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Net alkalinity and net acidity 1: Theoretical considerations

机译:净碱度和净酸度1:理论考虑

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Net acidity and net alkalinity are widely used, poorly defined, and commonly misunderstood parameters for the characterization of mine drainage. The authors explain theoretical expressions of 3 types of alkalinity (caustic, phenolphthalein, and total) and acidity (mineral, CO2, and total). Except for rarely-invoked negative alkalinity, theoretically defined total alkalinity is closely analogous to measured alkalinity and presents few practical interpretation problems. Theoretically defined "CO2-acidity" is closely related to most standard titration methods with an endpoint pH of 8.3 used for determining acidity in mine drainage, but it is unfortunately named because CO2 is intentionally driven off during titration of mine-drainage samples. Using the proton condition/mass-action approach and employing graphs to illustrate speciation with changes in pH, the authors explore the concept of principal components and how to assign acidity contributions to aqueous species commonly present in mine drainage. Acidity is defined in mine drainage based on aqueous speciation at the sample pH and on the capacity of these species to undergo hydrolysis to pH 8.3. Application of this definition shows that the computed acidity in mg L-1 as CaCO3 (based on pH and analytical concentrations of dissolved Fe-II, Fe-III, Mn, and Al in mg L-1): acidity(calculated) =50{1000(10(-pH)) + [2(Fe-II) + 3(Fe-III)]/56 + 2(Mn)/55 + 3(Al)/27} underestimates contributions from HSO4- and H+, but overestimates the acidity due to Fe3+ and Al3+. However, these errors tend to approximately cancel each other. It is demonstrated that "net alkalinity" is a valid mathematical construction based on theoretical definitions of alkalinity and acidity. Further, it is shown that, for most mine-drainage solutions, a useful net alkalinity value can be derived from: (1) alkalinity and acidity values based on aqueous speciation, (2) measured alkalinity minus calculated acidity, or (3) taking the negative of the value obtained in a standard method "hot peroxide" acidity titration, provided that labs report negative values. The authors recommend the third approach; i.e., net alkalinity = -Hot Acidity.
机译:净酸度和净碱度被广泛使用,定义不当,并且通常被误解为表征矿井排水的参数。作者解释了三种碱度(苛性碱,酚酞和总碱度)和酸度(矿物质,二氧化碳和总碱度)的理论表达式。除了很少调用的负碱度外,理论上定义的总碱度与测得的碱度非常相似,几乎没有实际的解释问题。理论上定义的“ CO2酸度”与大多数标准滴定方法密切相关,其终点pH值为8.3,用于确定矿山排水中的酸度,但是由于在矿山排水样品的滴定过程中有意驱散了CO2,因此命名不便。作者使用质子条件/质量作用方法并使用图形来说明随着pH值的变化而形成的物种,作者探索了主要成分的概念以及如何为矿井排水中常见的水生物种分配酸度。矿山排水中的酸度是基于样品pH值下的水形态和这些物质水解至pH 8.3的能力来定义的。应用此定义表明,以CaCO3计,以mg L-1计算的酸度(基于pH值和mg L-1中溶解的Fe-II,Fe-III,Mn和Al的分析浓度):酸度(计算值)= 50 {1000(10(-pH))+ [2(Fe-II)+ 3(Fe-III)] / 56 + 2(Mn)/ 55 + 3(Al)/ 27}低估了HSO4-和H +的贡献,但是高估了Fe3 +和Al3 +引起的酸度。但是,这些误差往往会相互抵消。证明“净碱度”是基于碱度和酸度的理论定义的有效数学构造。此外,还表明,对于大多数矿井排水溶液,有用的净碱度值可以从以下各项得出:(1)基于水体形态的碱度和酸度值;(2)测得的碱度减去计算出的酸度;或(3)如果实验室报告为负值,则使用标准方法“热过氧化物”酸度滴定法获得的值的负值。作者推荐了第三种方法。即净碱度=-热酸度。

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