Characterization of Phosphate Sequestration by a Lanthanum Modified Bentonite Clay: A Solid-State NMR, EXAFS, and PXRD Study

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Title: Characterization of Phosphate Sequestration by a Lanthanum Modified Bentonite Clay: A Solid-State NMR, EXAFS, and PXRD Study
Authors: Dithmer, Line, Lipton, Andrew S, Reitzel, Kasper, Warner, Terence Edwin, Lundberg, Daniel, Nielsen, Ulla Gro
Source: Dithmer, L, Lipton, A S, Reitzel, K, Warner, T E, Lundberg, D & Nielsen, U G 2015, ' Characterization of phosphate sequestration by a lanthanum modified bentonite clay: A solid-state NMR, EXAFS and PXRD study ', Environmental Science & Technology (Washington), vol. 49, no. 7, pp. 4559-4566 . https://doi.org/10.1021/es506182s
Publisher Information: American Chemical Society (ACS), 2015.
Publication Year: 2015
Subject Terms: Magnetic Resonance Spectroscopy, Lakes/chemistry, Aluminum Silicates/chemistry, Lanthanum/chemistry, Bentonite/chemistry, 02 engineering and technology, Eutrophication, 01 natural sciences, Phosphates, Lakes, X-Ray Absorption Spectroscopy, X-Ray Diffraction, Lanthanum, Phosphates/chemistry, Bentonite, Clay, Aluminum Silicates, Adsorption, 0210 nano-technology, Environmental Restoration and Remediation, 0105 earth and related environmental sciences
Description: Phosphate (Pi) sequestration by a lanthanum (La) exchanged clay mineral (La-Bentonite), which is extensively used in chemical lake restoration, was investigated on the molecular level using a combination of (31)P and (139)La solid state NMR spectroscopy (SSNMR), extended X-ray absorption spectroscopy (EXAFS), powder X-ray diffraction (PXRD) and sorption studies. (31)P SSNMR show that all Pi was immobilized as rhabdophane (LaPO4·n H2O, n ≤ 3), which was further supported by (139)La SSNMR and EXAFS. However, PXRD results were ambiguous with respect to rhabdophane and monazite (LaPO4). Adsorption studies showed that at dissolved organic carbon (DOC) concentration above ca. 250 μM the binding capacity was only 50% of the theoretical value or even less. No other La or Pi phases were detected by SSNMR and EXAFS indicating the effect of DOC is kinetic. Moreover, (31)P SSNMR showed that rhabdophane formed upon Pi sequestration is in close proximity to the clay matrix.
Document Type: Article
Language: English
ISSN: 1520-5851
0013-936X
DOI: 10.1021/es506182s
Access URL: https://pubmed.ncbi.nlm.nih.gov/25747941
https://pubs.acs.org/doi/pdf/10.1021/es506182s
https://pubs.acs.org/doi/10.1021/es506182s
https://core.ac.uk/display/50704027
http://www.osti.gov/scitech/biblio/1182872-characterization-phosphate-sequestration-lanthanum-modified-bentonite-clay-solid-state-nmr-exafs-pxrd-study
https://jglobal.jst.go.jp/detail?JGLOBAL_ID=201502234531699866
https://portal.findresearcher.sdu.dk/da/publications/characterization-of-phosphate-sequestration-by-a-lanthanum-modifi-2
http://pubs.acs.org/doi/abs/10.1021/es506182s
https://portal.findresearcher.sdu.dk/da/publications/6f4668cd-2a8c-4e20-b39a-f218433760fe
https://doi.org/10.1021/es506182s
Accession Number: edsair.doi.dedup.....09a938847bab696d35fdcc764e278e63
Database: OpenAIRE
Description
Abstract:Phosphate (Pi) sequestration by a lanthanum (La) exchanged clay mineral (La-Bentonite), which is extensively used in chemical lake restoration, was investigated on the molecular level using a combination of (31)P and (139)La solid state NMR spectroscopy (SSNMR), extended X-ray absorption spectroscopy (EXAFS), powder X-ray diffraction (PXRD) and sorption studies. (31)P SSNMR show that all Pi was immobilized as rhabdophane (LaPO4·n H2O, n ≤ 3), which was further supported by (139)La SSNMR and EXAFS. However, PXRD results were ambiguous with respect to rhabdophane and monazite (LaPO4). Adsorption studies showed that at dissolved organic carbon (DOC) concentration above ca. 250 μM the binding capacity was only 50% of the theoretical value or even less. No other La or Pi phases were detected by SSNMR and EXAFS indicating the effect of DOC is kinetic. Moreover, (31)P SSNMR showed that rhabdophane formed upon Pi sequestration is in close proximity to the clay matrix.
ISSN:15205851
0013936X
DOI:10.1021/es506182s