Experimental and numerical investigation of water freezing and thawing in fully saturated sand
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68407700%3A21110%2F24%3A00376803" target="_blank" >RIV/68407700:21110/24:00376803 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/68407700:21340/24:00376803
Výsledek na webu
<a href="https://doi.org/10.2478/johh-2024-0018" target="_blank" >https://doi.org/10.2478/johh-2024-0018</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.2478/johh-2024-0018" target="_blank" >10.2478/johh-2024-0018</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Experimental and numerical investigation of water freezing and thawing in fully saturated sand
Popis výsledku v původním jazyce
This paper presents an experimental and numerical study of the freezing-thawing behavior of water in fully saturated sand. A relatively inexpensive and easily replicable experimental procedure was developed to simulate the freezing-thawing cycles in a medium-sized sand sample placed in a modified commercial freezer. By insulating the sides and bottom of the sample well, while allowing good thermal conductivity at the top of the sample, a nearly vertical advance of the freezing and thawing front was achieved. A series of freeze-thaw cycles were performed with higher and lower temperature gradients. A numerical multiphysics model, assuming an axially symmetric geometry based on the transient heat transfer during the phase transition, used a parametric approach to estimate the effective thermal properties of the sand-water-ice system. A good agreement between experimental and modelling results was shown, but slightly different parameter sets were obtained for each temperature gradient. The presented method could be a simple way to characterize the freeze-thaw process in natural and artificial porous materials.
Název v anglickém jazyce
Experimental and numerical investigation of water freezing and thawing in fully saturated sand
Popis výsledku anglicky
This paper presents an experimental and numerical study of the freezing-thawing behavior of water in fully saturated sand. A relatively inexpensive and easily replicable experimental procedure was developed to simulate the freezing-thawing cycles in a medium-sized sand sample placed in a modified commercial freezer. By insulating the sides and bottom of the sample well, while allowing good thermal conductivity at the top of the sample, a nearly vertical advance of the freezing and thawing front was achieved. A series of freeze-thaw cycles were performed with higher and lower temperature gradients. A numerical multiphysics model, assuming an axially symmetric geometry based on the transient heat transfer during the phase transition, used a parametric approach to estimate the effective thermal properties of the sand-water-ice system. A good agreement between experimental and modelling results was shown, but slightly different parameter sets were obtained for each temperature gradient. The presented method could be a simple way to characterize the freeze-thaw process in natural and artificial porous materials.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
20101 - Civil engineering
Návaznosti výsledku
Projekt
<a href="/cs/project/GA21-09093S" target="_blank" >GA21-09093S: Vícefázové proudění, transport a změny struktury zeminy související se zamrzáním a rozmrzáním vody v podpovrchových vrstvách</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2024
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Hydrology and Hydromechanics
ISSN
0042-790X
e-ISSN
1338-4333
Svazek periodika
72
Číslo periodika v rámci svazku
3
Stát vydavatele periodika
SK - Slovenská republika
Počet stran výsledku
13
Strana od-do
336-348
Kód UT WoS článku
001292068500007
EID výsledku v databázi Scopus
2-s2.0-85201731648