A mechanism of abiotic immobilization of nitrate in forest ecosystems: the ferrous wheel hypothesis
Abstract
Forest soils, rather than woody biomass, are the dominant long‐term sink for N in forest fertilization studies and, by inference, for N from atmospheric deposition. Recent evidence of significant abiotic immobilization of inorganic‐N in forest humus layers challenges a previously widely held view that microbial processes are the dominant pathways for N immobilization in soil. Understanding the plant, microbial, and abiotic mechanisms of N immobilization in forest soils has important implications for understanding current and future carbon budgets. Abiotic immobilization of nitrate is particularly perplexing because the thermodynamics of nitrate reduction in soils are not generally favorable under oxic conditions. Here we present preliminary evidence for a testable hypothesis that explains abiotic immobilization of nitrate in forest soils. Because iron (and perhaps manganese) plays a key role as a catalyst, with Fe(II) reducing nitrate and reduced forms of carbon then regenerating Fe(II), we call this ‘the ferrous wheel hypothesis’. After nitrate is reduced to nitrite, we hypothesize that nitrite reacts with dissolved organic matter through nitration and nitrosation of aromatic ring structures, thus producing dissolved organic nitrogen (DON). In addition to ignorance about mechanisms of DON production, little is known about DON dynamics in soil and its fate within ecosystems. Evidence from leaching and watershed studies suggests that DON production and consumption may be largely uncoupled from seasonal biological processes, although biological processes ultimately produce the DOC and reducing power that affect DON formation and the entire N cycle. The ferrous wheel hypothesis includes both biological and abiological processes, but the reducing power of plant‐derived organic matter may build up over seasons and years while the abiotic reduction of nitrate and reaction of organic matter with nitrite may occur in a matter of seconds after nitrate enters the soil solution.
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The formation of complex organic macro-molecules (humus) may be promoted when a biochar is Fe- and Mn-nanoparticle-rich.
“The formation of complex organic macro-molecules (humus) may even be promoted when a biochar is Fe- and Mn-nanoparticle-rich (as the one used here) due to “ferrous wheel” type reactions73, alongside microbial activities2460.”
From Plant growth improvement mediated by nitrate capture in co-composted biochar (2015) · cites this paper as [73]
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BackgroundReview of denitrification in tropical and subtropical soils of terrestrial ecosystems
Xu, Y.-B., Xu, Z.-H., Cai, Z.-C., & Reverchon, F. (2013) · Journal of Soils and Sediments · doi:10.1007/s11368-013-0650-1 · Cited by 75
“This can be explained by the ferrous wheel hypothesis of (Davidson et al. 2003; Davidson et al. 2008), suggesting that anaerobic microsites promote favorable redox conditions for abiotic NO3 –N reduction.”
BackgroundNierop, K., Preston, C., & Verstraten, J. M. (2006) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2006.04.049 · Cited by 74 · see citing works
Wu, S.-H., Zhuang, G., Bai, Z., Cen, Y., Xu, S., Sun, H.-S., Han, X.-G., & Zhuang, X.-L. (2018) · Global Change Biology · doi:10.1111/gcb.14025 · Cited by 72 · see citing works
“The TOC and DON of the soil were measured following the methods of Davidson, Chorover, and Dail (2003).”
MethodWu, H., Dannenmann, M., Fanselow, N., Wolf, B., Yao, Z., Wu, X., Brüggemann, N., Zheng, X.-H., Han, X.-G., Dittert, K., et al. (2011) · Plant and Soil · doi:10.1007/s11104-010-0575-z · Cited by 72
“tion and N-stabilization in non-extractable organic pools (e. g. Davidson et al. 2003 ).”
BackgroundBarnes, R., Raymond, P., & Casciotti, K. (2008) · Biogeochemistry · doi:10.1007/s10533-008-9227-2 · Cited by 72 · see citing works
“dissolved organic nitrogen via reactions with dissolved organic material ( Davidson et al. 2003 ).”
BackgroundMitchell, M. J., Piatek, K., Christopher, S., Mayer, B., Kendall, C., & McHale, P. (2006) · doi:10.1007/s10533-005-4277-1 · Cited by 72
“Other studies have also suggested that even for upland soils that short periods of changing chemical oxidation/reduction conditions can influence NO 3 loss and retention (Davidson et al. 2003; Sickman et al. 2003).”
