Analytische Chemie
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Binder remnants in historical mortars represent a record of the connection between the raw materials that enter the kiln, the process parameters, and the end product of the calcination. Raman microspectroscopy combines high structural sensitivity with micrometre to sub-micrometre spatial resolution and compatibility with conventional thin-sectional samples in an almost unique fashion, making it an interesting complementary extension of the existing methodological arsenal for mortar analysis. Raman spectra are vibrational fingerprints of crystalline and amorphous compounds, and contain marker bands that are specific for minerals and their polymorphic forms. Relative intensities of bands that are related to the same crystalline species change according to crystal orientations, and band shifts can be caused by the incorporation of foreign ions into crystal lattices, as well as stoichiometric changes within solid solution series. Finally, variations in crystallinity affect band widths. These effects are demonstrated based on the analysis of three historical mortar samples: micrometric distribution maps of phases and polymorphs, crystal orientations, and compositional variations of solid solution series of unreacted clinker grains in the Portland cement mortars of two 19th century castings, and the crystallinities of thermal anhydrite clusters in a high-fired medieval gypsum mortar as a measure for the applied burning temperature were successfully acquired.
This overview article provides insight into how to apply Raman spectroscopy in combination with a confocal, optical microscope setup on polycrystalline material systems, in order to obtain quantitative information on phase distribution, grain sizes, crystal orientations and microstrain. Although the present work uses Cu(In,Ga)(S,Se)₂ absorber layers in corresponding thin-film solar cells as a model system to demonstrate the capabilities of Raman microspectroscopy, the approaches discussed may be applied to any organic or inorganic, polycrystalline materials system.
In the present chapter, the capabilities of Raman spectroscopy for the advanced characterisation of thin films for solar cells are reviewed. Raman spectroscopy is an optical, nondestructive technique based on the inelastic scattering of photons with elemental vibrational excitations in the material. The line shape and position of the Raman bands are determined by the crystalline structure and chemical composition of the measured samples, being sensitive to the presence of crystalline defects, impurities and strain. Presence of peaks characteristic of different phases also allows for the identification of secondary phases that are strongly related to the growth and process conditions of the films. All these aspects account for a strong interest in the analysis of the Raman spectra, providing a powerful nondestructive analytical tool for the structural and chemical assessment of the films. In addition, the combination of a Raman spectrometer with an optical microscope also allows for achieving a high spatial resolutions (of below 1 µm) when mapping surfaces and analyzing depth-resolved phase distributions in thin films.
The present chapter is divided into four main sections: The two first ones are devoted to a revision of the Fundamentals of Raman spectroscopy (Section 17.2) and Vibrational modes in crystalline materials (Section 17.3). Section 17.4 deals with the main experimental considerations involved in the design and implementation of a Raman scattering setup. This is followed by a detailed description of the application of Raman scattering for the structural and chemico-physical analysis of thin film photovoltaic materials (Section 17.5), with the identification of crystalline structure and secondary phases, evaluation of film crystallinity, analysis of chemical composition of semiconductor alloys, characterisation of nanocrystalline and amorphous layers, stress effects and crystal orientations. This includes the description of corresponding state of the art and recent case examples that illustrate the capabilities of the Raman technique for the advanced characterisation of layers and process monitoring in thin-film photovoltaic technologies.
Als schweizweit einziger Hersteller produzierte die Gesellschaft der Ludwig von Roll'schen Eisenwerke seit den 1870er Jahren granulierte Hochofenschlacke. Im Blashochofen von Choindez im Schweizer Jura wird bis Mitte der 1920er Jahre Bohnerz aus dem Delsberger Becken, das kontemporär publizierten Analysen zufolge als Spuren- bzw. Schwermetalle Titan, Chrom, Blei und Vanadium enthält, zu grauem Roheisen verhüttet. In zementgebundenen Mörtelmischungen des 19. und frühen 20. Jahrhunderts aus verschiedenen Regionen der Schweiz finden sich neben reliktischen Hüttensandsplittern vereinzelt bis zu fünfhundert Mikrometer große scharze Kugeln mit grünlichem Schimmer, wohl nicht gemahlener Schlackensand. Deren mittels Ramanmikroskopie (Phasenbestand) und energiedispersiver Röntgenspektroskopie am Rasterelektronenmikroskop (Elementanalytik) ermittelte Mineralogie ergibt in Form von Plattnerit PbO2, Rutil TiO2 und vermitlich Chromit Fe(II)Cr2O4 bzw. Nichromit (Ni,Co,Fe(II))(Cr,Fe(III),Al)2)4 Übereinstimmungen mit den nur die Elementzusammensetzung berücksichtigenden historischen Resultaten. Ebenfalls im Zusammenhang mit dem das Bohnerz begleitenden Boluston samt Huppererde zu sehen sind die Minerale Coelestin SrSO4 und Zirkon ZrSiO4, des Weiteren der Siliciumcarbidpolymorph Moissanit SiC als Reaktionsprodukt von Quarzsand und Brennstoff. Die Kohärenz zwischen um die Jahrhundertwende durchgeführten Analysen von Rohmaterial als auch Ofenbruch aus dem in Choindez betriebenen Hochofen und den in diesem Beitrag diskutierten Resultaten moderner analytischer Methoden spricht für den Gebrauch von granulierter Schlacke aus dem Hause Ludwig von Roll als Mörtelzuschlag. Die Hüttensandkörner, eigentlich latent hydraulisch, sind aufgrund der fehlenden Aufbereitung zu grob für eine effektive Hydratation und deshalb trotz reaktiver Glasphase und Klinkermineralien (Belit Ca2SiO4 und Monocalciumaluminat CaAl2O4) intakt in der Bindemittelmatrix erhalten.
Microstrain distributions were acquired in functional thin films by high-resolution X-ray microdiffraction measurements, using polycrystalline CuInSe2 thin films as a model system. This technique not only provides spatial resolutions at the submicrometre scale but also allows for analysis of thin films buried within a complete solar-cell stack. The microstrain values within individual CuInSe2 grains were determined to be of the order of 10^-4. These values confirmed corresponding microstrain distribution maps obtained on the same CuInSe2 layer by electron backscatter diffraction and Raman microspectroscopy.
Raman microspectroscopic imaging was just recently introduced into the analysis of cement stone. Here, we demonstrate this approach on 19th-century Roman and Portland cement mortars and extend it to gypsum-based samples originating from a medieval stucco sculpture (high-burnt gypsum) and a stucco ornament prefabricated at the beginning of the 20th century (plaster of Paris). Furthermore, the distributions of dolomite and Calcite were mapped in an accessory mineral grain with approx. 500 nm lateral Resolution demonstrating the ability for studying alteration processes such as dedolomitisation. As we would like to make this approach accessible to other researchers, we discuss its present status, advantages, limitations and pitfalls.