TY - CONF A1 - Kruschwitz, Sabine A1 - Feldmann, R. ED - Schuhmann, R. T1 - Zerstörungsfreie Feuchtemessung an Estrichen - ein multi-sensorischer Ansatz mit Methodenvergleich T2 - 8. CMM-Tagung 2015 - Innovative Feuchtemessung in Forschung und Praxis - Material - Prozesse - Systeme N2 - Feuchte und Salz können die Mikrostruktur poröser Baustoffe maßgeblich verändern, oft sind sie die Ursache von sowohl chemischen als auch mechanischen Schädigungen und Korrosion. Im speziellen Fall von Fußbodenestrichen ist gerade die Frage nach der Belegreife für Fußbodenleger von immer wiederkehrender Bedeutung. Dieser Beitrag beschäftigt sich mit den Vor- und Nachteilen verschiedener zerstörungsfreier, feuchtesensitiver Messmethoden und vergleicht die Ergebnisse mit denen der baustellenüblichen zerstörenden Tests. Kapazitive Methoden und Bodenradar scheinen am erfolgversprechensten im Bezug auf flächige Feuchtemessungen, aber auch sie eignen sich derzeit noch nicht als eigenständige, sofort ersetzbare Absolutmessgeräte, sondern eher als schnelle Relativverfahren fürs Monitoring. T2 - 8. CMM-Tagung 2015 - Innovative Feuchtemessung in Forschung und Praxis - Material - Prozesse - Systeme CY - Karlsruhe, Germany DA - 07.10.2015 KW - Estrich KW - Feuchtemessung KW - Radar KW - Hydratation KW - Baustoffe KW - Feuchte KW - Zerstörungsfreie Prüfung KW - Kapazitive Methoden PY - 2015 N1 - Serientitel: Innovative Feuchtemessung in Forschung und Praxis – Series title: Innovative Feuchtemessung in Forschung und Praxis VL - 8 SP - 79 EP - 91 AN - OPUS4-34763 LA - deu AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Gerrits, Ruben A1 - Wirth, R. A1 - Schreiber, A. A1 - Feldmann, Ines A1 - Knabe, Nicole A1 - Schott, J, A1 - Benning, L.G. A1 - Gorbushina, Anna T1 - High-resolution imaging of fungal biofilm-induced olivine weathering JF - Chemical Geology N2 - Many microorganisms including free-living and symbiotic fungi weather minerals through the formation of biofilms on their surface. Weathering thus proceeds not only according to the mineral’s chemistry and the environmental conditions but also according to the local biofilm chemistry. These processes can be dissected in experiments with defined environmental settings and by employing genetic tools to modify traits of the fungal biofilm. Biofilms of the rock-inhabiting fungus Knufia petricola strain A95 (wild-type, WT) and its melanin-deficient mutant (ΔKppks) were grown on polished olivine sections in subaerial (air-exposed) and subaquatic (submerged) conditions. After seven months of interaction at pH 6 and 25°C, the fungus-mineral interface and abiotic olivine surface were compared using high resolution transmission electron microscopy (HRTEM). The abiotic, subaquatic olivine section showed a 25 nm thick, continuous amorphous layer, enriched in Fe and depleted in Si compared to the underlying crystalline olivine. This amorphous layer formed either through a coupled interfacial dissolution reprecipitation mechanism or through the adsorption of silicic acid on precipitated ferric hydroxides. Its thickness was likely enhanced by mechanical stresses of polishing. Directly underneath a fungal biofilm (WT and mutant alike), the surface remained mostly crystalline and was strongly etched and weathered, indicating enhanced olivine dissolution. The correlation between enhanced olivine dissolution and the absence of a continuous amorphous layer is a strong indication of the dissolution-inhibiting qualities of the latter. We propose that the fungal biofilm sequesters significant amounts of Fe, preventing formation of the amorphous layer and driving olivine dissolution onwards. The seemingly similar olivine surface underneath both WT and mutant biofilms illustrates the comparably insignificant role of specific biofilm traits in the weathering of olivine once biofilm attachment is imposed. Under subaerial conditions, the absence of water on the abiotic surface prohibited olivine dissolution. This was overcome by the water retention capacities of both the WT and mutant biofilm: the olivine surface underneath subaerial fungal biofilms was as weathered as the corresponding subaquatic olivine surface. Under the studied environmental settings, the effect of fungal biofilms on olivine weathering seems to be universal, independent of the production of melanin, the composition of extracellular polymeric substances (EPS) or air-exposure. KW - Bio-weathering KW - Forsterite KW - Extracellular polymeric substances KW - Melanin KW - Black fungi PY - 2021 DO - https://doi.org/10.1016/j.chemgeo.2020.119902 