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首页> 外文期刊>Applied Geochemistry: Journal of the International Association of Geochemistry and Cosmochemistry >Alteration of nuclear glass in contact with iron and claystone at 90 degrees C under anoxic conditions: Characterization of the alteration products after two years of interaction
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Alteration of nuclear glass in contact with iron and claystone at 90 degrees C under anoxic conditions: Characterization of the alteration products after two years of interaction

机译:在缺氧条件下于90摄氏度与铁和粘土接触的核玻璃的蚀变:相互作用两年后蚀变产物的表征

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摘要

The present study investigates the alteration of a fractured glass block in contact with iron and Callovo-Oxfordian claystone at 90 degrees C under anoxic and water-saturated conditions. The alteration rates and the nature of glass alteration products at the different compact interfaces (glass-clay, glass-iron) and in cracks were assessed by solution chemistry and microscopic-scale techniques (scanning electron microscopy coupled with energy-dispersive X-ray microscopy, microRaman spectroscopy, and X-ray absorption fine structure spectroscopy). A significant but modest (two-fold) increase in glass alteration in contact with steel was observed, leading to an average alteration rate over the experiment of about 0.007-0.014 g/m(2)/d. This rate is significantly lower than forward rate r(0) in clay-equilibrated groundwater (1.7 g/m(2)/d), indicating that a decrease of the alteration rate was not hindered by the steel presence. The corrosionealteration interface was made up of successive layers of corrosion products in contact with iron, a layer of Fe silicates, and an altered glass layer enriched in Fe. Characterization of the glass block in direct contact with claystone revealed that the thickness of altered glass was much more important than at the glass-iron interface. The altered glass layer in contact with clay was slightly enriched in Fe and Mg, and depleted in alkali cations. Altered glass layers in cracks were usually limited to fringes thinner than 2 mm, with a thickness decreasing from the crack mouth, indicating that alteration is controlled by transport in the cracks. The fractures were partially filled with calcite and lanthanide hydroxocarbonate precipitates. These results contribute to the understanding of nuclear vitrified waste-iron-corrosion products interactions in a deep geological repository. (C) 2016 Elsevier Ltd. All rights reserved.
机译:本研究研究了缺氧和水饱和条件下,在90摄氏度下与铁和卡洛沃-牛津黏土接触时破裂的玻璃块的变化。通过溶液化学和微观尺度技术(扫描电子显微镜与能量色散X射线显微镜相结合)评估了不同致密界面(玻璃粘土,玻璃铁)和裂纹处的玻璃蚀变产物的蚀变率和性质。 ,显微拉曼光谱和X射线吸收精细结构光谱)。观察到与钢接触的玻璃蚀变显着但适度(两倍)增加,导致整个实验的平均蚀变率约为0.007-0.014 g / m(2)/ d。该速率显着低于粘土平衡的地下水中的前进速率r(0)(1.7 g / m(2)/ d),表明改变速率的降低不受钢存在的阻碍。腐蚀吸气界面由与铁接触的腐蚀产物的连续层,一层铁硅酸盐和一层富含铁的蚀变玻璃层组成。与粘土岩直接接触的玻璃块的特征表明,蚀变玻璃的厚度比在玻璃-铁界面处重要得多。与粘土接触的蚀变的玻璃层稍微富含Fe和Mg,并且贫化了碱金属阳离子。裂纹中被更改的玻璃层通常限于小于2毫米的条纹,其厚度从裂纹口开始减小,这表明更改是由裂纹中的传输控制的。裂缝中部分充满了方解石和镧系元素碳酸氢盐沉淀。这些结果有助于理解深层地质处置库中的核玻璃化废铁腐蚀产物的相互作用。 (C)2016 Elsevier Ltd.保留所有权利。

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