1,832 research outputs found
Lake Mladotice in the Western Czech Republic – Sediments as a Geoarchive for Flood Events and Pre- to Postcommunist Change in Land Use since 1872
Long-term flow field monitoring at the Upper Rhine floodplains
River hydrodynamicsOverbank flows and vegetatio
Hydrodynamic simulation of the effects of stable in-channel large wood on the flood hydrographs of a low mountain range creek, Ore Mountains, Germany
Large wood (LW) can alter the hydromorphological and hydraulic characteristics of rivers and streams and may act positively on a river's ecology by i.e. leading to increased habitat availability. On the contrary, floating as well as stable LW is a potential threat for anthropogenic goods and infrastructure during flood events. Concerning the contradiction of potential risks and positive ecological impacts, addressing the physical effects of stable large wood is highly important. Hydrodynamic models offer the possibility of investigating the hydraulic effects of anchored large wood. However, the work and time involved varies between approaches that incorporate large wood in hydrodynamic models. In this study, a two-dimensional hydraulic model is set up for a mountain creek to simulate the hydraulic effects of stable LW and to compare multiple methods of accounting for LW-induced roughness. LW is implemented by changing in-channel roughness coefficients and by adding topographic elements to the model; this is carried out in order to determine which method most accurately simulates observed hydrographs and to provide guidance for future hydrodynamic modelling of stable large wood with two-dimensional models.
The study area comprises a 282 m long reach of the Ullersdorfer Teichbächel, a creek in the Ore Mountains (south-eastern Germany). Discharge time series from field experiments allow for a validation of the model outputs with field observations with and without stable LW. We iterate in-channel roughness coefficients to best fit the mean simulated and observed flood hydrographs with and without LW at the downstream reach outlet. As an alternative approach for modelling LW-induced effects, we use simplified discrete topographic elements representing individual LW elements in the channel.
In general, the simulations reveal a high goodness of fit between the observed flood hydrographs and the model results without and with stable in-channel LW. The best fit of the simulation and mean observed hydrograph with in-channel LW can be obtained when increasing in-channel roughness coefficients throughout the reach instead of an increase at LW positions only. The best fit in terms of the hydrograph's general shape can be achieved by integrating discrete elements into the calculation mesh. The results illustrate that the mean observed hydrograph can be satisfactorily modelled using an adjustment of roughness coefficients.
In conclusion, a time-consuming and work-intensive mesh manipulation is suitable for analysing the more detailed effects of stable LW on a small spatio-temporal scale where high precision is required. In contrast, the reach-wise adjustment of in-channel roughness coefficients seems to provide similarly accurate results on the reach scale and, thus, could be helpful for practical applications of model-based impact assessments of stable LW on flood hydrographs of small streams and rivers
Implications of hydraulic anisotropy in periglacial cover beds for flood simulation in low mountain ranges (Ore Mountains, Germany)
The simulation of floods with conceptual rainfall-runoff models is a frequently used method for various applications in flood risk management. In mountain areas, the identification of the optimum model parameters during the calibration is often difficult because of the complexity and variability of catchment properties and hydrological processes. Central European mountain ranges are typically covered by Pleistocene periglacial slope deposits. The hydraulic conductivity of the cover beds shows a high degree of anisotropy, so it is important to understand the role of this effect in flood models of mesoscale mountain watersheds. Based on previous field work, the study analyses the sensitivity of the NASIM modeling system to a variation of vertical and lateral hydraulic conductivity for the Upper Flöha watershed (Ore Mountains, Germany). Depending on the objective function (Nash-Sutcliffe coefficient, peak discharge), two diametric parameter sets were identified both resulting in a high goodness-of-fit for total discharge of the flood events, but only one reflects the hydrological process knowledge. In a second step, the knowledge of the spatial distribution of the cover beds is used to investigate the potential for a simplification of the model parameterisation. The soil types commonly used for the spatial discretisation of rainfall-runoff models were aggregated to one main class (periglacial cover beds only). With such a simplified model, the total flood discharge and the runoff components were simulated with the same goodness of fit as with the original model. In general, the results point out that the anisotropy in the unsaturated zone, which is intensified by periglacial cover beds, is an important element of flood models. First, a parameter set corresponding to the hydraulic anisotropy in the cover beds is essential for the optimum reproduction of the flood dynamics. Second, a discretisation of soil types is not necessarily required for flood modeling in Central European mountain areas
Water and sediment pollution of intensively used surface waters during a drought period — a case study in Central Northern Namibia
Semiarid regions are often affected by water scarcity and poor water quality. Seasonal changes in precipitation and drought events increase the pressure of use on water bodies and their pollution. In Central Northern Namibia, a high seasonal intra- and inter-annual variability of precipitation caused a 5-year lasting drought period. In the semiarid region, ephemeral channels and water pans represent the main water source, besides the institutionalized water supply. No systematic analysis of its quality has been conducted so far. The states of the surface waters at the end of the dry season in 2017 and the end of the rainy seasons in 2018 and 2019 were characterized by the analysis of physical–chemical parameters, focusing on usability. The first results show coarse contamination of the waters, which results in high turbidity values. Salt concentrations, such as Ca2+ and Na+, greatly increased due to evaporation. Al is present in high concentrations in solid and liquid phases, which indicates direct anthropogenic pollution. Spatial differences are evident in the study area and based on the precipitation gradient, land use, and population density. The waters cannot be used as drinking water without prior treatment
Endbericht des Forschungsprojektes RuBuS
Der vorliegende Bericht behandelt die Ergebnisse des Forschungsprojektes
RUBUS, welches im Zeitraum November 2013 bis November 2015 von der Freien
Universität Berlin durchgeführt wurde. Gegenstand des Projektes ist die
Untersuchung der aktuellen Belastungssituation und der Dynamik der Sedimente
in der Rummelsburger Bucht als Teil der urbanen Spree in Berlin. Das Projekt
hat die Klärung der räumlichen Verteilung, Quantifizierung und Bewertung der
Schadstoffbelastung in den Sedimenten der Rummelsburger Bucht zum Ziel. Es
soll vor diesem Hintergrund die Ausbildung einer unbelasteten Sedimentauflage
geprüft werden, um damit auch der Frage nachzugehen, ob es möglicherweise zu
einer Remobilisierung von schadstoffbelasteten Sedimenten kommt. Um diese
Hypothese zu untersuchen wird ein indirekter Messansatz gewählt, der sowohl
die Erfassung der Randbedingungen als auch den qualitativen und quantitativen
Nachweis einer Sedimentremobilisierung berĂĽcksichtigt. Da die Prozesse als
solche nur schwer messbar sind, zielt dieser Ansatz darauf ab, entsprechende
Leitindikatoren zu wählen, anhand derer Mobilisierungsmechanismen und Ursachen
aufgezeigt werden können. Die Erfassung der Schadstoffe (Schwermetalle,
organische Verbindungen) erfolgt systematisch an 5 Schichten der obersten 15
cm des Gewässersedimentes und über die Erfassung von akkumuliertem Material in
Sedimentfallen. Die Beprobungen und kontinuierlichen Messungen werden an 15
über den gesamten Wasserkörper rasterförmig ausgelegten Bohr- bzw. Messpunkten
durchgefĂĽhrt. Zur Bemessung des potenziellen Risikos wird fĂĽr die
Feststoffphase der Consensus 2 - Wert der Sedimentqualitätsrichtlinien nach de
DECKERE et al. (2011) zugrunde gelegt und durch Elutionsversuche sowie
ökotoxikologische Tests ergänzt. Die Laborergebnisse zeigen, dass an allen
Standorten und in annähernd allen erfassten Sedimentschichten weitestgehend
sämtliche untersuchten Elemente und Verbindungen in zum Teil erheblichen
Konzentrationen nachgewiesen werden können. Die Konzentrationen variieren
sowohl in der Fläche als auch mit der Tiefe der Sedimentschichten. Die
Analysen und statistischen Tests weisen das nordwestliche Untersuchungsgebiet
als am stärksten belastet aus. Ungeachtet dieser räumlichen Variationen zeigen
die Ergebnisse, dass in der Rummelsburger Bucht eine durchgängige Belastung
der oberen 15 cm Sedimentschicht vorliegt. Eine flächendeckende Belastung kann
auch fĂĽr die beprobten Sedimentfallen nachgewiesen werden. Im Vergleich zum
Referenzstandort in der Spree zeigt sich, dass die Rummelsburger Bucht sowohl
hinsichtlich der Sedimentkerne als auch hinsichtlich der Sedimentfallen eine
durchgängig höhere Belastung aufweist. Effektbasierte SQG werden in den
meisten Fällen überschritten. Eine Untersuchung aquatischer Makrozoen durch
die Bundesanstalt für Gewässerkunde zeigt zudem, dass die Artenvielfalt gering
ist und sich das Vorkommen auf tolerante, euryöke Arten mit geringen
Ansprüchen an die Gewässer- und Sedimentqualität beschränkt. Für den hohen
gemessenen Sedimentumsatz ist vor allem die Remobilisierung von Sedimenten
innerhalb der Bucht verantwortlich. Die stark belasteten, sehr schluffhaltigen
Sedimente werden über eine permanente Strömung diffus über die gesamte
Seefläche verteilt. Als bisherige Ursache für den hohen Sedimentumsatz können
u.a. meteorologische Bedingungen und der Bootsverkehr identifiziert werden.
