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PowerPoint File available:. http://bl831.als.lbl.gov/ ~jamesh/powerpoint/ ACA_SINBAD_2013.ppt. Acknowledgements. Ken Frankel Alastair MacDowell John Spence Howard Padmore LBNL Laboratory Directed Research & Development (LDRD) ALS 8.3.1 creator: Tom Alber PRT head: Jamie Cate - PowerPoint PPT Presentation
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PowerPoint File available: http:// bl831.als.lbl.gov/ ~jamesh/powerpoint/ ACA_SINBAD_2013.ppt
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Page 1: PowerPoint File available:

PowerPoint File available:

http://bl831.als.lbl.gov/

~jamesh/powerpoint/

ACA_SINBAD_2013.ppt

Page 2: PowerPoint File available:

AcknowledgementsKen Frankel Alastair MacDowell

John Spence Howard PadmoreLBNL Laboratory Directed Research & Development (LDRD)

ALS 8.3.1 creator: Tom Alber PRT head: Jamie Cate

Center for Structure of Membrane ProteinsMembrane Protein Expression Center II

Center for HIV Accessory and Regulatory Complexes

W. M. Keck FoundationPlexxikon, Inc.

M D Anderson CRCUniversity of California Berkeley

University of California San FranciscoNational Science Foundation

University of California Campus-Laboratory Collaboration GrantHenry Wheeler

The Advanced Light Source is supported by the Director, Office of Science, Office of Basic Energy Sciences, Materials Sciences Division, of the US Department of Energy under contract No. DE-AC02-05CH11231 at Lawrence Berkeley National Laboratory.

Page 3: PowerPoint File available:

Simultaneous

INverse

Beam

Anomalous

Diffraction

Page 4: PowerPoint File available:

SINBAD diffractometer concept

Nucleus

Synthetic light collecting structureh,k,l

-h,-k,-l

Detec

tor Detector

Detec

tor Detector

d = 3.5 Å d = 3.5 Å

d = 3.5 Åd = 3.5 Å

sample injector

Mirr

ors

Mirr

ors

d = 3.5 Åλ = 5 Å

XFEL beam

Page 5: PowerPoint File available:

Why SINBAD?

I+ I-

Different crystal volumes

New source of error in SFX

Page 6: PowerPoint File available:

Why SINBAD?

I+ I-

Different crystal orientations

New source of error in SFX

Page 7: PowerPoint File available:

Why SINBAD?

I+ I-

Different beam intensities

New source of error in SFX

Page 8: PowerPoint File available:

Why SINBAD?

I+ I-

Different crystal positions

New source of error in SFX

Page 9: PowerPoint File available:

Why SINBAD?

I+ I-

Different structures (non-isomorphism)

New source of error in SFX

Page 10: PowerPoint File available:

Dynamic range

Why SINBAD?

I+ I-

New source of error in SFX

Page 11: PowerPoint File available:

Why SINBAD?

I+ I-

New source of error in SFX

Problem:How to get I+ and I-both on Ewald sphereat the same time?

ΔIano

Page 12: PowerPoint File available:

Ewald sphere 2

diffracted ra

y

λ*

λ*

θ

1Ewald sphere

λ*

(h,k,l)

diffracted ra

yλ*

θ

d*

Osculating Ewald Spheres

(-h,-k,-l)

d*

Page 13: PowerPoint File available:

SINBAD diffractometer concept

Nucleus

Synthetic light collecting structureh,k,l

-h,-k,-l

Detec

tor Detector

Detec

tor Detector

d = 3.5 Å d = 3.5 Å

d = 3.5 Åd = 3.5 Å

sample injector

Mirr

ors

Mirr

ors

d = 3.5 Åλ = 5 Å

XFEL beam

Page 14: PowerPoint File available:

Tolerances:

Time: ~10% of 100 fs

Distance: 3 μm

Angle: ~1% of mosaicity~100 μRad

Page 15: PowerPoint File available:

Can’t we just use scaling?

Ispot ≈ |F(hkl)|2

Page 16: PowerPoint File available:

Darwin’s Formula

I(hkl) - photons/spot (fully-recorded)

Ibeam - incident (photons/s/m2 )

re - classical electron radius (2.818x10-15 m)

Vxtal - volume of crystal (in m3)

Vcell - volume of unit cell (in m3)

λ - x-ray wavelength (in meters!)

