Issue 10, 2021

Abiotic reduction of nitrite by Fe(ii): a comparison of rates and N2O production

Abstract

Abiotic reduction of nitrite (NO2) by Fe(II) species (i.e., chemodenitrification) has been demonstrated in a variety of natural environments and laboratory studies, and is a potentially significant source of atmospheric nitrous oxide (N2O) emissions. It is, however, unclear how chemodenitrification rates and N2O yields vary among heterogeneous Fe(II) species under similar conditions and whether abiotic reduction competes with biological NO2 reduction. Here, we measured rates of NO2 reduction and extents of N2O production by several Fe(II) species under consistent, environmentally relevant conditions (i.e., pH 7.0, bicarbonate buffer, and 0.1 mM NO2). Nitrite reduction rates varied significantly among the heterogeneous Fe(II) species with half-lives (t1/2) ranging from as low as an hour to over two weeks following the trend of goethite/Fe(II) ∼ hematite/Fe(II) ∼ magnetites > maghemite/Fe(II) > sediment/Fe(II). Interestingly, we observed no clear trend of increasing NO2 reduction rates with higher magnetite stoichiometry (x = Fe2+/Fe3+). Nitrogen recovery as N2O also varied significantly among the Fe species ranging from 21% to 100% recovery. We further probed both chemodenitrification and biological denitrification in the absence and presence of added aqueous Fe(II) with a sediment collected from the floodplain of an agricultural watershed. While abiotic NO2 reduction by the sediment + Fe(II) was much slower than the laboratory Fe(II) species, we found near complete mass N balance during chemodenitrification, as well as evidence for both abiotic and biological NO2 reduction potentially occurring in the sediment under anoxic conditions. Our results suggest that in redox active sediments and soils both chemodenitrification and biological denitrification are likely to occur simultaneously, and that agricultural watersheds may be significant sources of N2O emissions.

Graphical abstract: Abiotic reduction of nitrite by Fe(ii): a comparison of rates and N2O production

Supplementary files

Article information

Article type
Paper
Submitted
07 jun 2021
Accepted
04 set 2021
First published
07 set 2021

Environ. Sci.: Processes Impacts, 2021,23, 1531-1541

Author version available

Abiotic reduction of nitrite by Fe(II): a comparison of rates and N2O production

T. C. Robinson, D. E. Latta, L. Notini, K. E. Schilling and M. M. Scherer, Environ. Sci.: Processes Impacts, 2021, 23, 1531 DOI: 10.1039/D1EM00222H

To request permission to reproduce material from this article, please go to the Copyright Clearance Center request page.

If you are an author contributing to an RSC publication, you do not need to request permission provided correct acknowledgement is given.

If you are the author of this article, you do not need to request permission to reproduce figures and diagrams provided correct acknowledgement is given. If you want to reproduce the whole article in a third-party publication (excluding your thesis/dissertation for which permission is not required) please go to the Copyright Clearance Center request page.

Read more about how to correctly acknowledge RSC content.

Social activity

Spotlight

Advertisements