predicting local geometric properties of dna from ...arbogast/cam397/gonzalez1.pdf · introduction...
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Introduction Geometric model Diffusion model Numerical method Preliminary results
Predicting local geometric properties of DNAfrom hydrodynamic diffusion data
O. Gonzalez and J. Li
UT-Austin
27 October 2008
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Introduction
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Goal
To obtain improved estimates of the material parameters thatdescribe sequence-dependent shape of DNA.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Approach
Refine parameters through hydrodynamic diffusion modeling.
GGTAATGCTTAACACCTGTACGTTAATTCGTAGGA
TACCCGTA
geometric
modeldiffusion
step modelrefinement
diffusionexperiment predicted
behavior
test shapesmeasuredbehavior
parameters
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Outline
1 Geometric model
2 Diffusion model
3 Numerical method
4 Preliminary results
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Geometric model
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Basepair model
DNA can be represented as a tube formed by oriented discs.
T A
CG
CG
GC
AT r
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Model parameters
XX
YYXY XY
X X
Y Y
η θ
T
A
C
G
(*,*,*)
X
(*,*,*) (*,*,*) (*,*,*)
CGA T
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
(*,*,*)
Y
ηXY = relative displacement for dimer step XY.
θXY = relative rotation for dimer step XY.
r = radius of tubular surface.
η = ηXY ∈ R26, θ = θXY ∈ R26, r ∈ R.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Parameter estimates
Tilt | Roll | Twist×10−1 (deg)†
X X
Y Y
Twist
RollTilt Slide
Rise
Shift
r
T A C G
A 0.0|1.1|2.9 −1.4|0.7|3.5 −0.1|0.7|3.2 −1.7|4.5|3.2T −1.4|0.7|3.5 0.0|3.3|3.8 −1.5|1.9|3.6 0.5|4.7|3.7G −0.1|0.7|3.2 −1.5|1.9|3.6 0.0|0.3|3.4 −0.1|3.6|3.3C −1.7|4.5|3.2 0.5|4.7|3.7 −0.1|3.6|3.3 0.0|5.4|3.6
†From x-ray data: Olson et al, PNAS 95 (1998) 11163.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Parameter estimates
Shift×10 | Slide×10 | Rise (A)†
X X
Y Y
Twist
RollTilt Slide
Rise
Shift
r
T A C G
A 0.0|−5.9|3.3 −0.3|−0.8|3.3 1.3|−5.8|3.4 0.9|−2.5|3.3T −0.3|−0.8|3.3 0.0| 0.5|3.4 −2.8| 0.9|3.4 0.9| 5.3|3.3G 1.3|−5.8|3.4 −2.8| 0.9|3.4 0.0|−3.8|3.4 0.5|−2.2|3.4C 0.9|−2.5|3.3 0.9| 5.3|3.3 0.5|−2.2|3.4 0.0| 4.1|3.4
†From x-ray data: Olson et al, PNAS 95 (1998) 11163.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Parameter estimates
Hydrated radius (A)‡
X X
Y Y
Twist
RollTilt Slide
Rise
Shift
r
r.= 13.
‡Using straight model: Tirado et al, J Chem Phys 81 (1984) 2047.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Model construction
X X X XX X X XS = X X X X
1 2 3 n1 2 3 n1 2 3 n
Points qa(S , η, θ), Curve γ(S , η, θ), Surface Γ(S , η, θ, r)∗.
* Assumed rigid.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Example 40-bp sequences
A=aqua, T=blue, G=gold, C=red
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Example 120-bp sequences
A=aqua, T=blue, G=gold, C=red
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Diffusion model
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Single molecule drift dynamics
Setup. Consider a single molecule in a fluid subject to externalloads.
v(t)
(t)
DNA
fluid
f τ
ω
ext ext
(v , ω)(t) = linear, angular velocities.
(f , τ)ext(t) = external force, torque.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Single molecule drift dynamics
Drift velocitiesωv ,
t
v , ω
t
v(t), ω(t) = 1T
∫ t+Tt v(s), ω(s) ds.
T = window size.
Governing eqns L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
.
