Computational solvation dynamics of oxyquinolinium betaine linked to trehalose

TL;DR

This study uses computer simulations to analyze water dynamics around biomolecules, specifically trehalose, revealing that measured solvent relaxation times underestimate the true hydration layer dynamics.

Contribution

It introduces a simulation approach to decompose and accurately interpret solvation dynamics contributions from different solvent regions around biomolecules.

Findings

Simulations accurately reproduce experimental Stokes shift data.

Only half of the observed shift is from retarded hydration layer water.

Measured relaxation times are lower bounds for true hydration layer dynamics.

Abstract

Studying the changed water dynamics in the hydration layers of biomolecules is an important step towards fuller understanding of their function and mechanisms, but has shown to be quite difficult. The measurement of the time-dependent Stokes shift of a chromophore attached to the biomolecule is a promising method to achieve this goal, as published in J. Phys. Chem. Lett. 5 (2014), 1845, where trehalose was used as biomolecule, 1-methyl-6-oxyquinolinium betaine as chromophore and water as solvent. An overall retardation of solvent molecules is then obtained by comparison of the linked system to the same system without trehalose, but contributions from different subgroups of solvent molecules, for example molecules close to or far from trehalose, are unknown. The difficulty arising from these unknown contributions of retarded and possibly unretarded solvent molecules is overcome in this work by conducting computer simulations on this system and decomposing the overall signal into contributions from various molecules at different locations. We performed non-equilibrium molecular dynamics simulation using a polarizable water model and a non-polarizable solute model and could reproduce the experimental time-dependent Stokes shift accurately for the linked trehalose-oxyquinolinium and the pure oxyquinolinium over a wide temperature range, indicating the correctness of our employed models. Decomposition of the shift into contributions from different solvent subgroups showed that the amplitude of the measured shift is made up only half by the desired retarded solvent molecules in the hydration layer, but to another half by unretarded bulk water, so that measured relaxation times of the overall Stokes shift are only a lower boundary for the true relaxation times in the hydration layer of trehalose.