The change of phase composition and the morphology of particles of hydrothermal titanosilicate precipitates during their aging

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During the study of phase formation under conditions of hydrothermal synthesis of alkaline titanosilicate systems (NH₄)₂TiO(SO₄)₂⋅H₂O или TiOSO₄⋅H₂O-Na₂SiO₃-NaOH-H₂O it was found that the formed titanosilicate solid phases differ both in composition and structure. The process of their aging under conditions of long-term exposure without forced heating is accompanied mainly by the loss of free water without noticeable structural and morphological changes. The exposure to the temperature of 70–100°С significantly accelerates the process of solid phase transformation. In these conditions, a porous system of particles is formed, which is confirmed by an increase in their specific surface area and total pore volume, as well as by an increase in the activity of the powders to absorb single- and double-charged cations. The effectiveness of hydrochloric acid treatment of fresh and especially aged precipitates on the ordering of the structure with the formation of crystals of a clear frame shape, inherent in the minerals zorite and ivanyukite, which contributes to increasing the sorption capacity of the final product is shown. The obtained results are used to adjust the technological regulations, which are used to test the technology of titanosilicate sorbent on the pilot plant.

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L. Gerasimova

Tananaev Institute of Chemistry – Subdivision of the Federal Research Centre “Kola Science Centre of the Russian Academy of Sciences”

编辑信件的主要联系方式.
Email: l.gerasimova@ksc.ru
俄罗斯联邦, 184209 Apatity, Murmansk region

E. Shchukina

Tananaev Institute of Chemistry – Subdivision of the Federal Research Centre “Kola Science Centre of the Russian Academy of Sciences”

Email: l.gerasimova@ksc.ru
俄罗斯联邦, 184209 Apatity, Murmansk region

A. Nikolaev

Tananaev Institute of Chemistry – Subdivision of the Federal Research Centre “Kola Science Centre of the Russian Academy of Sciences”

Email: l.gerasimova@ksc.ru

Corresponding Member of the RAS

俄罗斯联邦, 184209 Apatity, Murmansk region

S. Vinogradova

Tananaev Institute of Chemistry – Subdivision of the Federal Research Centre “Kola Science Centre of the Russian Academy of Sciences”

Email: l.gerasimova@ksc.ru
俄罗斯联邦, 184209 Apatity, Murmansk region

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2. Fig. 1. IR spectra of sorbent samples obtained from fresh sediments: STA-0-S (1), STM-0-S (2).

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3. Fig. 2. IR spectrum of a sorbent sample from aged sediment STA-P-S.

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4. Fig. 3. IR spectrum of a sorbent sample from aged sediment treated with HCl at T : L = 1 : 6, STA-P-S-2.

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5. Fig. 4. Diffraction patterns of sorbent samples: STA-0-S (1), STA-P-S (2), STA-P-S-1 (after treating the sorbent with a HCl solution, S : L = 1 : 3) (3), STA-P-S-2 (after treating the sorbent with a HCl solution, S : L = 1 : 6) (4). Designations: ● – zorite, × – ivanyukite.

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6. Fig. 5. Diffraction patterns of sorbent samples using STM: STM-0-S (1), STM-P-S (2), STM-P-S-1 (after treating the sorbent with a HCl solution, S : L = 1 : 3) (3), STM-P-S-2 (after treating the sorbent with a HCl solution, S : L = 1 : 6) (4). Designations: × – ivanyukite.

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7. Fig. 6. Diffraction patterns of sorbents obtained from aged titanosilicate sediments after their treatment with HCl solution: STA-P-1S (1), STA-P-2S (2), STM-P-1S (3), STM-P-2S (4). Designations: × – ivanyukite, o – zorite.

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8. Fig. 7. TEM image of sorbents: STA-O-S (a), STM-O-S (b).

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