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Introduction to Single-crystal Diffraction

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Introduction to Single-crystal Diffraction

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  1. This presentation will probably involve audience discussion, which will create action items. Use PowerPoint to keep track of these action items during your presentation • In Slide Show, click on the right mouse button • Select “Meeting Minder” • Select the “Action Items” tab • Type in action items as they come up • Click OK to dismiss this box • This will automatically create an Action Item slide at the end of your presentation with your points entered. Introduction toSingle-crystal Diffraction Biology 555 Andrew J. Howard 11 September 2018

  2. Diffraction: why Resolution Crystallography: how Experiment Formalism Lattice Symmetries Cell matrices Intensity relationships Images and measurements Rotation vs. Laue What we’ll discuss Single-crystal diffraction I

  3. Determining 3-D structures • We want to know the structures of macromolecules because we can understand function on the basis of structure • If we already know what the function is, we use the structure to figure out how it works • If we don’t know the function, we sometimes can use the structure to figure out what the function is. Single-crystal diffraction I

  4. How do we do this? • If we already know something about structure, we can use a variety of techniques (e.g. light scattering, X-ray absorption, EPR , fiber diffraction) to answer specific structural questions • If we don’t know anything: • Low resolution (details > 3Å):cryoEM, CD, SAXS, SANS • High resolution (details < 3Å) • single-crystal diffraction • multidimensional NMR Single-crystal diffraction I

  5. What does resolution mean? • In general it refers to the distance associated with the smallest detail discernible from a particular experiment or approach • Specific significance depends on the technique involved • In crystallography it’s related to the widest angle of diffraction measured, via Bragg’s law Single-crystal diffraction I

  6. Crystallography Determine 3-D structure by: • Making a well-ordered 3-D crystal • Identifying Bragg diffraction spots • Measuring their intensities • Correcting for systematic errors • Getting phase angles experimentally or by indirect reasoning • Calculating electron density by Fourier techniques • Relating electron density to atomic positions Single-crystal diffraction I

  7. Crystal growth • We’ll discuss this in detailTuesday • Recognize at the outset that protein crystals are artificial constructs: very few proteins naturally form 3-D ordered arrays • But there are systematic ways to induce crystallization Single-crystal diffraction I

  8. What does 3-D order do? • Briefly, we say that the 3-D order collapses what would otherwise be a fuzzy scattering pattern into a series of discrete spots • Each spot has 3 integer indices that characterize it (Why? 3 dimensions) • If we can identify each spot (determine the 3 integers) and measure the intensity of it, we have the Fourier amplitudes needed in the transform. Single-crystal diffraction I

  9. How does the experiment work? • Last time we showed a simple-minded derivation of Bragg’s law based on planes of diffracting objects • This is an oversimplificationbut it yields nl = 2Dsinq • n = integer order of plane • l = incoming X-ray wavelength • D = spacing between planes • q = angle between diffracting plane and incoming or outgoing beam direction Single-crystal diffraction I

  10. Bragg’s law cartoon Image courtesy Mineral Physics Institute, SUNY Stonybrook Single-crystal diffraction I

  11. Typical diffraction image • Obtained with monochromatic X-rays and with the crystal approximately stationary • This doesn’ttell the whole story of crystal diffraction, but it’s a start. Single-crystal diffraction I

  12. How would a small-molecule crystallographer react to that? • Too many spots! • In a typical small-molecule experiment with the crystal stationary, the Laue conditions are only satisfied for a very few Bragg spots—maybe 3. • So the small-molecule person would be impressed that hundreds of spots are visible in a still image Single-crystal diffraction I

  13. Laue conditions for Bragg diffraction spots Laue condition for 3-D crystals tells us: • Bragg diffraction occurs in discrete angular directions (rays  spots) • Each spot can be identified with three integer indices (h,k,l), e.g. (-6,11,-4) • For a given sample orientation, Laue condition is only satisfied for a few index values Single-crystal diffraction I

  14. 3-space vectors • Get used to thinking about ordered triples of numbers as vectors • That’s natural with things like diffraction vectors, since they exist in a three-space • But we can even treat a triple of reflection indices (h,k,l) as a vector h. • Convention: boldface lowercase letters (e.g. s, k, h) denote vectors; boldface capital letters (e.g. A, R) denote square matrices Single-crystal diffraction I

  15. What will we use this for? • We’re shooting electromagnetic waves exp(2pik0•x) at a sample • Scatter with amplitude exp(2pik•x) • Difference=exp(2pis•x) for s = k - k0 • I ~ |F|2 = [Sx f(x) exp(i(k•x-k0•x))]2 -k0 k s = k-k0 k k0 Single-crystal diffraction I

