multiphysics finite element physical modeling program (COMSOL Inc)
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COMSOL Inc
multiphysics finite element physical modeling program
Multiphysics Finite Element Physical Modeling Program, supplied by COMSOL Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/finite+element+program/multiphysics+software/pmc12273790-232-35-34
Average 90 stars, based on 1 article reviews
Multiphysics Finite Element Physical Modeling Program, supplied by COMSOL Inc, used in various techniques. Bioz Stars score: 90/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
https://www.bioz.com/product/finite+element+program/multiphysics+software/pmc12273790-232-35-34
Average 90 stars, based on 1 article reviews
multiphysics finite element physical modeling program - by Bioz Stars,
2026-09
90/100 stars
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1) Product Images from "A shallow mantle source for the Chang’e 5 lavas reveals how top-down heating prolonged lunar magmatism"
Article Title: A shallow mantle source for the Chang’e 5 lavas reveals how top-down heating prolonged lunar magmatism
Journal: Science Advances
doi: 10.1126/sciadv.adr1486
Figure Legend Snippet: ( A , C , and E ) The geometries and boundary conditions of COMSOL Multiphysics finite element thermal models for schematic cross sections of the crust and upper mantle in the region of the CE5 landing site. Compositions and thermal conductivities used for all models are shown in (A) and discussed in Materials and Methods. The upper KREEP layer represents Imbrium ejecta to the east of the CE5 landing site and begins generating heat at 3.9 Ga in all models. The lower KREEP layer has the composition of high-K KREEP . See Materials and Methods for more details on initial model conditions. ( B , D , and F ) Model results showing the temperature profiles of the crust and upper mantle at 2 Ga for each model. As these models are purely conductive and absolute temperatures are not necessarily applicable to the mantle, but rather these models show the relative heating effects of a subcrustal KREEP layer of either 5 km (D) or 10 km (F) thickness.
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