This master thesis deals with the interaction of humic acids with organic ions and effect of chemical modification of humic acids on this interaction. Rhodamine 6G was used as a model organic ion. The interaction were studied by fluorescence quenching, dialysis in diffusion cells and differential UV-VIS spectroscopy. Results showed that the bond between the reactants was not primarily dependent on carboxylic functional groups of humic acids. Fluorescence experiments indicated static quenching mechanism and differential UV-VIS spectroscopy demonstrated the existence of - interactions.

Les ressources en eau sont menacées par diverses formes de pollution et les procédés de traitement proposés sont souvent complexes avec des résultats qui ne sont pas toujours satisfaisants. Cette étude vise à développer un traitement, simple et peu coûteux pour réduire au maximum la présence dans l’eau des acides humiques (AH), un polluant organique. L’approche adoptée est la mise en place d’un procédé hybride combinant l’adsorption et la photocatalyse hétérogène réalisée avec le dioxyde de titane. La méthode d’adsorption a été réalisée d’une part avec du charbon actif et d’autre part avec trois argiles provenant de la Côte d’Ivoire. Le charbon actif a été préparé à partir des coques de coco selon une procédure assez simplifiée, sans additifs chimiques, dans le souci d’obtenir un adsorbant économique et écologique. Les trois argiles brutes (Dabou, Yamoussoukro et Katiola) ont chacune subi des opérations de purification pour obtenir des fractions pures. Des tests de caractérisation réalisés par diverses techniques (analyse élémentaire, DRX, adsorption d’azote, IR, etc.) ont été effectués sur les adsorbants obtenus. Les essais d’adsorption réalisés avec le charbon ont montré qu’aucune élimination des AH n’a été observé. La raison principale serait le manque de groupements fonctionnels sur la surface du charbon préparé. Les tests d’adsorption conduit avec les argiles ont montré que ces matériaux sont capables d’éliminer les AH. Les résultats ont révélé que l’argile la plus riche en kaolinite (celle de Yamoussoukro) a une capacité d’adsorption maximale largement supérieure (115 mg/g) par rapport aux autres (20 et 15 mg/g pour Dabou et Katiola respectivement). Cette différence trouve son explication dans la composition minéralogique et structurale de chacune des argiles. Les tests de photocatalyse menés ont montré une dégradation des macromolécules d’AH en des composés de plus petites tailles. La minéralisation de la matière organique a été observée avec une réduction du carbone organique total de l’ordre de 72 et 82 % respectivement aux pH 7 et 3. En mettant en série à pH 3, les deux procédés à savoir l’adsorption suivie de la photocatalyse, une réduction de 95% du carbone organique total des AH est obtenue. Le procédé hybride ainsi réalisé montre un avantage certain car il permet d’éliminer la quasi-totalité de la pollution organique initiale. / Water resources are threatened by various forms of pollution and the proposed treatment processes are often complex with results that are not always satisfactory. This study aims to develop a simple and inexpensive treatment to minimize the presence of humic acids (HA), an organic pollutant, in water. The approach adopted is the establishment of a hybrid process combining adsorption and heterogeneous photocatalysis performed with titanium dioxide. The adsorption method was carried out primary with activated carbon and secondary with three clays from Ivory Coast. Activated carbon was prepared from coconut shell by a simplified procedure, without chemical additives, in order to obtain an economic and ecological adsorbent. The three raw clays (Dabou, Yamoussoukro and Katiola) each underwent purification operations to obtain pure fractions. Characterization tests including various techniques (elemental analysis, XRD, nitrogen adsorption, IR, etc.) were carried out on the adsorbents obtained. Adsorption tests carried out with the coal showed that no elimination of HA was observed. The main reason is the lack of functional groups on the surface of the prepared coal. The adsorption tests conducted with the clays have shown that these materials are capable of removing HA. The results revealed that the clay richest in kaolinite (Yamoussoukro) has a much higher maximum adsorption capacity (115 mg/g) compared to the others (20 and 15 mg/g for Dabou and Katiola respectively). This difference found its explanation in the mineralogical and structural composition of each of the clays. Photocatalysis tests showed a degradation of the macromolecules of HA into smaller sizes compounds. The mineralization of the organic matter was observed with total organic carbon reduction rate equal to 72 and 82% at pH 7 and 3 respectively. By placing in series the two processes namely adsorption followed by photocatalysis, the removal percentage of HA obtained at pH 3, is about 95%. This hybrid process shows an advantage since it makes it possible to eliminate almost all of the initial organic pollution.

F�r die Therapie und Prophylaxe von Fischkrankheiten stehen nur wenige geeignete und zugelassene Medikamente zur Verf�gung. Daher kommt der Suche nach wirksamen und f�r Tier, Verbraucher und Umwelt sicheren Alternativen in der Fischhaltung eine besondere Bedeutung zu. �ber positive Effekte beim oralen Einsatz von Huminstoffen an landwirtschaftlichen Nutztieren, Zootieren und Heimtieren liegen eine Vielzahl von Berichten vor. Deshalb sollten in der vorliegenden Studie Huminstoffe (HS) in der �u�erlichen Anwendung bei Zierfischen und in der oralen Verabreichung �ber das Futter bei Nutzfischen n�her untersucht werden. Dazu wurden zwei Versuche (B I: Dauer 4 Tage; B II: Dauer 12 Tage) an Goldfischen (Carassius auratus) unter teichwirtschaftlichen Bedingungen, zwei Aufzuchtversuche (F I: Kv bis K3, Dauer: 1.000 Tage: F II: K0 bis K1, Dauer: 150 Tage) an Karpfen (Cyprinus carpio) in der Teichwirtschaft und ein Aufzuchtversuch (F III: vorgestreckte Brut bis 30 g Lebendmasse, 166 Tage) an Regenbogenforellen (Oncorhynchus mykiss) unter Laborbedingungen durchgef�hrt. Als Versuchsparameter dienten Mortalit�t und Morbidit�t, Wachstum und Futteraufwand in den Aufzuchtversuchen, pathologisch anatomische (einschlie�lich histologischer Befunde in B I und F II), parasitologische, bakteriologische und virologische Kriterien. Die Wasserqualit�t wurde regelm��ig ermittelt. In den Versuchen B I und B II wurde eine 10%ige Na-Humat-L�sung (HS vom Typ WH 67 SNa der Fa. Pharmawerk Weinb�hla) dem