MadSci Network: Chemistry |
Kimberly, the easiest way to test whether a compound is a hydrate is to heat (dry) it at temperatures above the boiling point of water. If you were to weigh the hydrated material before drying and after, and with a knowledge of the material (so that you had the molecular weight), and expecting that all water was driven off (you can continue to dry until the weight stops changing), then the final weight of the material allows you to calculate how many molecules of the material are left (in a unit called "moles", akin to "dozen" or "gross", or any such "collection" unit. Let's label this X). The difference in weight before and after drying can be used with the molecular weight of water to find how many molecules of water were driven off (again, in units of moles. Let's label this Y). Your hydrated formula is then: desicant molecule_X (H2O)_Y (reported with X and Y as the lowest whole numbers possible, see for example cobalt chloride hexahydrate) Because water is weakly bound to compounds such as cobalt (II) chloride, these materials serve as water "traps". The water can be driven off and the material reused to trap water again (these naterials are collectively called "desiccants"). There is a maximum amount of water which may be taken up by any particular substance, which depends upon the ability of the water molecules to pack closely enough to the substance so that they experience an attractive interaction with its electron "cloud". In the case of CoCl2, you can only pack 6 water molecules (the hexahydrate) in before there is no more physical room left. This means that you can use these materials to collect up to some particular level of water, which can be predicted by stoichiometry and mass of the desiccant. As such, they are often used to keep an enclosed volume free of water vapor and the items contained in this volume "dry". Using these materials to predict weather (humidity), estimate water concentrations in air, etc. is much more difficult. Knowledge of the uptake rates for water within the desiccant (which change with how much water is already there), the surface area (average) of the desiccant, and other such properties would be necessary to extract an estimate of the water concentration. Instead, humidity probes often depend upon physical phenomena to measure water vapor concentrations. One such method is with a strain gauge, which involves a change in the shape of a small piece of material with differing amounts of water "stuck" to it. This amount of water is "equilibrated" with the surface (as one molecule leaves, another sticks), rather than the case with a desiccant where the water binds tightly enough that it takes heat to remove. I hope this information is helpful. Please feel free to email me with further questions (weibelm@battelle.org) Bets Regards, Mike
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