High-temperature interaction of sol-gel-derived artificial volcanic ash (AVA) matching the bulk composition of the April 15, 2010 Eyjafjallajokull (Iceland) volcanic eruption with a standard 4 mol% (7 wt%) Y 2 O 3 -stabilized ZrO 2 (YSZ) electron-beam physical vapor deposition (EB-PVD) thermal barrier coating and a corresponding YSZ powder is investigated in order to access possible implications of similar volcanic ashes on the performance of coated turbine engine airfoils. Up to 9001C, AVA deposits and EB-PVD YSZ do not show significant interaction. Viscous flow above the glass transition of AVA (T g B9301C) yields proceeding wetting of EB-PVD YSZ coatings. At 11001C, the YSZ surface is covered by a dense glaze-like AVA overlay. At 12001C, AVA is mostly infiltrating the coating, leaving a crystalline plagioclase-and hematite-type residue at the interface. Moreover, some ZrSiO 4 is formed at the expense of YSZ. The overall thermochemical effects on short-term exposure of the EB-PVD YSZ coating to a small AVA load were moderate, in particular before complete infiltration. On the other hand, AVA acts as a solvent for the stabilizing Y 2 O 3 beyond 10001C and a progressive depletion of Y 2 O 3 in the YSZ is observed at the AVA/YSZ interface. Detrimental effects on YSZ phase stability and hence coating lifetime cannot be ruled out for long-term exposure and higher AVA loads.
II. Experimental ProcedureThe starting materials for the synthesis of AVA were Al(NO 3 ) 3 Á 9H 2 O, Fe(NO 3 ) 3 Á 9H 2 O, Mg(NO 3 ) 2 Á 6H 2 O, Ca(NO 3 ) 2 Á 4H 2 O, NaNO 3 , KNO 3 , Mn(NO 3 ) 2 Á 4H 2 O, tetraethyl orthosilicate (TEOS), tetra-ethyl orthotitanate (TEOT), and (NH 4 ) 2 HPO 4 (Merck, Darmstadt, Germany). A laboratory ball mill (Pulverisette 7 premium line, Fritsch, Idar-Oberstein, J. Smialek-contributing editor