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Heat extraction from a crystal depends on the thermal conductivity AND the temperature gradient. If you start with a colder crystal you can tolerate a larger temperature gradient before hitting the glass transition temperature, and thus, in principle, transfer heat more rapidly. I believe initial tests with Helium cooling didn't end up helping much if anything compared to lN2 because Helium has a poor heat capacity compared to N2 gas. I think these initial tests were reported by Gert Rosenbaum and others but I may be wrong here.

Bart

Ethan Merritt wrote:
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Ian wrote>

Unless of course the crystal isn't as cold as you think it is!
Essentially all of the energy of absorbed X-ray photons must ultimately
be degraded to thermal energy, and unless this is efficiently conducted
to the surface where it can be removed by the cold stream, it's going to
produce some 'hot spots' which given sufficient X-ray flux may be
sufficient to cause local melting of the water glass.


On Tuesday 25 April 2006 09:05 am, Sebastiaan Werten wrote:

In which case one might expect better stability of crystals if helium
cooling is applied (ceteris paribus). Has this been observed?


If you mean "can a colder crystal withstand a more intense beam?"
the "expected" improvement has not, to my knowledge, been observed.
Some references here:
        http://biop.ox.ac.uk/www/lj2000/garman/garman_01.html

My understanding is that the limiting factor is the thermal conductivity
of the crystal itself.  Heat (photons) is deposited internally, and
must be transferred through the body of the crystal and possibly through
a bead of surrounding frozen buffer before it can be lost to the
external cooling stream.  Making the crystal colder does not by itself
make this internal transfer any faster unless it also changes the
thermal conductivity. So if you start with a colder crystal it may
take fractionally longer to reach a harmful temperature, but the
x-ray flux that can be handled at equilibrium without continued
temperature rise remains the same.
One could speculate that the thermal conductivity will increase at
sufficiently cold temperatures (superconductivity), but I am dubious
this is relevant to protein crystals.
Note that this is a slightly different question than "does the crystal
diffract better, or decay more slowly".  The latter is a question that
can be asked of a crystal in thermal equilibrium at various temperatures.
        Hanson et al, J. Synchrotron Rad. (2002). 9, 375-381.

Perhaps someone can contribute additional pointers to relevant work.









Sebastiaan Werten.


----------

Unless of course the crystal isn't as cold as you think it is!
Essentially all of the energy of absorbed X-ray photons must ultimately
be degraded to thermal energy, and unless this is efficiently conducted
to the surface where it can be removed by the cold stream, it's going to
produce some 'hot spots' which given sufficient X-ray flux may be
sufficient to cause local melting of the water glass.  There could well
be a steep temperature gradient, liq N2 temperature at the surface and
much warmer towards the centre.  Also if low molecular weight solutes
are present the melting point could be locally depressed way below that
of pure water, so there wouldn't be quite so far to go to cause melting.
Admittedly I haven't looked at any calculations of what order of
magnitude the heating and heat conduction effects might be for a typical
flux and I could be way off beam but it's a least a theoretical
possibility.

-- Ian


-----Original Message-----
From: [EMAIL PROTECTED] [mailto:[EMAIL PROTECTED] On
Behalf Of James Holton
Sent: Tuesday, April 25, 2006 3:11 PM
To: Udupi Ramagopal
Cc: Uhnsoo Cho; [EMAIL PROTECTED]
Subject: Re: [ccp4bb]: Radiation damage problem

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It is definitely true that some sensitive residues decay quite a bit
faster than the high-resolution spots.  This has been repoted
in several
papers now.  What has not been repoted (to my knowledge) is a
convincing
connection between the decay of side chains involved in a crystal
contact and the loss of high-resolution data.  In all of the
studies I
have seen that measure the rate of loss of resolution, it is always
tightly related to dose.  If you know of a study where it has
been shown
to be related to something else, I would like to hear about it.

 I, personally, do not think that there is a connection between
specific damage near crystal contacts and loss of resolution.  My
reasoning is that a cryo-cooled crystal is permeated by a matrix of
glassy water.  Glassy water is a SOLID.  So, once cooled, the crystal
lattice is supported by a lot more than just crystal
contacts.  Kind of
like an insect preserved in amber.  Breaking bonds near the
contacts are
not going to do much more distortion to the overall lattice
than broken
bonds in the core or even in the solvent.  Diffraction is a
process that
occurs over dozens of unit cells.  There must be long-range
distortions
to impact it.  Site-specific damage, formally, only impacts
the B-factor
of that site.

-James Holton
MAD Scientist


Udupi Ramagopal wrote:


I think some times the sensitivity of residues involved in critical
cystal contacts
can disturb these valuable suggestions and calculations.

Ramu

On Mon, 24 Apr 2006, James Holton wrote:


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Disclaimer:

Radiation damage is a complex phenomenon, and many aspects

of radiation

damage at low temperature are still hard to explain, let

alone predict.

You DEFINITELY need to know things like the beamline's

brightness and

the concentrations of any atoms in your sample heavier

than oxygen to

even have a ghost of a chance of understanding the origin of your
problem.

However...

If you are used to this beamline and you "feel" that these

crystals are

decaying faster than "normal", then the most likely

problem is that you

have a heavy atom in your sample. This will cause your

crystal to absorb

a lot more x-rays than normal (doing more damage).

Anything heavier than

oxygen is a potential problem, and stuff in the solvent counts! The
"rule of thumb" is that the "absorptivity" of an atom is roughly
proportional to the atomic number. So, try doing things

like replacing

potassium with lithium or iodide with fluoride (each a

factor of 6).

Obviously, the more concentrated a heavy atom is, the

bigger the problem

will be.

Since beamline brigthnesses vary by a factor of 30,000

from place to

place, and crystal absorptivity can vary by a factor of 10 or more,
radiation damage questions can be hard to answer without

knowing flux,

beam size and sample composition.

But, if you do know these things...

The decay in protien crystals is generally proportional to

absorbed dose

(Joules/kg or "Gray"). Dose, in turn is proportional to fluence
(photons/mm^2) and the "extinction coefficient" of your

crystal in the

x-ray range. You get fluence (photons/mm^2) from flux

(photons/s) by

dividing by the beam size to get brightness (photons/mm^2/s) and
multiplying by the total exposure time (in seconds). Given

the beamline

flux, wavelength, beam size, and crystal composition the expected
lifetime of your crystal can be computed with a program

called RADDOSE

(Murray et. al. JSR (2005), 12, 268-75). Or you can "google" for
RADDOSE.

For example, you can expect the lifetime of your crystal will be
(roughly) cut in half by the addition of 4M NaCl, 5M

NH4SO4, 1 Se per 30

residues (at 0.97A), or 150 mM CsI.

-James Holton
MAD Scientist


Uhnsoo Cho wrote:


Dear bulletin members,
Sorry for non-CCP4 related questions.
Recently, I've got crystals which have a radiation damage problem.
It also has a weak diffraction because of the big unit

cell dimension

(about 300A in one direction), so I have to overexpose

crystals even

with the synchrotron beam.
The problem is that during the data collection, the

resolution decaded

gradually from 3 to 6A after certain number of frames

(about 30 or 40

frames).
Do you have any experiences or any suggestions that I can

evade this

radiation damage?
Any suggestions will be grateful.
Thank you.
Best regards,
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Uhn-Soo,Cho
Graduate student in Biological Structure Department
University of Washington.
HSB G514
1959 NE Pacific St.
Seattle, WA 98195-7420
Box. 357420
Fax #206-543-1524
Tel # 206-221-2435
~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~





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