H�lterungswasser so zugesetzt, dass eine Na-Humat-Konzentration von 10 mg L-1 entstand. Zweij�hrige, multifaktoriell erkrankte Goldfische (B I: N=2 x 322, B II: N=2 x 100) wurden dem Na-Humat-Bad t�glich f�r die Dauer einer Stunde (B I) bzw. von 1,5 bis 2 Stunden (B II) ausgesetzt. Die HS-Badehandlungen f�hrten in beiden Versuchen zu einer Senkung der Verluste (Mortalit�tsrate in B I: 0,6 versus 4,7 %, p<0,0005; B II: 8 versus 16 %, p<0,05). Bei Versuchsende war in den Versuchsgruppen (Na-Humat-Bad) der Gesundheitszustand, beurteilt nach �u�erlich sichtbaren Ver�nderungen an Haut, Flossen und Kiemen, deutlich verbessert (B I: p<1�10-16; B II: p<0,001). So waren (Signifikanzangaben nur f�r B II) vor allem H�morrhagien der Haut und der Flossen (p<0,05), Flossenrand- und Kiemennekrosen (p<0,05) sowie akute Kiemenentz�ndungen (p<0,02) verringert. Die Badebehandlungen bewirkten weiter eine geringere Auspr�gung integument�rer Mykosen der Haut, Flossen und Kiemen durch Pilze der Gattung Saprolegnia (p<0,05). Der Befall von Haut und Kiemen mit vorrangig protozo�ren Ektoparasiten konnte insgesamt ebenso vermindert werden (p<0,01) wie der Befall der Kiemen mit Ichthyophthirius sp. (p<0,05). Aus der beobachteten Milderung von Krankheitssymptomen umweltbedingter, bakterieller, ektoparasit�rer und mykotischer Genese nach Na-Humat-B�dern bei Goldfischen kann auf einen gewebeprotektiven, antiphlogistischen, antimykotischen und antiparasit�ren Effekt der Na-Humat-Behandlung geschlossen werden. In der Aufzucht von Karpfen (F I) und Regenbogenforellen (F III) wurden dem Futter 5 % Humocarb, formuliert� (HS vom Typ WH 67 A), im Karpfenversuch F II 5 % Cellu-Ligno-Karbon-Isolat (HS vom Typ WH 67 G, beide Produkte: Fa. Pharmawerk Weinb�hla) zugesetzt. In F I und F III wurde ein gleiches pelletiertes Alleinfutter f�r Forellen, in F II ein pelletiertes Alleinfutter f�r Karpfen eingesetzt. In Versuch F I (Besatzdichte der beiden Teiche (0,2 ha) jeweils 35.000 Kv ha-1) wiesen die Karpfen der Versuchs- gegen�ber der Kontrollgruppe h�here mittlere K�rpermassen auf. Der Unterschied zwischen den Gruppen bewegte sich mit einer Ausnahme (zu geringer Stichprobenumfang) zwischen p<0,05 (65 versus 45 g, 114. Tag) und p<0,0001 (1.146 versus 855 g, Versuchsende 1000. Tag). Der um die HS-Aufnahme bereinigte Futteraufwand des ersten Versuchsjahres war durch HS um 34 % verbessert. Die Futterquotienten in der zweiten und dritten Aufzuchtperiode waren durch die subjektive Futterzumessung (Nichtber�cksichtigung zwischenzeitlicher Verluste) verf�lscht. In Versuch F II (Besatzdichten der 2 x 3 Teiche (0,25 ha) 20.000, 30.000 bzw. 40.000 K0 ha-1) erhielten die Br�tlinge �ber die ersten zwei Wochen kein zus�tzliches Futter (nur Naturnahrung), anschlie�end wurde Weizenschrot zugef�ttert, erst ab dem 63. Tag das Versuchs- bzw. Kontrollfutter f�r 87 Tage. Bei Versuchsende war in den Gruppen der h�chsten Besatzdichte die Mortalit�t durch HS um ca. 20 % verringert (p<0,0001). Die Abfischungsmassen waren bei geringer Besatzdichte ann�hernd gleich, bei mittlerer Besatzdichte war die Kontrollgruppe, bei h�chster Besatzdichte die Versuchsgruppe favorisiert (statistische Pr�fung wegen des Fehlens von Einzeldaten nicht m�glich). Der um die HS-Aufnahme bereinigte Futteraufwand war in den HS-Gruppen bei geringer bzw. h�chster Besatzdichte um 5 bzw. 17 % verringert. In beiden Versuchen, F I und F II, wurde eine deutliche Verringerung des Gehaltes der inneren Organe Leber, Niere und Milz an fakultativ pathogenen Aeromonas- und Pseudomonas spp. nachgewiesen (p<0,05). Bei der Aufzucht von Regenbogenforellen (F III; N=2 x 25) trugen die durch den HS-Zusatz bedingten Ver�nderungen der Konsistenz von Futter und Kot zur Verminderung einer starken Belagbildung (Bewuchs aus Algen und anderen Mikroorganismen) sowie zur Vermeidung von Wassertr�bungen in den Aquarien, insbesondere bei h�heren Temperaturen, bei. Signifikante Unterschiede in den Kenndaten von Wachstum und Futteraufwand wurden nicht beobachtet. Insgesamt gesehen erscheint aber der Zusatz von 5 % HS zum Futter als zu hoch gew�hlt, da sich der Futteraufwand in den HS-Gruppen bei Ber�cksichtigung der Gesamtfuttermenge (einschlie�lich des 5%igen HS-Zusatzes) �berwiegend ung�nstiger gestaltete. Die Effekte der oralen Applikation von 5 % HS im Futter sind damit weit weniger augenf�llig als nach �u�erlicher Anwendung. Die zootechnischen Parameter waren �berwiegend mehr oder weniger unver�ndert; allein in Versuch F I war die K�rpermasse in der HS-Gruppen im Versuchsverlauf (Stichproben und Abfischung) in der Regel signifikant h�her als in der Kontrollgruppe. Von k�nftiger Bedeutung f�r die Aquarienhaltung von Fischen (und m�glicherweise in Klein- und Zierteichen) k�nnte die beobachtete Wasserkl�rung und die Verminderung einer Belagbildung aus Algen und anderen Mikroorganismen sein. Eine intestinale Wirkung der HS wird insoweit unterstellt, als in beiden Karpfenversuchen die inneren Organe einen verminderten Befall an beweglichen Aeromonaden und Pseudomonaden aufwiesen. / Prophylactic and therapeutic use of brown coal-derived humic substances of the type WH 67 in finfish and ornamental fish farming On the market, there is a limited number of suitable and approved drugs available for therapy and prophylaxis of fish diseases. The search for alternatives which are both effective and safe for animals, consumers and environment is therefore of special importance. There are numerous reports on positive effects of orally administered humic substances (HS) on agricultural livestock, zoo animals and pets. Therefore, the present study aimed on effects of HS for both external treatment of ornamental fish and oral application on culture fish via feed. Two experiments on goldfish (Carassius auratus) (exp. B I: 4 days; exp. B II: 12 days), and on common carp (Cyprinus carpio) (exp. F I: 1,000 days, fry to 3-year-old fish ; exp. F II: 150 days, fry to young-of-the-year size) were carried out under pond culture conditions. Additionally, one experiment on rainbow trout (Oncorhynchus mykiss) was carried out in the laboratory (exp. F III: 166 days, fingerlings up to 30 g body weight). The following parameters were examined: mortality, morbidity, growth, feed conversion ratio (exp. F I, F II, F III only), pathologic anatomical criteria (including histological examination of fish from B I and F II), parasitological investigation, bacteriological and virological state. Water quality was regularly examined as well. In the experiments B I and B II, a 10% sodium-humate solution (type WH 67 SNa, Pharmawerk