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Rola Wisłoka w kształtowaniu walorów środowiskowych i gospodarczych Podkarpacia

100%

Rak J. , Tchórzewska-Cieślak B.

tom Nr 5

210-213

Przedstawiono analizę funkcji Wisłoka obecnie i w przeszłości. Oszacowano atrakcyjność turystyczną doliny Wisłoka na podstawie stanu wód powierzchniowych, ukształtowania terenu i powierzchni lasów.

There has been presented the function of the Wisłok at present and the past. The touristic attractiveness of the Wisłok valley has been evaluated taking into consideration the state of its surface waters, configuration of the terrain and the area covered by forests.

Straty wody w sieciach wodociągowych zlewni rzeki Wisłok

84%

Dąbrowski W. , Granops M.

tom z. 32[180], cz.2

29-33

Several methods of water loss prediction were characterised and compared in respect to the information able to be received. Water loses for the town Rzeszów were listed on a month base and for all regions and towns in the Wisłok river basin on a year base. These loses have been compared with the data known from other parts of the country and it was concluded that except of the region Strzyżów all other water supply systems lose less water than the average amount in Poland. Three more towns in the basin of a significant water loses are Iwonicz Zdrój (30%), Łańcut (24%) and Krosno (20%).

Zbiornik wód podziemnych "dolina Wisłoka" na terenie zlewni rzeki Wisłok

84%

Dąbrowski W. , Puszkarewicz A.

tom z. 32[180], cz.2

35-41

There is a well documented groundwater aquifer to the North of the town Rzeszów. This aquifer is called the lower groundwater reservoir. In contrast very few is known about some aquifers located to the South of Rzeszow, except that in general they are of a small capacity, which is a general expectation for the most part of the Carpathian region. These aquifers are mainly of quaternary origin. The available bank of data refers to seventeen's, to the former hydrogeological atlases of Poland. These somewhat historical information were briefly summarised and the capacity of the upper reservoir evaluated first from hydrogeological atlases and then from the lowest flow rates in specific cross - sections of the Wisłok river.