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Mixed oxygen ionic and electronic conduction in CaFe0.2Ti0.8O3-δ:a combined oxygen permeation and electrical conductivity study

机译:CaFe0.2Ti0.8O3-δ中的混合氧离子和电子传导:氧渗透和电导率的组合研究

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摘要

A combined oxygen permeation and electricalconductivity study on CaFe0.2Ti0.8O3-δ was conductedin the temperature range of 1100-850℃, aiming atclarifying the oxygen transport mechanism. The oxideshows appreciated oxygen permeability at elevatedtemperature. An oxygen permeation flux of 6.37 X 108 molcm-2 s -1 was observed at 1 100℃ by applying an oxygenpartial pressure difference to a 0.84-mm thick disk-shaped sample (Po2(h) = 0.209 and Po2(l) = 0.004 atm).The apparent activation energy for oxygen permeationremained almost unchanged ( 170 kJ/mol) with thevariation of the sample thickness in the range of 2.5-0.8mm. This indicates that the oxygen permeation kineticsis controlled by the transport of charge carriers in thebulk of sample, and can by promoted by further reductionof the thickness. In combination with electricalconductivity measurements, the partial conductivitiesof oxygen ions and electron holes, σ1and σe, weredetermined. The value of σ1 is comparable to that forσe at the high temperature of 1 100℃, but the latterbecame dominant at reduced temperature. This is due tothe much higher activation energy associated with thetransport of oxygen ions (179-4-6 kJ/mol) than that forelectron holes (22-i-2 kJ/mol). It becomes clear thatincreasing the partial conductivity of oxygen ions inthe oxide should lead to the improvement of the oxygenpermeability of the oxide.
机译:在1100-850℃的温度范围内对CaFe0.2Ti0.8O3-δ进行了氧渗透和电导率的综合研究,旨在阐明氧的传输机理。该氧化物在升高的温度下显示出令人满意的透氧性。通过将氧气分压差施加到0.84毫米厚的圆盘形样品上,观察到在1.100℃下的氧气渗透通量为6.37 X 108 molcm-2 s -1(Po2(h)= 0.209和Po2(l)= 0.004当样品厚度在2.5-0.8mm范围内变化时,表观的氧渗透活化能几乎保持不变(170 kJ / mol)。这表明氧渗透动力学受样品主体中电荷载流子的运输控制,并且可以通过进一步减小厚度来促进。结合电导率测量,确定了氧离子和电子空穴的部分电导率σ1和σe。 σ1的值与1100e高温下的σe相当,但后者在降低的温度下占主导地位。这是由于与氧离子的传输相关的活化能(179-4-6 kJ / mol)比电子空穴(22-i-2 kJ / mol)高得多。清楚的是,增加氧化物中氧离子的部分电导率应导致氧化物的氧渗透性的改善。

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