Structure and catalytic properties of sulfated zirconia foams

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Trägerkatalysatoren auf Polymerbasis für industrielle Olefinpolymerisationsprozesse

Im Rahmen dieser Arbeit werden Trägersysteme auf Basis von Polystyrol nach unterschiedlichen Konzepten hergestellt und in Propen-, Ethen- sowie Ethen-Hexen-Polymerisationengetestet. Eine universelle Einsetzbarkeit wird durch das Konzept der nichtkovalenten Metallocenbindung erreicht.Mit partiell reversibel vernetzten Trägern, die nicht mehr vollständig fragmentieren können, wird es möglich, harte, gleichmäßige Produktteilchen mit Schüttdichten über 400g/l zu erhalten. Diese Systeme erreichen bei Ethen-Hexen-Copolymerisationen Produktivitäten über 2500 Gramm Produkt pro Gramm Katalysator und Stunde bei einem sehr gleichmäßigen Aktivitätsverlauf.

Emissions of volatile organic compounds from tropical savanna vegetation and biomass burning

This dissertation focuses on characterizing the emissions of volatile organic compounds (VOCs) from grasses and young trees, and the burning of biomass mainly from Africa and Indonesia. The measurements were performed with a proton-transfer-reaction mass spectrometer (PTR-MS). The biogenic emissions of tropical savanna vegetation were studied in Calabozo (Venezuela). Two field campaigns were carried out, the first during the wet season (1999) and the second during the dry season (2000). Three grass species were studied: T. plumosus, H. rufa and A. canescens, and the tree species B. crassifolia, C. americana and C. vitifolium. The emission rates were determined with a dynamic plant enclosure system. In general, the emissions increased exponentially with increasing temperature and solar radiation. Therefore, the emission rates showed high variability. Consequently, the data were normalized to a standard temperature of 30°C, and standard emission rates thus determined allowed for interspecific and seasonal comparisons. The range of average daytime (10:00-16:00) emission rates of total VOCs measured from green (mature and young) grasses was between 510-960 ngC/g/h. Methanol was the primary emission (140-360 ngC/g/h), followed by acetaldehyde, butene and butanol and acetone with emission rates between 70-200 ngC/g/h. The emissions of propene and methyl ethyl ketone (MEK) were <80 ngC/g/h, and those of isoprene and C5-alcohols were between 10-130 ngC/g/h. The oxygenated species represented 70-75% of the total. The emission of VOCs was found to vary by up to a factor of three between plants of the same species, and by up to a factor of two between the different species. The annual source of methanol from savanna grasses worldwide estimated in this work was 3 to 4.4 TgC, which could represent up to 12% of the current estimated global emission from terrestrial vegetation. Two of the studied tree species, were isoprene emitters, and isoprene was also their primary emission (which accounted for 70-94% of the total carbon emitted) followed by methanol and butene + butanol. The daytime average emission rate of isoprene measured in the wet season was 27 mgC/g/h for B. crassifolia, and 123 mgC/g/h for C. vitifolium. The daytime emissions of methanol and butene + butanol were between 0.3 and 2 mgC/g/h. The total sum of VOCs emission measured during the day in the wet season was between 30 and 130 mgC/g/h. In the dry season, in contrast, the methanol emissions from C. vitifolium saplings –whose leaves were still developing– were an order of magnitude higher than in the wet season (15 mgC/g/h). The isoprene emission from B. crassifolia in the dry season was comparable to the emission in the wet season, whereas isoprene emission from C. vitifolium was about a factor of three lower (~43 mgC/g/h). Biogenic emission inventories show that isoprenoids are the most prominent and best-studied compounds. The standard emission rates of isoprene and monoterpenes of the measured savanna trees were in the lower end of the range found in the literature. The emission of other biogenic VOCs has been sparsely investigated, but in general, the standard emissions from trees studied here were within the range observed in previous investigations. The biomass burning study comprised the measurement of VOCs and other trace-gas emissions of 44 fires from 15 different fuel types, primarily from Africa and Indonesia, in a combustion laboratory. The average sum of emissions (excluding CO2, CO and NO) from African fuels was ~18 g(VOC)/kg. Six of the ten most important emissions were oxygenated VOCs. Acetic acid was the major emission, followed by methanol and formaldehyde. The emission of methane was of the same order as the methanol emission (~5 g/kg), and that of nitrogen-containing compounds was ~1 g/kg. An estimate of the VOC source from biomass burning of savannas and grasslands worldwide suggests that the sum of emissions is about 56 Tg/yr, of which 34 Tg correspond to oxygenated VOCs, 14 Tg to unsaturated and aromatic compounds, 5 Tg to methane and 3 Tg to N-compounds. The estimated emissions of CO, CO2 and NO are 216, 5117 and 9.4 Tg/yr, respectively. The emission factors reported here for Indonesian fuels are the first results of laboratory fires using Indonesian fuels. Acetic acid was the highest organic emission, followed by acetol, a compound not previously reported in smoke, methane, mass 97 (tentatively identified as furfural, dimethylfuran and ethylfuran), and methanol. The sum of total emissions of Indonesian fuels was 91 g/kg, which is 5 times higher than the emissions from African fuels. The results of this study reinforces the importance of oxygenated compounds. Due to the vast area covered by tropical savannas worldwide, the biogenic and biomass burning emission of methanol and other oxygenated compounds may be important for the regional and even global tropospheric chemistry.