Weinb�hla) was mixed into the water until a sodium-humate concentration of 10 mg L-1 was reached. Two-year old, multifactorially diseased goldfish (B I: N= 2 x 322; B II: N= 2 x 100) were daily exposed to this water for a period of one (B I) and 1.5-2 (B II) hours, respectively. In both experiments the treatment of fish reduced in mortality (B I: 0.6 vs. 4.7 %, p<0.0005; B II: 8 vs. 16 %, p<0.05). Moreover, at the end of the experiments the sodium-humate treated fish showed a significantly improved health state (B I: p<10-16; B II: p<0.001) as indicated by externally visible changes of the skin, fins and gills. Specifically, reductions in haemorrhage of skin and fins (B II: p <0.05), and fin and gill necroses (B II: p<0.05), and gill inflammations (B II: p<0.02) were noted. Additionally, the sodium-humate treatment reduced integumental mucoses of skin, fins and gills (p<0.05) caused by Saprolegnia sp. The infection of skin and gills with protozoan parasites was reduced (p<0.01) as well. Ichthyophthirius sp. infections of the gills dropped significantly (p<0.05) in the treated fish groups as compared to the controls. Due to the observed mitigation of disease symptoms of environmental, bacterial, parasitic and fungal origin after a sodium-humate bath treatment of goldfish, a tissue protective, antiphlogistic, antimycotic and antiparasitic effect of sodium-humate can be concluded. For rearing of carp (F I) and rainbow trout (F III), 5 % Humocarb, formuliert� (type WH 67 A, Pharmawerk Weinb�hla) was mixed among the feed, while for the experiment F II 5 % Cellu-Ligno-Carbon-Isolat (type WH 67 G, Pharmawerk Weinb�hla) was added. In F I and F III a complete feed for trout was applied whereas for F II a complete feed for carp was used. In experiment F I (stocking density of both ponds 35,000 carp fry per ha) test fish revealed a higher mean body weight compared to the controls. With one exception (sample size to small), the difference between the groups was either significant (day 114: 65 vs. 45 g, p<0.05) or highly significant (day 1000: 1,146 versus 855 g, p<0.0001). The feed conversion ratio of the first experimental year (expurgated by HS-uptake) improved by 34 % due to HS application. Feed conversion ratio of the second and third year were falsified because of subjective feeding (which does not consider occurring losses). In experiment F II (stocking density of the 2 x 3 ponds (0,25 ha) were 20,000, 30,000 and 40,000 individuals per ha, respectively) no additional feed was given to the hatched fry during the first two weeks so that all the fish lived on natural feed items. Afterwards, bruised wheat grain was given until from day 63 either test or control feed was applied for a total of 87 days. At the end of the experiment, at the highest stocking density the mortality was significantly (p<0.0001) decreased by 20% in the test group supplied with HS. At low stocking density the total weight of fish at harvest was not different between the test and control group. However, at medium stocking density the average body weight was higher in the control whereas reverse conditions were observed at the highest stocking density (due to a loss of data no statistical analysis was possible). The feed conversion ratio (expurgated by the uptake of humic substances) was decreased in the test groups of low (5 %) and high (17 %) density. In both experiments (F I and F II) significantly reduced infections of the internal organs liver, kidney and spleen with potentially pathogenic Aeromonas and Pseudomonas spp. were detected. In the rainbow trout rearing (F III; N = 2 x 25), the HS-caused changes in consistency of feed and faeces impaired the formation of heavy algal films and large microorganism populations, and contributed to less turbid water turbidity in the aquaria, particularly at high temperatures. Significant differences in growth and feed conversion ratio could not be observed. In general, the addition of 5 % HS to the feed is regarded as being too high because the total amount of feed given (inclusive 5 % HS) is considered. The feed conversion ratio was higher in most of the HS-groups. Effects of oral application of 5 % HS in feed were thus less obvious than the bath treatment. Zootechnical parameters, in general, did not change. Merely in experiment F I the body weight of the HS-groups was significantly higher than that of the controls. In aquaria and small ponds used for ornamental fish breeding the observed cleaning of water and reduced formation of algal films and microorganism populations caused by HS could be of future importance. Intestinal effects of HS are assumed as internal organs revealed a reduced infection with both motile aeromonads and pseudomonads.

The storage of nuclear waste in deep geological formations is discussed worldwide as the main strategy for nuclear waste management. To ensure the confinement of the nuclear waste, a multiple barrier system which consists of engineered, geo-engineered, and geological barriers will be applied. Thereby, in Germany the definition of the isolating rock zone represents an important safety function indicator. Clay rock is internationally investigated as potential host rock for a repository and represents a part of the geological barrier. In the present work, the natural clay rock Opalinus Clay from the Mont Terri rock laboratory, Switzerland, was studied. In Germany, the direct disposal of the spent nuclear fuel without the reprocessing of the spent fuel is preferred. In case of water ingress, radionuclides can be released from the nuclear waste repository into its surroundings, namely the host rock of the repository. Humic acids, ubiquitous in nature, can be found associated with the inorganic components in natural clay rock (1.5×10–3 wt.