  16. Using these structure factors to determine a structure • We need all of these structure factors to determine electron densities: • r(r) = ShklFhkl exp(-2pi(s•r)) • Thus the electron density is the inverse Fourier transform of the structure factors • This is a triple sum over the three integer indices h = (h,k,l) • In principle it extends from -∞ to ∞ in all three indices; in practice it covers a narrower range Single-crystal diffraction I

  17. Relating s to h • The diffraction vector s is related to the index vector h in a simple way: • s = lA•hwhere A is a 3x3 matrix describing the reciprocal-space unit cell associated with the real sample • This is a concept we’ll revisit later Single-crystal diffraction I

  18. Relating h to s • A more intuitive description: • h = R•s / lwhere the index vector h(e.g. (6,-11,4)) is related to the diffraction vector s via a 3x3 matrix R describing the real-space unit cell • Columns of R = unit cell lengths a, b, c • Dot products between columns yield the unit cell angles a, b, g • Note that R = A-1 Single-crystal diffraction I

  19. Sample symmetry and R • The rotational symmetry of the unit cell gives rise to specific properties of the unit cell matrix R • If a=g=90º,b ≠90º, it’s monoclinic • a=b=g=90º, lengths unrestricted:orthorhombic • a=b=g=90º, a=b: tetragonal • a=b=90º, g=120º, a=b: hexagonal or trigonal • a=b=c, a=b=g: rhombohedral • a=b=c, a=b=gº: cubic • Those are the only possibilities, apart from redefinitions of what we mean by a, b, c. Single-crystal diffraction I

  20. Crystal systems I,II www.dkimages.com • Triclinica ≠ b ≠ c ≠ ≠ ≠90º • Monoclinica ≠ b ≠ c =  = 90º ≠ 90º Single-crystal diffraction I

  21. Crystal Systems III, IV • Orthorhombica ≠ b ≠ c =  =  = 90º • Tetragonala = b ≠c =  =  = 90º Single-crystal diffraction I

  22. Crystal systems V, VI • Cubica = b = c =  =  = 90º • Hexagonala = b ≠c =  = 90º = 120º Single-crystal diffraction I

  23. Crystal System 7 • Rhombohedrala = b = c =  =  ≠ 90º Single-crystal diffraction I

  24. Crystal systems and symmetries • Crystals must have 3-D translational order or they aren’t crystals • They may have rotational symmetries within the unit cell • The crystal systems are specifically associated with those symmetries Single-crystal diffraction I

  25. Kinds of symmetries • Rotations:2-fold, 3-fold,4-fold, 6-fold • Screw axes: rotation combined with a fractional translation • 2-fold: half a unit cell • 3-fold: 1/3 or 2/3 (=-1/3) • 4-fold: 1/4, 1/2, or 3/4 (=-1/4) • 6-fold: 1/6, 1/3, 1/2, 2/3 (-1/3), 5/6 (=-1/3) Single-crystal diffraction I

  26. Other symmetries • Centers of symmetry: r -r • Mirrors: you can figure that out; A mirror through Y maps(x, y, z) into (x, -y, z) • Glide planes: center of symmetry combined with translation Single-crystal diffraction I

  27. Specific symmetries • Triclinic: none • Monoclinic: twofold axis* about b • Orthorhombic: twofold axis*about a, b, c • Tetragonal: fourfold axis* about c • Cubic: threefold axis down body diagonal; twofold axis* perpendicular • Hexagonal: threefold* or sixfold axis* about c * can be screw or glide plane as well Single-crystal diffraction I

  28. Additional symmetries • Tetragonal:Sometimes twofolds perpendicular to the fourfold axis of symmetry • Trigonal:Twofold perpendicular to threefoldeither of two positions • Hexagonal:twofold perpendicular to sixfold • Cubic:fourfold perpendicular to 3 and 2 Single-crystal diffraction I

  29. A consequence of chirality • Recognize that almost all biopolymers are chiral • That means that they cannot be identical to their mirror images • Therefore they can’t crystallize in centrosymmetric spacegroups, i.e. with symmetries that involve • Centers of symmetry (x,y,z)  (-x,-y,-z) • Mirror planes (x,y,z)  (x,-y,z) • Glide planes (trust me on this one) Single-crystal diffraction I

  30. Is there a way around that? • Yes, if you’re dedicated enough. • Suppose you have a 105-aa protein for which the phase problem (see later…) can’t be solved. • Synthesize your L-amino-acid protein using ribosomal synthesis and also synthesize a D-amino acid version with nonbiological chemistry • Combine the L and D versions (1:1 ratio) • Crystallize the resulting racemic mixture • If you’re lucky, it’ll crystallize in spacegroup P-1,so that the D protein and the L protein are at (x,y,z) and (-x,-y,-z): that then simplifies solving the phase problem! Single-crystal diffraction I