Mikrosomale Biotransformation von Benzo[ghi]perylen, einem mutagenen polyaromatischen Kohlenwasserstoff ohne das Strukturelement der Bay-Region des kanzerogenen Benzo[a]pyrens

Kanzerogene polyaromatische Kohlenwasserstoffe (PAKs), wie Benzo[a]pyren, besitzen eine Bay-Region mit ortho-kondensiertem Benzoring. Dadurch ist die enzymatische Bildung von Bay-Region-Dihydrodiolepoxiden (Oxiranylring in der sterisch abgeschirmten Molekülbucht) möglich, die als ultimal kanzerogene Metaboliten der PAKs gelten. Diese lösen durch DNA-Modifikation Primärläsionen aus, die, sofern sie nicht enzymatisch repariert werden, bei der DNA-Replikation Fehler verursachen (Mu-tationen). Der Mehrstufenprozeß der Kanzerogenese (Promotion und Progression) führt schließlich zur neoplastischen Entartung der Zelle. Benzo[ghi]perylen (BghiP) repräsentiert eine Gruppe von PAKs, die keine „klassische“ Bay-Region besitzen und daher keine vicinalen Dihydrodiolepoxiden bilden können. Trotzdem ist BghiP mutagen, z. B. in den Stämmen TA98 und TA100 von Salmonella typhimurium (1,3- bzw. 4,3 his+-Revertanten/nmol) nach metabolischer Aktivierung mit der postmitochondrialen Fraktion von Ratten nach Behandlung mit 3-Methylcholanthren. Hemmung der mikrosomalen Epoxidhydrolase (mEH) mit 1,1,1-Trichlor-2-propenoxid (TCPO) steigert die bakterielle Mutagenität von BghiP im Stamm TA98 um das 4-fache, was Arenoxide als ultimale Mutagene wahrscheinlich macht. Dieses Ergebnis wird au-ßerdem durch Untersuchung der DNA-Bindung mit dem Verfahren des 32P-Postlabelings bestätigt (Dr. Fickler, Institut für Toxikologie, Universität Mainz). Danach bildete mikrosomal aktiviertes BghiP drei Addukte (ein Hauptaddukt, zwei Nebenaddukte), die durch Hemmung der mEH mit TCPO verstärkt wurden (das Hauptaddukt um 29%). Um den für die bakterielle Mutagenität von BghiP verantwortlichen Metaboliten zu identifizieren, wurde die mikrosomale Biotransformaton von BghiP aufgeklärt. Umsetzung von BghiP mit Lebermikrosomen von Ratten nach Behandlung mit Aroclor 1254 lieferte 17 mit Ethylacetat extrahierbare Metaboliten. Zwölf dieser Metaboliten konnten durch eine Kombination von chromatographischen, spektroskopi-schen und biochemischen Methoden identifiziert werden. Daraus ergeben sich zwei Biotransformati-onswege: Weg I beginnt mit einem Angriff von Cytochrom P450-abhängigen Monooxygenasen an Position 7 und der Bildung des 7-Phenols. Dieses wird dann in das 7,8- bzw. 7,10-Diphenol überführt, die schließlich zu den mehrkernigen Chinonen an der 7,8- bzw. 7,10-Position oxidiert werden. Im Bio-transformationsweg II werden die K-Regionen von BghiP durch Cytochrom P450 funktionalisiert. Zu-nächst entstehen das auf indirektem Weg identifizierte 3,4-Oxid und das 3,4,11,12-Bisoxid, die in mikrosomalen Umsetzungen von BghiP nur nach Hemmung der mEH gebildet werden. Enzymatische Hydrolyse des 3,4-Oxides ergibt das trans-3,4-Dihydrodiol, das zum 3,4-Chinon oxidiert wird. Ebenso entsteht aus dem 3,4,11,12-Bisoxid das trans-3,4-trans-11,12-Bisdihydrodiol, aus dem durch Oxidati-on das trans-3,4-Dihydrodiol-11,12-Chinon hervorgeht. Untersuchung der stereoselektiven enzymati-schen Bildung der K-Region-trans-Di¬hydrodiole ergaben eine präferentielle Entstehung der 3R,4R- bzw. 3R,4R,11R,12R-Enantiomere. Untersuchungen der bakteriellen Mutagenität der Hauptmetaboliten 3,4-Dihydrodiol und dem 7-Phenol machte deutlich, dass beide Biotransformationswege I und II von BghiP zur bakteriellen Mutagenität beitragen. Das 7-Phenol aus Weg I ist ein proximales Mutagen, was auch von Phenolen anderer PAKs bekannt ist. Das 3,4-Dihydrodiol aus Weg II wird so schwach zu Mutagenen aktiviert, dass dem vermutlich gebildete 3,4-Dihydrodiol-11,12-oxid keine große Bedeutung als ultimales Mutagen von BghiP zukommt. Die Bestimmung der direkten mutagenen Aktivität (ohne metabolische Aktivierung) der mutmaßlich ultimal mutagenen Arenoxide von BghiP ergab, dass die des 3,4,11,12-Bisarenoxides sehr gering war (1,3 his+-Revertanten/nmol im Stamm TA98). Das 3,4-Oxid hingegen bewirkte einen deutlichen gentoxischen Effekt in den Stämmen TA98 und TA100 (5,5 bzw. 10 his+-Revertanten/nmol). Dies wurde durch die Bestimmung der DNA-Bindung mit dem 32P-Postlabeling, in dem das 3,4-Oxid für das Hauptaddukt von BghiP verantwortlich gemacht werden konnte, bestätigt. Daher kommt dem 3,4-Oxid als ultimales Mutagen die größte Bedeutung für die Gentoxizität von BghiP zu. Die Ergebnisse dieser Arbeit lassen bei PAKs ohne Bay-Region auf Arenoxide schließen, die eine notwendige Voraussetzung für DNA-Bindung und Mutagenität sind.