Die mechanische Mobilisierbarkeit von feststoffgebundenen Schwermetallen und
zinnorganischen Verbindungen ist unter den vorherrschenden Bedingungen in der
Rummelsburger Bucht gering. Die chemisch-physikalischen Randbedingungen des
Untersuchungsgebiets sind im Jahreszyklus nur geringen Schwankungen
unterworfen, was der weiteren Fixierung der Schwermetalle entgegenkommt. MKW
und PAK werden hingegen durch die Elution in höheren Konzentrationen
freigesetzt, insbesondere aus den Schwebstoffen. Im Fall der PAK werden in den
meisten Proben die ZHK-UQN bzw. die JD-UQN der Europäischen
Wasserrahmenrichtlinie fĂĽr die Wasserphase ĂĽberschritten. Keiner der
biologischen Tests zeigt eine gefährliche Belastung an. Es werden jedoch mit
dem Sedimentkontakt- und dem Leuchtbakterientest bei mehreren Proben kritische
Belastungen ermittelt. Von den PAK geht offensichtlich keine Gefährdung für
die Testorganismen Vibrio fischeri (Leuchtbakterien) und Lemna minor
(Wasserlinsen) aus. Die Wasserlinsen reagieren durchgehend wenig sensitiv auf
die Inhaltsstoffe der Eluate. Es ist anzunehmen, dass die signifikant höhere
MKW-Freisetzung aus den Schwebstoffen (im Gegensatz zu den Sedimenten) die
toxische Wirkung im Leuchtbakterientest verursacht. Der Sedimentkontakttest
weist bei einer den Schadstoffgehalten nach relativ unbelasteten Probe einen
toxischen Effekt nach. Die hohen Schwermetallgehalte in den Sedimenten haben
keine Wirkung auf die Bakterien des Sedimentkontakttests, was darauf
hindeutet, dass sie nicht in bioverfĂĽgbarer Form vorliegen. Die Schwermetalle
scheinen unter stabilen Bedingungen gebunden vorzuliegen. Die PAK und MKW
zeigen eine deutlich höhere Dynamik in der Schadstoffmobilität. Die
Rummelsburger Bucht stellt selbst im internationalen Kontext eine Besonderheit
hinsichtlich der hohen Belastung mit organischen Schadstoffverbindungen und
Schwermetallen dar und zeigt, dass die industriellen FingerabdrĂĽcke der
Gesellschaft über äußerst lange Zeiträume erhalten bleiben und dies eine
Herausforderung fĂĽr Politik und Planung darstellt. Die Untersuchungsergebnisse
zeigen aber auch, dass die Rummelsburger Bucht einer ausreichend groĂźen
Dynamik unterliegt, welche zu einer (Re-) Mobilisierung dieser hochbelasteten
Sedimente fĂĽhren kann. Die Sedimente fungieren als langfristige potenzielle
Schadstoffquelle für den Wasserkörper und damit auch für die Spree.The present report covers the results of the research project RuBuS, realised
by the Freie Universität Berlin between November 2013 and 2015. The
investigated water body “Rummelsburger Bucht” is a former anabranch of the
Spree River located in the centre of Berlin. Covering an area of more than 45
ha, it is only at the upstream side connected to the main river course. For
almost a century, untreated industrial and municipal wastewater was discharged
into this river branch. Consequently, the quality of both the water and the
sediments decreased dramatically over that period. In order to address this
problem, the project “RuBuS” (co-financed by the Berlin State Government and
the European Funds for Social and Regional Development) was established for
the above mentioned period. To perform any risk assessment, the investigation
should provide an improved knowledge and a better understanding about the type
and spatio-temporal pattern of sediment contamination and dynamics. To detect
the spatial distribution of pollutants in the sediment, over 200 sediment
samplings were carried out via drill cores from 16 locations. The upper 15 cm
of each drill core was systematically divided into 5 layers (each of 3 cm) for
separate examination. The investigation of sedimentation and remobilisation
rates was accomplished by installing 18 sediment traps, which collected
deposits over more than a year. The presence of selected heavy metals and
organic pollutants in the sediments was determined for every position and
layer of the drill cores, as well as for all sediment traps. Detection of
changes in boundary conditions, influencing the spatial and temporal
distribution of sedimentation and resuspension, was accomplished by placing
devices within the water body and taking different mobile measurements. At all
sampling locations, flow conditions were recorded every week over the whole
water column with a vessel-mounted ADCP (Acoustic Doppler Current Profiler).
