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In the present study possible sources and pathways of the gasoline additive methyl tertiary-butyl ether (MTBE) in the aquatic environment in Germany were investigated. The objective of the present study was to clarify some of the questions raised by a previous study on the MTBE situation in Germany. In the USA and Europe 12 million t and 3 million t of MTBE, respectively, are used as gasoline additive. The detection of MTBE in the aquatic environment and the potential risk for drinking water resources led to a phase-out of MTBE as gasoline additive in single states of the USA. Meanwhile there is also an ongoing discussion about the substitution of MTBE in Europe and Germany. The annual usage of MTBE in Germany is about 600,000 t. However, compared to the USA, significant less data exists on the occurrence of MTBE in the aquatic environment in Europe. Because of its physico-chemical properties, MTBE readily vaporizes from gasoline, is water soluble, adsorbs only weakly to the underground matrix and is largely persistent to biological degradation. The toxicity of MTBE remains to be completely investigated, but MTBE in drinking water has low taste- and odor thresholds of 20-40 microgram/L. The present study was conducted by collecting water samples and analyzing them for their MTBE concentrations through a combination of headspace-solid phase microextraction (HS-SPME) and gas chromatography-mass spectrometry (GC-MS). The detection limit was 10 ng/L. The method was successfully tested in the framework of an interlaboratory study and showed recoveries of reference values of 89% (74 ng/L) and 104% (256 ng/L). The relative standard deviations were 12% and 6%. The investigation of 83 water samples from 50 community water systems (CWSs) in Germany revealed a detection frequency of 40% and a concentration range of 17-712 ng/L. The detection of MTBE in the drinking water samples could be explained by a groundwater pollution and the pathway river - riverbank filtration - waterworks. Rivers are important drinking water sources. MTBE is emitted into rivers through a variety of sources. In the present study, potential point sources were investigated, i.e. MTBE production sites/refineries/tank farms and groundwater pollutions. For this purpose, the spatial distribution of MTBE in three German rivers with the named potential emission sources located close to the rivers was investigated by analyzing 49 corresponding river water samples. The influence of the potential emission sources groundwater pollution and refinery/tank farm was successfully demonstrated in certain parts of the River Saale and the River Rhine. Increasing MTBE concentrations from 24 ng/L to 379 ng/L and from 73 ng/L to 5 microgram/L, respectively, could be observed in the parts investigated in these two rivers. The identification of such emission sources is important for future modeling. Further sources of MTBE emission into surface water are industrial (non-petrochemical) and municipal sewage plant effluents. In the present study long-term monitoring of water from the River Main (n=67 samples), precipitation (n=89) and industrial (n=34) and municipal sewage plant effluents (n=66) was conducted. The comparison of the data sets revealed that maximum MTBE concentrations in the River Main of up to 1 microgram/L were most possibly due to single industrial effluents with MTBE concentrations of up to 28 microgram/L (measured in this study). The average MTBE content of 66 ng/L in the River Main most probably originated from municipal sewage plant effluents and further industrial effluents. Background concentrations of <30 ng/L could be related to the direct atmospheric input via precipitation. A certain aspect of the atmospheric MTBE input is represented by the input of MTBE into river water or groundwater through snow. In the present study 43 snow samples from 13 different locations were analyzed for their MTBE content. MTBE could be detected in 65% of the urban and rural samples. The concentrations ranged from 11-613 ng/L and were higher than the concentrations in rainwater samples formerly analyzed. Furthermore, a temperature dependency and wash-out effects could be observed. The atmospheric input of MTBE was in part also visible in the analyzed groundwater samples (n=170). The detection frequencies in non-urban and urban wells were 24% and 63%, respectively. The median concentrations were 177 ng/L and 57 ng/L. In wells located in the vicinity of sites with gasoline contaminated groundwater, MTBE concentrations of up to 42 mg/L could be observed. The MTBE emission sources and the different pathways of MTBE in the aquatic environment demonstrated in the present study and other works raise the question whether the use of MTBE in a bulk product like gasoline should be continued in the future. Currently, possible substitutes like ethyl tertiary-butyl ether (ETBE) or ethanol are being discussed.
