Competitive adsorption and photodegradation of salicylate and oxalate on goethite
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60461373%3A22310%2F11%3A43892495" target="_blank" >RIV/60461373:22310/11:43892495 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/61388955:_____/11:00359745
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.cattod.2010.11.083" target="_blank" >http://dx.doi.org/10.1016/j.cattod.2010.11.083</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.cattod.2010.11.083" target="_blank" >10.1016/j.cattod.2010.11.083</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Competitive adsorption and photodegradation of salicylate and oxalate on goethite
Popis výsledku v původním jazyce
This work deals with the competitive adsorption and photodegradation of salicylate and oxalate on alpha-FeOOH (goethite) which is a predominant crystalline modification of iron oxide present in sea sediment. pH is a crucial parameter in goethite photodissolution; therefore, by means of a pH stat titration, pH was kept constant during all experiments. For either acidic (pH 3) or neutral (pH 6) pH values oxalate is preferentially adsorbed on the goethite surface. Thus, in the presence of oxalate, adsorption of salicylate is suppressed and for oxalate concentration 2 mM is even negligible. Without oxalate the photodegradation of salicylate on goethite is negligible due to the short circuiting effect of photo-generated h(+) and e(-). When oxalate is present in the system photodissolution of goethite takes place, which results in the formation of OH radicals and photodegradation of salicylate. At pH 3 photodissolution of goethite is faster than at pH 6; oxalate disappears and salicylate pho
Název v anglickém jazyce
Competitive adsorption and photodegradation of salicylate and oxalate on goethite
Popis výsledku anglicky
This work deals with the competitive adsorption and photodegradation of salicylate and oxalate on alpha-FeOOH (goethite) which is a predominant crystalline modification of iron oxide present in sea sediment. pH is a crucial parameter in goethite photodissolution; therefore, by means of a pH stat titration, pH was kept constant during all experiments. For either acidic (pH 3) or neutral (pH 6) pH values oxalate is preferentially adsorbed on the goethite surface. Thus, in the presence of oxalate, adsorption of salicylate is suppressed and for oxalate concentration 2 mM is even negligible. Without oxalate the photodegradation of salicylate on goethite is negligible due to the short circuiting effect of photo-generated h(+) and e(-). When oxalate is present in the system photodissolution of goethite takes place, which results in the formation of OH radicals and photodegradation of salicylate. At pH 3 photodissolution of goethite is faster than at pH 6; oxalate disappears and salicylate pho
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
CH - Jaderná a kvantová chemie, fotochemie
OECD FORD obor
—
Návaznosti výsledku
Projekt
<a href="/cs/project/1M0577" target="_blank" >1M0577: Výzkumné centrum pro nanopovrchové inženýrství</a><br>
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2011
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Catalysis Today
ISSN
0920-5861
e-ISSN
—
Svazek periodika
161
Číslo periodika v rámci svazku
1
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
7
Strana od-do
221-227
Kód UT WoS článku
000287730900037
EID výsledku v databázi Scopus
—