TY - JOUR A1 - García, O. A1 - Rz-Maribona, I. A1 - Gardei, André A1 - Riedl, Martin A1 - Vanhellemont, Y. A1 - Santarelli, M.L. A1 - Strupi Suput, J. T1 - Comparative study of the variation or the hydric properties and aspect of natural stone and brick after the application of 4 types of anti-graffiti N2 - In this article a comparative study of the behaviour of different commercial anti-graffiti on natural stone and brick is presented. 8 different European substrates were selected and 4 commercial anti-graffiti of different chemical nature were applied on these substrates. The variations of their hydric properties and aspect (colour and gloss) with regard to the untreated substrates were later studied in the laboratory. The results obtained permitted to assess the suitability of 4 of the main types of chemical formulations employed to be used as anti-graffiti. This study concludes that the sacrificial anti-graffiti with polymeric paraffins in its composition presents the lowest reductions of the hydric properties of the studied substrates, being also the variations in colour the least perceptible. KW - Graffiti KW - Sandstone KW - Limestone KW - Natural stone KW - Brick KW - Anti-graffiti KW - Porous substrates KW - Surface treatments KW - Anti-graffiti coatings KW - Hydric properties KW - Colour KW - Gloss PY - 2010 DO - https://doi.org/10.3989/mc.2010.45507 SN - 0465-2746 N1 - Sprachen: Spanisch/Englisch - Languages: Spanish/English VL - 60 IS - 297 SP - 1 EP - 14 CY - Madrid AN - OPUS4-21087 LA - mul AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - GEN A1 - Kus, J. A1 - Kaufhold, S. A1 - Klosa, D. A1 - Jianwei, M. A1 - Schmidt, Martin A1 - Suhendra, Suhendra T1 - Coal fire geothermometer: Controlling the extent and temperature field of underground coal fire zones T2 - 2nd International conference on coal fire research (ICCFR2) CY - Berlin, Germany DA - 2010-05-19 KW - Coal fires KW - Coal petrography KW - Coal mineralogy PY - 2010 SN - 978-3-86012-397-3 IS - Part 2 - Geosciences SP - 75 EP - 85 AN - OPUS4-21459 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - GEN A1 - Fischer, C. A1 - Wu, J. A1 - Meyer, U. A1 - Kong, B. A1 - Schmidt, Martin A1 - Wuttke, M. A1 - Drebenstedt, C. A1 - Barth, Uli A1 - Rüter, H. T1 - Eight years of successful bilateral cooperation: Milestones of sino-german research T2 - 2nd International conference on coal fire research (ICCFR2) CY - Berlin, Germany DA - 2010-05-19 KW - Underground coal fires KW - Sino-german cooperation PY - 2010 SN - 978-3-86012-397-3 IS - Introduction SP - 3 EP - 18 AN - OPUS4-21460 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - GEN A1 - Schoßig, Jörg A1 - Schmidt, Martin A1 - Krause, Ulrich A1 - Steinbach, J. T1 - Beurteilung des Selbstentzündungsverhaltens brennbarer Stäube mit Hilfe adiabatischer Warmlagerung T2 - 10. Fachtagung Anlagen-, Arbeits- und Umweltsicherheit CY - Köthen, Deutschland DA - 2010-11-04 KW - Anlagensicherheit KW - Umweltschutz KW - Sicherheitstechnik KW - Explosionsschutz PY - 2010 SN - 978-3-89746-119-2 SP - 1 EP - 7(?) CY - Frankfurt/M. AN - OPUS4-22621 LA - deu AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Kluge, Martin A1 - Ferrero, Fabio A1 - Schröder, Volkmar A1 - Acikalin, Hatice Aydan A1 - Steinbach, J. T1 - Modellazione del processo di autoaccensione del TFE KW - Convezione naturale (free convention) KW - Trasporto reattivo (reactive flow) KW - Reazione in fase gas (gas reaction) KW - Autoignizione (self-ignition) PY - 2011 SN - 0390-2358 N1 - Geburtsname von Kluge, Martin: Beckmann-Kluge, M. - Birth name of Kluge, Martin: Beckmann-Kluge, M. VL - 6 SP - 84 EP - 90 PB - ERIS CY - Milan AN - OPUS4-24094 LA - ita AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - CONF A1 - Kluge, Martin A1 - Ferrero, Fabio A1 - Schröder, Volkmar A1 - Acikalin, Hatice Aydan A1 - Steinbach, J. T1 - Improvements in the modeling of the self ignition of tetrafluoroethylene N2 - In order to prevent incidents in the industrial production of Teflon® from Tetrafluoroethylene (TFE), the safety related aspects of the self-heating process of TFE must be taken into account. Simulations of this self heating process were performed with COMSOL Reaction Engineering