scholarly journals Settlement characteristics of The Emerald Network "Khukhra" and "Riabyna" objects in Sumy region

2021 ◽  
pp. 119-126
Author(s):  
I. Tymochko ◽  
I. Solomakha ◽  
V. Shevchyk ◽  
O. Senchylo
Keyword(s):  
Large Population ◽  
Local Population ◽  
River Valley ◽  
Low Flow ◽  
Left Bank ◽  
Small Areas ◽  
Hay Meadows ◽  
Environmental Object ◽  
Amphibious Plants ◽  
Forest Remnants

The current state of biotope’s vegetation cover by natural and spontaneous origin of the Khukhra and Riabyna river valleys was researched, which are left-bank tributaries of the Vorskla river, as fragments of the preserved landscape within one of the western spurs of the Central Russian Upland. They are listed as perspective objects of the Emerald Network — Riabyna river valley in Sumy region (UA0000427) and Khukhra river valley in Sumy region (UA0000429). The obtained new data on environmental significance are data for the primary database formation in the monitoring organization of these territorial objects. The researched areas are mainly floodplains, small segments of pine terraces and slope’s fragments of these rivers native banks. The presence numbers of biotopes from Resolution 4 of the Berne Convention (C1.222; C1.223; C1.224, C1.32; C1.33; C1.4; C2.33; C2.34; C3.51; D5.2; E2.2; E5.4; F9.1; G1.11; G1.21; G1.22; G1.A4; G1.A1) are given for both explored objects, in addition, for the valley of the Riabyna river are indicated E1.3; E3.4, and for the Khukhra river — C3.4; E1.2. We have not confirmed the existence of such biotopes as C3.4, E1.3, C1.4 for these objects. Also, the presence of Sarmatian-type pine forests (G3.4232) was noted, which are timed to the elevations of pine terraces. Biotopes with constant excessive moisture are ubiquitous in the waters of low-flow artificial ponds. Eutrophic and mesotrophic vegetation of slow-flowing waters often occurs in shallow water along riverbeds. Biotopes groups of dwarf annual amphibious plants were observed only in fragments. Lowland swamps with sedge thickets without stagnant water are widespread in the floodplain, although they occupy small areas. Biotopes flooded pasture and hay meadows are a variety of options coenotic (herbaceous and cereal, wet and moist high-grass meadows). Biotopes of riparian shrubs, willow and willow-poplar floodplain forests are distributed in small fragments in the riverbed of floodplains. Mixed riparian floodplain and gallery forests occur in low-lying areas at the transition from the floodplain to the pine terrace. In general, shrub and forest vegetation on the terraces of these rivers are currently quite limited and fragmentary. Due to the reduction in the use of hayfields, in the floodplain the presence of indigenous forest remnants is quite relevant, which should be a source for their restoration in large areas. Important environmental object in these areas, as part of the Emerald Network is the local population of Ostericum palustre, and in the valley of the Khukhra river discovered a large population.

scholarly journals A new finding of a uniquely large population of Anacamptis morio (Orchidaceae) on the Left-Bank Ukraine

2019 ◽  
Vol 55 (1) ◽  
pp. 15-24
Author(s):  
Vasyl L. Shevchyk ◽  
Igor V. Solomakha ◽  
Oksana V. Shevchyk ◽  
Tetyana S. Dvirna ◽  
Volodymyr A. Solomakha ◽  
...  
Keyword(s):  
Age Structure ◽  
Nature Reserve ◽  
Large Population ◽  
Local Population ◽  
Average Density ◽  
Left Bank ◽  
Floodplain Forests ◽  
New Finding ◽  
The Creation ◽  
Generative Stage

Abstract The paper presents the results of the research of local population of Anacamptis morio (L.) R. M. Bateman on the territory of the Left-Bank Ukraine. The size of this population was estimated at about 250-300 thousand individuals. The average density of individuals per 1 m2 is 12, while in terms of age structure, dominate individuals in the generative stage (70-75%). A. morio inhabits fresh, forest-meadow biotopes. Its populations are found in fresh eutrophic and moist mesotrophic meadows and in coastal floodplain forests. This species is a part of vegetation of the Koelerio-Corynephoretea and Molinio-Arrhenatheretea classes. Considering the characteristics of the investigated A. morio population and its habitat we assert that the studied territory is unique, valuable and perspective for the creation of a nature reserve.

scholarly journals How Does Administrative Data Compare with Census Data for the Measurement of Internal Migration? The Case of Northern Ireland, 2001–2011