L,M ∈ R6×6 Hydrodynamic drag,mobility matrices of molecule.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Single molecule drift dynamics
Drift velocitiesωv ,
t
v , ω
t
v(t), ω(t) = 1T
∫ t+Tt v(s), ω(s) ds.
T = window size.
Governing eqns L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
.
L,M ∈ R6×6 Hydrodynamic drag,mobility matrices of molecule.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Single molecule drift dynamics
Drift velocitiesωv ,
t
v , ω
t
v(t), ω(t) = 1T
∫ t+Tt v(s), ω(s) ds.
T = window size.
Governing eqns L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
.
L,M ∈ R6×6 Hydrodynamic drag,mobility matrices of molecule.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Definition of hydrodynamic matrices
Stokes eqns
µ∆u = ∇p in R3\B∇ · u = 0 in R3\B
u = U[v , ω] on ∂Bu, p → 0 as |x | → ∞.
BCs, loadsU[v , ω] = v + ω × (x − c)
σ[u, p] = −pI + µ(∇u +∇uT
)f [σ] =
∫∂B σn dA
τ [σ] =∫∂B(x − c)× σn dA.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Definition of hydrodynamic matrices
Stokes eqns
µ∆u = ∇p in R3\B∇ · u = 0 in R3\B
u = U[v , ω] on ∂Bu, p → 0 as |x | → ∞.
BCs, loadsU[v , ω] = v + ω × (x − c)
σ[u, p] = −pI + µ(∇u +∇uT
)f [σ] =
∫∂B σn dA
τ [σ] =∫∂B(x − c)× σn dA.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Definition of hydrodynamic matrices
Linearity result. The map from (v , ω) ∈ R6 to (f , τ) ∈ R6 islinear and invertible:
(v , ω)Stokes−→ (u, p)
∂−→ σ
∫−→ (f , τ).
Thus there exists L,M ∈ R6×6 such that[fτ
]= −
[L1 L3
L2 L4
]︸ ︷︷ ︸
L
[vω
],
[vω
]= −
[M1 M3
M2 M4
]︸ ︷︷ ︸
M
[fτ
].
L,M are called the Stokes drag, mobility matrices.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Definition of hydrodynamic matrices
Linearity result. The map from (v , ω) ∈ R6 to (f , τ) ∈ R6 islinear and invertible:
(v , ω)Stokes−→ (u, p)
∂−→ σ
∫−→ (f , τ).
Thus there exists L,M ∈ R6×6 such that[fτ
]= −
[L1 L3
L2 L4
]︸ ︷︷ ︸
L
[vω
],
[vω
]= −
[M1 M3
M2 M4
]︸ ︷︷ ︸
M
[fτ
].
L,M are called the Stokes drag, mobility matrices.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Properties of hydrodynamic matrices
L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
L,M are symmetric, positive-definite.
L,M depend on shape of ∂B and and ref point c .
Must solve Stokes equations in R3\B to determine.
Characterize velocities (v , ω) for given loads (f , τ)ext.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Properties of hydrodynamic matrices
L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
L,M are symmetric, positive-definite.
L,M depend on shape of ∂B and and ref point c .
Must solve Stokes equations in R3\B to determine.
Characterize velocities (v , ω) for given loads (f , τ)ext.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Properties of hydrodynamic matrices
L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
L,M are symmetric, positive-definite.
L,M depend on shape of ∂B and and ref point c .
Must solve Stokes equations in R3\B to determine.
Characterize velocities (v , ω) for given loads (f , τ)ext.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Properties of hydrodynamic matrices
L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
L,M are symmetric, positive-definite.
L,M depend on shape of ∂B and and ref point c .
Must solve Stokes equations in R3\B to determine.
Characterize velocities (v , ω) for given loads (f , τ)ext.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Properties of hydrodynamic matrices
L
[vω
]=
[fτ
]ext
or
[vω
]= M
[fτ
]ext
L,M are symmetric, positive-definite.
L,M depend on shape of ∂B and and ref point c .
Must solve Stokes equations in R3\B to determine.
Characterize velocities (v , ω) for given loads (f , τ)ext.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Collective drift dynamics
Setup. Consider a dilute solution of identical molecules in a fluidsubject to external loads.
