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Interphase chromatin appeared to be a disordered assemblage of nucleosomes and could best be described by the polymer melt model.
In contrast to the textbook 30-nm fiber model, O. tauri chromatin resembles a disordered assemblage of nucleosomes akin to the polymer melt model.
They demonstrated that O. tauri chromatin resembles a disordered assembly of nucleosomes without the 30-nm chromatin structure compatible with the polymer melt model.
This article presents an R-package, airGR, to facilitate the implementation of the GR lumped hydrological models (including GR4J) and a snow-accumulation and melt model.
SWE reconstruction using satellite snow cover area and a melt model provides reasonable information that is suitable for hydrological applications.
We present some conclusions in Section 5. We employ the phase-field method for the crystallization of a pure material from its melt (model I in Wang et al., 1993).
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Further research should test the extended temperature-index melt models at the catchment scale, particularly in catchments where there have been rapid and well documented changes in forest cover.
Experimentally determined F and Cl partition coefficients were used in a hydrous melting model of a lherzolitic mantle metasomatized by slab fluid.
The size effect on the melting point depression of micro/nanoparticles is modelled at the liquid solid interface of the melting model.
Nevertheless, in the melting model presented below, we used an amphibole-bearing wehrlite (Médard et al. [2006]), because to date no melting modes are available for amphibole-bearing lherzolite.
Compared with the heat-only model, the utilization of the heat-mass coupled snow melting model can avoid overestimating the required heat fluxes to achieve a specific snow melting performance.
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