Analisi del ciclo di vita di processi chimici industriali: applicazione alla sintesi di acrilonitrile mediante reazione di ammonossidazione

La green chemistry può essere definita come “l’utilizzo di una serie di principi che riducono o eliminano l’uso o la formazione di sostanze pericolose nella progettazione, produzione e applicazione di prodotti chimici”. . È in questo contesto che si inserisce la metodologia LCA (Life Cycle Assessment), come strumento di analisi e di valutazione. Lo scopo del presente lavoro di tesi è l’analisi degli impatti ambientali associati a processi chimici, ambito ancora poco sviluppato nella letteratura degli studi di LCA. Viene studiato e modellato il ciclo di vita (dall’ottenimento delle materie prime fino alla produzione del prodotto) della reazione di ammonossidazione per la produzione di acrilonitrile, valutando e comparando due alternative di processo: quella tradizionale, che utilizza propilene ( processo SOHIO), e le vie sintetiche che utilizzano propano, ad oggi poco sviluppate industrialmente. Sono stati pertanto creati sei scenari: due da propene (SOHIO FCC, con propene prodotto mediante Fluid Catalytic Cracking, e SOHIO Steam), e quattro da propano (ASAHI, MITSUBISHI, BP povero e ricco in propano). Nonostante la produzione dell’alcano abbia un impatto inferiore rispetto all’olefina, dovuto ai minori stadi di processo, dai risultati emerge che l’ammonossidazione di propano ha un impatto maggiore rispetto a quella del propene. Ciò è dovuto ai processi catalitici che utilizzano propano, che differiscono per composizione e prestazioni, rispetto a quelli da propene: essi risultano meno efficienti rispetto ai tradizionali, comportando maggiori consumi di reattivi in input . Dai risultati emerge che gli scenari da propano presentano maggiori impatti globali di quelli da propene per le categorie Cambiamento climatico, Formazione di materiale e Consumo di combustibili fossili. Invece per la categoria Consumo di metalli un impatto maggiore viene attribuito ai processi che utilizzano propene, per la maggior percentuale di metalli impiegata nel sistema catalitico, rispetto al supporto. L’analisi di contributo, eseguita per valutare quali sono le fasi più impattanti, conferma i risultati. Il maggior contributo per la categoria Consumo di combustibili fossili è ascrivibile ai processi di produzione del propano, dell’ammoniaca e del solfato di ammonio ( legato all’ammoniaca non reagita ). Stessi risultati si hanno per la categoria Cambiamento climatico, mentre per la categoria Formazione di materiale particolato, gli impatti maggiori sono dati dai processi di produzione del solfato di ammonio, del propano e dell’acido solforico (necessario per neutralizzare l’ammoniaca non reagita). Per la categoria Consumo di metalli, il contributo maggiore è dato dalla presenza del catalizzatore. È stata infine eseguita un’analisi di incertezza tramite il metodo Monte Carlo, verificando la riproducibilità dei risultati.

