Presentation on theme: "Overview of the Phase Problem ProteinDataCrystalStructurePhases Remember We can measure reflection intensities We can calculate structure factors from."— Presentation transcript:
Overview of the Phase Problem ProteinDataCrystalStructurePhases Remember We can measure reflection intensities We can calculate structure factors from the intensities We can calculate the structure factors from atomic positions We need phase information to generate the image
x,y.z X-ray Diffraction Experiment All phase information is lost F hkl [Real Space][Reciprocal Space] What is the Phase Problem In the X-ray diffraction experiment photons are reflected from the crystal lattice (planes) in different directions giving rise to the diffraction pattern. Using a variety of detectors (film, image plates, CCD area detectors) we can estimate intensities but we loose any information about the relative phase for different reflections.
Let’s define a phase for an individual atom, j An atom at x j =0.40, y j =0.25, z j =0.10 for plane  For k = 0 (a 2D case) then For plane  Now to understand what this means…. j = 2 [ 2(0.40) + 1(0.25) + 3(0.10)] = 2 j = 2 [ 2(0.40) + 1(0.10)] = 2 Phases
201 Phases A B G C H D F I E A B G C H D F I E 0° 720° c0 a 201 planes 4p 360° 2p 1080° 6p 0.4, y, 0.1 D = 2 [ 2(0.40) + 1(0.10)] = 2
0 c a d hkl 6π 4π 2π Atom (j) at x,y,z φ Plane hkl Remember: We express any position in the cell as (1) fractional coordinates p xyz = x j a+y j b+z j c (2) the sum of integral multiples of the reciprocal axes hkl = ha* + kb* + lc* In General for Any Atom (x, y, z)
Phase for Any Atom
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 of measured reflections must be known.
Importance of Phases Hauptman amplitudes with Hauptman phases Hauptman amplitudes with Karle phases Karle amplitudes with Karle phases Karle amplitudes with Hauptman phases Phases dominate the image! Phase estimates need to be accurate
Understanding the Phase Problem The phase problem can be best understood from a simple mathematical construct. The structure factors (F hkl ) are treated in diffraction theory as complex quantities, i.e., they consist of a real part (A hkl ) and an imaginary part (B hkl ). If the phases, hkl, were available, the values of A hkl and B hkl could be calculated from very simple trigonometry: A hkl = |F hkl | cos ( hkl ) B hkl = |F hkl | sin ( hkl ) this leads to the relationship: (A hkl ) 2 + (B hkl ) 2 = |F hkl | 2 = I hkl
Argand Diagram The above relationships are often illustrated using an Argand diagram (right). From the Argand diagram, it is obvious that A hkl and B hkl may be either positive or negative, depending on the value of the phase angle, hkl. Note: the units of A hkl, B hkl and F hkl are in electrons. (A hkl ) 2 + (B hkl ) 2 = |F hkl | 2 = I hkl
sinΘ/λ f0f0 Here f j is the atomic scattering factor The scattering factor for each atom type in the structure is evaluated at the correct sinΘ/λ. That value is the scattering ability of that atom. Remember We now have an atomic scattering vector with a magnitude f 0 and direction φ j. The Structure Factor Atomic scattering factors
real imaginary Individual atom f j s Resultant F hkl A hkl B hkl The Structure Factor Sum of all individual atom contributions
Electron Density Remember the electron density (image of the molecule) is the Fourier transform of the structure factor F hkl. Thus Here V is the volume of the unit cell In practice, the electron density for one three-dimensional unit cell is calculated by starting at x, y, z = 0, 0, 0 and stepping incrementally along each axis, summing the terms as shown in the equation above for all hkl (as limited by the resolution of the data) at each point in space.
Solving the Phase Problem Small molecules Direct Methods Patterson Methods Molecular Replacement Macromolecules Multiple Isomorphous Replacement (MIR) Multi Wavelength Anomalous Dispersion (MAD) Single Isomorphous Replacement (SIR) Single Wavelength Anomalous Scattering (SAS) Molecular Replacement Direct Methods (special cases)
MACROMOLECULES Solving the Phase Problem SMALL MOLECULES The use of Direct Methods has essentially solved the phase problem for well diffracting small molecule crystals. Today, anomalous scattering techniques such as MAD or SAS are the most common techniques used for de novo structure determination of macromolecules. Both techniques require the presence of one or more anomalous scatterers in the crystal.
