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

机译:天然水热浓缩时产生酸:临界水含量和离子组成的影响

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摘要

Thermal evaporation of a variety of simulated pore waters from the region ofYucca 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.
机译:来自内华达州尤卡山地区的各种模拟孔隙水的热蒸发在蒸发的最后阶段产生了酸性液体和气体。制备了几种模拟的孔隙水,然后进行热蒸馏,以收集和分析所释放出的蒸气的馏分。在某些情况下,在蒸馏即将结束时收集的馏出液是高酸性的。在其他情况下,馏出液的pH在蒸馏过程中保持相对不变。结果表明,后面部分的pH值由水的初始组成决定。酸的产生源自镁离子的水解,尤其是在接近干燥时。在蒸馏即将结束时,硝酸镁和氯化镁开始失去水合水,极大地促进了它们的热分解以形成酸。当除去沉淀的碳酸钙时,进一步促进了酸的形成。具体来说,富含镁和硝酸盐(10-20 ppm)和低含量的碳酸氢盐的氯化钙富孔水会生成硝酸和盐酸的混合物,导致pH值在约95后急剧下降至1或更低蒸馏原始体积的%。镁含量低或中等的水以及碳酸氢盐含量高的水产生的碱性成分稍弱(pH 7-9)。如果钙的含量超过碳酸氢盐,则由于碳酸钙的沉淀,即使在存在碳酸氢盐的情况下,含适量镁的水也会产生酸。其他盐(例如,盐石和无水石膏)会促进酸性蒸气与残留碱性固体的分离。伴随着湿酸性气体的释放,对在尤卡山核废料处置场中的容器所考虑的合金的完整性有影响。 pH值极低的冷凝酸性气体,尤其是硝酸和盐酸的混合物,甚至能够腐蚀合金,例如镍基合金22,这些合金在较温和的条件下具有耐腐蚀性。

著录项

  • 来源
    《Journal of Contaminant Hydrology》 |2009年第4期|62-81|共20页
  • 作者单位

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

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

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

    Dominion Engineering Inc., 11730 Plaza America Drive, Suite 310, Reston, VA 20190, United States;

    Dominion Engineering Inc., 11730 Plaza America Drive, Suite 310, Reston, VA 20190, United States;

    Geosciences Management Institute, 1000 Nevada Way, Suite 106, Boulder City, NV 89005, United States;

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

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    yucca mountain; unsaturated zone; tydrolysis; thermal evaporation;

    机译:丝兰山非饱和带tylolysis;热蒸发;

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