Lab® and COMSOL® COMSOL Multiphysics®. A complex reaction net was employed, resulting in a model allows for a good agreement with experimentally achieved results. T2 - COMSOL Conference 2010 CY - Paris, France DA - 2010-11-17 KW - Heating KW - Free convection KW - Reactive flow KW - Gas reaction KW - Self ignition PY - 2010 N1 - Geburtsname von Kluge, Martin: Beckmann-Kluge, M. - Birth name of Kluge, Martin: Beckmann-Kluge, M. SP - 1 EP - 7 AN - OPUS4-24174 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Schmidt, Martin A1 - Wu, D. A1 - Norman, F. A1 - Vanierschot, M. A1 - Verplaetsen, F. A1 - Berghmans, J. A1 - van den Bulck, E. T1 - Numerical investigation on the self-ignition behaviour of coal dust accumulations: The roles of oxygen, diluent gas and dust volume N2 - Self-ignition of coal dust deposits poses a higher risk of fires in oxygen-enriched oxy-fuel combustion systems. In this work, we develop a numerical method, using the commercial software COMSOL Multiphysics, to investigate self-ignition behaviour of coal dust accumulations with a main emphasis on the roles of oxygen, diluent gas and dust volume. A one-step 2nd-order reaction kinetic model considering both coal density and oxygen density is used to estimate reaction rate using the kinetic parameters from previously conducted hot-oven tests. This model is validated to predict the transient temperature and concentration profiles of South African coal dusts until ignition. The computed self-ignition temperatures of dust volumes show a good agreement with experimental results. In addition, it is found that the inhibiting effect of carbon dioxide is comparatively small and oxygen consumption increases dramatically after ignition. Parameter analysis shows that the heating value and kinetic parameters have a comparatively pronounced effect on self-ignition temperature. The model provides a satisfactory explanation for the dependence of self-ignition behaviour on gas atmospheres, thus helping to further understand the fire risk of self-ignition in oxy-fuel combustion systems. KW - Ignition temperature KW - Oxy-fuel combustion KW - Fire safety KW - Self-ignition KW - Numerical simulation PY - 2017 DO - https://doi.org/10.1016/j.fuel.2016.10.063 SN - 0016-2361 SP - 500 EP - 510 AN - OPUS4-37885 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Seewald, J.S. A1 - Reeves, E.P. A1 - Bach, W. A1 - Saccocia, P.J. A1 - Craddock, P.R. A1 - Shanks III, W.C. A1 - Sylva, S.P. A1 - Pichler, T. A1 - Rosner, Martin A1 - Walsh, E. T1 - Submarine venting of magmatic volatiles in the Eastern Manus Basin, Papua New Guinea N2 - The SuSu Knolls and DESMOS hydrothermal fields are located in the back-arc extensional transform zone of the Eastern Manus Basin. In 2006, highly acidic and ΣSO4-rich vent fluids were collected at both sites and analyzed for the chemical and isotopic composition of major and trace species. Fluids exiting the seafloor have measured temperatures from 48 to 215 °C and are milky white in appearance due to precipitation of elemental S0. Vent fluid concentrations of Na, K, and Mg are depleted by as much as 30% relative to seawater, but have the same relative abundance. In contrast, the fluids are highly enriched in dissolved ΣCO2, Cl, SiO2(aq), Fe, and Al relative to seawater. Measured pH (25 °C) ranged from 0.95 to 1.87 and aqueous ΣSO4 ranged from 35 to 135 mmol/kg. The chemical and isotopic composition points to formation via subsurface mixing of seawater with a Na-, K-, Mg-, and Ca-free, volatile-rich magmatic fluid exsolved from subsurface magma bodies during a process analogous to subaerial fumarole discharge. Estimates of the magmatic end-member composition indicate a fluid phase where H2O > SO2 > CO2 ≈ Cl > F. The hydrogen and oxygen isotopic composition of H2O and carbon isotopic composition of ΣCO2 in the vent fluids strongly suggest a contribution of slab-derived H2O and CO2 to melts generated in the mantle beneath the Eastern Manus volcanic zone. Abundant magmatically-derived SO2 undergoes disproportionation during cooling in upflow zones and contributes abundant acidity, SO42-, and S0 to the venting fluids. Interaction of these highly acidic fluids with highly altered