Award Abstract # 1148459
Collaborative Research: Nitrate Reduction by Redox-modified Fe-bearing Clay Minerals

NSF Org: EAR
Division Of Earth Sciences
Recipient: UNIVERSITY OF ILLINOIS
Initial Amendment Date: July 31, 2012
Latest Amendment Date: July 31, 2012
Award Number: 1148459
Award Instrument: Standard Grant
Program Manager: Enriqueta Barrera
EAR
 Division Of Earth Sciences
GEO
 Directorate for Geosciences
Start Date: August 15, 2012
End Date: July 31, 2016 (Estimated)
Total Intended Award Amount: $280,000.00
Total Awarded Amount to Date: $280,000.00
Funds Obligated to Date: FY 2012 = $280,000.00
History of Investigator:
  • Joseph Stucki (Principal Investigator)
    jstucki@illinois.edu
Recipient Sponsored Research Office: University of Illinois at Urbana-Champaign
506 S WRIGHT ST
URBANA
IL  US  61801-3620
(217)333-2187
Sponsor Congressional District: 13
Primary Place of Performance: University of Illinois at Urbana-Champaign
IL  US  61820-7406
Primary Place of Performance
Congressional District:
13
Unique Entity Identifier (UEI): Y8CWNJRCNN91
Parent UEI: V2PHZ2CSCH63
NSF Program(s): Geobiology & Low-Temp Geochem
Primary Program Source: 01001213DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s):
Program Element Code(s): 729500
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Nitrate contamination in soils, sediments, and surface and ground water poses significant risks to human health and global environments. Even though much is known about nitrate degradation in soils, especially via microbiological pathways, a complete solution to this problem has been elusive. One missing piece to the puzzle which could be highly significant is the role played by iron-bearing soil clay minerals in promoting nitrate degradation. The long-term purpose of this project is to devise strategies for on-site or in-stream nitrate remediation using common clay minerals as the catalyst. Because the iron largely remains in the clay mineral it stays in place during the nitrate reaction and can, thus, be regenerated or cycled between its oxidized and reduced states to continue the nitrate reduction process.

Clay minerals are everywhere in nature. They make up a significant fraction of soils and of lake, river, and ocean sediments. Virtually all of these minerals contain iron, the electrical charge of which can be decreased (called 'reduction') by bacteria growing in and around them or increased (called 'oxidation') by atmospheric oxygen under well drained and well aerated conditions. This susceptibility to changes in electrical charge, which is known as an oxidation-reduction (redox) reaction, allows iron in the clay minerals to react with other chemical species which have a similar susceptibility to charge alteration. Nitrogen is one such element which, like iron, is susceptible to reduction or oxidation. Nitrate is a very common form of nitrogen and can be degraded or removed by redox reaction, which transform it into nitrite, atmospheric nitrogen, or ammonium, among other forms. A redox reaction between iron in the clay minerals and nitrate should be possible, but has never been investigated to any great extent. The purpose of this project is to test the hypothesis that clay minerals containing reduced iron can degrade nitrate to convert it to less harmful forms, include ammonium and atmospheric nitrogen. In this study, the clay minerals with be prepared by reacting them first with chemicals and bacteria to reduce the iron; then they will be treated chemically to make them more attractive for nitrate adsorption and reaction with the iron. The nitrogen species produced will be measured by an accelerated diffusion method, then the amount of nitrate changed to other species will be compared with the amount of oxidized and reduced iron before and after the reaction with nitrate.

