Role of Manganese Oxyhydroxides in the Transport of Rare Earth Elements Along a Groundwater Flow Path
Haiyan Liu,
Huaming Guo,
Olivier Pourret,
Yi Chen and
Rongxiao Yuan
Additional contact information
Haiyan Liu: School of Water Resources and Environmental Engineering, East China University of Technology, Nanchang 330013, China
Huaming Guo: State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China
Olivier Pourret: UniLaSalle, AGHYLE, 60026 Beauvais Cedex, France
Yi Chen: State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China
Rongxiao Yuan: State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China
IJERPH, 2019, vol. 16, issue 13, 1-20
Abstract:
Rare earth elements (REE) are known to be emerging contaminants in hydrosphere, but roles of hydrous manganese oxyhydroxides (HMO) in REE transport in groundwater remains unknown. In this study, groundwater was sampled along a flow path in the North China Plain to determine the behavior of REE surface complexation to HMO by a modeling and field study approach. Results show that the proportion of neodymium (Nd) complexed by HMO ranges from 0.2% to 95.8%, and from 0.3% to 99.6% in shallow groundwater and deep groundwater, respectively. The amount of complexed REE increases along the flow path. REE bound to HMO exhibit decreasing trends with increasing atomic number. The process was determined to be independent of pH, HMO content, and metal loading. This finding further demonstrates HMO-REE complexation plays a key role in transport of REE in groundwater through preferential scavenging of light REE (LREE) over heavy REE (HREE). Nevertheless, carbonate ligands appear to be robust competitors in reducing the amount of REE sorbed to HMO when solution pH rises above 8.0. Assuming that 50% of Mn concentration occurs as HMO, the amount of complexed REE was predicted to show a more marked decrease in LREE compared to that of HREE.
Keywords: Lanthanides; China; Sorption; Modeling; Aquifer; Cerium anomaly; Critical zone (search for similar items in EconPapers)
JEL-codes: I I1 I3 Q Q5 (search for similar items in EconPapers)
Date: 2019
References: View references in EconPapers View complete reference list from CitEc
Citations: View citations in EconPapers (1)
Downloads: (external link)
https://www.mdpi.com/1660-4601/16/13/2263/pdf (application/pdf)
https://www.mdpi.com/1660-4601/16/13/2263/ (text/html)
Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.
Export reference: BibTeX
RIS (EndNote, ProCite, RefMan)
HTML/Text
Persistent link: https://EconPapers.repec.org/RePEc:gam:jijerp:v:16:y:2019:i:13:p:2263-:d:243271
Access Statistics for this article
IJERPH is currently edited by Ms. Jenna Liu
More articles in IJERPH from MDPI
Bibliographic data for series maintained by MDPI Indexing Manager ().