Wyniki wyszukiwania - BazTech

1

Obliczanie przepływów maksymalnych rocznych o określonym prawdopodobieństwie przewyższenia w małej zlewni z zastosowaniem metod statystycznych oraz metod pośrednich

Banasik K., Byczkowski A., Hejduk L., Gładecki J.

Woda-Środowisko-Obszary Wiejskie

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2012

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T. 12, z. 3

17-26

PL

W pracy przedstawiono wyniki obliczeń przepływów maksymalnych rocznych prawdopodobnych (WQp), określonych metodami statystycznymi oraz metodami pośrednimi, w małej zlewni rzeki Zagożdżonka, położonej na Równinie Radomskiej, ok. 100 km na południe od Warszawy. Dane do obliczeń statystycznych pochodzą z własnych badań hydrologicznych, prowadzonych przez Katedrę Inżynierii Wodnej SGGW (d. Katedrę Budownictwa Wodnego) od 1962 r. Wyniki porównań wykazują znaczne różnice między wartościami WQp, określonymi różnymi metodami. Uzasadnia to potrzebę doskonalenia metod pośrednich wyznaczania przepływów maksymalnych prawdopodobnych w małych zlewniach rzecznych.

EN

Direct (statistical) and indirect methods have been applied for estimating T-year flood flows at the gauging station of a small lowland river Zagożdżonka located in Radom Plain ca. 100 km south of Warsaw. River flow data used for statistical analysis were collected by the Department of Water Engineering, Warsaw University of Life Sciences - SGGW since 1962. Comparison of the study results showed significant differences of T-year flood flows estimated with various methods. This confirms the need to continue the improvement of indirect methods for small catchments.

2

W sprawie definicji powodzi

Byczkowski A.

Przegląd Geofizyczny

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2005

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Z. 1-2

73-76

EN

As generally assumed a flood occurs when the river overtops and inundates the floodplain. The paper suggests extension of the definition and classification of floods. The flood should be defined as the phenomenon of inundation of the certain territory with the waters of various genesis affecting: threat of human life as well as the economical and moral losses. In proposed classification the floods are differentiated on: the river ones, local accumulation of the rain or snowmelt water and coastal floods.

3

Przepływy maksymalne prawdopodobne dla małej rzeki nizinnej - porównanie metod

Banasik K., Byczkowski A., Gładecki J.

Przegląd Naukowy Inżynieria i Kształtowanie Środowiska

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2004

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Vol. 13, No. 2

14--20

EN

Two inderect methods of T-year flood estimation have been applied for a small agricultural watershed. The results have been compared with values of application of statistical (direct) method. Significant differences have been obtained applying various methods for estimating peak flood flow with return period of 2- and 100-year.

4

Stan zasobów wód powierzchniowych na obszarze Leśnego Kompleksu Promocyjnego (LKP) Lasy Puszczy Kozienickiej oraz sposoby pokrycia występujących niedoborów wody

Ciepielowski A., Fortuński M., Banasik K., Byczkowski A.

Czasopismo Techniczne. Środowisko

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2002

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R. 99, z. 4-Ś

5--18

EN

The article is devoted to an analysis of surface water resources on the Forest Promotion Area (LKP) - the Puszcza Kozienicka Forest - and of forest sites occurring there, as well as of the character of their moisture. On that background there was a concept presented for potentials of increasing water resources through development of technical facilities of small retention. The research area covers several river catchments, among which a hydrological research is carried out since 1962 only on the Zagożdżonka stream in its upper part, in a catchment of area A = 82.4 km2 (Fig. 1). The results of that research are as follows: - The precipitation feeding (P) is 613 mm on the annual average, and it schows decreasing trends during the research period, this trend being not significant statistically. The similar phenomenon is observed in the country scale. - The runoff (H) is 112 mm on the annual average, and it also shows decreasing trends. The reasons of this state of things lie in the character of the precipitation feeding, and in anthropological factors as well. - Average runoffs per unit (SSq) are 3.74 l/skm2. This figure find its confirmation in an elaboration made for Poland (Stachy 1987), where average runoffs per unit in the region under study were below 4.0 l/skm2, and they were distincly lower than the country average equal to 5.2 l/skm2. The abovesaid proves that the Zagożdżonka stream catchment up to the Płachty Stare profile is representative for the Forest Promotion Area under study. The analysis of forest site moisture character shows a domination of fresh and dry sites, covering 85% of the LKP area. These data prove that water resources of the LKP Puszcza Kozienicka forest should be treated as poor ones. An increase of water resources could be reached through protection and restoration of potential places of their occurrence: non-runoff areas, throughflow areas with natural and artificial water eyes and through adaptation of amelioration systems. The technical solutions (Stanke and Chabiera 1996) proposed up today must be verified. Those objects should be of a pro-ecological character, not only in view of materials used, technology, and utilisation, but also of exploitation rules and well. A proposal is put to organise a monitoring system for possible control of water resources, of the condition of technical facilities and of their impact on the environment.

5

Wytwórnie mieszanek asfaltowych na polskim rynku

Byczkowski A.

Drogownictwo

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2001

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nr 9

282-283

PL

Autor podaje rodzaje (oraz producentów) wytwórni mieszanek bitumicznych dostępnych na polskim rynku.