Dom x SO3 Ω x A
Physicaldomain
(r,Q)
Configurationspace
Local coordspace
(q,η )
Dom
ext
extτ
f
σ = mass concentration in config space.
hext = (f , τ)ext = external loads.
M = Stokes mobility matrix.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Collective drift dynamics
Governing eqns
Dom x SO3 Ω x A
(r,Q) (q,η )
Dom
ext
extτ
f
σt + g−1∇ · (gJ) = 0 in Ω× A, t > 0J · n = 0 on (∂Ω)× A, t ≥ 0J · n periodic on Ω× (∂A), t ≥ 0σ = σ0 in Ω× A, t = 0.
J = −D∇σ + σChext, D = βbMbT , C = bMc .β = Boltzmann factor. g , b, c = geometric factors.
D,C ∈ R6×6 local diffusion, convection matrices.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Collective drift dynamics
Governing eqns
Dom x SO3 Ω x A
(r,Q) (q,η )
Dom
ext
extτ
f
σt + g−1∇ · (gJ) = 0 in Ω× A, t > 0J · n = 0 on (∂Ω)× A, t ≥ 0J · n periodic on Ω× (∂A), t ≥ 0σ = σ0 in Ω× A, t = 0.
J = −D∇σ + σChext, D = βbMbT , C = bMc .β = Boltzmann factor. g , b, c = geometric factors.
D,C ∈ R6×6 local diffusion, convection matrices.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Collective drift dynamics
Length, time scales
Dom x SO3Dom Molecule
ext
extτ
f
L
L
1
Trans: ttrn = time to drift across Dom
Rot: trot = time to drift across SO3
trotttrn
∼(`
L
)2
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Collective drift dynamics
Experimentsext
extτ
f
L
M =
»M1 M3M2 M4
–, trot
ttrn∼
(`L
)2
type scale measureable
ultracentrifugedyn light scattering
ttrn Dtrn =1
3tr(M1)
birefringencecircular dichroism
trot Drot =1
2tr(P⊥
d M4P⊥d )∗
* d=molecular axis of polarization
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
Stokes eqns
Γ= B
Bµ∆u = ∇p in R3\B∇ · u = 0 in R3\B
u = U[v , ω] on ∂Bu, p → 0 as |x | → ∞.
Gu,p(x , y),Hu,p(x , y) = stokeslet, stresslet (Green’s) functions.
Surface potentials
u(x) = λ∫
γGu(x , ξ)ψ(y(ξ)) dAξ + (1− λ)
∫ΓHu(x , y)ψ(y) dAy
p(x) = λ∫
γGp(x , ξ)ψ(y(ξ)) dAξ + (1− λ)
∫ΓHp(x , y)ψ(y) dAy .
ψ(y) = potential density. λ, φ = conditioning parameters.
(u, p) satisfy Stokes eqns w/o BC for any ψ, λ, φ.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
Stokes eqns
ξ γ
y
n(y) φ
Γ= B
µ∆u = ∇p in R3\B∇ · u = 0 in R3\B
u = U[v , ω] on ∂Bu, p → 0 as |x | → ∞.
Gu,p(x , y),Hu,p(x , y) = stokeslet, stresslet (Green’s) functions.
Surface potentials
u(x) = λ∫
γGu(x , ξ)ψ(y(ξ)) dAξ + (1− λ)
∫ΓHu(x , y)ψ(y) dAy
p(x) = λ∫
γGp(x , ξ)ψ(y(ξ)) dAξ + (1− λ)
∫ΓHp(x , y)ψ(y) dAy .
ψ(y) = potential density. λ, φ = conditioning parameters.
(u, p) satisfy Stokes eqns w/o BC for any ψ, λ, φ.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
Integral eqn for ψξ γ
y
n(y) φ
Γ= Bλ
∫γ
Gu(x , ξ)ψ(y(ξ)) dAξ
+ (1− λ)∫ΓHu(x , y)[ψ(y)− ψ(x)] dAy
= U[v , ω](x), ∀x ∈ Γ.
Operator has bounded inverse, integrands ∀λ ∈ (0, 1), φ ∈ (0, φΓ).
