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Erice school, June 2012<br />

<strong>SAD</strong>/<strong>MAD</strong> <strong>phasing</strong><br />

Zbigniew Dauter<br />

Natl. Cancer Inst. / Argonne Natl. Lab.


Structure factor<br />

F P = Σ j f j<br />

.exp 2πi(h . r j )<br />

Structure factor F P can be expressed in the form of


Structure factor with heavy atoms<br />

F PH = Σ j f j<br />

.exp 2πi(h . r j ) + Σ h f h. exp 2πi(<br />

F PH = F P +<br />

al structure factor F PH as a sum of contributions of norm


Anomalous scattering<br />

normal scattering<br />

θ <br />

θ <br />

anomalous (resonant) scattering<br />

Additional contribution if the energy of X-rays is


Structure factor and anomalous effect<br />

For anomalously scattering atoms<br />

f j = fº j (θ) + f’ j (λ) + i . f” j (λ)<br />

Anomalous correction f” is proportional<br />

to absorption and fluorescence and<br />

dispersive correction f’ is its derivative


Anomalous corrections f’ and f” for Se<br />

black –<br />

theory for single<br />

atom in vacuum<br />

Absorption edge<br />

for Se at 0.979 Å<br />

blue –<br />

measured curve<br />

from real sample<br />

ten the extra EXAFS features (e.g. white line) occurring


nfluence of anomalous effect on phases<br />

i . exp iα<br />

= i . (cos α + i . sin α)<br />

= i . cos α – sin α <br />

= i . sin (90 o +α) + cos (90<br />

= exp i . (90 o +α)<br />

f j = fº j (θ) + f’ j (λ) + i . f” j (λ)<br />

Anomalous correction if” shifts the phase


nfluence of anomalous effect on phases<br />

Anomalous correction if” shifts the phase


Friedel pair: F(h) and F(-h)<br />

Anomalous correction f”<br />

causes the positive<br />

phase shift of both<br />

F(h) and F(-h)<br />

in effect<br />

|F(h)| ≠ |F(-h)|<br />

and<br />

Friedel’s Law<br />

is broken


Friedel pair: F(h) and *F(-h)<br />

|F(h)| ≠ |F(-h<br />

Friedel’s La<br />

does not ho<br />

t is customary to present F(-h) as *F(-h), with its phase


Friedel pair more realistically<br />

f º (S) = 16<br />

f”(S) = 0.56<br />

for λ = 1.5<br />

f º (Hg) = 82<br />

f”(Hg) ≈ 4.<br />

for λ < 1.0<br />

e anomalous differences are 1 – 5 % of the total intensit


Bijvoet difference<br />

e observed anomalous Bijvoet difference ΔF ± = |F + | - |F


Bijvoet difference<br />

ΔF ± = 2 F” sin(ϕ – ϕ )


Bijvoet difference depends on (ϕ T – ϕ A )<br />

The observed Bijvoet difference ΔF ± is largest when<br />

o<br />

o


Locating anomalous atoms from ΔF<br />

Most proper for locating anomalous atoms are F A ’s,<br />

but they are not measurable directly, however<br />

ΔF ± = 2 F ” A sin(ϕ T - ϕ A ) = 2 F A (f”/fo ) sin(ϕ T - ϕ A )<br />

therefore<br />

ΔF ± ≈ F A for large Bijvoet differences<br />

Measured anomalous differences can be used to<br />

locate anomalous atoms by Patterson or direct methods


There are two places wh<br />

the properly oriented pin<br />

vector 2F” corresponds<br />

anomalous difference ΔF<br />

ingle-wavelength Anomalous Diffraction)<br />

f the anomalous substructure is known, F A , F’ A , F” A , ϕ A


<strong>SAD</strong> phase ambiguity<br />

ϕ <strong>SAD</strong> = (ϕ 1 + ϕ 2 )<br />

F <strong>SAD</strong> = F T . FOM<br />

where<br />

figure-of-meri<br />

FOM = cos (α<br />

t is not known which solution is correct, therefore one ca


Electron density map<br />

F good F wrong F good + F wrong<br />

ince Fourier summation is additive, the resulting electro


Solvent flattening<br />

F good F wrong F good + F wrong<br />

e featureless solvent regions of this map can be flattene


With errors in measured |F | and |F |<br />

The measured amplitudes are not perfectly accurate,


With errors in measured |F | and |F |<br />

In effect, the phase probability varies<br />

o<br />

P anom (ϕ Τ )=N exp{-[ΔF ± +2F” A sin(ϕ T -ϕ A


Known partial structure<br />

P part (ϕ Τ )=N exp{2[F T F A )/F N2 ] co<br />

The case where normal and anomalous vectors


With both probabilities combined<br />

When anomalous and partial structure probabilities


emote (high energ<br />

Multi-wavelength anomalous diffraction)<br />

peak (white line)<br />

edge (inflection po<br />

These three wavelengths give largest differences


Multi-wavelength anomalous diffraction)<br />

peak (maximum f”, medium f<br />

edge (maximum f’, medium f<br />

remote (large f”, very small f<br />

These three wavelengths give largest differences


Analytical <strong>MAD</strong> (after Hendrickson)<br />

|F Τ+ | 2 = |F To | 2 + y 2 – 2 |F To | y cosα<br />

y 2 = |F A ’| 2 + |F A ”| 2 = |F A | 2 [(f’ 2 +f” 2 )/f o2 ]<br />

y cosα = x 1 + x 2 = |F A | (f’/f o ) cosδ + |F A | (f’/f<br />

δ = ϕ A - ϕ T<br />

Law of cosines applied


Analytical <strong>MAD</strong> (after Hendrickson)<br />

T ± | 2 = |F To | 2 + a(λ) |FA| 2<br />

+ b(λ) |F To | |F A | cos(ϕ T – ϕ A )<br />

± c(λ) |F To | |F A | sin(ϕ T – ϕ A )<br />

a(λ) = (f’ 2 + f” 2 )/f o2<br />

b(λ) = 2 f’/f o<br />

c(λ) = 2 f”/f o<br />

the same for all reflection<br />

at the same wavelength<br />

stem of equations with three unknowns, |F To |, |F A |, (ϕ T -<br />

n be solved analytically with more than one wavelength<br />

en |F A | is used to locate anomalous substructure and<br />

lculated ϕ A gives |F To | and ϕ T necessary for the map


Probabilistic <strong>MAD</strong><br />

owadays <strong>MAD</strong> <strong>phasing</strong> is based on a probabilistic appro<br />

Maximum Likelihood, taking into account various effects<br />

e errors in measured amplitudes, inaccuracies of the<br />

bstructure model, non-isomorphism, or even radiation<br />

mage and anisotropy of f”.<br />

Excellent and powerful programs are widely available:<br />

SHARP, PHASER, SOLVE, MLPHARE


<strong>SAD</strong> with peak wavelength


<strong>SAD</strong> with edge wavelength


<strong>MAD</strong> with two wavelengths<br />

Only one of possible solutions


<strong>MAD</strong> with two wavelengths<br />

Probability for the correct solution


Excit

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