  31. A simple R matrix • ( asinb 0 a cosb )R = ( 0 b 0 ) ( 00 c ) • Monoclinic, b along Y, c along Z • Unit cell volume = detR = abcsinb • As we rotate the crystal about X this matrix will be left-multiplied by a rotation matrix Single-crystal diffraction I

  32. Rotated R matrix • The rotation matrix associated with a rotation W about X is( 1 0 0 )Q = ( 0 cosWsinW ) ( 0 -sinWcosW) • Thus R’ = QR =( asinb 0 acosb ) ( 0 bcosWc sinW ) ( 0 -bsinWc cosW) Single-crystal diffraction I

  33. Realities of crystal symmetry • It occasionally happens that relationships in R that look like higher symmetries are not reflected in the underlying rotational symmetry • You can rely on relationships among intensities to sort that out. • These relationships among intensities are critical for merging data even without accidental correspondences. Single-crystal diffraction I

  34. Intensity relationships • All unit cells: I(h,k,l) = I(-h,-k,-l)unless anomalous diffraction present (Friedel’s law) • Monoclinic: I(h,k,l) = I(-h,k,-l) • Orthorhombic:I(h,k,l) = I(h,-k,-l) = I(-h,k,-l)= I(-h,-k,l) • Tetragonal:I(h,k,l) = I(-k,h,l) = I(-h,-k,l)= I(k,-h,l) Single-crystal diffraction I

  35. Intensity relationships, cont’d • Tetragonal with twofolds:All symmetry elements from orthorhombic and tetragonals • Cubic:I(h,k,l) = I(k,l,h) = I(l,h,k)plus orthorhombic relations • Cubic with fourfolds:As above, plus tetragonals • Hexagonal/ Trigonal:I(h,k,l) = I(k,i,l) = I(i,h,l)fori = -h-k Single-crystal diffraction I

  36. Intensity relations, concluded • Trigonal with twofold (“312”):I(h,k,l) = I(k,i,l) = I(i,h,l)=I(-k,-h,-l) = I(-i,-k,-l) = I(-h,-i,-l) • Trigonal with twofold (“321”):I(h,k,l) = I(k,i,l) = I(i,h,l)=I(k,h,-l) = I(i,k,-l) = I(h,i,-l) • Hexagonal:I(h,k,l) = I(k,i,l) = I(i,h,l)=I(-h,-k,l) = I(-k,-i,l) = I(-i,-h,l) • Hexagonal with twofolds:as above plus those also equalI(-k,-h,-l) = I(-i,-k,-l) = I(-h,-i,-l)=I(k,h,-l) = I(i,k,-l) = I(h,i,-l) Single-crystal diffraction I

  37. A single monochromatic shot won’t tell us about all the spots • Since the Laue condition is only satisfied for a tiny fraction of the total list of spots at any given sample position, to measure all the spots we need many different sample positions or many different wavelengths • Many positions: rotate the sample • Many wavelengths: polychromatic diffraction Single-crystal diffraction I

  38. Which is better? They both have their uses • Polychromatic (“Laue”) takes advantage of inherently polychromatic incoming radiation • Rotation is easier to understand what the individual spots mean • Quality of data is often higher with rotation data: see next slide Single-crystal diffraction I

  39. Typical rotation image (-11,-15,0)reflection 2sec expos. SER-CAT 22-BM beamline Single-crystal diffraction I

  40. Simulated Polychromatic Image Courtesy Renz Research, Inc. Single-crystal diffraction I

  41. Why is rotation data often of higher quality? • Individual atomic scattering amplitudes f are themselves wavelength-dependent; that dependence scales away if l constant or close to constant • Detector response is wavelength dependent • Background scatter is often higher with Laue Single-crystal diffraction I

  42. Rotation vs. Laue, concluded • Sometimes spots overlap harmonically in Laue; that problem doesn’t occur in monochromatic experiments • Spatial overlaps (even without harmonic overlaps) are worse in Laue • With conventional sources, we can’t really get much intensity from Bremsstrahlung, so we’re stuck Single-crystal diffraction I

  43. Special use of Laue • The phenomenally high fluence achievable with Laue means that one can obtain a complete diffraction pattern in microseconds or even nanoseconds of exposure • If you only need one pattern to determine the structure (which is only occasionally true!) this enables you to determine a structure in a single shot • This allows for true time-resolved crystallography Single-crystal diffraction I

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