Approximation∑Nb=1 Kabψb = Ua[v , ω], a = 1, . . . ,N.
(v , ω) −→ ψ −→ (f , τ)︸ ︷︷ ︸6 times
−→ L −→ M −→ (Dtrn,Drot).
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
Integral eqn for ψξ γ
y
n(y) φ
Γ= Bλ
∫γ
Gu(x , ξ)ψ(y(ξ)) dAξ
+ (1− λ)∫ΓHu(x , y)[ψ(y)− ψ(x)] dAy
= U[v , ω](x), ∀x ∈ Γ.
Operator has bounded inverse, integrands ∀λ ∈ (0, 1), φ ∈ (0, φΓ).
Approximation∑Nb=1 Kabψb = Ua[v , ω], a = 1, . . . ,N.
(v , ω) −→ ψ −→ (f , τ)︸ ︷︷ ︸6 times
−→ L −→ M −→ (Dtrn,Drot).
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
Conditioning vs (λ, φ)
0 0.2 0.4 0.6 0.8 10
1
σ min
λ
1
7
13
σ max
0.1 0.3 0.5 0.7 0.90.5
1
1.5
2
2.5
3
λ
log 10
(σm
ax/σ
min
)φ/φΓ =
1
8(dots),
2
8(crosses),
3
8(pluses),
4
8(stars), . . ..
Condition numberσmax
σmin≤ 101.5 for (λ, φ/φΓ) near (
1
2,1
2).
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Numerical method
Accuracy vs h
4 8 12 16 2028.45
28.5
28.55
28.6
1/h
|F|
5 10 15 2065.3
65.4
65.5
65.6
1/h
|T|
|∆f ||f | ,
|∆τ ||τ | ≤ 0.1% over range of geometries of interest.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Preliminary results
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Application: radius estimation
Given: Measured values of Dtrn and Drot on various sequences.
Find: Radius r of hydrated DNA using two different geometricalmodels:
Classic straight model.
Sequence-dependent model.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Results for classic model: Dtrn vs length
0 20 40 60 80 100 120 140 1601
1.5
2
2.5
3
3.5
4
4.5
5
basepairs n
dim
ensi
onle
ss D
t x
n
Symbols: experiments (ultracentrifuge, light scattering,electrophoresis).
Curves: numerics w/r = 10, 11, . . . , 15A (top to bottom).
Results predict DNA radius of r = 10− 15A.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Results for sequence-dependent model: Dtrn vs length
0 20 40 60 80 100 1201
1.5
2
2.5
3
3.5
4
4.5
5
basepairs n
dim
ensi
onle
ss D
t x
n
Curves: numerics w/r = 10, 11, . . . , 15A (top to bottom).
Crosses, pluses: random sequences w/r = 10, 15A.
Results show systematic offset.
Results now predict DNA radius of r = 12− 17A.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Results for classic model: Drot vs length
0 20 40 60 80 100 120 140 1600
0.5
1
1.5
2
2.5
3
basepairs n
dim
ensi
onle
ss D
r x
n^3
Assume: polarization axis is long principal axis.
Symbols: experiments (birefringence, light scattering).
Curves: numerics w/r = 12, 11, . . . , 18A (top to bottom).
Results predict DNA radius of r = 13− 17A.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Results for sequence-dependent model: Drot vs length
0 20 40 60 80 100 1200
0.5
1
1.5
2
2.5
3
3.5
4
basepairs n
dim
ensi
onle
ss D
r x
n^3
Assume: polarization axis is long principal axis.
Curves: numerics w/r = 12, 11, . . . , 18A (top to bottom).
Crosses, pluses: random sequences w/r = 12, 18A.
Results show dramatic dependence on curvature.
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA
Introduction Geometric model Diffusion model Numerical method Preliminary results
Concluding remarks
Simplest model of sequence-dependent DNA geometry involves
many parameters (η ∈ R26, θ ∈ R26, r ∈ R).
Estimates for all parameters exist, but there is little consensus.
Hydrodynamic modeling offers promising approach to validate
and refine parameters.
Successful realization of approach poses many challenges.
Support
NSF
O. Gonzalez and J. Li UT-Austin
Hydrodynamic modeling of DNA