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Seasonal photochemical transformations of nitrogen species in a forest stream and lake.
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- Author(s): Porcal P;Porcal P; Kopáček J; Kopáček J; Tomková I; Tomková I
- Source:
PloS one [PLoS One] 2014 Dec 31; Vol. 9 (12), pp. e116364. Date of Electronic Publication: 2014 Dec 31 (Print Publication: 2014).- Publication Type:
Journal Article; Research Support, Non-U.S. Gov't- Language:
English - Source:
- Additional Information
- Source: Publisher: Public Library of Science Country of Publication: United States NLM ID: 101285081 Publication Model: eCollection Cited Medium: Internet ISSN: 1932-6203 (Electronic) Linking ISSN: 19326203 NLM ISO Abbreviation: PLoS One Subsets: MEDLINE
- Publication Information: Original Publication: San Francisco, CA : Public Library of Science
- Subject Terms:
- Abstract: The photochemical release of inorganic nitrogen from dissolved organic matter is an important source of bio-available nitrogen (N) in N-limited aquatic ecosystems. We conducted photochemical experiments and used mathematical models based on pseudo-first-order reaction kinetics to quantify the photochemical transformations of individual N species and their seasonal effects on N cycling in a mountain forest stream and lake (Plešné Lake, Czech Republic). Results from laboratory experiments on photochemical changes in N speciation were compared to measured lake N budgets. Concentrations of organic nitrogen (Norg; 40-58 µmol L-1) decreased from 3 to 26% during 48-hour laboratory irradiation (an equivalent of 4-5 days of natural solar insolation) due to photochemical mineralization to ammonium (NH4+) and other N forms (Nx; possibly N oxides and N2). In addition to Norg mineralization, Nx also originated from photochemical nitrate (NO3-) reduction. Laboratory exposure of a first-order forest stream water samples showed a high amount of seasonality, with the maximum rates of Norg mineralization and NH4+ production in winter and spring, and the maximum NO3- reduction occurring in summer. These photochemical changes could have an ecologically significant effect on NH4+ concentrations in streams (doubling their terrestrial fluxes from soils) and on concentrations of dissolved Norg in the lake. In contrast, photochemical reactions reduced NO3- fluxes by a negligible (<1%) amount and had a negligible effect on the aquatic cycle of this N form.
- References: Water Res. 2001 Oct;35(15):3688-96. (PMID: 11561631)
Environ Sci Technol. 2006 Jun 15;40(12):3775-81. (PMID: 16830541)
J Environ Monit. 2009 May;11(5):1064-71. (PMID: 19436866)
Anal Sci. 2004 Jan;20(1):153-8. (PMID: 14753275)
Sci Total Environ. 2003 Jul 1;310(1-3):73-85. (PMID: 12812732) - Accession Number: E1UOL152H7 (Iron)
N762921K75 (Nitrogen) - Publication Date: Date Created: 20150101 Date Completed: 20160112 Latest Revision: 20181113
- Publication Date: 20240104
- Accession Number: PMC4281116
- Accession Number: 10.1371/journal.pone.0116364
- Accession Number: 25551441
- Source:
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