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Wyświetlanie 1-2 z 2
Tytuł:
Wpływ częstotliwości pomiarów transportu fluwialnego na określenie jego wielkości i dynamiki podczas wezbrań w zlewniach o zróżnicowanym użytkowaniu na przykładzie rzeki Silnicy i Sufraganiec (Kielce)
Frequency of fi eld measurements as a clue for determination of the magnitude and dynamics of the fluvial transport during high water stands within catchments of different use as exemplified by the rivers Silnica and Sufraganiec (Kielce)
Autorzy:
Ciupa, T.
Powiązania:
https://bibliotekanauki.pl/articles/886343.pdf
Data publikacji:
2008
Wydawca:
Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie
Tematy:
czestotliwosc pomiaru
dynamika wod
hydrologia
koncentracja zawiesiny
odplywy jednostkowe
rzeka Silnica
rzeka Sufraganiec
rzeki
transport fluwialny
uzytkowanie zroznicowane
wezbrania wod
wody powierzchniowe
zlewnie
Opis:
A major problem in the quantitative hydrological studies, especially fl uvial, might be dealing with assessment of methods and results basing on error analyses. As for the mountain and Upland Rivers, the most common source of the errors could be low frequency of measurements and collection of samples. These particular studies have been carried out for the 8 sectors (sub-catchments) of the Silnica and Sufraganiec catchments of different use. The urban catchments of the river Silnica has been spread over 49.40 km2, and agricultural-woodland catchments of Sufraganiec has embraced 62.01 km2. During 11 high rivers’ stands, of variable origin, a few parameters have been determined, i.e. single unit outfl ow, concentration of suspended matter, concentration of dissolved matter, and temperature of the river waters every hours for the summer months and every two hours for the winter months. All the daily values of the above mentioned parameters have been compared with those values at 7 o’clock every day, and calculated mean values for the particular high rivers’ stand. Maximum error for the values of single unit outfl ow has been highly variable compare to the other values, being in the range of 65.4 to 873%. The highest spatial variability of the mean error of the measurements has been observed during high rivers’ stands related to the convection rains, whereas the smallest spatial variability of that error has been noted during high rivers’ stands due to widespread rains. The highest error while assessing our results has been found at the end of the urban catchments (Pakosz, Białogon). Maximum error for the concentration of the suspended matter has changed from 83.6 to 604.5%. Similarly, maximum error for the concentration of the dissolved matter has changed from 80.9 to 132.2%, whereas mean values have shown an error of 98.5 to 101.7%. All the observations have led to a conclusion that error for all the determined values is directly related to the space modifi ed anthropogenically. If that space increases, the error for measuring parameters of the fl uvial transport increases too. It means, that only high frequency of fi eld measurements of the fl uvial transport could reduce the errors while determining parameters of the transport. Ideally, more or less continuous measurements could reveal some complex mechanisms of fl uvial transport.
Źródło:
Scientific Review Engineering and Environmental Sciences; 2008, 17, 2[40]
1732-9353
Pojawia się w:
Scientific Review Engineering and Environmental Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Hydrogeomorfologiczne skutki intensywnych opadów na międzyrzeczu Bystrzycy i Giełczwi (Wyżyna Lubelska)
Hydrogeomorphological effects of intensive rainfalls on the Bystrzyca and Gielczew interfluve (Lublin Upland)
Autorzy:
Michalczyk, Z.
Janicki, G.
Rodzik, J.
Siwek, K.
Powiązania:
https://bibliotekanauki.pl/articles/887204.pdf
Data publikacji:
2008
Wydawca:
Szkoła Główna Gospodarstwa Wiejskiego w Warszawie. Wydawnictwo Szkoły Głównej Gospodarstwa Wiejskiego w Warszawie
Tematy:
Wynioslosc Gielczewska
Wyzyna Lubelska
hydrogeomorfologia
intensywnosc opadow
miedzyrzecze
odplywy
opady atmosferyczne
rozklad opadow
rzeka Bystrzyca
rzeka Gielczew zob.rzeka Gielczewka
rzeka Gielczewka
rzeka Gielczwianka zob.rzeka Gielczewka
splyw powierzchniowy
Opis:
On the 31st July – 6th August 2005 in Lublin surroundings, high and intensive rainfalls appeared (Table 1). The highest one took place at night of 3rd–4th August and its level exceeded 100 mm in two stations (Fig. 1). It was the rain of changeable intensity to 1 mm·min–1, lasting 4–5 hours. In the area of 400 square kilometers enclosed with 100 mm isohyet, an intensive runoff with erosional effects appeared. Its size in rural area was conditioned by land use, crop structure, fi eld pattern and road network. Majority of corn fi elds determined the predominance of dispersed runoff and little rainwash. Concentration of runoff and linear erosion took place only on small area of: roads, fi elds with root plants and fi elds of aerated soil (Fig. 3). The maximum of erosion rate in the fi eld scale reached: 200 t·ha–1 of translocated material and 70 t·ha–1 of carried material, fi eld surface lowering by 5 mm and convex parts of slope by 8 cm. Deposition of material, in form of fans and proluvial covers took place in dry valley fl oors. Concentrated runoff formed here episodic channels: transport and deposition in channels being fl at and erosional channels in crops with uncovered soil. Below roads crossing the channels, potholes with the capacity to 50 m3 and bars of eroded material were formed. Most of moved soil material was left within dry valleys whereas water runoff was the main source of fl ood waters in river valleys. Specifi c outfl ow from dry valley catch ments, with the area of 5 square km, reached 1–2.5 m3·(s·km2)–1. In valleys of small perennial fl ows with catchment area less than 50 square km (for instance: Skrzyniczanka, upper Stawek and Sierotka Streams), located in zone of the highest rainfall, local fl oods appeared. They caused losses in road and hydrotechnical infrastructure. Waves from these catchments, with specifi c outfl ow to 0.8 m3·(s·km2)–1, caused relatively smaller fl ood waters in higher valleys in next days (Fig. 2). Five-times growth of fl ow in Biskupice on the Giełczew River and seven-times one in Sobianowice on the Bystrzyca river occurred. On 4th–11th August period, about 12 mm of water fl owed from these catchments but in the Czerniejówka catchment, level of groundwater raised about 30–70 cm.
Źródło:
Scientific Review Engineering and Environmental Sciences; 2008, 17, 4[42]
1732-9353
Pojawia się w:
Scientific Review Engineering and Environmental Sciences
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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