic of river and ground waters (Outer zone of the Precarpathian deep)." Geology and Geochemistry of Combustible Minerals 1, no. 182 (January 23, 2020): 76–86. http://dx.doi.org/10.15407/ggcm2020.01.076.

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Geochemical peculiarities of river and groundwaters of the Outer zone of the Precarpathian deep have been established. It is revealed that the main feature of the distribution of salt composition indicators in the Dniester River and its influxes is hydrochemical zonality, which does not depend on the flow direction of the rivers, but is consistent with the physics-geographical and geological features of the area to which the man-made factor is imposed. There is an increase in concentrations of sulfate, calcium in the left bank confluent of the river Shchyrka. The waters from the Tysmenytsya, Kolodnitsa and Dniester rivers in the village Kolodrubi are characterized by the highest amounts of sodium and chlorides and are sodium chloride-hydrocarbonate composition. The water composition of the Dniester River (Rozvadiv village), its confluents Bystrytsia and Letnyanka are hydrocarbonate calcium (sodium-magnesium-calcium), Shchyrka, Vereshchitsa – sulfate-hydrocarbonate calcium (magnesium-calcium). The index of biochemical oxygen consumption for 5 days in the waters of Tysmenytsya River reached 4.5 mg O2/dm3, while in other rivers it was 0.70‒3.20 mg O2/dm3. The content of O2 soluble in the waters of the river Vereshchytsya was 0.29 mg/dm3, the value of biochemical oxygen consumption was 11.4 mg O2/dm3. In the chemical composition of river waters, there is an increase in the concentrations of sodium, potassium and chloride ions from the left bank to the right bank confluents of the Dniester. In the left-bank confluents, in the chemical composition of water dominate the contents of calcium and hydrocarbons ions. The heterogeneity of the lithological composition, the instability of the thickness of the aquifer both in the horizontal and vertical directions, and the different technogenic influence form the irregularity of pollution and its local distribution in groundwater.
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Cios, Stanisław. "Information on huchen, Hucho hucho (L.), from historical Polish sources." Archives of Polish Fisheries 23, no. 1 (March 1, 2015): 17–24. http://dx.doi.org/10.1515/aopf-2015-0002.

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Abstract This paper presents historical information on the Danube huchen, Hucho hucho (L.), in Polish sources from the sixteenth to early twentieth centuries in the Danube, Prut, Dniester, and Vistula river basins. These accounts concern the historical distribution of the species and its economic importance, culinary value, fishing methods, and artificial reproduction and propagation. The occurrence of huchen in the Dniester River basin until the beginning of the eighteenth century merits special interest, because this river is not mentioned by any modern source on the natural distribution of this species. The extinction of the huchen in this river can likely be attributed to anthropogenic changes in the environment that were associated mainly with agricultural development.
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Tomeniuk, O. "Exploration of loesses in Volyn-Podillia region as a cornerstone of Yuriy Polians’kyi’s scientific quests." Visnyk of the Lviv University. Series Geography, no. 39 (December 15, 2011): 342–63. http://dx.doi.org/10.30970/vgg.2011.39.2196.

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On the basis of the detailed analysis of scientific works, written by Yuriy Polians’kyi, the main scientific achievements of the scholar are characterized. These works are concerning researches of loesssoil stratum on the Middle Dniester region. In particular, progressive technique of researches of Quaternary deposits and using of the newest terminology are considered. Yuriy Polianskyi’s major scientific ideas are analyzed: loess and terraces, loess and glaciations, loess and Paleolithic, stratigraphic significance of fossil soils in loess-soil stratum etc. The influence of scientific achievements of Yuriy Polians’kyi at the field of loess problematic on the development of modern palaeogeographic researches of loess of Ukraine is analyzed. Key words: loess, terraces, fossil soils, glaciations, Pleistocene, Paleolithic, Dniester, Volyn-Podillia region.
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37

Ivanova, Svetlana V., Viktor I. Klochko, Aleksander Kośko, Marzena Szmyt, Gennadiy N. Toschev, and Piotr Włodarczak. "‘Yampil Inspirations’: A Study of the Dniester Cultural Contact Area at the Frontier of Pontic and Baltic Drainage Basins." Baltic-Pontic Studies 20, no. 1 (June 1, 2015): 407–25. http://dx.doi.org/10.1515/bps-2017-0009.

