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In the case of dilute HCl where the addition of a salt is not problematic for a particular application, one may consider the addition of anhydrous
calcium chloride (or, a concentrated solution thereof) as a possibility. The reason relates to the apparent significant increase in the so called
'activity level' upon adding MgCl2 or CaCl2 or NaCl (in declining order of preference). Here is a real world reference relating to practical
significance in the field of Hydrometallury where leaching out minerals from ores efficiently and cheaply is a major concern. Source: See
"Hydrometallurgy in Extraction Processes", Vol I, by C. K. Gupta and T. K. Mukherjee, page 15 at http://books.google.com/books?id=F7p7W1rykpwC&pg=PA15 .
Note, the author claims there is data confirming that a 2M HCl in 3M MgCl2 or CaCl2 (and also FeCl3) behaves like 7M HCl!
Here is a quote on the matter of discussion in one of the reference sources previously provided by Bfesser on Thermodynamic Activity (see http://en.wikipedia.org/wiki/Thermodynamic_activity ):
"When a 0.1 M hydrochloric acid solution containing methyl green indicator is added to a 5 M solution of magnesium chloride, the color of the
indicator changes from green to yellow—indicating increasing acidity—when in fact the acid has been diluted. Although at low ionic strength
(<0.1 M) the activity coefficient approaches unity, this coefficient can actually increase with ionic strength in a high ionic strength regime. For
hydrochloric acid solutions, the minimum is around 0.4 M.[1]"
[Edited on 22-10-2014 by AJKOER] |