Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy

The transport characteristics of iron nanoparticles prepared with a green tea, polyphenol-rich solution, were investigated for two granular media, pure silica sand and sand coated with aluminium hydroxide. The GT-nZVI injection caused a sharp decrease in the effluent pH and increase in the redox pot...

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Main Authors: M. Chrysochoou, M. Mcguire, G. Dahal
Format: Article
Language:English
Published: AIDIC Servizi S.r.l. 2012-07-01
Series:Chemical Engineering Transactions
Online Access:https://www.cetjournal.it/index.php/cet/article/view/7291
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spelling doaj-193f980188f34f228845fb9b9d05d3162021-02-22T21:07:13ZengAIDIC Servizi S.r.l.Chemical Engineering Transactions2283-92162012-07-012810.3303/CET1228021Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil MineralogyM. ChrysochoouM. McguireG. DahalThe transport characteristics of iron nanoparticles prepared with a green tea, polyphenol-rich solution, were investigated for two granular media, pure silica sand and sand coated with aluminium hydroxide. The GT-nZVI injection caused a sharp decrease in the effluent pH and increase in the redox potential, which is attributed to the presence of free Fe3+ and polyphenols in the suspension, respectively. The breakthrough curves for total Fe in the outflow indicated that some aggregation and deposition of nanoparticles occurred in both types of sand. However, the majority of the iron mass was detected in the outflow (73 % in the uncoated and 62 % in the coated sand), indicating good transport of the nanoparticles. XRF results indicated that no iron was retained on the Al-coated sand particles, while 4% of the injected Fe was deposited on the pure silica particles. This behaviour is attributed to the electrostatic interactions between the positively charged nanoparticles and the positively charged Al- coatings vs. negatively charged silica in the pH range of the experiments. The “missing” iron in the Al- coated sand columns was observed as a reddish brown precipitate in the 0.7 µm filter that was placed in the outflow of the columns; thus, increased agglomeration was observed compared to the pure silica sand columns. This study shows that soil geochemistry can have a significant effect on the transport characteristics of nanoparticles in porous media.https://www.cetjournal.it/index.php/cet/article/view/7291
collection DOAJ
language English
format Article
sources DOAJ
author M. Chrysochoou
M. Mcguire
G. Dahal
spellingShingle M. Chrysochoou
M. Mcguire
G. Dahal
Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy
Chemical Engineering Transactions
author_facet M. Chrysochoou
M. Mcguire
G. Dahal
author_sort M. Chrysochoou
title Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy
title_short Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy
title_full Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy
title_fullStr Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy
title_full_unstemmed Transport Characteristics of Green-Tea Nano-scale Zero Valent Iron as a Function of Soil Mineralogy
title_sort transport characteristics of green-tea nano-scale zero valent iron as a function of soil mineralogy
publisher AIDIC Servizi S.r.l.
series Chemical Engineering Transactions
issn 2283-9216
publishDate 2012-07-01
description The transport characteristics of iron nanoparticles prepared with a green tea, polyphenol-rich solution, were investigated for two granular media, pure silica sand and sand coated with aluminium hydroxide. The GT-nZVI injection caused a sharp decrease in the effluent pH and increase in the redox potential, which is attributed to the presence of free Fe3+ and polyphenols in the suspension, respectively. The breakthrough curves for total Fe in the outflow indicated that some aggregation and deposition of nanoparticles occurred in both types of sand. However, the majority of the iron mass was detected in the outflow (73 % in the uncoated and 62 % in the coated sand), indicating good transport of the nanoparticles. XRF results indicated that no iron was retained on the Al-coated sand particles, while 4% of the injected Fe was deposited on the pure silica particles. This behaviour is attributed to the electrostatic interactions between the positively charged nanoparticles and the positively charged Al- coatings vs. negatively charged silica in the pH range of the experiments. The “missing” iron in the Al- coated sand columns was observed as a reddish brown precipitate in the 0.7 µm filter that was placed in the outflow of the columns; thus, increased agglomeration was observed compared to the pure silica sand columns. This study shows that soil geochemistry can have a significant effect on the transport characteristics of nanoparticles in porous media.
url https://www.cetjournal.it/index.php/cet/article/view/7291
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