% in Opalinus Clay). They can be released under certain conditions. Due to their variety of functional groups, humic acids are very strong complexing agents for metal ions. They have inherent redox abilities and a colloidal conformation in solution. Because of these characteristics, humic acids can affect the mobility of metal ions such as actinides. Furthermore, in the near-field of a repository elevated temperatures have to be considered due to the heat production resulting from the radioactive decay of the various radionuclides in the nuclear waste. This work focuses on the interaction of uranium, as main component of spent nuclear fuel, with Opalinus Clay and studies the influence of humic acid and elevated temperature on this interaction. For investigation of the retention behavior of the clay and the mobility of U(VI) in the system, batch sorption and diffusion experiments were performed. To clarify which U(VI) and humic acid species were present under the applied conditions, aqueous speciation modeling was used. Additionally, the U(VI) speciation in solution and on the clay surface was investigated by spectroscopic methods. Prior to the investigation of the ternary system U(VI) / humic acid / clay, the applied batches of Opalinus Clay were characterized (e.g., specific surface area, carbon content, cation exchange capacity, elemental composition, particle size distribution). Leaching studies with Opalinus Clay in synthetic Opalinus Clay pore water (pH 7.6, It = 0.34 mol/L) and in NaClO4 (pH 3 – 10, I = 0.1 mol/L) were performed to identify the competing ions and their concentrations in the background electrolytes. These data were used to calculate the U(VI) and humic acid speciation in solution. Calcium and carbonate ions are present under pore water conditions as well as in 0.1 mol/L NaClO4 from pH 7 to 8.5, due to dissolution of calcite (mineral fraction in Opalinus Clay). Thus, the U(VI) speciation is dominated by the aquatic Ca2UO2(CO3)3 complex. In the case of pore water, Ca2UO2(CO3)3(aq) is also the dominant U(VI) species in the presence of humic acid, which was corroborated by time-resolved laser-induced fluorescence spectroscopic measurements. A significantly changed speciation was found in 0.1 mol/L NaClO4 in the presence of humic acid. At pH > 7, the negatively charged UO2(CO3)2HA(II)4– complex determines the U(VI) speciation, thus repressing the Ca2UO2(CO3)3(aq) complex. In addition, the speciation of humic acid is influenced from ions leached out from Opalinus Clay. The CaHA(II) complex is the dominating humic acid species in solution. Batch sorption experiments in 0.1 mol/L NaClO4 showed that Opalinus Clay has the strongest retardation effect on U(VI) in the pH range from pH 4.5 to 7. However, under environmentally relevant conditions (pH > 7), the sorption of U(VI) onto Opalinus Clay is very weak. Under pore water conditions, a distribution coefficient (Kd) of 0.0222 ± 0.0004 m3/kg was determined, which was shown to be independent of solid-to-liquid ratios ≥ 60 g/L. In addition, in pore water, the U(VI) sorption onto Opalinus Clay is not influenced by humic acid, which is supported by the speciation results. Extended X ray absorption fine-structure investigations confirmed this batch sorption result. The U(VI) diffusion experiments performed in pore water at 25 °C with Opalinus Clay bore core samples confirmed the Kd value obtained by batch sorption experiments. In the diffusion experiments at 60 °C, a change in the U(VI) speciation occurred. Beside Ca2UO2(CO3)3(aq), a colloidal U(VI) species was formed. Almost equivalent apparent diffusion coefficient (Da) values were determined for the diffusion of the aqueous U(VI) species at 25 and 60 °C through Opalinus Clay. Thus, based on the investigations in the present study the breakthrough of U(VI) through Opalinus Clay is expected to be independent of the temperature and should occur nearly at the same time. Modeling calculations showed that it would take about 10 years until a detectable amount of 233U(VI) (1×10–9 mol/L) migrates through an 11 mm thick Opalinus Clay sample. Two distinct humic acid size fractions – a large- and a small-sized colloid fraction – diffused through the Opalinus Clay samples. Within three months, the high molecular size humic acid colloids migrated only about 500 µm into the clay, whereas the low molecular size fraction diffused through the entire Opalinus Clay samples and were consequently detected in the receiving reservoirs. These findings demonstrate a filtration effect of the compacted clay. The diffusion experiments revealed that the effect of humic acid on U(VI) diffusion is negligible and, under the studied conditions, independent of temperature. The obtained results contribute to data bases used for modeling of interaction and migration processes in uranium / clay rock systems. Thus, the collected sorption and diffusion data are not only relevant for safety assessment of nuclear waste repositories but also for any clay-containing system present in the environment, where the geochemical interaction with uranium contaminated water plays a role. Concerning the suitability of Opalinus Clay as host rock for a nuclear waste repository, it can be concluded, that Opalinus Clay has a relatively high retardation potential for U(VI). In case of water ingress U(VI) as part of the nuclear waste is released into the clay formation. Under near-neutral pH conditions, it will be complexed by calcium and carbonate ions leached out from Opalinus Clay, whereby Ca2UO2(CO3)3(aq) is formed. This complex is only weakly retarded by sorption onto the clay, which can contribute to an enhanced mobility of U(VI) in the host rock. However, the U(VI) migration through the clay rock is governed by molecular diffusion. This decelerates the migration of Ca2UO2(CO3)3(aq) through Opalinus Clay and thus it represents the decisive retardation process in the investigated system. Additionally, under environmentally relevant conditions, humic acid has no significant influence on U(VI) / Opalinus Clay interaction even at an elevated temperature of 60 °C. This was shown by speciation, sorption, as well as diffusion experiments. / Eine weltweit diskutierte Strategie zum Umgang mit radioaktiven Abfällen ist deren Endlagerung in tiefen geologischen Formationen. Zur Abschirmung der Umwelt vor den schädlichen Einflüssen des radioaktiven Abfalls soll ein Multibarrierensystem bestehend aus technischen, geotechnischen und geologischen Barrieren im Endlager dienen. Dabei ist in Deutschland die Definition des einschlusswirksamen Gebirgsbereichs ein wichtiger sicherheitstechnischer Indikator. Tongestein wird als potentielles Endlagerwirtsgestein und Teil der geologischen Barriere international erforscht. In der vorliegenden Arbeit wurde das natürliche Tongestein Opalinuston aus dem Mont Terri Felslabor, Schweiz, untersucht. In Deutschland wird die direkte Endlagerung des abgebrannten Kernbrennstoffes ohne Wiederaufarbeitung des Brennstoffs favorisiert. Bei Wassereinbruch können Radionuklide aus dem Abfall in die Umgebung des Endlagers freigesetzt werden, d. h. sie können in Kontakt mit dem Wirtsgestein kommen. Ubiquitär in der Natur vorkommende Huminsäuren können mit den anorganischen Komponenten des natürlichen Tongesteins vergesellschaftet sein (1.5×10–3 Gew.