ω - rotation speed (radians/s)

L - Lorentz factor (speed/speed)

P - polarization factor

(1+cos2(2θ) -Pfac∙cos(2Φ)sin2(2θ))/2

A - attenuation factor

exp(-μxtal∙lpath)

F(hkl) - structure amplitude (electrons)

C. G. Darwin (1914)

P A | F(hkl) |2I(hkl) = Ibeam re2

Vxtal

Vcell

λ3 LωVcell

Page 17: PowerPoint File available:

Darwin’s Formula

I(hkl) - photons/spot (fully-recorded)

Ibeam - incident (photons/s/m2 )

re - classical electron radius (2.818x10-15 m)

Vxtal - volume of crystal (in m3)

Vcell - volume of unit cell (in m3)

λ - x-ray wavelength (in meters!)

ω - rotation speed (radians/s)

L - Lorentz factor (speed/speed)

P - polarization factor

(1+cos2(2θ) -Pfac∙cos(2Φ)sin2(2θ))/2

A - attenuation factor

exp(-μxtal∙lpath)

F(hkl) - structure amplitude (electrons)

C. G. Darwin (1914)

P A | F(hkl) |2I(hkl) = Ibeam re2

Vxtal

Vcell

λ3 LωVcell

Page 18: PowerPoint File available:

Darwin’s Formula

I(hkl) - photons/spot (fully-recorded)

Ibeam - incident (photons/s/m2 )

re - classical electron radius (2.818x10-15 m)

Vxtal - volume of crystal (in m3)

Vcell - volume of unit cell (in m3)

λ - x-ray wavelength (in meters!)

ω - rotation speed (radians/s)

L - Lorentz factor (speed/speed)

P - polarization factor

(1+cos2(2θ) -Pfac∙cos(2Φ)sin2(2θ))/2

A - attenuation factor

exp(-μxtal∙lpath)

F(hkl) - structure amplitude (electrons)

C. G. Darwin (1914)

P A | F(hkl) |2I(hkl) = Ibeam re2

Vxtal

Vcell

λ3 LωVcell

Page 19: PowerPoint File available:

Greenhough-Helliwell Formula

ΔΦ - reflecting range (radians)

2η - mosaic spread (radians)

L - Lorentz factor (speed/speed)

θ - Bragg angle

λ - x-ray wavelength

Δλ - wavelength spread

γHV - horizontal and vertical

beam divergence (radians)

Greenhough & Helliwell (1983)

ΔΦ = L sin2θ (2η + Δλ/λ tanθ)

+ ((L2sin22θ - 1)γH2 + γV

2)1/2

Page 20: PowerPoint File available:

Greenhough-Helliwell Formula

ΔΦ - reflecting range (radians)

2η - mosaic spread (radians)

L - Lorentz factor (speed/speed)

θ - Bragg angle

λ - x-ray wavelength

Δλ - wavelength spread

γHV - horizontal and vertical

beam divergence (radians)

Greenhough & Helliwell (1983)

ΔΦ = L sin2θ (2η + Δλ/λ tanθ)

+ ((L2sin22θ - 1)γH2 + γV

2)1/2

Page 21: PowerPoint File available:

Lorentz Factor

Ewald sphere

spin

dle

axi

s

diffracted ra

y

Page 22: PowerPoint File available:

Darwin’s Formula

I(hkl) - photons/spot (fully-recorded)

Ibeam - incident (photons/s/m2 )

re - classical electron radius (2.818x10-15 m)

Vxtal - volume of crystal (in m3)

Vcell - volume of unit cell (in m3)

λ - x-ray wavelength (in meters!)

ω - rotation speed (radians/s)

L - Lorentz factor (speed/speed)

P - polarization factor

(1+cos2(2θ) -Pfac∙cos(2Φ)sin2(2θ))/2

A - attenuation factor

exp(-μxtal∙lpath)

F(hkl) - structure amplitude (electrons)

C. G. Darwin (1914)

P A | F(hkl) |2I(hkl) = Ibeam re2

Vxtal

Vcell

λ3 LωVcell

Page 23: PowerPoint File available:

Integral under curve

-0.1

0.1

0.3

0.5

0.7

0.9

-2 -1.5 -1 -0.5 0 0.5 1 1.5 2

inte

nsity

“Full” Spot

Page 24: PowerPoint File available:

Integral under curve

-0.1

0.1

0.3

0.5

0.7

0.9

-2 -1.5 -1 -0.5 0 0.5 1 1.5 2

inte

nsity

Spot on “Still”

Page 25: PowerPoint File available:

What is "partiality"?

