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NRC Publications Archive Archives des publications du CNRCThis publication could be one of several versions: author's original, accepted manuscript or the publisher's version. / La version de cette publication peut être l'une des suivantes : la version prépublication de l'auteur, la version acceptée du manuscrit ou la version de l'éditeur. For the publisher's version, please access the DOI link below./ Pour consulter la version de l'éditeur, utilisez le lien DOI ci-dessous.http://dx.doi.org/10.1021/es301047dEnvironmental Science & Technology, 46, 11, pp. 6035-6040, 2012-05-07 Aerobic mineralization of Nitroguanidine by Variovorax strain VC1 isolated from soil Perreault, Nancy N.; Halasz, Annamaria; Manno, Dominic; Thiboutot, Sonia; Ampleman, Guy; Hawari, Jalal ABSTRACT: Nitroguanidine (NQ) is an energetic material that is used as a key ingredient of triple-base propellants and is currently being considered as a TNT replacement in explosive formulations. NQ was efficiently degraded in aerobic microcosms when a carbon source was added. NQ persisted in unamended microcosms or under anaerobic conditions. An aerobic NQ-degrading bacterium, Variovorax strain VC1, was isolated from soil microcosms containing NQ as the sole nitrogen source. NQ degradation was inhibited in the presence of a more favorable source of nitrogen. Resting cells of VC1 degraded NQ effectively (54 μmol h −1 g −1 protein) giving NH 3 (50.0%), nitrous oxide (N 2 O) (48.5%) and CO 2 (100%). Disappearance of NQ was accompanied by the formation of a key intermediate product that we identified as nitrourea by comparison with a reference material. Nitrourea is unstable in water and suffered both biotic and abiotic decomposition to eventually give NH 3 ,N 2 O, and CO 2 . However, we were unable to detect urea. Based on products distribution and reaction stoichiometry, we suggested that degradation of NQ, O 2 NNC(NH 2 ) 2 , might involve initial enzymatic hydroxylation of the imine, CN bond, leading first to the formation of the unstable α-hydroxynitroamine intermediate, O 2 NNHC(OH)-(NH 2 ) 2 , whose decomposition in water should lead to the formation of NH 3 ,N 2 O, and CO 2 . NQ biodegradation was induced by nitroguanidine itself, L-arginine, and creatinine, all being iminic compounds containing a guanidine group. This first description of NQ mineralization by a bacterial isolate demonstrates the potential for efficient microbial remediation of NQ in soil.