-% in Opalinuston). Unter bestimmten Bedingungen können die Huminsäuren freigesetzt werden. Ihre Struktur enthält eine Vielzahl von funktionellen Gruppen, was sie zu starken Komplexbildnern für Metallionen macht. Sie besitzen Redoxeigenschaften und bilden in Lösung eine kolloidale Konformation aus. Aufgrund dieser Charakteristika können sie die Mobilität von Metallionen wie den Actinoiden beeinflussen. Weiterhin sind im Nahfeld eines Endlagers erhöhte Temperaturen zu erwarten, welche aus der Wärmefreisetzung beim radioaktiven Zerfall der verschiedenen Radionuklide im radioaktiven Abfall resultieren. Die vorliegende Studie konzentriert sich auf die Untersuchung der Wechselwirkung von Uran, als Hauptkomponente des endgelagerten abgebrannten Kernbrennstoffs, mit Opalinuston und untersucht dabei den Einfluss von Huminsäure und erhöhter Temperatur. Um das Rückhaltevermögen des Tongesteins gegenüber U(VI) und die U(VI)-Mobilität im System zu ermitteln, wurden Sorptions- und Diffusionsversuche durchgeführt. Zur Klärung, welche U(VI)- und Huminsäurespezies unter den untersuchten Bedingungen vorliegen, wurde die aquatische Speziation berechnet. Zusätzlich wurde die U(VI)-Speziation in Lösung und an der Tonoberfläche mit spektroskopischen Methoden untersucht. Vor der Untersuchung des ternären Systems U(VI) / Huminsäure / Ton wurden die eingesetzten Opalinuston-Chargen charakterisiert (z. B. spezifische Oberfläche, Kohlenstoffgehalt, Kationenaustauschkapazität, elementare Zusammensetzung, Partikelgrößenverteilung). Anschließend wurden Auslaugungsversuche mit Opalinuston in synthetischem Opalinustonporenwasser (pH 7.6, It = 0.34 mol/L) und in NaClO4 (pH 3 – 10, I = 0.1 mol/L) durchgeführt, um relevante Konkurrenzionen zu identifizieren und deren Konzentration in den Hintergrundelektrolyten zu bestimmen. Die erhaltenen Daten wurden zur Berechnung der U(VI)- und Huminsäurespeziation in Lösung verwendet. Unter Porenwasserbedingungen sowie in 0.1 mol/L NaClO4 von pH 7 bis 8.5 liegen, durch die Auflösung von Calcit (Mineralphase im Opalinuston), Calcium- und Carbonationen in Lösung vor. Dadurch wird die U(VI)-Speziation von dem aquatischen Ca2UO2(CO3)3-Komplex dominiert. Im Falle des Porenwassers ist Ca2UO2(CO3)3(aq) auch in Gegenwart von Huminsäure die dominierende U(VI)-Spezies. Dies wurde durch zeitaufgelöste laserinduzierte fluoreszenzspektroskopische Messungen nachgewiesen. Eine signifikante Änderung der U(VI)-Speziation tritt in 0.1 mol/L NaClO4 in Gegenwart von Huminsäure auf. Bei pH > 7 bestimmt der negativ geladene UO2(CO3)2HA(II)4–-Komplex die U(VI)-Speziation, wobei der Anteil von Ca2UO2(CO3)3(aq) zurückgedrängt wird. Auch die Huminsäurespeziation wird durch die vom Opalinuston ausgelaugten Ionen beeinflusst. So ist der CaHA(II)-Komplex die dominierende Huminsäurespezies in Lösung. Sorptionsversuche in 0.1 mol/L NaClO4 zeigten, dass Opalinuston gegenüber U(VI) den stärksten Retardationseffekt im pH-Bereich 4.5 bis 7 aufweist. Unter umweltrelevanten Bedingungen hingegen (pH > 7) ist die U(VI)-Sorption an Opalinuston sehr schwach. Unter Porenwasserbedingungen wurde ein Verteilungskoeffizient (Kd) von 0.0222 ± 0.0004 m3/kg ermittelt, der von Fest-Flüssig-Verhältnissen ≥ 60 g/L unabhängig ist. Außerdem wird die U(VI)-Sorption an Opalinuston in Porenwasser nicht von Huminsäure beeinflusst. Dies wird durch die Ergebnisse aus den Speziations-rechnungen unterstützt. Röntgenabsorptionsspektroskopische Untersuchungen bestätigten ebenfalls dieses Sorptionsergebnis. Die U(VI)-Diffusionsexperimente in Porenwasser bei 25 °C unter Verwendung von Opalinustonbohrkernstücken bestätigten den Kd-Wert der Sorptionsexperimente. In den Diffusionsexperimenten bei 60 °C trat eine Änderung in der U(VI)-Speziation auf. Neben Ca2UO2(CO3)3(aq) wurde eine kolloidale U(VI)-Spezies gebildet. Für die Diffusion der aquatischen U(VI)-Spezies durch Opalinuston bei 25 und 60 °C wurden annähernd gleiche scheinbare (apparente) Diffusionskoeffizienten (Da) bestimmt. Das bedeutet, der Durchbruch von U(VI) durch Opalinuston ist unabhängig von den hier untersuchten Temperaturen und wird deshalb etwa zum gleichen Zeitpunkt erwartet. Modellierungen zeigten, dass es etwa zehn Jahre dauern würde, bis eine detektierbare Menge an 233U(VI) (1×10–9 mol/L) durch ein 11 mm-dickes Opalinustonbohrkernstück migrieren würde. Zwei verschiedene Huminsäuregrößenfraktionen diffundierten durch die Opalinustonproben – eine große und eine kleine kolloidale Größenfraktion. Innerhalb von drei Monaten migrierten die hochmolekularen Huminsäurekolloide nur 500 µm in den Ton, während die niedermolekularen Huminsäurekolloide durch die gesamten Opalinustonproben diffundierten und dadurch im Auffangreservoir detektiert werden konnten. Diese Resultate demonstrieren den Filtrationseffekt des Tongesteins. Die Diffusionsversuche zeigten, dass der Einfluss von Huminsäure auf die U(VI)-Diffusion, unabhängig von der in dieser Arbeit verwendeten Temperatur, vernachlässigbar ist. Die erhaltenen Ergebnisse tragen zu Datenbanken bei, die für die Modellierung von Wechselwirkungs- und Migrationsprozessen in Uran / Tongestein-Systemen genutzt werden. Das bedeutet, die gesammelten Sorptions- und Diffusionsdaten sind nicht nur für den Langzeitsicherheitsnachweis eines Endlagers für radioaktive Abfälle von Relevanz, sondern auch für jedes tonhaltige System in der Umwelt, bei dem die geochemische Wechselwirkung mit urankontaminierten Wässern eine Rolle spielt. Bezüglich der Eignung von Opalinuston als Wirtsgestein für ein Endlager radioaktiver Abfälle lässt sich schlussfolgern, dass Opalinuston ein relativ hohes Retardationspotential bezüglich U(VI) aufweist. Wenn U(VI) als Bestandteil des radioaktiven Abfalls bei Wassereinbruch im Endlager in die Umgebung freigesetzt wird, wird es unter umweltrelevanten Bedingungen von Calcium- und Carbonationen, welche aus dem Opalinuston herausgelöst werden, komplexiert. Dabei bildet sich Ca2UO2(CO3)3(aq). Dieser Komplex wird nur schwach durch Sorption am Tongestein zurückgehalten, was zu einer erhöhten U(VI)-Mobilität im Wirtsgestein führen kann. Im untersuchten System wird die U(VI)-Migration durch das Tongestein jedoch durch molekulare Diffusion bestimmt. Sie verzögert die Migration von Ca2UO2(CO3)3(aq) durch Opalinuston und stellt somit den maßgeblichen Retardationsprozess im System dar. Huminsäure hat keinen signifikanten Einfluss auf die U(VI) / Opalinuston-Wechselwirkung, sogar bei einer erhöhten Temperatur von 60 °C. Dies wurde mittels Speziationsmodellierungen sowie durch Sorptions- und Diffusionsversuche gezeigt.

No description available.