SIR and SAS Methods 1.Need a heavy atom (lots of electrons) or a anomalous scatterer (large anomalous scattering signal) in the crystal. SIR - heavy atoms usually soaked in. SAS - anomalous scatterers usually engineered in as selenomethional labels. Can also be soaked. 2.SIR collect a native and a derivative data set (2 sets total). SAS collect one highly redundant data set and keep anomalous pairs separate during processing. SAS - may want to choose a scatterer or wavelength that enhances the anomalous signal. 3.Must find the heavy atoms or anomalous scatterers can use Patterson analysis or direct methods. 4.Must resolve the bimodal ambiguity. use solvent flattening or similar technique
Heavy Atom Derivatives Heavy atom derivatives are generally prepared by soaking crystals in dilute (2 - 20 mM) solutions of heavy atom salts (see Table II below for some examples). Crystal cracking is generally a good indication that that heavy atom is interacting with the crystal lattice, and suggests that a good derivative can be obtained by soaking the crystal in a more dilute solution. Once derivative data has been collected, the merging R factor (R merge ) between the native and derivative data sets can be used to check for heavy atom incorporation and isomorphism. R merge values for isomorphous derivatives range from 0.05 to 0.15. Values below 0.05 indicate that there is little heavy atom incorporation. Values above 0.15 indicate a lack of isomorphism between the two crystals. Heavy atom derivatives MUST be isomorphous
Finding the Heavy Atoms or Anomalous Scatterers The Patterson function - a F 2 Fourier transform with = 0 - vector map (u,v,w instead of x,y,z) - maps all inter-atomic vectors - get N 2 vectors!! (where N= number of atoms) The Difference Patterson Map SIR - | F| 2 = |F nat - F der | 2 SAS - | F| 2 = |F hkl - F -h-k-l | 2 Patterson map is centrosymmetric - see peaks at u,v,w & -u, -v, -w Peak height proportional to Z i Z j Peak u,v,w’s give heavy atom x,y,z’s - Harker analysis Origin (0,0,0) maps vector of atom to itself From Glusker, Lewis and Rossi
Harker Analysis Patterson symmetry = Space group symmetry minus translations Example Space group P2 1 P2 1 space group symmetry operators x,y,z -x,1/2+y,-z x,y,z -x,1/2+y,-z x,y,z[(x,y,z) - (x,y,z)][(x,y,z) - (-x,1/2+y,-z)] -x,1/2+y,-z[(-x,1/2+y,-z) – (x,y,z)][(-x,1/2+y,-z) – (-x,1/2+y,-z)] x,y,z -x,1/2+y,-z x,y,z0002x,-1/2, 2z -x,1/2+y,-z-2x, 1/2,-2z000 Harker section v = 1/2 where to look for heavy atom vectors ±2x, 1/2, ±2z Automated programs SOLVE, SHELXD, BNP are available
A Note About Handedness
The Phase Triangle Relationship O N M L OLM = OLN Q F P, F PH, F H and -F H are vectors (have direction) F P <= obtained from native data F PH <= obtained from derivative or anomalous data F H <= obtained from Patterson analysis F PH = F P + F H Need value of F H From Glusker, Lewis and Rossi
The Phase Triangle Relationship O N M L Q In simplest terms, isomorphous replacement finds the orientation of the phase triangle from the orientation of one of its sides. It turns out, however, that there are two possible ways to orient the triangle if we fix the orientation of one of its sides. From Glusker, Lewis and Rossi
Single Isomorphous Replacement X 1 true or false X 2 true or false From Glusker, Lewis and Rossi Note: F P = protein F H = heavy atom F P1 = heavy atom derivative The center of the F P1 circle is placed at the end of the vector - F H1. The situation of two possible SIR phases is called the “phase ambiguity” problem, since we obtain both a true and a false phase for each reflection. Both phase solutions are equally probable, i.e. the phase probability distribution is bimodal.
Resolving the Phase Ambugity X 1 true or false X 2 true or false From Glusker, Lewis and Rossi Note: F P = protein F H = heavy atom F P1 = heavy atom derivative The center of the F P1 circle is placed at the end of the vector - F H1. Add more information: (1)Add another derivative (Multiple Isomorphous Replacement) (2)Use a density modification technique (solvent flattening) (3)Add anomalous data (SIR with anomalous scattering)
Multiple Isomorphous Replacement X true X false X fals Exact overlap at X 1 dependent on data accuracy dependent on HA accuracy called lack of closure From Glusker, Lewis and Rossi Note: F P = protein F H1 = heavy atom #1 F H2 = heavy atom #2 F P1 = heavy atom derivative F P2 = heavy atom derivative The center of the F P1 and F P1 circles are placed at the end of the vector -F H1 and -F H2, respectively. We still get two solutions, one true and one false for each reflection from the second derivative. The true solutions should be consistent between the two derivatives while the false solution should show a random variation.
Solvent Flattening Similar to noise filtering Resolve the SIR or SAS phase ambiguity B.C. Wang, 1985 Electron density can’t be negative Use an iterative process to enhance true phase! From Glusker, Lewis and Rossi
The solvent flattening process was made practical by the introduction of the ISIR/ISAS program suite (Wang, 1985) and other phasing programs such DM and PHASES are based on this approach.
Handedness Can be Determined by Solvent Flattening
Does the Correct Hand Make a Difference? YES! The wrong hand will give the mirror image!
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: f AD = f n + f' + i f” f n is 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 f n f" is an imaginary term which also arises from the AD effect f" is always positive and 90° ahead of (f n + 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, I hkl = I -h-k-l (Firedel’s Law). With AD effects, I hkl ≠ I -h-k-l (Friedel’s Law breaks down). Accurate measurement of Friedel pair differences can be used to extract starting phases if the AD effect is large enough.
