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bibliography:
Pushkar’ov, O. V., Sevruk, I. M., Dolin, V. V.2019. Influence of
palygorskite structure on the adsorption of tritium from aqueous solutions. Geo&Bio,
18: 158–163. (In Ukrainian)
doi: https://doi.org/10.15407/gb1813
authors
(with orcid and affiliation):
Aleksandr Pushkarev
https://orcid.org/0000-0002-4382-8620
Institute
of Geochemistry of
Environment, NAS
of Ukraine (Kyiv, Ukraine)
Iryna Sevruk (Rudenko)
https://orcid.org/0000-0003-2407-0735
Institute
of Geochemistry of
Environment, NAS
of Ukraine (Kyiv, Ukraine)
Vitaliy Dolin
https://orcid.org/0000-0002-1962-9277
Institute
of Geochemistry of
Environment, NAS
of Ukraine (Kyiv, Ukraine)
pdf: pdf
summary:
The aim of the work
is to determine the possibility of using the palygorskite adsorbent in removing
tritium from protium-tritium water (HTO). The article is based on results of
experiments using palygorskite from the Cherkassy deposit (Ukraine) and
tritiated water ("HTO"). The performed studies evaluated the
adsorption of tritium from an aqueous solution and the effect of hydrogen isotope
fractionation in a stationary closed system "HTO-palygorskite". The
mechanisms of delaying the super heavy hydrogen isotope in the structure of a
natural clay mineral are explained. The ribbon-channel structure of
palygorskite provides the possibility of accumulating tritium in the raw
mineral up to 3.3 Bq × g-1 (or 9.19 × 10‑15 g / g). It is
established that the accumulation of tritium is a multistage process. It is
determined that the adsorption capacity of palygorskite is due to uncompensated
charges on the surface of mineral particles, the presence of zeolite and
coordinately bound water in the channels, where molecular HTO → H2O
exchange occurs between the mineral and tritiumated water, and also by ionic OT
→ OH substitution in the octahedral layers of the mineral. During surface
adsorption processes, due to their dynamic nature, the magnitude of adsorption,
that is, the delay of molecules by the surface is a kinetic factor that
determines the ratio of adsorbed and desorbed molecules. This creates
conditions for the possible fractionation of molecules with different molecular
masses (H2O and HTO), with the predominant retention on the
adsorption surface of mineral particles of more inertial NTO molecules. As a
result, up to 59 % of tritium absorbed by the mineral accumulates in the
surface adsorbed form in the original palygorskite. The distribution of tritium
is determined in four structural positions: in a surface-adsorbed, coordinately
bound, zeolite, and strongly bound forms. The predominance of a strongly bound
form (22 % of the total tritium content in the mineral) over channel water
was revealed. The rationality of using palygorskite for the accumulation of
tritium from aqueous solutions was determined.
Key words:
tritium,
hydrogen, heavy isotopes of hydrogen, palygorskite, adsorption, fractionation.
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