Experimental evaluation of the influence of saturation media on the mineralogical and physicochemical stability of bentonites
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F13%3A10193059" target="_blank" >RIV/00216208:11310/13:10193059 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.1016/j.clay.2013.10.002" target="_blank" >http://dx.doi.org/10.1016/j.clay.2013.10.002</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.clay.2013.10.002" target="_blank" >10.1016/j.clay.2013.10.002</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Experimental evaluation of the influence of saturation media on the mineralogical and physicochemical stability of bentonites
Popis výsledku v původním jazyce
Three bentonite buffer materials (Rokle bentonite, FEBEX bentonite, and Mock-Up-CZ mixture composed of 85% Rokle bentonite, 10% silica sand and 5% graphite) interacted with natural water collected from Josef Underground Educational Facility (UEF) Czech Republic, and four different types of artificial groundwater enriched in K+ and/or Mg2+. The experimental material was prepared in the form of (1) highly compacted samples, (2) dispersion of bentonites (both at temperature of 95 degrees C), (3) drill holefilling during in situ tests at the Josef UEF (at ordinary temperature), and (4) common batch laboratory experiments (at 20 degrees C and at 80-90 degrees C). Partial samples were extracted after 3, 6, 12, and/or 18 months of interaction in the first three set-ups, and after 1 week, 2 weeks, 1 month, 2 months, 3 months, 4 months, 5 months, 7 months, 10 months, and 12 months in the batch experiment. Phase composition and its potential changes were evaluated by X-ray diffraction. In the f
Název v anglickém jazyce
Experimental evaluation of the influence of saturation media on the mineralogical and physicochemical stability of bentonites
Popis výsledku anglicky
Three bentonite buffer materials (Rokle bentonite, FEBEX bentonite, and Mock-Up-CZ mixture composed of 85% Rokle bentonite, 10% silica sand and 5% graphite) interacted with natural water collected from Josef Underground Educational Facility (UEF) Czech Republic, and four different types of artificial groundwater enriched in K+ and/or Mg2+. The experimental material was prepared in the form of (1) highly compacted samples, (2) dispersion of bentonites (both at temperature of 95 degrees C), (3) drill holefilling during in situ tests at the Josef UEF (at ordinary temperature), and (4) common batch laboratory experiments (at 20 degrees C and at 80-90 degrees C). Partial samples were extracted after 3, 6, 12, and/or 18 months of interaction in the first three set-ups, and after 1 week, 2 weeks, 1 month, 2 months, 3 months, 4 months, 5 months, 7 months, 10 months, and 12 months in the batch experiment. Phase composition and its potential changes were evaluated by X-ray diffraction. In the f
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
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Návaznosti
Z - Vyzkumny zamer (s odkazem do CEZ)<br>S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2013
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Applied Clay Science
ISSN
0169-1317
e-ISSN
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Svazek periodika
86
Číslo periodika v rámci svazku
DECEMBER
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
10
Strana od-do
1-10
Kód UT WoS článku
000328597100001
EID výsledku v databázi Scopus
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