Topic 2 Flashcards

-Describe the similarities and differences between all-atom and coarse-grained force fields. -Explain how coarse-graining attempts to address the length and timescale problems in molecular dynamics -Compare three different methods for developing coarse-grained interaction potentials/force fields -Evaluate a coarse-grained simulation study of a biological system

1
Q

Briefly discuss and compare three different force-fields, using the alcohol octanol as an example.

A
  • All-atom: An all atom/atomistic force-field treats each atom explicitly. At every step, the simulation must input all bonding/non-bonding interactions in a system. In long molecules like octanol, this can lead to many dihedral angles needing to be specified for all differing ~-OH chains. Very precise however, computationally costly.
  • United-atom: cheaper way to describe the system that saves computational time, but still expensive. It does this by grouping less chemically involved hydrogen atoms into CH­2 groups. Good for lipid descriptions
  • Coarse graining: 4-5 heavy atoms with their H’s are grouped into a single interaction site, saving large amount of computational effort. Octanol is split into a polar (hydrophilic) and non-polar (hydrophobic) half. Lose a degree of chemical detail as cannot capture hydrogen bonding explicitly. However partial charges assigned to these blocks to describe electrostatic and non-bonding interactions.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Using a course-grained forcefield allows simulation of larger … for … timescales than with all-atom forcefields, giving a higher chance of overcoming … …

A

Using a course-grained forcefield allows simulation of larger systems for longer timescales than with all-atom forcefields, giving a higher chance of overcoming kinetic barriers.

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

What are three ways in which coarse graining allow simualtion on larger systems for longer timescales?

A
  • Decrease in total number of particles N
  • Larger time step
  • Smoother energy landscape
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

How does a decrease in total number of particles N ‘speed up’ a coarse grain simulation?

A
  • A decrease in total number of particles reduces the number of force calculations required at each step.
  • Resulting in less computational time needed to move the system forward one-time step, as less forces and energies must be calculated each step.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

How does larger time-step ‘speed up’ a coarse grain simulation?

A
  • A ​time step for integration needs to be smaller than the highest frequency motion in a system.
  • The verlet algorithm can be used to move an atom through calculation of the force, with respect to all other atoms, to apply in one timestep, which should be constant.
  • A time step may be suitable for bond stretch of a low frequency (left), resulting in it being closer to its equilibrium value. However, the same force acting on a higher frequency motion (right) results in a high energy final position, leading to assumption of force being constant over our chosen timestep to be invalid.
  • Timesteps should be 10x smaller than highest frequency motion, which are generally bond stretches of light hydrogen atoms.
  • By removing bonds involving them, a larger time step can be used, as particles of higher mass oscillate slower. Each time step now propagates us further forward in time.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

How does a smoother energy landscape ‘speed up’ coarse graining?

A
  • Rugged energy landscape of an atomistic model has many local minima.
  • Averaging that occurs through coarse-graining results in a smoother energy landscape with less local trapping/friction and faster dynamics.
  • Beads can slide over each other much easier
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

Why must we develop new interaction potentials for coarse grained systems?

A
  • Coarse-grained particles do not interact in the same way that atoms do.
  • New coarse-grained potentials must be developed that are unique to each system.
  • Parameterising is a large challenge as takes a lot of time to predict the correct output.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

What are two methods of generating course-grained interaction potentials?

A
  • Use an analytical functional form with associated parameters; like atomistic interaction potentials but with CG beads
  • Numerically fitting data from atomistic simulations using tabulated potentials (list of r’s between atoms with corresponding F’s/E’s – useful for complex systems where don’t have analytical function)
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What is mapping, and why is it essential for developing a CGP? (PPQ)

A
  • The first stage in developing a CG interaction potential (CGP) is to define mapping of the atomistic system in to a CG one.
  • Essential for new molecules and there are many ways to assign atomistic structure depending on what interactions are expected to be the focus.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

What are 2 general rules of mapping?

A
  • Each bead will inherit the mass/charge of its constituents
  • Must maintain the overall shape of the molecule (otherwise may not replicate the correct self-assembled structure)
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Outline how you would produce a CG trajectory from an atomistic simulation using a bottom up approach

A
  • First, run a reference atomistic simulation to use as our benchmark (however does not necessarily equal experimental/ab initio PES)
  • Extract effective CG potentials using a trajectory of a system (a series of snapshots over time).
  • Each snapshot in the atomistic simulation will have positions for all atoms at each timestep which will be used to find their corresponding Force/Energy.
  • A CG pseudo trajectory can be attained by grouping atoms in to beads using the beads centre of mass based on an atomistic average.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

What is an RDF?

A
  • A radial distribution function g(r) shows the probability of finding a particle at distance r from a reference particle.
  • At small distances there is a low probability of finding another atom due to coulombic repulsion (LJP?)
  • Shells form around the reference particle as other bands of particles appear, with depletion zones between them.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

How does an RDF used as a target reference functions help form non-bonded potentials from the trajectory of a system?

A
  • Goal is to form a CGP that reproduces the RDF obtained from atomistic simulations.
  • The CG RDF, g(i) is linked to the trajectory of our system CG trajectory,
  • Which in turn is linked to an atomistic RDF, g(ref), derived from an atomistic trajectory.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

What is the potential mean force and how is it related to g(ref)?

