Numerical modeling of heat exchange and unsaturated–saturated flow in porous media
We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltr...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Kačur, Jozef [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2019transfer abstract |
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| Schlagwörter: |
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| Umfang: |
13 |
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| Übergeordnetes Werk: |
Enthalten in: Growth and welfare implications of sector-specific innovations - Güner, İlhan ELSEVIER, 2022, an international journal, Amsterdam [u.a.] |
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| Übergeordnetes Werk: |
volume:77 ; year:2019 ; number:6 ; day:15 ; month:03 ; pages:1668-1680 ; extent:13 |
| Links: |
|---|
| DOI / URN: |
10.1016/j.camwa.2018.06.009 |
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ELV045964696 |
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| 245 | 1 | 0 | |a Numerical modeling of heat exchange and unsaturated–saturated flow in porous media |
| 264 | 1 | |c 2019transfer abstract | |
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| 520 | |a We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. | ||
| 520 | |a We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. | ||
| 650 | 7 | |a Porous media |2 Elsevier | |
| 650 | 7 | |a Heat and mass transport |2 Elsevier | |
| 650 | 7 | |a Heat exchange |2 Elsevier | |
| 650 | 7 | |a Model scaling |2 Elsevier | |
| 650 | 7 | |a Unsaturated flow |2 Elsevier | |
| 700 | 1 | |a Mihala, Patrik |4 oth | |
| 700 | 1 | |a Tóth, Michal |4 oth | |
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2019 |
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10.1016/j.camwa.2018.06.009 doi GBV00000000000582.pica (DE-627)ELV045964696 (ELSEVIER)S0898-1221(18)30333-X DE-627 ger DE-627 rakwb eng 330 VZ 83.03 bkl 83.10 bkl Kačur, Jozef verfasserin aut Numerical modeling of heat exchange and unsaturated–saturated flow in porous media 2019transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Elsevier Mihala, Patrik oth Tóth, Michal oth Enthalten in Elsevier Science Güner, İlhan ELSEVIER Growth and welfare implications of sector-specific innovations 2022 an international journal Amsterdam [u.a.] (DE-627)ELV008987521 volume:77 year:2019 number:6 day:15 month:03 pages:1668-1680 extent:13 https://doi.org/10.1016/j.camwa.2018.06.009 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 83.03 Methoden und Techniken der Volkswirtschaft VZ 83.10 Wirtschaftstheorie: Allgemeines VZ AR 77 2019 6 15 0315 1668-1680 13 |
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10.1016/j.camwa.2018.06.009 doi GBV00000000000582.pica (DE-627)ELV045964696 (ELSEVIER)S0898-1221(18)30333-X DE-627 ger DE-627 rakwb eng 330 VZ 83.03 bkl 83.10 bkl Kačur, Jozef verfasserin aut Numerical modeling of heat exchange and unsaturated–saturated flow in porous media 2019transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Elsevier Mihala, Patrik oth Tóth, Michal oth Enthalten in Elsevier Science Güner, İlhan ELSEVIER Growth and welfare implications of sector-specific innovations 2022 an international journal Amsterdam [u.a.] (DE-627)ELV008987521 volume:77 year:2019 number:6 day:15 month:03 pages:1668-1680 extent:13 https://doi.org/10.1016/j.camwa.2018.06.009 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 83.03 Methoden und Techniken der Volkswirtschaft VZ 83.10 Wirtschaftstheorie: Allgemeines VZ AR 77 2019 6 15 0315 1668-1680 13 |
| allfields_unstemmed |
10.1016/j.camwa.2018.06.009 doi GBV00000000000582.pica (DE-627)ELV045964696 (ELSEVIER)S0898-1221(18)30333-X DE-627 ger DE-627 rakwb eng 330 VZ 83.03 bkl 83.10 bkl Kačur, Jozef verfasserin aut Numerical modeling of heat exchange and unsaturated–saturated flow in porous media 2019transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Elsevier Mihala, Patrik oth Tóth, Michal oth Enthalten in Elsevier Science Güner, İlhan ELSEVIER Growth and welfare implications of sector-specific innovations 2022 an international journal Amsterdam [u.a.] (DE-627)ELV008987521 volume:77 year:2019 number:6 day:15 month:03 pages:1668-1680 extent:13 https://doi.org/10.1016/j.camwa.2018.06.009 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 83.03 Methoden und Techniken der Volkswirtschaft VZ 83.10 Wirtschaftstheorie: Allgemeines VZ AR 77 2019 6 15 0315 1668-1680 13 |
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10.1016/j.camwa.2018.06.009 doi GBV00000000000582.pica (DE-627)ELV045964696 (ELSEVIER)S0898-1221(18)30333-X DE-627 ger DE-627 rakwb eng 330 VZ 83.03 bkl 83.10 bkl Kačur, Jozef verfasserin aut Numerical modeling of heat exchange and unsaturated–saturated flow in porous media 2019transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Elsevier Mihala, Patrik oth Tóth, Michal oth Enthalten in Elsevier Science Güner, İlhan ELSEVIER Growth and welfare implications of sector-specific innovations 2022 an international journal Amsterdam [u.a.] (DE-627)ELV008987521 volume:77 year:2019 number:6 day:15 month:03 pages:1668-1680 extent:13 https://doi.org/10.1016/j.camwa.2018.06.009 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 83.03 Methoden und Techniken der Volkswirtschaft VZ 83.10 Wirtschaftstheorie: Allgemeines VZ AR 77 2019 6 15 0315 1668-1680 13 |
