552
for further analysis underkeel and vertical clearance
in study area.
2 STUDY AREA
The importance of the Vistula River as a inland
waterway in goods transport is marginal. In the
distance Solec Kujawski - Gdańsk (approx. 180 km)
there are insufficient navigational conditions for IV
class international waterway (Figure 1 A). On the
research section Vistula River corresponds to two
classes of navigability: II (from km 718+000 to km
910+000) and III (from km 910+000 to estuary to the
Gdansk Gulf) [6]. Lower Vistula include approx. 350
km part of river from Narew river. The hydrological
regime of the lower Vistula is mostly defined by
water flows prevailing in the mid-section of the river
as well as the inflow of water from the Narew river.
High water levels tend to occur in March and April,
less frequently in summer. The former are related to
early-spring melt-water runoff, the latter – usually
short-term – result from summer rainfalls. In both
cases flood waves are formed with a relative height of
3–5 m, maximum of up to 7 m [3]. In this time inland
navigation is impossible. The lowest water levels on
the Lower Vistula are from August to November, the
second part of the navigation season. The annual
average water level (AWL) of the Vistula in the
Fordon (Bydgoszcz) gauging station for the years
1984–2015 amounts to 319 cm [7]. In this period water
levels below AWL was observed for less than 50
days in fourteen navigational seasons. Also in the
same period water levels below AWL was observed
for more than 120 days only in two years. So generally
the average amount of days favorable for navigation
in the navigational season is only 59 days. Currently
an additional problem is hydrological draught.
Drought is defined as a stage below-normal water
availability [9]. While this time there are channel
forms fragment featuring mid-channel, near-island
and lateral sandbars, which modify the depth
conditions in waterway, so navigation in this area is
very complicated [5, 8].
3 AIM AND METHODS
The location of the Multimodal Platform has
possibilities to be connected to the national road
(highway A1 Gdansk-Lodz; express way S5 Poznan-
Nowe Marzy and main road no. 10 Szczecin-
Warszawa) and rail main line network (no. 201 Nowa
Wies Wielka – Gdynia; no. 18 Kutno - Pila) so is
possibility to increase the importance of the Vistula
River Waterway in good transport [5].
Figure 1. The main study area. (green line) against the
background of a map of inland waterways in Poland (A), a
diagram of the dynamics of changes in the depth of the
riverbed and the location of the Vistula navigation route (B)
and depths on the Vistula navigation route from Solec
Kujawski to Gdańsk (C) (area for analysis of underkeel
clearance highlighted in red).
The aim of this work is assessment of limitation for
inland ships in the area of planned multimodal port
near Bydgoszcz. The analysis of navigation conditions
was carried out to verify typical inland vessel traffic
on the Vistula stretch from Gdansk to Bydgoszcz-
Solec Kujawski (Figure 1 A). On this stretch of
shipping lane is 9 bridge structures and 6 power
transmission lines located [10]. Height of power
transmission lines is more than 14 m, so they are
omitted in this research. Bridges are characterized by
highly diversified technical parameters, in particular
vertical clearance - from 5.28 to 12.5 m. On the other
hand hydrological condition in this place are very
specific. For example, average water levels drop
below mean low water stages 90 days a year - in dry
years, this occurs on 200 days per annum. The lowest
water levels are recorded in August, September and
November. In addition hydrological regime of the
lower Vistula is mostly defined by water flows
prevailing in the mid-section of the river as well as
the inflow of water from the Narew river. High water
levels tend to occur in March and April, less
frequently in the summer [3]. The Lower Vistula in
study area is characterized by high dynamics of
riverbed movement and channel depth changes,
which results from the transport of sandy material on
the bottom (Figure 1 B).
3.1 Underkeel clearance analysis assumptions
In research the own data from depth measurements
Vistula River in 36 cross-sections and in the
longitudinal profile of the shipping lane were used for
determination of mean actual depth in given sections
between km 766.0 and km 775.0 (fragment of a
waterway - representing small depths at average
Vistula’s water flow - Figure 1 C). Channel depth and
geodetic measurements were performed in June 2016
using a motorboat equipped with the following
devices: single-beam echo sounder (SBES) Teledyne
ODOM ECHOTRAC E2 and geodetic rover GPS
GNSS Trimble 5800. The morphological mapping
were conducted on a digital terrain model (DTM) of
the bathymetry based on the collected depth data and
geodetic surveys in the field. We used an open-source
Geographic Information System software QGIS 2.16.3.