Simulation of S-Entropy Production during the Transport of Non-Electrolyte Solutions in the Double-Membrane System
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27200%2F20%3A10245084" target="_blank" >RIV/61989100:27200/20:10245084 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.mdpi.com/1099-4300/22/4/463" target="_blank" >https://www.mdpi.com/1099-4300/22/4/463</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.3390/e22040463" target="_blank" >10.3390/e22040463</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Simulation of S-Entropy Production during the Transport of Non-Electrolyte Solutions in the Double-Membrane System
Popis výsledku v původním jazyce
Using the classical Kedem-Katchalsky' membrane transport theory, a mathematical model was developed and the original concentration volume flux (J(v)), solute flux (J(s)) characteristics, and S-entropy production by J(v), ((psi S)Jv) and by J(s) ((psi S)Js) in a double-membrane system were simulated. In this system, M-1 and M-r membranes separated the l, m, and r compartments containing homogeneous solutions of one non-electrolytic substance. The compartment m consists of the infinitesimal layer of solution and its volume fulfills the condition V-m -> 0. The volume of compartments l and r fulfills the condition V-l = V-r -> infinity. At the initial moment, the concentrations of the solution in the cell satisfy the condition C-l < C-m < C-r. Based on this model, for fixed values of transport parameters of membranes (i.e., the reflection (sigma(l), sigma(r)), hydraulic permeability (L-pl, L-pr), and solute permeability (omega(l), omega(r)) coefficients), the original dependencies C-m = f(C-l - C-r), J(v) = f(C-l - C-r), J(s) = f(C-l - C-r), (psi S)Jv = f(C-l - C-r), (psi S)Js = f(C-l - C-r), R-v = f(C-l - C-r), and R-s = f(C-l - C-r) were calculated. Each of the obtained features was specially arranged as a pair of parabola, hyperbola, or other complex curves.
Název v anglickém jazyce
Simulation of S-Entropy Production during the Transport of Non-Electrolyte Solutions in the Double-Membrane System
Popis výsledku anglicky
Using the classical Kedem-Katchalsky' membrane transport theory, a mathematical model was developed and the original concentration volume flux (J(v)), solute flux (J(s)) characteristics, and S-entropy production by J(v), ((psi S)Jv) and by J(s) ((psi S)Js) in a double-membrane system were simulated. In this system, M-1 and M-r membranes separated the l, m, and r compartments containing homogeneous solutions of one non-electrolytic substance. The compartment m consists of the infinitesimal layer of solution and its volume fulfills the condition V-m -> 0. The volume of compartments l and r fulfills the condition V-l = V-r -> infinity. At the initial moment, the concentrations of the solution in the cell satisfy the condition C-l < C-m < C-r. Based on this model, for fixed values of transport parameters of membranes (i.e., the reflection (sigma(l), sigma(r)), hydraulic permeability (L-pl, L-pr), and solute permeability (omega(l), omega(r)) coefficients), the original dependencies C-m = f(C-l - C-r), J(v) = f(C-l - C-r), J(s) = f(C-l - C-r), (psi S)Jv = f(C-l - C-r), (psi S)Js = f(C-l - C-r), R-v = f(C-l - C-r), and R-s = f(C-l - C-r) were calculated. Each of the obtained features was specially arranged as a pair of parabola, hyperbola, or other complex curves.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10700 - Other natural sciences
Návaznosti výsledku
Projekt
—
Návaznosti
N - Vyzkumna aktivita podporovana z neverejnych zdroju
Ostatní
Rok uplatnění
2020
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Entropy
ISSN
1099-4300
e-ISSN
—
Svazek periodika
22
Číslo periodika v rámci svazku
4
Stát vydavatele periodika
CH - Švýcarská konfederace
Počet stran výsledku
11
Strana od-do
—
Kód UT WoS článku
000537222600083
EID výsledku v databázi Scopus
—