phase problem

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Phase problem sorts out all the problem which occurs after the x-ray crystallization data. In this way, we have to find out maximum values of phases and amplitude both to give the better picture of electron density map and later it is verified and validated upto maximum refined 3-D structure.

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Page 1: Phase problem
Page 2: Phase problem

PHASE

PROBLEM

SWARAJ PRASAD

M.Phil BIOINFORMATICS

?

Page 3: Phase problem

Why Do We Need the Phase?

Structure Factor

Fourier transform

Inverse Fourier transform

Electron Density

In order to reconstruct the molecular image (electron density)

from its diffraction pattern both the intensity and phase, which

can assume any value from 0 to 2 , of each of the thousands ofmeasured reflections must be known.

Page 4: Phase problem

WHAT IS PHASE PROBLEM?

• From x-ray diffraction, we have obtained two parameters

• A. Amplitudes

• B. Phases

• In almost most of the cases amplitudes are retrieved but retrieving of phases is a bit difficult issue.

• In small molecule crystallography basic assumptions on atomicity and amplitudes can give rise to phase extraction.

• But, it is not possible in macromolecular crystallography.

• From that we need a different system which include, MIR, MR, SAD,MAD, AS, etc.

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Methods to solve phase problem

Molecular Isomprphous Replacement Method

A. Single Isomorphous Replacement Method

Anomalous Scattering Method

A. Single wavelength anomalous diffraction

method(SAD)

B. Multiple wavelength anomalous diffraction

method(MAD)

Page 8: Phase problem

Single Isomorphous Replacement Method

The contribution of the added heavy atom to the structure-factor amplitudes and phases is best illustrated on an Argand diagram.

The amplitudes of a reflection are measured for the native crystal, |fp|, and for the derivative crystal, |fph|.

The isomorphous difference, |fh| ’ |fph| |fp|, can be used as an estimate of the heavy atom.

Structure-factor amplitude to determine the heavy atom’s positions using patterson or direct methods.

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Argand diagram for SIR. |FP| is the

amplitude of a reflection for the native

crystal and |FPH| is that for the derivative

crystal.

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Anomalous Dispersion Methods

All elements display an anomalous dispersion (AD) effect in X-ray diffraction .

For elements such as e.g. C,N,O, etc., AD effects are negligible.

For heavier elements, especially when the X-ray wavelength approaches an atomic

absorption edge of the element, these AD effects can be very large.

The scattering power of an atom exhibiting AD effects is:

fAD = fn + f' + i f”

fnis the normal scattering power of the atom in absence of AD effects

f' arises from the AD effect and is a real factor (+/- signed) added to fnf" is an imaginary term which also arises from the AD effect

f" is always positive and 90 ahead of (fn + f') in phase angle

The values of f' and f" are highly dependent on the wave-length of the X-

radiation.

In the absence AD effects, Ihkl = I-h-k-l (Firedel’s Law).

With AD effects, Ihkl ≠ I-h-k-l (Friedel’s Law breaks down).

Page 11: Phase problem

Breakdown of Friedel’s Law

(Fhkl Left) Fn represents the total scatteringby "normal" atoms without AD effects, f’

represents the sum of the normal and real ADscattering values (fn + f'), f" is theimaginary AD component and appears 90° (at aright angle) ahead of the f’ vector and thetotal scattering is the vector F+++.

(F-h-k-l Right) F-n is the inverse of Fn (at -

hkl) and f’ is the inverse of f’, the f" vector

f’

f’

Page 12: Phase problem

Multiple Wavelength Anomalous Diffraction

method

Isomorphous replacement has several problems:

Nonisomorphism between crystals (unit-cell changes, reorientation of the protein.

Conformational changes, changes in salt and solvent ions.

Problems in locating all the heavy atoms.

Problems in refining heavy-atom positions, occupancies.

Thermal parameters and errors in intensity measurements.

Data are collected from a single crystal at several wavelengths, typically three, in order to maximize the absorption and dispersive effects.

Wavelengths are chosen at the absorption (f’’) peak (λ1), at the point of inflection on the absorption curve (λ 2), where the dispersive term f ‘ has its minimum, and at a remote wavelength (λ 3 and/or λ 4) to maximize the dispersive difference to λ 2.

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This Multiwavelength Anomalous Diffraction

method often gives very strong phase

information and is the source of many new

structures.

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SINGLE WAVELENGTH ANOMALOUS DIFFRACTION

SAD can simply utilize the intrinsic anomalous scatterers

present in the macromolecule, such as the S atoms of

cysteine and methionine or bound ions.

The challenge is in maximizing and measuring the very

small signal, since the Bijvoet ratio can be as low as 1%

when the typical merging R factor is several times this

value.

The trick lies in making multiple measurements of

reflections at an appropriate wavelength in order to

achieve a high multiplicity that will give statistically

accurate measurements of the anomalous difference.

The data should also be as complete as possible

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2.1 A ° electron-density map for the S-SAD example before and after density modification using SHELXE

Page 19: Phase problem

A SHELXE-derived 2.1 A ° resolution electron-density map phased froma Hg-SAD data set with superimposed polyalanine trace produced bySHELXE. The view is down the crystallographic threefold axis.

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PHASE IMPROVEMENT

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(a) 2.6 A ° MIR electron density. (b) Electron density after solvent flattening and histogram matching in DM. The solvent envelope determined by DM is shown in green.

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