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Abstract The article presents the present state of research on the general issue of the Dniester Region of cultural contacts between communities settling the Baltic and Pontic drainage basins. Some five domains of research shall be brought to discussion in which it is possible to see fresh opportunities for archaeological study, on the basis of ‘Yampil studies’ on Dniester-Podolia (forest-steppe) barrow-culture ceremonial centres from the latter half of the 4th millennium and first half of the 3rd millennium BC. This relates to the peoples of the Eneolithic and the Early Bronze Age. In terms of topogenesis, embracing the Pontic-Tripolye, Yamnaya and Catacomb cultures, as well as Globular Amphora and Corded Ware in central prehistoric Europe.
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Rusu, V., L. Postolachi, A. Maftuleac, and T. Lupascu. "Pecularities of Phosphorus Forms Dynamics in Bottom Sediments of River Dniester (Moldova)." Chemistry Journal of Moldova 7, no. 2 (December 2012): 78–83. http://dx.doi.org/10.19261/cjm.2012.07(2).22.

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Seasonal, spatial and multi-annual dynamics of phosphorus forms in bottom sediments and their interstitial water for river Dniester was evaluated. The spatial dynamics of phosphorus forms in the bottom sediments along river had, in general, the same trend during of 2004 and 2009 years, being recorded the increasing tendency along river Dniester for inorganic phosphorus and decreasing tendency for organic phosphorus. Multi-annual dynamics for 2004-2010 years showed a tendency of increasing of all phosphorus forms in bottom sediments; the highest values being registered during 2010 year. Spatial and seasonal dynamics of phosphorus forms in bottom sediments and their interstitial water were generally in correspondence, although sometimes with some differences.
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Perets, Khrystyna, Oksana Vovk, Oleh Orlov, and Olena Lutsyshyn. "The properties of river alluviums of the Upper-Dniester alluvial plain." Visnyk of the Lviv University. Series Geography, no. 51 (December 27, 2017): 293–303. http://dx.doi.org/10.30970/vgg.2017.51.8867.

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Alluvial soil formation is a dynamic process, the main prerequisite of which is the regular, periodic flooding of the river floodplain with flood waters, which are enriched with multidispersed organic and mineral particles. During the last century, about 80 % of territory of the Upper-Dniester alluvial plain was transformed by means of hydrotechnical construction: waterproof dams and drainage channels have broken the wide river floodplains into isolated fragments, making impossible the free flow of flood waters, enriched with silt. The results of the study of stratification patterns of the river silt in the riverbed floodplain, depending on the flow velocity, granulometric composition, physical and chemical properties, given its role in the floodplain soil formation are given. The granulometric composition of the Dniester River silt changes downstream from the sandy to the heavy-loamy; In the floodplains of the Stryj and Svicha rivers medium- and heavy-loamy deposits are postponed, respectively. In the upper part of the Upper- Dniester alluvial plain (Chaikovichi 1, 2) accumulates a silt with predominance of the medium and fine sand fraction, which forms a good filtration ability of soils, whereas downstream the physical clay content increases (up to 47.2 %), which makes the river silt an important source of mineral nutrition of plants. The domination (over 40 %)in silt granulometric composition the rough dust fraction (Ustia 1, Zalisky 1) contributes to the improvement of the water-physical properties of alluvial soils and provides optimal conditions for the biota functioning. For the investigated river alluviums an alkaline reaction of the extract (pH (H2O) = 7,44–8,03) and low content of humus (0,54–3,80 %) are characteristic. The amount of nitrogen in the silt varies within 1,47–18,20 mg/100 g of soil. The river alluviums of the Upper-Dniester alluvial plain are an active factor in floodplain soil formation, since it optimizes the water-physical and physical-chemical properties of alluvial soils. But the influence area of silt on the soilsis sharply reduced and is limited only to the space in front of the dams. In the soils outside the dam, to which no fresh alluvial material comes, the hydrological regime is rebuilt and properties change substantially, up to the loss of their typological alluvial features. Key words: river alluviums, silt, floodplain, the Upper-Dniester alluvial plain, alluvial soils, hydrotechnical fragmentation.
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40

Kalyn, B. M., M. V. Khromova, and V. Ia Vishchur. "Estimation of quality of surface water of Dniester river basin within Lviv and Khmelnytsk regions." Ukrainian Journal of Ecology 10, no. 6 (December 28, 2020): 127–32. http://dx.doi.org/10.15421/2020_271.