mineral assemblages in the upflow zone are responsible for extensive aqueous mobilization of SiO2(aq), Fe, and Al. Temporal variability in the speciation and abundance of aqueous S species between 1995 and 2006 at the DESMOS vent field suggests an increase in the relative abundance of SO2 in the magmatic end-member that has mixed with seawater in the subsurface. Results of this study constrain processes responsible for the formation of hot-spring fluids in magmatically active back-arc environments and the resulting chemical exchange between the lithosphere and water column. PY - 2015 DO - https://doi.org/10.1016/j.gca.2015.04.023 SN - 0016-7037 SN - 1872-9533 VL - 163 SP - 178 EP - 199 PB - Elsevier Science CY - New York, NY AN - OPUS4-33433 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - Becker, D. A1 - Konnertz, Nora A1 - Böhning, Martin A1 - Schmidt, J. A1 - Thomas, A. T1 - Light-switchable polymers of intrinsic microporosity N2 - The interest in (micro)porous systems is greater than ever before with microporous polymers finding application in areas such as gas storage/separation and catalysis. In contrast to the vast majority of publications on microporous polymers seeking ever higher values for surface area or uptake capacity for a particular gas, this work presents a means to render a microporous system responsive to electromagnetic stimuli. The incorporation of a diarylethene (DAE) derivative in the backbone of a polymer of intrinsic microporosity (PIM) produces a microporous system that exhibits photochromism as proven by UV–vis absorption and NMR studies. In the resulting DAE-PIM, surface area is not a fixed unalterable property but can be influenced by the external and nondestructive stimulus light in a reversible manner. Furthermore, in combination with Matrimid, free-standing membranes can be produced that display light-switchable diffusivity and permeability for carbon dioxide and oxygen. In this way, material scientists are offered the potential to employ only one system that can assume several states with different properties for each. KW - Gaspermeation KW - Diffusion KW - Polymer intrinsischer Mikroporosität KW - UV-VIS PY - 2016 DO - https://doi.org/10.1021/acs.chemmater.6b02619 SN - 0897-4756 VL - 28 IS - 23 SP - 8523 EP - 8529 PB - ACS CY - Whashington,DC AN - OPUS4-38735 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER - TY - JOUR A1 - De la Rosa, J. M. A1 - Martin-Sanchez, Pedro Maria A1 - Santiago-Cortes, S. A1 - Hermosin, B. A1 - Knicker, H. A1 - Saiz-Jimenez, C. ED - De la Rosa, J. M. T1 - Structure of melanins from the fungi Ochroconis lascauxensis and Ochroconis anomala contaminating rock art in the Lascaux Cave N2 - Two novel species of the fungal genus Ochroconis, O. lascauxensis and O. anomala have been isolated from the walls of the Lascaux Cave, France. The interest in these fungi and their melanins lies in the formation of black stains on the walls and rock art which threatens the integrity of the paintings. Here we report solid-state cross polarization magic-angle spinning 13C and 15N nuclear magnetic resonance (NMR) spectroscopy and surface-enhanced Raman spectroscopy (SERS) of the melanins extracted from the mycelia of O. lascauxensis and O. anomala in order to known their chemical structure. The melanins from these two species were compared with those from other fungi. The melanins from the Ochroconis species have similar SERS and 13C and 15N NMR spectra. Their chemical structures as suggested by the data are not related to 3,4-dihydroxyphenylalanine, 5,6-dihydroxyindole or 1,8-dihydroxynaphthalene precursors and likely the building blocks from the melanins have to be based on other phenols that react with the N-terminal amino acid of proteins. The analytical pyrolysis of the acid hydrolysed melanin from O. lascauxensis supports this assumption. KW - Microbiology KW - Biodeterioration KW - Melanins KW - Fungi PY - 2017 UR - https://nbn-resolving.org/urn:nbn:de:kobv:b43-435345 DO - https://doi.org/10.1038/s41598-017-13862-7 SN - 2045-2322 VL - 7 SP - 13441, 1 EP - 13441, 11 PB - Nature AN - OPUS4-43534 LA - eng AD - Bundesanstalt fuer Materialforschung und -pruefung (BAM), Berlin, Germany ER -