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天然水热浓缩过程中的产酸现象:临界含水量及离子组成的影响

Acid generation upon thermal concentration of natural water: the critical water content and the effects of ionic composition.

作者信息

Pulvirenti April L, Needham Karen M, Adel-Hadadi Mohamad A, Marks Charles R, Gorman Jeffrey A, Shettel Donald L, Barkatt Aaron

机构信息

Department of Chemistry, The Catholic University of America, Washington, DC 20064, United States.

出版信息

J Contam Hydrol. 2009 Oct 13;109(1-4):62-81. doi: 10.1016/j.jconhyd.2009.08.003. Epub 2009 Aug 20.

Abstract

Thermal evaporation of a variety of simulated pore waters from the region of Yucca Mountain, Nevada, produced acidic liquids and gases during the final stages of evaporation. Several simulated pore waters were prepared and then thermally distilled in order to collect and analyze fractions of the evolved vapor. In some cases, distillates collected towards the end of the distillation were highly acidic; in other cases the pH of the distillate remained comparatively unchanged during the course of the distillation. The results suggest that the pH values of the later fractions are determined by the initial composition of the water. Acid production stems from the hydrolysis of magnesium ions, especially at near dryness. Near the end of the distillation, magnesium nitrate and magnesium chloride begin to lose water of hydration, greatly accelerating their thermal decomposition to form acid. Acid formation is promoted further when precipitated calcium carbonate is removed. Specifically, calcium chloride-rich pore waters containing moderate (10-20 ppm) levels of magnesium and nitrate and low levels of bicarbonate produced mixtures of nitric and hydrochloric acid, resulting in a precipitous drop in pH to values of 1 or lower after about 95% of the original volume was distilled. Waters with either low or moderate magnesium content coupled with high levels of bicarbonate produced slightly basic fractions (pH 7-9). If calcium was present in excess of bicarbonate, waters containing moderate levels of magnesium produced acid even in the presence of bicarbonate, due to the precipitation of calcium carbonate. Other salts such as halite and anhydrite promote the segregation of acidic vapors from residual basic solids. The concomitant release of wet acid gas has implications for the integrity of the alloys under consideration for containers at the Yucca Mountain nuclear waste repository. Condensed acid gases at very low pH, especially mixtures of nitric and hydrochloric acid, are capable of corroding even alloys, such as nickel-based Alloy 22, which are considered to be corrosion-resistant under milder conditions.

摘要

对内华达州尤卡山地区多种模拟孔隙水进行热蒸发,在蒸发的最后阶段产生了酸性液体和气体。制备了几种模拟孔隙水,然后进行热蒸馏,以收集和分析逸出蒸汽的馏分。在某些情况下,蒸馏接近尾声时收集的馏出物酸性很强;在其他情况下,馏出物的pH值在蒸馏过程中相对保持不变。结果表明,后期馏分的pH值由水的初始成分决定。酸的产生源于镁离子的水解,尤其是在接近干燥时。蒸馏接近尾声时,硝酸镁和氯化镁开始失去结晶水,大大加速了它们的热分解以形成酸。当沉淀的碳酸钙被除去时,酸的形成会进一步促进。具体来说,富含氯化钙、镁含量适中(10 - 20 ppm)、硝酸盐含量适中且碳酸氢盐含量低的孔隙水会产生硝酸和盐酸的混合物,在蒸馏掉约95%的原始体积后,pH值会急剧下降至1或更低。镁含量低或适中且碳酸氢盐含量高的水会产生弱碱性馏分(pH值为7 - 9)。如果钙的含量超过碳酸氢盐,即使存在碳酸氢盐,含有适量镁的水也会产生酸,这是由于碳酸钙的沉淀。其他盐类,如石盐和硬石膏,会促进酸性蒸汽与残留碱性固体的分离。湿酸性气体的同时释放对尤卡山核废料储存库中考虑用于容器的合金的完整性有影响。极低pH值的冷凝酸性气体,尤其是硝酸和盐酸的混合物,甚至能够腐蚀在较温和条件下被认为耐腐蚀的合金,如镍基合金22。

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