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As an example, Fig. 2 shows the chemical composition of particles between 1 and 1.5 µm in diameter as a function of measurement altitude over Tinfou for May 19, 2006, 11:24 to 11:42 h. On this day, the mineral dust layer extended up to approximately 4.5 km. The composition of the layer was quite homogeneous, except the sulfate-silicate mixtures on the ground and at the top of the layer being more abundant than within. The latter indicates anthropogeneous influence in the boundary layer as well as in the tropospheric background. On the other hand, the layer was not homogeneous in the horizontal as is shown by Fig. 1. 140 km to the north east, a significantly higher content of calcium-bearing particles can be detected, appearing as a mode around 3 µm diameter. elevation, m a. s. l. 5,000 4,000 3,000 2,000 1,000 iron rich titanium rich carbonates other calcium rich gypsum halite 0.00 0.20 0.40 0.60 0.80 1.00 relative abundance quartz silicates mixtures sulfates carbonaceous other Fig. 2: Relative abundance of particle classes as function of altitude over Tinfou, Morocco - 160 -
Diploma Theses Keil, Matthias; Entwicklung eines geologischen Modells zur Entstehung von Erdfällen in Nordhessen; Engineering Geology; Juli 2006. Naser, Simon Marek; Erkundung von Deichen mit Georadar-Möglichkeiten und Grenzen; Engineering Geology; April 2006. Schnitzspan, Anne; Risikoevaluation eines Rutschungsgebietes in Graach an der Mosel; Engineering Geology; April 2006. Magister Theses Witt, Bettina; Stadteilentwicklung als Konzept der Stadtförderung. Vergleichende Untersuchung zu Notwendigkeit und Umsetzung von Stadtteilförderungsprogrammen am Beispiel dreier Stadtteile; Geography; March 06 Hartmann, Simone; Neue Konzeptionen in der Planung von Großsiedlungen und Stadtteilen. Erfahrungen aus Fehlplanungen und Fehlentwicklungen von Großsiedlungen der 60er Jahre dargestellt am Beispiel Darmstadt Neu-Kranichstein; Geography; March 06 PhD Theses Lindstaedt, Tamara; Regionsmarketing und die Bedeutung regionsbezogener Identität - Der Übergangsbereich der Verdichtungsräume Rhein-Main und Rhein-Neckar als Beispiel; Geography; October 06 Vester, Barbara ; Feinstaubexposition im urbanen Hintergrundaerosol des Rhein-Main- Gebietes: Ergebnisse aus Einzelpartikelanalysen; Environmental Mineralogy; July 06 Zeiß (Blau), Tatjana ; Die Struktur sekundärer Versorgungsstandorte im südlichen Rhein-Main-Gebiet und die modellhafte Entwicklung eines räumlichen Verteilungsmusters; Geography; October 06 - 161 -
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ANNUAL REPORT 2 0 0 6 FACULTY OF MA
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Annual Report 2006 Faculty 11 Mater
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Preface The year 2006 of the Depart
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difference of numerical and analyti
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Institute of Materials Science Phys
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Research Projects Bulk Amorphous Al
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el Dsoki, C.; Landersheim, V. ; Kau
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Das, J.; Kim, K. B.; Xu, W.; Wei, B
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Staff Members Head Prof. Dr. Jürge
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Zhou L.; Rixecker G.; Aldinger F.;
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concerned with the synthesis and ch
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Publications Fleissner, A.; Schmid,
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• Surface analysis The UHV-surfac
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T. Mayer, U. Weiler, E. Mankel and
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Thin films The Thin Film division w
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Berky, W.; Gottschalk, S.; Elliman,
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Guest Scientists Research Projects
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Hesse, S.; Zimmermann, J.; von Segg
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Structure Research The research in
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Research Projects Functional Advanc
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Dincer, I.; Elerman, Y.; Elmali, A;
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hexakis(imidazole)nickel(II)bis(for
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Chemical Analytics The chemical ana
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Collaborations The above mentioned
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Hoffmann, P.; Non-Invasive Identifi
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Ferroelectrics For this class of ma
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Materials Modelling The research ac
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Materials for Renewable Energies In
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Joint Research Laboratory Nanomater
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Collaborative Research Center (SFB)
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B7 P.I.: Prof. H. v. Seggern / Dr.
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The glass transition temperature (T
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transition allows to investigate at
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Relative density 1.00 0.95 0.90 0.8
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Fig. 2 shows the time dependencies
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Dielectric interface trap engineeri
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∆V C q th eff 12 −2 p ( VGS = 0
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Fig. 3: Schematic of the photovolta
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synthesis and analysis of interface
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Fig. 2: Resistivity vs temperature
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Fig. 2: X-ray appearance near-edge
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Capacity [mAhg -1 ] 700 600 500 400
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Texture investigations and field em
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screening effects. Gold coating of
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Figure 2 shows a selected region of
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The spectrum shows that apart from
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The effect of crystallinity on the
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Electrochemical investigation and c
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This phenomenon can be understood c
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∆ = 0 − exhibiting dominance of
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constituents. The requirement of va
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In order to assess the influence of
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In this study, we have therefore de
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Fig. 1: Proposed models for a) Pt,
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Synthesis of oxide-polymer nanocomp
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Page 140 and 141: Fig. 1: Aerial photo of the Lake Li
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Page 144 and 145: tower stripping, and therefore much
Page 146 and 147: Diffusion and reaction in micro- an
Page 148 and 149: Rift dynamics, uplift and climate c
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Page 154 and 155: The Effect of LiF Addition on the S
Page 156 and 157: In case of the undoped sintered B6O
Page 158 and 159: Microstructures in Omphacite and Ot
Page 160 and 161: Modelling phase-assemblage diagrams
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