scholarly journals On the origin of inflected “non-finite” forms: the infinitive vs the supine

Diacronia ◽  
2016 ◽  
Author(s):  
Adina Dragomirescu ◽  
Alexandru Nicolae
Keyword(s):  
Functional Structure ◽  
The Novel ◽  
Eastern Area ◽  
Republic Of Moldova ◽  
The North ◽  
North Eastern ◽  
The Common ◽  
The Republic ◽  
Diachronic Changes ◽  
North Eastern Part

This paper deals with two verbal forms which, despite being traditionally labelled as “non-finite”, display inflection/agreement. We will focus on the behaviour and origin of the inflected infinitive attested in Romance and in languages from other families, against which we analyse the novel inflected supine found in the north-eastern area where Romanian is spoken (comprising the Republic of Moldova, Ukraine and the north-eastern part of the Romanian province of Moldova). The goal of the paper is to identify the common paths of diachronic change of these verbal forms and to put forward a formal account of the observed diachronic changes. From a diachronic perspective, our analysis shows that the functional structure of non-finite forms may become more enriched, a conclusion that is at odds with traditional findings, which generally argue for simplification, not enrichment of functional structure. At the same time, the proposed analysis also offers some insights into the diachrony of the supine marker de.

scholarly journals XI. An Account of Observations, made by Lord Webb Seymour and Professor Playfair, upon some Geological Appearances in Glen Tilt, and the adjacent Country

1815 ◽  
Vol 7 (2) ◽  
pp. 303-375 ◽  
Author(s):  
Webb Seymour
Keyword(s):  
Peat Moss ◽  
The South ◽  
The North ◽  
South West ◽  
North Eastern ◽  
Principal Branch ◽  
Adjacent Country ◽  
The Common ◽  
Common Character ◽  
North Eastern Part

1. The river Tilt is a principal branch of the Tay, which rises on the borders of Aberdeenshire, and runs towards the south-west, through the north-eastern part of the county of Perth. A portion of the valley along its course, for about ten miles above Blair of Atholl, is called Glen Tilt.The adjacent country presents the common character of the Highlands. It is mountainous and rugged, and the surface, except in the lower parts of the valleys, is chiefly covered with heath. Peat-moss frequently occurs.

Distribution of Diphyllobothrium latum in the populations of pike in lakes of Transbaikalia

2016 ◽  
Vol 3 (1) ◽  
pp. 41-48 ◽  
Author(s):  
Жепхолова ◽  
O. Zhepkholova ◽  
Дугаров ◽  
Zh. Dugarov ◽  
Толочко ◽  
...  
Keyword(s):  
Adult Stage ◽  
Human Infection ◽  
Selenga River ◽  
The North ◽  
North Eastern ◽  
The Republic ◽  
Diphyllobothrium Latum ◽  
North Eastern Part ◽  
Parasitological Study

Objective of research. The aim of the study was to explore the degree of contamination of pike and other fish species, plerosarcoidoma Diphyllobothrium latum in water bodies of the Baikal region. Materials and methods. In 2009-2014 was conducted parasitological study on infestation role of the D. latum plerocercoids of various species of fish. Just investigated 20 specimens of pike, 38 – burbot, 91 – perch and ruff 73 specimens in lakes of the North-Eastern part of Transbaikalia, located located in different districts of the Republic of Buryatia. The infection of fish with plerocercoids of D. latum were evaluated by extensiveness (EI), the abundance index (EI) and the intensity of infection (AI). Results and discussion. The pike infestation with plerocercoids of D. latum in lake. Goose in 2013-2014 decreased in 3 times compared with a maximum in 1973-1974 and was 0.8 % most Often, the D. latum plerocercoids are localized in the adipose tissue, the gonads, the wall of the swim bladder, liver, peritoneal epithelium, muscle, the wall of the stomach and the villagesince respectively 40,9 %; 13,8; 9,1; 9,1; 9,1; 4,5; 4,5; 4,5 and 4.5 % of cases. In Transbaikalia the fish parasitize three species of tapeworms, of which the epidemiological importance of the D. latum, D. dendriticum. D. ditremum in humans does not develop until the adult stage. In the region annually celebrate 150-450 cases of difillobotrioza in humans. In the basin of the Selenga river is-the reputed source of human infection by difillobotrioza are pike and perch, the infected with its good-Azerbaijani D. latum and the Baikal omul Coregonus migratorius infected with D. dendriticum. EI Baikal omul D. dendriticum is 62.3-100 %, and IO – 4,0-9,8 copies of This cestode is brought in the Selenga river from oz. The Baikal in the autumn spawning of Arctic Cisco. On owasco-FDI sample of human feces is impossible to distinguish the species D. latum and D. dendriticum. Probably in the Selenga region of Buryatia, there is a hotbed of difillobotrios caused by these two species of cestodes.

