Tytuł pozycji:
Studies of bed forms in the Wisloka river and water reservoir at Krempna
- Tytuł:
-
Studies of bed forms in the Wisloka river and water reservoir at Krempna
- Autorzy:
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Michalec, B.
- Powiązania:
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https://bibliotekanauki.pl/articles/905886.pdf
- Data publikacji:
-
2007
- Wydawca:
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Polska Akademia Nauk. Stowarzyszenie Infrastruktura i Ekologia Terenów Wiejskich PAN
- Źródło:
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Infrastruktura i Ekologia Terenów Wiejskich; 2007, 3
1732-5587
- Język:
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angielski
- Prawa:
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Wszystkie prawa zastrzeżone. Swoboda użytkownika ograniczona do ustawowego zakresu dozwolonego użytku
- Dostawca treści:
-
Biblioteka Nauki
-
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Attempt was undertaken at determination of the kind of river bed forms occurring
on the bottom of the Wisłoka River and in the water reservoir at Krempna.
The paper aims at examination of the conditions of bed forms and determination of
their kinds according to classification criteria. Conditions of formation of bottom
forms were defined according to the criteria given by Simons and Richardson [after
Dabkowski et al. 1982], Robert [after Radecki-Pawlik 2006], Zanke [1982],
Hjulsröm [after Sundborg 1967], Ashley [1990] and van Rijn [1984]. In the course
of studies three measurements of velocity in appointed cross-sections were performed
during the period July-September 2005.
During measurements samples of bottom sediments were collected and their
granulometric compositions determined. Great differentiation in the granulometric
composition was found in particular parts of the point bars giving evidence of the
process of process of washing out small fractions from the interstitial spaces in the
proximal part of the point bars. The examined bars were qualified according to the
criteria by Ashley to the type of lateral and point bars of lens-like shapes in longitudinal
profile.
Bed deposit samples from the reservoir at Krempna were collected. The bed
deposits of the reservoir are constituted of fine mineral material. Variability of
granulation in deposits layers was stated. According to the Zanke’s nomogram in
two examined reservoir cross-sections no movement of bed material exist and according
to the Simons and Richardson’s diagram in the examined cross-sections
the bed should be flat. However, in the inflow cross-sections II at the higher flow
and bed-shear stress over 1 N·m-2 ripples may occur. This is confirmed by underwater
photos taken in the Krempna reservoir. They permitted to define the morphological
structure of the bed. In the reservoir, the occurrence of bed forms was
not found.