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The problem of deterioration of the ecological condition of river basins of Ukraine is extremely important. Particular attention is paid to transboundary rivers, which include the Dniester River. The article describes the physical and geographical conditions of the Dniester basin, analyzes the scale of water use and discharge of return water in to the surface reservoirs in the basin. The use of water resources of the basin by different sectors of the economy is studied. 50% in Lviv region and 72% in Khmelnytsk region of abstracted water is used for commercial and drinking purposes, respectively 30% and 25% - for production. The largest sources of river basin pollution within Lviv and Khmelnytsk regions are considered. The main pollutants of surface water bodies in Lviv region in terms of the amount of effluents are enterprises of housing and communal services, enterprises of heat and power, chemical and petrochemical, machine-building and food industries. Among the enterprises of Khmelnytsk region, the largest volumes of wastewater discharges are carried out by the enterprises of heat and power, housing and communal services, food and construction industries. It is established that the major factors influencing the deterioration of surface in the river basin are disposals of sewage. The ecological danger from hydrosphere pollution in the Dniester basin has been assessed on the basis of pollutant concentrations. The results of monitoring water pollution in the river Dniester basin testified that the main pollutants that exceed the level compared to the maximum permissible concentration are nitrites, and for its tributaries river Lug and river Smotrych also ammonium salt, nitrates, sulfates and phosphates. As a result of a comprehensive assessment of the water quality of the river basin, the characteristics assigned to them are weakly and moderately polluted. Except for pollution of water objects, the urgent problem demanding the solution is the acting landscape structure in the basin of river Dniester. The disturbed structure of territories is the result of excessive agricultural land use and reduction of the area of natural lands. We came up with the priority tasks are to minimize the discharges of polluted return water into the water bodies, to improve the economic mechanism of water use and implement of water protection measures, to optimize the landscape-ecological structure of the territory, in particular increase the areas of nature reserve fund.
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41

Kovalchuk, M. S., G. S. Kompanets, T. M. Sokur, L. A. Figura, Yu V. Kroshko, and A. V. Usminska. "THE EVOLUTION OF SEDIMENTATION IN DNIESTER PERECRATON DEPRESSION." Collection of Scientific Works of the Institute of Geological Sciences of the NAS of Ukraine 3 (December 16, 2010): 47–56. http://dx.doi.org/10.30836/igs.2522-9753.2010.146977.

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42

Kulakovska, L., V. Usik, P. Haesaerts, B. Ridush, Thorsten Uthmeier, and Thomas C. Hauck. "Upper Paleolithic of Middle Dniester: Doroshivtsi III site." Quaternary International 359-360 (March 2015): 347–61. http://dx.doi.org/10.1016/j.quaint.2014.10.034.

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43

Lisowskiy, Andriy. "Morphogenesis of typical chernozem of Podillia-Dniester region." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 170–77. http://dx.doi.org/10.30970/vgg.2013.44.1221.

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The results morphogenetic studies of typical chornozems of Podillia-Dniester region have been analyzed. Based on comprehensive analysis of structure and profile of main morphological conducted genetic analysis of soil profile has been evaluated. Correlative relationship was found in formation of humus and carbonate black soil profile in different geomorphological elements and under different hydrothermal conditions. Key words: typical chornozem, soil profile, horizon genetic, morphological features, correlation, coefficient of variation, standard deviation.
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Trysnyuk, Vasyl, Taras Trysnyuk, and Viacheslav Okhariev Viktor Shumeiko. "CARTOGRAPHIC MODELS OF DNIESTER RIVER BASIN PROBABLE FLOODING." Scientific Bulletin Series D : Mining, Mineral Processing, Non-Ferrous Metallurgy, Geology and Environmental Engineering 32, no. 1 (2018): 51–55. http://dx.doi.org/10.37193/sbsd.2018.1.07.

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Theme of the paper is the solution of flooding geo-models creation for Dniester river basin territory, which uses contact and remote measurements. Natural and anthropogenic factors causing groundwater level rising were analyzed for localization of flooded zones and forecasting of geometric characteristics.
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Sheshnitsan, Tatyana L., Sergey S. Sheshnitsan, and Marina V. Kapitalchuk. "CONTENTS OF MANGANESE, ZINC, COPPER AND MOLYBDENUM IN THE HAIR OF THE FARM ANIMALS IN THE LOWER DNIESTER VALLEY." South of Russia: ecology, development 13, no. 4 (January 4, 2019): 166–73. http://dx.doi.org/10.18470/1992-1098-2018-4-166-173.