100%

Page 26: PowerPoint File available:

What is "partiality"?

50%

Page 27: PowerPoint File available:

What is "partiality"?

50%

Page 28: PowerPoint File available:

What is "partiality"?

90%

Page 29: PowerPoint File available:

What is "partiality"?

15%

Page 30: PowerPoint File available:

What is "partiality"?

1%

Page 31: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

Page 32: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

Page 33: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

Page 34: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

Page 35: PowerPoint File available:

What is "partiality"?

100% !

Page 36: PowerPoint File available:

What is "partiality"?

90%

Page 37: PowerPoint File available:

What is "partiality"?

80%

Page 38: PowerPoint File available:

What is "partiality"?

50%

Page 39: PowerPoint File available:

What is "partiality"?

20%

Page 40: PowerPoint File available:

Bra

gg, Ja

mes

& B

osa

nquet

(19

21

). P

hilo

s. M

ag. Ser.

6, 4

1, 3

09

–3

37

.

Page 41: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

F(0,0,0)

Partiality is always 100% !

Page 42: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

F(0,0,0)

Partiality is always 100% !

Page 43: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

F(0,0,0)

Partiality is always 100% !

Page 44: PowerPoint File available:

What is “partiality”?

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

F(0,0,0)

Partiality is always 100% !

Page 45: PowerPoint File available:

Why SINBAD?

I+ I-

Different crystal orientations

New source of error in SFX

Page 46: PowerPoint File available:

F(h,k,l)

Ewald sphere

spectral dispersion

λ1*

λ2*

F(0,0,0)

100%

~90%

Page 47: PowerPoint File available:

F(h,k,l)

Ewald sphere

spectral dispersion

λ1*

λ2*

F(0,0,0)

100%

~45%

Page 48: PowerPoint File available:

Ewald sphere

spectral dispersion

λ1*

λ2*

F(0,0,0)

F(h,k,l)

100%

0%

Page 49: PowerPoint File available:

F(h,k,l)

F(0,0,0)

beam divergence

Ewald sphere

diffracted ra

yd*

λ*

λ*

Page 50: PowerPoint File available:

beam divergence

Ewald sphere

λ*

λ*

F(0,0,0)

d*

diffra

cted

ray

Page 51: PowerPoint File available:

Ewald’s “mosaic” picture

Page 52: PowerPoint File available:

F(0,0,0)

mosaic spread

Ewald sphere

diffracted ra

y

λ*

λ* d*

d*

F(h,k,l)

Page 53: PowerPoint File available:

F(0,0,0)

Ewald sphere

diffracted ra

y

λ*

λ*

d*

F(h,k,l)

mosaic spread

Page 54: PowerPoint File available:

F(0,0,0)

mosaic spread

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

Page 55: PowerPoint File available:

F(0,0,0)

Ewald sphere

diffracted ra

y

λ*

λ* d*

F(h,k,l)

mosaic spread

Page 56: PowerPoint File available:

F(0,0,0)

mosaic spread

Ewald sphere

diffracted ra

y

λ*

λ* d*

d*

F(h,k,l)

Page 57: PowerPoint File available:

F(0,0,0)

mosaic spread

Ewald sphere

λ*

d*

F(h,k,l)

Page 58: PowerPoint File available:

F(0,0,0)

mosaic spread

Ewald sphere

diffracted ra

yd*

λ*

λ*

F(h,k,l)

Page 59: PowerPoint File available:

F(0,0,0)

mosaic spread

Ewald sphere

λ*

d*

F(h,k,l)