VL - 559 SP - 119902 PB - Elsevier B.V. AN - OPUS4-51403 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Chen, Cong A1 - Müller, Bernd R. A1 - Prinz, Carsten A1 - Stroh, Julia A1 - Feldmann, Ines A1 - Bruno, Giovanni T1 - The correlation between porosity characteristics and the crystallographic texture in extruded stabilized aluminium titanate for diesel particulate filter applications JF - Journal of the European Ceramic Society N2 - Porous ceramic diesel particulate filters (DPFs) are extruded products that possess macroscopic anisotropic mechanical and thermal properties. This anisotropy is caused by both morphological features (mostly the orientation of porosity) and crystallographic texture. We systematically studied those two aspects in two aluminum titanate ceramic materials of different porosity using mercury porosimetry, gas adsorption, electron microscopy, X-ray diffraction, and X-ray refraction radiography. We found that a lower porosity content implies a larger isotropy of both the crystal texture and the porosity orientation. We also found that, analogous to cordierite, crystallites do align with their axis of negative thermal expansion along the extrusion direction. However, unlike what found for cordierite, the aluminium titanate crystallite form is such that a more pronounced (0 0 2) texture along the extrusion direction implies porosity aligned perpendicular to it. KW - Preferred orientation KW - X-ray refraction KW - Pore orientation KW - Crystal structure KW - Extrusion KW - Microstructure-property relations PY - 2020 DO - https://doi.org/10.1016/j.jeurceramsoc.2019.11.076 SN - 0955-2219 VL - 40 IS - 4 SP - 1592 EP - 1601 PB - Elsevier Ltd. AN - OPUS4-50325 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Gerrits, Ruben A1 - Pokharel, R. A1 - Breitenbach, Romy A1 - Radnik, Jörg A1 - Feldmann, Ines A1 - Schuessler, J.A. A1 - von Blanckenburg, F. A1 - Gorbushina, Anna A1 - Schott, J. T1 - How the rock-inhabiting fungus K. petricola A95 enhances olivine dissolution through attachment JF - Geochimica et Cosmochimica Acta N2 - Free-living and mycorrhizal fungi are able to enhance the weathering of rock and other solid substrates. Deciphering the exact mechanisms of these natural processes requires their experimental simulation. Moreover, by performing these simulations with genetically amenable rock-weathering fungi, one can knock-out certain fungal traits and consequently identify their weathering-relevant function. Here, the effect of the rock-inhabiting fungus, Knufia petricola A95, on the dissolution kinetics of an Fe-bearing olivine (Mg1.86Fe0.19SiO4) is investigated at 25 °C and pH 6 using reproducible batch and mixed flow experiments. The availability of a melanin-deficient mutant (ΔKppks) of K. petricola A95, which produces more extracellular polymeric substances (EPS) than the wild type (WT), enables the comparative study of the role of melanin and EPS in olivine dissolution. In abiotic dissolution experiments, the olivine dissolution rate decreased considerably over time at pH 6 but not at pH 3.5. This inhibition of abiotic olivine dissolution at pH 6 was most likely caused by the in-situ oxidation of ferrous Fe and/or the precipitation of ferric hydroxides at the olivine surface. In corresponding biotic experiments at pH 6, both the wild type K. petricola and its melanin-deficient mutant ΔKppks solubilised and bound significant amounts of Fe released by olivine dissolution. Fe oxidation and precipitation were thus prevented and olivine dissolution proceeded faster than in the abiotic experiments. By sequestering Fe directly at the olivine surface, the attached wild type K. petricola cells were particularly efficient at preventing the oxidation of Fe at the mineral surface: the slowdown of olivine dissolution almost completely disappeared. The attachment capacity of these wild type cells is most likely mediated by wild type-specific EPS. Our presented experimental systems allow the oxidation of mineral-released Fe and include a rock-inhabiting fungus, thus simulating chemical, physical and biological conditions that set dissolution rates in a way that is relevant to natural ecosystems. KW - Black fungi KW - Bio-weathering KW - Forsterite KW - Knock-out mutant KW - Extracellular polymeric substances KW - Melanin Adhesion PY - 2020 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-509332 DO - https://doi.org/10.1016/j.gca.2020.05.010 VL - 282 SP - 76 EP - 97 PB - Elsevier Ltd. AN - OPUS4-50933 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER -