scholarly journals Mixing MARTINI: Electrostatic Coupling in Hybrid Atomistic–Coarse-Grained Biomolecular Simulations

2013 ◽  
Vol 117 (13) ◽  
pp. 3516-3530 ◽  
Author(s):  
Tsjerk A. Wassenaar ◽  
Helgi I. Ingólfsson ◽  
Marten Prieß ◽  
Siewert J. Marrink ◽  
Lars V. Schäfer
2007 ◽  
Vol 111 (27) ◽  
pp. 7812-7824 ◽  
Author(s):  
Siewert J. Marrink ◽  
H. Jelger Risselada ◽  
Serge Yefimov ◽  
D. Peter Tieleman ◽  
Alex H. de Vries

2021 ◽  
Vol 61 (3) ◽  
pp. 144-151
Author(s):  
Shoji TAKADA

2015 ◽  
Vol 17 (13) ◽  
pp. 8393-8406 ◽  
Author(s):  
Srinivasa M. Gopal ◽  
Alexander B. Kuhn ◽  
Lars V. Schäfer

How accurate is bundled SPC water as inner shell solvent for hybrid all-atom/coarse-grained simulations?


2019 ◽  
Vol 116 (39) ◽  
pp. 19484-19489 ◽  
Author(s):  
Chen Bai ◽  
Arieh Warshel

The elucidation of the detailed mechanism used by F0 to convert proton gradient to torque and rotational motion presents a major puzzle despite significant biophysical and structural progress. Although the conceptual model has advanced our understanding of the working principles of such systems, it is crucial to explore the actual mechanism using structure-based models that actually reproduce a unidirectional proton-driven rotation. Our previous work used a coarse-grained (CG) model to simulate the action of F0. However, the simulations were based on a very tentative structural model of the interaction between subunit a and subunit c. Here, we again use a CG model but with a recent cryo-EM structure of cF1F0 and also explore the proton path using our water flooding and protein dipole Langevin dipole semimacroscopic formalism with its linear response approximation version (PDLD/S-LRA) approaches. The simulations are done in the combined space defined by the rotational coordinate and the proton transport coordinate. The study reproduced the effect of the protomotive force on the rotation of the F0 while establishing the electrostatic origin of this effect. Our landscape reproduces the correct unidirectionality of the synthetic direction of the F0 rotation and shows that it reflects the combined electrostatic coupling between the proton transport path and the c-ring conformational change. This work provides guidance for further studies in other proton-driven mechanochemical systems and should lead (when combined with studies of F1) to a complete energy transduction picture of the F0F1-ATPase system.


Author(s):  
R. E. Ferrell ◽  
G. G. Paulson

The pore spaces in sandstones are the result of the original depositional fabric and the degree of post-depositional alteration that the rock has experienced. The largest pore volumes are present in coarse-grained, well-sorted materials with high sphericity. The chief mechanisms which alter the shape and size of the pores are precipitation of cementing agents and the dissolution of soluble components. Each process may operate alone or in combination with the other, or there may be several generations of cementation and solution.The scanning electron microscope has ‘been used in this study to reveal the morphology of the pore spaces in a variety of moderate porosity, orthoquartzites.


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