Treatment of ballast water; how to test a system with a modular concept?

A variety of methods were successfully applied to examine the efficacy of a modular ballast water system according to the standards as adopted by the International Maritime Organization. The ballast water treatment system had a capacity of 530 m3 h(-1) consisted of a pump system, a hydrocyclone, a 50 microm mesh-size self-cleaning filter and an installation for the addition of a chemical disinfectant (PERACLEAN Ocean). The land-based testing facility used natural sea water of high turbidity during the spring phytoplankton bloom. The mesozooplankton fraction was inspected with a standard binocular. Larger zooplankton were effectively removed with the filter; the smaller sized fraction containing larvae and nauplia were killed after chemical treatment. The phytoplankton component was monitored using flow cytometry. The huge colonies of the phytoplankton Phaeocystis globosa were disrupted in the hydrocyclone liberating the colony cells which passed as single cells through the filter. These cells remained viable but were finally killed in the secondary (chemical) step. Bacteria also passed all mechanical treatment steps unharmed but were killed in the final step. Viability tests with SYTOX Green, which were specifically designed for phytoplankton, showed that mechanical treatment did not affect the percentage of viable cells a short-term, but after several hours the viable cell counts dropped down to 70%. Phytoplankton cells recovered within a single day and formed a new dense bloom rapidly. The bacteriostatic component of the chemical disinfectant (H2O2) remained present for several days preventing regrowth of bacteria for up to 15 days after addition. In conclusion, the IMO standards were met using the modular ballast water treatment unit and the applied instruments and assays were effective and rapid tools to qualify and quantify the organisms present as well as their viability.

Formation and long-term fate of non-extractable residues in outdoor lysimeter studies.

Long-term outdoor lysimeter studies using (14)C-labelled compounds allow the quantification of the 'non-extractable residue fraction'. More than 20 lysimeter studies under realistic environmental conditions showed that more than 80% of residual carbon of the molecule is retained in the topsoil layer even after several years. Generally, 50-90% of this residual radiocarbon is regarded as 'soil bound residue'. Microbial biomass is present in large quantities in topsoil and continuously influences chemical and biochemical alteration of pesticide molecules that may interact directly with the total soil organic matter. Labelling techniques using radioactive isotopes like (14)C have been used to characterize these residues in the humus matrix. Our studies have been directed to the investigation of extractability and/or bioavailability of these residues in long-term investigations.

Characterisation of soil-bound residue fractions of the fungicide dithianon by gel permeation chromatography and polyacrylamide gel electrophoresis.

The degradation of the (14)C-labelled fungicide dithianon in an orthic luvisol was investigated under standardized conditions in comparison to stimulated microbial activity by an amendment of maize straw. The compound is characterized by mineralization losses of approximately 33% and the formation of non-extractable bound residues of approximately 63% in 64 days. Despite the major role of microorganisms in mineralizing this compound, the formation of bound residues is not biotically induced. Gel permeation chromatography and polyacrylamide gel electrophoresis, as different size separation techniques of the humic acids fractions, showed differences in the distribution patterns of non-extractable residues depending on the addition of straw material. The results presented support the existence of humic substances in soil as a micellar system rather than as a biopolymer.

Microbial release and degradation of nonextractable anilazine residues.

Humic substance fractions obtained from a degraded loess soil taken from a long-term lysimeter experiment with the fungicide anilazine were incubated in aerated liquid cultures together with native soil microorganisms. Biomineralization, remobilization of [U-phenyl-(14)C]anilazine, respectively, its metabolites, and changes of the humic matrix were observed under variable nutrient conditions. Stimulated microbial activity favored the degradation of nonextractable (14)C-anilazine residues. However, nitrogen deficiency enhanced structural changes in the humic substances, which seemed to be used then as a nitrogen source. Along with the microbial degradation of the humic substances, parts of the bound anilazine residues became remobilized. Furthermore with the use of AMD-TLC, dihydroxy anilazine was detected within the nonextractable residues. The portion of rather weak bondings between the soil organic acids and the anilazine residues turned out to be considerably lower in the humic acids fractions than in the fulvic acids fraction.

A wind tunnel for measuring the gaseous losses of environmental chemicals from the soil/plant system under field-like conditions.

Volatilization from treated areas is a major source of pesticide residues in air, fog, and rain. This may lead to long-range transport of pesticide residues to remote areas. Up to now most information on pesticide volatilization has come from laboratory experiments under controlled conditions. A new system has been designed and developed to measure the volatile losses of(14)C-labelled chemicals after application; the method compares with agricultural practice of treating soils or plants grown in lysimeters. Sensitive analytical methods guarantee a distinction between residues of unchanged pesticide, its metabolites or(14)CO2 as a mineralization product released into the air.

Aged and bound herbicide residues in soil and their bioavailability. Part 2: Uptake of aged and non-extractable (bound) [carbonyl-14C]methabenzthiazuron residues by maize.

[Carbonyl-14C]methabenzthiazuron (MBT) was applied to growing winter wheat in an outdoor lysimeter. The amount applied corresponded to 4 kg Tribunil/ha. 140 days after application the 0-2.5 cm soil layer was removed from the lysimeter. This soil contained about 40% of the applied radioactivity. Using 0,01 M CaCl2 solution or organic solvents, the extractable residues were removed from the soil. The bioavailability of the non-extractable as well as aged residues remaining in the soil was investigated in standardized microecosystems containing 1.5 kg of dry soil. During a 4 weeks period the total uptake (4 maize plants/pot) amounted up to 3.6; 2.2; and 0.9% of the radioactivity from soils containing aged MBT residues, MBT residues non-extractable with 0.01 M CaCl2 or MBT residues non-extractable with organic solvents, respectively. About 20% of the radioactivity found in maize leaves represented chromatographically characterized parent compound. At the end of the plant experiment the soil was extracted again with 0.01 M CaCl2 and with organic solvents. The soil extracts and also the organic phases obtained from the aqueous fulvic acid solution contained unchanged parent compound.