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Catalytic SO3 Decomposition Activity and Stability of Pt Supportedon Anatase TiO2 for Solar Thermochemical Water-SplittingCycles

机译:负载Pt的催化SO3分解活性和稳定性。锐钛矿型TiO2用于太阳热化学水分解的研究周期数

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摘要

Pt-loaded anatase TiO2 (Pt/TiO2-A) was found to be a highly active and stable catalyst for SO3 decomposition at moderate temperatures (∼600 °C), which will prove to be the key for solar thermochemical water-splitting processes used to produce H2. The catalytic activity of Pt/TiO2-A was found to be markedly superior to that of a Pt catalyst supported on rutile TiO2 (Pt/TiO2-R), which has been extensively studied at a higher reaction temperature range (≥800 °C); this superior activity was found despite the two being tested with similar surface areas and metal dispersions after the catalytic reactions. The higher activity of Pt on anatase is in accordance with the abundance of metallic Pt (Pt0) found for this catalyst, which favors the dissociative adsorption of SO3 and the fast removal of the products (SO2 and O2) from the surface. Conversely, Pt was easily oxidized to the much less active PtO2 (Pt4+), with the strong interactions between the oxide and rutile TiO2 forming a fully coherent interface that limited the active sites. A long-term stability test of Pt/TiO2-A conducted for 1000 h at 600 °C demonstrated that therewas no indication of noticeable deactivation (activity loss ≤4%) over the time period; this was because the phase transformationfrom anatase to rutile was completely prevented. The small amountof deactivation that occurred was due to the sintering of Pt and TiO2 and the loss of Pt under the harsh reaction atmosphere.
机译:发现负载铂的锐钛矿型TiO2(Pt / TiO2-A)是在中等温度(〜600°C)下分解SO3的高活性和稳定催化剂,将被证明是所用太阳能热化学水分解工艺的关键产生H2。发现Pt / TiO2-A的催化活性明显优于负载在金红石TiO2上的Pt催化剂(Pt / TiO2-R),后者已在更高的反应温度范围(≥800°C)进行了广泛研究;尽管在催化反应后以相似的表面积和金属分散体对两者进行了测试,但仍发现这种优异的活性。 Pt对锐钛矿的较高活性取决于该催化剂中金属Pt的丰度(Pt 0 ),这有利于SO3的解离吸附和产物(SO2和O2)的快速去除。 )。相反,Pt容易被氧化成活性较低的PtO2(Pt 4 + ),氧化物与金红石TiO2之间的强相互作用形成了一个完全连贯的界面,从而限制了活性位点。 Pt / TiO2-A在600°C下进行1000 h的长期稳定性测试表明没有明显的失活迹象(活动度≤4%);这是因为相变从锐钛矿到金红石完全被阻止。少量失活的发生是由于Pt和TiO2的烧结以及苛刻的反应气氛下Pt的损失。

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