H2 Production Mechanisms in Irradiated Portlandite: Surface and Volume Contributions

IF 3.3 3区 化学 Q2 CHEMISTRY, PHYSICAL The Journal of Physical Chemistry C Pub Date : 2024-11-07 DOI:10.1021/acs.jpcc.4c05914
Thibaut Herin, Antonino Alessi, Stéphane Poyet, Pascal Bouniol, Sophie Le Caër
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Abstract

Calcium hydroxide or portlandite (Ca(OH)2) is the second most abundant hydrate in cementitious materials. The latter form the basis of the coating matrices of some forms of radioactive waste. Under ionizing radiation, this results in the production of radiolytic molecular hydrogen, which, when it accumulates in the environment, may raise safety concerns. It is important, therefore, to understand how radiation interacts with these materials, and especially with portlandite. This hydroxide is of particular interest: on exposure to irradiation, it not only leads to the immediate production of molecular hydrogen but also to a delayed production over long periods of time (days or even weeks) after the irradiation stops. It follows that it is important to determine the reaction mechanisms operating in this system. This was carried out here based on experiments with electron paramagnetic resonance spectroscopy, which identified the different radicals generated under radiation. As a result, we have been able to show that the immediate production of H2 is due to the stabilization of electrons on the surface of the portlandite, followed by surface reactions that encourage the immediate release of H2 into the gaseous atmosphere. When the dose increases, the number of these sites drops, leading to a fall in the production of the molecular hydrogen immediately released. The delayed production of H2 is due to the formation of hydrogen atoms followed by their dimerization within the portlandite crystal lattice, with the result that the molecular hydrogen molecules are trapped. In this case, the movement of the hydrogen atoms in the crystal lattice sets the CaO radicals in motion. At low doses, these radicals dimerize to form CaO-OCa peroxides. At higher doses, the CaO radicals can react with hydrogen atoms, which restricts the formation of the trapped H2. The range of different reaction intermediates identified reflects the richness of the chemical processes involved in the mechanisms, which accounts for the behavior of portlandite on exposure to irradiation.

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辐照硅酸盐岩中的 H2 生成机制:表面和体积贡献
氢氧化钙或波长石(Ca(OH)2)是胶凝材料中第二大水合物。后者是某些形式放射性废物涂层基质的基础。在电离辐射下,会产生放射性分子氢,当其在环境中积累时,可能会引发安全问题。因此,了解辐射与这些材料,尤其是与波长石的相互作用非常重要。这种氢氧化物尤其引人关注:在受到辐照时,它不仅会立即产生分子氢,还会在辐照停止后的很长一段时间(几天甚至几周)内延迟产生。因此,确定该系统的反应机制非常重要。我们在电子顺磁共振光谱实验的基础上,确定了在辐照下产生的不同自由基。结果表明,H2 的立即产生是由于波长石表面电子的稳定,随后的表面反应促使 H2 立即释放到气体环境中。当剂量增加时,这些位点的数量减少,导致立即释放的分子氢的产生量减少。H2 的延迟产生是由于氢原子形成后在波长石晶格内发生二聚化,导致氢分子被截留。在这种情况下,氢原子在晶格中的运动会引发 CaO- 自由基的运动。低剂量时,这些自由基二聚形成 CaO-OCa 过氧化物。在较高剂量下,CaO- 自由基可与氢原子发生反应,从而限制了捕获的 H2 的形成。已确定的不同反应中间体的范围反映了机理中涉及的化学过程的丰富性,这也说明了波长石在暴露于辐照时的行为。
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来源期刊
The Journal of Physical Chemistry C
The Journal of Physical Chemistry C 化学-材料科学:综合
CiteScore
6.50
自引率
8.10%
发文量
2047
审稿时长
1.8 months
期刊介绍: The Journal of Physical Chemistry A/B/C is devoted to reporting new and original experimental and theoretical basic research of interest to physical chemists, biophysical chemists, and chemical physicists.
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