Entwicklung einer Thermodesorptionseinheit für die GC/MS zur Bestimmung hochreaktiver, biogener Kohlenwasserstoffe und deren Anwendung im Rahmen von Labor- und Feldstudien

Flüchtige organische Verbindungen (volatile organic compounds, VOCs), besonders rnTerpene, gelten als Vorläufer des sekundären organischen Aerosols (secondary rnorganic aerosols, SOA). Terpene werden von Pflanzen zur Abwehr oder zur rnAttraktion von Bestäubern emittiert. Ungesättigten Verbindungen, wie Sesquiterpene, rnsind sehr ozonolyseempfindlich und weisen nur geringe Konzentrationen in der rnAtmosphäre auf. Zudem lassen sie sich mit handelsüblichen rnThermodesorptionseinheiten meist nicht ohne Artefakte nachweisen, da sie eine hohe rnReaktivität mit vielen Oberflächen zeigen. rnDiese Arbeit präsentiert Forschungsergebnisse der qualitativen und rn(semi)quantitativen Auswertungen flüchtiger organischer Verbindungen in rnLaborstudien und biogenen Emissionsproben (Feldmessungen) mittels rnThermodesorption-Gaschromatographie-Massenspektrometrie (TD-GC/MS). Speziell rnzur Analyse hochreaktiver Verbindungen wurde eine Thermodesorptionseinheit für die rnGC/MS entwickelt. Diese besteht aus einer Kryofokussierung, einem Desorptionsofen rnund einer Heizung. Die Steuerung erfolgt über eine eigens dafür geschaffene rnBedienoberf läche von Labview® an einem PC über eine nachgeschaltete SPS rn(speicherprogrammierbare Steuerung). Das komplette Desorptionsprogramm und der rnStart der GC/MS-Analyse wurden automatisiert. rnDie Quantifizierung alle Proben wurde über Diffusionsquellen und rnVergleichsmessungen durch auf Adsorptionsröhrchen aufgebrachte rnVerdünnungsreihen realisiert. Um Informationen über die mutmaßlichen Vorläufer des rnsekundären organischen Aerosols zu erhalten, wurde zudem eine Ozon-Scrubber-rnMethode basierend auf Propen entwickelt. Diese wurde anhand von Standards in einer rnReaktionskammer getestet und in Feldmessungen erfolgreich angewendet. rnQuantitative Analysen zeigen, dass die meisten Terpene so vollständig vor der rnOzonolyse bewahrt werden können. Für hochreaktive Analyte wie α-Humulen oder rnβ-Caryophyllen wurden Wiederfindungsraten von über 80 % erreicht. So konnte die rnTemperaturabhängigkeit der Terpen-Emissionen der Fichte (Picea abies) in rnFeldmessungen nachgewiesen werden. rnEine weitere Anwendungsmöglichkeit wurde mit der Unterscheidung verschiedener rnArten der gleichen Gattung anhand der Emissionsmuster und der möglichen rnAbgrenzung verschiedener Bestäubertypen am Beispiel der Gattung Salvia untersucht. rnDie Emissionsanalysen zeigen, dass eine Zuordnung der Verwandtschaftsverhältnisse rnzusätzlich zu anderen Vergleichen möglich ist. Das gleiche gilt für die Differenzierung rnvon Bestäubertypen. Die Ergebnisse der Feldmessungen wurden durch rnMethodenvergleich zwischen biogenen Emissionsmessungen mit anschließender rnTD-GC/MS-Analyse und Extraktionen der jeweiligen Blüten/Blätter mit rnanschließender GC/MS-Messung bestätigt.

