RESUMEN
Antimony, extensively used in energy applications, poses toxicity and contamination concerns, especially in anaerobic environments where its impact on microbial activity is poorly understood. Emerging remedies, like biochar, show promise in soil and water treatment. This study investigates biochar's influence on methanogenic activity under Sb(V) and Sb(III) stress using anaerobic sludge as inoculum and lactate as the carbon source. Sb(III) and Sb(V) were introduced at varied concentrations (5-80 mg/L), with or without biochar, monitoring changes in biogas production, pH, Sb, and lactate levels over time. Experiments with Sb(V) also involved calculating mass balance and electron distribution. Results showcased the following significant enhancements: biochar notably improved COD removal and biogas production in Sb(III) spiked conditions, up to 5-fold and 2-fold increases, respectively. Sb(III) removal reached up to 99% with biochar, while in high Sb(V) concentrations, biochar reduced the adverse effect on biogas production by 96%. Adsorption capacities favored biomass (60.96 mg Sb(III)/gVSS, and 22.4 mg Sb(V)/gVSS) over biochar (3.33 mg Sb(III)/g, and 1.61 mg Sb(V)/g) for both Sb species. This study underscores biochar's potential to mitigate metalloid impact on methanogenic activity while aiding Sb removal from liquid phase, suggesting promising implications for remediation and methane production enhancement strategies.
Asunto(s)
Antimonio , Carbón Orgánico , Euryarchaeota , Biocombustibles , Ácido Láctico , MetanoRESUMEN
This study investigates the potential of humic substances (HS) and graphene oxide (GO), as extracellular electron acceptors (EEA) for nitrification, aiming to explore alternatives to sustain this process in wastewater treatment systems. Experimental results demonstrate the conversion of ammonium to nitrate (up to 87 % of conversion) coupled to the reduction of either HS or GO by anaerobic consortia. Electron balance confirmed the contribution of HS and GO to ammonium oxidation. Tracer analysis in incubations performed with 15NH4+ demonstrated 15NO3- as the main product with a minor fraction ending as 29N2. Phylogenetic analysis identified Firmicutes, Euryarchaeota, and Chloroflexi as the microbial lineages potentially involved in anoxic nitrification linked to HS reduction. This study introduces a new avenue for research in which carbon-based materials with electron-accepting capacity may support the anoxic oxidation of ammonium, for instance in bioelectrochemical systems in which carbon-based anodes could support this novel process.
Asunto(s)
Carbono , Nitrificación , Carbono/química , Electrones , Grafito/química , Filogenia , Oxidación-Reducción , Compuestos de Amonio/metabolismo , Anaerobiosis , Nitratos/metabolismo , Bacterias/metabolismoRESUMEN
Coastal sediments play a central role in regulating the amount of land-derived reactive nitrogen (Nr) entering the ocean, and their importance becomes crucial in vulnerable ecosystems threatened by anthropogenic activities. Sedimentary denitrification has been identified as the main sink of Nr in marine environments, while anaerobic ammonium oxidation with nitrite (anammox) has also been pointed out as a key player in controlling the nitrogen pool in these locations. Collected evidence in the present work indicates that the microbial biota in coastal sediments from Baja California (northwestern Mexico) has the potential to drive anaerobic ammonium oxidation linked to Mn(IV) reduction (manganammox). Unamended sediment showed ammonification, but addition of vernadite (δMnO2 with nano-crystal size â¼15 Å) as terminal electron acceptor fueled simultaneous ammonium oxidation (up to â¼400 µM of ammonium removed) and production of Mn(II) with a ratio ∆[Mn(II)]/∆[NH4+] of 1.8, which is very close to the stoichiometric value of manganammox (1.5). Additional incubations spiked with external ammonium also showed concomitant ammonium oxidation and Mn(II) production, accounting for â¼30 % of the oxidized ammonium. Tracer analysis revealed that the nitrogen loss associated with manganammox was 4.2 ± 0.4 µg 30N2/g-day, which is 17-fold higher than that related to the feammox process (anaerobic ammonium oxidation linked to Fe(III) reduction, 0.24 ± 0.02 µg 30N2/g-day). Taxonomic characterization based on 16S rRNA gene sequencing revealed the existence of several clades belonging to Desulfobacterota as potential microorganisms catalyzing the manganammox process. These findings suggest that manganammox has the potential to be an additional Nr sink in coastal environments, whose contribution to total Nr losses remains to be evaluated.
Asunto(s)
Compuestos de Amonio , Nitrógeno , Nitrógeno/análisis , Anaerobiosis , Sedimentos Geológicos/química , Compuestos Férricos , Ecosistema , ARN Ribosómico 16S/genética , México , Óxidos , Oxidación-Reducción , DesnitrificaciónRESUMEN
Se obtuvieron los valores reales de los hematócritos capilares a las 24 y 48 horas de vida, em una muestra hospitalária, representativa de nuestra población; los resultados fueron 58 ñ 7% (XñIDS) para ambas. Se relacionaron, estos resultados con el hematócrito inicial (50 ñ 5%), que se había informado en la primera parte de la serie. La relación entre los hematócritos capilares y el inicial fue muy buena, y entre los capilares mismos fue mejor aún. Esta relación persistió al dividir la muestra en cuatro grupos según: el Apgar, el llanto (si se presentó antes o depués del pinzamiento) y las características del líquido amniótico. Lo que demuestra que los hematócritos capilares, son tan confiables como el hematócrito venoso, central o periférico, (en este caso el de sangre de cordón umbilical), contrario a lo comunicado previamente en la literatura. También se analizó la presencia de circular de cordón, cuando esto fue posible