Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals

Biotic and abiotic laboratory experiments of nitrate and nitrite reduction by Fe-containing minerals were performed and the isotopic fractionation of the different reactions was calculated in order to determine whether it is possible to distinguish biotic and abiotic reactions involving N compounds....

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Main Authors: Margalef-Marti Rosanna, Carrey Raul, Soler Albert, Otero Neus
Format: Article
Language:English
Published: EDP Sciences 2019-01-01
Series:E3S Web of Conferences
Online Access:https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_12013.pdf
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spelling doaj-f1ea3f611b76440a9b8986de8f2cdb152021-02-02T05:38:25ZengEDP SciencesE3S Web of Conferences2267-12422019-01-01981201310.1051/e3sconf/20199812013e3sconf_wri-162018_12013Isotopic fractionation associated to nitrate attenuation by ferrous iron containing mineralsMargalef-Marti Rosanna0Carrey Raul1Soler Albert2Otero NeusGrup MAIMA, SGR Mineralogia Aplicada, Geoquímica i Geomicrobiologia, Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona (UB)Grup MAIMA, SGR Mineralogia Aplicada, Geoquímica i Geomicrobiologia, Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona (UB)Grup MAIMA, SGR Mineralogia Aplicada, Geoquímica i Geomicrobiologia, Departament de Mineralogia, Petrologia i Geologia Aplicada, Facultat de Ciències de la Terra, Universitat de Barcelona (UB)Biotic and abiotic laboratory experiments of nitrate and nitrite reduction by Fe-containing minerals were performed and the isotopic fractionation of the different reactions was calculated in order to determine whether it is possible to distinguish biotic and abiotic reactions involving N compounds. Results of biotic experiments showed nitrate reduction up to 96 % with transient NO2- accumulation and no significant N2O production. No significant nitrate attenuation was observed in abiotic nitrate reduction experiments. Abiotic experiments of nitrite reduction showed a rapid decrease in nitrite concentrations in those experiments with added Fe2+ coupled with a significant N2O production. Preliminary results of the N and O isotopic fractionation of the biotic experiments of nitrate reduction show differences in the ε15NNO3 and ε18ONO3 when different minerals were added. The abiotic experiments of nitrite reduction contrarily, showed similar ε15NNO2 in all the experiments.https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_12013.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Margalef-Marti Rosanna
Carrey Raul
Soler Albert
Otero Neus
spellingShingle Margalef-Marti Rosanna
Carrey Raul
Soler Albert
Otero Neus
Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
E3S Web of Conferences
author_facet Margalef-Marti Rosanna
Carrey Raul
Soler Albert
Otero Neus
author_sort Margalef-Marti Rosanna
title Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
title_short Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
title_full Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
title_fullStr Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
title_full_unstemmed Isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
title_sort isotopic fractionation associated to nitrate attenuation by ferrous iron containing minerals
publisher EDP Sciences
series E3S Web of Conferences
issn 2267-1242
publishDate 2019-01-01
description Biotic and abiotic laboratory experiments of nitrate and nitrite reduction by Fe-containing minerals were performed and the isotopic fractionation of the different reactions was calculated in order to determine whether it is possible to distinguish biotic and abiotic reactions involving N compounds. Results of biotic experiments showed nitrate reduction up to 96 % with transient NO2- accumulation and no significant N2O production. No significant nitrate attenuation was observed in abiotic nitrate reduction experiments. Abiotic experiments of nitrite reduction showed a rapid decrease in nitrite concentrations in those experiments with added Fe2+ coupled with a significant N2O production. Preliminary results of the N and O isotopic fractionation of the biotic experiments of nitrate reduction show differences in the ε15NNO3 and ε18ONO3 when different minerals were added. The abiotic experiments of nitrite reduction contrarily, showed similar ε15NNO2 in all the experiments.
url https://www.e3s-conferences.org/articles/e3sconf/pdf/2019/24/e3sconf_wri-162018_12013.pdf
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AT carreyraul isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals
AT soleralbert isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals
AT oteroneus isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals
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