Joe,

As David said many different types of salt crystals can grow in the presence of phosphate, even when the concentrations of PO4 or many divalent cations are VERY low (10s of micromolar or less). Struvite is common (NH4MgPO4) when ammonium sulfate is the precipitant, mM magnesium is present, and the pH is >7; struvite is a common mineral in kidney stones. If we have removed phosphate just before crystallization, as with a spin desalting column (best way) or by repeated spin concentration (poorer way), we always redouble check "hits" in divalent cation containing conditions with a variety of controls (e.g., keep the filtrate fraction from the last spin concentration step).

Michael



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On Jan 23, 2008, at 4:06 AM, David Briggs wrote:

Hi Joe,

I've known most salt crystals in Phosphate - and I think most people
are weary of phosphate.

Also, Calcium Sulphate is a fairly common one, esp if your buffers are
titrated with sulphuric acid. Fluoride Ions are also prone to form
salt crystals with transition metal ions.

HTH,

Dave


On 22/01/2008, Joe Krahn <[EMAIL PROTECTED]> wrote:
Salt crystals are common in macromolecular crystallography. Has anyone
tried to tabulate salt crystal forms that commonly occur?

I just identified a salt crystal as Mirabilite, made of Na2SO4·10H2O.
The high water content makes them rather soft, and may not be recognized
as salt right away. In this case, it probably happened because the
buffer was made with Na·Citrate + HCl instead of citric acid, while
trying to optimize conditions. So, characterization of salt crystals can
help to avoid the conditions that cause them.

There is probably a reasonably small number of salt crystal forms that are very common in crystallization trials. Maybe it would be useful to
tabulate common salt crystals to help guide optimization experiments.
Has anyone else tried to use salt crystal information beyond ensuring
that it is not protein?

Joe Krahn



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David C. Briggs PhD
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