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Aim. The aim is to identify the differences in the accumulation of manganese, zinc, copper and molybdenum in the hair of farm animals (cows and goats) and their spatial differentiation in the valley of the Lower Dniester. Methods. Sampling and sample preparation were carried out in accordance with generally accepted methods. The determination of metal content in hair samples was carried out in accredited laboratories using atomic absorption spectrometry (AAS) and Inductively Coupled Plasma Spectroscopy (ICP-S). Results. For the first time, data are presented on the content of biogenic metals (manganese, zinc, copper, molybdenum) in the hair of the tail of black-and-white cows and Russian White and Saanen goats in the valleys of the Lower Dniester. Conclusions. It is shown that the concentration of trace elements in the hair of farm animals reflects the relative homogeneity of the biogeochemical conditions of the Lower Dniester valley. It is established that cows and goats are characterized by a sharply differing elemental status for the studied metals estimated on the basis of an analysis of their concentrations in the hair of the tail. At the same time, the effect of hair color on the content of elements was revealed only for molybdenum in cows, and for goats there were no significant interbreed differences in metal concentrations.
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46

Popuiac, Aurelia. "Rare Earths in Geological Formations of Central Region of the Dniester River Basin, Republic of Moldova." Advances in Geology 2015 (January 5, 2015): 1–13. http://dx.doi.org/10.1155/2015/713282.

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In the different varieties of crystalline basement of Archean and Proterozoic age and in Vendian (Ediacaran) basal layers of platform coverture in the Central Basin of the Dniester River were found relatively high concentrations of Lanthanum, Cerium, Yttrium, Ytterbium, and Scandium. Because the petrographic formations, which are genetic associated with RE elements in Dniester region are absent, the origin of these elements is unclear. At the same time, in the geological mapping, it was detect that geochemical aureoles of REE, found in the northern region of Republic of Moldova, are generated by accessory minerals monazite and zircon present in the rock of basement platform and fragments of crystalline rock in the composition of terrigenous formations from basal levels of sedimentary coverture. Probably mentioned minerals are brought from Ukrainian Crystalline Shield regions, in which are spread varieties of granitic rocks and alkaline pegmatite. It is not excluded that in these basal layers in the sedimentogenes processes and differentiation of detrital material to be formed the mechanic aureoles rich in monazite and zircon, which in turn can form significant concentrations of rare earths. To solve the perspective problem of detection of industrial mineral accumulations of RE in the central region of the Dniester River basin, it is necessary to conduct within this area detailed geological and geochemical research.
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47

Tortyk, Mykola. "Assessment of physical alluvial soils of floodplains of lower part of Dniester River." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 364–71. http://dx.doi.org/10.30970/vgg.2013.44.1244.

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The results of studies of physical condition of alluvial floodplain soils of Lower Dniester River and its component Turunchuk Island are given. Key words: alluvial soils, grain size, microagregative composition, density, structure, water-physical properties.
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48

Shevtsova, L. V., N. Ya Babich, and V. V. Semchenko. "An Ecologically Justified Operating Mode of the Dniester Reservoir as a Factor of Preservation of the Ecosystem of the Dniester Delta." Hydrobiological Journal 39, no. 6 (2003): 11–22. http://dx.doi.org/10.1615/hydrobj.v39.i6.20.

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49

Trysnyuk, Vasyl, Taras Trysnyuk, Anatolii Nikitin, Anatolii Kurylo, and Olga Demydenko. "Geomodels of space monitoring of water bodies." E3S Web of Conferences 280 (2021): 09016. http://dx.doi.org/10.1051/e3sconf/202128009016.

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Theme of the paper is the solution of flooding geomodels creation for Dniester river basin territory, which uses contact and remote measurements. Natural and anthropogenic factors causing groundwater level rising were analyzed for localization of flooded zones and forecasting of geometric characteristics. Geographic information systems for researched area include the spatial binding of the hydrological elements and observation points, digital model of relief preparation, basin allocation catchment, flooded areas modeling. Structural features include the size and shape of object, brightness disposal within the object, image texture, some others. Possibility of available remote sensing data use allows reducing temporal and economic cost for conducting additional ground measurements for possible flooded areas determining. These methods of geomodels creation are realized for the territory of Dniester Canyon, the hydrogeologic feature of which is connected to the Upper Cretaceous horizon and groundwater.
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50

Sova, Olha. "Gross chemical composition of soil of Sian-Dniester Upland." Visnyk of the Lviv University. Series Geography, no. 44 (November 28, 2013): 333–43. http://dx.doi.org/10.30970/vgg.2013.44.1241.

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The results of studies of the gross chemical composition of soil of Sian-Dniester upland were given. Features of oxide content in soils and soil-forming rocks were considered. The changes that take place in one of the most conservative substances of soil due to anthropogenic use are analyzed. Key words: grey forest soils, dark grey podzolic soils, podzolized chernozems, gross chemical composition, oxides molar ratio, leaching, constitutional water.
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