Na atualidade estudos direcionados para a avaliação do risco químico e do impacto ambiental produzidos por compostos químicos de uso intensivo, como agrotóxicos, petroquímicos e fármacos, vêm ganhando importância por elucidarem as implicações ao meio ambiente e à saúde pública decorrentes deste uso pela sociedade moderna de forma a estabelecer parâmetros restritivos para suas aplicações, evitando-se danos posteriores. Este Estudo compreendeu as observações de sorção e de interação do antibiótico de uso animal e agrícola oxitetraciclina (OTC) com solos brasileiros e ácidos húmicos (AH) extraídos de solos, tendo-se como objetivos gerais comprovar a sorção aos solos e aos AH e verificar a influência da matéria orgânica (MO) e do pH sobre a sorção, definindo quais os mecanismos moleculares de interação envolvidos, cabendo destacar que as tetraciclinas são uma das principais classes de antibióticos utilizadas na pecuária brasileira, tanto para tratamento de enfermidades quanto como Antibióticos Promotores de Crescimento (APC), além de serem freqüentemente aplicados na agricultura para controle de fungos e bactérias. Utilizou-se a Cromatografia Líquida de Alta Eficiência (CLAE) para a coleta de dados quantitativos que permitiram a construção de isotermas de sorção solo-OTC em pH 4,8 e AH-OTC em três valores de pH (3,1, 4,8 e 8,3) para a comprovação da sorção e da influência do conteúdo de MO no primeiro caso, e na sorção aos AH, para o segundo caso. Os solos foram caracterizados conforme procedimento padrão da EMBRAPA, enquanto que os AH foram caracterizados segundo procedimentos recomendados pela literatura por meio das técnicas instrumentais de Análise Elementar, Absorção na Região do Infravermelho Médio, Ressonância Magnética Nuclear e Ressonância Paramagnética Eletrônica. Foram utilizadas as técnicas espectroscópicas de Absorção na Região do Infravermelho (Próximo e Médio) e Absorção e Fluorescência na Região do UV-Visível, para a avaliação dos possíveis mecanismos de interação envolvidos, como ligação de hidrogênio, interação hidrofóbica e transferência de elétrons. A isoterma de Freundlich apresentou-se como um modelo matemático adequado para a verificação da sorção solos-OTC e AH-OTC, a partir da aplicação de um método cromatográfico adequado, comprovando a sorção para os dois casos, bem como o efeito do conteúdo de MO dos solos e do pH do meio sobre a capacidade e a intensidade da sorção, a qual foi quantificada como de capacidade de sorção inferior em comparação a dados obtidos em clima temperado e de alta capacidade de sorção quando comparada à legislação ambiental brasileira. Foi observado que a OTC interagiu com os AH em uma larga faixa de valores de pH, indo de 3,1 a 8,3. Contudo, o meio no qual foi possível observar de uma forma mais acentuada a interação entre AH e OTC foi o meio básico (pH 8,2), sendo notado a existência de mecanismos de interação associados e dependentes do pH do meio, como: ligação de hidrogênio, interação hidrofóbica e transferência de prótons. / At present further studies on the risk assessment of chemical and environmental impact produced by chemical-intensive, such as pesticides, petrochemicals and pharmaceuticals, have gained importance for elucidating the implications for the environment and public health arising from this use by modern society to establish restrictive parameters for their applications, avoiding further damage. This Study comprised observations of sorption and interaction of antibiotic for animal and agriculture use oxytetracycline (OTC) with brazilian soils and humic acids (HA) extracted from soil, having as objectives to prove the general sorption to soils and the AH and the influence of organic matter (OM) and pH on the sorption, which define the molecular mechanisms of interaction involved, highlighting that tetracyclines are a major classes of antibiotics used in the brazilian cattle industry, both for treatment of diseases such as antibiotic growth promoters (AGP), and frequently also applied in agriculture to control fungi and bacteria. The High Performance Liquid Chromatography (HPLC) was used to collect quantitative data that allowed the construction of sorption isotherms soils-OTC in pH 4.8 and AH-OTC in three pH values (3.1, 4, 8 and 8.3) for proof of sorption and the influence of OM content in the first case, and sorption to AH, for the second case. The soils were characterized as standard procedure of EMBRAPA, while AH were characterized according to procedures recommended by the literature by means of instrumental techniques for Elemental Analysis, Absorption in the Region of the Middle Infrared, Nuclear Magnetic Resonance and Electron Paramagnetic Resonance. The Spectroscopic Absorption in the Infrared Region (Middle) and Fluorescence and Absorption in the Region and the UV-Visible were used for the evaluation of interaction mechanisms involved, such as hydrogen bonding, hydrophobic interactions and electron transfer. The Freundlich isotherm was presented as a mathematical model suitable for the verification of soils-OTC sorption and AH-OTC sorption from the application of a chromatographic method that is suitable, proving the sorption for the two cases as well as the effect of OM content of soils and the pH on the capacity and sorption intensity, which was quantified as the lower sorption capacity in comparison with data from temperate and high sorption capacity when compared to Brazilian environmental legislation. It was observed that the OTC interacted with the HA in a wide range of pH values, ranging from 3.1 to 8.3. However, the way in which it was possible to observe a more pronounced interaction between HA and OTC was the basic medium (pH 8.2), and noted the existence of mechanisms of interaction associated and dependent on pH, such as: link hydrogen, hydrophobic interaction and proton transfer.

