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)
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)
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.
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