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Oxygen vacancy doping of hematite analyzed by electrical conductivity and thermoelectric power measurements

机译:通过电导率和热电功率分析分析赤铁矿的氧空位掺杂

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摘要

Hematite (α−Fe2O3) is known for poor electronic transport properties, which are the main drawback of this material for optoelectronic applications. In this study, we investigate the concept of enhancing electrical conductivity by the introduction of oxygen vacancies during temperature treatment under low oxygen partial pressure. We demonstrate the possibility of tuning the conductivity continuously by more than five orders of magnitude during stepwise annealing in a moderate temperature range between 300 and 620 K. With thermoelectric power measurements, we are able to attribute the improvement of the electrical conductivity to an enhanced charge-carrier density by more than three orders of magnitude. We compare the oxygen vacancy doping of hematite thin films with hematite nanoparticle layers. Thereby we show that the dominant potential barrier that limits charge transport is either due to grain boundaries in hematite thin films or due to potential barriers that occur at the contact area between the nanoparticles, rather than the potential barrier within the small polaron hopping model, which is usually applied for hematite. Furthermore, we discuss the transition from oxygen-deficient hematite α−Fe2O3−x towards the magnetite Fe3O4 phase of iron oxide at high density of vacancies.
机译:赤铁矿(α-Fe2O3)以较差的电子传输性能而闻名,这是该材料在光电应用中的主要缺点。在这项研究中,我们研究了在低氧分压下通过温度处理过程中引入氧空位来增强电导率的概念。我们证明了在300到620 K之间的中等温度范围内的逐步退火过程中,可以连续调节电导率超过五个数量级的可能性。通过热电功率测量,我们能够将电导率的提高归因于电荷的增加载流子密度增加三个数量级以上。我们比较了赤铁矿薄膜与赤铁矿纳米颗粒层的氧空位掺杂。因此,我们表明,限制电荷传输的主要势垒是由于赤铁矿薄膜中的晶界,还是由于发生在纳米粒子之间接触区域的势垒,而不是由于小极化子跳跃模型中的势垒。通常用于赤铁矿。此外,我们讨论了在高空位密度下从缺氧赤铁矿α-Fe2O3-x向氧化铁磁铁矿Fe3O4相的转变。

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