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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2019-01-01
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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 |
work_keys_str_mv |
AT margalefmartirosanna isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals AT carreyraul isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals AT soleralbert isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals AT oteroneus isotopicfractionationassociatedtonitrateattenuationbyferrousironcontainingminerals |
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