Answers are grounded in this paper and cite their sources.
In molecular dynamics simulations of RNA, Mg2+ ion force field parameters remain highly sensitive to the choice of water model and nucleic acid force field. The choice of Mg2+ force field parameters requires intentional thought, and although recent trends in nucleic acid force field development increasingly use the OPC water model, the compatibility of Mg2+ parameters with the OL3/OPC combination is insufficiently characterized. Here, we benchmark a panel of Mg2+ force fields: first in water boxes containing OPC with a single Mg2+ ion, and then in simulations with the Varkud satellite ribozyme stem loop V (SLV) as a model RNA, using the OL3 force field with LJbb corrections (OL3-LJbb). While most Mg2+ models are designed to reproduce the experimental ordering of hydration shells, they still differ substantially in diffusion coefficients and hydration free energies, reflecting the known trade-off between reproducing hydration thermodynamics and ion-oxygen distances in divalent-cation parametrization. These differences translate directly to RNA simulations, where Mg2+ models with slower diffusion and overly favorable hydration free energies promote long time-scale RNA binding events (“chelation”) and disrupt Mg2+-driven conformational changes. Together, these results highlight the need to validate divalent ion parameters specifically within the water model and RNA force field environment used for production-phase RNA molecular simulations, as well as demonstrate the Varkud satellite ribozyme as a sensitive benchmark for Mg2+/RNA/solvent force field compatibility.
No takes yet. Share an insight, caveat, or question.
Fisher et al. (2026) studied this question.
Synapse has enriched 10 related papers. Consider them for comparative context: