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4th EucheMs chemistry congress

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Poster Session 1<br />

s923<br />

chem. Listy 106, s587–s1425 (2012)<br />

Poster session 1 - Environmental Radio<strong>chemistry</strong><br />

P - 0 1 2 6<br />

urAniuM SorPtion And AMS MeASureMentS<br />

i. SPendLiKovA 1 , M. neMeC 1 , f. SeBeStA 1 ,<br />

P. Steier 2 , G. wALLner 3<br />

1 Czech Technical University in Prague, Department of Nuclear<br />

Chemistry, Prague 1, Czech Republic<br />

2 University of Vienna, Vera Laboratory, Vienna, Austria<br />

3 University of Vienna, Department of Inorganic Chemistry,<br />

Vienna, Austria<br />

The uranium separation from natural waters was studied at<br />

the Department of Nuclear Chemistry in late 80’s and early 90’s.<br />

TiO-PAN sorbent (titanium dioxide embedded in<br />

polyacrylonitrile) showed high sorption capacity for this element.<br />

This composite sorbent is planned to be used for uranium<br />

preconcentration for measuring environmental 236U/U ratios by<br />

Acceleration Mass Spectrometry (AMS) in bilateral cooperation<br />

with the University of Vienna. After the preliminary AMS results<br />

showing anthropogenic contamination in TiO-PAN sorbent, the<br />

preparation of titanium oxide was studied with a strong emphasis<br />

on elimination of this contamination. Several samples of titanium<br />

oxide were prepared from an organic uranium-free compound.<br />

These samples were studied using X-Ray Diffraction for their<br />

crystal structure and using selective sorption of nitrogen gas for<br />

their specific surface area. Their sorption properties were also<br />

evaluated.<br />

Presently we are focusing on finding a water source which<br />

is not anthropogenically contaminated in order to use this water<br />

for further experiments and on the following separation and<br />

concentration steps for AMS sample preparation.<br />

Keywords: uranium; titanium oxide;<br />

4 th <strong>EucheMs</strong> <strong>chemistry</strong> <strong>congress</strong><br />

P - 0 1 2 7<br />

retention ProCeSSeS of SeLeniuM SPeCieS on<br />

CzeCh GrAnitiC roCK<br />

K. videnSKA 1 , v. hAvLovA 2<br />

1 Institute of Chemical Technology, Analytical Chemistry,<br />

Prague, Czech Republic<br />

2 Nuclear Research Institute Rez, Waste Management & Fuel<br />

Cycle Chemistry, Rez, Czech Republic<br />

Selenium (Se-79, T = 6.5·10 1/2 4yrs) belongs among fission<br />

products with long lifetime, high mobility and prevailing anionic<br />

character. Retention of selenium depends on its oxidation state<br />

therefore knowledge of migration behaviour under different<br />

conditions can significantly improve input into performance and<br />

safety assessment models.<br />

Granite is considered as a potential host rock for deep<br />

geological disposal of radioactive waste in several countries,<br />

including Czech Republic. Considering that, retention processes<br />

of selenium species on granitic rock were investigated using<br />

sorption and diffusion experiments. Granitic rock from Melechov<br />

massive (Centre Bohemian Massive, Czech Republic) was used<br />

as a representative for crystalline rock material.<br />

The sorption batch experiments were conducted on the<br />

crushed granite, which was sieved into several fractions with<br />

defined grain size. Mineral composition of each granitic fraction<br />

was evaluated using X-ray diffraction. The through-diffusion<br />

experiments were conducted on the granitic discs of the same<br />

origin (Melechov Massive, average 50 mm, and length 10 mm).<br />

Granitic discs were saturated with experimental tracer solution<br />

Na SeO or Na SeO . Afterwards they were placed into diffusion<br />

2 3 2 4<br />

cells. Due the saturation we can directly observed steady state<br />

diffusion processes.<br />

The X-ray diffraction results showed differences in mineral<br />

composition of granitic fractions (different content of quartz,<br />

feldspar, plagioclase, mica, chlorite, kaolinite). The<br />

enrichment/depletion, namely concerning Fe containing phases<br />

(micas) can influence the extent of both sorption and diffusion of<br />

observed tracers.<br />

Sorption experiments revealed that retention of selenite was<br />

higher then sorption of selenate. Granitic fractions enriched in<br />

mica indicated increased affinity to selenite. However, presence<br />

of mica did not influence sorption behaviour of selenate. The<br />

diffusion experiments suggested similar trend: selenite exhibited<br />

lower diffusion movement through rock samples in comparison<br />

with selenate. Selenate was proved to be rather mobile, almost<br />

non-sorbing specie.<br />

Acknowledgement: This research was supported by project of<br />

Ministry of Trade and Industry FR-TI1/362.<br />

Keywords: selenium; granite; retention;<br />

AUGUst 26–30, 2012, PrAGUE, cZEcH rEPUbLIc

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