Spatial variation in microbial community structure, richness, and diversity in an alluvial aquifer.

Relatively little is known regarding the spatial variability of microbial communities in aquifers where well fouling is an issue. In this study 2 water wells were installed in an alluvial aquifer located adjacent to the North Saskatchewan River and an associated piezometer network developed to facilitate the study of microbial community structure, richness, and diversity. Carbon utilization data analysis revealed reduced microbial activity in waters collected close to the wells. Functional PCR and quantitative PCR analysis indicated spatial variability in the potential for iron-, sulphate-, and nitrate-reducing activity at all locations in the aquifer. Denaturing gradient gel electrophoresis analysis of aquifer water samples using principal components analyses indicated that the microbial community composition was spatially variable, and denaturing gradient gel electrophoresis sequence analysis revealed that bacteria belonging to the genera Acidovorax , Rhodobacter , and Sulfuricurvum were common throughout the aquifer. Shannon's richness (H') and Pielou's evenness (J') indices revealed a varied microbial diversity (H' = 1.488-2.274) and an even distribution of microbial communities within the aquifer (J' = 0.811-0.917). Overall, these analyses revealed that the aquifer's microbial community varied spatially in terms of composition, richness, and metabolic activity. Such information may facilitate the diagnosis, prevention, and management of fouling.

Transient response of microbial communities in a water well field to application of an impressed current.

Deterioration of water wells due to clogging and corrosion over time is a common problem where solutions may be costly and ineffective. Pilot studies have suggested that impressed current or cathodic protection may be used to reduce microbially-induced declines in water well performance. Two water wells in an alluvial aquifer close to the North Saskatchewan River were selected to study the response of subsurface microbial communities to the application of an impressed current as an anti-fouling technology. The treated well was exposed to an impressed current while the untreated well was used as a reference site. Biofilms grown on in situ coupons under the influence of the impressed current were significantly (p < 0.05) thicker (mean thickness = 67.3 µm) when compared to the biofilms (mean thickness = 19.3 µm) grown outside the electric field. Quantitative PCR analyses showed significantly (p < 0.05) higher numbers of total bacteria, iron- and nitrate-reducers in the electrified zone. Molecular analysis revealed that the predominant bacteria present in biofilms grown under the influence of the impressed current belonged to Rhodobacter spp., Sediminibacterium spp. and Geobacter spp. In addition to favouring the growth of biofilms, direct microscopic and ICP-AES analyses revealed that the impressed current also caused the deposition of iron and manganese on, and in the vicinity of, the well screen. Together, these factors contributed to rapid clogging leading to reduced specific pumping capacities of the treated well. The study revealed that the impressed current system was not effective as an anti-fouling technology but actually promoted both microbial growth and physical clogging in this aquifer.

Effect of pumping on the spatio-temporal distribution of microbial communities in a water well field.

A water well field adjacent to the North Saskatchewan River (City of North Battleford, Saskatchewan, Canada) with a history of rapid deterioration of both well water quality and yield was selected to study the spatial and temporal distribution of subsurface microbial communities and their response to water pumping. A range of conventional cultural, microscopic and molecular techniques, including confocal laser scanning microscopy (CLSM), Biolog, qPCR and Denaturing Gradient Gel Electrophoresis (DGGE), was used during this study. Redox data and water and sediment chemistry showed that the aquifer was anoxic and harbored substantial amounts of Fe and Mn. CLSM analyses of incubated coupons indicated extensive biofilm growth in the zone immediately surrounding the well and was coincident with reduced water well yield. PCR screening and qPCR analyses showed that the potential for iron- and sulfate-reducing activity increased with proximity to the well. Bacterial communities inhabiting the zone closest to the well showed the greatest changes and differences in metabolic activities and composition as revealed by PCA (Principal Components Analysis) of the Biolog and DGGE data. The sequence analysis of all the samples revealed that Sulfuricurvum spp., Methylobacter spp., Geobacter spp. and Rhodobacter spp. were most commonly detected in this aquifer. Overall the findings demonstrated that the microbial numbers, metabolic activities and the community composition changed in response to water pumping but effects did not extend beyond 1-2m zone from the well.