Prispevok k sucasnej koncepcii hydrogeografického vyskumu podzemnych vôd a vodny potencial juznej asti Vychodoslovenskej niziny. (A contribution to the contemporary conception of hydrogeographical research of undergroundwaters and the water
The conception of hydrogeographical research of undergroundwaters is outlined and methodical approaches are explained. Problems of natural environment water potential and a balance valuation of ground water resources are given on exemple
Anthropogenic changes in water conditions in the Lublin area
Anthropogenic impact on water conditions (Vistula and Oder river basins)
Groundwater ; Hydraulic works ; Lublin ; Poland ; Urban development ; Water ; Water circulation ; Water needs ; Water quality ; Water resources ; Watershed
is supplied with water almost solely from underground resources, a situation which has been dictated by excellent-quality and easy-available undergroundwaters and small resources of surface water. A high level of exploitation of the undergroundwaters has led
The development of the city of Lublin has been closely associated with the exploitation of water resources in the Bystrzyca river basin. The extension of this city ditinctly affects the water conditions of the middle part of this basin. Lublin
The Flushing Time Based on Underground Supply in the Upper-Most Located Łeczna-Włodawa Lakes
Geological structure ; Hydrological regime ; Lake ; Poland ; Precipitation ; Undergroundwater ; Water body ; Water shortage ; Water supply ; Watershed ; genetic types of supply ; lakes ; underground inflow ; water mixing
, the lakes in question constitute a distinctive group among the Łeczna-Włodawa Lakes. They are located in the borderland of the Cretaceous Chełm Hills (part of the Polish Uplands) and Polish Lowland. The quantity of the undergroundwater supply was one
, as super-passive due to their water flushing time (>10 years). However, the average flushing time of the water in lakes Tarnowskie, Chuteckie, Pniówno and Syczyńskie, based on the underground supply, amounted to 606, 211, 54 and 79 days, respectively
Flushing time (Tf) is an important factor which determines the hydrological, ecological and chemical functioning of lakes. However, it has never been calculated on the basis of underground supply for Polish Lakes. Due to their high altitudes
of the key factors which make these lakes so distinctive. During periods of low precipitation, water shortages occurred in the lakes, especially Pniówno and Syczyńskie. The Łeczna-Włodawa Lakes are commonly distinguished, among other Polish water bodies
Carrying capacity ; Ground water;Undergroundwater ; Hydro-electric station ; Navigation ; Rill wash;Runoff ; Romania ; Water ; Water resources ; Water use
and turbidity levels are also discussed. Undergroundwater sources are described and a review of demand gives particular attention to hydroelectricity and water transport.
In relation to population, Romania's water supplies are quite modest. They are essentialy provided by the rivers. The factors responsible for both maximum and minimum runoff are discussed and particular reference is made to the floods of 1970. Load
Water resources of the Karakum are made up by undergroundwater encounted everywhere and by temporary surface run-offs which are formed on clay catchment areas during rainfalls. Fresh and slightly saline undergroundwater is confined to the Amudarya
valley, the Karakum Canal and other aboveground sources of water and also exists in the form of undergroundwater lenses of various origin and size. 8 large undergroundwater lenses with the total amount of water over 80 km3 have been found and studied
Moznosti regrenej analyzy a Fouriérovych radov pri studiu rezimu podzemnych vôd na priklade casti Vychodoslovenskej niziny. (Possibilities of regression analysis and Fourier series in the study of undergroundwaters regime on the example of a part
Mathematical generalization of the regime of undergroundwaters in a part of the East slovakian Lowland by means of regression analysis and Fourier series. (MS).
Manâbe'va masâ'el-e âh dar Irân, âb-hâ-ye sathi va zir-zamini va masâ'el-e bahre-bardâri az anhâ. Vol. 1.. (Sources and problems of water in Iran, surface and undergroundwaters, and problems of their exploitation)
The A. divides his book into two sections, surface water and undergroundwaters. He considers various governmental measures taken during the past decades for the study of measurement of water. He proposes possibilities for change| he deals with dams
, spring water and artificial wells, qanât and carst water. (ABSTR. IR.).
Podzemni odtok v dilcich castech povodi reky Moravy Underground runoff in partial water reaches of Morava river basin
The reduced values have been derived from sets of underground runoff monthly values determined by separation of hydrograms that have been balanced by applying K. Kille's method. The results obtained have been connected with natural conditions
5 chapters : the earth as a water planet| the sea (dimensions, structure, natural resources, utilization, protection)| inland waters (rivers, lakes, undergroundwater, glaciers)| utilization and protection of water| systematic explanations
Drinking water ; Ground water;Undergroundwater ; Hungary ; Hydrochemistry ; Hydrogeology ; Water quality
The A. provides a hydrogeological evaluation of the arsenic content of the artesian drinking water on the Great Hungarian Plain. The article is based upon 2 000 reliable analyses and shows the spatial and subsurface distribution of the arsenic
Wasserbesorgungsmoglichkeiten der Umgebung von Aggtelek. (Possibilities of water supply in the surroundings of Aggtelek)
In addition to the analysis of the hydrogeological significance of the formations in the surroundings of Aggtelek, the A. intends to present a comprehensive view on the probable flow directions of the undergroundwaters, their spatial distribution
, the approximate volume of stored waters etc. (CK).
This paper presents the influence of relief and geological structure of the dune-covered areas of the Vistula pradolina upon the distribution and differentiation of the surface waters phenomena and the pattern of the undergroundwater table
. The researches proved that the influence of the dunes on the distribution of underground watersheds depends on the local lithological conditions, the gradients of the undergroundwater table, the thickness of the aeration zone, the hydrographical relations
Prognoza vplyvu sustavy vodnych diel na Dunaji a Dolnom Vahu na pôdne pomery prilahlej oblasti. (Prognosis of water buildings on Danube and Law Vah rivers effect on soil conditions in surrounding territory)
In the territory of the great water building Gabcikovo is supposed a decrease of land productivity in connection with lowering of undergroundwater levels. The water building Nagymaros will in extent areas help optimalize undergroundwater levels
and similar situation is supposed by water buildings on Vah river too. (MS).