Results will be presented at scientific conferences, published in scientific journals, and reported to NSF.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Joseph W. Stucki, Kai Su, Linda Pentráková, and Martin Pentrák "Methods for handling redox-sensitive smectite dispersions" Clay Minerals , v.49 , 2014 , p.359 10.1180/claymin.2014.049.3.02
KAI SUADI RADIANYAEL MISHAELLIZHONG YANGJOSEPH W. STUCKI "NITRATE REDUCTION BY REDOX-ACTIVATED,POLYDIALLYLDIMETHYLAMMONIUM-EXCHANGED FERRUGINOUS SMECTITE" Clays and Clay Minerals , v.60 , 2012 , p.464?472 10.1346/CCMN.2012.0600503
Linda Pentráková, Kai Su, Martin Pentrák, and Joseph W. Stucki "A review of microbial redox interactionswith structural Fe in clay minerals" Clay Minerals , v.48 , 2013 , p.543 10.1180/claymin.2013.048.3.10
Martin Pentrák, Linda Pentráková, Adi Radian, Yael Mishael, Joseph W. Stucki "Nitrate reduction by redox-modified smectites exchanged with Chitosan" Clays and Clay Minerals , v.62 , 2014 , p.403 10.1346/CCMN.2014.0620504
Pentrak, M., Pentrakova, L., Radian, A., Mishael, Y. G., and Stucki, J. W. "Nitrate reduction by redox-modified smectites exchanged with chitosan." Clays and Clay Minerals , v.62 , 2014 , p.403 10.1346/CCMN.2014.0620504
Pentrakova, L., Su, K., Pentrak, M., and Stucki, J. W. "The 10th George Brown Lecture: A review of microbial redox interactions with structural Fe in clay minerals." Clay Minerals , v.48 , 2013 , p.543 10.1180/claymin.2013.048.3.10
Stucki, J. W., Su, K., Pentrak, M., and Pentrakova, L. "Methods for handling redox-sensitive smectite dispersions." Clay Minerals , v.49 , 2014 , p.473 10.1180/claymin.2014.049.3.02
Su, K., Radian, A., Mishael, Y., Yang, L., and Stucki, J. W. "Nitrate reduction by redox-activated, polydiallyldimethylammonium-exchanged ferruginous smectite." Clays and Clay Minerals , v.59 , 2012 , p.464 10.1346/CCMN.2012.0600503
Zhao, L., Dong, H., Kukkadapu, R. K., Zeng, Q., Edelmann, R. E., Pentrak, M., and Agrawal, A. "Biological redox cycling of iron in nontronite and its potential application in nitrate removal." Environmental Science and Technology , v.49 , 2015 , p.5493 10.1021/acs.est.5b00131

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

Overview

The long-term purpose of this project was to devise strategies for on-site or in-stream nitrate remediation using common, natural materials called clay minerals. The clay minerals have a very large surface area and are the most chemically active inorganic fraction of natural soils and sediments. They are also mined from pure deposits. This project studied their potential as a resource to eliminate nitrate from drinking water and lakes, rivers, and oceans. The unique contribution of this study was that it taught us how to attract nitrate to the surfaces of the clay minerals, which are normally not attracted due to like-charge repulsion (both are negatively charged), and how to convert them to less harmful forms once they were adsorbed at the surface. The conversion occurred by a redox reaction with the iron that is located in the clay crystal structure, in which the iron in its 2+ form, labeled iron(II), reacted with nitrate, converting it to nitrite, ammonium, and/or other products, and the iron changed to its 3+ form, labeled iron(III). An intermediate step was required to attract the nitrate, which was to reverse the charge on the clay mineral from negative to positive. This was done by adsorbing a large organic cation (positively charged ion) to the clay surfaces, which created a strong electrostatic attraction for the nitrate. We tested two large cations, one synthetic, named poly-diallyldimethylammonium (pDADMAC), and one natural, named chitosan. Both were very effective at attracting nitrate, but chitosan was preferred because it attracted more nitrate and it is derived from naturally occurring organisms.

Intellectual Merit

The specific objectives of the project were to: (1) Establish the baseline level of nitrate reduction by iron redox-modified clay minerals with no organic cation present. (2) Determine the effects of the organic cation (charge reversal) at the clay mineral surface on the reactivity of the redox-modified clay minerals toward nitrate. And (3) determine the distribution of nitrogen species between solid and solution phases. We analyzed both the solution and solid phases of and around the clay mineral after reaction with nitrate. We found nitrite in solution and nitrate, nitrite, and ammonium adsorbed to the solid phase. Further reaction would probably remove all of the nitrite from solution. We also analyzed the clay mineral crystals for iron(II) and iron(III) and confirmed that the nitrate had indeed converted some of the iron(II) to iron(III), confirming that a redox reaction had occurred.

Broader Impact

These results will have a broad impact on at least three branches of the water treatment industry. First, drinking water treatment plants current remove nitrate from the water, but instead of changing it they just transfer it back to the river or put it into a municipal waste water stream. The results from the present study indicate a way whereby the nitrate can be removed and eliminated. Second, agricultural fields receiving nitrate fertilizer generally are unable to retain and use all of it, so a good portion of it runs off the field into ditches and field tile drains. This water finds its way to rivers, lakes, and oceans, causing algae blooms and other unhealthy and unsightly consequences. The results from the present study will help us construct filters that can intercept that water in the ditches and streams and eliminate the nitrate from it. And third, water reclamation districts deal with municipal and industrial waste, but often do not do anything to remove nitrate from their discharge water. This could change with a straight-forward and inexpensive method for doing it. Results from this project suggest that it can be done with a filtration system based on reversed-charge, redox-activated clay minerals.


Last Modified: 10/13/2016
Modified by: Joseph W Stucki

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