Estudou-se o emprego da Cromatografia a Líquido por Injeção Seqüencial (SIC) explorando o uso de uma cela de longo caminho óptico com guia de onda (LCW) de 100 cm para a melhora dos limites de detecção (LOD) e quantificação (LOQ) na determinação de atrazina (ATR), propazina (PRO) e simazina (SIM). Para isto, utilizou-se uma fase móvel com composição de 44:56 (v v-1) metanol : tampão acetato de amônio 1,25 mM, pH 4,7, coluna monolítica e a detecção espectrofotométrica em 238 nm. Obtiveram-se valores de LOD e LOQ, respectivamente, de 1,76 e 5,86 &#181;g L-1 para ATR, 4,51 e 15 &#181;g L-1 para PRO e 2,25 e 7,5 &#181;g L-1 para SIM. Com o emprego da cela de longo caminho óptico os valores de LOD ficaram abaixo dos recomendados pela US-EPA, que permite para águas potáveis uma concentração de 3 &#181;g L-1 para ATR, 4 &#181;g L-1 para SIM e 10 &#181;g L-1 para PRO. Realizaram-se estudos de adsorção de SIM, PRO e ATR e seus metabólitos desisopropilatrazina (DIA), desetilatrazina (DEA) e 2-hidroxiatrazina (HAT) em solo, ácido húmico e solo modificado com ácido húmico. Para isso foi utilizado um sistema de monitoramento on-line composto por um filtro tangencial e uma bomba peristáltica para circulação da suspensão. Foram realizados estudos cinéticos em duas etapas e, em ambas, foi utilizado um mix dos compostos com concentração inicial de 1,0 mg L-1 e gradiente de eluição passo a passo para a separação dos compostos utilizando três fases móveis com composições de 15 ou 28, 40 e 50% (v v-1) metanol : tampão acetato de amônio 1,25 mM pH 4,7. Na primeira etapa o tempo de contato entre triazinas e adsorventes foi de 90 min. Na segunda etapa foi utilizado apenas o solo como adsorvente e o tempo de contato foi de 24 h. Para a primeira etapa do estudo só foi possível aplicar modelo cinético de pseudo-segunda ordem, o qual permitiu estimar os valores de massa adsorvida de triazina por massa de adsorvente, sendo que o ácido húmico é o material com maior capacidade adsortiva (1470 ± 43&#181;g g-1 para DIA a 2380 ± 51 &#181;g g-1 para PRO). O composto mais adsorvido em solo é PRO (26,5 ± 0,1 &#181;g g-1). A presença de ácido húmico no solo aumentou a adsorção de ATR (de 19,4 ± 0,7 para 23 ± 2 &#181;g g-1), de HAT (10,9 ± 0,7 para 18 ± 2 &#181;g g-1) e de PRO (26,5 ± 0,7 para 29,8 ±0,2 &#181;g g-1), mas diminuiu a adsorção de SIM e não afetou DIA e DEA. No estudo com tempo de contato de 24 h foi possível aplicar modelos de pseudo-primeira e segunda ordem. Os resultados obtidos confirmaram a maior adsorção de PRO, seguidos da ATR. HAT, SIM, DEA e DIA apresentaram as menores taxas de adsorção em solo, sendo que os dois últimos apresentaram uma tendência de dessorção após 4 h de contato, tendo maior potencial de lixiviação para corpos d\'água próximos aos locais de aplicação. / This work describes the use of Sequential Injection Liquid Chromatography (SIC) coupled to a long path length optical flow cell with 100 cm long Liquid Core Waveguide (LCW) to improve the limits of detection (LOD) and quantification (LOQ) for determination of atrazine (ATR), propazine (PRO) and simazine (SIM). Separation was achieved with a mobile phase composition of 44:56 (v v-1) methanol:1.25 mM ammonium acetate buffer, pH 4.7, monolithic column and spectrophotometric detection at 238 nm. The values of LOD and LOQ were, respectively, 1.76 and 5.86 &#181;g L-1 for ATR, 4.51 and 15 &#181;g L-1 for PRO and 2.25 and 7.5 &#181;g L-1 for SIM. The LOD values achieved with the employment of long optical path cell were lower than those recommended by US-EPA, which allows for drinking water, maximum concentration levels of 3 &#181;g L-1 for ATR, 4 &#181;g L-1 for SIM and 10 &#181;g L-1 for PRO. Adsorption of SIM, PRO and ATR, as well as their metabolites desisopropylatrazine (DIA), desethylatrazine (DEA) and 2-hidroxyatrazine (HAT) on soil, humic acid and soil modified with humic acidic was studied. An on-line monitoring system was assembled, composed of a tangential filter and a peristaltic pump for circulation of the suspension. Kinetic studies were carried out in two steps, and in both, it was used a mix of compounds with initial concentration of 1,0 mg L-1 and a stepwise gradient elution for separation of the compounds using three mobile phases with compositions of 15 or 28, 40 and 50% (v v-1) methanol: 1.25 mM ammonium acetate buffer, pH 4.7. In the first step the contact time between triazines and adsorbents was 90 minutes. In a second study made only with soil, the contact time was 24 h. Data obtained in the first stage of the study was only fitted to pseudo-second order kinetic equation, which allowed one to estimate the values of the adsorbed mass of triazine per mass of adsorbent. Humic acid was the material with higher adsorptive capacity (from 1470 ± 43 &#181;g g-1 for DIA to 2380 ± 50 &#181;g g-1 for PRO). In soil, PRO exhibited the highest adsorption (26.5 ± 0.1 &#181;g g-1). The presence of humic acid in the soil increased adsorption of ATR (19.4±0.7 to 23±2 &#181;g g-1), HAT (10.9 ± 0.7 to 18 ± 2 &#181;g g-1) and PRO (26.5 ± 0.7 to 29.8 ± 0.2 &#181;g g-1), but decreased adsorption of SIM, not affecting DIA and DEA. In the study with contact time of 24 h, it was possible apply pseudo-first and pseudo-second order equations for SIM, ATR and PRO. The results confirmed the greatest adsorption of PRO, followed by ATR. HAT, SIM, DEA and DIA had low rates of adsorption on soil, the latter two showed a trend of desorption after 4 h of contact, having the greatest potential for leaching to water bodies near to the places of application.

Estudaram-se as propriedades ácido base e de complexação com íons Cu(II) dos ácidos húmico (AH) e fúlvico (AF) extraídos de vermicomposto. O isolamento e a purificação foram realizados de acordo com o método descrito pela Sociedade Internacional de Substâncias Húmicas (IHSS). Estudaram-se as propriedades ácido-base por titulação potenciométrica em meio de KNO3 0,10 mol L-1 utilizando-se funções de Gran modificadas. Caracterizaram-se cinco classes de grupos ionizáveis, constatando-se predominância de grupos carboxílicos sobre grupos fenólicos e amínicos, especialmente para o AF, cuja acidez total foi maior do que a do AH. Estudaram-se as propriedades complexantes com íons Cu(II) nos pH 4, 5 e 6 por titulação potenciométrica com um eletrodo íon-seletivo para Cu(II), adotando-se os métodos de Scatchard e de regressão não linear com a equação de Langmuir para tratamento de dados. Em pH 5 e 6 caracterizaram-se duas classes de sítios de complexação, enquanto em pH 4, apenas uma classe foi caracterizada. De maneira geral, a estabilidade e a capacidade de complexação aumentaram com o pH, indicando a competição de prótons pelos sítios de complexação. Os resultados indicam maior estabilidade e capacidade para a complexação com AH em relação ao AF. Esta tendência foi verificada por funções diferenciais de equilíbrio diferenciais aplicadas em baixos graus de ocupação de sítios. / Acid base and complexation with Cu(II) ions were studied for humic (AH) and fulvic (AF) acids extracted from vermicompost. The isolation and purification was performed according the procedure described by the International Humic Substances Society (IHSS). The acid base properties were studied by potentiometric titration in 0,10 mol L-1 KNO3 using modified Gran functions. Five classes of ionizable sites were characterized, showing a predominance of carboxylic over phenolic and aminic groups, especially for AF, which has total acidity larger than the one determined for AH. Complexing properties with Cu(II) ions were studied by potentiometric titration at pH 4, 5 and 6 using Cu(II) ion-selective electrode. Data treatment was performed using the Scatchard method, as well as non-linear regression with the Langmuir equation. At pH 5 and 6, two classes of binding sites were characterized, but at pH 4 only a single complexing site was characterized. Stability and capacity increased with pH, suggesting competition of protons by the binding sites. The results indicate larger stability and capacity for complexation with AH in comparison with AF. This trend was also verified by differential equilibrium functions at low degree of site occupation.