(Table 2) Chemical composition of gases in basalts from DSDP Leg 65 Holes

Basalts from different structural provinces in the ocean basins, such as mid-ocean ridges, island arcs, and oceanic plateaus, show marked differences in major and minor element composition stemming from differences in magma source. In addition, there are variations even within individual provinces, based on such processes as crystal fractionation, secondary alteration, and hydrothermal alteration. It is also known that hydrothermal processes can cause changes in the gas composition of submarine basalts. For example, Zolotarev et al. (1978) have established that hydrothermal alteration frequently causes an increase in the CO2 content of basalts. If the homogeneity in composition and concentration of organic gases in oceanic basalts is associated with degassing during epimagmatic alteration, it would be interesting to investigate the relative abundance of gas phases in young basalts from midoceanic ridges. This chapter deals with the distribution of organic gases and CO2 in young basalts recovered on Leg 65 from the Gulf of California. Our aim was to establish the relationship between gas composition and degree of alteration.

Hydrocarbon gases in Tertiary and Quaternary sediments offshore Peru

Hydrocarbon gases (methane, ethane, propane, isobutane, n-butane, ethene, and propene) are present in Tertiary and Quaternary shelf, upper-slope, and lower-slope deposits of the Peruvian continental margin. Methane dominates the composition of the hydrocarbon gas at all 10 sites examined during Ocean Drilling Program (ODP) Leg 112. Generation of methane is regulated by the amount of sulfate in pore water. Wherever sulfate concentrations approach or equal zero, methane concentrations increase rapidly, reaching values near 100,000 µL/L of wet sediment at eight of the 10 sites. Methane at all 10 sites results from methanogenesis, which is inhibited where sulfate is present and microbial reduction of sulfate occurs. Hydrocarbon gases heavier than methane also are present, but at much lower concentrations than methane. These hydrocarbons are thought to result from early thermal and microbial diagenesis, based on relative gas compositions and trends of concentrations with depth. With few exceptions, the results obtained in the shipboard and shore-based laboratories are comparable for methane and ethane in sediments of Leg 112. Reanalyses of canned sediments from ODP Leg 104 and from Deep Sea Drilling Project (DSDP) Legs 76 and 84 show that gas samples can be stored for as long as 8 yr, but the amounts of individual hydrocarbon gases retained vary. Nevertheless, the trends of the data sets with depth are similar for fresh and stored samples.

Low-molecular-weight hydrocarbons in sediments at DSDP Sites 89-585 and 89-586

C2-C8 hydrocarbon concentrations (about 35 compounds identified, including saturated, aromatic, and olefinic compounds) from 38 shipboard sealed, deep-frozen core samples of Deep Sea Drilling Project Sites 585 (East Mariana Basin) and 586 (Ontong-Java Plateau) were determined by a gas stripping-thermovaporization method. Total concentrations, which represent the hydrocarbons dissolved in the pore water and adsorbed on the mineral surfaces of the sediment, vary from 20 to 630 ng/g of rock at Site 585 (sub-bottom depth range 332-868 m). Likewise, organic-carbon normalized yields range from 3*10**4 to 9*10**5 ng/g Corg, indicating that the organic matter is still in the initial, diagenetic evolutionary stage. The highest value (based on both rock weight and organic carbon) is measured in an extremely organic-carbon-poor sample of Lithologic Subunit VB (Core 585-30). In this unit (504-550 m) several samples with elevated organic-carbon contents and favorable kerogen quality including two thin "black-shale" layers deposited at the Cenomanian/Turonian boundary (not sampled for this study) were encountered. We conclude from a detailed comparison of light hydrocarbon compositions that the Core 585-30 sample is enriched in hydrocarbons of the C2-C8 molecular range, particularly in gas compounds, which probably migrated from nearby black-shale source layers. C2-C8 hydrocarbon yields in Site 586 samples (sub-bottom depth range 27-298 m) did not exceed 118 ng/g of dry sediment weight (average 56 ng/g), indicating the immaturity of these samples.