Breakdown of Friedel’s Law (F hkl Left) F n represents the total scattering by "normal" atoms without AD effects, f’ represents the sum of the normal and real AD scattering values (f n + f'), f" is the imaginary AD component and appears 90° (at a right angle) ahead of the f’ vector and the total scattering is the vector F +++. (F -h-k-l Right) F -n is the inverse of F n (at - hkl ) and f’ is the inverse of f’, the f" vector is once again 90° ahead of f’. The resultant vector, F --- in this case, is obviously shorter than the F +++ vector. f’
Collecting Anomalous Scattering Data Anomalous scatterers, such as selenium, are generally incorporated into the protein during expression of the protein or are soaked into the crystals in a manner similar to preparing a heavy atom derivative. Bromine, iodine, xeon and traditional heavy atom compounds are also good anomalous scatterers. The anomalous signal, the difference between |F +++ | and |F --- | is generally about one order of magnitude smaller than that between |F PH (hkl)|, and |F P (hkl)|. Thus, the signal-to-noise (S/n) level in the data plays a critical role in the success of anomalous scattering experiments, i.e. the higher the S/n in the data the greater the probability of producing an interpretable electron density map. The anomalous signal can be optimized by data collection at or near the absorption edge of the anomalous scatterer. This requires a tunable X-ray source such as a synchrotron. The S/n of the data can also be increased by collecting redundant data. The two common anomalous scattering experiments are Multiwavelength Anomalous Dispersion (MAD) and single wavelength anomalous scattering/dfiffraction (SAS or SAD) The SAS technique is becoming more popular since it does not require a tunable X-ray source.
Increasing Number of SAS Structures
Increasing S/n with Redundancy
Multiwavelength Anomalous Dispersion From Glusker, Lewis and Rossi Note: F P = protein F H1 = heavy atom F + PH = F +++ F - PH = F --- F + H” = f” +++ F - H” = f” --- The center of the F + PH and F - PH circles are placed at the end of the vector -F + H” and -F - H” respectively. In the MAD experiment a strong anomalous scatterer is introduced into the crystal and data are recorded at several wavelengths (peak, inflection and remote) near the X-ray absorption edge of the anomalous scatterer. The phase ambiguity resolved a manner similar to the use of multiple derivatives in the MIR technique.
Single Wavelength Anomalous Scattering The SAS method, which combines the use of SAS data and solvent flattening to resolve phase ambiguity was first introduced in the ISAS program (Wang, 1985). The technique is very similar to resolving the phase ambiguity in SIR data. The SAS method does not require a tunable source and successful structure determination can be carried out using a home X-ray source on crystals containing anomalous scatterers with sufficiently large f” such as iron, copper, iodine, xenon and many heavy atom salts. The ultimate goal of the SAS method is the use of S-SAS to phase protein data since most proteins contain sulfur. However sulfur has a very weak anomalous scattering signal with f” = 0.56 e - for Cu X-rays. The S-SAS method requires careful data collection and crystals that diffract to 2Å resolution. A high symmetry space group (more internal symmetry equivalents) increases the chance of success. The use of soft X-rays such as Cr K ( = 2.2909Å) X-rays doubles the sulfur signal ( f” = 1.14 e - ). There over 20 S-SAS structures in the Protein Data Bank.
What is the Limit of the SAS Method f” = 0.56e - using Cu K X-rays
Molecular replacement has proven effective for solving macromolecular crystal structures based upon the knowledge of homologous structures. The method is straightforward and reduces the time and effort required for structure determination because there is no need to prepare heavy atom derivatives and collect their data. Model building is also simplified, since little or no chain tracing is required. The 3-dimensional structure of the search model must be very close (< 1.7Å r.m.s.d.) to that of the unknown structure for the technique to work. Sequence homology between the model and unknown protein is helpful but not strictly required. Success has been observed using search models having as low as 17% sequence similarity. Several computer programs such as AmoRe, X-PLOR/CNS PHASER are available for MR calculations. Molecular Replacement
Use a model of the protein to estimate phases Must be a structural homologue (RMSD < 1.7Å) Two step process 1. find orientation of model (red ==> black) 2. find location of orientated model (black ==> blue) px.cryst.bbk.ac.uk/03/sample/molrep.htm
Molecular Replacement Use a model of the protein to estimate phases Need to determine model’s orientation in X 1 s unit cell Use a Patterson rotation search ( The coordinate system is rotated by an angle around the original z axis, then by an angle around the new y axis, and then by an angle around the final z axis. zyz convention
Molecular Replacement Use a model of the protein to estimate phases Need to determine orientated model’s location in X 1 s unit cell Use an R-factor search Orientated model is stepped through the X 1 unit cell using small increments in x, y, and z (eg. x => x+ step) Point where R is lowest represents the correct location Other faster methods are available e.g. PHASER