Im Rahmen dieser Arbeit wurden vier verschiedene Methoden zur Separation, Identifikation sowie Quantifizierung von Silber-Nanopartikeln (Ag-NP) entwickelt. Mittels asymmetrischer Fluss-Feldflussfraktionierung (AF4) in Kombination mit einem induktiv gekoppelten Plasma-Massenspektrometer (ICP-MS) konnten eine gute Trennung und hohe Wiederfindungsraten gefunden werden. Eine systematische Studie möglicher Probenverluste während der Methodenoptimierung zeigte, dass der größte Verlust durch die Ag+-Ionen verursacht wurde, während Verluste durch Ablagerungen auf der Membran vernachlässigbar waren. Für Citrat-stabilisierte Ag-NP konnten mittels Hohlfaser-Fluss-Feldflussfraktionierung (HF5) gute Trennergebnisse erreicht und der hydrodynamische Durchmesser bestimmt werden. Zur Bestimmung der Partikelanzahlgrößenverteilung und des geometrischen Durchmessers von Partikeln in unbekannter Matrix wurde die Isotopenverdünnungsanalyse (IVA) erfolgreich mit der Einzelpartikel ICP-MS kombiniert. Weiterhin wurde eine Hochdruckflüssigkeitschromatographie(HPLC)-IVA-ICP-MS-Methode entwickelt, mit welcher NP und ihre korrespondierenden Ionen getrennt und quantifiziert werden konnten. Ein Vergleich der Ansätze zeigt, dass eine Kombination mehrerer Methoden nötig ist, um alle relevanten Informationen über die NP zu erhalten. Zum Abschluss wurde mit den entwickelten Methoden das Umweltverhalten der Ag-NP in einer Huminsäure(HS)-Suspension untersucht. Hierbei wurden erste Stabilisierungseffekte in Bezug auf die Ag-Konzentration und Partikelanzahl festgestellt. Zudem konnte mittels HF5 und HPLC für kleine NP in HA eine Modifikation in Form der Ausbildung eines zweiten, kleineren NP-Signals beobachtet werden. / In this work, four different methods for the separation, identification, and quantification of silver nanoparticles (Ag-NP) were developed. Using asymmetric flow field-flow fractionation (AF4) in combination with inductively coupled plasma mass spectrometry (ICP-MS), a good separation and high recovery rates were found. A systematic investigation of possible sample losses during the method optimization showed that Ag+ ions caused the highest loss and only negligible amounts of Ag residues on the membrane were found. For citrate-stabilized Ag-NP, hollow fiber flow-field flow fractionation (HF5) analyses achieved good results for the separation and calculation of the hydrodynamic diameters. In order to determine the particle number size distribution and the geometric diameter for samples in unknown matrices, isotope dilution analysis (IVA) was successfully combined with single particle ICP-MS. Additionally, a high-performance liquid chromatography (HPLC)-IVA-ICP-MS approach was developed, which was able to separate and quantify NP and their corresponding ions. A comparison of the methods showed that a combination of different approaches is necessary to obtain all relevant information. Finally, the methods were applied to analyze the environmental behavior of Ag-NP in a humic acid (HS) suspension. Here, first stabilization effects in terms of the Ag concentration and particle number concentration were detected. Using HF5 and HPLC for the analysis of small NPs in HS, a modification in the form of a second, smaller NP signal was observed.

Orientador: Maria Helena Moraes / Banca: Roberto Lyra Villas Bôas / Banca: Itamar Andrioli / Banca: Ricardo Ralish / Banca: Itamar Rosa Teixeira / Resumo: O presente trabalho teve como objetivo avaliar o efeito da utilização de adubos orgânicos, produzidos por diferentes processos de reciclagem de dejetos bovinos criados em sistema de confinamento para novilhos superprecoces, nos atributos químicos e físicos de um LATOSSOLO VERMELHO Distrófico e na produtividade da cultura do milho. O experimento foi conduzido por duas safras agrícolas, 2002/2003 e 2003/2004. Utilizou-se o delineamento experimental em blocos casualizados com quatro repetições e seis tratamentos: T1 = efluente de biodigestor; T2 = esterco de esterqueira; T3 = composto orgânico; T4 = vermicomposto; T5 = adubo mineral; T6 = testemunha (sem utilização de adubos). As parcelas possuíam 15 m de comprimento por 8 m de largura, com área total de 120 m2. As quantidades para cada fonte orgânica foram calculadas com base nos seus teores de nitrogênio, para aplicação de 120 kg ha-1 de N. No tratamento T5 utilizou-se uma formulação N-P2O5-K2O, com base na análise do solo para P e K, e também 120 kg ha-1 de N, dos quais 30 kg foram aplicados na base e o restante em cobertura, em uma única aplicação, aos 33 e 37 dias após a emergência das plantas, na primeira e segunda safra, respectivamente. Os adubos orgânicos foram incorporados ao solo por meio de uma gradagem, antes da semeadura. O milho, cv. híbrido DKB 350 foi semeado dia 6 de janeiro de 2003 na primeira safra, e no dia 26 de dezembro de 2003 na segunda safra, com espaçamento de 90 cm entre linhas, e população de 55000 plantas por hectare. Os atributos do solo foram avaliados nas camadas de 0-0,10 e 0,10-0,20 e 0,20-0,30 m. Os atributos físicos avaliados foram o diâmetro médio ponderado, a argila dispersa em água, a resistência à penetração, a condutividade hidráulica saturada, a densidade do solo, porosidade total, macro e microporosidade...(Resumo completo, clicar acesso eletrônico abaixo) / Abstract: The present work had as its aim to evaluate the effect of cattle manure usage, produced by different processes of bovine dejections recycling raised in pen system for superprecocious steers in the chemical and physical properties of a distrophyc Red Oxisol and in the maize productivity. The experiment was carried out by two crop harvests 2002/2003 and 2003/2004. A completely randomized block design was used with four replications and six treatments: T1 = biodigestor effluent; T2 = cattle manure; T3 = organic composition; T4 = vermicompost; T5 = mineral fertilizer; T6 = witness (without fertilizer application). The parcels were 15 meters long and 8 meters wide, with a total area of 120 square meters. The amounts for each organic source had been calculated based on their nitrogen concentration, for a N application of 120 kg ha-1. In T5 treatment, a N-P2-O5-K2O formula was used, based on the soil analysis for P and K, and also 120 kg ha-1 of N, of which 30 kg were applied in the base and the rest in the covering, in a single application, at 33 and 37 days after the plant emerging, in the first and second harvests, respectively. The organic matter had been incorporated to the soil by grading, before sowing. The maize, cv. Hybrid DKB 350 was sown in January 6th, 2003 in the first harvest and in December 26th, 2003 in the second harvest, with a distance of 90 cm between the lines and a population of 55,000 plants per linear meter. The soil attributes were evaluated in the 0-0,10 and 0,10-0,20 and 0,20-0,30 layers. The evaluated physical attributes were the mean weighed diameter, the water dispersed clay, the penetration resistance, the saturated hydraulic conductivity, the soil bulk density, total porosity, macro and microporosity. Concerning the chemical attributes, the fractioned organic matter, macro and micronutrients, pH... (Complete abstract, click eletronic address below) / Doutor