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Michael Hoppe

    Organisation und DV-Unterstützung der Personalwirtschaft
    Das Böse nebenan
    Die klassische und neoklassische Theorie der Genossenschaften
    Active Listening: Improve Your Ability to Listen and Lead, First Edition (Spanish for Spain)
    Das hallstattzeitliche Gräberfeld von Beilngries "Im Ried-Ost", Lkr. Eichstätt, Oberbayern
    Magnetic, structural, and electronic properties of NiFe2O4 ultrathin films
    • 2016

      The physical properties of transition-metal oxides are influenced by the competition among charge, spin, and orbital degrees of freedom. Advances in deposition techniques enable the growth of thin film heterostructures with atomically sharp interfaces, allowing for the exploration of novel nanoelectronic functionalities and phenomena unique to these interfaces. Oxides that exhibit both magnetic and insulating properties present a promising avenue for enhancing spintronic devices through effective spin-filter effects generated by spin-dependent tunneling. The spinel ferrite NiFe2O4 is particularly promising due to its dual properties at room temperature. This research investigates the interplay between magnetic, electronic, and structural properties in NiFe2O4. Thin films are deposited on Nb-doped SrTiO3 substrates using pulsed laser deposition, with careful evaluation of growth conditions to achieve high-quality, epitaxial films. Emphasis is placed on the effects of reduced dimensionality in ultrathin films (d < 4nm), revealing enhanced saturation magnetization coinciding with reduced lattice constants under compressive strain. Various analyses, including HAXPES, XANES, and XMCD spectroscopy, confirm a consistent cationic coordination across film thickness, ruling out cationic inversion as a cause for enhanced magnetization. Instead, a novel interfacial magnetism is discovered, driven by ferromagnetic ordering of Ti electrons,

      Magnetic, structural, and electronic properties of NiFe2O4 ultrathin films
    • 2005

      The construction of the Main-Danube-Canal in the now dry Ottmaring valley, east of Beilngries, destroyed approximately 21,000 m² of a significant Hallstatt cemetery in southern Germany. This site had previously been partially excavated by Theodor Thenn between 1889 and 1917 and analyzed by W. Torbrügge in the early 1960s. The graves utilized slabs of locally sourced Upper Jurassic limestone. The documented findings classify the burial chambers into three types: Type A (cairn larger than the chamber), Type B (similar within a stone circle), and Type C (cairn not exceeding chamber size and within a stone circle). Additionally, three types of stone circles were identified: Type A (alternating vertical and horizontal stones), Type B (only vertical stones), and Type C (dry-stone wall of horizontal stones). Notably, the numerous small cremation pit burials found between the tumuli appeared in five variants, many topped with a stone grave stele (Type D). The tumuli were organized into at least six groups, constructed in a manner that revealed recognizable horizontal stratigraphy.

      Das hallstattzeitliche Gräberfeld von Beilngries "Im Ried-Ost", Lkr. Eichstätt, Oberbayern