Water quality parameters like oxygen, turbidity, chlorophyll-(a) and
temperature were also measured weekly with a mobile multiparameter sensor at
all stations in 50 cm steps. In addition, these parameters were continuously
recorded every 10 minutes with stationary sensors at different water depths
(1, 2 and 3 m) from the beginning of the monitoring. For mobile measurements
the probe YSI 6600 V2 was used, whereas permanent recording was done with
Cyclops-7 and MiniDot devices from PME. A weather station was set up on the
shore side to determine wind conditions, precipitation, temperature and solar
radiation, concerning the external impacts on water currents, turbulences and
algae-bloom. The scope of the investigation included the determination of the
total content of inorganic (Hg, Cd, Cr, Pb, Ni, Cu, Zn) and organic compounds
(polycyclic aromatic hydrocarbons (PAH), total petroleum hydrocarbons (TPH),
selected nitro-compounds, selected organotin compounds and polychlorinated
biphenyls (PCB, AOX and EOX) in the sediment and suspended matter. The
relevant particle size for the investigation of samples for heavy metals was <
63 ÎĽm and for the organic components < 2 mm. The compounds were detected by
ICP-OES, ICP-MS and AAS analyses. Grain size distributions weredetermined
using laser diffractometry and sieving. An elemental analyser was used to
determine the presence of carbon and nitrogen in the samples. The release of
soluble components upon contact with water is considered one of the main
mechanisms leading to a potential hazard to the environment. The research into
soluble and easily mobile sediment-bounded pollutants is based upon a 24 hour
batch test. In addition, certain toxic effects of the sediments were
determined by ecotoxicological test methods. Three species were chosen as
relevant test organisms: Vibrio fischeri for the luminescent bacteria test,
Lemna minor for the Duckweed growth inhibition test and Arthrobacter
globiformis for the sediment contact test. In addition, the thresholds of the
sediment quality guidelines, published by de Deckere et al. (2011), were used
to assess the solid contents. The study demonstrated that so far the
concentration of organic and inorganic pollutants in the sediments has
remained very high. The total contents of the PAHs and all heavy metals
exceeded the effect-based threshold values according to de Deckere et al.
(2011). The results were compared to the “consensus 2” thresholds to identify
the measured concentrations, which have surpassed the limits and now giving
rise to concern regarding toxicity. The only exception among the heavy metals
was mercury. With respect to organic pollution the reference point in the
Spree River, which is not very far away from the sheet pile wall, showed
concentrations below the threshold value. In contrast, the reference point
disclosed pollution by heavy metals except for cadmium and mercury
concentrations, which were below the threshold. However, the load of heavy
metals at the reference point was lower than the one found in the bay. A
different spatial distribution of the organic contamination was observed for
the sediments of the “Rummelsburger Bucht”. In terms of contamination with
PAHs, Cd and Pb, areas with different loads could be defined, this was
statistically proven with a significant difference greater than 99%. The less
contaminated area was situated between the sheet pile wall and the centre of
the bay. Higher loads (sampling sites 10-15) were found from the centre of the
water body to the north-western shore. However, the sediments in the traps
showed a homogeneous distribution of the measured pollutants. It was also
found, that the level of contamination commonly increased with sediment depth,
except at the sampling sites right in the centre of the bay, which revealed no
clear tendency to increase or decrease depending on the depth. With regard to
the level of the European Environmental Quality Standards (EQS), the results
of the 24 hour batch test indicated a low mobility of the heavy metals,
organotin compounds and Benzo(a)pyrene. By contrast, other PAH compounds
exceeded in several eluates the annual average maximum concentration permitted
by the EQS. The results of the Luminescent bacteria test demonstrated for the
eluates of sediment cores, that all samples are not or harmless polluted (non-
or low toxic effect). However, with the exception of two samples, all of the
eluates of suspended particles were critically polluted, they showed a
moderate or increased toxic effect. The recorded high turnover rates of
sediments were most likely caused by a remobilisation of local sources within
the “Rummelsburger Bucht”. These highly contaminated and silty sediments can
be evenly distributed over the whole area of the water body due to very slow
but constant currents with changing directions. Up to now, specific
meteorological boundary conditions and motorboat-traffic have been identified
as some of the main reasons for the remobilisation and local transport of the
sediments, as well as external sediment sources could be neglected. The
research project “RuBuS” provides a detailed insight into this water body. It
gives a better understanding how changes in boundary conditions affect the
spatial and temporal distribution of sedimentation and the resuspension of
sediments. The study demonstrates, that so far the concentration of organic
and inorganic pollutants in the sediments has remained on an exceptionally
high level. The “Rummelsburger Bucht” can be considered as a case study about
spatio-temporal pattern of sediment contamination and dynamics of the Spree
River and about areas of conflict presented by highly stressed urban water
bodies. A high pressure on demands of local residents for recreational and
commercial use of the “Rummelsburger Bucht” needs to improve the environmental
situation by a targeted and affordable management plan
Microplastics in Namibian river sediments – a first evaluation
The African continent is rarely the focus of microplastics research, although the ubiquity of microplastics in the environment is undisputed and still increasing. Due to the high production and use of plastic products and the partial lack of recycling systems in many parts of the African continent, it can be assumed that microplastic particles are already present in limnic and terrestrial ecosystems. Few studies, mainly from South Africa and the Northern African region, show a contamination with microplastics, especially in marine environments. This study aims to explore the presence and composition of microplastics in fluvial sediments of the major catchments in Namibia with a regional focus on the Iishana system in Northern Namibia, as one of the most densely populated areas in the country. In March 2019 and March 2021, at the end of the rainy seasons, sediments from the Iishana system and of the largest river catchments were sampled. Extraction was performed by density separation using the Microplastic Sediment Separator (MPSS) with the separation solution sodium chloride (density of 1.20 g/cm3). The particle size was determined by filtration and fractionation, and the polymer type by measurement with ATR-FTIR spectroscopy (minimum particle size 0.3 mm). Microplastics were found in the sediments of each river system, most of the particles in the Iishana system (average of 13.2 particles/kg dry weight). The perennial, the ephemeral rivers, and the Iishana system are similar concerning polymer type and particle size. Polyethylene and polypropylene were the dominant polymer types. Most of the particles were found in the size fractions 0.3 – 0.5 mm and 0.5 – 1.0 mm. The particles were found mainly as fragments and films, the majority transparent and brown
GNSS mobile road dam surveying for TanDEM-X correction to improve the database for floodwater modeling in northern Namibia
The aim of this study is the improvement of the TanDEM-X elevation model for future floodwater modeling by implementing surveyed road dams and the use of filter algorithms. Modern satellite systems like TanDEM-X deliver high-resolution images with a high vertical and horizontal accuracy. Nevertheless, regarding special usage they sometimes reach their limits in documenting important features that are smaller than the grid size. Especially in the context of 2D-hydrodynamic flood modelling, the features that influence the runoff processes, e.g. road dams and culverts, have to be included for precise calculations. To fulfil the objective, the main road dams were surveyed, especially those that are blocking the flood water flowing from south Angola to the Etosha Pan in northern Namibia. First, a Leica GS 16 Sensor was installed on the roof of a car recording position data in real time while driving on the road dams in the Cuvelai Basin. In total, 532 km of road dams have been investigated during 4 days while driving at a top speed of 80 km/h. Due to the long driving distances, the daily regular adjustment of the base station would have been necessary but logistically not possible. Moreover, the lack of reference stations made a RTK and Network-RTK solution likewise impossible. For that reasons, the Leica SmartLink function was used. This method is not dependent on classic reference stations next to the GNSS sensor but instead works with geostationary satellites sending correction data in real time. The surveyed road dam elevation data have a vertical accuracy of 4.3 cm up to 10 cm. These precise measurements contribute to rectifying the TanDEM-X elevation data and thus improve the surface runoff network for the future floodwater model and should enhance the floodwater prediction for the Cuvelai Basin
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