Page 60: PowerPoint File available:

mosaic spread = 0 º

Page 61: PowerPoint File available:

mosaic spread = 0.1º

Page 62: PowerPoint File available:

mosaic spread = 0.2º

Page 63: PowerPoint File available:

mosaic spread = 0.4º

Page 64: PowerPoint File available:

mosaic spread = 0.6º

Page 65: PowerPoint File available:

mosaic spread = 0.8º

Page 66: PowerPoint File available:

mosaic spread = 1.0º

Page 67: PowerPoint File available:

mosaic spread = 1.5º

Page 68: PowerPoint File available:

mosaic spread = 2.0º

Page 69: PowerPoint File available:

mosaic spread = 2.5º

Page 70: PowerPoint File available:

mosaic spread = 3.2º

Page 71: PowerPoint File available:

mosaic spread = 6.4º

Page 72: PowerPoint File available:

mosaic spread = 12.8º

Page 73: PowerPoint File available:

Ewald’s “mosaic” picture

What isthis stuff?

Page 74: PowerPoint File available:

Darwin’s original picture

Page 75: PowerPoint File available:

“mosaicity” with visible light

Page 76: PowerPoint File available:

10 atoms 0.1 μm

Scattering: line of atoms

50 atoms 0.5 μm100 atoms 1 μm200 atoms 2 μm300 atoms 3 μm400 atoms 4 μm500 atoms 5 μm1000 atoms 10 μm

position on detector (mm)

inte

nsity

(ph

oton

s/S

R/a

tom

)

Page 77: PowerPoint File available:

Scattering: line of atomspe

ak in

tens

ity (

phot

ons/

SR

)

number of atoms in line

“coherence length”

•depends on detector distance !!!•integrated intensity never changes•peak intensity depends on size

Page 78: PowerPoint File available:

10 atoms 0.1 μm

Integral under curve

50 atoms 0.5 μm100 atoms 1 μm200 atoms 2 μm300 atoms 3 μm400 atoms 4 μm500 atoms 5 μm

position on detector (mm)

inte

nsity

(ph

oton

s/S

R/a

tom

)

Spot Intensity

Page 79: PowerPoint File available:

Can’t we just rotate the crystal?

1 μm

100 fs= 90 km/s

9 nm

17.26 km/s (90 km/s)2

0.5 μm= 1.5 x 1015 G = 0.5 nN

Page 80: PowerPoint File available:

Can’t we just rotate the crystal?

NO

Why do we want to rotate the crystal?

Page 81: PowerPoint File available:

The “nanocrystal advantage”

Ispot = k Ncells

Ewald sphererange

2

Page 82: PowerPoint File available:

Fraunhofer Formula

Ipixel - photons/pixel/s

Ibeam - incident (photons/s/m2 )

re - classical electron radius (2.818x10-15 m)

hkl - index of pixel (a·(up+us)/λ)

a - orientation (recip. cell vectors)

up,us - unit vector pointing at pixel,source

λ - x-ray wavelength (in meters!)

N - number of cells (each direction)

Ω - solid angle of pixel (steradian)

P - polarization factor

(1+cos2(2θ) -Pfac∙cos(2Φ)sin2(2θ))/2

A - attenuation factor exp(-μxtal∙lpath)

F(hkl) - structure amplitude (electrons)

Circa 1820s

see: Kirian et al. (2010)

P A | F(hkl) |2sin(πN·hkl)

sin(π·hkl)Ipixel = Ibeam re

2 Ω2

Page 83: PowerPoint File available:

Scattering: atom by atom

0

0.5

1

1.5

2

2.5

3

3.5

4

4.5

0 0.5 1 1.5 2

one

two

h index

inte

nsity

Page 84: PowerPoint File available:

Scattering: atom by atom

0123456789

10

0 0.5 1 1.5 2

one

two

three

h index

inte

nsity

Page 85: PowerPoint File available:

Scattering: atom by atom

0

2

4

6

8

10

12

14

16

18

0 0.5 1 1.5 2

two

three

four

h index

inte

nsity

Page 86: PowerPoint File available:

Scattering: atom by atom

0

5

10

15

20

25

30

0 0.5 1 1.5 2

three

four

five

h index

inte

nsity

Page 87: PowerPoint File available:

Scattering: atom by atom

0

5

10

15

20

25

30

35

40

0 0.5 1 1.5 2

four

five

six

h index

inte

nsity

Page 88: PowerPoint File available:

Scattering: atom by atom

0

10

20

30

40

50

60

0 0.5 1 1.5 2

five

six

seven

h index

inte

nsity

Page 89: PowerPoint File available:

Scattering: atom by atom

0

10

20

30

40

50

60

70

0 0.5 1 1.5 2

six

seven

eight

h index

inte

nsity

Page 90: PowerPoint File available:

Scattering: atom by atom

0

10

20

30

40

50

60

70

80

90

0 0.5 1 1.5 2

seven

eight

nine

h index

inte

nsity

Page 91: PowerPoint File available:

Inter-Bragg spots over-sample unit cell

Page 92: PowerPoint File available:

square

Page 93: PowerPoint File available:

round

Page 94: PowerPoint File available:

Why SINBAD?

