Actually, there is a particular kind of "freezing" than can be a good thing: cubic ice. The specific volume of cubic ice is about 2% higher than that of amorphous solid water (or hyperquenched glassy water). In cases where the "preferred" specific volume of the protein lattice is a little bigger than the "preferred" specific volume of the stuff in the solvent channels upon vitrification, a small amount of cubic ice "character" can actually make your crystal diffract better.

Basically, a mis-match in the "preferred" volume of the protein and solvent creates stress, and stress makes high-angle spots go away (see Juers et al. 2001, 2004). I think this is one of the most under-appreciated things about screening for cryos, and seems to be the main cause of that mythical "one crystal in a thousand that diffracted well" problem. In my experience, this means you are being very consistent in your cryo-cooling but you made one mistake. Final density upon flash-cooling is VERY sensitive to the cooling rate, and little things like the thickness of the layer of cold N2 gas above your liquid N2 can change the cooling rate by a factor of 100 or so (Warkentin et al. 2006).

You can tell if you've got some cubic ice character by looking at the background of your diffraction pattern. Hexagonal ice has three rings at 3.45, 3.68, and 3.91 A, whereas cubic ice only has the 3.68 A ring. Moreover, noone has ever grown a macroscopic crystal of cubic ice, and the smaller the crystallites get, the broader the 3.68 A ring becomes. Eventually, it can be hard to tell the difference between nano-crystalline cubic ice and the diffuse background expected for "amorphous" solvent. You have to look carefully at the width of the "water ring", because the first major diffuse ring from amorphous solid water is also at 3.68 A. In fact, all the major diffraction peaks of cubic ice are precisely centered on the diffuse rings of amorphous solid water. This is perhaps not a coincidence, but it does mean that there is a continuum of states between a sharp "ice ring" and an amorphous "water ring". Your best diffraction may well be somewhere in the middle.

-James Holton
MAD Scientist

On 11/15/2012 10:12 AM, A Leslie wrote:
Dear Sebastiano,

This is not entirely straight-forward. The Oxford English dictionary gives the first definition of "freeze" relevant to this discussion as: "Of (a body of) water: be converted into or become covered with ice through loss of heat"

This is certainly not what we want to do to our crystals.

However, another definition in OED is:
"Cause (a liquid) to solidify by removal of heat", suggesting that this does not necessarily mean the formation of crystals.

The Larousse Dictionary of Science and Technology (1995) has the following definition: "Freeze-drying (Biol.) A method of fixing tissues sufficiently rapidly as to inhibit the formation of ice-crystals."

The Dictionary of Microbiology and Molecular Biology (3rd Ed) in the entry on "Freezing" has the sentence: "Rapid freezing tends to prevent the ice crystal formation by encouraging vitrification".

Both of these erstwhile volumes therefore suggest that freezing does not necessarily imply the formation of crystals. However, the term is ambiguous, while vitrification is not.

Personally I use "cryocooled" instead.

Best wishes,

Andrew



On 15 Nov 2012, at 17:13, Sebastiano Pasqualato wrote:


Hi folks,
I have recently received a comment on a paper, in which referee #1 (excellent referee, btw!) commented like this:

"crystals were vitrified rather than frozen."

These were crystals grew in ca. 2.5 M sodium malonate, directly dip in liquid nitrogen prior to data collection at 100 K. We stated in the methods section that crystals were "frozen in liquid nitrogen", as I always did.

After a little googling it looks like I've always been wrong, and what we are always doing is doing is actually vitrifying the crystals. Should I always use this statement, from now on, or are there english/physics subtleties that I'm not grasping?

Thanks a lot,
ciao,
s


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