BackgroundBiotic and abiotic processes of nitrogen immobilization in the soil-residue interface
Moritsuka, N., Yanai, J., Mori, K., & Kosaki, T. (2004) · Soil Biology and Biochemistry · doi:10.1016/j.soilbio.2004.02.024 · Cited by 72 · see citing works
Plant diversity, CO2, and N influence inorganic and organic N leaching in grasslands.
Dijkstra, F., West, J., Hobbie, S., Reich, P., & Trost, J. J. (2007) · Ecology · doi:10.1890/06-0733 · Cited by 71 · see citing works
“can form DON (Davidson et al. 2003), potentially increasing DON production and loss in the enriched N plots.”
BackgroundLutz, S., Trauth, N., Musolff, A., van Breukelen, B. V., Knöller, K., & Fleckenstein, J. (2020) · Water Resources Research · doi:10.1029/2019wr025528 · Cited by 70 · see citing works
“A mechanism that is potentially active during winter is the abiotic immobilization of NO3 − into soil organic matter following reaction with Fe2+ species (Davidson et al., 2003; McPhillips et al., 2015).”
BackgroundAbiotic nitrate incorporation in soil: is it real?
Colman, B. P., Fierer, N., & Schimel, J. (2007) · doi:10.1007/s10533-007-9111-5 · Cited by 68
“…at high concentrations (the recommended 5% HgCl2 is 0.18 M Hg2+) that may interfere with a proposed mechanism for abiotic NO3 – incorporation that depends on redox chemistry (Adamson 1952; Hush et al. 1960; Raposo et al. 2000), such as the hypothesized ‘‘ferrous wheel’’ of Davidson et al. (2003).”
BackgroundInfluentialSleutel, S., Vandenbruwane, J., Schrijver, A. D., Wuyts, K., Moeskops, B., Verheyen, K., & Neve, S. D. (2009) · doi:10.5194/bgd-6-7133-2009 · Cited by 68
“Davidson et al. (2003) described an abiotic mechanism10 producing DON through reaction of nitrite with DOM.”
Providoli, I., Bugmann, H., Siegwolf, R., Buchmann, N., & Schleppi, P. (2006) · doi:10.1016/j.soilbio.2005.11.019 · Cited by 66
Taylor, A., & Bottomley, P. (2006) · doi:10.1016/j.soilbio.2005.08.001 · Cited by 66
Saunders, T. J., McClain, M., & Llerena, C. (2006) · doi:10.1002/hyp.6215 · Cited by 65
“Although not directly investigated during any previous field study, the abiotic immobilization of NO3� to DON ( Davidson et al., 2003 ), if functioning within the catchment, could also play a role in NO3� immobilization.”
InfluentialBeidler, K. V., & Pritchard, S. G. (2017) · Plant and Soil · doi:10.1007/s11104-017-3393-8 · Cited by 64 · see citing works
“As plant materials decay, microbial enzymes depolymerize organic substrates, potentially forming reactive amino and phenol groups that can also condense into nitrogen-rich complexes (Haider et al. 1965; Kelley and Stevenson 1996; Davidson et al. 2003; Berg and McClaugherty 2008).”
BackgroundPan, F.-F., Yu, W.-T., Ma, Q., Zhou, H., Jiang, C.-M., Xu, Y.-G., & Ren, J.-F. (2017) · Biology and Fertility of Soils · doi:10.1007/s00374-017-1177-1 · Cited by 64
“Abiotic processes in soil also play an important role in N retention and supply (Davidson et al. 2003; Moritsuka et al. 2004).”
BackgroundZhu, X.-M., Chen, H., Zhang, W., Huang, J., Fu, S.-L., Liu, Z., & Mo, J. (2015) · Plant and Soil · doi:10.1007/s11104-015-2676-1 · Cited by 64
“The by-products of these processes then react with inorganic N to form more resistant compounds (Davidson et al. 2003).”
