期刊
AQUATIC GEOCHEMISTRY
卷 27, 期 3, 页码 207-220出版社
SPRINGER
DOI: 10.1007/s10498-021-09396-0
关键词
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资金
- NSF Geobiology and Low-Temperature Geochemistry grant [EAR1826940]
- NASA Earth and Space Science Fellowship [NNX15AR62H]
- Agouron Institute Geobiology Postdoctoral Fellowship
- NSF Chemical Oceanography [OCE-1558738]
- NASA [NNX15AR62H, 803015] Funding Source: Federal RePORTER
Recent studies have revealed the potential interaction between Mn and nitrogen species, shedding light on the abiotic oxidation mechanism of nitrite by Mn(III)-pyrophosphate under environmentally relevant conditions. The reaction involves two one-electron transfer steps and shows that nitrous acid serves as the reductant in the process, leading to the formation of nitrate as the end-product. This work provides a mechanistic perspective on the important relationship between Mn and nitrogen in environmental settings.
Given their environmental abundances, it has been long hypothesized that geochemical interactions between reactive forms of manganese and nitrogen may play important roles in the cycling of these elements. Indeed, recent studies have begun shedding light on the possible role of soluble, ligand-bound Mn(III) in promoting abiotic transformations under environmentally relevant conditions. Here, using the kinetic data of Karolewski et al. (Geochim Cosmochim Acta 293:365-378, 2021), we provide the chemical mechanism for the abiotic oxidation of nitrite (NO2-) by Mn(III)-pyrophosphate, (MnPP)-P-III, to form nitrate (NO3-). Nitrous acid (HNO2), not NO2-, is the reductant in the reaction, based on thermodynamic and kinetic considerations. As soluble Mn(III) complexes react in a one-electron transfer reaction, two one-electron transfer steps must occur. In step one, HNO2 is first oxidized to nitrogen dioxide, center dot NO2, a free radical via a hydrogen atom transfer (HAT) reaction. We show that this inner sphere reaction process is the rate-limiting step in the reaction sequence. In step two, center dot NO2 reacts with a second (MnPP)-P-III complex to form the nitronium ion (NO2+), which is isoelectronic with CO2. Unlike the poor electron-accepting capability of CO2, NO2+ is an excellent electron acceptor for both OH- and H2O, so NO2+ reacts quickly with water to form the end-product NO3- (step 3 in the reaction sequence). Thus, water provides the O atom in this nitrification reaction in accordance with the O-isotope data. This work provides mechanistic perspective on a potentially important interaction between Mn and nitrogen species, thereby offering a framework in which to interpret kinetic and isotopic data and to further investigate the relevance of this reaction under environmental conditions.
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