Characterization of sorbed volatile hydrocarbons from the Peru margin

Bacterial and thermogenic hydrocarbons are present in the sorbed-gas fraction of Peru margin sediments. At Ocean Drilling Program (ODP) Sites 681, 682, 684, and 686, bacterial gases are restricted to the early diagenetic zones, where dissolved sulfate has been exhausted and methanogenesis occurs. Methane migrating into the sulfate zone at Sites 681, 684, 686, and possibly 682, has been consumed anaerobically by methanotrophs, maintaining the low concentrations and causing an isotope shift in d13C(CH4) to more positive values. Significant amounts of C2+ hydrocarbons occur at the shelf Sites 680/681, 684, and 686/687, where these hydrocarbons may be associated with hypersaline fluids. There is evidence at Site 679 that sorbed C2+ hydrocarbons may also have been transported by hypersaline fluids. This characteristic C2+ hydrocarbon signature in the sorbed-gas fractions of sediments at Site 679 is not reflected in data obtained using the conventional "free-," "canned-," or "headspace-gas" procedures. The molecular and isotope compositions of the sorbed-gas fraction indicate that this gas may have a thermogenic source and may have spilled over with the hypersaline fluids from the Salaverry Basin into the Lima Basin. These traces of thermogenic hydrocarbon gases are over-mature (about 1.5% Ro) and are discordant with the less-mature sediments in which they are found. This observation supports the migration of these hydrocarbons, possibly from continental sources. Sorbed-gas analyses may provide important geochemical information, in addition to that of the free-gases. Sorbed-gases are less sensitive to activities in the interstitial fluids, such as methanogenesis and methanotrophy, and may faithfully record the migration of hydrocarbons associated with hypersaline fluids.

Molecular and stable isotope composition of headspace and total hydrogencarbon gases of ODP Leg 104 sites

Molecular and isotope compositions of headspace and total (free + sorbed) hydrocarbon gases from drilled cores of the three ODP Leg 104 Sites 642, 643, and 644 of the Voring Plateau are used to characterize the origin and distribution of these gases in Holocene to Eocene sediments. Only minor amounts of methane were found in the headspace (0.1 to < 0.001 vol%). Although methane through propane are present in all of the total gas samples, different origins account for the concentration and composition variations found. Site 643 at the foot of the outer Voring Plateau represents a geological setting with poor hydrocarbon generating potential, (sediments with low TOC and maturity overlying oceanic basement). Correspondingly, the total gas concentrations are low, typical for background gases (yield C1 - 4 = 31 to 232 ppb, C1/C2+ = 0.6 to 4; delta13C(CH4) -22 per mil to -42 per mil) probably of a diagenetic origin. Holocene to Eocene sediments, which overlie volcanic units, were drilled on the outer Vdring Plateau, at Holes 642B and D. Similar to Site 643, these sediments possess a poor hydrocarbon generating potential. The total gas character (yield C1 - 4 = 20 to 410 ppb; C1/C2+ = 1.7 to 13.3; delta13C(CH4) ca. -23 per mil to -40 per mil) again indicates a diagenetic origin, perhaps with the addition of some biogenic gas. The higher geothermal gradient and the underlying volcanics do not appear to have any influence on the gas geochemistry. The free gas (Vacutainer TM) in the sediments at Site 644 are dominated by biogenic gas (C1/C2+ > 104; delta13C(CH4) -77 per mil). Indications, in the total gas, of hydrocarbons with a thermogenic signature (yield C1 - 4 = 121 to 769 ppb, C1/ C2+ = 3 to 8; delta13C(CH4) = -39 per mil to -71 per mil), could not be unequivocally confirmed as such. Alternatively, these gases may represent mixtures of diagenetic and biogenic gases.