scholarly journals Drought Assessment in the Moldavian Plain

2016 ◽  
Vol 10 (1) ◽  
pp. 161-170
Author(s):  
Liviu Ioan Pelin
Keyword(s):  
Classical Method ◽  
Aridity Index ◽  
Precipitation Regime ◽  
Drought Assessment ◽  
The North ◽  
Dry Spells ◽  
North Eastern ◽  
The Republic ◽  
North Eastern Part ◽  
Continental Climate

Abstract The Moldavian Plain, located in the North-Eastern part of Romania, has a temperate-continental climate with a nuance of excessivity in the precipitation regime. This paper aims to analyse droughts in the Moldavian Plain for the period 1961-2010, by using a classical method - the de Martonne Aridity Index, and two other less known indices developed in Romania and the Republic of Moldova. Among these indices, the Dry Spells Index demonstrates a increasing frequency of dry years in recent decades.

scholarly journals Pressure and fluid dynamic characterisation of the Dutch subsurface

2012 ◽  
Vol 91 (4) ◽  
pp. 465-490 ◽  
Author(s):  
J.M. Verweij ◽  
H.J. Simmelink ◽  
J. Underschultz ◽  
N. Witmans
Keyword(s):  
Regional Differences ◽  
Regional Difference ◽  
Fluid Dynamic ◽  
Fluid Pressure ◽  
Burial History ◽  
Eastern Area ◽  
The North ◽  
North Eastern ◽  
Neogene Sediment ◽  
North Eastern Part

AbstractThis paper presents and discusses the distribution of fluid and leak-off pressure data from the subsurface of onshore and offshore Netherlands in relation to causes of formation fluid overpressure and the permeability framework. The observed fluid pressure conditions demonstrate a clear regional difference between the southern and the north and north-eastern part of the study area. In the southern area, formation fluid pressures are close to normal and well below measured leak-off pressures. In the north, formation fluids are overpressured and may locally even approach the measured leak-off pressures. The regional differences in fluid overpressure can, in large part, be explained by differences in geologic framework and burial history. In the south, relatively low rates of sedimentary loading and the presence of relatively permeable sedimentary units have led to the currently observed normally pressured conditions. In the northern area, relatively rapid Neogene sediment loading plays an important role in explaining the observed overpressure distributions in Cenozoic mudstones, Cretaceous Chalk and Rijnland groups, and probably also in Jurassic units. The permeability framework of the northern and north-eastern area is significantly affected by Zechstein and Triassic salt deposits and structures. These units are characterised by very low permeability and severely restrict fluid flow and pressure dissipation. This has created hydraulically restricted compartments with high overpressures (for example overpressures exceeding 30 MPa in the Lower Germanic Trias Group in the Terschelling Basin and Dutch Central Graben).

The influence of submesoscale eddies on hydrochemical parameters and structural and functional characteristics of phytoplankton in the north-eastern part of the Black Sea

2019 ◽  
pp. 24-40
Author(s):  
Sergey B. Kuklev ◽  
Vladimir A. Silkin ◽  
Valeriy K. Chasovnikov ◽  
Andrey G. Zatsepin ◽  
Larisa A. Pautova ◽  
...  
Keyword(s):  
Anticyclonic Eddy ◽  
The Black Sea ◽  
Hydrochemical Parameters ◽  
North East ◽  
The North ◽  
Seasonal Thermocline ◽  
North Eastern ◽  
Quantitative Indicators ◽  
The City ◽  
North Eastern Part

On June 7, 2018, a sub-mesoscale anticyclonic eddy induced by the wind (north-east) was registered on the shelf in the area of the city of Gelendzhik. With the help of field multidisciplinary expedition ship surveys, it was shown that this eddy exists in the layer above the seasonal thermocline. At the periphery of the eddy weak variability of hydrochemical parameters and quantitative indicators of phytoplankton were recorded. The result of the formation of such eddy structure was a shift in the structure of phytoplankton – the annual observed coccolithophores bloom was not registered.

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