Metal–organic complexes as a major sink for rare earth elements in soils
Petr S. Fedotov
A B E , Olga B. Rogova C , Rustam Kh. Dzhenloda A B and Vasily K. Karandashev A D
+ Author Affiliations
- Author Affiliations
A National University of Science and Technology ‘MISiS’, 4 Leninsky Prospect, Moscow 119049, Russia.
B V. I. Vernadsky Institute of Geochemistry and Analytical Chemistry, Russian Academy of Sciences, 19 Kosygin Street, Moscow 119991, Russia.
C V. V. Dokuchaev Soil Science Institute, 7 building 2 Pyzhevskiy Per, Moscow 119017, Russia.
D The Institute of Microelectronics Technology and High-Purity Materials, Russian Academy of Sciences, 6 Institution Street, Chernogolovka 142432, Russia.
E Corresponding author. Email: fedotov_ps@mail.ru
Environmental Chemistry 16(5) 323-332 https://doi.org/10.1071/EN18275
Submitted: 23 December 2018 Accepted: 25 March 2019 Published: 24 April 2019
Environmental context. The role of rare earth elements in soil–plant systems remains unclear. We use continuous-flow extraction, designed to mimic natural conditions while minimising artefacts, to study in vitro chemical fractionation of rare earth elements in soil. The study reveals a predominant association of rare earth elements and metal-organic complexes independent of soil type and contamination, and thereby provides valuable insights into the behaviour of these elements in soil–plant systems.
Abstract. The role of rare earth elements (REEs) in soil–plant systems has attracted increasing attention but still remains somewhat unclear. Along in vivo studies on the uptake of REEs by plants, in vitro chemical fractionation of REEs in soil according to their physicochemical mobility can offer additional insights into the behaviour of REEs. In the present work, the fractionation of REEs was studied with the example of background, aerially and hydrogenically contaminated soil samples using dynamic (continuous flow) extraction, which allows natural conditions to be mimicked and artefacts to be minimised. The eluents applied addressed exchangeable, specifically sorbed, bound to Mn oxides, bound to metal–organic complexes, and bound to amorphous and poorly ordered Fe/Al oxides fractions extractable by 0.05 M Ca(NO3)2, 0.43 M CH3COOH, 0.1 M NH2OH·HCl, 0.1 M K4P2O7 at pH 11, and 0.1 M (NH4)2C2O4 at pH 3.2 respectively. The distribution of trace metals (such as Pb, Cu, Zn, Ni) between separated fractions varies with sample and is dependent on the type of contamination. However, for all samples, the recoveries of REEs by pyrophosphate are surprisingly high, up to 40–45 % of their total concentrations in background and anthropogenically transformed floodplain soils. As compared to metal–organic complexes, the contents of REEs bound to Fe/Al oxides are fairly low, no more than 12 %. REEs in other fractions may be taken into consideration only for aerially contaminated soil. Such a predominant association of REEs and metal–organic complexes (i.e. humic and fulvic compounds) independent of the type of soil has not been reported before.
Additional keywords: dynamic extraction, fractionation.
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