2021 ◽  
Author(s):  
Brian Foley ◽  
Tony Champion ◽  
Ian Shuttleworth
Keyword(s):  
Administrative Data ◽  
Internal Migration ◽  
Census Data ◽  
Local Population ◽  
Population Data ◽  
Population Estimates ◽  
Demographic Groups ◽  
Small Areas ◽  
Intercensal Period ◽  
Statistical Agencies

AbstractThe paper compares and contrasts internal migration measured by healthcard-based administrative data with census figures. This is useful because the collection of population data, its processing, and its dissemination by statistical agencies is becoming more reliant on administrative data. Statistical agencies already use healthcard data to make migration estimates and are increasingly confident about local population estimates from administrative sources. This analysis goes further than this work as it assesses how far healthcard data can produce reliable data products of the kind to which academics are accustomed. It does this by examining migration events versus transitions over a full intercensal period; population flows into and out of small areas; and the extent to which it produces microdata on migration equivalent to that in the census. It is shown that for most demographic groups and places healthcard data is an adequate substitute for census-based migration counts, the exceptions being for student households and younger people. However, census-like information is still needed to provide covariates for analysis and this will still be required whatever the future of the traditional census.

Physiological-biotechnological aspects of drought resistance of narrow-leaved lavender (Lavandula angustifolia mill.)

2021 ◽  
Vol 12 (3) ◽  
Author(s):  
O Klyachenko ◽  
◽  
I Shliakhtun ◽  
Keyword(s):  
Aquatic Vegetation ◽  
Left Bank ◽  
Small Areas ◽  
Code Of Phytosociological Nomenclature ◽  
Higher Aquatic Vegetation ◽  
Nature Park ◽  
Original Field ◽  
Natural Boundaries ◽  
Phytosociological Nomenclature ◽  
Coenotic Diversity

National Nature Park “Pyryatynsky” is a valuable reserve of flora and vegetation of the Left-Bank Dnipro. The extensive hydrological network of the Udai River and the wide representation within this nature reserve of floodplain reservoirs are the reason for the high diversity of plant communities of higher aquatic vegetation. In this article we classified the communities of order Callitricho-Batrachietalia in National nature park "Pyryatynskyi" and identify the features of their syntaxonomic and ecological differentiation. Fragmentary and non-comlete information about this type of vegetation are existed in literature, however, without geobotanical releves and detailed characteristics of the structure of phytoceonoses, synecology and synchorology. All obtained results based on original field data. In total, 22 geobotanical releves were performed during the period 2010–2017. The description of communities was carried out within their natural boundaries. Treatment of fitosociological data was performed with the JUICE software package. The nomenclature of syntaxons was consistent with the International Code of Phytosociological Nomenclature (ICFN).The order of Callitricho-Batrachietalia on the territory of NPP "Pyriatynsky" is represented by alliance Batrachion aquatilis Gehu 1961 and 4 associations (Batrachietum aquatilis Gehu 1961, Potameto perfoliati–Batrachietum circinati Sauer 1937, Hottonietum palustris Sauer 1947, Veronico beccabungae–Callitrichetum stagnalis (Oberdorfer 1957) Th. Müller 1962). This is first prodrome of order Callitricho-Batrachietalia for territory of National Nature Park “Pyryatynskyi”. The communities of this syntaxon occupy small areas and have a limited distribution in the region. Most of them are rare and vulnerable to changes in environmental conditions. Monitoring of their structure, chorology and dynamics is an important task to maintain and preserve the species and coenotic diversity of NPP "Pyryatynsky".

scholarly journals In the Sorraia River Valley (Coruche, Portugal): Settlement Dynamics of Ancient Peasant Societies on the Left Bank of the Lower Tagus River (5500 to 1800 B.C.E.)

2021 ◽  
Vol 31 ◽  
pp. 95-158
Author(s):  
Ana Catarina Sousa ◽  
Victor S. Gonçalves ◽  
André Texugo ◽  
Ana Ramos-Pereira
Keyword(s):  
Bronze Age ◽  
River Valley ◽  
Early Bronze Age ◽  
Left Bank ◽  
Late Neolithic ◽  
Economic Changes ◽  
Tagus River ◽  
Settlement Dynamics

This article is the result of archaeological and paleoenvironmental investigations carried out within the scope of the ANSOR project in the Sorraia valley (Coruche), on the left bank of the Lower Tagus. In the analysis of settlement dynamics between 5500 and 1800 a.n.e. we considered four moments: 1) The first peasant societies of the ancient Neolithic; 2) The Middle and Late Neolithic; 3) Chalcolithic; 4) The Early Bronze Age. The Sorraia valley was also framed in the framework of the Center and South of Portugal during the period under analysis. Interpretative models are presented for changes in the implantation patterns in the four stages under study, oscillating between paleoenvironmental factors and the socio-economic changes registered in the old peasant societies. 