A
  • Links the potential of mean force (average force that an atom experiences due to its neighbours) to the radial distribution function at that point.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Why can we not use VPMF as a pair potential in our CG model? (not imp)

A
  • Contains manybody contributions from all particles in the system.
  • Want a pairwise interaction potential showing how energy varies with r, the sum of which equals our RDF.
How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

How is VPMF used in Iterative Boltzmann Inversion iteratively?

A
  • VPMF =kBTln[gref(r)] instead is used as a starting guess for VCG (intermolecular CG potential)
  • Vi+1CG(r) = ViCG(r) + kBTln[gi(r) / gref(r)] is our improved guess after each iteration
  • gref(r) is our target probability distribution from atomistic simulation
  • gi(r) is the probability distribution from a CG simulation using the ith potential
  • Difference between the two moves us closer of further to result
17
Q
  • How does our improved guess for the intermolecular CG potential [VCGi+1(r)] change when gi(r) = gref(r)? – 1 on graph
A

kBTln…= 0, no change to interaction potential needed as CG simulation produces same pairwise structure as atomistic

18
Q
  • How does our improved guess for the intermolecular CG potential [VCGi+1(r)] change when gi(r) < gref(r)? – 2 on graph
A
  • kBT… is -ve
  • probability of finding particle (correlation between CG beads) at that r underestimated.
  • Equation will lower pairwise CG energy at that r, making interaction more favourable
19
Q
  • How does our improved guess for the intermolecular CG potential [VCGi+1(r)] change when gi(r) < gref(r)? – 3 on graph
A
  • kBTln… is +ve
  • probability of finding particle (correlation between CG beads) at that r overestimated.
  • Equation raises pairwise CG energy at that r, making interaction more appropriately favourable (less than before).
20
Q
  • Why does it take so long to produce a CG potential through IBI that is like an atomistic trajectory?
A
  • Must iteratively calculate each pairwise interaction in your system using the IBI method until a full CG tabulated potential that is like the original atomistic trajectory is gained.
  • However once this is done, CG allows us to reach much higher simulation times.
21
Q
  • What is a problem with the IBI discussed in lectures as well as an example of this being solved?
A
  • It takes only a singular atomistic simulation into account as a reference that will be under certain set conditions. This is a problem if one wanted to study phase transitions, which are dependent temperature changes.
  • Moore et al (2016) developed a CGP constructed using many different atomistic simulations at varying temperatures to account for this, known as multi-state IBI.
22
Q
  • What is force matching and how does it differ to Iterative Boltzmann inversion?
A
  • IBI tried to match the structure of an atomistic simulation where the RDF is used to reach our target data.
  • Force matching aims to match forces on the CG interaction sites with the forces at the atomistic level.
23
Q
  • What is an example of a property one may want to look for using force matching?
A
  • Force matching is ideal for looking at thermodynamic properties, for example a partition coefficient.
24
Q
  • Explain the process of force matching. (don’t need to know in detail)
A
  • A set of reference forces is collected through running an atomistic simulation
  • A reference force Firef on a CG bead = sum of associated atomistic forces on beads constituents fγ , generating a pseudo CG trajectory acting as our target.
  • Match the set of CG forces to the reference forces to minimise (image)
  • Filp is the Net force on site i in atomistic config l
  • Filref is the force determined by the trail force field (similar to VPMF). Often an existing CGP that is then adapted to fit closer to chosen reference.
25
Q
  • What kind of approaches are IBI and force matching and what is the alternative?
A
  • They are both bottom-up approaches, where a reference atomistic simulation is used to construct an effective CGP for our system which takes a long time to do. Inverse Monte Carlo (IMC) is another.
  • Alternatively, one can use a top-down approach, which is generally used for investigating thermodynamic properties.
26
Q
  • What are some advantages of both bottom-up and top-down approaches?
A
  • Bottom-up: capable of capturing fine detail of interaction as CG interactions are extracted from reference atomistic simulations
  • Top-down: provide potentials that are more easily transferable and applicable to experimental data.
27
Q
  • What is an example of a top-down approach?
A
  • The MARTINI force field, a CG potential fitted to reproduce experimental target data, using few parameters and standard interaction potentials to maximise transferability.
  • A choice of building blocks calibrated against experimental oil/water partition coefficients are available to build a system
28
Q
  • What is a disadvantage of the MARTINI force-field?
A
  • No systematic way for developing potentials and introducing new molecules unavailable in building blocks.
29
Q
  • Give examples of two systems that require a CG potential
A
  • van Eerden et al – simulation of a large photosynthetic protein complex with membrane bound and water bound parts. Would be very difficult to simulate this complex system for long atomistically.
  • Fowler et al – using the MARTINI FF to study the effects of embedded proteins on membrane stiffness using a course grained model.
30
Q
  • What are some disadvantages of CG models?
A
  • A model can be too biased, and very untransferable to another system
  • A model may only be parameterised for a specific class of molecules, showing a lack of compatibility
  • Model may be too coarse to capture desired behaviour
31
Q
  • Water must be described accurately in CG models, why is this?
A
  • Present in abundance in many biological systems, showing complex behaviours within those systems. Models generally are split in to three categorise to parameterise water (implicit, explicit, and polarizable)