Development of chromium(VI)-free defect etching solutions for application on silicon substrates
(2008)
In the production of integrated circuits (ICs), photolithography plays a key role in wafer structuring. The basic principle of photolithography is the selective processing of areas (etching, implantation, metallisation etc.) while the others are covered and therefore protected by the resist. After each process step the resist, now modified, has to be removed. In the history of semiconductor manufacturing this has been accomplished with a mixture of H2SO4 and H2O2, H2SO4 and O3 or a plasma etch. As the structure sizes decreased they reached a stage where they had to be exposed to light of shorter wavelengths for the photolithography, going from i-line (365 nm) to DUV (248 nm and 193 nm). This change in wavelength now requires new resists and therewith new stripping methods. Beside the changes in the resist the finer structures are also more sensitive to damages caused by the resist strip. Along with this the demand for cost reduction and environment-friendliness poses a big challenge for modern resist stripping. In this study ozone in deionised water (DI/O3) was the basic chemistry investigated as it is cost efficient in production and disposal as well as environment friendly. Furthermore it is a chemistry known to cause no damage to the wafers. DI/O3 has been successfully applied to strip i-line resists. The challenge now is to find ways and means to make DI/O3 strip even highly implanted DUV resists which currently can only be removed by a plasma etch. To achieve this a detailed understanding of the behaviour of ozone in DI water and the influence of factors both chemical and physical on the stripping efficiency at the different stages in the process is necessary. Along with this, methods which enable the elucidation of resist structures and the changes they undergo during the process of photolithography as well as during the ozone strip have to be developed. This will enable us to understand the mechanisms involved and hence, ideally, develop ozone-based stripping solutions customized for each resist and process step. For this purpose the ozone decomposition in DI water with and without additives was studied via UV-Vis spectroscopy. Radicals generated within the ozone decomposition were trapped and quantified, the resists were studied directly on the wafer with IR and Raman spectroscopy and stripped with DI/O3-mixtures and different setups to find optimum conditions for a complete and damage free resist strip. UV-Vis spectroscopy at 260 nm was used to study ozone decomposition and the factors, both chemical and physical, which influence it. These factors are pH, different additives at the same pH, temperature and mixing of the solution. For the radical determination trapping reactions with MeOH and DMSO both forming CH2O which is further converted to DDL as the detectable species were compared with a variation of the classical iodometric titration acting as an absolute method without the need of calibration. IR spectroscopy proved to be a suitable method for the structural characterisation of the resists and the tracking of the changes undergone during the various processing steps as well as the ozone based stripping. For the stripping with DI/O3 IR spectroscopy delivered well-defined spectra. These displayed significant peak changes which support the assumption of classical ozonolysis as the decomposition mechanism for the unimplanted resist. For the study of the resist crust originating from ion implantation IR was fundamentally unsuitable and was replaced by Raman spectroscopy and microscopy. Raman spectra showed the crust to be of a highly carbon containing structure. Regrettably, the peak assignable to the crust was too broad for the exact composition of the crust to be determined. The wavelength region of the peak corresponds to that of peaks of glassy carbon and highly ordered and conventional graphite. Such a broad peak suggests that the structure of the crust is not uniform but contains more than one carbon modification. As the purpose of all these studies is to enable or improve DI/O3 based resist stripping on unimplanted as well as high-dose implanted resists the removal efficiency of DI/O3 spiked with different additives that alter the pH was studied. For these unimplanted resists the maximum efficiency could be achieved at pH = 5 – 7. Lowering or increasing the pH beyond this range gave poor results. The stripping of highly implanted resists could be achieved only at harsh conditions with a high pH-level of 12 - 13 with a narrow process window showing no stripping at lower pHs and severe damages at higher levels. The principle application of DI/O3 stripping chemistry could be proved but the currently required process time unfortunatelly is too long for commercial application and needs further optimisation.