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10.1016/j.camwa.2018.06.009 doi GBV00000000000582.pica (DE-627)ELV045964696 (ELSEVIER)S0898-1221(18)30333-X DE-627 ger DE-627 rakwb eng 330 VZ 83.03 bkl 83.10 bkl Kačur, Jozef verfasserin aut Numerical modeling of heat exchange and unsaturated–saturated flow in porous media 2019transfer abstract 13 nicht spezifiziert zzz rdacontent nicht spezifiziert z rdamedia nicht spezifiziert zu rdacarrier We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Elsevier Mihala, Patrik oth Tóth, Michal oth Enthalten in Elsevier Science Güner, İlhan ELSEVIER Growth and welfare implications of sector-specific innovations 2022 an international journal Amsterdam [u.a.] (DE-627)ELV008987521 volume:77 year:2019 number:6 day:15 month:03 pages:1668-1680 extent:13 https://doi.org/10.1016/j.camwa.2018.06.009 Volltext GBV_USEFLAG_U GBV_ELV SYSFLAG_U 83.03 Methoden und Techniken der Volkswirtschaft VZ 83.10 Wirtschaftstheorie: Allgemeines VZ AR 77 2019 6 15 0315 1668-1680 13 |
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| author |
Kačur, Jozef |
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Kačur, Jozef ddc 330 bkl 83.03 bkl 83.10 Elsevier Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Numerical modeling of heat exchange and unsaturated–saturated flow in porous media |
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330 VZ 83.03 bkl 83.10 bkl Numerical modeling of heat exchange and unsaturated–saturated flow in porous media Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow Elsevier |
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ddc 330 bkl 83.03 bkl 83.10 Elsevier Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow |
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ddc 330 bkl 83.03 bkl 83.10 Elsevier Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow |
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ddc 330 bkl 83.03 bkl 83.10 Elsevier Porous media Elsevier Heat and mass transport Elsevier Heat exchange Elsevier Model scaling Elsevier Unsaturated flow |
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Growth and welfare implications of sector-specific innovations |
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Numerical modeling of heat exchange and unsaturated–saturated flow in porous media |
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Kačur, Jozef |
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Growth and welfare implications of sector-specific innovations |
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Kačur, Jozef |
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10.1016/j.camwa.2018.06.009 |
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330 |
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numerical modeling of heat exchange and unsaturated–saturated flow in porous media |
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Numerical modeling of heat exchange and unsaturated–saturated flow in porous media |
| abstract |
We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. |
| abstractGer |
We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. |
| abstract_unstemmed |
We discuss the numerical modeling of heat and mass transport in unsaturated–saturated porous media. The heat is transported by infiltrated water underlying capillary and gravitation driven forces. Heat energy is governed by molecular diffusion, convection, dispersion and exchange between the infiltrated water and porous media matrix. An unsaturated–saturated flow is considered with boundary conditions reflecting the external driven forces. The presented mathematical model is motivated by analysis of hygrothermal isolation properties of facades. The main contribution is focused on the determination of model parameters including soil parameters, dispersion coefficients, thermal transmission coefficient, thermal conductivity of porous media matrix and external transmission coefficients. The used mathematical model does not include the vapor transport and its phase exchange with water due to vaporization and condensation. It will be the next step of our research. Thus, practical applications of our model are limited. The developed numerical method is a good candidate for solving corresponding inverse problems. Numerical experiments support our method. |
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Numerical modeling of heat exchange and unsaturated–saturated flow in porous media |
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https://doi.org/10.1016/j.camwa.2018.06.009 |
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Mihala, Patrik Tóth, Michal |
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2024-07-06T18:58:10.240Z |
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