scholarly journals Cauldrons and Buried Treasures of the Middle Yenisei Region in the Early Iron Age

2021 ◽  
Vol 20 (7) ◽  
pp. 121-134
Author(s):  
Andrei P. Borodovsky ◽  
Yuri V. Oborin
Keyword(s):  
Iron Age ◽  
River Valley ◽  
Early Iron Age ◽  
Left Bank ◽  
Yenisei River ◽  
The Yenisei River

Purpose. The article dwells upon discoveries of cauldrons and buried treasures of the Early Iron Age on the territory of the Middle Yenisei region. The work contains a review of such main recent discoveries and an analysis of different variants of occurrence of cauldrons in the buried treasures of the Paleometal Epoch. They include self-containment of a cauldron hidden as part of the buried treasure; a cauldron as one of the containers for the buried treasure items; integral small-sized cauldrons as part of the buried treasure object set; pieces of cauldrons as part of the buried treasures. Results. The authors developed a map of 21 buried treasures on the territory of the Middle Yenisei region, whose object set included cauldrons. It allowed identifying a territorial uniqueness of location of cauldrons being part of ‘accidental’ discoveries as well as buried treasures. The archaeological microzoning approach enabled to define several compact areas that were characterized by multiple discoveries of buried treasures with cauldrons. One of them is the northeastern territories of the Middle Yenisei. This is the middle course of the Kan river valley in the vicinity of Terskoe village. Other areas of localization of finds of cauldrons are located in the northwest – from the Kosogolskie lakes to the middle course of the Iyus river. The same can be said about the presence of the distribution of such finds in the southern territory. It is localized mainly from the Askiz steppe and to the left bank of the Yenisei river in this area. The analysis of object sets focused on identification of repeated sets of items (mirrors, axes, belt fixtures, jewelry) in buried treasures that included cauldrons. Conclusion. The publication puts forward a hypothesis concerning the potential of using cauldrons as a buried treasure container in terms of its dating range. Based on the contents of buried treasures that included cauldrons, relative chronological lines of these object sets from the Scythian to the Xiongnu and Xianbei time for the Middle Yenisei region was proposed.

Estimation of the annual runoff distribution of the Siverskyi Donets River Basin in the period of current climate change

2020 ◽  
Author(s):  
Hanna Bolbot ◽  
Vasyl Grebin
Keyword(s):  
Climate Change ◽  
River Basin ◽  
Annual Runoff ◽  
Low Flow ◽  
Left Bank ◽  
Spring Flood ◽  
Current Period ◽  
Current Climate ◽  
Annual Runoff Distribution ◽  
The Right

<p>The most urgent tasks facing hydrologists of Ukraine and the world include identifying patterns of rivers hydrological regime against the background of global warming, and assessing these changes. Changes in the annual runoff distribution under climate change impact require separate investigation of anthropogenically altered catchments, such as the Siverskyi Donets River Basin. Siverskyi Donets is the largest river in Eastern Ukraine and the main source of water supply for Kharkiv, Luhansk and Donetsk regions.</p><p>The annual runoff distribution of the Siverskyi Donets River Basin was evaluated by two periods: to the beginning of pronounced climatic changes and the current period. The research is proposed for three water year types: wet year, average year and dry year. The Siverskyi Donets Basin is a complicated water body with peculiar physico-geographical conditions, because of that annual runoff distribution is somewhat different for the left-bank tributaries, right-bank tributaries and, in fact, the Siverskyi Donets River itself.</p><p>It is found that the most runoff of the wet year for both periods is in the spring months. The current period is characterized by a much smaller runoff of spring flood (from the volume of annual runoff) than in the previous period. The annual runoff distribution is offset. Some differences can be observed between the left and right tributaries. For the left-bank tributaries, which has less anthropogenic load, climate change has led to a significant increase of winter and summer-autumn low flow periods. On the right tributaries of the Siverskyi Donets, which are flowing within the industrial part of the Donbass, the low flow period has not changed, or even decreased. Such situation is due to the decrease of mine water disposal because of the industrial production decrease in the region.</p><p>The largest part of the annual runoff in the average year falls on February and March. In the current period, the spring flood has decreased, but the summer and autumn low flow period has increased. The left-bank tributaries runoff during the winter low period is decrease. Instead, the runoff attributable to the autumn and winter low period has increased for the right-bank tributaries and the Siverskyi Donets itself.</p><p>Analyzing the runoff distribution of dry year, we can conclude that the most wet is February. At present, in dry years, spring flood practically are not allocated from the hydrograph; the baseflow months runoff significantly increased. The volume of winter runoff of the Siverskyi Donets River Basin is increased. Actually, for the Siverskyi Donets River the runoff of the summer period has increased and the runoff of the winter and autumn periods has decreased at the present stage.</p><p>The annual runoff distribution of the Siverskyi Donets River Basin in the current climate change has undergone significant changes: the spring flood has decreased and the summer-autumn low flow has increased.</p>

scholarly journals Contrasting dynamics of hydrological processes in the Volta River basin under global warming

2021 ◽  
Author(s):  
Moctar Dembélé ◽  
Mathieu Vrac ◽  
Natalie Ceperley ◽  
Sander J. Zwart ◽  
Josh Larsen ◽  
...  
Keyword(s):  
Climate Change ◽  
Global Warming ◽  
River Basin ◽  
General Circulation ◽  
Climate Models ◽  
Greenhouse Gas Emission ◽  
Local Population ◽  
Hydrologic Model ◽  
Mitigation Strategies ◽  
Low Flow

Abstract. A comprehensive evaluation of the impacts of climate change on water resources of the West Africa Volta River basin is conducted in this study, as the region is expected to be hardest hit by global warming. A large ensemble of twelve general circulation models (GCM) from CMIP5 that are dynamically downscaled by five regional climate models (RCM) from CORDEX-Africa is used. In total, 43 RCM-GCM combinations are considered under three representative concentration pathways (RCP2.6, RCP4.5 and RCP8.5). The reliability of each of the climate datasets is first evaluated with satellite and reanalysis reference datasets. Subsequently, the Rank Resampling for Distributions and Dependences (R2D2) multivariate bias correction method is applied to the climate datasets. The corrected simulations are then used as input to the fully distributed mesoscale Hydrologic Model (mHM) for hydrological projections over the twenty-first century (1991–2100). Results reveal contrasting changes in the seasonality of rainfall depending on the selected greenhouse gas emission scenarios and the future projection periods. Although air temperature and potential evaporation increase under all RCPs, an increase in the magnitude of all hydrological variables (actual evaporation, total runoff, groundwater recharge, soil moisture and terrestrial water storage) is only projected under RCP8.5. High and low flow analysis suggests an increased flood risk under RCP8.5, particularly in the Black Volta, while hydrological droughts would be recurrent under RCP2.6 and RCP4.5, particularly in the White Volta. Disparities are observed in the spatial patterns of hydroclimatic variables across climatic zones, with higher warming in the Sahelian zone. Therefore, climate change would have severe implications for future water availability with concerns for rain-fed agriculture, thereby weakening the water-energy-food security nexus and amplifying the vulnerability of the local population. The variability between climate models highlights uncertainties in the projections and indicates a need to better represent complex climate features in regional models. These findings could serve as a guideline for both the scientific community to improve climate change projections and for decision makers to elaborate adaptation and mitigation strategies to cope with the consequences of climate change and strengthen regional socio-economic development.

scholarly journals General Description of Hydrogen Sulfide Mineral Waters on the Left Bank of the Alazani River

2021 ◽  
pp. 127-141
Author(s):  
Marine Mardashova ◽  
◽  
Tamar Miqava ◽  
Keyword(s):  
Hydrogen Sulfide ◽  
Local Population ◽  
Sulfide Mineral ◽  
Mineral Waters ◽  
Left Bank ◽  
General Description ◽  
Mineral Springs ◽  
Regional Center ◽  
Left Tributary ◽  
The Village

The study object is located in the main hydrographic unit of Shida Kakheti - on the left bank of Alazani river, along the southern slope of the Greater Caucasus and includes a strip starting from the village of Shakriani (Telavi district), ending with the regional center Lagodekhi (Lagodekhi gorge, left tributary of the Alazani river). Within this zone, hydrogen sulfide (H2S) mineral springs are prevalent. Besides, these waters are opened by exploratory - hydrogeological wells. Among these springs, "Torghva Bath" and "Lagodekhi Bath" are especially popular among the local population. The first of these is located in the upper reaches of the Story Valley, and the second - in Lagodekhi gorge, 7 km away from the settlement. The mineral springs "Muni Tsakaro" and "Mkrali Waters" are also important for their healing properties. Based on the analysis of theoretical and field materials, Kakheti hydrogen sulfide waters are characterized in detail and possibly their use for resort purposes.

scholarly journals Assessment of Hydro-Meteorological Condition of Kathmandu (Nagdhunga)-Naubise-Mugling Road and Bridges

2018 ◽  
Vol 4 ◽  
pp. 125-136
Author(s):  
Ram Krishna Regmi
Keyword(s):  
Meteorological Data ◽  
Meteorological Condition ◽  
River Valley ◽  
Annual Rainfall ◽  
Left Bank ◽  
Design Flood ◽  
Hydrological Condition ◽  
Hilly Area ◽  
The Road ◽  
Crossing Structures

The Kathmandu (Naghdhunga)-Naubise-Mugling (KNM) road has passed hilly area from Nagdhunga to Naubise (about 13%) after passing Naubise the road alignment passes river valley of the Mahesh Khola and Trishuli River, initially the road alignment follows on left bank of the Mahesh Khola valley upto Galchhi before meeting with Trishuli River. After Galchhi, road alignment follows the left bank of the Trishuli River valley upto Mugling (about 87%). The present study deals with the hydrological condition of the KNM road by analysing the existing hydro-meteorological data, reviewing the reports/documents of the previous studies and visiting the study area. The annual rainfall of the study area is found to be of increasing pattern. It is necessary to construct new crossing structures along with replacing some of the existing culverts in the existing road. Existing side drains are more or less adequate but the capacity might to be increased during  he improvement works. In the proposed new alignment 113 cross drains are necessary to construct and proposed side drains will be adequate for passing the design flood. Some of the stretches of the existing road are very close to the river and are vulnerable of being toe cutting and flooding from the river.

scholarly journals DYNAMICS OF THE NUMBER OF THE STEPPER SNAKE VIPERA RENARDI IN THE SOUTH OF THE LEFT BANK OF UKRAINE

2021 ◽  
pp. 63-72
Author(s):  
Selyunina Z. V. ◽  
Markautsan О. Е. ◽  
Dubov S. V.
Keyword(s):  
Protected Areas ◽  
Black Sea ◽  
Abiotic Factors ◽  
Local Population ◽  
Biosphere Reserve ◽  
Irrigated Agriculture ◽  
The Black Sea ◽  
Forest Steppe ◽  
Left Bank ◽  
The South

The steppe viper (Vipera renardi (= ursinii) Christoph, 1861) is a background species of snakes in the steppe zone of southern left-bank Ukraine. This species is a figurant in the Red Book of Ukraine and is protected in accordance with the Bern Convention. According to the IUCN Red List, Vipera renardi has a Vulnerable species (VU) status, which is assigned to species that are under threat of becoming endangered. Anthropogenic transformation, namely, plowing, afforestation, irrigated agriculture, fires, synanthropization, etc., lead to the fact that in the Black Sea steppe, in the Lower Dnieper arenas of steppe, the viper disappears. This species has been preserved in the protected areas of the region and in the less transformed areas of the coastal and sandy steppe. The study area includes the forest-steppe areas of the Black Sea Biosphere Reserve (BSBR) and the territory of the “Svyatoslav’s Biloberezhzhya” National Nature Park (NNP BS) on the Kinburn Peninsula, the Black Sea areas and the islands of Tendrivska and Yahorlytska Bays, which are part of the Black Sea Biosphere Reserve. The dynamics of the number of steppe vipers also depends on abiotic factors too. In wetter years and the next 1-2 years, the number of vipers in the region decreases. In dry years, the number of steppe vipers increases. In the last 20 years, according to the results of long-term monitoring, the dynamics of the steppe viper population has a negative trend both in the Black Sea steppe and in the arenas of the Lower Dnieper.The cyclic dynamics of the steppe viper in our region is 3-5 years, the highest amplitude is 1.4 units, the maximum values of the relative abundance over the past 20 years have decreased from 1.5 to 0.4 ind./km, the minimum - from 0.3 to 0,1 ind./km. To preserve the population of this species in the south of the left-bank Ukraine, it is necessary to increase the areas with limited use of natural resources, namely, with the prohibition of plowing, prevention of excessive grazing and exploitation of sand deposits. In addition, it is required to strengthen environmental education and propaganda among the local population about the need to preserve the steppe viper in natural conditions and change the hypertrophied thought about the danger of this snake. The extensive network of protected areas in the region: reserves, national nature parks, regional landscape parks, protected tracts, etc., contributes to the conservation of this species. Key words: steppe viper, Black Sea steppe, Lower Dnieper arenas, population dynamics, monitoring.

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