I+ I-

Different structures (non-isomorphism)

New source of error in SFX

Page 95: PowerPoint File available:

Dear James

The story of the two forms of lysozyme crystals goes back to about 1964 when it was found that the diffraction patterns from different crystals could be placed in one of two classes depending on their intensities. This discovery was a big set back at the time and I can remember a lecture title being changed from the 'The structure of lysozyme' to 'The structure of lysozyme two steps forward and one step back'. Thereafter the crystals were screened based on intensities of the (11,11,l) rows to distinguish them (e.g. 11,11,4 > 11,11,5 in one form and vice versa in another). Data were collected only for those that fulfilled the Type II criteria. (These reflections were easy to measure on the linear diffractometer because crystals were mounted to rotate about the diagonal axis). As I recall both Type I and Type II could be found in the same crystallisation batch . Although sometimes the external morphology allowed recognition this was not infallible.

The structure was based on Type II crystals. Later a graduate student Helen Handoll examined Type I. The work, which was in the early days and before refinement programmes, seemed to suggest that the differences lay in the arrangement of water or chloride molecules (Lysozyme was crystallised from NaCl). But the work was never written up. Keith Wilson at one stage was following this up as lysozyme was being used to test data collection strategies but I do not know the outcome.

An account of this is given in International Table Volume F (Rossmann and Arnold edited 2001) p760.

Tony North was much involved in sorting this out and if you wanted more info he would be the person to contact. I hope this is helpful. Do let me know if you need more.

Best wishes

Louise

Non-isomorphism in lysozyme

Page 96: PowerPoint File available:

0

100

200

300

400

500

600

700

800

900

0 1 2 3

F(11,11,4)

F(11,11,5)

Johnson’s ratio

Str

uct

ure

fac

tor

(e- )

Non-isomorphism in lysozyme

Page 97: PowerPoint File available:

0

100

200

300

400

500

600

700

800

900

0 1 2 3

F(11,11,4)

F(11,11,5)

Johnson’s ratio

Str

uct

ure

fac

tor

(e- )

Non-isomorphism in lysozyme

Page 98: PowerPoint File available:
Page 99: PowerPoint File available:

RH 84.2% vs 71.9% Riso = 44.5%RMSD = 0.18 Å

Non-isomorphism in lysozyme

Page 100: PowerPoint File available:

Dear James

The story of the two forms of lysozyme crystals goes back to about 1964 when it was found that the diffraction patterns from different crystals could be placed in one of two classes depending on their intensities. This discovery was a big set back at the time and I can remember a lecture title being changed from the 'The structure of lysozyme' to 'The structure of lysozyme two steps forward and one step back'. Thereafter the crystals were screened based on intensities of the (11,11,l) rows to distinguish them (e.g. 11,11,4 > 11,11,5 in one form and vice versa in another). Data were collected only for those that fulfilled the Type II criteria. (These reflections were easy to measure on the linear diffractometer because crystals were mounted to rotate about the diagonal axis). As I recall both Type I and Type II could be found in the same crystallisation batch . Although sometimes the external morphology allowed recognition this was not infallible.

The structure was based on Type II crystals. Later a graduate student Helen Handoll examined Type I. The work, which was in the early days and before refinement programmes, seemed to suggest that the differences lay in the arrangement of water or chloride molecules (Lysozyme was crystallised from NaCl). But the work was never written up. Keith Wilson at one stage was following this up as lysozyme was being used to test data collection strategies but I do not know the outcome.

An account of this is given in International Table Volume F (Rossmann and Arnold edited 2001) p760.

Tony North was much involved in sorting this out and if you wanted more info he would be the person to contact. I hope this is helpful. Do let me know if you need more.

