Review



multiphysics finite element physical modeling program  (COMSOL Inc)

 
  • Logo
  • About
  • News
  • Press Release
  • Team
  • Advisors
  • Partners
  • Contact
  • Bioz Stars
  • Bioz vStars
    • 90
      Buy from Supplier

    Structured Review

    COMSOL Inc multiphysics finite element physical modeling program
    ( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> 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.
    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, 2026-08
    90/100 stars

    Images

    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

    ( 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.
    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.

    Techniques Used:



    Similar Products

    2d plane strain finite element program abaqus 2017  (Abaqus Inc)
    86
    Abaqus Inc 2d plane strain finite element program abaqus 2017
    2d Plane Strain Finite Element Program Abaqus 2017, supplied by Abaqus Inc, used in various techniques. Bioz Stars score: 86/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/finite+element+program/abaqus+element+finite+software/10__1016_slash_j__geotexmem__2026__04__011-63-2-8
    Average 86 stars, based on 1 article reviews
    2d plane strain finite element program abaqus 2017 - by Bioz Stars, 2026-08
    86/100 stars
    		  Buy from Supplier
    non linear finite element program abaqus  (Abaqus Inc)
    86
    Abaqus Inc non linear finite element program abaqus
    Non Linear Finite Element Program Abaqus, supplied by Abaqus Inc, used in various techniques. Bioz Stars score: 86/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/finite+element+program/abaqus+element+finite+software/pm41888195-5-16-20
    Average 86 stars, based on 1 article reviews
    non linear finite element program abaqus - by Bioz Stars, 2026-08
    86/100 stars
    		  Buy from Supplier
    abaqus finite element program  (Abaqus Inc)
    86
    Abaqus Inc abaqus finite element program
    Abaqus Finite Element Program, supplied by Abaqus Inc, used in various techniques. Bioz Stars score: 86/100, based on 1 PubMed citations. ZERO BIAS - scores, article reviews, protocol conditions and more
    https://www.bioz.com/product/finite+element+program/abaqus+element+finite+software/10__3390_slash_en18246548-50-7-7
    Average 86 stars, based on 1 article reviews
    abaqus finite element program - by Bioz Stars, 2026-08
    86/100 stars
    		  Buy from Supplier
    multiphysics finite element physical modeling program  (COMSOL Inc)
    90
    COMSOL Inc multiphysics finite element physical modeling program
    ( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> 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.
    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, 2026-08
    90/100 stars
    		  Buy from Supplier
    finite element solver program ansys 2022  (ANSYS inc)
    90
    ANSYS inc finite element solver program ansys 2022
    ( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> 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.
    Finite Element Solver Program Ansys 2022, supplied by ANSYS 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/finite+element+solver+program+ansys+2022/pm40498810-258-1-5
    Average 90 stars, based on 1 article reviews
    finite element solver program ansys 2022 - by Bioz Stars, 2026-08
    90/100 stars
    		  Buy from Supplier
    three-dimensional (3d) finite element model (fem) program  (Abaqus Inc)
    90
    Abaqus Inc three-dimensional (3d) finite element model (fem) program
    ( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> 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.
    Three Dimensional (3d) Finite Element Model (Fem) Program, supplied by Abaqus 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/3d+finite+element+model/pm40489789-136-34-32
    Average 90 stars, based on 1 article reviews
    three-dimensional (3d) finite element model (fem) program - by Bioz Stars, 2026-08
    90/100 stars
    		  Buy from Supplier
    finite element method (fem)–ansys program  (ANSYS inc)
    90
    ANSYS inc finite element method (fem)–ansys program
    ( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> 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.
    Finite Element Method (Fem)–Ansys Program, supplied by ANSYS 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/ansys+cfx/pm40572832-2-6-8
    Average 90 stars, based on 1 article reviews
    finite element method (fem)–ansys program - by Bioz Stars, 2026-08
    90/100 stars
    		  Buy from Supplier
    finite element software program ansys workbench 18.0  (ANSYS inc)
    90
    ANSYS inc finite element software program ansys workbench 18.0
    ( A , C , and E ) The geometries and boundary conditions of COMSOL <t>Multiphysics</t> 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.
    Finite Element Software Program Ansys Workbench 18.0, supplied by ANSYS 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/ansys+cfx/pm40462021-75-8-12
    Average 90 stars, based on 1 article reviews
    finite element software program ansys workbench 18.0 - by Bioz Stars, 2026-08
    90/100 stars
    		  Buy from Supplier

    Image Search Results


    ( 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.

    Journal: Science Advances

    Article Title: A shallow mantle source for the Chang’e 5 lavas reveals how top-down heating prolonged lunar magmatism

    doi: 10.1126/sciadv.adr1486

    Figure Lengend 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.

    Article Snippet: A series of two-dimensional thermal evolution models for a simplified east-west cross section of the local region of the Moon in northern Oceanus Procellarum where the CE5 basalts were collected were constructed using the COMSOL Multiphysics finite element physical modeling program.

    Techniques: