Cyanobacterial toxins are toxic substances produced by cyanobacteria or blue-green-algae. The can occur in surface waters wordwide and have to be removed sufficiently when using infested surface waters as drinking water source. Bank filtration has been used since 150 years for drinking water (pre-)treatment and utilizes natural elimination processes like sorption and degardation in the sub-surface. During several research projects the German Federal Environmental Agency (Umweltbundesamt, UBA) carried out field investigations and experiments in different scales in order to assess under which conditions secure elimination of microcystins (the most common group of cyanobacterial toxins) takes place. Filtration of cells on the sediment surface is the most prominent process for eliminating the primarily cell-bound toxins. Middle to coarsly grained sands eliminated more than 99.9 % of intracellular toxins within the first 10 centimeters. Elimination of extracellular microcystin during underground passage is mainly due to biodegradation. Reversible adsorption processes do not reduce the total load but lead to longer contact times for extended biodegradation. Laboratory experiments showed that high clay and silt content is crucial for maximum adsorption. However, redox conditions play an important role for degradation rates: under aerobic conditions half lives of less than one day occured frequently whereas anoxic conditions resulted in lag phases of one day and more as well as in half lives of up to 25 days. Field experiments could show that temperature is crucial for degradation velocity under natural conditions.

Cyanobacterial toxins are substances produced by cyanobacteria that occur in surface waters world wide. The most common group of cyanobacterial toxins is the group of structurally similar microcystins (MCYST). Sand passage as used in slow sand filtration, artificial recharge and bank filtration has shown to be effective in eliminating microcystins in many cases. For secure drinking water production from surface waters infested by microcystins removal has to be ensured in a wide variety of cases met in the field. It was therefore the aim of experiments in technical and semitechnical scale on the UBA’s experimental field in Berlin to test some worst case scenarios for the reliability of microcystin elimination during sand passage. Experiments were conducted with virgin sand (no previous contact to MCYST) and high filtration rates as well as under anaerobic conditions. The results show that the greatest problem for MCYST elimination can be found under anaerobic conditions as degradation is not complete and may lead to harmful residual concentrations.

After installation of phosphorus elimination plants at the inflows of the eutrophic Lake Tegel and Schlachtensee, phosphorus (P) loading declined by a factor of 40 and 100, respectively. This resulted in a pronounced reduction of phosphorus concentrations in the lake water, followed by a decline of chlorophyll-a concentrations. However, for many years P release from sediments due to mineralization and desorption of sedimentary P continued. In Schlachtensee, the presence of nitrate above the sediment suppresses P release, because the Fe/P ratio is sufficient to provide enough aerobic sorption capacity. In Lake Tegel, some P release occurs even under aerobic conditions because of the low aerobic P sorption capacity of the sediments. There, nitrate could moderate the P release peaks which occur when the Fe-P cycle at the sediment water interface is disturbed by precipitation of iron sulfide after reduction of sulfate during times of high mineralization intensity. The potentially mobile P pool in the sediments of both lakes is rather small, indicating that the P release could subside after sufficient reduction of the external P load in Lake Tegel and the disruption of the internal P cycle in Schlachtensee.

Microcystins (MCYST) are a group of toxic substances produced by cyanobacteria (‘blue-green-algae’). In case of cyanobacterial blooms microcystin concentrations in surface waters may reach values far above the value proposed as provisional guideline for drinking water by the WHO of 1 µg/L for MCYST-LR. For drinking water production via underground passage it is therefore necessary to ensure removal to a large extent. For this reason experiments with extracellular microcystins were conducted in the laboratory as well as in a natural setting on the UBA’s (German Federal Environmental Agency) experimental field for simulation of underground passage. Laboratory batch experiments showed that adsorption of microcystins can be neglected in sandy material (kd < 1 cm³/g). Batch and column experiments identified biodegradation as the predominant elimination process in these sediments. The degradation rates derived from laboratory column experiments as well as semi-technical scale enclosure experiments varied between 0.2 d–1 and 18 d–1. In the worst case this means a half life of 2.8 days, so that under aerobic conditions contact times of several days should be sufficient to eliminate MCYST to an extent safe for use as drinking water.

Cylindrospermopsin (CYN) is a potent hepatotoxin produced by different cyanobacteria of the order Nostocales, which is widely distributed in freshwaters and considered a hazard to wildlife and humans. In Europe, only Aphanizomenon flos-aquae is identified as CYN producer so far and the seasonal variability of CYN was not studied yet. Therefore, we studied the seasonal dynamics of the particulate and dissolved CYN concentrations in relation to the cyanobacterial occurrence and environmental factors in two German lakes over two years. Total CYN reached maximum concentrations of 0.34 and 1.80 µg L-1 in Melangsee and Langer See, respectively. In both lakes, the dissolved CYN fraction peaked after the particulate fraction, and reached higher values indicating that CYN is poorly decomposed and accumulates in the water. The cyanobacterial community was very diverse in both lakes, including potentially CYN producing species such as Cylindrospermopsis raciborskii, Anabaena bergii and Aphanizomenon flos-aquae. However, these species could be excluded as the major CYN producers. The stronges significant correlation was found for Aphanizomenon gracile and CYN, strongly indicating that the species is the main CYN producer in Langer See. CYN was also correlated with Planktothrix agardhii in Langer See and Pseudanabaena limnetica in Melangsee, but species of the order scillatoriales are not known to produce CYN. In Melangsee the CYN producer could not be identified. Different correlations of CYN with abiotic factors in the two lakes indicate the presences of further undetected CYN producers as well as different regulation mechanisms of their dynamic and the variability of CYN.