Best wishes

Louise

Non-isomorphism in lysozyme

Page 101: PowerPoint File available:

Non-isomorphism = dehydration?

= 1 nL

100 μm

Page 102: PowerPoint File available:

Anomalous difference is resilient to non-isomorphism

Nucleus

Synthetic light collecting structure

0 20 40 60 80 100

Riso (%)

1.0

0.8

0.6

0.4

0.2

Co

rrel

atio

n C

oef

fici

ent

of

ΔF

ano 100 x 100

lysozyme PDBs

Page 103: PowerPoint File available:

Why SINBAD?

New sources of error in SFX:

1.Partiality

2.Dynamic range

3.Jitter

4.Non-isomorphism

?

Page 104: PowerPoint File available:

SINBAD diffractometer concept

Nucleus

Synthetic light collecting structureh,k,l

-h,-k,-l

Detec

tor Detector

Detec

tor Detector

d = 3.5 Å d = 3.5 Å

d = 3.5 Åd = 3.5 Å

sample injector

Mirr

ors

Mirr

ors

d = 3.5 Åλ = 5 Å

XFEL beam

Page 105: PowerPoint File available:

h,k,l

-h,-k,-l

Detec

tor Detector

Detec

tor Detectorλ = 5 Å

sample

injector

Si(111)

52.87degSi(111)Si(111)

Si(111)

Si(111)

Si(111)

2 Multilayer mirrorsd=2nm, W/B4C

KB Horiz focusKB vertical focus

~ 1m

Page 106: PowerPoint File available:

How to reflect x-rays at 90° ?

λ = 2 d sinθSilicon: absorbs ~50%/bounce

Diamond:Unit cell too small

Platinum:Too soft = high mosaic

Iridium: high hardnessCsI: just miss edge

d = 0.7 λ

Want:Large structure factorLow absorbance

Most promising:

Page 107: PowerPoint File available:

Summaryhttp://bl831.als.lbl.gov/~jamesh/powerpoint/ACA_SINBAD_2013.ppt

• SFX introduces new sources of error

• Software solutions are tractable, but hard

• SINBAD could solve them “in hardware”

• Non-isomorphism can be controlled?

• Mono xtal has applications for seeding

Page 108: PowerPoint File available:

Muybridge’s galloping horse (1878)

Page 109: PowerPoint File available:

Muybridge’s multi-camera

Page 110: PowerPoint File available:

Hot questions: 21st centuryhow do molecules work?

Beernink, Endrizzi, Alber & Schachman (1999). PNAS USA 96, 5388-5393.

Page 111: PowerPoint File available:

a “crystal” of horses

Page 112: PowerPoint File available:

realistic “crystal” of horses

Page 113: PowerPoint File available:

average structure: galloping horse

Page 114: PowerPoint File available:

not enough signal

Page 115: PowerPoint File available:

brighter light

Page 116: PowerPoint File available:

even brighter

Page 117: PowerPoint File available:

very bright light

Page 118: PowerPoint File available:

average structure: galloping horse

Page 119: PowerPoint File available:

Horse: real and reciprocal

Page 120: PowerPoint File available:

Supporting a model with data

Page 121: PowerPoint File available:

Molecular Dynamics Simulation

1aho Scorpion toxin

0.96 Å resolution64 residuesSolvent: H20 + acetate

Cerutti et al. (2010).J. Phys. Chem. B 114, 12811-12824.

using realcrystal’s lattice

Page 122: PowerPoint File available:

30 conformers from 24,000

Page 123: PowerPoint File available:

Electron density from 24,000 conformers

Page 124: PowerPoint File available:

Regular model with real data!

Page 125: PowerPoint File available:

Molecular Dynamics vs Observation

Fobs

1aho.cif 1aho.pdb

Fsim FcalcFcalc

Rcryst= 0.137 Rcryst= 0.116Rvault = 0.69

refined_vs_Fsim.pdb

LSQ rmsd = 0.43Å

rmsd = 1.05 Å

1aho 64-residue scorpion toxin in water to 1.0 Å resolution

Rvault = 0.48 to 4 Å

Riso =

Page 126: PowerPoint File available:

Molecular Dynamics vs Observation

RMSD1.05 Å

Page 127: PowerPoint File available:

Molecular Dynamics vs Observation

RMSD0.45 Åaligned


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