Silicon wafers such as Silicon on Insulator (SOI) and strained silicon on Insulator (sSOI) are the essential and basic materials of advanced microelectronic devices. However, they often show various kinds of crystal defects which impair the function of these devices. The most efficient method to date, for detecting such defects and for determining their density, is to delineate them by etching the wafers with a suitable etching solution and characterise them via light optical microscopy. Etch pits are formed at defect sites which are etched at a faster rate than at the perfect lattice. The standard etching solution used for SOI and sSOI is a dilute version of Secco. As Secco contains carcinogenic and environmentally hazardous chromium (VI), the use of which is or will be restricted by law in many countries, suitable chromium (VI)-free etching solutions like Organic Peracid Etches (OPE), modified Chemical Polishing Etches (CP) like CP4 mod and mixtures with organic oxidizing agents like chloranil (CA) have been developed for the successful delineation of various types of crystal defects.
However there are still nanometer-sized defects which are hard to detect or escape detection by this method. Copper decoration is a well known method to magnify these defects. It consists in applying a copper nitrate solution to the back of the SOI or sSOI wafer. On annealing, copper diffuses through the substrate and the BOX (buried oxide) to the SOI/sSOI film and on quenching to room temperature, copper precipitates as copper silicide, SiCu3, foremost at crystal defects where the lattice strain is greater than at perfect lattice sites. These silicides increase the volume in these parts of the crystal lattice and defect magnification occurs. A considerable disadvantage of this method is its tendency for artefact formation, when the copper concentration used is too high, with the copper precipitating at the film surface. The consequence is a higher density of etch pits whereby true defect etch pits cannot be differentiated from those caused by artefacts.
The aim of this thesis is to show that the processes of decorating and etching can be combined successfully to delineate all crystal defects in SOI and sSOI. An ideal result would have been to find a copper decoration procedure that decorates all existing crystal defects at a copper concentration that avoids artefact formation.
Determination of the distribution of halocarbons in the tropical upper troposphere and stratosphere
(2008)
The aim of this thesis was to investigate distributions of 32 volatile chlorinated and/or brominated halocarbons that are currently believed to be present in the tropical upper troposphere and stratosphere and to contribute to stratospheric ozone depletion and also to global warming. For this purpose an analytical system was established, which is capable to measure ultra-low concentrated atmospheric trace gases. A quadrupole Mass Spectrometric (MS) Detector was attached to an existing Gas Chromatograph with pre-concentration system and Electron Capture Detector (ECD). The characterisation of the chromatographic system was significantly enhanced by the subsequent identification of 48 additional volatile organic compounds. Furthermore a Gaussian fit algorithm, which was developed in the workgroup, was applied to the chromatographic signals. This algorithm was proven to reflect peaks quantitatively and to enhance the performance of the integration process – especially the reproducibilities for peaks with a low signal to noise ratio. As it is known that the Electron Capture Detector responds nonlinear the new MS detector was checked for such behaviour and found to respond linear. In logical consistency the complete quantification process including e.g. pre-concentration of trace gases and signal integration can be considered as linear responding within the investigated parameter ranges. Moreover, the long term stability of the targeted halocarbons was proven inside the calibration standard containers over a period of 25 months. Many substances were also found to be stable inside the containers used for storage of air samples but a number of substances showed significant concentration changes. These were mainly CH3Cl (methyl chloride), CH3Br (methyl bromide), CH2Cl2 (dichloromethane), CHCl3 (chloroform), CCl4 (tetrachloromethane), C2Cl4 (tetrachloroethene), CH3CCl3 (methyl chloroform), CH2ClCH2Cl (1,2-dichloroethane) und C2H5Cl (chloroethane). But the number of affected substances and also the corresponding concentration changes varied between the individual containers. A systematic investigation of the influence of possible causes (e.g. air sampling methods, container materials) is recommended. Results from both internal detectors were compared and revealed biases and disadvantages of the ECD caused by its lower selectivity and its nonlinear response behaviour. Consequently the MS detector was chosen for the quantification of atmospheric trace gases. The quantification process was performed relative to externally calibrated air standards. To assess the uncertainties connected with different absolute calibration scales cross-comparisons between calibration standards of three different laboratories were carried out. Most substances’ calibrations agreed within the measurement uncertainties but significant differences were observed for CF2ClBr (H1211), CH3Cl (methyl chloride), CH2Cl2 (dichloromethane), CHCl3 (chloroform), CCl4 (tetrachloromethane) and CH3CCl3 (methyl chloroform). As five of these substances were also observed to show concentration changes inside sample containers it is likely, that such changes are responsible for calibration differences. In addition to the detailed assessment of uncertainties connected with the analytical quantification process a set of air samples was available for measurements. These samples mainly originated from the upper troposphere and lower and middle stratosphere in the tropics and the determined halocarbon quantities were used to investigate their distributions in the respective atmospheric regions. In detail, the altitudinal distributions and interrelations of 17 long-lived halocarbons in the tropical stratosphere were determined and compared with those of other stratospheric regions. Tracer-tracer-correlations of these substances in the tropical stratosphere were found to differ from those in mid- and high-latitudes. Characteristic fit functions relative to CF2Cl2 (F12) which are valid for the tropical stratosphere in 2005 were derived as well as time-independent fit functions of fractional release factors (FRFs) relative to the mean age of air. Both sets of correlations could be used for the parameterisation and evaluation of models and also to reassess the Global Warming Potentials (GWPs) of the corresponding halocarbons which might affect future climate predictions. However, the data set on halocarbons in the tropical stratosphere is still insufficient to investigate the variability of tracer-tracer-correlations and FRFs caused by dynamical and photochemical processes. Therefore it is important for future research to perform additional measurements there and – if possible – to extend the measurements to the upper tropical stratosphere in order to characterise the sink of those halocarbons that are still present in these altitudes. In addition, the amount of chlorine and bromine present in the form of organic compounds inside and above the main stratospheric entrance region (the Tropical Tropopause Layer, TTL) was quantified in the frame of a case study. This was possible because of a cooperation with scientists from the University of East Anglia which carried out measurements of six additional halocarbons leading to a total of 28 quantified target substances. Ten of these substances have short atmospheric lifetimes compared with the mean transport times of tropospheric air to the stratosphere (i.e. lifetimes below 0.5 years) and show non-uniform distributions in the upper troposphere. The contribution of these substances to stratospheric ozone depletion is subject of an ongoing scientific debate. In the performed case study a fraction range of short-lived halocarbons of 6 – 8 % (0.98 – 1.25 ppt) relative to the sum of bromine from organic substances and of 1.1 – 1.4 % (36.6 – 47.1 ppt) for the corresponding sum of chlorine was calculated to enter the stratosphere above Brazil in June 2005. Moreover by combining the data with tropospheric reference data and age of air observations the abundances of inorganic chlorine and bromine (Cly and Bry) were derived. At an altitude of 34 km an amount of 3062 ppt of Cly and 17.5 ppt of Bry from organic source gases was calculated. The latter is significantly lower than Bry mixing ratios inferred from quasisimultaneous BrO measurements at 33 km altitude above Brazil (Dorf, 2005, Dorf et al., 2008). But at the University of East Anglia indications for the presence of unknown brominated organic substances in the TTL were found which might cause this difference. Finally, a major result of this thesis adds to the knowledge of the composition of the troposphere as three Chlorofluorocarbons (CFCs) were first observed. Trifluorochloroethene, 3-chloropentafluoropropene and 4,4-dichlorohexafluoro-1-butene were found in air samples collected at the Taunus Observatory near Frankfurt (Main) and the Jungfraujoch High Altitude Research Station in Switzerland (Laube and Engel, 2008). Identification was possible because of an air plume containing high concentrations of these substances. It is suggested that the abundances found on this occasion originated from a local source. The atmospheric lifetimes of these substances are expected to be rather short as they contain a double bond. A quantitative calibration could only be derived for trifluorochloroethene but not for the other species by now. Thus, a relative sensitivity method was derived to get a first indication of the observed atmospheric abundances. All three CFCs could also be detected in air masses representative of background conditions, though with much lower concentrations. These species and some of their degradation products are toxic and could also be relevant for stratospheric and tropospheric ozone depletion. It is important to find out more about their atmospheric distributions, lifetimes, sinks and sources and their ability to reach the stratosphere to assess their possible influence on the global atmosphere. This will be done in the frame of the project "CLEARFOGG – Checking Layers of the Earths AtmospheRe For halogenated Ozone-depleting and Greenhouse Gases". This research project aims to perform a systematic scan of the atmosphere because there are indications for the presence of a number of halogenated organic compounds which are unknown by now. It was recently decided to be funded by the British National Environmental Research Council and will be carried out at the University of East Anglia mainly by the author of this thesis.