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The work focuses on the potential of structural and chemical examinations by scanning electron microscopy based methods for archaeometric studies on ceramics. Achieved by a single preparation technique (polished block sections), the feasibility and benefits of electron backscatter diffraction are demonstrated as case studies using polychrome examples of pre-Columbian pottery (Wari, Moche and Cajamarca). Elemental and phase maps allow for separate consideration of clay and temper. Identification of mineral phases and intergrowths of temper particles provide information for clarifying clay procurement and firing techniques with respect to local versus non-local pottery to enlighten trade relations, technological transfer and shared heritage of pre-Columbian cultures.
The synthesis route and thermoelectric characterization of n-type Fe2-xTi1+xO5 (0 ≤ x ≤ 0.5) and Fe1.75(Ti1-yNby)1.25O5 (0 ≤ y ≤ 0.05) are presented. Their electrical conductivity obeys the small polaron model and their Seebeck coefficient is weakly dependent on temperature. The carrier concentration is increased with increasing Ti content in Fe2-xTi1+xO5, thus improving the electrical conductivity and decreasing the absolute values of the Seebeck coefficient. The composition with x = 0.5 shows reduced electrical conductivity contradicting the change in the carrier concentration, as it contains more microcracks than the other compositions. Fe2-xTi1+xO5 exhibits extremely low thermal conductivity. Fe2-xTi1+xO5 with x = 0.25 exhibits the highest ZT, ~ 0.014 at 1000 K. Therefore, a limited extent microcracks are beneficial to thermoelectric properties; however, when they are too extended they can be detrimental. On the contrary to Fe2TiO5, Nb substitution into Fe1.75Ti1.25O5 does not obviously improve its thermoelectric properties.