Modes of occurrence of rare earth elements in peat from Western Siberia

Modes of occurrence of rare earth elements in peat from Western Siberia

מידע ביבליוגרפי
Parent link:Journal of Geochemical Exploration
Vol. 184, pt. A.— 2017.— [P. 40-48]
מחברים אחרים: Arbuzov S. I. Sergey Ivanovich, Maslov S. G. Stanislav Grigorevich, Finkelman R. B. Robert Barr, Mezhibor A. M. Antonina Mikhailovna, Iljenok (Il'enok) S. S. Sergey Sergeevich, Blokhin M. G. Maksim Gennadjevich, Peregudina E. V. Elena Vladimirovna
סיכום:Title screen
Selective leaching of rare earth elements (REE) from peat samples from Western Siberia indicates unanticipated modes of r occurrence. It has been determined that from 40 to 80% of the total REE in the peat is accounted for in the hydrolyzable and water-soluble substances, 10–30% of the REE is concentrated in humic acids. Minerals in peat play a minor role in the accumulation of REE. In general, no > 25% of REE is accounted for in mineral association. Among the mineral forms of REE in peat, clastogenic phosphates (monazite, xenotime, crandallite group) and zircon are the dominant hosts. REE are distributed in different phases of the peat: the water-soluble and hydrolyzable substances are relatively enriched in light REE, and humic substances are enriched in heavy REE.
Режим доступа: по договору с организацией-держателем ресурса
שפה:אנגלית
יצא לאור: 2017
נושאים:
электронный ресурс
труды учёных ТПУ
peat
rare earth elements
modes of occurrence
conditions of peat formation
торф
редкоземельные элементы
возникновение
формирование
גישה מקוונת:https://doi.org/10.1016/j.gexplo.2017.10.012
פורמט: אלקטרוני Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656700
תיאור
סיכום:Title screen
Selective leaching of rare earth elements (REE) from peat samples from Western Siberia indicates unanticipated modes of r occurrence. It has been determined that from 40 to 80% of the total REE in the peat is accounted for in the hydrolyzable and water-soluble substances, 10–30% of the REE is concentrated in humic acids. Minerals in peat play a minor role in the accumulation of REE. In general, no > 25% of REE is accounted for in mineral association. Among the mineral forms of REE in peat, clastogenic phosphates (monazite, xenotime, crandallite group) and zircon are the dominant hosts. REE are distributed in different phases of the peat: the water-soluble and hydrolyzable substances are relatively enriched in light REE, and humic substances are enriched in heavy REE.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1016/j.gexplo.2017.10.012

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