BackgroundSihi, D., Davidson, E., Savage, K., & Liang, D. (2019) · Global Change Biology · doi:10.1111/gcb.14855 · Cited by 63 · see citing works
Self-citationClark, C., Hobbie, S., Venterea, R., & Tilman, D. (2009) · Global Change Biology · doi:10.1111/j.1365-2486.2008.01811.x · Cited by 62 · see citing works
“Although speculative, we suspect that the sandy soils and low productivity at our site indicate a low potential for N retention via either biotic or abiotic mechanisms (Aber et al., 1998; Kaye et al., 2002; Davidson et al., 2003).”
BackgroundSoil Nitrogen Cycling following Montane Forest Conversion in Central Sulawesi, Indonesia
Corre, M., Dechert, G., & Veldkamp, E. (2006) · doi:10.2136/sssaj2005.0061 · Cited by 62
“Recently, this fast NO32 reaction is considered as a possible mechanism contributing to N retention in temperate ecosystems ( Davidson et al., 2003 ).”
BackgroundFang, H., Yu, G.-R., Cheng, S.-L., Zhu, T., Zheng, J.-J., Mo, J., Yan, J., & Luo, Y.-Q. (2011) · doi:10.1007/s10533-010-9438-1 · Cited by 57
“Based on long-term N addition experiments, soils, rather than plants, are the dominant long-term N sink from atmospheric deposition (Nadelhoffer et al. 1999; Davidson et al. 2003; Lohse and Matson 2005).”
BackgroundWestbrook, C., & Devito, K. (2004) · Biogeochemistry · doi:10.1023/b:biog.0000025739.04821.8e · Cited by 55 · see citing works
“It is likely that a large portion of this lost extractable N was due to abiotic processes (Dail et al. 2001; Davidson et al. 2003 ), but further investigation is needed to determine the exact quantities.”
BackgroundTang, Z.-S., Deng, L., An, H., Yan, W., & Shangguan, Z.-P. (2017) · Ecological Engineering · doi:10.1016/j.ecoleng.2016.11.039 · Cited by 54 · see citing works
Beaver Ponds: Resurgent Nitrogen Sinks for Rural Watersheds in the Northeastern United States.
Lazar, J. G., Addy, K., Gold, A., Groffman, P., Mckinney, R., & Kellogg, D. Q. (2015) · Journal of Environmental Quality · doi:10.2134/jeq2014.12.0540 · Cited by 54 · see citing works
High Nitrate Retention during Winter in Soils of the Hubbard Brook Experimental Forest
Judd, K., Likens, G., & Groffman, P. (2007) · Ecosystems · doi:10.1007/s10021-007-9027-x · Cited by 54
Denitrification is the major nitrous acid production pathway in boreal agricultural soils
Bhattarai, H., Wanek, W., Siljanen, H., Ronkainen, J., Liimatainen, M., Hu, Y., Nykänen, H., Biasi, C., & Maljanen, M. (2021) · Communications Earth & Environment · doi:10.1038/s43247-021-00125-7 · Cited by 53
- Authors
- Davidson, E. A., Chorover, J., & Dail, D. B.
- Affiliations
- Woodwell Climate Research Center (US)
- University of Arizona (US)
- University of Maine (US)
- Corresponding author
- Davidson, Eric A.
- Venue
- Global Change Biology
- Publisher
- Wiley
- Published
- 2003-02
- Volume
- 9
- Issue
- 2
- Pages
- 228-236
- ISSN
- 1354-1013 (ISSN-L)
- 1365-2486
- OpenAlex
- W2145062256
- Cited by
- 333
- References
- 65
- Citations by year
- 2026: 6 · 2025: 8 · 2024: 6 · 2023: 12 · 2022: 8 · 2021: 15 · 2020: 12 · 2019: 16 · 2018: 14 · 2017: 17 · 2016: 20 · 2015: 18 · 2014: 13 · 2013: 11 · 2012: 14
- FWCI
- 29.82
- Type
- journal article
- Language
- en
- Open access
- closed
- Locations
- Global Change Biology (publishedVersion)
- Funders
- National Science Foundation
- Pennsylvania State University
- Topics
- Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil Carbon and Nitrogen Dynamics
- Physical Sciences › Environmental Science › Environmental Chemistry › Soil and Water Nutrient Dynamics
- Life Sciences › Agricultural and Biological Sciences › Plant Science › Plant nutrient uptake and metabolism
- Keywords
- forest soils, dissolved organic nitrogen, dissolved organic matter, nitrogen cycling, forest humus, atmospheric nitrogen deposition
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